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Thursday, June 29, 2017

The Sun, a Primer

The Sun is a huge, glowing ball at the center of our solar system. The sun provides light, heat, and other energy to Earth. The sun is made up entirely of gas. Most of it is a type of gas that is sensitive to magnetism. This sensitivity makes this type of gas so special that scientists sometimes give it a special name: plasma. The planets and their moons, dwarf planets, tens of thousands of asteroids, and trillions of comets revolve around the sun. The sun and all these objects are in the solar system. Earth travels around the sun at an average distance of about 92,960,000 miles (149,600,000 kilometers) from it.

An Extreme Ultraviolet Imaging Telescope (EIT) image of the Sun and a huge, handle-shaped prominence, taken on September 14,1999, in the 304 angstrom wavelength. Prominences are huge clouds of relatively cool dense plasma suspended in the Sun's hot, thin corona. At times, they can erupt, escaping the Sun's atmosphere. Image credit: NASA/European Space Agency

The sun's radius (distance from its center to its surface) is about 432,000 miles (695,500 kilometers), approximately 109 times Earth's radius. The following example may help you picture the relative sizes of the sun and Earth and the distance between them: Suppose the radius of Earth were the width of an ordinary paper clip. The radius of the sun would be roughly the height of a desk, and the sun would be about 100 paces from Earth.

The part of the sun that we see has a temperature of about 5500 degrees C (10,000 degrees F). Astronomers measure star temperatures in a metric unit called the Kelvin (abbreviated K). One Kelvin equals exactly 1 Celsius degree (1.8 Fahrenheit degree), but the Kelvin and Celsius scales begin at different points. The Kelvin scale stars at absolute zero, which is -273.15 degrees C (-459.67 degrees F). Thus, the temperature of the solar surface is about 5800 K. Temperatures in the Sun's core reach over 15,000,000 K (27,000,000 degrees F).

The energy of the sun comes from nuclear fusion reactions that occur deep inside the sun's core. In a fusion reaction, two atomic nuclei join together, creating a new nucleus. Fusion produces energy by converting nuclear matter into energy.

The sun, like Earth, is magnetic. Scientists describe the magnetism of an object in terms of a magnetic field. This is a region that includes all the space occupied by the object and much of the surrounding space. Physicists define a magnetic field as the region in which a magnetic force could be detected—as with a compass. Physicists describe how magnetic an object is in terms of field strength. This is a measure of the force that the field would exert on a magnetic object, such as a compass needle. The typical strength of the sun's field is only about twice that of Earth's field.

But the sun's magnetic field becomes highly concentrated in small regions, with strengths up to 3,000 times as great as the typical strength. These regions shape solar matter to create a variety of features on the sun's surface and in its atmosphere, the part that we can see. These features range from relatively cool, dark structures known as sunspots to spectacular eruptions called flares and coronal mass ejections.

Flares are the most violent eruptions in the solar system. Coronal mass ejections, though less violent than flares, involve a tremendous mass (amount of matter). A single ejection can spew approximately 20 billion tons (18 billion metric tons) of matter into space. A cube of lead 3/4 mile (1.2 kilometers) on a side would have about the same mass.

The sun was born about 4.6 billion years ago. It has enough nuclear fuel to remain much as it is for another 5 billion years. Then it will grow to become a type of star called a red giant. Later in the sun's life, it will cast off its outer layers. The remaining core will collapse to become an object called a white dwarf, and will slowly fade. The sun will enter its final phase as a faint, cool object sometimes called a black dwarf.

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Wednesday, June 28, 2017

Are You an Umbraphile? You May Be After August 21!

um-bra-phile (ˈəm-brə-ˌfī(-ə)l) noun. 1. an avid observer of, or a person with a great interest in, eclipses. [from Latin umbra ‘shade’ and Greek philos ‘loving’]

An umbraphile is, literally, a "shadow lover." He or she is addicted to total solar eclipses. Those who have not stood in the moon’s shadow may not understand. But those who have, do. For many umbraphiles, it is way of life. These are the “solar eclipse chasers.” Once every 16 months, on average, umbraphiles drop what they are doing and travel, by whatever means necessary, to gather along a narrow strip in some remote corner of the globe defined by the laws of celestial mechanics.

The next total solar eclipse will occur August 21, crossing the continental United States from coast to coast. Are you an umbraphile? If you aren't, you may be very soon!

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Tuesday, June 27, 2017

Have You Made Your Reservations for the August 21 Total Solar Eclipse?

There are less than two months until the August 21 total solar eclipse. The path of totality will pass from coast to coast across the entire continental United States. The path of totality is about 70 miles wide. So, there are lots of great places in the U.S. you can see the event.

The Path of Totality for the August 21, 2017 Total Solar Eclipse. Image Credit: NASA

If you are coming from outside the path of totality and hope to stay overnight within the path August 20, before the August 21 event, you should make your plans now if you have not done so already. Hotels are filing up fast, and are already filled up in some locations.

Please do not wing this! The Department of Transportation is asking that people DO NOT pull off to the side of the interstate. Visit the DoT website where you can see how traffic may be affected by the eclipse. Visit the Fact Sheet link below.

2017 Solar Eclipse Transportation Fact Sheet for State and Local Departments of Transportation

Here are the states through which the center line of the path of totality will pass.

  • Oregon
  • Idaho
  • Wyoming
  • Nebraska
  • Kansas
  • Missouri
  • Kentucky
  • Tennessee
  • Georgia
  • South Carolina


To get more of an idea of the location of the path of totality, check out this list of major cities that will be in the path.

  • Corvallis, Albany and Lebanon, Oregon
  • Idaho Falls, Idaho
  • Casper, Wyoming
  • Grand Island, Lincoln Nebraska
  • St Joseph, Missouri
  • Kansas City, Kansas
  • St Louis, Missouri
  • Bowling Green, Kentucky
  • Nashville, Tennessee
  • Greenville, South Carolina
  • Columbia, South Carolina


The website Eclipse2017.org has a great page to see what cities will be in the path and how long totality will last at those locations. Follow the link below.

Cities that lie in the Path of Totality

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Sunday, June 25, 2017

Make a Pinhole Camera to View the Solar Eclipse

Pinhole Camera

You don't need a lot of money to observe a solar eclipse in complete safety. With just a few simple supplies, you can make a pinhole camera that lets you watch a solar eclipse safely and easily from anywhere. 

