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International Space Station News

Sunday, July 26, 2009

Saturnian Moon Shows Evidence of Ammonia

Saturn's moon Enceladus, seen by the Cassini spacecraftData collected during two close flybys of Saturn's moon Enceladus by NASA's Cassini spacecraft add more fuel to the fire about the Saturnian ice world containing sub-surface liquid water. The data collected by Cassini's Ion and Neutral Mass Spectrometer during Enceladus flybys in July and Oct. 2008, were released in the July 23 issue of the journal Nature. "When Cassini flew through the plume erupting from Enceladus on October 8 of last year, our spectrometer was able to sniff out many complex chemicals, including organic ones, in the vapor and icy particles," said Hunter Waite, the Cassini Ion and Neutral Mass Spectrometer Lead Scientist from the Southwest Research Institute in San Antonio, Texas. "One of the chemicals definitively identified was ammonia."

On Earth, the presence of ammonia means the potential for sparkling clean floors and counter tops. In space, the presence of ammonia provides strong evidence for the existence of at least some liquid water.

How could ammonia equate to liquid water inside an ice-covered moon in one of the chillier neighborhoods of our solar system? As many a homeowner interested in keeping their abodes spick and span know, ammonia promptly dissolves in water. But what many people do not realize is that ammonia acts as antifreeze, keeping water liquid at lower temperatures than would otherwise be possible. With the presence of ammonia, water can exist in a liquid state to temperatures as low as 176 degrees Kelvin (-143 degrees Fahrenheit).

"Given that temperatures in excess of 180 Kelvin (-136 degrees Fahrenheit) have been measured near the fractures on Enceladus where the jets emanate, we think we have an excellent argument for a liquid water interior," said Waite.

Cassini discovered water vapor and particles spewing from Enceladus in 2005. Since then, scientists have been trying to determine if the plume originates from a liquid source inside the moon or is due to other causes.

"Ammonia is sort of a holy grail for icy volcanism," said William McKinnon, a scientist from Washington University in Saint Louis, Missouri. "This is the first time we've found it for sure on an icy satellite of a giant planet. It is probably everywhere in the Saturn system."

Just how much water is contained within Enceladus' icy interior is still up for debate. So far, Cassini has made five flybys of Enceladus, one of the chief targets for Cassini's extended mission. Two close flybys are scheduled for November of this year, and two more close flybys are scheduled for April and May of 2010. Data collected during these future flybys may help settle the debate.

"Where liquid water and organics exist, is there life?" asked Jonathan Lunine a Cassini scientist from the University of Arizona, Tucson. "Such is the case for Earth; what was found on Enceladus bolsters this moon's promise for containing potential habitable environments." The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Cassini orbiter was designed, developed and assembled at JPL. JPL manages the mission for the Science Mission Directorate at NASA Headquarters in Washington.

More information about the Cassini mission is available at http://www.nasa.gov/cassini or http://saturn.jpl.nasa.gov .

A 21st Century-Style Return to the Moon

The three Apollo 11 crew men await pickup by a helicopter from the USS Hornet, prime recovery ship for the historic Apollo 11 lunar landing missionMembers of the 920th Rescue Wing work on a mockup Orion crew exploration vehicle off the coast of Port Canaveral, Fla.It was an extraordinary feat when Apollo engineers designed a spacecraft to go somewhere no human had ever gone before. Especially when that place was the moon - 240,000 miles from Earth. Now forty years after the first moon landing, NASA has turned its attention back to lunar missions, this time planning to stay longer.

The spacecraft to carry future explorers to the moon, the Orion crew exploration vehicle, looks very similar to the Apollo spacecraft. The crew module borrows the familiar conical shape with a curved heatshield, which has proven to be the optimal shape for missions returning from the moon.

Additionally, Orion and Apollo both use the same heat-resistant thermal material, called AVCOAT, to shield the capsules from heat generated by the 25,000 mile-per-hour atmosphere re-entry from missions to the moon.

However, the Orion crew module is one-third larger than the Apollo command module and the inside will be different. Engineers will incorporate advances in technology into the interior and since the plan for missions to the moon is different, different types of systems are being designed also.

When Apollo astronauts visited the moon, they only stayed for a few days at a time, three astronauts traveled to lunar orbit on Apollo, and then only two descended to the moon’s surface.

When America returns to the moon, four astronauts will ride in Orion to lunar orbit and then all of them will move into the Altair lunar lander to go explore the moon. Orion will operate on its own in lunar orbit, standing by for the return trip to Earth.

Orion will start out supporting week-long missions and then will be able to support up to 210-day missions when astronauts eventually live and work at outposts on the moon.

Being able to operate autonomously in lunar orbit will be a key factor in Orion being able to support longer missions. Its systems will operate automatically, with Mission Control watching from Earth, while the crew explores the moon.

By going to the moon for extended periods of time, astronauts will search for resources and learn how to work safely in a harsh environment -- stepping stones to future exploration. The moon also offers many clues about the time when the planets were formed.

To support longer missions, Orion also will have larger tanks to carry the fuel for course adjustments during the trip and will use advanced solar array technology to collect sunlight for conversion into electricity. Apollo used fuel cell technology (as does the space shuttle), which requires oxygen and hydrogen be carried along for the ride. Using solar arrays saves weight that can be used to enhance safety and launch more cargo.

Orion will have more power, too. It will hold six batteries for power storage and will use a 120V DC power distribution system, compared to Apollo’s three-battery storage and 28V DC system.

Orion’s crew module will feature a streamlined glass cockpit interface for the astronauts, with about ten times fewer switches than Apollo’s roughly 450 switches.

Tuesday, July 21, 2009

STS-127 Crew Completes Second Spacewalk

Spacewalkers Dave Wolf and Tom Marshburn wrapped up a six hour, 53 minute spacewalk at 6:20 p.m. EDT.

Wolf and Marshburn completed most of their planned tasks, deferring a video camera setup to a future spacewalk. Wolf removed three hardware spares – a Ku-Band Space-to-Ground Antenna, a Pump Module and a Linear Drive Unit, from the Integrated Cargo Carrier – Vertical Light Deployable (ICC-VLD). With each spare in hand, Wolf rode the space station robotic arm from the ICC to the Port 3 external stowage platform (ESP-3), where he and Marshburn attached them for long-term storage. Julie Payette and Doug Hurley operated the robotic arm. Marshburn mounted a grapple bar onto an ammonia tank assembly so that the STS-128 space shuttle mission in August can move the tank by robotic arm. Marshburn also attached two insulation sleeves for the Space Station to International Space Shuttle Power Transfer System.

This was the second of five STS-127 spacewalks, the 127th in support of International Space Station assembly and maintenance, totaling 792 hours, 31 minutes. It was the 215th American spacewalk in history. It was Wolf’s sixth spacewalk, totaling 38 hours, 44 minutes and placing him 19th on the all-time list. It was Marshburn’s first excursion.

NASA Television airs a Mission Status briefing at 8:30 p.m. with STS-127 Lead Flight Director Holly Ridings and STS-127 Lead Extravehicular Activity Officer Kieth Johnson.

Space Shuttle Mission: STS-127


Spacewalker Dave Wolf
Astronauts Conduct Spacewalk on Historic Anniversary

The crews aboard the International Space Station and space shuttle Endeavour honored the legacy of Apollo 11 by conducting a spacewalk on the same day that 40 years ago captured the world’s attention when Neil Armstrong and Buzz Aldrin walked on the Moon for the first time.

Mission specialists Dave Wolf and Tom Marshburn performed a six hour, 53 minute extravehicular excursion to complete a number of station hardware installation tasks.

Exiting from the Quest Airlock at 10:27 a.m., Wolf removed three hardware spares – a Ku-Band Space-to-Ground Antenna, a Pump Module and a Linear Drive Unit, from an Integrated Cargo Carrier. With each spare in hand, Wolf rode the space station robotic arm to the P3 Truss where a stowage platform awaited. There he and Marshburn attached them for long-term storage.

Mission Specialist Julie Payette and Pilot Doug Hurley operated the robotic arm. Marshburn mounted a grapple bar onto an ammonia tank assembly so that the next space shuttle crew of STS-128 can move the tank by robotic arm. Marshburn also attached two insulation sleeves for external power connectors to the Station to Shuttle Power Transfer System. Wolf and Marshburn completed most of the planned tasks, but deferred a video camera installation.

Expedition 20 commander Gennady Padalka and Flight Engineer Frank De Winne replaced components of the Waste Hygiene Compartment toilet in the Destiny laboratory. The system’s dose pump failed Sunday. After Padalka and De Winne replaced the separator pump, control panel and the COT, a container that holds liquid, the system was activated and performed normally.

NASA's 'Mr. Eclipse' Retires but Still Chasing Shadows

The path of the total solar eclipse on July 22, 2009, will sweep across nearly half of Earth, beginning in India and ending in the Pacific Ocean.Have you ever glimpsed the moon's shadow as it passes in front of the sun's disk casting a dark shadow on Earth and revealing the sun's ephemeral outer atmosphere? Have you witnessed Earth's shadow as it slowly sweeps over a full moon, taking successively bigger bites until the entire disk is red-tinged and darkly shaded? If so, then you already know the wonderment of chasing celestial shadows.

And if you have ever looked up the "where," "when," and "what type" for an eclipse, you may be familiar with Fred Espenak, better known as "Mr. Eclipse."

American astrophysicist Fred Espenak has had a long and prolific career at NASA's Goddard Space Flight Center in Greenbelt, Md. Since 1978, Espenak has provided eclipse bulletins -- detailed descriptions of eclipse predictions, maps, and weather information for upcoming eclipses -- for NASA as well as inspiration to legions of eclipse aficionados. He also has authored several works on eclipse predictions, including the Fifty Year Canon of Solar Eclipses: 1986-2035 and the Fifty Year Canon of Lunar Eclipses: 1986-2035.

Espenak's passion for astronomy and eclipses began when he was about 7 or 8 years old. "I was visiting my grandparents out in their summer home in Long Island," he recalls. "One of the neighborhood boys had a small telescope. I remember taking a look at the moon through that telescope for the first time. I think I pestered my father for 2 years after that before I got my first telescope. And that just ignited my interest in astronomy."

Since then, Espenak has observed more than 20 eclipses in person. Whether total, partial or annular, each eclipse is as different in character as two siblings, says Espenak. "Each has special features to it," says Espenak.

Eclipses come in two types: solar and lunar. An eclipse of the sun happens when the moon passes directly between Earth and the sun. When the moon's shadow falls on Earth, people within that shadow see part (or all) of the sun's disk covered, or eclipsed, by the moon. During a lunar eclipse, Earth passes between the sun and moon and blocks sunlight from reaching the moon. Because of the geometry of eclipses, whether your see all or part of an eclipse depends on where you are located on Earth.

An eclipse of the sun can be total, partial, or annular. During a total solar eclipse, the moon blocks the sun's entire disk for those standing within the "path of totality," the path of the moon's dark inner shadow, or umbra. Observers in the moon's faint outer shadow (penumbra) will witness partial coverage of the sun.

An annular eclipse happens when the tip of the moon's umbra doesn't quite reach Earth. For observers situated beneath the umbral shadow, the moon will look slightly smaller than the sun, with a thin ring, or annulus, of sunlight remaining visible during the eclipse. An annular eclipse is also called a hybrid eclipse.

Which kind of eclipse is Espenak's favorite? "I like solar eclipses and lunar eclipses for two different reasons."

"Nothing can compare to a total solar eclipse," he says. "But you're putting all your eggs in one basket when you go on a solar eclipse expedition because you've only got usually two, or three, or four precious minutes when you've got that opportunity to see the sun's corona. All the equipment has to be working perfectly. The weather has to cooperate. You've got to be at the right place at the right time. It is very stressful."

"A lunar eclipse is a very beautiful event, but it doesn't have that excitement of a solar eclipse, where you've just got those two minutes. The total phase usually lasts an hour or more, so it's much more of a leisurely event. You can sit back, watch, and relax." Lunar eclipses also happen more frequently than solar eclipses.

Though he recently retired from NASA, don't expect Espenak's passion for chasing shadows to wane any time soon. "I think the beauty of the eclipses is something that anybody can appreciate," he says. "What I usually tell people is if they ever have the opportunity to see a total solar eclipse, or if they're on a vacation and a total solar eclipse just happens to be taking place nearby, get into the path of the total eclipse," says Espenak.

His next expedition will take him to the Pacific Ocean to observe a total solar eclipse on July 22. The path of totality begins in India, crosses through Nepal, Bangladesh, Bhutan, Myanmar, and China. The duration of totality will last 6 minutes, 39 seconds. A partial eclipse will be visible in parts of Asia, Indonesia, and the Pacific Ocean.

Related Links:

For more information about the July 22 eclipse, visit www.nasa.gov/eclipse or http://eclipse.gsfc.nasa.gov

NASA And Google Launch Virtual Exploration of The Moon

Two astronauts placed an American flag on the Moon’s surface during a television broadcast of the event.Forty years ago on July 20, 1969, the world watched as the crew of Apollo 11 took the first steps on the surface of the moon.

To celebrate this historic occasion, NASA and Google announced the launch of the Moon in Google Earth, an interactive, 3D atlas of the moon, viewable with Google Earth 5.0.

The announcement was made during a press conference at the Newseum in Washington, featuring remarks by Apollo 11 astronaut Buzz Aldrin; Alan Eustace, a Google senior vice president; Andrew Chaikin, author and space historian; and Anousheh Ansari, the first female space tourist.

With the Moon in Google Earth, users can explore a virtual moonscape, follow guided tours from astronauts Buzz Aldrin and Jack Schmidt, view high-resolution "street view" style panoramic images and see previously unreleased footage captured from the lunar surface.

Whether rediscovering iconic moments from the history of lunar exploration, or learning about them for the first time, the Moon in Google Earth enables users to better understand the moon and mankind's relationship to it using an immersive, 3D experience.

The result of a close collaboration with NASA, the Moon in Google Earth showcases current and historic content about the moon. All NASA data sets used in the Moon in Google Earth are included on a non-exclusive basis.

"Today's announcement builds on the ongoing relationship with Google that Ames Research Center initiated in November 2006, when we signed a Space Act Agreement to foster collaboration with our Silicon Valley neighbor," said S. Pete Worden, director of NASA's Ames Research Center at Moffett Field, Calif. "We're excited to be a part of this latest chapter in Google's efforts to bring virtual exploration of the moon to anyone with a computer."

In addition to satellite imagery and topographical data, the following layers can be explored:

• Featured Satellite Imagery – Explore overlaid satellite imagery and detailed descriptions of selected areas on the moon from Arizona State University's "Lunar Image of the Week."
• Spacecraft Imagery - View selected imagery captured by the Apollo Metric Camera, and the Clementine and the Lunar Orbiter spacecraft
• Apollo Missions – Travel back to the Apollo era and discover the landing sites of Apollo missions 11-17. Explore "street view" style panoramic images, watch previously unreleased footage from spacecraft films and read about the places astronauts saw on their trips to the moon.
• Guided Tours – Take a narrated tour of the moon with Apollo astronauts Buzz Aldrin (Apollo 11) and Jack Schmitt (Apollo 17)
• Historic Maps – Explore Apollo-era geologic and topographic maps of the moon.
• Human Artifacts – Learn about the various types of exploratory equipment that humans have left on the moon and where those objects can be found today.

