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        {
            "id": 14143,
            "url": "https://svs.gsfc.nasa.gov/14143/",
            "result_type": "Produced Video",
            "release_date": "2022-04-21T13:50:00-04:00",
            "title": "Lunar Eclipse Essentials - Updated",
            "description": "Learn more about how a lunar eclipse works by watching this video! || LunarEclipseEssentialThumbnail.jpg (1280x720) [319.2 KB] || LunarEclipseEssentialsThumbnail1.jpg (1280x720) [284.0 KB] || LunarEclipseEssentialThumbnail_print.jpg (1024x576) [267.9 KB] || LunarEclipseEssentialThumbnail_searchweb.png (320x180) [89.3 KB] || LunarEclipseEssentialThumbnail_thm.png (80x40) [5.5 KB] || Lunar_Eclipse_Essentials_UPDATED_YouTube.webm (1280x720) [13.9 MB] || Lunar_Eclipse_Essentials_UPDATED_YouTube.mp4 (1280x720) [203.5 MB] || Lunar_Eclipse_Essentials_UPDATED.mov (1280x720) [1.6 GB] || ",
            "hits": 301
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        {
            "id": 4593,
            "url": "https://svs.gsfc.nasa.gov/4593/",
            "result_type": "Visualization",
            "release_date": "2018-12-21T09:00:00-05:00",
            "title": "Earthrise in 4K",
            "description": "On December 24, 1968, Apollo 8 astronauts Frank Borman, Jim Lovell, and Bill Anders became the first humans to witness the Earth rising above the moon's barren surface. Now we can relive the astronauts' experience, thanks to data from NASA's Lunar Reconnaissance Orbiter. Complete transcript available.Watch this video on the NASA Goddard YouTube channel. || YOUTUBE_1080_G2018_Earthrise_Master_VX-300368_youtube_1080.mp4 (1920x1080) [882.1 MB] || earthrise_print.jpg (3840x2160) [515.7 KB] || earthrise_print_searchweb.png (180x320) [52.8 KB] || earthrise_print_thm.png (80x40) [4.6 KB] || TWITTER_720_G2018_Earthrise_Master_VX-300368_twitter_720.mp4 (1280x720) [114.9 MB] || FACEBOOK_720_G2018_Earthrise_Master_VX-300368_facebook_720.mp4 (1280x720) [641.1 MB] || YOUTUBE_720_G2018_Earthrise_Master_VX-300368_youtube_720.mp4 (1280x720) [832.1 MB] || G2018_Earthrise_Master_Output.en_US.srt [6.8 KB] || G2018_Earthrise_Master_Output.en_US.vtt [6.7 KB] || G2018_Earthrise_Master.webm (3840x2160) [107.0 MB] || G2018_Earthrise_Master.mp4 (3840x2160) [500.2 MB] || G2018_Earthrise_Master.mov (3840x2160) [19.6 GB] || G2018_Earthrise_Master.mp4.hwshow [82 bytes] || ",
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        {
            "id": 11831,
            "url": "https://svs.gsfc.nasa.gov/11831/",
            "result_type": "Produced Video",
            "release_date": "2015-04-03T12:00:00-04:00",
            "title": "NASA On Air: Lunar Eclipse April 4, 2015 at 4:58 AM PDT (4/4/2015)",
            "description": "LEAD: Early risers on Saturday morning (April 4, 2015) will have a chance to see the shortest total lunar eclipse of the century.1. The moon will turn red as it crosses the earth’s long shadow for less than five minutes.2. Why is the moon red rather than dark if it is in the earth’s shadow?3. Turns out the earth’s atmosphere acts as a filter and a prism.4. Similar to a sunset, the light becomes red.5. The earth’s atmospheric 'lens' bends this red light only slightly, which is enough to bask the 2000-mile diameter moon in red light.6. The lunar eclipse starts at 4:58 AM Pacific Daylight Time.TAG: Best viewing will be in the Western United States, early Saturday morning. The next total eclipse is not until September 2015. || WC_Lunar_Eclipse-1920-MASTER_iPad_1920x0180_print.jpg (1024x576) [110.7 KB] || WC_Lunar_Eclipse-1920-MASTER_iPad_1920x0180_searchweb.png (320x180) [68.5 KB] || WC_Lunar_Eclipse-1920-MASTER_iPad_1920x0180_web.png (320x180) [68.5 KB] || WC_Lunar_Eclipse-1920-MASTER_iPad_1920x0180_thm.png (80x40) [4.4 KB] || WC_Lunar_Eclipse-1920-MASTER_1920x1080.mov (1920x1080) [484.4 MB] || WC_Lunar_Eclipse-1920-MASTER_1280x720.mov (1280x720) [564.7 MB] || WC_Lunar_Eclipse-1920-MASTER_NBC_Today.mov (1920x1080) [160.1 MB] || WC_Lunar_Eclipse-1920-MASTER_WEA_CEN.wmv (1280x720) [12.8 MB] || WC_Lunar_Eclipse_.avi (1280x720) [16.8 MB] || WC_Lunar_Eclipse-1920-MASTER_baron.mp4 (1920x1080) [14.8 MB] || WC_Lunar_Eclipse-1920-MASTER_prores.mov (1920x1080) [404.8 MB] || WC_Lunar_Eclipse-1920-MASTER_iPad_960x540.m4v (960x540) [51.1 MB] || WC_Lunar_Eclipse-1920-MASTER_iPad_1280x720.m4v (1280x720) [81.8 MB] || WC_Lunar_Eclipse-1920-MASTER_iPad_1920x0180.m4v (1920x1080) [160.1 MB] || WC_Lunar_Eclipse-1920-MASTER_iPad_1920x0180.webm (1920x1080) [3.0 MB] || ",