A pinhole camera is a simple camera without a lens. Instead of a lens, it has a tiny aperture, a pinhole. Light from a scene passes through the aperture and projects an inverted image, which is known as the camera obscura effect.

Remember: You should never look at the sun directly without equipment that's specifically designed for looking at the sun. Even using binoculars or a telescope, you could severely damage your eyes or even go blind! The totality portion of a solar eclipse is safe. But looking at anything as bright as the sun is NOT safe without proper protection. And no, sunglasses do NOT count. 

Now, let's make a pinhole camera! You will need the following materials.
  • 2 pieces of white card stock
  • 1 piece of unused, smooth, aluminum foil
  • 1 pair of scissors
  • 1 roll of tape
  • 1 pin or paper clip

Image Credit: NASA/JPL-Caltech


1. Cut a square hole into the middle of one of your pieces of card stock.
Image Credit: NASA/JPL-Caltech


2. Tape a piece of aluminum foil over the hole.
Image Credit: NASA/JPL-Caltech


3. Use your pin or paper clip to poke a small hole in the aluminum foil.
Image Credit: NASA/JPL-Caltech


4. Place your second piece of card stock on the ground and hold the piece with aluminum foil above it (foil facing up). Stand with the sun behind you and view the projected image on the card stock below! The farther away you hold your camera, the bigger your projected image will be.

To make your projection a bit more defined, try putting the bottom piece of card stock in a shadowed area while you hold the other piece in the sunlight.
Image Credit: NASA/JPL-Caltech


5. For extra fun, try poking multiple holes in your foil, making shapes, patterns and other designs. Each hole you create will turn into its own projection of the eclipse, making for some neat effects. Grab a helper to take photos of your designs for a stellar art project you can enjoy even after the eclipse has ended. 
Image Credit: NASA/JPL-Caltech

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Saturday, June 24, 2017

Ugarit Total Solar Eclipse

Trivia: The Ugarit Total Solar Eclipse

In 1948, a clay tablet was discovered in the port city of Ugarit in Northern Syria. In the text of the tablet, a Mesopotamian historian noted, "On the day of the new moon, in the month of Hiyar, the sun was put to shame, and went down in the daytime, with Mars in attendance." Scientists realized the text described a total solar eclipse in which the planet Mars was visible during totality.

Researchers originally dated the eclipse event as May 3, 1375 B.C. But further study suggested a different eclipse. Researchers considered the dating of the tablet, combined with the text's statement of the month in which the eclipse occurred and the fact that Mars was seen during totality. This evidence pointed to the total eclipse of March 5, 1223 B.C. The revised findings were first published in 1989 in the journal Nature.

The Ugarit eclipse is one of the earliest solar eclipses recorded. The path of totality began in the Atlantic Ocean, crossed north-western Afrca, Turkey, and central Asia.

The Accelerating Moon, the Decelerating Earth

The dating of ancient solar eclipses provides astronomers with reference points to determine long-term evolution of angular momentum in the Earth-Moon system--that is, it helps astronomers understand how the moon's orbit and Earth's rotation have changed over time. The revised date--March 5, 1223 B.C.--implies that the secular deceleration of Earth's rotation has changed very little during the past 3,000 years.

Secular What?

Ocean tides are caused by the gravitational pull of the moon (and, to a lesser extent, the Sun). The resulting tidal bulge in Earth's oceans is dragged ahead of the moon in its orbit due to the daily rotation of Earth. As a consequence, the ocean mass offset from the Earth-Moon line exerts a pull on the moon and accelerates it in its orbit. Conversely, the moon's gravitational tug on this mass exerts a torque that decelerates the rotation of Earth. The length of the day gradually increases as energy is transferred from Earth to the moon, causing the lunar orbit and period of revolution about Earth to increase.

You can learn more about secular acceleration from the following NASA article.

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Thursday, June 22, 2017

Total Solar Eclipse of January 1, 1889

Trivia: The Total Solar Eclipse of January 1, 1889, also known as the New Year’s Day Eclipse of 1889.

The path of totality began in the Bering Sea, crossed the North Pacific Ocean, passed through California to the north of San Francisco, through northern Nevada, Idaho, northwestern Wyoming, Montana, the northwestern part of North Dakota, and into central Canada, passing through southern Manitoba, and finishing on the western edge of Ontario.

The first photograph of a solar eclipse was taken during solar eclipse of July 28, 1851. But even with this technological advancement, most of the recorded observations of a total solar eclipse remained in the form of the written word and drawings. For the January 1, 1889 eclipse, a group of amateur and professional astronomers joined forces with a new photography society in San Francisco. They agreed to combine their resources to observe and record the eclipse. One example of the efforts was a photographic plate on which multiple exposures were made, showing many partial eclipse phases leading to totality.

On February 7, the group reunited in downtown San Francisco and presented their observations. The group enjoyed the experience so much that they agreed to form their own astronomical society, called the Astronomical Society of the Pacific (ASP). Originally a society of forty members, the ASP has grown to a national society dedicated to astronomy education and outreach. The ASP helps people of all ages learn astronomy and helps those people share their knowledge with others.

You can learn more about the ASP at the society’s official website:

www.astrosociety.org

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Wednesday, June 21, 2017

Two NASA Briefings on the Total Solar Eclipse of August 21, 2017

On June 21, representatives from NASA, other federal agencies, and science organizations, provided important viewing safety, travel and science information on the August 21, 2017 total solar eclipse. This eclipse will be the first in 99 years that will cross the entire continental United States.
Two briefings were held at the Newseum in Washington. The briefings aired live on NASA Television and streamed on the agency’s website.

Over the course of 100 minutes, 14 states across the United States will experience more than two minutes of darkness in the middle of the day. Additionally, a partial eclipse will be viewable across all of North America. The eclipse will provide a unique opportunity to study the sun, Earth, moon and their interaction because of the eclipse’s long path over land coast to coast. Scientists will be able to take ground-based and airborne observations over a period of an hour and a half to complement the wealth of data and images provided by space assets.