To view the Moon in Google Earth, open Google Earth 5.0 and switch modes from "Earth" to "Moon" on the top toolbar. To learn more about Moon in Google Earth, visit: earth.google.com/moon.

The Moon in Google Earth was jointly developed by Google, the NASA Ames Intelligent Robotics Group, and the SETI Institute as part of NASA's Planetary Content project.

Data sets for the Moon in Google Earth were developed with the assistance of the United States Geologic Survey (USGS), Arizona State University and the Lunar and Planetary Institute. The Japan Aerospace Exploration Agency provided terrain data from the Kaguya orbiter. The initial release does not contain any imagery from the Lunar Reconnaissance Orbiter.

The NASA Lunar Mapping and Modeling Project provided a high-resolution base map and 3D terrain model covering a portion of the nearside lunar equatorial region, which was developed using new digital scans of the Apollo 15 Metric Camera (orbit 33) images made by Arizona State University and NASA's Johnson Space Center in Houston. he NASA Exploration Systems Mission Directorate Analogs Program provided content for the Apollo 17 tour.

For more information about NASA's plans to return to the moon and explore beyond visit exploration.nasa.gov.

New NASA Images Indicate Object Hits Jupiter

This image shows a large impact on Jupiter's south polar region captured on July 20, 2009Scientists have found evidence that another object has bombarded Jupiter, exactly 15 years after the first impacts by the comet Shoemaker-Levy 9.

Following up on a tip by an amateur astronomer, Anthony Wesley of Australia, that a new dark "scar" had suddenly appeared on Jupiter, this morning between 3 and 9 a.m. PDT (6 a.m. and noon EDT) scientists at NASA's Jet Propulsion Laboratory in Pasadena, Calif., using NASA's Infrared Telescope Facility at the summit of Mauna Kea, Hawaii, gathered evidence indicating an impact.

New infrared images show the likely impact point was near the south polar region, with a visibly dark "scar" and bright upwelling particles in the upper atmosphere detected in near-infrared wavelengths, and a warming of the upper troposphere with possible extra emission from ammonia gas detected at mid-infrared wavelengths.

"We were extremely lucky to be seeing Jupiter at exactly the right time, the right hour, the right side of Jupiter to witness the event. We couldn't have planned it better," said Glenn Orton, a scientist at JPL.

Orton and his team of astronomers kicked into gear early in the morning and haven't stopped tracking the planet. They are downloading data now and are working to get additional observing time on this and other telescopes.

This image was taken at 1.65 microns, a wavelength sensitive to sunlight reflected from high in Jupiter's atmosphere, and it shows both the bright center of the scar (bottom left) and the debris to its northwest (upper left).

"It could be the impact of a comet, but we don't know for sure yet," said Orton. "It's been a whirlwind of a day, and this on the anniversary of the Shoemaker-Levy 9 and Apollo anniversaries is amazing."

Shoemaker-Levy 9 was a comet that had been seen to break into many pieces before the pieces hit Jupiter in 1994.

Leigh Fletcher, a NASA postdoctoral fellow at JPL who worked with Orton during these latest observations said, "Given the rarity of these events, it's extremely exciting to be involved in these observations. These are the most exciting observations I've seen in my five years of observing the outer planets!"

The observations were made possible in large measure by the extraordinary efforts of the Infrared Telescope Facility staff, including telescope operator William Golisch, who adroitly moved three instruments in and out of the field during the short time the scar was visible on the planet, providing the wide wavelength coverage.

Monday, July 20, 2009

Mystery Source of Solar Wind Heating Identified

The solar wind, shown here in a plot of data from the Ulysses spacecraft, flows away from the sun at a million miles per hour and is heated by a turbulent cascade.The solar wind is hotter than it should be, and for decades researchers have puzzled over the unknown source of energy that heats it. In a paper published in the June 12 issue of Physical Review Letters, NASA scientists say they may have found the answer.

"The energy source is turbulence," says co-author Melvyn Goldstein, chief of the Geospace Physics Laboratory at NASA's Goddard Space Flight Center, Greenbelt, Md. "The sun heats the solar wind by stirring it up."

It's a bit like stirring your coffee--in reverse. When you stir your morning cup of Joe, the coffee cools off. But when the sun stirs the solar wind, the solar wind heats up.

The basic concept introduced by physicist Lewis Richardson in 1920.A true cascade of water and turbulence at the Iguazu Falls in Argentina.Jupiter's swirling Great Red Spot surrounded by turbulent swirls and eddies.Consider the coffee. When you stir it with a spoon, the stirring produces swirls and vortices in the liquid. The vortices fragment into smaller and smaller eddies until, at the smallest scales, the motions dissipate and the energy turns into heat. Because energy cascades down from the large swirls to the smaller ones, the process is called a turbulent cascade.

Theoretically, the turbulent cascade should heat the coffee. Real coffee cools off, however, because the act of stirring brings warm coffee from the depths of the cup into contact with cooler air above. Cool air absorbs the heat—the heat the coffee had to begin with plus the heat you added by stirring—and you can take a sip without scalding yourself.

But there is no cool air in space, and therein lies the difference between coffee and solar wind.

The sun stirs the solar wind with fast streams of gas that pour out of holes in the sun's atmosphere. Essentially, the solar wind stirs itself. The stirring produces swirls and eddies; larger eddies break into smaller ones, producing a cascade of energy that eventually dissipates as heat. The temperature shoots up and there is no cool air to stop it.

"We've suspected for years that turbulence heats the solar wind," says Fouad Sahraoui, lead author of the paper and a visiting NASA Fellow from the Centre National de la Recherche Scientifique (CNRS) in France. "Now we're getting detailed measurements of the process in action."

The key data came from a quartet of European spacecraft collectively known as Cluster, launched in 2000 to study the giant bubble of magnetism that surrounds Earth. The magnetosphere protects our planet from solar wind and cosmic rays. It contains the Van Allen radiation belts, auroras, and giant electrical "ring currents" of staggering power. Cluster spends much of its time inside the magnetosphere, where the spacecraft can study the wide variety of phenomena at work there.

One day in March 2006, the four spacecraft took a brief excursion outside the bubble into the solar wind. For three hours, their sensors made rapid-fire measurements of electromagnetic waves and turbulent eddies in the million-kilometer-per-hour gas flowing past them.

"That was when we made the discovery," says Goldstein. "Turbulent energy was cascading from large scale structures around 1,000,000 kilometers (621,400 miles) in size all the way down to structures as small as 3 kilometers (1.8 miles). At the small end of the cascade, energy was absorbed by electrons in the solar wind."

Sahraoui and Goldstein would like to confirm their findings and flesh out the details by sending Cluster back into the solar wind for more than "three lucky hours." But the basic result seems solid enough: Turbulent heating boosts the temperature of the solar wind near Earth from tens of thousands of degrees (the value theoreticians expect) to hundreds of thousands or more.

Goldstein says such turbulent heating probably happens in many other astrophysical situations, from stellar winds to planetary magnetospheres to black holes. There's even a down-to-Earth application: nuclear fusion reactors. Turbulence inside experimental fusion chambers can produce instabilities that destroy the confinement of the fusion plasma.

"The solar wind is a natural laboratory for understanding this physics," says Sahraoui, "and we are planning more observations to see how common the phenomenon might be."

Related Links:

Cluster – home page
http://sci.esa.int/science-e/www/area/index.cfm?fareaid=8

Cluster's insight into space turbulence – press release
http://sci.esa.int/science-e/www/object/index.cfm?fobjectid=44480

The Solar Wind – a tutorial
http://solarscience.msfc.nasa.gov/SolarWind.shtml

Evidence of a Cascade and Dissipation of Solar-Wind Turbulence at the Electron Gyroscale, F. Sahraoui et al, Phys. Rev. Lett. 102, 231102 (2009)
http://scitation.aip.org/getabs/servlet/GetabsServlet?prog=normal&id=PRLTAO000102000023231102000001&idtype=cvips&gifs=yes

Waste and Hygiene Compartment Status

Aboard the International Space Station, astronauts Mike Barratt and Frank De Winne will be replacing parts of the U.S. Destiny laboratory’s Waste and Hygiene Compartment, or WHC. The parts likely were contaminated earlier today when the system’s dose pump failed after running for about 15 minutes. The pump introduces the correct amount of chemicals into the system to help separate liquids from solid waste. About six liters of pre-treated water may have flowed into the pump separator and other areas it does not belong, flooding the separator.

Space Shuttle Mission: STS-127


Integrated Cargo Carrier
Crews Tackle Robotics, Prepare for Monday Spacewalk

The Space Shuttle Endeavour and International Space Station crews were successful in their robotic arm tasks today, but encountered a problem with one of the bathrooms on the station.

Robotic arm operators aboard Endeavour and the station installed the Integrated Cargo Carrier – Vertical Light Deployable, or ICC-VLD --- a cargo pallet--- on the port side of the space station’s mobile base system. Station arm operators Julie Payette and Tim Kopra finished the move at 12:55 p.m. EDT.

The pallet contains three hardware spares that spacewalkers Dave Wolf and Tom Marshburn will move to a stowage platform on the outside of the Port 3 truss during Monday’s spacewalk.

The Kibo robotic arm was commanded through a series of calibrations in preparation for later use in the mission, when Japan Aerospace Exploration Agency payloads will be transferred from the Exposed Section, another platform where the experiments are temporarily mounted, to the newly installed Exposed Facility for operation. The Exposed Facility was installed on the aft end of Kibo Saturday.

Wolf and Marshburn spent the remainder of their day preparing special tools, reviewing procedures and beginning their campout for the second spacewalk, which is set to start Monday at 11:28 a.m.

Meanwhile, station flight controllers and crew members spent part of the day troubleshooting a problem with the Waste and Hygiene Compartment, or WHC, the toilet in the U.S. Destiny module. The system’s dose pump failed after running for about 15 minutes Sunday. The pump introduces the correct amount of chemicals into the system to help separate liquids from solid waste. Expedition 20 flight engineers Mike Barratt and Frank De Winne began work on the toilet to replace parts that likely were contaminated.

The WHC is one of two toilet systems aboard the space station. Temporarily, the six station crew members will use the facilities in the Russian Zvezda module while the seven Endeavour astronauts will use the shuttle Waste Compartment System, or WCS, that is located in Endeavour’s middeck.

The temporary shutdown of the U.S. toilet on the station will not impact joint docked operations.

› Read more

STS-127 Additional Resources
› Mission Press Kit (6.9 Mb PDF)
› Mission Summary (429 Kb PDF)
› Meet the STS-127 Crew

Apollo 11 40th Anniversary: Celebrating the 'Giant Leap'

Images from Apollo 11. Top left: Apollo 11 commander Buzz Aldrin and Flight Director Gene Kranz at a

› LRO Sees Apollo Landing Sites | › Flickr: Anniversary Events→ | › Restored Moonwalk Video | › Real-Time Mission Audio › Onboard Voice Recordings | › Interactive: Explore the Landing Site and Eagle | › More Features

Dryden Flight Research Center's Contributions to Apollo's Moon Landing Success

The late Joseph Algranti maneuvers the first Lunar Landing Research Vehicle, or LLRV, over Edwards Air Force Base' South Base ramp area on Aug. 19, 1966.NASA's Flight Research Center at Edwards Air Force Base (renamed the Dryden Flight Research Center), generally thought of as an aeronautical flight-test facility in the 1960s, made a number of contributions to the NASA space program during that era as well.

For example, researchers explored the concept of paraglider landings for a space vehicle and the use of wingless spacecraft that could glide to precise landings, but it was the X-15 hypersonic research program and the Lunar Landing Research Vehicle that had the most direct impact on the Apollo missions to the Moon.

The North American Aviation X-15 rocket planes--designed to explore the problems of atmospheric and space flight at supersonic and hypersonic speeds--served as flying laboratories, carrying scientific experiments above the reaches of the atmosphere. Many research results from the X-15 program at Dryden Flight Research Center contributed directly to the success of the Apollo lunar missions, now being celebrated on the 40th anniversary of the first moon landing on July 20, 1969. North American – later North American Rockwell, then Rockwell International – served as prime contractor for both the X-15 and Apollo Command/Service Module spacecraft.

Designers of the Apollo CSM drew upon experience from the X-15 program, and even used the X-15 as a test bed for new materials. Advanced titanium and nickel-steel alloys developed for the X-15 were used in the Apollo and later spacecraft designs. The discovery of localized hot spots on the X-15, for example, led to development of a bi-metallic 'floating retainer' concept to dissipate stresses in the X-15's windshield. This technology was subsequently applied to the Apollo and space shuttle orbiter windshields.

The X-15's performance allowed researchers to accurately simulate the aerodynamic heating conditions that the Apollo Saturn rocket would face, and allowed full recovery of test equipment, calibration of results, and repeated testing where necessary. In 1967, technicians applied samples of cryogenic insulation--designed for use on the Apollo Saturn V second stage--to the X-15's speed brakes to test the material's adhesive characteristics and response to high temperatures.

X-15 re-entry experience and heat-transfer data were also valuable, and led to design of a computerized mathematical model for aerodynamic heating that was used in the initial Apollo design study. Lessons learned from X-15 turbulent heat-transfer studies contributed to the design of the Apollo CSM because designers found that they could build lighter-weight vehicles using less thermal protection than was previously thought possible.

Following the challenge by president John F. Kennedy in 1962 to land on the moon, two groups began working on a way to prepare astronauts for the critical descent and landing on the moon. The problems facing them were considerable: how to build a free-flying simulator that could negate 5/6ths of the Earth's gravity while entirely eliminating the effects of the atmosphere, since the moon had no atmosphere and only 1/6th of Earth's gravity.

Ideas for this unique type of flying machine had begun circulating at Dryden Flight Research Center, a year earlier. Center engineers initially didn't know that Bell Aircraft Company, later Bell Aerosystems, was also working on the task, but by the end of the year, the center had awarded a study contract to Bell. Bell was the only firm in the United States that had significant experience developing vertical takeoff aircraft using jet lift for takeoff and landing. After winning a contract from the center to design and build the machines in 1963, Bell delivered two Lunar Landing Research Vehicles or LLRVs--often called 'flying bedsteads' due to their ungainly appearance--to the Flight Research Center in 1964 for flight testing and development.

The LLRV had a jet engine hung vertically in the middle of the frame, fixed inside two gimbals, allowing the vehicle itself to rotate as much as 40 degrees in any direction while the jet remained vertically aligned. A series of hydrogen peroxide thrusters, eight around the frame's center and four at each corner, provided lunar simulation thrust that the pilot controlled.

Three analog computers took data on side forces and vehicle weight and produced just enough jet thrust so that, in lunar simulation, the LLRV descended as though in lunar gravity. Any gusts of wind were cancelled when the computers sensed them and fired thrusters to automatically cancel the wind. There were no mechanical links between the pilot and the engine or thrusters: everything was sent to the computers that, in turn, commanded the thrust desired.

During flight tests, a pilot directed the LLRV to climb about 300 feet, initiated lunar simulation mode, and then had less than eight minutes to complete a safe descent. Research flying over the next two-and-half years yielded a configuration suitable for astronaut training, and Bell subsequently built three similar craft--Lunar Landing Training Vehicles--that were sent to the Manned Spaceflight Center in Houston, now the Johnson Space Center. One of the LLRVs at the Flight Research Center was also sent to Houston for the training.