            "hits": 116
        },
        {
            "id": 11828,
            "url": "https://svs.gsfc.nasa.gov/11828/",
            "result_type": "Produced Video",
            "release_date": "2015-04-02T11:00:00-04:00",
            "title": "Understanding Lunar Eclipses",
            "description": "Find out why the moon occasionally changes color. || c-1280.jpg (1280x720) [179.1 KB] || c-1024.jpg (1024x576) [129.7 KB] || c-1024_print.jpg (1024x576) [121.5 KB] || c-1024_searchweb.png (320x180) [64.6 KB] || c-1024_print_thm.png (80x40) [11.6 KB] || ",
            "hits": 431
        },
        {
            "id": 11756,
            "url": "https://svs.gsfc.nasa.gov/11756/",
            "result_type": "Produced Video",
            "release_date": "2015-03-17T11:00:00-04:00",
            "title": "Water On The Moon",
            "description": "A NASA spacecraft has found evidence of water ice buried beneath the lunar surface. || c-1280.jpg (1280x720) [254.2 KB] || c-1024.jpg (1024x576) [188.7 KB] || c-1024_print.jpg (1024x576) [170.1 KB] || c-1024_searchweb.png (320x180) [90.3 KB] || c-1024_print_thm.png (80x40) [18.3 KB] || ",
            "hits": 191
        },
        {
            "id": 4129,
            "url": "https://svs.gsfc.nasa.gov/4129/",
            "result_type": "Visualization",
            "release_date": "2013-12-20T10:00:00-05:00",
            "title": "Earthrise: The 45th Anniversary",
            "description": "In December of 1968, the crew of Apollo 8 became the first people to leave our home planet and travel to another body in space. But as crew members Frank Borman, James Lovell, and William Anders all later recalled, the most important thing they discovered was Earth.Using photo mosaics and elevation data from Lunar Reconnaissance Orbiter (LRO), this video commemorates the 45th anniversary of Apollo 8's historic flight by recreating the moment when the crew first saw and photographed the Earth rising from behind the Moon. Narrator Andrew Chaikin, author of A Man on the Moon, sets the scene for a three-minute visualization of the view from both inside and outside the spacecraft accompanied by the onboard audio of the astronauts.The visualization draws on numerous historical sources, including the actual cloud pattern on Earth from the ESSA-7 satellite and dozens of photographs taken by Apollo 8, and it reveals new, historically significant information about the Earthrise photographs. It has not been widely known, for example, that the spacecraft was rolling when the photos were taken, and that it was this roll that brought the Earth into view. The visualization establishes the precise timing of the roll and, for the first time ever, identifies which window each photograph was taken from.The key to the new work is a set of vertical stereo photographs taken by a camera mounted in the Command Module's rendezvous window and pointing straight down onto the lunar surface. It automatically photographed the surface every 20 seconds. By registering each photograph to a model of the terrain based on LRO data, the orientation of the spacecraft can be precisely determined.Andrew Chaikin's article Who Took the Legendary Earthrise Photo From Apollo 8? appeared in the January, 2018 issue of Smithsonian magazine. It includes the story of the making of this visualization.A Google Hangout discussion of this visualization between Ernie Wright (creator of the visualization), Andrew Chaikin, John Keller (LRO project scientist), and Aries Keck (NASA media specialist) was held on December 20, 2013. A replay of that hangout is available here.Ernie Wright presented a talk about the making of this animation at the 2014 SIGGRAPH Conference in Vancouver. He also wrote a NASA Wavelength blog entry about Earthrise that includes links to educator resources related to LRO. || ",