The June 21 briefings were:

Logistics Briefing
  • Thomas Zurbuchen, associate administrator of NASA’s Science Mission Directorate at the agency’s headquarters in Washington
  • Vanessa Griffin, director of the National Oceanic and Atmospheric Administration’s Office of Satellite and Product Operations in Suitland, Maryland
  • Brian Carlstrom, deputy associate director of Natural Resource Stewardship and Science at the National Park Service in Washington
  • Martin Knopp, associate administrator of the Office of Operations in the Federal Highway Administration at the U.S. Department of Transportation in Washington


Science Briefing
  • Thomas Zurbuchen
  • Angela Des Jardins, principal investigator of the Eclipse Ballooning Project at Montana State University, Bozeman
  • Angela Speck, professor of astrophysics and director of astronomy at the University of Missouri, Columbia
  • Dave Boboltz, program director of solar physics in the Division of Astronomical Sciences at the National Science Foundation in Arlington, Virginia
  • Linda Shore, executive director of the Astronomical Society of the Pacific in San Francisco
  • Matt Penn, astronomer at the National Solar Observatory in Tucson, Arizona


For more information on the eclipse, and how to safely view it, visit:



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Thursday, May 18, 2017

Saturn's Shortening Shadow

Saturn's shadow across the rings, as seen from the Cassini spacecraft. Image Credit: NASA/JPL-Caltech/Space Science Institute

The Cassini spacecraft continues sending back great images and data during the Grand Finale portion of its mission at Saturn. Here we see a sign of the changing seasons at Saturn, in that the planet’s shadow across the rings is shortening.

The above image was taken at a distance of about 760,000 miles (1.2 million kilometers) from Saturn. The image scale is 46 miles (73 kilometers) per pixel.

To learn more, read the full article here.

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Wednesday, April 26, 2017

Cassini's Big Finish Begins

Saturn eclipsing the sun, seen from behind by the Cassini orbiter. Earth can be seen as a small dot between the rings on the upper, left-hand side. Image Credit: NASA/JPL/Space Science Institute

(My apologies for the "big finish." But because the other phrase is so prevalent, I just had to find something to say other than "grand finale,” at least once.)

The NASA Cassini mission is winding down, quite literally. On April 26, the Cassini spacecraft became the first to dive between Saturn and its ring system. This begins the spacecraft’s “grand finale” in which it will make 22 amazing orbits and, on September 15, enter Saturn’s atmosphere and burn up. The spacecraft will be useful until the very last moment–it will be sending back data continuously, including measurements of the composition of Saturn’s atmosphere, rotation rate and interior structure.

Until that time, the instrument teams have several new observations to make. These include understanding a Saturn radiation belt, discovered inside the rings in 2004, and taking close-up pictures of the rings and other features.

Read the 2004 Article: New Radiation Belt

The spacecraft will also image Saturn’s cloud tops at close range, weigh its ring system (which will indicate just how old it is), sample the atmosphere of the planet and its rings, and measure Saturn’s internal structure.

Read the NASA PDF Resource on the Mission (published 1997)

Originally called Cassini-Huygens, the mission involves ESA, NASA and the Italian Space Agency. The idea of the mission began in 1982, when the European Science Foundation and the American National Academy of Sciences formed a working group to investigate future cooperative missions. Two European scientists suggested a paired Saturn Orbiter and Titan Probe as a possible joint mission. In 1983, NASA's Solar System Exploration Committee recommended the same Orbiter and Probe pair as a core NASA project. NASA and the European Space Agency (ESA) performed a joint study of the potential mission from 1984 to 1985. ESA continued with its own study in 1986, while American astronaut Sally Ride, in her 1987 report, also examined and approved of the Cassini mission.

In 1988, NASA Associate Administrator for Space Science and Applications Len Fisk wrote to his counterpart at ESA, Roger Bonnet, strongly suggesting that ESA choose the Cassini mission from the three candidates at hand and promising that NASA would commit to the mission when ESA did.

Read the Article: Launch of Cassini Spacecraft

On October 15, 1997, a Titan IVB/Centaur rocket launched from Cape Canaveral Air Force Station in Florida, sending the Cassini orbiter and its Huygens probe on a seven-year, 2.2-billion mile journey to the Saturn system.

Read About the Spacecraft

The mission arrived at Saturn on July 1, 2004. The mission was originally planned for four years. But Cassini-Huygens was so successful that the mission multiple times, eventually to 2017. It has flown past seven of the larger satellites, including giant Titan – which is larger than the planet Mercury. The orbiter passed Titan more than 70 times. Flying within 880 km of the moon, it studied Titan’s orange clouds and nitrogen-rich atmosphere. It also mapped its surface with an imaging radar.

On Christmas Day 2004, Huygens separated from Cassini. Three weeks later, it entered Titan’s thick atmosphere, becoming the first probe to land on the surface of a planetary satellite (other than Earth’s moon). Protected by a heat shield, the probe slowed from 18,000 to 1,400 km per hour in just three minutes. Soon after, a large parachute opened. At a height of about 160 km, the probe began to take pictures and study the atmosphere. For more than two hours, data from Huygens were received and stored on Cassini as it flew overhead.

Read More

To learn more about Cassini, Huygens, Saturn, Titan, the rest of the Saturn system, and the Grande Finale, check out these links.

Read About the Mission

See the Mission Timeline

Read the FAQ for Cassini – The Grand Finale

Read the 2017 Article: Bittersweet feeling as Cassini mission embarks on its ‘grand finale’ ahead of death plunge

Read the 2014 Article: Cassini 10 Years at Saturn Top 10 Discoveries

Read the 2017 April Article: Cassini Completes Final -- and Fateful -- Titan Flyby

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Tuesday, April 04, 2017

What is an Orbit?

or-bit (ˈȯr-bət) noun. 1. a. A path described by one body in its revolution about another (as by the earth about the sun or by an electron about an atomic nucleus); also, one complete revolution of a body describing such a path. b. A circular path. [Middle English, from Medieval Latin orbita, from Latin, rut, track, probably from orbis]

An orbit is a regular, repeating path that one heavenly body takes around another body. A body which orbits another body is a satellite of the other body. So, the moon is a satellite of Earth, while at the same time, Earth is a satellite of the sun, along with the other planets, comets, asteroids, and many other bodies in the solar system. And remember that the sun orbits the center of our Milky Way galaxy. So, the sun is a satellite of the Milky Way.

A satellite can be classified as natural or artificial. The moon, Earth and other heavenly bodies are natural satellites. All orbiting objects made by humans are artificial satellites. The first artificial satellite was Sputnik 1, launched in 1957. A more recent example is the International Space Station, which was launched in pieces and assembled in orbit.


Most orbiting bodies move along or close to an imaginary flat surface. This imaginary surface is called the ecliptic plane.


What Shape Is an Orbit?