Apollo 11 commander Neil Armstrong recalled later that his landing on the moon on July 20, 1969 was a familiar job because of the LLTV’s authenticity.

As a side note, today's aircraft with fly-by-wire digital electronic control systems trace their lineage to the LLRV and its analog computers, and to the engineers who worked on that project. They cut their teeth on computer-controlled flight systems with the LLRV, allowing them the confidence to modify an F-8 jet fighter into the first aircraft with pure digital fly-by-wire electronic controls.

Partially restored by a movie company in the late 1990s, one of the two original Lunar Landing Research Vehicles remains on sheltered display today at NASA Dryden.

Friday, July 17, 2009

Crew Inspects Shuttle, Prepares for Docking

Astronauts aboard Space Shuttle Endeavour spent their first full day in space conducting a routine inspection of their thermal protection system ahead of docking Friday.

While inspections take place to ensure Endeavour’s wing leading edge panels and nosecap are in good shape, imagery experts will continue to assess the overall health of the shuttle’s thermal protection system. The early review indicates only a few minor dings in some tiles is present in video due to some unexpected losses of small foam pieces from the external tank.

Endeavour’s crew also checked out spacesuits that will be used during the five spacewalks planned during the docked phase of the mission. In preparation for docking, the crew tested rendezvous equipment, installed an orbiter docking system “centerline” camera and extended the docking ring atop the docking system before heading for its eight hour sleep period beginning about 9 p.m. EDT.

Space Shuttle Mission: STS-127



S127-E-005141: Astronaut Dave Wolf
Crew Completes First Full Day in Space

En route to the International Space Station, astronauts aboard space shuttle Endeavour spent their first full day in space conducting a routine inspection of their thermal protection system ahead of docking at 1:55 p.m. EDT Friday.

While inspections take place to ensure Endeavour’s wing leading edge panels and nosecap are in good shape, imagery experts will continue to assess the overall health of the shuttle’s Thermal Protection System. The early review indicates only a few minor dings in some tiles is present in video due to some unexpected losses of small foam pieces from the External Tank.

Thursday’s five-hour inspection took place as the seven crew members prepare for the docking to the station as the two spacecraft pass high above the Tasman Sea bridging the gap between southern Australia and New Zealand.

Meanwhile, space shuttle Discovery is being readied at NASA’s Kennedy Space Center for its next mission targeted for mid August. Its launch to the station will deliver supplies and logistics to support the six crew members living and working aboard the complex.

Discovery is targeted to roll to the Vehicle Assembly Building Monday to be mated to its External Tank and Solid Rocket Boosters before being hauled to the launch pad a week later.

NASA Releases Restored Apollo 11 Moonwalk Video

NASA released Thursday newly restored video from the July 20, 1969, live television broadcast of the Apollo 11 moonwalk. The release commemorates the 40th anniversary of the first mission to land astronauts on the moon.

The initial video release, part of a larger Apollo 11 moonwalk restoration project, features 15 key moments from the historic lunar excursion of Neil Armstrong and Buzz Aldrin.

Comparison image showing video still of Neil Armstrong and Buzz Aldrin raising the American flag on the moon, before (left) and after (right) restoration.
Comparison image showing video still of Neil Armstrong and Buzz Aldrin raising the American flag on the moon, before (left) and after (right) restoration.
> Larger image
> Apollo 11 Partial Restoration HD Videos

A team of Apollo-era engineers who helped produce the 1969 live broadcast of the moonwalk acquired the best of the broadcast-format video from a variety of sources for the restoration effort. These included a copy of a tape recorded at NASA's Sydney, Australia, video switching center, where down-linked television from Parkes and Honeysuckle Creek was received for transmission to the U.S.; original broadcast tapes from the CBS News Archive recorded via direct microwave and landline feeds from NASA's Johnson Space Center in Houston; and kinescopes found in film vaults at Johnson that had not been viewed for 36 years.

"The restoration is ongoing and may produce even better video," said Richard Nafzger, an engineer at NASA's Goddard Space Flight Center in Greenbelt, Md., who oversaw television processing at the ground tracking sites during Apollo 11. "The restoration project is scheduled to be completed in September and will provide the public, future historians, and the National Archives with the highest quality video of this historic event."

NASA contracted with Lowry Digital of Burbank, Calif., which specializes in restoring aging Hollywood films and video, to take the highest quality video available from these recordings, select the best for digitization, and significantly enhance the video using the company's proprietary software technology and other restoration techniques.

Under the initial effort, Lowry restored 15 scenes representing the most significant moments of the three and a half hours that Armstrong and Aldrin spent on the lunar surface. NASA released the video Thursday at a news conference at the Newseum in Washington.

On July 20, 1969, as Armstrong made the short step off the ladder of the Lunar Excursion Module onto the powdery lunar surface, a global community of hundreds of millions of people witnessed one of humankind's most remarkable achievements live on television.

The black and white images of Armstrong and Aldrin bounding around the moon were provided by a single small video camera aboard the lunar module. The camera used a non-standard scan format that commercial television could not broadcast.

NASA used a scan converter to optically and electronically adapt these images to a standard U.S. broadcast TV signal. The tracking stations converted the signals and transmitted them using microwave links, Intelsat communications satellites, and AT&T analog landlines to Mission Control in Houston. By the time the images appeared on international television, they were substantially degraded.

At tracking stations in Australia and the United States, engineers recorded data beamed to Earth from the lunar module onto one-inch telemetry tapes. The tapes were recorded as a backup if the live transmission failed or if the Apollo Project needed the data later. Each tape contained 14 tracks of data, including bio-medical, voice, and other information; one channel was reserved for video.

A three-year search for these original telemetry tapes was unsuccessful. A final report on the investigation is expected to be completed in the near future and will be publicly released at that time.

Information and materials for the July 16 media briefing on the Apollo footage can be found here:

http://www.nasa.gov/mission_pages/apollo/40th/apollo11_conference.html

NASA Television will provide an HD video feed of the Apollo footage hourly from 12 - 7 p.m. on July 16 and 17. Each feed is one hour. For NASA TV streaming video, downlink and schedule information, visit:

http://www.nasa.gov/ntv

A copy of the newly restored scenes from the Apollo 11 restoration effort can be found at:

http://www.nasa.gov/multimedia/hd/apollo11.html

NASA's Apollo 40th anniversary Web sites provide easy access to various agency resources and multimedia about the program and the history of human spaceflight, including a gallery of Apollo multimedia features. Visit the site at:

http://www.nasa.gov/apollo40th

Taking Flight To Seek Out The Least Understood Climate Driver

NASA Langley’s B200 aircraftThe High Spectral Resolution Lidar on the B200 captured this measurement of backscatter from aerosols on a flight from the Gulf Coast near Houston back to Oklahoma.Earth’s atmosphereA NASA research plane spent the month of June crisscrossing the southern Great Plains in search of more detailed information on the least understood variable in long-term climate change scenarios.

Tiny suspended particles are nearly everywhere in the atmosphere, and what we see as dust, smoke, soot or haze in the sky scientists study collectively as aerosols. Some aerosols are easy to see with the naked eye, however, they have proven difficult to pin down in terms of their impact on the climate and, in the long run, climate change.

The month of flights – from a Department of Energy Climate Research Facility near Ponca City, Oklahoma – were conducted in part to help evaluate algorithms to be used in the upcoming Glory mission as well as to address NASA’s larger goal of getting a tighter grip on the important but poorly quantified impact of aerosols on climate. A team from NASA’s Langley Research Center flew the center’s B200 plane for the research flights. The B200 was outfitted with a lidar instrument which measures vertical profiles of aerosols and an instrument called a polarimeter, developed by the Goddard Institute for Space Studies, that measures polarized light scattered by aerosols to gather more accurate details about the size, shape and composition of aerosols.

Aerosols directly affect Earth’s energy budget – the balance of incoming and outgoing radiation – by absorbing and scattering incoming solar rays. That impact is understood only within a large margin of uncertainty. Aerosols also influence cloud formation. The microscopic particles help form water and ice clouds and can change cloud properties – often leading to greater cloud cover and a cooling effect. This indirect effect has been even harder to measure and model than the direct effect. It accounts for the largest uncertainty in models used for predicting future climate, according to the Intergovernmental Panel on Climate Change (IPCC) 2007 report. This finding led the U.S. Climate Change Science Program (CCSP), in a report released in January 2009, to state the case for much-needed improvements in both measuring and modeling aerosols in the atmosphere including their interactions with clouds. The commonly accepted range of potential surface temperature increase over the course of a century – assuming a doubling of atmospheric carbon dioxide – is 1.2 degrees to 4.7 degrees Celsius. Most of the temperature increase should occur in the latter part of the century. The majority of the uncertainty that leads to that wide range in the prediction of heating is due to unknowns about the impact of aerosols.

“Such a range is too wide to meaningfully predict the climate response to greenhouse gases,” the CCSP report concluded.

The flights in Oklahoma were designed to offer a closer look at aerosol-cloud interactions and see how the airborne polarimeter – called the Research Scanning Polarimeter (RSP) – and lidar – called the High Spectral Resolution Lidar (HSRL) – could work together to give a more complete picture of aerosols. Data from the flights – which covered a vast region of the southern plains, in an attempt to capture useful data over a common type of land surface – will test the algorithms to be used to process data gathered by the Aerosol Polarimetry Sensor (APS) that will fly on the Glory satellite. In addition, the flights also served as a test of the instruments’ ability to make measurements of the size, type, amount, and distribution of aerosols.

Brian Cairns, the Goddard Institute for Space Studies-based principal investigator for the RSP instrument and the Aerosol Polarimetry Sensor that will fly on Glory, said polarimetry could eventually significantly improve remote sensing measurements of aerosol size and substantially reduce the uncertainty related to measurements of amounts of aerosols.

On the more experimental end, Cairns said, scientists are using the data from the lidar and polarimeter to look at the concentration of water droplets in clouds – an important parameter that could be significantly influenced by the presence of manmade aerosols, such as pollution. Determining a suitable method for measuring droplet concentration could go a long way toward making better estimates of the influence aerosols have on cloud properties.

“You’re really just trying to get the number concentration of droplets,” Cairns said. “Over oceans, it’s not that variable within a given type of clouds. But with the addition of some pollution, that could change.”

In the long line of NASA’s ground-, airborne- and satellite-based instruments designed to observe aerosols, these flights pairing the RSP and HSRL provides another important perspective.

“The idea is we can combine data from the two instruments to get more detailed information about the aerosols,” said Rich Ferrare, a research scientist with the HSRL team at Langley. “We can combine the data to get more than either, alone, can provide.”

Ferrare also said that while satellite-based sensors provide a global view of aerosol coverage, airborne measurements allow scientists to get a closer look at the still incompletely understood processes of aerosol-cloud interactions. Studying that full range is necessary to ultimately reduce the unknowns about aerosols and their impact on climate.

“Just from the measurement standpoint, you’ve got to be able to look at the small scale, to see how those processes work,” Ferrare said. “You also need global measurements from satellites. Then you need to improve the models.

“There are a lot of things involved in reducing those error bars.”

Related Links:

> High Spectral Resolution Lidar (HSRL)
> Glory: Observing the Earth's Aerosols and Solar Irradiance

Viewing History

 Viewing History
Adjacent to the Kennedy Space Center thousands of spectators camped out on beaches and roads to watch the launch of Apollo 11, which launched at 9:32 a.m. Eastern on July 16, 1969.

The launch of Apollo 11 was the culmination of 8 years of hard work by thousands of scientists and technicians. Four days later, Apollo 11 commander Neil Armstrong stepped out of the lunar module and took "one small step" in the Sea of Tranquility, calling it "a giant leap for mankind."

Thursday, July 16, 2009

Bolden and Garver Confirmed by U.S. Senate

NASA Administrator Charles Bolden and Deputy Administrator Lori Garver at their Senate confirmation hearing

Charles Frank Bolden, Jr., was confirmed by the U.S. Senate on Wednesday as the twelfth administrator of the National Aeronautics and Space Administration. Lori Beth Garver was confirmed as NASA's deputy administrator.

As administrator, Bolden will lead the NASA team and manage its resources to advance the agency's missions and goals.

"It is an honor to have been nominated by President Obama and confirmed by the Senate to lead this great NASA team," Bolden said. "Today, we have to choose. Either we can invest in building on our hard-earned world technological leadership or we can abandon this commitment, ceding it to other nations who are working diligently to push the frontiers of space."

"If we choose to lead, we must build on our investment in the International Space Station, accelerate development of our next generation launch systems to enable expansion of human exploration, enhance NASA's capability to study Earth's environment, lead space science to new achievements, continue cutting-edge aeronautics research, support the innovation of American entrepreneurs, and inspire a rising generation of boys and girls to seek careers in science, technology, engineering and math."

Bolden's confirmation marks the beginning of his second stint with NASA. His 34-year career with the Marine Corps included 14 years as a member of NASA's Astronaut Office. After joining the office in 1980, he traveled to orbit four times aboard the space shuttle between 1986 and 1994, commanding two of the missions. His flights included deployment of the Hubble Space Telescope and the first joint U.S.-Russian shuttle mission, which featured a cosmonaut as a member of his crew.

During his astronaut career, Bolden also drew technical assignments as the Astronaut Office safety officer; technical assistant to the director of Flight Crew Operations; special assistant to the director of the Johnson Space Center; chief of the Safety Division at Johnson (overseeing safety efforts for the return to flight after the 1986 Challenger accident); lead astronaut for vehicle test and checkout at the Kennedy Space Center; and assistant deputy administrator at NASA Headquarters. He was inducted into the U.S. Astronaut Hall of Fame in May 2006.

Immediately prior to Bolden's nomination for the NASA administrator's job, he was employed as the chief executive officer of JACKandPANTHER LLC, a small business enterprise providing leadership, military and aerospace consulting, and motivational speaking. A resident of Houston, the 62-year-old South Carolina native earned a bachelor of science degree in electrical science from the U.S. Naval Academy in 1968. He completed flight training in 1970 and became a naval aviator, serving as a combat pilot in Southeast Asia and later, as a test pilot. Bolden retired from the Marine Corps in 2003 with the rank of major general.

Like Bolden, Garver's confirmation as deputy administrator marks the second time she has worked for NASA. Her first stint at the agency was from 1996 to 2001. Initially, she served as a special assistant to the NASA administrator and senior policy analyst for the Office of Policy and Plans, before becoming the associate administrator for the Office of Policy and Plans. Reporting to the NASA administrator, she oversaw the analysis, development and integration of policies and long-range plans, the NASA Strategic Management System, and the NASA Advisory Council.

As deputy administrator, Garver will be NASA's second in command. She is responsible to the administrator for providing overall leadership, planning, and policy direction for the agency. Garver will represent NASA to the Executive Office of the President, Congress, heads of government agencies, international organizations, and external organizations and communities. She also will oversee the work of NASA’s functional offices, including the Office of the Chief Financial Officer, Office of General Counsel and Office of Strategic Communications.

