See Spot on Jupiter. See Spot Glow.

Jupiter's Great Red Spot
New thermal images from powerful ground-based telescopes show swirls of warmer air and cooler regions never seen before within Jupiter's Great Red Spot. Image credit: NASA/JPL/ESO and NASA/ESA/GSFC
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New thermal images from powerful ground-based telescopes show swirls of warmer air and cooler regions never seen before within Jupiter's Great Red Spot, enabling scientists to make the first detailed interior weather map of the giant storm system.

The observations reveal that the reddest color of the Great Red Spot corresponds to a warm core within the otherwise cold storm system, and images show dark lanes at the edge of the storm where gases are descending into the deeper regions of the planet. These types of data, detailed in a paper appearing in the journal Icarus, give scientists a sense of the circulation patterns within the solar system's best-known storm system.

"This is our first detailed look inside the biggest storm of the solar system," said Glenn Orton, a senior research scientist at NASA's Jet Propulsion Laboratory in Pasadena, Calif., who was one of the authors of the paper. "We once thought the Great Red Spot was a plain old oval without much structure, but these new results show that it is, in fact, extremely complicated."

Sky gazers have been observing the Great Red Spot in one form or another for hundreds of years, with continuous observations of its current shape dating back to the 19th century. The spot, which is a cold region averaging about 110 Kelvin (minus 260 degrees Fahrenheit) is so wide about three Earths could fit inside its boundaries.

The thermal images obtained by giant 8-meter (26-foot) telescopes used for this study -- the European Southern Observatory's Very Large Telescope in Chile, the Gemini Observatory telescope in Chile and the National Astronomical Observatory of Japan's Subaru telescope in Hawaii -- have provided an unprecedented level of resolution and extended the coverage provided by NASA's Galileo spacecraft in the late 1990s. Together with observations of the deep cloud structure by the 3-meter (10-foot) NASA Infrared Telescope Facility in Hawaii, the level of thermal detail observed from these giant observatories is comparable to visible-light images from NASA's Hubble Space Telescope for the first time.

One of the most intriguing findings shows the most intense orange-red central part of the spot is about 3 to 4 Kelvin (5 to 7 degrees Fahrenheit) warmer than the environment around it, said Leigh Fletcher, the lead author of the paper, who completed much of the research as a postdoctoral fellow at JPL and is currently a fellow at the University of Oxford in England. This temperature differential might not seem like a lot, but it is enough to allow the storm circulation, usually counter-clockwise, to shift to a weak clockwise circulation in the very middle of the storm. Not only that, but on other parts of Jupiter, the temperature change is enough to alter wind velocities and affect cloud patterns in the belts and zones.

"This is the first time we can say that there's an intimate link between environmental conditions -- temperature, winds, pressure and composition - and the actual color of the Great Red Spot," Fletcher said. "Although we can speculate, we still don't know for sure which chemicals or processes are causing that deep red color, but we do know now that it is related to changes in the environmental conditions right in the heart of the storm."

Unlocking the secrets of Jupiter's giant storm systems will be one of the targets for infrared spacecraft observations from future missions including NASA's Juno mission.

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WISE Captures a Cosmic Rose

A new infrared image from NASA's Wide-field Infrared Survey  Explorer, or WISE, shows a cosmic rosebud blossoming with new stars.
A new infrared image from NASA's Wide-field Infrared Survey Explorer, or WISE, shows a cosmic rosebud blossoming with new stars. Image credit: NASA/JPL-Caltech/UCLA
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A new infrared image from NASA's Wide-field Infrared Survey Explorer, or WISE, shows a cosmic rosebud blossoming with new stars. The stars, called the Berkeley 59 cluster, are the blue dots to the right of the image center. They are ripening out of the dust cloud from which they formed, and at just a few million years old, are young on stellar time scales.

The rosebud-like red glow surrounding the hot, young stars is warm dust heated by the stars. Green "leafy" nebulosity enfolds the cluster, showing the edges of the dense, dusty cloud. This green material is from heated polycyclic aromatic hydrocarbons, molecules that can be found on Earth in barbecue pits, exhaust pipes and other places where combustion has occurred.

Red sources within the green nebula indicate a second generation of stars forming at the surface of the natal cloud, possibly as a consequence of heating and compression from the younger stars. A supernova remnant associated with this region, called NGC 7822, indicates that a massive star has already exploded, blowing the cloud open in a "champagne flow" and leaving behind this floral remnant. Blue dots sprinkled throughout are foreground stars in our Milky Way galaxy.

Berkeley 59 and NGC 7822 are located in the constellation of Cepheus at a distance of about 3,300 light-years from Earth.

Infrared light is color coded in this picture as follows: blue shows 3.4-micron light; cyan, 4.6-micron light; green, 12-micron light; and red, 22-micron light.

JPL manages the Wide-field Infrared Survey Explorer for NASA's Science Mission Directorate, Washington. The principal investigator, Edward Wright, is at UCLA. The mission was competitively selected under NASA's Explorers Program managed by the Goddard Space Flight Center, Greenbelt, Md. The science instrument was built by the Space Dynamics Laboratory, Logan, Utah, and the spacecraft was built by Ball Aerospace & Technologies Corp., Boulder, Colo. Science operations and data processing take place at the Infrared Processing and Analysis Center at the California Institute of Technology in Pasadena. Caltech manages JPL for NASA. More information is online at http://www.nasa.gov/wise . Additional images are at http://wise.astro.ucla.edu .

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The Wizard Nebula

The Wizard Nebula
This image of the open star cluster NGC 7380, also known as the Wizard Nebula, is a mosaic of images from the WISE mission spanning an area on the sky of about 5 times the size of the full moon. NGC 7380 is located in the constellation Cepheus about 7,000 light-years from Earth within the Milky Way Galaxy. The star cluster is embedded in a nebula, which spans some 110 light-years. The stars of NGC 7380 have emerged from this star-forming region in the last 5 million years or so, making it a relatively young cluster.