            "hits": 498
        },
        {
            "id": 4109,
            "url": "https://svs.gsfc.nasa.gov/4109/",
            "result_type": "Visualization",
            "release_date": "2013-10-02T00:00:00-04:00",
            "title": "Lunar Far Side: From Luna 3 to LRO",
            "description": "In October of 1959, the Luna 3 spacecraft launched from the Baikonur Cosmodrome in Kazakhstan. Luna 3 was the third spacecraft to reach the Moon and the first to send back pictures of the Moon's far side. The pictures were noisy and indistinct, but because the Moon always presents the same face to the Earth, they offered views of a part of the Moon that had never been seen before.The far side of the Moon is surprisingly different. The most striking difference evident in the Luna 3 pictures is the absence of the large, dark seas of cooled lava, called maria, that cover a substantial fraction of the Earth-facing near side. The far side is instead densely peppered with impact craters of every size and age.Fifty years later, in June of 2009, Lunar Reconnaissance Orbiter (LRO) launched from Kennedy Space Center in Florida. Using LRO's global elevation maps and photographic mosaics, both of which are of unprecedented quality and detail, it's possible to accurately recreate the view captured in the pictures from Luna 3. As seen here, Luna 3 was directly over 12°N 120°E at a distance of 61,700 kilometers above the surface, and its camera was banked 17.5° clockwise from vertical relative to the Moon's north pole.The thicker blue longitude line at 90°E, along the left side of the LRO image, marks the boundary between the near and far sides of the Moon. To the left of that line are the familiar maria Crisium (the circular spot near the 9 o'clock position), Marginis, Smythii (both east of Crisium), Humboldtianum (in the north), Australe (near the south pole), and the eastern edge of Fecunditatis. The bright spot near the center of the disk is a complex of unnamed craters bordered by King, Langemak, Gregory, and Abul Wafa craters. The brightness is enhanced because it's near the subsolar point. The dark, sharp-edged shield shape in the southern hemisphere, with the white dot in the middle, is Tsiolkovskiy crater and its central peak. The dark spot to the southeast of Tsiolkovskiy is the crater Jules Verne. The mare in the northeast is Moscoviense. || ",
            "hits": 335
        },
        {
            "id": 11283,
            "url": "https://svs.gsfc.nasa.gov/11283/",
            "result_type": "Produced Video",
            "release_date": "2013-07-25T00:00:00-04:00",
            "title": "Smiling In Space",
            "description": "The Mona Lisa is already one of the most famous paintings in the world, but it’s now being recognized for another reason: a digital version of it traveled 240,000 miles to the Lunar Reconnaissance Orbiter (LRO), a NASA satellite orbiting the moon. A black and white image of the painting was divided into an array of pixels, and each pixel was converted into one of 4,096 shades of gray. The image piggybacked on signals already being used to track the satellite, enabling simultaneous tracking and communication. Different shades of gray were represented by delaying the transmission of each laser pulse by a precise amount of time. After correcting transmission errors caused by Earth’s atmosphere, the demonstration became one of the first successful examples of laser communication at planetary distances, a method capable of much higher data transmission than traditional radio signals. Watch the video to learn more. || ",
            "hits": 102
        },
        {
            "id": 11137,
            "url": "https://svs.gsfc.nasa.gov/11137/",
            "result_type": "Produced Video",
            "release_date": "2013-01-17T12:00:00-05:00",
            "title": "NASA Beams Mona Lisa to Lunar Reconnaissance Orbiter at the Moon",