"I am very excited about the opportunity to serve under Charlie Bolden's leadership," Garver said. "My previous five years at NASA exposed me to the incredible talent of the workforce there. The unbelievable achievements of this team over its 50-year history are unmatched. I look forward to working with Charlie and the NASA team to make our agency work as effectively as it can for the American people."

A 48-year-old Michigan native, Garver earned a bachelor's degree in political science and economics from Colorado College in 1983. Her focus immediately turned to space when she accepted a job working for Sen. John Glenn from 1983 to 1984. She since has served in a variety of senior roles in the nonprofit, government and commercial sectors.

From January 2001 until her nomination as NASA's deputy administrator, Garver was a full-time consultant as the president of Capital Space, LLC, and senior advisor for space at the Avascent Group. In these roles, she provided strategic planning, technology feasibility research and business development assistance, as well as merger, acquisition and strategic alliance support, to financial institutions and Fortune 500 companies.

For a detailed biography of Bolden, visit:

http://www.nasa.gov/about/highlights/bolden_bio.html

For a detailed biography of Garver, visit:

http://www.nasa.gov/about/highlights/garver_bio.html

For more information about NASA and agency programs on the Internet, visit:

http://www.nasa.gov

NASA And The National Symphony Orchestra Salute Apollo Legacy

Mezzo-Soprano Denyce GravesR&B Singer Chaka KhanJamia Nash cuddling a bear.NASA is kicking off events to commemorate the achievements of the Apollo program and the 40th anniversary of the first lunar landing. On July 18, NASA and the National Symphony Orchestra under the baton of Emil de Cou will host a free concert, “Salute to Apollo: The Kennedy Legacy,” at 8 p.m. EDT at the John F. Kennedy Center for Performing Arts’ Concert Hall.

Special guests at the event include Apollo 11 astronaut Buzz Aldrin and space shuttle Commander Scott Altman, who led the last servicing mission to the Hubble Space Telescope.

Aldrin and Atlman, who will narrate highlights from Gustav Holst’s The Planets, will join a stellar lineup of performers including mezzo-soprano Denyce Graves, R&B singer Chaka Khan and singer and actress Jamia Nash. The evening will include two selections written by Tena Clark including the Grammy nominated song Way Up There to be performed by Khan. Clark also wrote special lyrics dedicated to the Hubble astronauts for her other song written for Build-A-Bear Workshop entitled Let’s Talk About Love. The 12-year-old Nash will sing these special lyrics.

The rest of the program includes selections from John Williams and Antonin Dvorák. The music will be enhanced by footage of the Apollo missions, and other NASA programs projected on a large screen above the orchestra.

NASA's Apollo missions and 40th anniversary Web sites provide easy access to various agency resources about the program and the history of human spaceflight, including a gallery of Apollo multimedia features.

Related Sites:

> Kennedy Center
> Apollo 40th Anniversary Web site
> Apollo Missions

After Five Years, NASA's Aura Shines Brightly

Ozone destruction in the 2004-2005 Arctic winter, as measured by the Microwave Limb Sounder on NASA's Aura spacecraft.Aura's Tropospheric Emission Spectrometer measured the distribution of heavy(depicted in red) and light (depicted in blues and purples) water vapor molecules over Earth's tropics.Aura spacecraftOn July 15, 2004, NASA's Aura spacecraft launched from California's Vandenberg Air Force Base on a mission to study Earth's ozone layer, air quality and climate. Aura's data are helping scientists address global climate change issues such as global warming; the global transport, distribution and chemistry of polluted air; and ozone depletion in the stratosphere, the layer of Earth's atmosphere that extends from roughly 15 to 50 kilometers (10 to 30 miles) in altitude.

Two of Aura's four instruments were designed, built and managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif.: the Microwave Limb Sounder and the Tropospheric Emission Spectrometer. Five years after launch, both instruments are still going strong, providing a wealth of data to climate scientists around the world.

Microwave Limb Sounder

The Microwave Limb Sounder is a second-generation instrument that is helping scientists improve our understanding of ozone in Earth's stratosphere, especially how it is depleted by processes of chlorine chemistry. The instrument measures naturally occurring microwave thermal emission from the edge of Earth's atmosphere to remotely sense vertical profiles of atmospheric gases, temperature, pressure and cloud ice.

Research results to date from Aura's Microwave Limb Sounder include findings pertinent to the loss of ozone in the polar stratosphere; water vapor and cloud ice processes in the upper troposphere--the region of our atmosphere that extends from roughly 10 to 15 kilometers (6 to 10 miles) in altitude--that affect climate; measurements of stratospheric chlorine and bromine, two gases involved in the destruction of ozone; the chemistry of hydrogen in the stratosphere and mesosphere (the layer of Earth's atmosphere directly above the stratosphere); chemical and physical processes at and near the tropical tropopause (the boundary between the troposphere and the stratosphere); the dynamics and transport of chemicals in the stratosphere; and pollution in the upper troposphere, to name just a few.

"It has been extremely gratifying to see how the Microwave Limb Sounder observations have been used by scientists around the world in important and creative studies that have improved our understanding of the complex processes affecting our atmosphere," said Microwave Limb Sounder Principal Investigator Nathaniel Livesey of JPL.

Tropospheric Emission Spectrometer

The Tropospheric Emission Spectrometer is an infrared sensor designed to study Earth's troposphere, the layer of Earth's atmosphere where we live. The spectrometer is gathering data on how gases are distributed globally in Earth's lower atmosphere. These data are being used to create three-dimensional models of the chemistry of the lower atmosphere, the interactions between the lower atmosphere and the biosphere, and the exchange of gases between Earth's troposphere and stratosphere.

While the Tropospheric Emission Spectrometer can detect and measure many components of the troposphere, one of its main purposes is to study ozone. Low levels of ozone are a natural component of the troposphere, but higher levels, usually associated with polluted environments, are dangerous to plants and animals, including humans. The spectrometer is providing important data on where ozone in the troposphere comes from and how it interacts with other chemicals in the atmosphere.

Research highlights so far from the spectrometer include studies that validate how pollutants are transported globally from continent to continent; differentiation of "heavy" water vapor from normal vapor, which can be used to track evaporation and precipitation cycles in the atmosphere; the first direct measurements of how ozone in the upper troposphere contributes to climate change; monitoring ozone and its transport at or near Earth's surface; and measuring ammonia-a significant source of aerosols-in the lower atmosphere.

"The biggest impact made by the Tropospheric Emission Spectrometer to date has been to demonstrate that it is possible to make accurate measurements of ozone in the lower atmosphere (troposphere) despite the fact that there is 10 times more ozone in the stratosphere," said Tropospheric Emission Spectrometer Principal Investigator Reinhard Beer of JPL.

NASA's Goddard Space Flight Center manages the Aura mission for NASA's Science Mission Directorate, Washington.

Keeping a 'Trained Eye' on the James Webb Space Telescope

Diagram of James Webb Space Telescope Instruments including OTEJames Webb Space Telescope vs. Hubble Mirror Sizes.Pictured with the OTE mockup is Josh Levi, the OTE Integration and Test leadNASA and Northrop Grumman are keeping a "trained eye" on the James Webb Space Telescope, by training their engineers on how to handle and assemble the telescope's Optical Telescope Element (OTE), also known as the "eye" of the telescope.

Recently, a mock-up of the OTE’s Primary Mirror Backplane Assembly (PMBA), which supports the telescope’s mirror segments, was used to simulate how the element frame will be handled when the actual components of the telescope are being assembled.

The OTE's support frame will actually house all 18 of the Primary Mirror Segment Assemblies that comprise the Primary Mirror on the telescope. The OTE gathers the light coming from space and directs it into the science instruments.

The James Webb Space Telescope is the next-generation premier space observatory, exploring deep space phenomena from distant galaxies to nearby planets and stars. The Webb Telescope will give scientists clues about the formation of the universe and the evolution of our own solar system, from the first light after the Big Bang to the formation of star systems capable of supporting life on planets like Earth.

The Webb telescope needs a large mirror (made up of the 18 mirrors) to collect as much light as possible to see galaxies from the beginning of the Universe. The Webb telescope scientists and engineers have determined that a primary mirror 6.5 meters (21.3 feet) across is needed to collect enough light to measure these galaxies.

As with the assembly of any satellite or spacecraft, it's important for engineers to practice first, so, a mock-up of the PMBA was created at Northrop Grumman, Redondo Beach, Calif. for that purpose. Engineers there are simulating the handling, installation and alignment of the frame as they will when doing so with the flight hardware. They also check for clearance problems in advance of moving the real telescope between Northrop Grumman’s facility in Redondo Beach Calif. and NASA Goddard Space Flight Center in Greenbelt, Md."When it comes to handling one-of-a-kind space telescopes, practice makes perfect," said Lee Feinberg, NASA Optical Telescope Element Manager at Goddard.

Charles Atkinson, Deputy Telescope Manager, Northrop Grumman Aerospace Systems said, "Even though it is many months from when we will perform the Integration and Test of the actual flight hardware, the mock-up has already been incredibly beneficial. The OTE's large size and many handling and test configurations make early demonstrations very important when laying out the handling equipment and volume necessary to perform the various integration and test operations."

The other major components of the OTE include the Secondary Mirror Assembly and its tripod support, the secondary mirror support structure, the Aft Optics Subsystem which contains the tertiary mirror and the fine steering mirror, the Deployable Tower Assembly, along with electronics and thermal control hardware. In addition to holding the OTE together, the PMBA will be where the science instruments, in the Integrated Science Instrument Module, are installed in the Observatory.

The Primary Mirror Backplane Assembly that holds the OTE is too wide to fit inside a rocket. So, the answer to making it fit is to enable the OTE to fold up. That's just what the engineering team has enabled the OTE to do. Once folded it will fit into a rocket, and once launched will then unfold in space under the command of messages transmitted from Earth.

All of the flight primary mirror segments that will populate the OTE have completed the grinding phase. "With all 18 flight mirror segments in the final polishing stage of production its time to start preparations for their installation, beginning with the challenging task of handling the telescope’s outsized mounting structure," said Mark Clampin, Webb Telescope Observatory Project Scientist at Goddard.

The 18 primary mirror segments in the OTE are made up of three slightly different shapes, consisting of six mirrors of each shape. Another challenge to engineers was to make the mirrors light enough to launch, so they solved that problem by using a metal called Beryllium.

Once the actual OTE structure is built and finalized and the mirrors have been completed, the mirrors will be integrated into the OTE. "Mirror installation begins on the structure in August 2011 and the telescope is built with the mirrors in May 2012," Feinberg said. NASA Goddard is managing the overall development effort for the Webb Telescope. The telescope, being built by Northrop Grumman, is a joint project of NASA and many U.S. partners, the European Space Agency and the Canadian Space Agency. The Webb telescope is expected to launch in 2014.

Related Link:

> JWST Project web site

Endeavour, STS-127 Crew Begin Complex Mission

Space shuttle Endeavour and its crew of seven astronauts are in orbit after an on-time launch at 6:03 p.m. EDT from NASA's Kennedy Space Center in Florida. Following a smooth countdown with no technical issues and weather that steadily improved throughout the afternoon, the shuttle lifted off from Launch Pad 39A and began its orbital chase of the International Space Station.

"It was a testimony for this entire launch and flight control team," Launch Director Pete Nickolenko said of the countdown and successful liftoff, which came on the sixth launch attempt after technical issues and weather concerns prevented the first five tries. "It was an outstanding effort, and it made the complex look really easy. It really was a case of persistence."

Bill Gerstenmaier, associate administrator for Space Operations, also commended the launch effort, but cautioned that the mission to come is "very challenging," with five spacewalks and robotic activities scheduled. "The teams are fully prepared -- they're ready to go do what they need to go do, and we look forward to the exciting activities as we install the Exposed Facility out on the Kibo module."

Space Shuttle Mission: STS-127

Liftoff of space shuttle Endeavour
Endeavour Reaches Orbit
The 16-day mission will feature five spacewalks and complete construction of the Japan Aerospace Exploration Agency's Kibo laboratory. Astronauts will attach a platform to the outside of the Japanese module that will allow experiments to be exposed to space.

The STS-127 crew members are Commander Mark Polansky, Pilot Doug Hurley and Mission Specialists Dave Wolf, Christopher Cassidy, Tom Marshburn, Tim Kopra and Canadian Space Agency astronaut Julie Payette. Kopra will join the space station crew and replace Japanese astronaut Koichi Wakata. Wakata will return to Earth on Endeavour to conclude a three-month stay at the station.

STS-127 Additional Resources
› Mission Press Kit (6.9 Mb PDF)
› Mission Summary (429 Kb PDF)
› Meet the STS-127 Crew

Wednesday, July 15, 2009

Astronomers, royalty, rock stars to inaugurate world's largest telescope

world's largest telescopeFour hundred years after Galileo first turned his handmade telescope toward the heavens, the world's largest, most technologically advanced telescope is set to make its formal debut.

The inauguration of the Gran Telescopio Canarias — with its 10.4-meter diameter mirror, the telescope has more light-collecting area than any other — is scheduled for July 24 in Spain's Canary Islands. Officials and astronomers from the University of Florida, the only U.S. institution that is part of the project, will join more than 500 astronomers, journalists and celebrities in a ceremony presided over by Spain's King Juan Carlos I and Queen Sofia.

"The completion and inauguration of the GTC is a huge milestone for astronomy and for the University of Florida in collaboration with its partners in Spain and Mexico," UF Provost Joe Glover said. "We look forward to our astronomers playing a central role in the major discoveries this uniquely powerful telescope will enable."

Perched 7,874 feet above sea level on a mountain on the island of La Palma, the GTC has 6 square meters more light collecting area than any of the roughly one dozen 8- to 10-meter telescopes worldwide. With a mirror composed of 36 hexagonal segments thought to have the smoothest surfaces ever made, it is also the world's most technologically advanced optical telescope. Sensors keep the mirrors aligned to counteract the force of gravity, with the result that they act as a single surface, even as the telescope is rotated and aligned in place.

Spain owns 90 percent, Mexico 5 percent and UF 5 percent of the telescope under construction since 2000. UF contributed $5 million toward the $180 million project — and its astronomers designed and built one of the first two astronomical instruments for the telescope, a multimillion dollar heat-sensing camera called CanariCam.

Stan Dermott, chairman of UF's astronomy department, said the GTC's size and technical attributes enable it not only to gather more light than any other telescope, but also resolve the light into sharper and clearer focus. For astronomers, he said, those capabilities make it a powerful tool to study cosmic origins – the early days of the universe and the very early moments in the mysterious births of stars, planets and galaxies.

"The interpretation of the structure of the disks where new planets form is highly dependent on the quality of the image," he said, adding that the GTC also will enable the discoveries of new planets, possibly including the first habitable planet.

The telescope gathers the light, but only astronomical instruments can reveal the mysteries it contains. The car engine-sized CanariCam, built at UF but now in La Palma and expected to become operational next year, "sees" the infrared light — the invisible light that accompanies heat — emitted by stars and planets as they form in space. It also sees the light that, in its visible form, is obscured by the dust clouds and gas in space.

CanariCam is unique among mid-infrared cameras in its ability to determine the direction of polarized light and accomplish coronagraphy, which blocks the bright light of stars to make faint planets nearby more visible. Those abilities will help it reveal cool planets and more about the role of magnetic fields in planet and star formation, said Charles Telesco, UF astronomy professor and the principal investigator on the CanariCam project.