Orbits come in different shapes. All orbits are elliptical, which means they are the shape of an ellipse, similar to an oval. For the planets, the orbits are almost circular. The orbits of comets have a different shape. They are highly eccentric or "squashed." They look more like thin ellipses than circles.


Satellites that orbit Earth, including the moon, do not always stay the same distance from Earth. Sometimes they are closer, and at other times they are farther away. The closest point a satellite comes to Earth is called its perigee. The farthest point is the apogee. For planets and other bodies that orbit the sun, the point in their orbit closest to the sun is perihelion. The farthest point is called aphelion. Earth reaches its aphelion during summer in the Northern Hemisphere. The time it takes a satellite to make one full orbit is called its period. For example, Earth has an orbital period of one year. The inclination of an orbit is the angle the orbital plane when compared with Earth's equator.


This diagram of an Earth orbit demonstrates an elliptical orbit and shows apogee, perigee, aphelion, and perihelon. Image Credit: NOAA

How Do Objects Stay in Orbit?

An object in motion will stay in motion unless something pushes or pulls on it. This statement is called Newton's first law of motion. Without gravity, an Earth-orbiting satellite would go off into space along a straight line. With gravity, it is pulled back toward Earth. A constant tug-of-war takes place between the satellite's tendency to move in a straight line, or momentum, and the tug of gravity pulling the satellite back.

An object's momentum and the force of gravity have to be balanced for an orbit to happen. If the forward momentum of one object is too great, it will speed past and not enter into orbit. If momentum is too small, the object will be pulled down and crash. When these forces are balanced, the object is always falling toward the planet, but because it's moving sideways fast enough, it never hits the planet. Orbital velocity is the speed needed to stay in orbit. At an altitude of 150 miles (242 kilometers) above Earth, orbital velocity is about 17,000 miles per hour. Satellites that have higher orbits have slower orbital velocities.

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Sunday, April 02, 2017

What is an Eclipse?

e-clipse (i-ˈklips) noun. 1. a. The total or partial obscuring of one celestial body by another. b. The passing into the shadow of a celestial body. Compare OCCULTATION, TRANSIT. [Middle English, from Anglo-French, from Latin eclipsis, from Greek ekleipsis, from ekleipein to omit, fail, suffer eclipse, from ex- + leipein to leave]

An eclipse happens when one heavenly body, such as a moon or planet, moves into the shadow of another heavenly body. There are two types of eclipses as seen from Earth: an eclipse of the moon and an eclipse of the sun.

An eclipse of the moon...

The moon moves in an orbit around Earth, and at the same time, Earth orbits the sun. Sometimes Earth moves between the sun and the moon. When this happens, Earth blocks the sunlight that normally is reflected by the moon. Instead of light hitting the moon’s surface, Earth's shadow falls on it. This is an eclipse of the moon—a lunar eclipse. A lunar eclipse can happen only when the moon is full.

A lunar eclipse can be seen from Earth at night. There are two types of lunar eclipses: total lunar eclipses and partial lunar eclipses.

A total lunar eclipse happens when the moon and the sun are on exact opposite sides of Earth. Although the moon is in Earth's shadow, some sunlight reaches the moon. The sunlight passes through Earth's atmosphere, which causes Earth’s atmosphere to filter out most of the blue light. This makes the moon appear red to people watching from Earth.

A partial lunar eclipse happens when only a part of the moon enters Earth's shadow. In a partial eclipse, Earth's shadow appears very dark on the side of the moon facing Earth. What people see from Earth during a partial lunar eclipse depends on how the sun, Earth and moon are lined up.

A lunar eclipse usually lasts for a few hours. At least two partial lunar eclipses happen every year, but total lunar eclipses are rare. It is safe to look at a lunar eclipse.

A lunar eclipse. Image credit: NASA

An eclipse of the sun...

Sometimes when the moon orbits Earth, it moves between the sun and Earth. When this happens, the moon blocks the light of the sun from reaching Earth. This causes an eclipse of the sun, or solar eclipse. During a solar eclipse, the moon casts a shadow onto Earth.

There are three types of solar eclipses. The first is a total solar eclipse. A total solar eclipse is only visible from a small area on Earth. The people who see the total eclipse are in the center of the moon’s shadow when it hits Earth. The sky becomes very dark, as if it were night. For a total eclipse to take place, the sun, moon and Earth must be in a direct line.

The second type of solar eclipse is a partial solar eclipse. This happens when the sun, moon and Earth are not exactly lined up. The sun appears to have a dark shadow on only a small part of its surface.

The third type is an annular (pronounced “ANN-you-ler”) solar eclipse. An annular eclipse happens when the moon is farthest from Earth. Because the moon is farther away from Earth, it seems smaller. It does not block the entire view of the sun. The moon in front of the sun looks like a dark disk on top of a larger sun-colored disk. This creates what looks like a ring around the moon.

A solar eclipse. Image credit: NASA

During a solar eclipse, the moon casts two shadows on Earth. The first shadow is called the umbra (pronounced “UM-bruh”). This shadow gets smaller as it reaches Earth. It is the dark center of the moon’s shadow. The second shadow is called the penumbra (pronounced “pe-NUM-bruh”). The penumbra gets larger as it reaches Earth. People standing in the penumbra will see a partial eclipse. People standing in the umbra will see a total eclipse.

The umbra and penumbra. Image credit: NASA

Solar eclipses happen approximately once every 18 months. Unlike lunar eclipses, solar eclipses only last for a few minutes.

You should never look directly at the sun. It can permanently damage your eyes. You must use proper safety equipment to look at any type of solar eclipse. More on this later.

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Monday, March 27, 2017

Journey to the Shadow, No. 1

On August 21, millions of people will look skyward to witness a spectacle not seen in 38 years—a total eclipse over the continental United States. This time, the shadow will span the continental U.S. from coast to coast, the first to do so since 1918. Even those in the U.S. who will not be in the path of totality, will see a partial solar eclipse.

The August 21 eclipse might be the most viewed sky event in history. The Sun’s shadow will travel from Oregon to South Carolina. In addition, the shadow will pass over thousands of miles of the Pacific and Atlantic oceans. But the shadow will touch no other land.

This will be the first total solar eclipse to cross the continental United States in 38 years. One eclipse did pass over Hawaii in 1981. But the last for the continental U.S. was February 26, 1979. Sadly, few saw it because observers had to be in one of only five states in the northwest, and the wintry weather was bad along the path of totality.