WISE, the Wide-field Infrared Survey Explorer mission, scans the entire sky in infrared light, picking up the glow of hundreds of millions of objects and producing millions of images. The mission is designed to uncover objects never seen before, including the coolest stars, the universe's most luminous galaxies and some of the darkest near-Earth asteroids and comets. Its vast catalogs will help answer fundamental questions about the origins of planets, stars and galaxies.

WISE joins two other infrared missions in space -- NASA's Spitzer Space Telescope and the Herschel Space Observatory, a European Space Agency mission. WISE is different from these missions in that it will survey the entire sky. It is designed to cast a wide net to catch all sorts of unseen cosmic treasures, including rare oddities. All four infrared detectors aboard WISE were used to make this image.

NGC 7380 was discovered by Caroline Herschel in 1787. Her brother, William Herschel, discovered infrared light in 1800.

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IMAX Premieres ‘Hubble 3D’ on Friday, March 19

Narrated by award-winning actor Leonardo DiCaprio, a film documenting the STS-125 shuttle mission to upgrade the Hubble Space Telescope will arrive in theaters on Friday, March 19. The film is a joint venture between NASA, the IMAX Corporation and Warner Bros. Pictures.

The IMAX 3-D cameras launched aboard space shuttle Atlantis on May 11, 2009, during the STS-125 mission to repair the Hubble Space Telescope. Astronauts use dthe cameras to document the mission's five spacewalks to repair and upgrade Hubble. The IMAX footage will be combined with breathtaking detailed images of distant galaxies from Hubble.

The IMAX team trained Atlantis' crew at NASA's Johnson Space Center in Houston to operate the cameras. One was mounted outside the crew cabin in the shuttle's cargo bay to capture IMAX 3-D images of the historic final servicing mission. The commander and pilot will double as filmmakers as two teams of spacewalking astronauts -- working in tandem with the shuttle's robotic arm -- perform some of the most challenging work ever undertaken in space as they replace and refurbish many of the telescope's precision instruments.

Through the world's most immersive cinematic experience, "Hubble 3D" will give audiences a front row seat as the story unfolds. It will reveal the cosmos as never before, allowing viewers of all ages to explore the grandeur of the nebulae and galaxies, the birth and death of stars, and some of the greatest mysteries of our celestial surroundings, all in IMAX 3-D.

IMAX's longstanding partnership with NASA has enabled millions of people to travel into space through a series of award-winning IMAX films. The IMAX 3-D camera made its first voyage into space in 2001 for the production of "Space Station 3D." The "Hubble 3D" film mark Warner Bros. Pictures' first venture into space.

For more information and additional Webisodes, visit http://www.imax.com/hubble/.

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NASA Ames ‘Tops Out’ First Building in Thirty Years

The final beam was placed as the building, called Sustainability Base, reached its height and completed its skeletal structure"Beam me up!" was the message signed on the final beam hoisted into place on the iron skeleton of NASA’s new building, called Sustainability Base, Friday, March 12, 2010.

Although not yet completed, Sustainability Base has begun ushering in a new era of innovation, good will and renewed American tradition. Under construction at NASA’s Ames Research Center, Moffett Field, Calif., the building advances the standard for what it means to be “green.” Sustainability Base is expected to achieve a platinum rating under the Leadership in Energy and Environmental Design (LEED) standards for environmentally sustainable. The building, however, goes beyond LEED to serve as a showcase of NASA and partner ingenuity, incorporating technologies designed for space exploration and applied to improve life here on our home planet. Sustainability Base will be a window to the future on Earth.

"It will be one of the greenest and highest performance building in the federal government," said Steve Zornetzer, associate administrator of NASA Ames. "Today is a good day to celebrate. It's a good day to stop, reflect and show appreciation for work that was well done."

It will be one of the greenest and highest performance buildings in the federal government, said Steve Zornetzer, associate administrator of NASA AmesTogether, NASA and Swinerton Builders workers and management signed the final beam as part of a celebration, called the "Topping Out." No one really knows how or when it originated, but the tradition places an evergreen tree, a flag or both on the last beam as it is lifted into place, it signifies the structure has reached its height and the skeleton is completed.

"As a company, we are proud to be part of a green effort that is so successful," said Dan Beyer, vice president of Swinerton Builders., San Francisco, Calif. "The tree signifies new growth as the building construction comes to fruition and is used over time; the flag represents who we are as Americans."

Over the years, the Topping Out custom remains important to ironworkers in the steel construction industry. For some, the evergreen symbolizes the successful completion of construction without loss of life, for others, it’s a good luck charm for the occupants. Similarly, the flag also has multiple meanings: the construction of a federal building, patriotism, or the American dream. Whatever the interpretation, it welcomes the future while providing a link with the past.

"We need buildings like this to bring back America," said John W. Elwood, vice president of Swinerton, Builders, Santa Clara, Calif. "The flag represents our full support for our country and our American troops. The evergreen tree is our good luck charm."

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UV exposure has increased over the last 30 years, but stabilized since the mid-1990s

Ultraviolet radiation can damage DNA by distorting its structureNASA scientists analyzing 30 years of satellite data have found that the amount of ultraviolet (UV) radiation reaching Earth's surface has increased markedly over the last three decades. Most of the increase has occurred in the mid-and-high latitudes, and there's been little or no increase in tropical regions.

The new analysis shows, for example, that at one line of latitude — 32.5 degrees — a line that runs through central Texas in the northern hemisphere and the country of Uruguay in the southern hemisphere, 305 nanometer UV levels have gone up by some 6 percent on average since 1979.