UF astronomer Eric Ford became one of the first astronomers worldwide to use the GTC earlier this year. Dermott said he anticipates that about 60 astronomy faculty, graduate students, postdoctoral associates and others — most of the members of the department — will become involved with GTC-related observations or research. He stressed that access to such a prominent telescope is key to success in astronomical research.

"All the objects we study are remote, and you have to get your information from looking at images," he said. "If the competition has a better image than you, you are basically out of business. So having the GTC puts our students and faculty on the front line."

There is far more demand for the world's largest telescopes than available nights, with the result that most astronomers get far less time than they want — and in some years, none at all. UF's part ownership of the GTC means that its astronomers are guaranteed 20 nights each year. UF'S instrument-building program will result in additional nights, as will UF astronomers' collaborations with Mexican and Spanish astronomers, Dermott said.

Brian May, lead guitarist of the rock group Queen and an astronomer himself, is expected to be among the celebrities present for the inauguration. 2009, the International Year of Astronomy, celebrates Galileo's first telescope observations in 1609.

NASA JPL Scientist Receives Presidential Early Career Award

Josh Willis

Josh Willis, an oceanographer at NASA's Jet Propulsion Laboratory in Pasadena, Calif., has been honored by President Barack Obama with the 2009 Presidential Early Career Award for Scientists and Engineers. The award is the highest honor bestowed by the U.S. government on young professionals in the early stages of their independent research careers.

Willis is one of 100 beginning researchers to receive the 2009 award. This year's recipients also include three faculty members with the California Institute of Technology in Pasadena, which manages JPL for NASA. The honorees will receive their awards this fall at a White House ceremony.

A researcher in JPL's Ocean Circulation Group, Willis uses satellite data as well as data collected at sea to study the impact of global warming on the ocean. His studies of ocean warming and sea level rise have been widely used by colleagues around the world and were cited in the 2007 report of the Intergovernmental Panel on Climate Change. That report shared the 2007 Nobel Peace prize with Vice President Al Gore. Willis frequently lectures to the public and works with students to educate them about climate change issues and human impacts on global warming.

Established by President Bill Clinton in 1996, the Presidential Early Career Award for Scientists and Engineers annually honors researchers whose early accomplishments show the greatest promise for strengthening America's leadership in science and technology and contributing to the awarding agencies' missions. The awards are made to those whose innovative work is expected to lead to future breakthroughs.

Recipients are selected from among nine federal departments and agencies based on two criteria: pursuit of innovative research at the frontiers of science and technology, and a commitment to community service as demonstrated through scientific leadership, public education or community outreach. Winning scientists and engineers receive up to a five-year research grant to further their study in support of critical government missions.

"These extraordinarily gifted young scientists and engineers represent the best in our country," Obama said in a White House news release. "With their talent, creativity and dedication, I am confident that they will lead their fields in new breakthroughs and discoveries and help us use science and technology to lift up our nation and our world."

Willis holds a Bachelor of Science degree in physics and mathematics from the University of Houston; a Master of Science degree in physics from the University of California, San Diego, in La Jolla, Calif.; and a doctorate in oceanography from the Scripps Institution of Oceanography, University of California, San Diego. He joined JPL in 2004. Previous honors include JPL's Charles K. Witham Environmental Stewardship Award.

He and his wife, Dr. Dixie Aragaki, live in Los Angeles.

The three Caltech recipients are John O. Dabiri, an expert in biological propulsion who studies mechanics and dynamics of biological propulsion and fluid dynamic energy conversion; Beverley J. McKeon, who studies experimental manipulation of wall-bounded flows for improved flow characteristics; and Joel A. Tropp, who is developing new algorithms for solving inverse problems, a basic challenge that arises throughout the mathematical sciences.

1969 Apollo 11 News Release

On July 14, 1969, two days before the launch of the Apollo 11 mission, NASA's Lewis Research Center (now Glenn) issued this news release. The release highlights the center's role in the Apollo program and outlines the team effort required to accomplish a manned mission to the moon. It also captures the excitement of the era as the world anticipated a successful landing.

Note: On March 1, 1999 the Lewis Research Center officially became the NASA John H. Glenn Research Center at Lewis Field. Because of the historical nature of this release, references to NASA Lewis have not been changed.

NASA Lewis Research Center press release header
FOR IMMEDIATE RELEASE


CLEVELAND, Ohio, July 14 -- The Apollo program has been described at various times by astronauts, engineers, space agency officials and newspaper editorials as a magnificent "team effort." Indeed, the team which is accomplishing this complex program to explore the Moon comprises hundreds of thousands of government and contractor employees throughout the nation.

One member of the National Aeronautics and Space Administration team, the Lewis Research Center, provided important early research as well as subsequent direct technical support to the Apollo program. The Center's contributions included:
  • Pioneer research in rocket tests with liquid hydrogen and liquid oxygen systems;
  • Engineering studies of tanks, lines, and liquefiers for liquid hydrogen;
  • Wind tunnel tests of Saturn vehicles and of the Launch Escape Subsystem;
  • Studies in the Zero Gravity Research Facility for settling propellants in fuel tanks;
  • Technical consultation and advice in such areas as safety, fuel cell performance, rocket engine combustion, propellant pump design and thrust chamber fabrication.
Among the shapers of history in the early years of the space program was Lewis' present Director, Dr. Abe Silverstein. In 1958, when he was Associate Director of Lewis, Dr. Silverstein was called to Washington to help organize NASA, which was, as the Successor of National Advisory Committee for Aeronautics (NACA), to be the nation's civilian agency for meeting the challenge of space.

Within the new agency, Dr. Silverstein was appointed the Headquarters Director of Space Flight Programs with responsibility for developing and initiating all space missions. Many of those missions are going on today, others such as Ranger and Mercury have ended.

Among the many missions conceived at that time was a manned journey to the Moon and back. Dr. Silverstein himself named it "Apollo" after one of the most versatile of the Greek gods. Dr. Silverstein recalls he chose the name after perusing a book of mythology at home one evening, early in 1960. He thought that the image of "Apollo riding his chariot across the Sun was appropriate to the grand scale of the proposed program."

When did the program originate? The idea of a lunar mission was first officially introduced at a meeting of NASA program planners in Nov. 1959 at Wallops Island, Va. However between that time and President John F. Kennedy's historic space commitment of 1961, much of the basic mission remained to be worked out. During this time Dr. Silverstein chaired the committee that determined the characteristics of the Saturn family of launch vehicles, including the use of liquid hydrogen-oxygen propellants.

Long before Apollo was ever planned or named, the Lewis Research Center in Cleveland was advancing the propulsion technology which would help make the mission possible.

As early as the latter part of the 1940's, Lewis had begun research on high energy liquid and solid propellants under the direction of Dr. Walter T. Olson, now an Assistant Director of Lewis, and by 1952 this work included studies of liquid hydrogen-liquid oxygen.

Initial Lewis investigations used very small thrust chambers in the range 100 to 1000 lbs. thrust. Over the course of the next decade, rocket engineers and scientists experimented with a variety of thrust chamber designs to achieve high combustion efficiency and smooth burning; and they measured heat transfer rates within the thrust chamber and demonstrated how to cool the chamber and nozzle with liquid hydrogen. Since hydrogen, the lightest of the elements, in its liquid state boils at -423 deg F, and the oxidizer, liquid oxygen, is stored at -29 deg F, another major concern was how to handle the cryogenic propellants themselves.

By 1958, as the United States entered the space business the Lewis Research Center had tested a fully cooled, liquid hydrogen-liquid oxygen thrust chamber at the, then large scale of 20,000 lbs. thrust.

The experience Lewis propulsion experts gained in the field of high energy propellants later led to the development of the 15,000 lb. liquid hydrogen-liquid oxygen engine designated RL-10. Two of these engines power the upper stage of the Atlas-Centaur launch vehicle that has been under Lewis management since 1962. (Atlas-Centaur launched the Surveyor spacecraft that landed on the moon, and the Mariner space craft that will fly by Mars on July 31 and Aug. 5.

Much of the same technology developed by Lewis for Centaur was particularly applicable to the J-2 liquid hydrogen-oxygen engines of the Saturn second stage (S-II).

Consequently, a number of Lewis staff members -- men by then well experienced in high energy propulsion systems -- were called upon by NASA Headquarters to serve on the technical assessment teams which recommended the contractor to build the F-l and J-2 engines. Dr. Silverstein chaired the Source Board which made the final selection of the F-l contractor. Work began on the F-l engine, the nation's largest, in 1958 and on the J-2 in 1960.

During the course of development of these engines, Lewis continued its technical support in the form of consultation with NASA's Marshall Space Flight Center, Huntsville, Ala. Melvin Hartmann and Ambrose Ginsburg, Lewis fluid systems engineers, served on a Marshall committee to review problems being experienced by the F-l turbopump. These and other specialists served as consultants on a J-2 review committee. Among the topics discussed and of particular interest to the Lewis men was the inducer, that component which draws the boiling cold hydrogen into the pumps. Previous research conducted on this component at Lewis' Plum Brook Station near Sandusky, O., helped verify data of the Marshall Center that showed the inducers would permit a desired low pressure in the fuel tank.

Lewis also assisted a Marshall task group in achieving combustion stability in the F-l engine. Dr. Richard Priem, experienced in advanced rocket combustion, was one of this group studying the "rocket screaming", a phenomenon caused by strong resonant pressure waves and which can destroy a rocket engine in seconds. One other area of consultation with Marshall during the F-1 develop- ment was on fabrication of the thrust chamber. Walter Russell, a fabrication specialist served on the committee to review the materials and processes for the fabrication of the furnace-brazed thrust chamber and its jacket.

Staff members also lent their technical knowledge to other areas of the Apollo propulsion systems. Early studies were conducted at Lewis on the type of storable propellants to be carried on the upper stage of the Saturn V vehicle and on the spacecraft.

The Center's unique Zero-Gravity Facility was called upon to do two jobs for the Apollo program. In mid-1960, engineers used this facility to help solve the problem of problem of re- starting the Service Module's propulsion system in space. Using surface tension phenomena observed during these studies, Lewis engineers assisted in designing a retainer for the propellant in the fuel tank. This retainer would keep enough propellant at the bottom of the tank to ensure that propellant would enter the pump and re-start the engine.

The Zero-Gravity Facility was used to help solve a similar problem in the S-IVB third stage of the Saturn V for the Marshall Center. In flight when the S-IVB engine shuts down, auxiliary hydrogen-peroxide thrusters are turned on to settle the sloshing propellants. During the coast phase the propellants are maintained in the bottom of the fuel tank by the thrust obtained when boiled off hydrogen gas is ducted through a small thruster system. Studies in the Zero- G Facility were able to determine the proper size of these various thrusters.

One of the astronaut's concerns about how weightlessness in space might affect fuel cell performance drew helpful information from Lewis too. Fuel cells are carried aboard the Service Module to provide electric power to spacecraft systems. Consequently, Lewis researchers investigated this area and made known to the Manned Spacecraft Center that the condenser of the fuel cell did not depend on gravity to operate properly. Lewis also was asked by MSC to determine the heat transfer characteristics of the condenser; this information was used in a computer simulation of the spacecraft's electrical power subsystem.

During 1967 Lewis engineers were consulting on the overall combustion and system stability of the Lunar module ascent engine, the critical propulsion system for the Ascent Stage which returns the astronauts from the moon to lunar orbit. John Wanhainen, a chemical rocket expert, was part of a task group to overcome the high frequency combustion instability noted in the engine. Two other engineers, Robert Dorsch and Leon Wenzel, ran analog computer analyses of low frequency combustion instability characteristics.

The Center's 8 x 6-foot transonic and 10 x 10-foot supersonic wind tunnels were used in extensive tests on models of Saturn booster stages.

The first such tests were made in the late 1950's when engineers studied base flow and heating tests on the SIB booster, the eight-engine first stage of the Saturn I. The 1/45th scale model had real, working rocket engines of 250 lbs. thrust each. Data were taken over a range of speeds from takeoff to Mach 3.5 and of altitudes from sea level to 150,000 feet. This simulation of actual flight conditions provided valuable information on the pressure and heat loads experienced on the base and engines' compartment of the SI vehicle. By varying the size and location of flow deflectors and shroud air scoops-- devices to channel the air to best advantage--engineers were able to minimize the pressure and heating loads. Another study on the SI helped optimize vehicle flight stability and air pressure distribution.

In the 1964-1966 period base flow and heating also were studied in both wind tunnels for the SI C first stage of the Saturn V. Also, the force required to move the engine nozzles for directional control had to be measured. These measurements helped determine the size of the actuators required to gimbal the engines. In all manned missions, safety of the public, the astronauts, and the operating crew, is a major concern to the NASA. In case a mission must be terminated early, one of the first options the astronauts have is to employ the Launch Escape Vehicle and Tower which stands atop the Command Module. This escape system propels the Command Module out and away from the Saturn V. During 1964 tests were made on the system in the Lewis Research Center's 8 x 6 tunnel at the request of the Manned Spacecraft Center. In the tunnel, a model of the escape system attached to the Command Module was released at various angles to determine its stability under simulated flight conditions.

Safety was the subject that brought I. Irving Pinkel, now Lewis' Assistant Director for Aerospace Safety, to serve as a consultant to the Apollo 204 Review Board. In that capacity and as a member of the team which investigated the causes of the spacecraft fire which took the lives of three astronauts early in 1967, Pinkel helped to recommend changes in the capsule to prevent a future tragedy.

Through extensive consulting on fracture mechanics, Lewis professionals have assisted in improving both the more than 140 pressure vessels of the Saturn V, and the SII fuel tank. Particular contributions by Lewis materials scientists to the construction of pressure vessels included improved test methods, and methods of design and analyses used on new concepts in fracture mechanics technology. Other materials scientists and engineers provided fracture research data on the critical weldments of the SII fuel and on the tank material itself; they also recommended cryogenic proof tests, and suggested flight conditions to reduce wind loads on the vehicle.

Thus, Lewis scientists and engineers, like thousands of others who have served the Apollo team, have their hopes riding high with Apollo 11.

Mars Dust Devil Has Colorful Effect in Image Series

The panoramic camera (Pancam) on NASA's Mars Exploration Rover Spirit was taking exposures with different color filters during the 1,919th Martian day.Scientists have combined a trio of shots taken seconds apart through different colored filters to create a special-effects portrait of a moving dust devil on Mars.

The panoramic camera on NASA's Mars Exploration Rover Spirit was taking exposures through different filters during the 1,919th Martian day of Spirit's mission (May 27, 2009) as part of constructing a large color panorama. Three westward shots, with several seconds intervening between them, caught a whirlwind in motion. A composite image combining the three exposures to make a color image of the Martian ground shows the dust devil in different colors, according to where it was on the horizon when each exposure was taken.

Dust devils occur on both Mars and on Earth when solar energy heats the surface, resulting in a layer of warm air just above the surface. Since the warmed air is less dense than the cooler atmosphere above it, it rises, making a swirling thermal plume that picks up the fine dust from the surface and carries it up into the atmosphere. This plume of dust moves with the local wind.

More than 650 dust devils have been recorded by Spirit since its operations began in 2004. The mission is currently in its third season of dust devils on Mars, which typically begin in Martian spring.