Before the 1979 eclipse, there was the eclipse of March 7, 1970. That eclipse passed up the U.S. east coast. More people directly saw that eclipse than the 1979 eclipse, but because that was 47 years ago, few in the United States are still with us who saw the 1970 total eclipse with their own eyes.

For August 21 total eclipse, I plan to add my name to the list of those who have seen a total eclipse for themselves. I plan to stand in the path of totality and experience night in the daytime. Along the way, I will review the phenomenon which we call solar and lunar eclipses. I will recount the history, delve into the mythology, and try to separate the fact from fiction. This is just my first step. Join me on my journey to the shadow.

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Sunday, June 29, 2014

IRIS Solar Observatory Celebrates First Year

Friday marked the first year on orbit for NASA's newest solar observatory. On June 27, 2013, the Interface Region Imaging Spectrograph (IRIS) was launched into Earth orbit. IRIS, observes the low level of the sun's atmosphere -- a constantly moving area called the interface region -- in better detail than has ever been done before.

This combined image shows the March 29, 2014, X-class flare as seen through the eyes of different observatories. The Solar Dynamics Observatory (SDO) is on the bottom/left, which helps show the position of the flare on the sun. The darker orange square is IRIS data. The red rectangular inset is from Sacramento Peak. The violet spots show the flare's footpoints from RHESSI. Image Credit: NASA/IRIS/LMSAL/Duberstein

During its first year in space, IRIS provided detailed images of the interface region, finding even more turbulence and complexity than expected. The interface region lies at the core of many outstanding questions about the sun's atmosphere, such as how solar material in the corona reaches millions of degrees, several thousand times hotter than the surface of the sun itself, or how the sun creates giant explosions like solar flares and coronal mass ejections. The interface region is also where most of the ultraviolet emission is generated that impacts the near-Earth space environment and Earth’s climate.

In its first year, IRIS witnessed dozens of solar flares, including one X-class flare, and the foot points of a coronal mass ejection, or CME. IRIS must commit to pointing at certain sections of the sun at least a day in advance, so catching these eruptions in the act involves educated guesses and a little bit of luck.

The IRIS instrument captures two kinds of data on all its observations: IRIS collects both images of the sun and a kind of data called spectra. A spectrograph splits the light from a given point on the sun into its discrete wavelengths – a technique that ultimately allows scientists to measure temperature, velocity and density of the solar material behind the slit. When looking at the onset of a flare or at the foot points of a CME, therefore, scientists can parse out how the material moves, and shed light on what causes these eruptions.

The spectra are a crucial tool in the IRIS arsenal to understand the interface region. The solar material there is relatively dense and giant swaths of material roil up and down. Figuring out how the material moves and heats up provides information about how energy courses through the region, changing along the way between heat, movement and magnetic energy. One of the first science papers published with IRIS data used these spectra to provide unique, faster-than-ever characterization of how solar material in sunspots follows a repeated pattern of quick heating while accelerating upward, followed by an even faster rebound downward. This oscillation has been seen before, but never with the quick time cadence that is IRIS' hallmark.

Scientists are in the process of analyzing the data from IRIS's first year, and will have more results to share shortly. The prime mission lasts until summer 2015. Lockheed Martin’s Solar & Astrophysics Laboratory, Palo Alto, California, designed and manages the mission. The Harvard-Smithsonian Center for Astrophysics in Cambridge, Massachusetts, built the telescope. Montana State University in Bozeman, Montana. helped design the spectrograph. NASA's Ames Research Center in Moffett Field, California, provides mission operations and ground data systems. NASA's Goddard Space Flight Center in Greenbelt, Maryland, manages the Small Explorer Program for NASA's Science Mission Directorate in Washington, D.C. The Norwegian Space Centre provides regular downlinks of science data. Other contributors include the University of Oslo and Stanford University in Stanford, California.

To learn more about NASA's IRIS mission, visit: http://iris.gsfc.nasa.gov/
 

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LDSD Test #1 Initial Results Announced

NASA held a media teleconference this morning to discuss yesterday’s near-space test flight of the agency's Low-Density Supersonic Decelerator (LDSD), which took place off the coast of the U.S. Navy's Pacific Missile Range Facility in Kauai, Hawaii. The events of the test were recounted.

LDSD Test Vehicle #1, retrieved from the Pacific Ocean following its test on June 28 2014. The deflated, tan-colored SIAD can be seen extending beyond the frame of the test vehicle. Image Credit: NASA/JPL-Caltech

A high-altitude balloon launch occurred at 8:45 a.m. HST (11:45 a.m. PDT/2:45 p.m. EDT) from the Hawaiian island facility. At 11:05 a.m. HST (2:05 p.m. PDT/5:05 p.m. EDT), the LDSD test vehicle dropped away from the balloon as planned and began powered flight. The balloon and test vehicle were about 120,000 feet over the Pacific Ocean at the time of the drop. The vehicle splashed down in the ocean at approximately 11:35 a.m. HST (2:35 p.m. PDT/5:35 p.m. EDT), after the engineering test flight concluded. The test vehicle hardware, black box data recorder and parachute were all recovered later in the day.

"We are thrilled about yesterday's test," said Mark Adler, project manager for LDSD at NASA's Jet Propulsion Laboratory in Pasadena, California. "The test vehicle worked beautifully, and we met all of our flight objectives. We have recovered all the vehicle hardware and data recorders and will be able to apply all of the lessons learned from this information to our future flights."

This test was the first of three planned for the LDSD project, developed to evaluate new landing technologies for future Mars missions. While this initial test was designed to determine the flying ability of the vehicle, it also deployed two new landing technologies as a bonus. Those landing technologies will be officially tested in the next two flights, involving clones of the saucer-shaped vehicle.

"Because our vehicle flew so well, we had the chance to earn 'extra credit' points with the Supersonic Inflatable Aerodynamic Decelerator [SIAD]," said Ian Clark, principal investigator for LDSD at JPL. "All indications are that the SIAD deployed flawlessly, and because of that, we got the opportunity to test the second technology, the enormous supersonic parachute, which is almost a year ahead of schedule."

The Supersonic Inflatable Aerodynamic Decelerator (SIAD) is a large, doughnut-shaped first deceleration technology that deployed during the flight. The second is an enormous parachute (the Supersonic Disk Sail Parachute). Imagery downlinked in real-time from the test vehicle indicates that the parachute did not deploy as expected, and the team is still analyzing data on the parachute so that lessons learned can be applied for the next test flights, scheduled for early in 2015.