The primary culprit: decreasing levels of stratospheric ozone, a colorless gas that acts as Earth’s natural sunscreen by shielding the surface from damaging UV radiation.

The finding reinforces previous observations that show UV levels are stabilizing after countries began signing an international treaty that limited the emissions of ozone-depleting gases in 1987. The study also shows that increased cloudiness in the southern hemisphere over the 30-year period has impacted UV.

Jay Herman, a scientist at NASA's Goddard Space Flight Center in Greenbelt, Md., stitched together data from several earth observing satellites — including NASA's Aura satellite, NOAA weather satellites, and commercial satellites — to draw his conclusions. The results were published in the Journal of Geophysical Research in February.

"Overall, we're still not where we'd like to be with ozone, but we're on the rightThe high latitudes of the southern hemisphere have seen ultraviolet exposure increase by as much as a quarter track," said Jay Herman. "We do still see an increase in UV on a 30-year timescale, but it's moderate, it could have been worse, and it appears to have leveled off."

In the tropics, the increase has been minimal, but in the mid-latitudes it has been more obvious. During the summer, for example, UV has increased by more than 20 percent in Patagonia and the southern portions of South America. It has risen by nearly 10 percent in Buenos Aires, a city that's about the same distance from the equator as Little Rock, Ark. At Washington, D.C.'s latitude — about 35 degrees north — UV has increased by about 9 percent since 1979.

The southern hemisphere tends to have more UV exposure because of the ozone hole, a seasonal depletion of the ozone layer centered on the South Pole. There are also fewer particles of air pollution — which help block UV — due to the comparatively small numbers of people who live in the southern hemisphere.

Despite the overall increases, there are clear signs that ultraviolet radiation levels are on the verge of falling. Herman's analysis, which is in agreement with a World Meteorological Report published in recent years, shows that decreases in ozone and corresponding increases in UV irradiance leveled off in the mid-nineties.

The Many Sides of Radiation
The largest increases in UV (shown in white, red, orange, and yellow) have occurred in the southern hemisphere during summers
Shorter ultraviolet wavelengths of light contain more energy than the infrared or visible portions of sunlight that reach Earth’s surface. Because of this, UV photons can break atmospheric chemical bonds and cause complex health effects.

Longer wavelengths (from 320 to 400 nanometers) — called UV-A — cause sunburn and cataracts. Yet, UV-A can also improve health by spurring the production of Vitamin D, a substance that's critical for calcium absorption in bones and that helps stave off a variety of chronic diseases.

UV-B, which has slightly shorter wavelengths (from 320 to 290 nanometers), damages DNA by tangling and distorting its ladder-like structure, causing a range of health problems such as skin cancer and diseases affecting the immune system.

As part of his study, Herman developed a mathematical technique to quantify the biological impacts of UV exposure. He examined and calculated how changing levels of ozone and ultraviolet irradiance affect life. For Greenbelt, Md., for example, he calculated that a 7 percent increase in UV yielded a 4.4 percent increase in the damage to skin, a 4.8 percent increase in damage to DNA, a 5 percent increase in Vitamin D production, and less than a percent of increase in plant growth.

"If you go to the beach these days, you're at slightly higher risk of getting skin cancer (without protection)," Herman said, though he noted the risk would have been even greater in the absence of regulations on ozone-depleting substances.
Electromagnetic radiation exists in a range of wavelengths, which are delineated into major divisions for our convenience
Last year, one of Herman's Goddard colleagues, Paul Newman, published a study showing that the ozone hole likely would have become a year-round fixture and UV radiation would increase 650 percent by 2065 in mid-latitude cities if not for the Montreal Protocol, an international treaty signed in 1987 that limited the amount of ozone-depleting gases countries could emit.

Clouds and Hemispheric Dimming

In addition to analyzing ozone and ultraviolet trends, Herman also used satellite data to study whether changes in cloudiness have affected UV trends. To his surprise, he found that increased cloudiness in the southern hemisphere produced a dimming effect that increased the shielding from UV compared to previous years.

In the higher latitudes especially, he detected a slight reduction — typically of 2 to 4 percent -- in the amount of UV passing through the atmosphere and reaching the surface due to clouds. "It’s not a large amount, but it’s intriguing," Herman said. "We aren’t sure what’s behind it yet."

Vitali Fioletov, a Canadian scientist and member of the World Meteorological Organization's advisory group on ultraviolet radiation, agreed that Herman’s findings about cloudiness warrant additional investigation. "I found the cloud effects on the global scale to be the most interesting aspect of the study,” he said. "This isn't something you could see without satellites."

Herman synthesized measurements from the Total Ozone Mapping Spectrometer (TOMS) aboard Nimbus 7 and Earth Probe, the Ozone Monitoring Instrument (OMI) on NASA’s Aura satellite, NASA’s Sea-Viewing Wide Field-of-view sensor (SeaWiFS) on the commercial SeaStar satellite, and the Solar Backscatter Ultraviolet Instrument (SBUV) on several polar orbiting NOAA weather satellites.

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RSS rollback, payload to the pad delayed at least 24 hours

Last night, while venting shuttle Discovery's aft fuel propellant tanks in preparation for fuel loading, the Right Reaction Control System (RRCS) fuel helium tank pressure unexpectedly decreased in unison with the RRCS fuel propellant tank.

Troubleshooting overnight revealed at least one helium isolation valve that is leaking or is remaining in the open position when it is expected to be closed.

Following a review meeting this morning, engineers have decided to complete Orbital Maneuvering System (OMS) Reaction Control System fuel loading, Solid Rocket Booster Hydraulic Power Unit (HPU) tilt system and Auxiliary Power Unit (APU) hydrazine loads this weekend.