Monday, July 13, 2009

Stephan's Quintet--A Galaxy Collision in Action

Stephan's Quintet, a compact group of galaxies discovered about 130 years ago and located about 280 million light years from Earth, provides a rare opportunity to observe a galaxy group in the process of evolving from an X-ray faint system dominated by spiral galaxies to a more developed system dominated by elliptical galaxies and bright X-ray emission. Being able to witness the dramatic effect of collisions in causing this evolution is important for increasing our understanding of the origins of the hot, X-ray bright halos of gas in groups of galaxies.

NASA Scientists Dive Deep to Learn More about Life on the Moon, Mars

NASA and the Canadian Space Agency invite journalists and the public on Tuesday, July 14, to observe the international, multidisciplinary Pavilion Lake Research Project team as it studies the origin of rare freshwater carbonate rock structures that thrive in Pavilion Lake, British Columbia, Canada.

Reporters will have an opportunity to interview Pavilion Lake Research Project scientists from 9 a.m. to 5 p.m. PDT on July 14 as they study and explore the unique underwater formations and conduct research about life in extreme environments. Journalists interested in attending must register before July 13 at:

http://www.pavilionlake.com/participants/2009-media-access

A park permit is required for filming at Pavilion Lake. Reporters should e-mail Rob Enns at Rob.Enns@gov.bc.ca to obtain a permit.

Scientists believe the carbonate rock structures, known as microbialites, first were formed by microorganisms more than 2.5 billion years ago. Today, environments rich in microbialites are seen as potential analogs for the biological, geological and chemical processes of early Earth. Similar processes possibly occurred on other planets, such as Mars.

Using a combination of underwater vehicles and scuba divers, the research project blends science and technology to advance knowledge of astrobiology and examine how humans could explore the moon and Mars.

Pavilion Lake Research Project science team members, including a pair of NASA astronauts, will be available for interviews at the event.

For more information about NASA's plans lunar surface analogs, visit:

http://www.nasa.gov/exploration/home/analogs.html

The Pavilion Lake Research Project science team is providing mission updates on Twitter at:

http://www.twitter.com/pavilionlake

For more information about this year's Pavilion Lake Research Project and a list of participants and partner organizations, visit:

http://www.pavilionlake.com

Thursday, July 09, 2009

Astronaut Safety Gets Max Attention

The Max Launch Abort System launched at 6:26 a.m.NASA's next generation of spacecraft will have the safest-ever astronaut escape system, a modern-day version of the reliable Apollo system. Like Apollo, the Orion launch abort system will swiftly propel the crew capsule away from the nose of the Ares I rocket and out of harm's way in case of an emergency on the launch pad or during ascent to orbit.

Also -- as was the practice at times during development of key Apollo elements -- while NASA engineers are working on the Orion launch abort system, another NASA team is investigating an alternate launch abort concept.

The alternate system, called Max Launch Abort System, or MLAS, was successfully tested in a simulated pad abort test at NASA's Wallops Flight Facility, Wallops Island, Va., July 8.

MLAS was named after Maxime (Max) Faget, a Mercury-era pioneer. Faget was the designer of the Project Mercury capsule and holder of the patent for the "Aerial Capsule Emergency Separation Device," which is commonly known as the escape tower.

The unpiloted test was part of an assessment by the NASA Engineering and Safety Center (NESC) of a potential alternate launch abort system concept which could be used for future piloted spacecraft. The prototype, used in the test to evaluate means to safely propel a spacecraft and its crew from an errant rocket, represents a departure from the tower launch abort system used during Apollo launches and retained for the Constellation Program. A primary objective of the MLAS test is to provide the NASA workforce with additional direct implementation experience in flight testing a spacecraft concept useful in the Agency's future efforts to design, optimize and test spacecraft.

The bullet-shaped MLAS concept will not replace the Orion abort system.

NASA's Constellation Program has three years toward designing the Orion crew exploration vehicle and the Ares launch vehicles that will return humans to the moon to live and work. The spacecraft designs are based on the technical principles established during the Apollo and Space Shuttle programs - yet incorporates the latest technology to expand the spacecraft's operational flexibility. The Orion launch abort system offers a proven method of pulling the crew out of danger in the event of an emergency on the launch pad or during the climb to Earth orbit.

MLAS is of potential interest because it is theorized to have aerodynamic performance benefits, weight savings and be relatively simple in some spacecraft applications. Much of the potential gains would be accomplished by eliminating the launch abort tower, which also means eliminating the attitude control motors.

The MLAS demonstration vehicle consists of a full-scale composite fairing, a full-scale crew module simulator and four solid rocket abort motors mounted in the boost skirt with motor mass simulators in the forward fairing. Test items of interest began at the seven second mark with burnout of the solid motors. The test is primarily a demonstration of unpowered flight along a stable trajectory, MLAS vehicle reorientation and stabilization, followed by crew module simulator separation from the MLAS fairing, stabilization and the parachute recovery of the crew module simulator.

Data from the MLAS pad abort test has the potential to help the Orion Project in several ways. MLAS is the first demonstration of a passively-stabilized launch abort system on a vehicle in this size and weight class. It is the first attempt to acquire full-scale aero-acoustic data -- the measurement of potentially harmful noise levels due to the capsule moving through the air at high speeds -- from a faired capsule in flight. It also is the first to demonstrate full scale fairing and crew module separation and collect associated aerodynamic and orientation data. In addition, data from the parachute element will help validate simulation tools and techniques for Orion's parachute system development.

The NESC, located at NASA's Langley Research Center, Hampton, Va., is an independently funded NASA program that draws on technical experts from across all NASA centers to provide objective engineering and safety assessments of critical, high risk projects.

NESC partners in the MLAS effort include Northrop Grumman Corporation. The company developed and produced the MLAS composite fairing, fins, drag plates, and motor cage structure. Company personnel based in Wallops Island, Va., performed the structures and mechanism assembly as well as providing vehicle integration and flight test support. Northrop Grumman's subcontractor, Ensign Bickford Aerospace and Defense, Simsbury, Conn., provided pyrotechnic separation system mechanisms. Jacobs Technology, Tullahoma, Tenn., and partner Airborne Systems, Santa Ana, Calif., provided landing systems design and support.

Wallops contractors who supported the demonstration include Hawk Institute for Space Sciences, Computer Sciences Corporation, VT Griffin and Honeywell Technical Solutions, Inc. The NASA Sounding Rocket Operations Contract (NSROC) based at Wallops also provided support.

Each of the NASA Centers participated in the Agency-wide MLAS effort by providing engineers and technicians, analysts, designers, mission assurance specialists and/or use of their test facilities.

For images and video of the test firing, visit:

www.nasa.gov/centers/wallops/missions/mlas.html

For more information about NASA's Constellation Program, visit:

www.nasa.gov/constellation

Atlantic Ocean Temperatures at End of June 2009

Sea temperature at the end of June 2009

The first month of the 2009 Atlantic hurricane season drew to a close without so much as a tropical storm, but that isn't unusual. According to the National Hurricane Center, the 1944-2002 average for named storms in June was only about 0.75, which means they don't occur every year. When they do form, it is usually the Gulf of Mexico that brews them up, and this image of sea surface temperatures on June 30, 2009, shows why.

Based on a blend of observations from the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) on NASA's Aqua satellite and MODIS on the Terra satellite, the image shows temperatures that are generally warm enough to sustain hurricanes in yellow, orange and red. The waters of the Caribbean Sea (south of Cuba), the Gulf of Mexico, and the Atlantic off the Southeast coast were all warm enough to fuel hurricanes, while most of the tropical Atlantic between the Americas and Africa was still too cool.

The northwestern Caribbean Sea, the Gulf of Mexico, and the nearshore waters of Florida, Georgia, and the Carolinas are all considered "likely" areas for June tropical storm formation (white dashed outline), but storms are especially likely in the northeastern Gulf of Mexico (white oval). The black lines on the image show the average paths that June storms tend to follow. One track takes storms through the Caribbean Sea, brushing the western tip of Cuba, and arcing across northern Florida to follow the warm waters of the Gulf Stream. The other track favored by June storms is in the western Gulf of Mexico. Storms cross Mexico's Yucatan Peninsula and head north toward the Texas side of the U.S. Gulf Coast.

Storms occur often enough in June and July for those months to be considered part of the hurricane season, but named storms don't really start to accumulate until August. By the end of July there still will have been fewer than two named storms on average; by the end of August, the number is closer to five.

NASA and ESA Establish a Mars Exploration Joint Initiative

Mars, as seen by the Hubble Space Telescope in 1997The following joint statement was issued today by NASA and the European Space Agency (ESA):

On June 29 and 30 the NASA Associate Administrator for Science (Ed Weiler) and ESA Director of Science and Robotic Exploration (David Southwood) met in Plymouth, England, to establish a way for a progressive program for exploration of the Red Planet. The outcome of the bilateral meeting was an agreement to create a Mars Exploration Joint Initiative (MEJI) that will provide a framework for the two agencies to define and implement their scientific, programmatic and technological goals at Mars.

Discussions between NASA and ESA began in December 2008, driven by the ESA Ministerial Council's recommendation to seek international cooperation to complete the ExoMars mission and to prepare further Mars robotic exploration missions. At the same time, NASA was reassessing its Mars Exploration Program portfolio after the launch of its Mars Science Laboratory was delayed from 2009 to 2011. This provided NASA and ESA with an opportunity to increase cooperation and expand collective capabilities. To investigate the options in depth, a joint NASA/ESA engineering working group was established, along with a joint executive board to steer the efforts and develop final recommendations on how to proceed.

At the bilateral meeting in Plymouth, the executive board recommended NASA and ESA establish MEJI, spanning launch opportunities in 2016, 2018 and 2020, with landers and orbiters conducting astrobiological, geological, geophysical and other high-priority investigations, and leading to the return of samples from Mars in the 2020's. The director and associate administrator agreed, in principle, to establish the Initiative and continue studies to determine the most viable joint mission architectures.

NASA and ESA also agreed to establish a joint architecture review team to assist the agencies in planning the mission portfolio. As plans develop, they will be reviewed by ESA member states for approval and by the U.S. National Academy of Sciences. This unique collaboration of missions and technologies will pave the way for exciting discoveries at Mars.

Wednesday, July 08, 2009

STS-127 Astronauts Arrive at Kennedy

The seven astronauts set to launch aboard space shuttle Endeavour arrived at NASA's Kennedy Space Center on Tuesday afternoon, touching down on the Shuttle Landing Facility in a Gulfstream jet.

"I can tell you that this crew and the entire operations team are both eager and ready to get to work," said STS-127 Commander Mark Polansky after the crew stepped onto the runway. "Hopefully the next time we talk to you will be from orbit."

The STS-127 launch countdown will officially begin Wednesday at 10 p.m. when clocks begin ticking backward from T-43 hours. Liftoff is set for July 11 at 7:39 p.m.

Space Shuttle Mission: STS-127


The STS-127 astronauts arrive at Kennedy Space Center.
STS-127 Mission Overview

The 16-day mission will feature five spacewalks and complete construction of the Japan Aerospace Exploration Agency's Kibo laboratory. Astronauts will attach a platform to the outside of the Japanese module that will allow experiments to be exposed to space.

The STS-127 crew members are Commander Mark Polansky, Pilot Doug Hurley and Mission Specialists Dave Wolf, Christopher Cassidy, Tom Marshburn, Tim Kopra and Canadian Space Agency astronaut Julie Payette. Kopra will join the space station crew and replace Japanese astronaut Koichi Wakata. Wakata will return to Earth on Endeavour to conclude a three-month stay at the station.

STS-127 Additional Resources
Mission Press Kit (6.9 Mb PDF)
Mission Summary (429 Kb PDF)
Meet the STS-127 Crew

NASA Satellite Reveals Dramatic Arctic Ice Thinning

ICESat measurements of the distribution of winter sea ice thickness over the Arctic Ocean in 2008.Arctic sea ice thinned dramatically between the winters of 2004 and 2008, with thin seasonal ice replacing thick older ice as the dominant type for the first time on record. The new results, based on data from a NASA Earth-orbiting spacecraft, provide further evidence for the rapid, ongoing transformation of the Arctic's ice cover.

Scientists from NASA and the University of Washington in Seattle conducted the most comprehensive survey to date using observations from NASA's Ice, Cloud and land Elevation Satellite, known as ICESat, to make the first basin-wide estimate of the thickness and volume of the Arctic Ocean's ice cover. Ron Kwok of NASA's Jet Propulsion Laboratory in Pasadena, Calif., led the research team, which published its findings July 7 in the Journal of Geophysical Research-Oceans.

The Arctic ice cap grows each winter as the sun sets for several months and intense cold ensues. In the summer, wind and ocean currents cause some of the ice naturally to flow out of the Arctic, while much of it melts in place. But not all of the Arctic ice melts each summer; the thicker, older ice is more likely to survive. Seasonal sea ice usually reaches about 2 meters (6 feet) in thickness, while multi-year ice averages 3 meters (9 feet).

Using ICESat measurements, scientists found that overall Arctic sea ice thinned about 0.17 meters (7 inches) a year, for a total of 0.68 meters (2.2 feet) over four winters. The total area covered by the thicker, older "multi-year" ice that has survived one or more summers shrank by 42 percent.

Previously, scientists relied only on measurements of area to determine how much of the Arctic Ocean is covered in ice, but ICESat makes it possible to monitor ice thickness and volume changes over the entire Arctic Ocean for the first time. The results give scientists a better understanding of the regional distribution of ice and provide better insight into what is happening in the Arctic.

"Ice volume allows us to calculate annual ice production and gives us an inventory of the freshwater and total ice mass stored in Arctic sea ice," said Kwok. "Even in years when the overall extent of sea ice remains stable or grows slightly, the thickness and volume of the ice cover is continuing to decline, making the ice more vulnerable to continued shrinkage. Our data will help scientists better understand how fast the volume of Arctic ice is decreasing and how soon we might see a nearly ice-free Arctic in the summer."

In recent years, the amount of ice replaced in the winter has not been sufficient to offset summer ice losses. The result is more open water in summer, which then absorbs more heat, warming the ocean and further melting the ice. Between 2004 and 2008, multi-year ice cover shrank 1.54 million square kilometers (595,000 square miles) -- nearly the size of Alaska's land area.

During the study period, the relative contributions of the two ice types to the total volume of the Arctic's ice cover were reversed. In 2003, 62 percent of the Arctic's total ice volume was stored in multi-year ice, with 38 percent stored in first-year seasonal ice. By 2008, 68 percent of the total ice volume was first-year ice, with 32 percent multi-year ice.

"One of the main things that has been missing from information about what is happening with sea ice is comprehensive data about ice thickness," said Jay Zwally, study co-author and ICESat project scientist at NASA's Goddard Space Flight Center in Greenbelt, Md. "U.S. Navy submarines provide a long-term, high-resolution record of ice thickness over only parts of the Arctic. The submarine data agree with the ICESat measurements, giving us great confidence in satellites as a way of monitoring thickness across the whole Arctic Basin."

The research team attributes the changes in the overall thickness and volume of Arctic Ocean sea ice to the recent warming and anomalies in patterns of sea ice circulation.