In order to get larger payloads to Mars, and to pave the way for future human explorers, cutting-edge technologies like LDSD are critical. Among other applications, this new space technology will enable delivery of the supplies and materials needed for long-duration missions to the Red Planet.

"This entire effort was just fantastic work by the whole team and is a proud moment for NASA's Space Technology Mission Directorate," said Dorothy Rasco, deputy associate administrator for the Space Technology Mission Directorate at NASA Headquarters in Washington. "This flight reminds us why NASA takes on hard technical problems, and why we test - to learn and build the tools we will need for the future of space exploration. Technology drives exploration, and yesterday's flight is a perfect example of the type of technologies we are developing to explore our solar system."

NASA's Space Technology Mission Directorate funds the LDSD mission, a cooperative effort led by NASA's Jet Propulsion Laboratory in Pasadena, California. NASA's Technology Demonstration Mission program manages LDSD at NASA's Marshall Space Flight Center in Huntsville, Alabama. NASA's Wallops Flight Facility in Wallops Island, Virginia, coordinated support with the Pacific Missile Range Facility and provided the balloon systems for the LDSD test.

For more information about the LDSD space technology demonstration mission, visit:
http://go.usa.gov/kzZQ

For more information about the Space Technology Mission Directorate, visit:
http://www.nasa.gov/spacetech

The follow-along page from the media teleconference can be found at: http://www.nasa.gov/jpl/ldsd/telecon2014/
 

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Saturday, June 28, 2014

LDSD Test #1 Complete. Results Pending.

NASA has reported that at approximately 5:05pm EDT today, the Low-Density Supersonic Decelerator (LDSD) test vehicle successfully dropped from its balloon. The initial indications are that its rockets fired as expected. A news teleconference is scheduled for tomorrow, June 29, at 7 a.m. HST (10 a.m. PDT, 1 p.m. EDT) to discuss the test flight.

The balloon launch occurred at 8:45 a.m. HST (11:45 a.m. PDT/2:45 p.m. EDT) from the US Navy's Pacific Missile Range Facility in Kauai, Hawaii. At 11:05 a.m. HST (2:05 p.m. PDT/5:05 p.m. EDT), the test vehicle dropped away from the balloon (as planned), and powered flight began. The balloon and test vehicle were about 120,000 feet over the Pacific Ocean at the time of the drop. The vehicle splashed down in the ocean at approximately 11:35 a.m. HST (2:35 p.m. PDT/5:35 p.m. EDT), after the engineering test flight concluded.

This test was the first of three planned for the LDSD project, developed to evaluate new landing technologies for future Mars missions. While this initial test was designed to determine the flying ability of the vehicle, it also deployed two new landing technologies as a bonus. Those landing technologies will be officially tested in the next two flights, involving clones of the saucer-shaped vehicle.

Initial indications are that the vehicle successfully flew its flight test profile as planned, and deployed the two landing technologies. The first is a doughnut-shaped tube called the Supersonic Inflatable Aerodynamic Decelerator (SIAD), with early indications that it deployed as expected. The second is an enormous parachute (the Supersonic Disk Sail Parachute). Imagery downlinked in real-time from the test vehicle indicates that the parachute did not deploy as expected.

In order to get larger payloads to Mars, and to pave the way for future human explorers, cutting-edge technologies like LDSD are critical. Among other applications, this new space technology will enable delivery of the supplies and materials needed for long-duration missions to the Red Planet.

The upper layers of Earth's stratosphere are the most similar environment available to match the properties of the thin atmosphere of Mars. The LDSD mission developed this test method to ensure the best prospects for effective testing of the new and improved technologies.

Media and the public may listen online at: http://www.nasa.gov/news/media/newsaudio

NASA's LDSD program is part of the agency's Space Technology Mission Directorate, which is innovating, developing, testing and flying hardware for use in NASA's future missions.


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Watch NASA's LDSD Test Live!

After a series of weather delays, NASA will attempt to launch the Low-Density Supersonic Decelerator (LDSD) into Earth's atmosphere today to test technology that could be used to land on Mars.

A balloon carrying the LDSD test vehicle is scheduled to lift off today from its pad at the U.S. Navy's Pacific Missile Range Facility in Kauai, Hawaii. The vehicle, which resembles a flying saucer, is designed to test landing technologies for future Mars missions.

Click here to watch live: http://www.ustream.tv/nasajpl2

This first of three LDSD flights will determine the flying qualities of the test vehicle. As a bonus, the flight plan also includes deployment of two new technologies -- an inflatable device and mammoth parachute. However, those landing technologies are not officially scheduled to be tested until next summer, in two additional LDSD flights.

The above chart gives an overview of the first planned test of the Low-Density Supersonic Decelerator (LDSD). Image Credit: NASA/JPL-Caltech

After liftoff, the balloon carrying the LDSD test vehicle will slowly float upward, taking several hours to reach an altitude of 120,000 feet (36,600 meters). At that point, the balloon will release the vehicle and its rocket will kick in, boosting the craft to an altitude of 180,000 feet (54,900 meters).

When the test vehicle reaches 180,000 feet and is traveling at about Mach 3.8, it will deploy the first of the new technologies, a doughnut-shaped tube called the Supersonic Inflatable Aerodynamic Decelerator (SIAD). The SIAD decelerates the test vehicle to approximately Mach 2.5. The test vehicle will then deploy a mammoth parachute (the Supersonic Disk Sail Parachute), which will carry it safely to a controlled water impact about 40 minutes after being dropped from the balloon.

The website will be updated as event milestones occur, at the top of the page. More information on LDSD is online at: http://go.usa.gov/kzZQ

NASA's LDSD program is part of the agency's Space Technology Mission Directorate, which is innovating, developing, testing and flying hardware for use in NASA's future missions.


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Cassini: Ten Years at Saturn and Counting

This coming Monday will mark a decade since a bus-sized robotic traveler from Earth first soared over the icy rings of Saturn and fired its engines to fall into orbit. On June 30, the Cassini mission will celebrate 10 years of exploring the planet, its rings and moons.

Image Credit: NASA/JPL-Caltech

The Cassini spacecraft, carrying the European Space Agency's Huygens probe, arrived in the Saturn system on June 30, 2004, for a four-year primary mission. Since 2008, NASA has granted the mission three extensions, allowing scientists an unprecedented opportunity to observe seasonal changes as the planet and its retinue completed one-third of their nearly 30-year-long trek around the sun.