Engineers will meet again Monday morning to discuss options.

Currently, Rotating Service Structure (RSS) rotation will be delayed to no earlier than Tuesday, March 16; and payload delivery to the pad will be delayed to no earlier than Wednesday, March 17.

Launch still is targeted for April 5.

Space Shuttle Mission: STS-131

STS-131 Commander Alan Poindexter and  Mission Specialist Dorothy Metcalf-Lindenburger in T-38 jet.
Image above: STS-131 Commander Alan Poindexter and Mission Specialist Dorothy Metcalf-Lindenburger prepare for take off in a NASA T-38 trainer jet.
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› Meet the STS-131 Crew

Discovery and Crew Prepare for STS-131 Mission
Commander Alan Poindexter is set to lead the STS-131 mission to the International Space Station aboard space shuttle Discovery. Joining Poindexter will be Pilot Jim Dutton and Mission Specialists Rick Mastracchio, Clay Anderson, Dorothy Metcalf-Lindenburger, Stephanie Wilson and Naoko Yamazaki of the Japan Aerospace Exploration Agency.

Discovery will carry a multi-purpose logistics module filled with science racks for the laboratories aboard the station. The mission has three planned spacewalks, with work to include replacing an ammonia tank assembly, retrieving a Japanese experiment from the station’s exterior, and switching out a rate gyro assembly on the S0 segment of the station’s truss structure.

STS-131 will be the 33rd shuttle mission to the station.

Additional Resources

› Reusable Solid Rocket Motor and Solid Rocket Boosters

Orbiter Status

› About the Orbiters

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Solar ‘Current of Fire’ Speeds Up

In today's issue of Science, NASA solar physicist David Hathaway reports that the top of the sun's Great Conveyor Belt has been running at record-high speeds for the past five years.

"I believe this could explain the unusually deep solar minimum we've been experiencing," says Hathaway. "The high speed of the conveyor belt challenges existing models of the solar cycle and it has forced us back to the drawing board for new ideas."

The Great Conveyor Belt is a massive circulating current of fire (hot plasma) within the sun. It has two branches, north and south, each taking about 40 years to complete one circuit. Researchers believe the turning of the belt controls the sunspot cycle.

Right: An artist's concept of the sun's Great Conveyor Belt. [larger image]

Hathaway has been monitoring the conveyor belt using data from the Solar and Heliospheric Observatory (SOHO). The top of the belt skims the surface of the sun, sweeping up knots of solar magnetism and carrying them toward the poles. SOHO is able to track those knots—Hathaway calls them "magnetic elements"--and thus reveal the speed of the underlying flow.

"It's a little like measuring the speed of a river on Earth by clocking the leaves and twigs floating downstream," Hathaway explains.

SOHO's dataset extends all the way back to 1996 and spans a complete solar cycle. Last year, Lisa Rightmire, a student of Hathaway from the University of Memphis, spent the entire summer measuring magnetic elements. When she plotted their speeds vs. time, she noticed how fast the conveyor belt has been going.

A note about "fast": The Great Conveyor Belt is one of the biggest things in the whole solar system and by human standards it moves with massive slowness. "Fast" in this context means 10 to 15 meters per second (20 to 30 miles per hour). A good bicyclist could easily keep up.

Below: The velocity of the Great Conveyor Belt (a.k.a. "meridianal flow") since 1996. Note the higher speeds after ~2004. credit: Hathaway and Rightmire, 2010. [larger image]

The speed-up was surprising on two levels.

First, it coincided with the deepest solar minimum in nearly 100 years, contradicting models that say a fast-moving belt should boost sunspot production. The basic idea is that the belt sweeps up magnetic fields from the sun's surface and drags them down to the sun's inner dynamo. There the fields are amplified to form the underpinnings of new sunspots. A fast-moving belt should accelerate this process.

So where have all the sunspots been? The solar minimum of 2008-2009 was unusually deep and now the sun appears to be on the verge of a weak solar cycle.

Instead of boosting sunspots, Hathaway believes that a fast-moving Conveyor Belt can instead suppress them "by counteracting magnetic diffusion at the sun's equator." He describes the process in detail in Science ("Variations in the Sun's Meridional Flow over a Solar Cycle," 12 March 2010, v327, 1350-1352).

The second surprise has to do with the bottom of the Conveyor Belt.

SOHO can only clock the motions of the visible top layer. The bottom is hidden by ~200,000 kilometers of overlying plasma. Nevertheless, an estimate of its speed can be made by tracking sunspots.

"Sunspots are supposedly rooted to the bottom of the belt," says Hathaway. "So the motion of sunspots tells us how fast the belt is moving down there."

He's done that—plotted sunspot speeds vs. time since 1996—and the results don't make sense. "While the top of the conveyor belt has been moving at record-high speed, the bottom seems to be moving at record-low speed. Another contradiction."

Right: An artist's concept of the Solar Dynamics Observatory (SDO). Launched in Feb. 2010, SDO will be able to look inside the sun to study the conveyor belt in greater detail, perhaps solving the mysteries Hathaway and Rightmire have uncovered. [larger image]

Could it be that sunspots are not rooted to the bottom of the Conveyor Belt, after all? "That's one possibility" he notes. "Sunspots could be moving because of dynamo waves or some other phenomenon not directly linked to the belt."

What researchers really need is a good look deep inside the sun. NASA's Solar Dynamics Observatory, launched in February 2010, will provide that when its instruments come online later this year. SDO is able to map the sun's interior using a technique called helioseismology. SOHO can do the same thing, but not well enough to trace the Great Conveyor Belt all the way around. SDO's advanced sensors might reveal the complete circuit.

And then…? "It could be the missing piece we need to forecast the whole solar cycle," says Hathaway.