"The near-zero replenishment of the multi-year ice cover, combined with unusual exports of ice out of the Arctic after the summers of 2005 and 2007, have both played significant roles in the loss of Arctic sea ice volume over the ICESat record," said Kwok.

For images of the Arctic sea ice decline, visit: http://www.nasa.gov/topics/earth/features/icesat-20090707.html .

For more information about ICESat, visit: http://icesat.gsfc.nasa.gov .

For more information about NASA and agency programs, visit: http://www.nasa.gov .

JPL is managed for NASA by the California Institute of Technology in Pasadena.

NASA Research to Help Aircraft Avoid Ocean Storms, Turbulence

An astronaut photo showing a series of mature thunderstorms located near the Parana River in southern Brazil.
Convective Weather

A prototype system could provide commercial airline pilots with key weather and turbulence forecasts when flying over remote regions of the ocean where little real- or near-real-time data is available now. The NASA-funded system, being developed by the National Center for Atmospheric Research (NCAR), combines computer models and data from five operating NASA satellites with an artificial intelligence system to predict turbulence. The system is on track for testing next year, with the goal of ultimately giving pilots a regularly updated picture of potential storms over the ocean so that they can fly away from or around danger. This photograph, acquired in February 1984 by an astronaut aboard the space shuttle, shows a series of mature thunderstorms in southern Brazil.

Deep Convective Clouds, seen from above, over the Atlantic Ocean.
Deep Convective Clouds

A 2009 astronaut photo from the International Space Station (ISS) of deep convective clouds, seen from above, over the Atlantic Ocean. Free standing and embedded towering convective clouds are particularly dangerous to aircraft flying over the open ocean.

NASA and NCAR are working to identify turbulence from breaking gravity waves that are generated by rapidly rising deep convection.
Turbulence Waves and Deep Convection

NASA and NCAR are working to develop a near-real-time forecast that identifies turbulence from breaking gravity waves that are generated by rapidly rising deep convection. This image from NASA's MODIS instrument (Moderate Resolution Imaging Spectroradiometer) shows gravity waves over the ocean. Atmospheric gravity waves (also called atmospheric internal waves) occur either when a uniform layer of air blows over a large obstacle, like a mountain or island or when rapidly rising, deep convection perturbs a stable layer from below, as in the oceanic case we have illustrated. When the air hits the obstacle or is disturbed by rising convection from below, the horizontal ribbons of uniform air are disturbed, which forms a wave pattern. This wave pattern in the air impresses itself onto sea waves when it touches the surface of the ocean. In addition to the surface mimicking the wave pattern, wave clouds can form as well, creating potential turbulence for aircraft.

Lidar, like CALIPSO's, can be used to tell a lot about cloud height and to validate and tune the aviation convection applications.
Slicing through the Atmosphere

NASA uses advanced satellite instruments to study the atmosphere. One instrument, CALIPSO, uses a lidar system to make a 3-D view of clouds. CALIPSO data will be used as a source of precise validation and tuning for these NASA/NCAR applications under development. Click on the image or below to view an animation showing a series of CALIPSO curtain images from around the globe.

View related animation

What Lies inside the Sun?

Artist's concept image of the SDO satellite orbiting the Sun.When a pond's surface is calm, you can see more clearly into its depths. As it turns out, the same is true for the sun.

Researchers are excited that the sun's surface is calmer now than it's been in almost a century. It's a rare opportunity - the first since the Space Age began - to peer more clearly into the sun's mysterious interior.

Now Playing: Hello Little SDO


To take advantage of the opportunity, NASA is about to launch the Solar Dynamics Observatory (SDO). SDO is expected to launch this year, as early as November 2009.

"That's perfect timing," says Dean Pesnell, a solar physicist at the Goddard Space Flight Center in Greenbelt, Md. "The sun is experiencing a century-class solar minimum, offering the clearest possible views."

"SDO will actually see through the sun's surface," added Pesnell. "The process is a little like taking an ultrasound of a pregnant mother. You can see the baby right through the skin."

The sensor that performs this trick is called the Helioseismic and Magnetic Imager (HMI). It can sense acoustic waves moving through the sun, and turn those waves into a fairly clear image of the interior.

"There's a lot going on inside the sun that we don't understand," notes Todd Hoeksema, a solar physicist at Stanford University, Palo Alto, Calif. where the HMI was built. "The Solar Dynamics Observatory is bound to deliver some big discoveries."

The biggest discovery of all would be the inner workings of the solar dynamo. Deep beneath the sun's visible surface, massive currents of electrically-charged gas (plasma) circulate in patterns that give rise to the sun's powerful magnetic field. Almost all solar activity from sunspots to solar flares is regulated by this inner dynamo.

Now Playing: Inside the Sun

"Understanding how the dynamo works is a holy grail for stellar physics," says Pesnell. "It is the key to forecasting solar activity and space weather."

The problem is these deep flows are hidden from view. The sun's surface is bright and opaque, so it is impossible to look through it. Instead, solar physicists study the sun's interior the same way that geologists look deep into the Earth-via seismology. Just as earthquakes trigger seismic waves that travel through the Earth, shifting mass in the sun sends pressure waves rippling through its interior. These p modes (p for pressure) bounce around inside the sun, causing the star to ring like an enormous bell. HMI detects the surface vibrations, which in turn can be analyzed to reveal the depths.

Sunspots can get in the way of the waves, distorting their times and frequencies, making it tricky to figure out what's really happening inside the complicated solar interior. That's why the current lack of sunspots is good for helioseismology.

"You have more sensitivity to what's happening deep in the sun when there's not as much interference from the surface," Hoeksema explains. At the peak of the solar cycle, sunspots are numerous. So far in 2009, the sun's surface has been free of sunspots about 80 percent of the time - the most tranquil it's been since 1913.

From a geosynchronous orbit 22,000 miles above Earth's surface, SDO will observe helioseismic waves more precisely than ever before. The current gold standard for observing the sun is a satellite called the Solar and Heliospheric Observatory, or SOHO, which maps helioseismic activity with mega-pixel resolution once every minute or so. HMI will up the ante to 16 megapixels every 45 seconds, resulting in a far more detailed view of the solar interior.

SDO will also improve on SOHO by beaming its torrent of raw data down to Earth unprocessed. Because of limited download bandwidth, SOHO performs some calculations while the data are still onboard the spacecraft. Only the results are beamed to scientists. Since SOHO was launched in 1995, scientists have since devised better ways to process the data and correct for errors. But there's no way they can apply these new techniques to SOHO imagery because the data have already been "crunched" by the time they leave the spacecraft.

To give scientists full access to its original data, SDO will have a continuous, 150 megabit per second download link. In comparison, most home high-speed internet connections are only 1 to 10 megabits per second.

Somewhere in all those p modes will be the telltale signs of solar jet streams, subsurface winds, proto-sunspots, and the solar dynamo itself - all "seen" with unprecedented clarity.

With the sun so calm, now is a great time to look.

Related links:

> Helioseismology (Stanford University)

> Goddard SDO page

> HMI on Twitter

Tuesday, July 07, 2009

Space Station Marathon

Sunlight glints from the space station's solar arrays on May 22, 2009If you've never seen a spaceship with your own eyes, now's your chance.

The International Space Station (ISS) has recently started a remarkable series of flybys over the United States. Beginning the first weekend of July, the station has been appearing once, twice, and sometimes three times a day successively. No matter where you live, you should have at least a few opportunities to see the biggest spaceship ever built.

Check NASA's ISS Tracker for flyby times.

The ISS has been under construction for nearly 11 years, and it has grown very large and very bright. The station is now more than 350 ft wide (wider than a football field), has 12,600 cubic feet of labs and living quarters, and on Earth would weigh about 670,000 lb. Sunlight illuminating the massive outpost makes it shine fifteen times brighter than Sirius, the brightest star in the sky.

Sometimes it is even brighter than that. Sunlight glinting from the station's flat surfaces (mainly solar arrays) produce dazzling flares as much as six hundred times brighter than Sirius. For astronomers: On the scale of visual magnitudes, space station flares register -8.

"The station flared spectacularly on May 22 when it passed over my backyard observatory in the Netherlands," reports amateur astronomer Quintus Oostendorp. "I knew the ISS was coming, so I had my telescope ready and I was able see exactly what happened."

At present, the flares are unpredictable. No one knows when they will happen or exactly how bright they will be. Any given flyby could be interrupted by one-and that's what makes the watch so much fun.

The marathon of space station flybys won't stop until mid-to-late July (depending on your location). That gives space shuttle Endeavour, currently scheduled to launch on July 11, time to reach the space station and join the show. As the shuttle approaches station for docking, many observers will witness a memorable double flyby-Endeavour and the ISS sailing side by side across the starry night sky.

Endeavour is on yet another space station construction mission. This time it will deliver a "space porch" to be added to Japan's Kibo science laboratory module. The porch is not a place where astronauts can sit, relax and watch the stars drift by (although that is not a bad idea); it is a science platform. When an experiment needs to be exposed to the hard vacuum or energetic radiation of space, it can placed outside on the porch to take advantage of the space station's unique research environment. The official name of the porch is the Kibo Japanese Experiment Module Exposed Facility and it will add its own small contribution to the station's reflected luminosity in the night sky.

Coldest Known Objects in Space

Artist's concept of Planck, with Earth in the background.
The detectors of Planck's High Frequency Instrument reached their amazingly low operational temperature of -273.05 degrees Celsius (-459.49 degrees Fahrenheit), making them the coldest known objects in space. The spacecraft has also just entered its final orbit around the second Lagrange point of the sun-Earth system, called L2.

For more information, go to the story on ESA's Planck site at http://www.esa.int/SPECIALS/Planck/SEM0Y5S7NWF_0.html

Ozone, Nitrogen Change the Way Rising CO2 Affects Earth's Water

The diagram shows the microscopic structure of a leaf, and the processes of photosynthesis and transpiration.Through a recent modeling experiment, a team of NASA-funded researchers have found that future concentrations of carbon dioxide and ozone in the atmosphere and of nitrogen in the soil are likely to have an important but overlooked effect on the cycling of water from sky to land to waterways.

The researchers concluded that models of climate change may be underestimating how much water is likely to run off the land and back into the sea as atmospheric chemistry changes. Runoff may be as much as 17 percent higher in forests of the eastern United States when models account for changes in soil nitrogen levels and atmospheric ozone exposure.

"Failure to consider the effects of nitrogen limitation and ozone on photosynthesis can lead us to underestimate regional runoff," said Benjamin Felzer, an ecosystem modeler at Lehigh University in Bethlehem, Pa. "More runoff could mean more contamination and flooding of our waterways. It could also mean fewer droughts than predicted for some areas and more water available for human consumption and farming. Either way, water resource managers need more accurate runoff estimates to plan better for the changes."

Felzer and colleagues from the Massachusetts Institute of Technology (MIT) in Cambridge and the Marine Biology Laboratory in Woods Hole, Mass., published their findings recently in the Journal of Geophysical Research – Biogeosciences.

Plants play a significant role in Earth's water cycle, regulating the amount of water cycling through land ecosystems and how long it stays there. Plants draw in water from the atmosphere and soil, and they discharge it naturally through transpiration, the tail end of photosynthesis when water vapor and oxygen are released into the air.

The amount of water that plants give up depends on how much carbon dioxide is present in the atmosphere. Studies have shown that despite a global drop in rainfall over land in the past 50 years, runoff has actually increased.

Other studies have shown that increasing CO2 is changing how plant "pores," or stomata, discharge water. With elevated CO2 levels, leaf pores contract and sometimes close to conserve internal water reserves. This "stomatal conductance" response increases water use efficiency and reduces the rate of transpiration.

Plants that release less water also take less of it from the environment. With less water being taken up by plants, more water is available for groundwater or runs off the land surface into lakes, streams, and rivers. Along the way, it accumulates excess nutrients and pollutants before emptying into waterways, where it affects the health of fish, algae, and shellfish and contaminate drinking water and beaches. Excess runoff can also contribute to flooding.

Sometimes rising CO2 has the opposite effect, Felzer noted, promoting vegetation growth by increasing the rate of photosynthesis. More plant growth can lead to a thicker canopy of leaves with increased transpiration and less runoff. However, this effect has been shown to be smaller than the effect of reduced stomatal conductance.

Aware of these cycles, Felzer and colleagues used theoretical models to project various future scenarios for the amount of carbon dioxide in the atmosphere and what it would mean to the changing water cycle in forests east of the Mississippi River. They found that runoff would increase anywhere from 3 to 6 percent depending on location and the amount of the increase in CO2.

Felzer and colleagues also examined the role of two other variables -- atmospheric ozone and soil-based nitrogen -- in the changing water cycle. Excess ground-level ozone harms the cells responsible for photosynthesis. Reductions in photosynthesis leads to less transpiration and cycling of water through leaves and more water added to runoff.

In most boreal and temperate forests, the rate of photosynthesis is also limited by the availability of nutrients such as nitrogen in the soil. The less nitrogen in the soil, the slower their rate of photosynthesis and transpiration.

"The increase in runoff is even larger when nitrogen is limited and environments are exposed to high ozone levels," said Felzer. In fact, the team found an additional 7 to 10 percent rise in runoff when nitrogen was limited and ozone exposure increased.

"Though this study focuses on Eastern U.S. forests, we know nitrogen and ozone effects are also important in South America and Europe. One region has seen a net increase and the other a net runoff reduction," said co-author Adam Schlosser of the Center for Global Change Science at MIT. "Our environment and quality of life depend on less uncertainty on this front."

Related Links:

> Importance of carbon-nitrogen interactions and ozone on ecosystem hydrology during the 21st century

> How Plants Can Change Our Climate

> Who is Ben Felzer?

> Ozone's Effects on Plants

Sunday, July 05, 2009

NASA Updates Shuttle Prelaunch Events and Countdown Details

News conferences, events and operating hours for the news center at NASA's Kennedy Space Center, Fla., have been updated for the launch of space shuttle Endeavour. The shuttle's STS-127 mission to the International Space Station is scheduled to lift off at 7:39 p.m. EDT on Saturday, July 11.

On Tuesday, July 7, Endeavour's seven astronauts are scheduled to arrive at Kennedy at about 2 p.m. NASA Television will provide live coverage as Commander Mark Polansky makes a brief statement to reporters. Badged journalists planning to cover the event must be at Kennedy's news center by 12:30 p.m. for transportation to the Shuttle Landing Facility.

NASA will provide continuous STS-127 online updates, including a webcast and a blog at:

http://www.nasa.gov/shuttle

On launch day, a blog originating from Kennedy will update the countdown beginning at 2:30 p.m. The blog is the definitive Internet source for information leading up to launch. During the mission, visitors to NASA's shuttle Web site can read about the crew's progress and watch the spacewalks live. As Endeavour's flight wraps up, NASA will offer a blog detailing the spacecraft's return to Earth.

Live updates to the NASA Twitter feed will be added throughout the shuttle launch countdown from Kennedy. To access the NASA Twitter feed, visit:

http://www.twitter.com/nasa

Detailed lists of countdown milestones, news briefing times and participants, and hours of operation for Kennedy's news center and media credentialing office are available at:

http://www.nasa.gov/mission_pages/shuttle/news

For NASA TV streaming video, scheduling and downlink information, visit:

http://www.nasa.gov/ntv

NASA Phoenix Results Point to Martian Climate Cycles

Trenches dug by PhoenixMosaic of images from the Surface Stereo Imager camera on NASA's Phoenix Mars LanderFavorable chemistry and episodes with thin films of liquid water during ongoing, long-term climate cycles may sometimes make the area where NASA's Phoenix Mars mission landed last year a favorable environment for microbes.