"Having a healthy, long-lived spacecraft at Saturn has afforded us a precious opportunity," said Linda Spilker, Cassini project scientist at NASA's Jet Propulsion Laboratory in Pasadena, California. "By having a decade there with Cassini, we have been privileged to witness never-before-seen events that are changing our understanding of how planetary systems form and what conditions might lead to habitats for life."

After 10 years at Saturn, Cassini has beamed back to Earth hundreds of gigabytes of scientific data, enabling the publication of more than 3,000 scientific reports. Representing just a sampling, 10 of Cassini's top accomplishments and discoveries are:

  • The Huygens probe makes first landing on a moon in the outer solar system (Titan)
  • Discovery of active, icy plumes on the Saturnian moon Enceladus
  • Saturn's rings revealed as active and dynamic -- a laboratory for how planets form
  • Titan revealed as an Earth-like world with rain, rivers, lakes and seas
  • Studies of Saturn's great northern storm of 2010-2011
  • Studies reveal radio-wave patterns are not tied to Saturn's interior rotation, as previously thought
  • Vertical structures in the rings imaged for the first time
  • Study of prebiotic chemistry on Titan
  • Mystery of the dual, bright-dark surface of the moon Iapetus solved
  • First complete view of the north polar hexagon and discovery of giant hurricanes at both of Saturn's poles


"It's incredibly difficult to sum up 10 extraordinary years of discovery in a short list, but it's an interesting exercise to think about what the mission will be best remembered for many years in the future," Spilker said.
Further details about each of these discoveries are available at: http://saturn.jpl.nasa.gov/news/cassinifeatures/10thannivdiscoveries/

In celebration of the 10th anniversary, members of the Cassini team selected some of their favorite images for a gallery, describing in their own words what makes the images special to them. The gallery is available at: http://saturn.jpl.nasa.gov/news/cassinifeatures/10thannivimages/

While Cassini was originally approved for a four-year study of the Saturn system, the project's engineers and scientists had high hopes that the mission might carry on longer, and designed the system for endurance. The spacecraft has been remarkably trouble-free, and from an engineering standpoint, the main limiting factor for Cassini's lifetime now is how much propellant is left in its tanks. The mission owes a great deal of its longevity to skillful and efficient piloting by the mission's navigation and operations teams.

"Our team has done a fantastic job optimizing trajectories to save propellant, and we've learned to operate the spacecraft to get the most out of it that we possibly can," said Earl Maize, Cassini project manager at JPL. "We're proud to celebrate a decade of exploring Saturn, and we look forward to many discoveries still to come."

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. JPL, a division of the California Institute of Technology, Pasadena, manages the mission for NASA's Science Mission Directorate in Washington.

Get more information about Cassini at the following sites:

http://www.nasa.gov/cassini

http://saturn.jpl.nasa.gov



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Thursday, January 30, 2014

Plato May Be the Third Cosmic Vision

The concept known as Plato seems destined to be the next mission in ESA's Cosmic Vision program. Plato was chosen by an expert panel as the standout candidate in a competition run by the European Space Agency (ESA). The Paris-based organization's Science Policy Committee will now have the final say at its meeting in February. If given the go-ahead, Plato would probably not launch until 2024.

The name of the mission is an acronym that stands for PLAnetary Transits and Oscillations of stars. It is not really one telescope but rather a suite of 34 telescopes mounted on a single satellite. The intention is for Plato to sweep about half the sky, to investigate some of its brightest and nearest stars. It would monitor these stars for the tell-tale tiny dips in light that occur when planets move across their faces.

Critically, Plato would be tuned to seek out rocky worlds orbiting in the "habitable zone" - the region around a star where water can keep a liquid state. A fundamental part of its quest would be to perform an intricate study of the host stars themselves, using their pulsations to probe their structure and properties.

Such observations, termed asteroseismology, would provide key, complementary information for the proper characterization of the rocky worlds. Although other missions have pursued this kind of science before, Plato is described as a major leap forward in capability. The hope is that it could find really promising targets for follow-up by the big ground-based telescopes due to come online in the next decade. These facilities, which will have primary mirrors measuring tens of meters in diameter, should be able to examine the atmospheres of distant worlds for possible life signatures. The James Webb Space Telescope, the successor to Hubble, due for launch at the end of this decade, would likely still be working in 2024/2025 and could also pursue Plato's discoveries.

Plato has spent the past two years in an assessment process that has pitted it against four other concepts. These alternatives included another planet observatory (Echo), an asteroid mission (Marco Polo-R), an X-ray telescope (Loft), and a satellite that would perform a precise test of Einstein's equivalence principle (STE-Quest).

All were competing to be the third medium-class launch opportunity to be offered under ESA's so-called Cosmic Vision program, which defines the organization's space science priorities. "Medium class" means a cost to the agency of no more than about 600m euros (£490m; $820m), although following the practice of previous missions this does not include the budget for instruments. These are usually provided directly by ESA's national member agencies and mean the final price tag can approach one billion euros. All the competitors were invited to make a final presentation to representatives of the scientific community, industry, and national member agencies on January 21. This was followed by closed-session discussions by two working groups, which rated the quality of the missions. Their recommendations were then passed to ESA's top space science advisory committee (SSAC) to make an evaluation. It proposed that Plato be carried forward as the mission of choice, and this preference has now been sent on by ESA's executive to the SPC. The committee has the prerogative of "selection" at its February 19 gathering, and could still reject Plato - but this would be a major surprise.

The final green light is known as "adoption" in ESA-speak. This is unlikely to happen until 2015, after member states have made firm commitments on their participation and an industrial team to build the satellite has been identified. One big industrial contribution from the UK seems assured. This would be the camera detector at the base of the telescope suite. Supplied by e2v in Chelmsford, the array of more than 130 charge-coupled devices would be 0.9 square meters in area. This would make it the largest camera system ever flown in space, and twice the size of the array e2v produced for ESA's recently launched Gaia telescope.

The first two medium-class missions to be selected under ESA's Cosmic Vision program in 2011 were Solar Orbiter, a space telescope to study the Sun, to launch in 2017; and Euclid, a telescope to investigate "dark energy", to fly in 2020.

NASA plans a similar mission to Plato called Tess (Transiting Exoplanet Survey Satellite) in 2017, but the specifications mean that its rocky worlds will probably be in closer orbits around lower-mass stars than the discoveries made by the European project. In other words, the Plato planets are more likely to be in the habitable zones of more Sun-like stars.