"It's a little like measuring the speed of a river on Earth by clocking the leaves and twigs floating downstream," Hathaway explains.

SOHO's dataset extends all the way back to 1996 and spans a complete solar cycle. Last year, Lisa Rightmire, a student of Hathaway from the University of Memphis, spent the entire summer measuring magnetic elements. When she plotted their speeds vs. time, she noticed how fast the conveyor belt has been going.

A note about "fast": The Great Conveyor Belt is one of the biggest things in the whole solar system and by human standards it moves with massive slowness. "Fast" in this context means 10 to 15 meters per second (20 to 30 miles per hour). A good bicyclist could easily keep up.

Below: The velocity of the Great Conveyor Belt (a.k.a. "meridianal flow") since 1996. Note the higher speeds after ~2004. credit: Hathaway and Rightmire, 2010. [larger image]

The speed-up was surprising on two levels.

First, it coincided with the deepest solar minimum in nearly 100 years, contradicting models that say a fast-moving belt should boost sunspot production. The basic idea is that the belt sweeps up magnetic fields from the sun's surface and drags them down to the sun's inner dynamo. There the fields are amplified to form the underpinnings of new sunspots. A fast-moving belt should accelerate this process.

So where have all the sunspots been? The solar minimum of 2008-2009 was unusually deep and now the sun appears to be on the verge of a weak solar cycle.

Instead of boosting sunspots, Hathaway believes that a fast-moving Conveyor Belt can instead suppress them "by counteracting magnetic diffusion at the sun's equator." He describes the process in detail in Science ("Variations in the Sun's Meridional Flow over a Solar Cycle," 12 March 2010, v327, 1350-1352).

The second surprise has to do with the bottom of the Conveyor Belt.

SOHO can only clock the motions of the visible top layer. The bottom is hidden by ~200,000 kilometers of overlying plasma. Nevertheless, an estimate of its speed can be made by tracking sunspots.

"Sunspots are supposedly rooted to the bottom of the belt," says Hathaway. "So the motion of sunspots tells us how fast the belt is moving down there."

He's done that—plotted sunspot speeds vs. time since 1996—and the results don't make sense. "While the top of the conveyor belt has been moving at record-high speed, the bottom seems to be moving at record-low speed. Another contradiction."

Right: An artist's concept of the Solar Dynamics Observatory (SDO). Launched in Feb. 2010, SDO will be able to look inside the sun to study the conveyor belt in greater detail, perhaps solving the mysteries Hathaway and Rightmire have uncovered. [larger image]

Could it be that sunspots are not rooted to the bottom of the Conveyor Belt, after all? "That's one possibility" he notes. "Sunspots could be moving because of dynamo waves or some other phenomenon not directly linked to the belt."

What researchers really need is a good look deep inside the sun. NASA's Solar Dynamics Observatory, launched in February 2010, will provide that when its instruments come online later this year. SDO is able to map the sun's interior using a technique called helioseismology. SOHO can do the same thing, but not well enough to trace the Great Conveyor Belt all the way around. SDO's advanced sensors might reveal the complete circuit.

And then…? "It could be the missing piece we need to forecast the whole solar cycle," says Hathaway. "It's a little like measuring the speed of a river on Earth by clocking the leaves and twigs floating downstream," Hathaway explains.

SOHO's dataset extends all the way back to 1996 and spans a complete solar cycle. Last year, Lisa Rightmire, a student of Hathaway from the University of Memphis, spent the entire summer measuring magnetic elements. When she plotted their speeds vs. time, she noticed how fast the conveyor belt has been going.

A note about "fast": The Great Conveyor Belt is one of the biggest things in the whole solar system and by human standards it moves with massive slowness. "Fast" in this context means 10 to 15 meters per second (20 to 30 miles per hour). A good bicyclist could easily keep up.

Below: The velocity of the Great Conveyor Belt (a.k.a. "meridianal flow") since 1996. Note the higher speeds after ~2004. credit: Hathaway and Rightmire, 2010. [larger image]

The speed-up was surprising on two levels.

First, it coincided with the deepest solar minimum in nearly 100 years, contradicting models that say a fast-moving belt should boost sunspot production. The basic idea is that the belt sweeps up magnetic fields from the sun's surface and drags them down to the sun's inner dynamo. There the fields are amplified to form the underpinnings of new sunspots. A fast-moving belt should accelerate this process.

So where have all the sunspots been? The solar minimum of 2008-2009 was unusually deep and now the sun appears to be on the verge of a weak solar cycle.

Instead of boosting sunspots, Hathaway believes that a fast-moving Conveyor Belt can instead suppress them "by counteracting magnetic diffusion at the sun's equator." He describes the process in detail in Science ("Variations in the Sun's Meridional Flow over a Solar Cycle," 12 March 2010, v327, 1350-1352).

The second surprise has to do with the bottom of the Conveyor Belt.

SOHO can only clock the motions of the visible top layer. The bottom is hidden by ~200,000 kilometers of overlying plasma. Nevertheless, an estimate of its speed can be made by tracking sunspots.

"Sunspots are supposedly rooted to the bottom of the belt," says Hathaway. "So the motion of sunspots tells us how fast the belt is moving down there."

He's done that—plotted sunspot speeds vs. time since 1996—and the results don't make sense. "While the top of the conveyor belt has been moving at record-high speed, the bottom seems to be moving at record-low speed. Another contradiction."

Right: An artist's concept of the Solar Dynamics Observatory (SDO). Launched in Feb. 2010, SDO will be able to look inside the sun to study the conveyor belt in greater detail, perhaps solving the mysteries Hathaway and Rightmire have uncovered. [larger image]

Could it be that sunspots are not rooted to the bottom of the Conveyor Belt, after all? "That's one possibility" he notes. "Sunspots could be moving because of dynamo waves or some other phenomenon not directly linked to the belt."