Interpretations of data that Phoenix returned during its five months of operation on a Martian arctic plain fill four papers in this week's edition of the journal Science, the first major peer-reviewed reports on the mission's findings. Phoenix ended communications in November 2008 as the approach of Martian winter depleted energy from the lander's solar panels.

"Not only did we find water ice, as expected, but the soil chemistry and minerals we observed lead us to believe this site had a wetter and warmer climate in the recent past -- the last few million years -- and could again in the future," said Phoenix Principal Investigator Peter Smith of the University of Arizona, Tucson.

A paper about Phoenix water studies, for which Smith is the lead author with 36 coauthors from six nations, cites clues supporting an interpretation that the soil has had films of liquid water in the recent past. The evidence for water and potential nutrients "implies that this region could have previously met the criteria for habitability" during portions of continuing climate cycles, these authors conclude.

The mission's biggest surprise was finding a multi-talented chemical named perchlorate in the Martian soil. This Phoenix finding caps a growing emphasis on the planet's chemistry, said Michael Hecht of NASA's Jet Propulsion Laboratory, Pasadena, Calif., who has 10 coauthors on a paper about Phoenix's soluble-chemistry findings.

"The study of Mars is in transition from a follow-the-water stage to a follow-the-chemistry stage," Hecht said. "With perchlorate, for example, we see links to atmospheric humidity, soil moisture, a possible energy source for microbes, even a possible resource for humans."

Perchlorate, which strongly attracts water, makes up a few tenths of a percent of the composition in all three soil samples analyzed by Phoenix's wet chemistry laboratory. It could pull humidity from the Martian air. At higher concentrations, it might combine with water as a brine that stays liquid at Martian surface temperatures. Some microbes on Earth use perchlorate as food. Human explorers might find it useful as rocket fuel or for generating oxygen.

Another surprise from Phoenix was finding ice clouds and precipitation more Earth-like than anticipated. The lander's Canadian laser instrument for studying the atmosphere detected snow falling from clouds. In one of this week's reports, Jim Whiteway of York University, Toronto, and 22 coauthors say that, further into winter than Phoenix operated, this precipitation would result in a seasonal buildup of water ice on and in the ground.

"Before Phoenix we did not know whether precipitation occurs on Mars," Whiteway said. "We knew that the polar ice cap advances as far south as the Phoenix site in winter, but we did not know how the water vapor moved from the atmosphere to ice on the ground. Now we know that it does snow, and that this is part of the hydrological cycle on Mars."

Evidence that water ice in the area sometimes thaws enough to moisten the soil comes from finding calcium carbonate in soil heated in the lander's analytic ovens or mixed with acid in the wet chemistry laboratory. The University of Arizona's William Boynton and 13 coauthors report that the amount of calcium carbonate "is most consistent with formation in the past by the interaction of atmospheric carbon dioxide with liquid films of water on particle surfaces."

The new reports leave unsettled whether soil samples scooped up by Phoenix contained any carbon-based organic compounds. The perchlorate could have broken down simple organic compounds during heating of soil samples in the ovens, preventing clear detection.

The heating in ovens did not drive off any water vapor at temperatures lower than 295 degrees Celsius (563 degrees Fahrenheit), indicating the soil held no water adhering to soil particles. Climate cycles resulting from changes in the tilt and orbit of Mars on scales of hundreds of thousands of years or more could explain why effects of moist soil are present.

The Phoenix mission was led by Smith at the University of Arizona with project management at JPL and development partnership at Lockheed Martin, Denver. Information and images from the mission are available online at http://phoenix.lpl.arizona.edu and http://www.nasa.gov/phoenix .

Saluting Our Nation's Independence

 Saluting Our Nation

NASA Dryden's four F/A-18 mission support aircraft flew in formation for a pilot proficiency flight on Nov. 24, 2008, in this image. NASA Dryden photographer Tom Tschida created this composite image from an original image taken by Carla Thomas.

A Super-Efficient Particle Accelerator

A Super-Efficient Particle AcceleratorThis image, created from data obtained from NASA's Chandra X-ray Observatory and the European Southern Observatory's Very Large Telescope, shows a part of the roughly circular supernova remnant known as RCW 86. This remnant of an exploded star may be the one observed in 185 AD by Chinese astronomers. By studying it, astronomers gained a better understanding of new details about the role of supernova remnants as the Milky Way's super-efficient particle accelerator

Thursday, July 02, 2009

NASA's Fermi Telescope Probes Dozens of Pulsars

With NASA's Fermi Gamma-ray Space Telescope, astronomers now are getting their best look at those whirling stellar cinders known as pulsars. In two studies published in the July 2 edition of Science Express, international teams have analyzed gamma-rays from two dozen pulsars, including 16 discovered by Fermi. Fermi is the first spacecraft able to identify pulsars by their gamma-ray emission alone.

A pulsar is the rapidly spinning and highly magnetized core left behind when a massive star explodes. Most of the 1,800 cataloged pulsars were found through their periodic radio emissions. Astronomers believe these pulses are caused by narrow, lighthouse-like radio beams emanating from the pulsar's magnetic poles.

"Fermi has truly unprecedented power for discovering and studying gamma-ray pulsars," said Paul Ray of the Naval Research Laboratory in Washington. "Since the demise of the Compton Gamma Ray Observatory a decade ago, we've wondered about the nature of unidentified gamma-ray sources it detected in our galaxy. These studies from Fermi lift the veil on many of them."

The Vela pulsar, which spins 11 times a second, is the brightest persistent source of gamma rays in the sky. Yet gamma rays -- the most energetic form of light -- are few and far between. Even Fermi's Large Area Telescope sees only about one gamma-ray photon from Vela every two minutes.

"That's about one photon for every thousand Vela rotations," said Marcus Ziegler, a member of the team reporting on the new pulsars at the University of California, Santa Cruz. "From the faintest pulsar we studied, we see only two gamma-ray photons a day."

Radio telescopes on Earth can detect a pulsar easily only if one of the narrow radio beams happens to swing our way. If not, the pulsar can remain hidden.

A pulsar's radio beams represent only a few parts per million of its total power, whereas its gamma rays account for 10 percent or more. Somehow, pulsars are able to accelerate particles to speeds near that of light. These particles emit a broad beam of gamma rays as they arc along curved magnetic field lines.

All-sky map image showing the positions and names of 16 new pulsars
This all-sky map shows the positions and names of 16 new pulsars (yellow) and eight millisecond pulsars (magenta) studied using Fermi's LAT. The famous Vela, Crab, and Geminga pulsars (right) are the brightest ones Fermi sees. The pulsars Taz, Eel, and Rabbit have taken the nicknames of nebulae they are now known to power. The Gamma Cygni pulsar resides within a supernova remnant of the same name.
Credit: NASA/DOE/Fermi LAT Collaboration
> Larger image
> Larger image (unlabeled)

The new pulsars were discovered as part of a comprehensive search for periodic gamma-ray fluctuations using five months of Fermi Large Area Telescope data and new computational techniques.

"Before launch, some predicted Fermi might uncover a handful of new pulsars during its mission," Ziegler added. "To discover 16 in its first five months of operation is really beyond our wildest dreams."

Like spinning tops, pulsars slow down as they lose energy. Eventually, they spin too slowly to power their characteristic emissions and become undetectable.

But pair a slowed dormant pulsar with a normal star, and a stream of stellar matter from the companion can spill onto the pulsar and increase its spin. At rotation periods between 100 and 1,000 times a second, ancient pulsars can resume the activity of their youth. In the second study, Fermi scientists examined gamma rays from eight of these "born-again" pulsars, all of which were previously discovered at radio wavelengths.

"Before Fermi launched, it wasn't clear that pulsars with millisecond periods could emit gamma rays at all," said Lucas Guillemot at the Center for Nuclear Studies in Gradignan, near Bordeaux, France. "Now we know they do. It's also clear that, despite their differences, both normal and millisecond pulsars share similar mechanisms for emitting gamma rays."

NASA's Fermi Gamma-ray Space Telescope is an astrophysics and particle physics partnership, developed in collaboration with the U.S. Department of Energy, along with important contributions from academic institutions and partners in France, Germany, Italy, Japan, Sweden, and the U.S.

Nobel Prize Winner and NASA's Blueshift Podcast Take You on a Data Journey

Dr. John C. Mather is a Senior Astrophysicist in the Observational Cosmology Laboratory at NASA's Goddard Space Flight Center.Dr. John Mather, a Nobel Prize-winning astrophysicist at NASA's Goddard Space Flight Center in Greenbelt, Md. joined the Blueshift podcast on June 18th to share his sense of what makes scientific data beautiful. "I think it's worth a lot of attention to portraying the information in the best possible graphic way," he said. "Data are beautiful when they tell a story."

Blueshift, a series of podcasts produced by Goddard's Astrophysics Science Division, offers listeners a backstage pass to the division's groundbreaking discoveries, innovative technology, new missions, and other exciting stories.

"Blueshift's summer series kicks off with Dr. Mather's interview," said Sara Mitchell, Director of Blueshift."This four part series will follow the stories of missions, scientists, and iconic images as we see how science data is captured and communicated." Podcast listeners will find additional material and images related to each show on the Blueshift web site.

In the episode, John Mather describes how science and data are communicated -- and the absolute importance of imagery to share data so the world can understand it. In 2006, both he and George Smoot at the University of California, Berkeley, Calif., shared the Nobel Prize in Physics. They won for their work on NASA's Cosmic Background Explorer, a satellite that mapped radiation emitted when the universe was less than 400,000 years. The mission created the first-ever "baby picture" of the cosmos.

If you think that satellites just relay the images that we see here on Earth, you'll be in for a big surprise. Dr. Mather discusses how data are assembled, polished and transformed into images, animations and illustrations.

Mather also describes how the new James Webb Space Telescope, slated for launch in 2014, will build upon the valuable science and breathtaking imagery of Hubble. Webb will see the most distant objects in the cosmos and take astrophysicists further back in time than ever before!

The term "blueshift" relates to a change in the spectrum of an object that is moving toward us. "We chose Blueshift because we aim to bring the universe of astrophysics at Goddard directly to our listeners," Mitchell said.

To learn more about Blueshift, subscribe to the podcast or listen to archived episodes, please visit:

http://universe.nasa.gov/blueshift

Five Things About Hurricanes

Hurricane Gustav moved along the southern side of Jamaica on Aug. 29, 2008.JPL scientist Bjorn LambrigtsenJPL scientist Bjorn Lambrigtsen goes on hurricane watch every June. He is part of a large effort to track hurricanes and understand what powers them. Lambrigtsen specializes in the field of microwave instruments, which fly aboard research planes and spacecraft, penetrating through thick clouds to see the heart of a hurricane. While scientists are adept at predicting where these powerful storms will hit land, there are crucial aspects they still need to wrench from these potentially killer storms.

Here are thoughts and factoids from Lambrigtsen in the field of hurricane research.

1. Pinpointing the moment of birth

Most Atlantic hurricanes start as a collection of thunderstorms off the coast of Africa. These storm clusters move across the Atlantic, ending up in the Caribbean, Gulf of Mexico or Central America. While only one in 10 of these clusters evolve into hurricanes, scientists do not yet know what triggers this powerful transformation. Pinpointing a hurricane's origin will be a major goal of a joint field campaign in 2010 between NASA and the National Oceanic and Atmospheric Administration (NOAA).

2. Predicting intensity

Another focus of next year's research campaign will be learning how to better predict a storm's intensity. It is difficult for emergency personnel and the public to gauge storm preparations when they don't know if the storm will be mild or one with tremendous force. NASA's uncrewed Global Hawk will be added to the 2010 research armada. This drone airplane, which can fly for 30 straight hours, will provide an unprecedented long-duration view of hurricanes in action, giving a window into what fuels storm intensity.

3. Deadly force raining down

Think about a hurricane. You imagine high, gusting winds and pounding waves. However, one of the deadliest hurricanes in recent history was one that parked itself over Central America in October 1998 and dumped torrential rain. Even with diminished winds, rain from Hurricane Mitch reached a rate of more than 4 inches per hour. This caused catastrophic floods and landslides throughout the region.

4. Replenishing "spring"

Even though hurricanes can wreak havoc, they also carry out the important task of replenishing the freshwater supply along the Florida and southeastern U.S. coast and Gulf of Mexico. The freshwater deposited is good for the fish and the ecological environment.

5. One size doesn't fit all

Hurricanes come in a huge a variety of sizes. Massive ones can cover the entire Gulf of Mexico (about 1,000 miles across), while others are just as deadly at only 100 miles across. This is a mystery scientists are still trying to unravel.

NASA and NOAA conduct joint field campaigns to study hurricanes. The agencies use research planes to fly through and above hurricanes, and scientists collect data from NASA spacecraft that fly overhead. NOAA, along with its National Hurricane Center, is the U.S. government agency tasked with hurricane forecasting.

For more information on how NASA and JPL study hurricanes, go towww.nasa.gov/hurricane and http://tropicalcyclone.jpl.nasa.gov

Tanking Test Complete; STS-127 on Track for July 11 Launch

A test fueling of space shuttle Endeavour's external tank revealed no gaseous hydrogen leaks, verifying recent repairs were successful, NASA managers confirmed during a Wednesday afternoon news conference at NASA's Kennedy Space Center in Florida.

The tanking test began at 6:52 a.m. EDT Wednesday. During the next three hours, teams in the Launch Control Center watched closely for signs of a leak as liquid oxygen and liquid hydrogen poured into the massive orange tank. Previous attempts to launch Endeavour on the STS-127 mission were scrubbed by a leak in the area of the Ground Umbilical Carrier Plate, which attaches a gaseous hydrogen vent line to the external tank. Crews worked tirelessly to investigate and repair the problem.

"There were absolutely no leak indications whatsoever noted on the two leak detectors," said Launch Director Pete Nickolenko. "We'll continue to look at the data, and our next step is to move toward launch."

Endeavour's launch is targeted for July 11 at 7:39 p.m.

Space Shuttle Mission: STS-127

Space shuttle Endeavour undergoes a tanking test Wednesday, July 1.
STS-127 Mission Overview
The 16-day mission will feature five spacewalks and complete construction of the Japan Aerospace Exploration Agency's Kibo laboratory. Astronauts will attach a platform to the outside of the Japanese module that will allow experiments to be exposed to space.

The STS-127 crew members are Commander Mark Polansky, Pilot Doug Hurley and Mission Specialists Dave Wolf, Christopher Cassidy, Tom Marshburn, Tim Kopra and Canadian Space Agency astronaut Julie Payette. Kopra will join the space station crew and replace Japanese astronaut Koichi Wakata. Wakata will return to Earth on Endeavour to conclude a three-month stay at the station.

STS-127 Additional Resources
Mission Press Kit (6.9 Mb PDF)
Mission Summary (429 Kb PDF)
Meet the STS-127 Crew
Flow Valve Fact Sheet (447 Kb PDF)

 

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