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Friday, January 24, 2014

NEOWISE Reactivation Plus 25 Days

In its first 25 days of operations, the newly reactivated NEOWISE mission has detected 857 minor bodies in our solar system, including 22 near-Earth objects (NEOs) and four comets. Three of the NEOs are new discoveries; all three are hundreds of meters in diameter and dark as coal.


NEOWISE originally was called the Wide-field Infrared Survey Explorer (WISE), which had made the most comprehensive survey to date of asteroids and comets. The spacecraft was shut down in 2011 after its primary mission was completed. But in September 2013, it was reactivated, renamed and given a new mission, which is to assist NASA's efforts to identify the population of potentially hazardous near-Earth objects (NEOs). NEOWISE also can assist in characterizing previously detected asteroids that could be considered potential targets for future exploration missions.

More than 100 asteroids were captured in the above view from NASA's Wide-field Infrared Survey Explorer, or WISE, during its primary all-sky survey. Image credit: NASA/JPL-Caltech/UCLA

The NEOWISE mission has just passed its post-restart survey readiness review, and the project has verified that the ability to measure asteroid positions and brightness is as good as it was before the spacecraft entered hibernation in early 2011. At the present rate, NEOWISE is observing and characterizing approximately one NEO per day, giving astronomers a much better idea of the objects' sizes and compositions.

Out of the more than 10,500 NEOs that have been discovered to date, only about 10 percent have had any physical measurements made of them; the reactivated NEOWISE will more than double that number.

JPL manages the NEOWISE mission for NASA's Science Mission Directorate in Washington. The Space Dynamics Laboratory in Logan, Utah, built the science instrument. Ball Aerospace & Technologies Corp. of Boulder, Colo., built the spacecraft. 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 on NEOWISE is online at: http://www.jpl.nasa.gov/wise/ .


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Thursday, January 23, 2014

Landers That "Think On Their Feet", So to Speak

Engineers at NASA's Jet Propulsion Laboratory in Pasadena, California, are testing a sophisticated flight-control algorithm that could allow for more precise, pinpoint landings of future Martian spacecraft.

Flight testing of the new Fuel Optimal Large Divert Guidance algorithm - G-FOLD for short - for planetary pinpoint landing is being conducted jointly by JPL engineers in cooperation with Masten Space Systems in Mojave, Calif., using Masten's XA-0.1B "Xombie" vertical-launch, vertical-landing experimental rocket.

NASA's Space Technology Mission Directorate is facilitating the tests via its Game-Changing Development and Flight Opportunities Programs; the latter managed at NASA's Dryden Flight Research Center at Edwards Air Force Base, Calif. The two space technology programs work together to test game-changing technologies by taking advantage of Flight Opportunities' commercially provided suborbital platforms and flights.

Current powered-descent guidance algorithms used for spacecraft landings are inherited from the Apollo era. These algorithms do not optimize fuel usage and significantly limit how far the landing craft can be diverted during descent. The new G-FOLD algorithm invented by JPL autonomously generates fuel-optimal landing trajectories in real time and provides a key new technology required for planetary pinpoint landing. Pinpoint landing capability will allow robotic missions to access currently inaccessible science targets. For crewed missions, it will allow increased precision with minimal fuel requirements to enable landing larger payloads in close proximity to predetermined targets.

Masten Space Systems launched the Xombie July 30, 2013 from the company's test pad at the Mojave Air and Space Port. JPL and Masten are planning to conduct a second flight test with a more complicated divert profile in August, pending data analysis.

To simulate a course correction during a Martian entry in the July test, Masten's Xombie was given a vertical descent profile to an incorrect landing point. About 90 feet into the profile, the G-FOLD flight control software was automatically triggered to calculate a new flight profile in real-time, and the rocket was successfully diverted to the "correct" landing point some 2,460 feet away.

On September 20, 2013, another flight was made at the Mojave Air and Space Sport in the California desert. This flight was the conclusion of the test campaign to assess the performance of the G-FOLD algorithm under mission conditions. More ambitious than the previous flights, this test had the Xombie vehicle initially travel diagonally away from the target landing site. This simulated a worst-case spacecraft landing maneuver and forced the G-FOLD algorithm to calculate, in real time, a flight path that crossed over itself to reach the safe landing site.

The accurately executed half-mile-long (0.8-kilometer), three-dimensional divert shows the potential of what G-FOLD could mean for future space missions. Compared to the software used to land NASA's Mars Curiosity rover in August 2012, G-FOLD can provide six times more divert range for a lander of that class. Such a capability would be needed for landing on Europa or for human missions to Mars. G-FOLD also may reduce the difficulty of future robotic missions to Mars, allowing rovers to land closer to features of interest instead of driving long distances to reach them. A future rover similar to Curiosity might be able to land right next to a target of scientific interest like Mount Sharp instead of driving for a year to get there.

Even though this is the culmination of the current round of testing, JPL still has far-reaching plans for G-FOLD and for further tests of other landing technologies. "G-FOLD presents a dramatic improvement in our ability to execute large divert maneuvers with limited fuel," said Martin Regehr, who leads JPL's Autonomous Descent and Ascent Powered-flight Testbed (ADAPT). To further enhance future mission capability, JPL plans to use ADAPT to demonstrate terrain-relative navigation using the Lander Vision System (LVS) together with G-FOLD in 2014.

Click Here to Watch the September 20 Flight.

This effort was performed by JPL, with participation from the University of Texas at Austin; Masten Space Systems, Inc., Mojave, California; and NASA's Flight Opportunity Program, which is managed by NASA's Dryden Flight Research Center, Edwards, California.

Masten Space Systems is one of seven suborbital reusable launch companies contracted by NASA's Flight Opportunities Program to fly experiments in sub-orbital space to verify new technologies work as expected in this harsh environment.

JPL, a division of the California Institute of Technology, Pasadena, manages the Curiosity project for NASA's Science Mission Directorate, Washington. For information about Curiosity's accomplishments over the past year, visit: http://mars.jpl.nasa.gov/msl .

For more on flight tests of Curiosity's landing radar, visit: http://www.nasa.gov/topics/solarsystem/features/F-18_flying_msl_radar.html .

For more on NASA's Space Technology Mission Directorate, visit: http://www.nasa.gov/directorates/spacetech/home/ .


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