What researchers really need is a good look deep inside the sun. NASA's Solar Dynamics Observatory, launched in February 2010, will provide that when its instruments come online later this year. SDO is able to map the sun's interior using a technique called helioseismology. SOHO can do the same thing, but not well enough to trace the Great Conveyor Belt all the way around. SDO's advanced sensors might reveal the complete circuit.

And then…? "It could be the missing piece we need to forecast the whole solar cycle," says Hathaway.


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Global Map of Mercury

In December 2009, the first high-resolution global map of Mercury was made publicly available. These images are from MESSENGER, a NASA Discovery mission to conduct the first orbital study of the innermost planet, Mercury. Members of the MESSENGER team and experts from the U. S. Geological Survey (USGS) used images from MESSENGER's three Mercury flybys and from the Mariner 10 mission in 1974-75 to create a global mosaic that covers 97.7% of Mercury's surface at a resolution of 500 meters/pixel (0.31 miles/pixel).

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Version 1.2 of the NASA App is Now Available!

The first official NASA App invites you to discover a wealth of NASA information right on your iPhone or iPod Touch. The NASA App collects, customizes and delivers an extensive selection of dynamically updated information, images and videos from various online NASA sources in a convenient mobile package. It is available free of charge on the App Store from Apple directly on iPhone and/or iPod Touch or within iTunes.

What's new in version 1.2:

  • Facebook® Connect for easy sharing of images, videos, tweets and mission information
  • Integrated Twitter™ client for posting, retweeting, replying to, and direct messaging
  • NASAImages.org collection - With over 125,000 new images to browse and search
  • "Center" button for the orbital tracking feature
  • Advanced search option
  • Offline caching system
Version 1.1 changes:
  • Visible sighting opportunities listed for the International Space Station (ISS) and Space Shuttle, by home location and through search for location
  • Richer Mission details and more content
  • Enhancements to Videos and Updates panels
  • High-resolution image option (configured in device settings)
  • Status updates on upcoming launches
  • Prevent sleep mode setting for tracking launches (configured in device settings)

The Application Features These Screens:


For more information about the NASA's App for iPhone or iPod touch, visit:

http://www.nasa.gov/nasaapp

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NASA Announces Systems Engineering Student Competition

NASA's Exploration Systems Mission Directorate is inviting teams of undergraduate and graduate students throughout the country to participate in the fourth annual Systems Engineering Paper Competition. Participants in the competition will submit a paper on an Exploration Systems mission topic.

The deadline to register for the competition is April 16. Papers are due April 23. The winning teams will be announced in May. Awards include up to $3,500 in cash scholarships and VIP invitations to attend a future space shuttle or rocket launch at NASA's Kennedy Space Center in Florida.

The competition is designed to engage students in the science, technology, engineering and math, or STEM, disciplines critical to NASA's missions.

For information about the competition and how to apply, visit:

http://education.ksc.nasa.gov/esmdspacegrant/SystemsEngineering.htm

For information about NASA's education programs, visit:

http://www.nasa.gov/education

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NASA Awards Civil Design, Engineering and Services Contract

NASA has selected Jones Edmunds & Associates, Inc. of Gainesville, Fla., to provide civil and environmental design, engineering and other professional services. Services will be provided at NASA's Kennedy Space Center and Cape Canaveral Air Force Station in Florida, Vandenberg Air Force Base in California, and overseas emergency space shuttle landing sites. The work will rehabilitate, modernize or provide new facilities and systems at these locations.

This new indefinite-delivery, indefinite-quantity contract begins in March 2010 with a five year ordering period. The maximum potential value of this contract is approximately $25 million.

Jones Edmunds & Associates will provide services for the design of sewage treatment facilities, road repair and development, and parking facilities. the company also will be responsible for the design of new and reconfigured structures and facilities, building envelope, interior finishes, and site development. The work includes storm water management and utilities as well as facility equipment designed to process and condition hazardous and industrial waste products. Additional work involved includes HVAC and plumbing, industrial and institutional electrical systems, grounding, lighting, lightning protection, fire alarm and detection systems, and construction management.

For information about NASA and agency programs, visit:

http://www.nasa.gov

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Cassini Data Show Ice and Rock Mixture Inside Titan

This artist's illustration shows the likely interior structure of Saturn's moon Titan deduced from gravity field data collected by NASA's Cassini spacecraft.
This artist's illustration shows the likely interior structure of Saturn's moon Titan deduced from gravity field data collected by NASA's Cassini spacecraft.
› Full image and caption

By precisely tracking NASA's Cassini spacecraft on its low swoops over Saturn's moon Titan, scientists have determined the distribution of materials in the moon's interior. The subtle gravitational tugs they measured suggest the interior has been too cold and sluggish to split completely into separate layers of ice and rock.

The finding, to be published in the March 12 issue of the journal Science, shows how Titan evolved in a different fashion from inner planets such as Earth, or icy moons such as Jupiter's Ganymede, whose interiors have split into distinctive layers.

"These results are fundamental to understanding the history of moons of the outer solar system," said Cassini Project Scientist Bob Pappalardo, commenting on his colleagues' research. Pappalardo is with NASA's Jet Propulsion Laboratory in Pasadena, Calif. "We can now better understand Titan's place among the range of icy satellites in our solar system."

Scientists have known that Titan, Saturn's largest moon, is about half ice and half rock, but they needed the gravity data to figure out how the materials were distributed. It turns out Titan's interior is a sorbet of ice studded with rocks that probably never heated up beyond a relatively lukewarm temperature. Only in the outermost 500 kilometers (300 miles) is Titan's ice devoid of any rock, while ice and rock are mixed to various extents at greater depth.

"To avoid separating the ice and the rock, you must avoid heating the ice too much," said David J. Stevenson, one of the paper's co-authors and a professor of planetary science at the California Institute of Technology in Pasadena. "This means that Titan was built rather slowly for a moon, in perhaps around a million years or so, back soon after the formation of the solar system."

This incomplete separation of ice and rock makes Titan less like Jupiter's moon Ganymede, where ice and rock have fully separated, and perhaps more like another Jovian moon, Callisto, which is believed to have a mixed ice and rock interior. Though the moons are all about the same size, they clearly have diverse histories.

The Cassini measurements help construct a gravity map, which may help explain why Titan has a stunted topography, since interior ice must be warm enough to flow slowly in response to the weight of heavy geologic structures, such as mountains.

Creating the gravity map required tracking minute changes in Cassini's speed along a line of sight from Earth to the spacecraft as it flew four close flybys of Titan between February 2006 and July 2008. The spacecraft took paths between about 1,300 to 1,900 kilometers (800 to 1,200 miles) above Titan.

"The ripples of Titan's gravity gently push and pull Cassini along its orbit as it passes by the moon and all these changes were accurately recorded by the ground antennas of the Deep Space Network within 5 thousandths of a millimeter per second [0.2 thousandths of an inch per second] even as the spacecraft was over a billion kilometers [more than 600 million miles] away," said Luciano Iess, a Cassini radio science team member at Sapienza University of Rome in Italy, and the paper's lead author. "It was a tricky experiment."

The results don't speak to whether Titan has an ocean beneath the surface, but scientists say this hypothesis is very plausible and they intend to keep investigating. Detecting tides induced by Saturn, a goal of the radio science team, would provide the clearest evidence for such a hidden water layer.

A Cassini interdisciplinary investigator, Jonathan Lunine, said of his colleagues' findings, "Additional flybys may tell us whether the crust is thick or thin today." Lunine is with the University of Rome, Tor Vergata, Italy, and the University of Arizona, Tucson. "With that information we may have a better understanding of how methane, the ephemeral working fluid of Titan's rivers, lakes and clouds, has been resupplied over geologic time. Like the history of water on Earth, this is fundamental to a deep picture of the nature of Titan through time."

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. JPL, a division of Caltech, manages the project for NASA's Science Mission Directorate in Washington. The Cassini orbiter was designed, developed and assembled at JPL. Cassini's radio science subsystem has been jointly developed by NASA and the Italian Space Agency (ASI).

More Cassini information is available, at http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov

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Bursting at the Seams

Dramatic plumes, both large and small, spray water ice out from many locations along the famed 'tiger stripes' near the south pole of Saturn's moon Enceladus. The tiger stripes are fissures that spray icy particles, water vapor and organic compounds.

This mosaic was created from two high-resolution images that were captured by the narrow-angle camera when NASA's Cassini spacecraft flew past Enceladus and through the jets on Nov. 21, 2009. Imaging the jets over time will allow Cassini scientists to study the consistency of their activity.

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Three FASTSAT Instruments Pass Tests

The MINI-ME instrumentThe outer layers of Earth's atmosphere hold many secrets yet to be uncovered and three scientific instruments will fly soon on the FASTSAT-HSV01 satellite and seek to uncover them to benefit us here on Earth. Known as MINI-ME, PISA and TTI, these instruments recently passed a series of important final tests to prove their readiness for spaceflight.

These instruments were conceived and built at NASA's Goddard Space Flight Center in Greenbelt, Md., and were integrated to the satellite and tested at NASA's Marshall Spaceflight Center, Huntsville, Ala.

MINI-ME, acronym for Miniature Imager for Neutral Ionospheric atoms and Magnetospheric Electrons, is a low energy neutral atom imager which will detect neutral atoms formed in the plasma population of the Earth's outer atmosphere to improve global space weather prediction. Low energy neutral atom imaging is a technique first pioneered at Goddard which allows scientists to observe remotely various trapped charged particle populations around Earth that we would normally only be able to observe in-situ through direct instrument contact with the particles.

Michael Collier, Principal Investigator for the MINI-ME instrument at NASA Goddard said, "The satellite has gone through vibration, thermal, and Electromagnetic Interference (EMI) tests and everything looks great. The MINI-ME instrument is performing as expected."

The PISA instrumentPISA is an acronym for the Plasma Impedance Spectrum Analyzer, which will test a new measurement technique for the thermal electron populations in the ionosphere, and their density structuring, which can interfere with or scatter radio signals used for communication and navigation. PISA will tell scientists on Earth when and where the ionosphere becomes structured or turbulent. That will give us better predictions of how space weather will affect GPS signals.

Doug Rowland, PISA's Principal Investigator at NASA Goddard said, "PISA has completed the same tests that the Mini-ME endured and has just passed powered Electromagnetic Interference Test. PISA is on track for spacecraft to be packed up and delivered to the launch site." The EMI, vibration and thermal testing are critical tests for all instruments and satellites before they're loaded aboard a rocket and put into orbit.

The Thermospheric Temperature Imager, or TTI, will provide the first global-scale measurements of thermospheric temperature profiles in the 56-168 mile (90-270 km) region of the Earth's atmosphere. The temperature profile sets the scale height of the thermosphere which determines the density at orbital altitudes and therefore the aerodynamic drag experienced by military spacecraft.

John Sigwarth, TTI's Principal Investigator at NASA Goddard, said "The TTI survived the satellite launch vibration levels, being blasted with radio waves, and the TTI had a great thermal vacuum test. We were able to characterize the operation of the instrument in space-like environments and the TTI is ready for launch. We are eagerly anticipating obtaining great data from orbit."

Electromagnetic Interference or EMI testing is done to ensure that powerful ground-based communications and radar systems do not cause interference on the satellite or instrument systems.

Vibration testing is an important part of the testing process, because when the rocket carrying the satellite lifts off and travels through Earth's atmosphere it experiences intense vibrations. Successful vibration testing assures scientists and engineers that their instrument will remain intact and fully functional after launch.

Thermal testing is also critical, because of the extreme temperatures in space. Scientists need to be sure that the instruments will maintain function at extreme temperatures, from the extreme heat the rocket carrying the satellite will experience during launch and when it travels through Earth's atmosphere into the cold void of space.

"With the completion of the last phase of environmental testing of the integrated FASTSAT-HSV01 spacecraft, our team is focused on readying the satellite and its six science and technology instruments, for its near term shipment to Kodiak, Alaska, and for an on time launch no earlier than May 28, 2010," said FASTSAT Project Manager Mark Boudreaux at NASA Marshall.

"FASTSAT-HSV" means "Fast, Affordable, Science and Technology Satellite, Huntsville" The development, integration, test and operations of the three instruments is a collaborative effort between NASA Goddard, NASA Marshall, and the U.S. Naval Academy, Annapolis, Md.

FASTSAT-HSV01 will be flying a total of six instruments approved by the U.S. Department of Defense (DoD) Space Experiments Review Board multi-spacecraft/payload mission named STP-S26, which is executed by the DoD Space Test Program (STP) at the Space Development and Test Wing (SDTW), Kirtland Air Force Base, N.M. which is a unit of the Air Force Space and Missile Systems Center. The mission was designated S26 to correspond to the 26th small launch vehicle mission in STP's more than 40 year history of flying DoD space experiments. The mission will launch four satellites and three cubesats into low earth orbit.

The satellite was created at NASA Marshall with the Von Braun Center for Science and Innovation, in partnership with Dynetics, a corporate partner.

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Go into a NASA Clean Room Daily with the Webb Telescope via NASA’s ‘Webb-cam’

Screen capture from the clean room Webb-camHow often can you say that you've seen the components of a space telescope being worked on at NASA? The answer is probably "rarely, if ever." However, thanks to NASA's Goddard Space Flight Center in Greenbelt, Md., that has now changed.

Web cameras in Goddard's largest clean room are now providing daily, live coverage of work being done on components of the upcoming James Webb Space Telescope. You could say they're "Webb-cams" and they provide one image per minute so people can see what happens behind the scenes. Of course, the work happens during regular working hours, so there may not be action on screen all the time.

John Decker, Webb telescope Deputy Project Manager at NASA Goddard was the motivator in getting the "Webb-cam" up and running. "I thought it would be a great way for everyone to see what happens behind the scenes as components of this exciting new space telescope are being tested and coming together here at NASA Goddard," Decker said.

The Webb telescope project is managed at Goddard, and several components of this next generation space telescope are already in a clean room here.

view of Goddard's High Bay Clean Room
This panorama shows the inside of Goddard's High Bay Clean Room, as seen from the observation deck.

› Larger image
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 telescope is a joint project of NASA, the European Space Agency, and the Canadian Space Agency and is expected to launch in 2014.

Clean rooms are like operating rooms in hospitals. They are pristine areas kept as free as possible of contaminants that could interfere with delicate technology. There are several clean rooms at NASA Goddard.

Anyone that works in a clean room, such as engineers and scientists, have to wear sterile bodysuits, head covers, gloves, boots, and face masks. It takes about 10 to 15 minutes to get dressed before entering, and it's important because even one speck of dust or a fingerprint could severely damage the sensitive telescope components and instruments. Clean rooms act to filter out these harmful contaminants through a unique ventilation system and an entire wall of air filters.

The clean room ventilation system circulates almost one million cubic feet of air every minute through 9,000 square feet of HEPA filters located along one wall. The HEPA filters are specially designed to last several decades. All of these features provide the largest Goddard clean room with a Class-10,000 rating. That means any cubic foot of air in the clean room has no more than 10,000 particles floating around in it larger than 0.5 microns. A micron is one-millionth of a meter, and typical “outside” air has millions of such particles. A human hair is between 20 and 200 microns wide.

The advantage to the Webb-cam is that the average person doesn't need to do a micron-type clean up and spend time donning protective gear. Anyone can sit at their computer and see what's going on, no matter what they're wearing.

Related Links

› Watch the Goddard clean room Web cam
› More James Webb Space Telescope images at Goddard's Flickr page
› More about NASA's James Webb Space Telescope
› More about Goddard's clean room
› Other Goddard testing chambers

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Snapshot of the International Space Station

 Snapshot of the International Space Station
On March 13, 2008, the International Space Station passed across the field-of-view of Germany's remote sensing satellite, TerraSAR-X, at a distance of 195 kilometers, or 122 miles, and at a relative speed of 34,540 kilometers per hour, or more than 22,000 mph.

In contrast to optical cameras, radar does not 'see' surfaces. Instead, it is much more aware of the edges and corners which bounce back the microwave signal it transmits. Smooth surfaces such as those on the station's solar generators or the radiator panels used to dissipate excess heat, unless directly facing the radar antenna, tend to deflect rather than reflect the radar beam, causing these features to appear on the radar image as dark areas. The radar image of the station therefore looks like a dense collection of bright spots from which the outlines of the space station can be clearly identified. The central element on the station, to which all the modules are docked, has a grid structure that presents a multiplicity of reflecting surfaces to the radar beam, making it readily identifiable. This image has a resolution of about one meter (about 39 inches). In other words, objects can be depicted as discrete units--that is, shown separately--provided that they are at least one meter apart. If they are closer together than that, they tend to merge into a single block on a radar image.

Since this image was taken, the station has expanded and is more than 90 percent complete, including a full complement of solar arrays.


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