            "description": "As part of the first demonstration of laser communication with a satellite at the moon, scientists with NASA's Lunar Reconnaissance Orbiter (LRO) beamed an image of the Mona Lisa to the spacecraft from Earth.The iconic image traveled nearly 240,000 miles in digital form from the Next Generation Satellite Laser Ranging (NGSLR) Station at NASA's Goddard Space Flight Center in Greenbelt, MD, to the Lunar Orbiter Laser Altimeter (LOLA) instrument on the spacecraft. By transmitting the image piggyback on laser pulses that are routinely sent to track LOLA's position, the team achieved simultaneous laser communication and tracking.To learn more about how it happened, watch the video below! || ",
            "hits": 58
        },
        {
            "id": 4000,
            "url": "https://svs.gsfc.nasa.gov/4000/",
            "result_type": "Visualization",
            "release_date": "2012-11-20T12:00:00-05:00",
            "title": "Moon Phase and Libration, 2013",
            "description": " || The data in the table for the entire year can be downloaded as a JSON file or as a text file. || moon.0002.jpg (730x730) [94.6 KB] || comp.0001.tif (1920x1080) [2.3 MB] || ",
            "hits": 332
        },
        {
            "id": 3936,
            "url": "https://svs.gsfc.nasa.gov/3936/",
            "result_type": "Visualization",
            "release_date": "2012-04-19T00:00:00-04:00",
            "title": "Earthrise",
            "description": "The famous color photograph known as Earthrise, as well as a black-and-white image taken a minute earlier, document the moment when Earth was seen for the first time by human eyes from behind the Moon. They were taken on December 24, 1968 by the crew of Apollo 8, the first humans to leave low Earth orbit.The sight of a small, intensely blue Earth rising above the barren, gray horizon of the Moon was one of the few things that NASA and the crew of Apollo 8 had not thoroughly planned and rehearsed beforehand. As historian Robert Poole noted, this lack of preparation meant that the sight of Earth came with the force of a revelation, not just for the astronauts but for everyone on the ground. We came all this way to explore the Moon, Apollo 8 astronaut Bill Anders said, and the most important thing is that we discovered the Earth.Using the latest elevation data from Lunar Reconnaissance Orbiter, this visualization attempts to recreate what the astronauts saw. The virtual camera of the rendering software is put in the position of the Apollo 8 spacecraft at the time of the photographs, as the spacecraft emerged from its fourth pass behind the Moon. It shows a two-minute interval centered on 16:39:06 UT (10:39 a.m. Houston time) on December 24, 1968. This is around the time of AOS (acquisition of signal), the moment when radio contact is re-established after being lost on the far side of the Moon.The position and motion of the spacecraft are based on a state vector, a set of (x, y, z) position and (vx, vy, vz) velocity values, published in NASA's Apollo 8 Mission Report about a year after the flight. The animator translated these values, given in Moon-centered inertial coordinates for Besselian year 1969.0, into a modern coordinate system, then calculated an orbit. The spacecraft was 110 km (68 miles, 60 nautical miles) above the surface of the Moon at 11.2°S 113.8°E when the Earthrise photograph was taken. || ",
            "hits": 411
        },
        {
            "id": 10951,
            "url": "https://svs.gsfc.nasa.gov/10951/",
            "result_type": "Produced Video",
            "release_date": "2012-04-19T00:00:00-04:00",
            "title": "Earthrise 2.0",
            "description": "On December 24, 1968, three Apollo astronauts circled the moon, becoming the first humans ever to do so. On their fourth orbit, Apollo 8 Commander Frank Borman interrupted the studies of the moon's cratered terrain to roll the spacecraft, bringing the three main windows around to face the direction of travel. All of a sudden, a bright sliver of light appeared from behind the lunar horizon. Within seconds, a sphere with dazzling white swirls and vivid shades of blue came into view. The astronauts quickly positioned the onboard cameras, first capturing a black-and-white image of Earth rising, and then snapping a color photo of the Blue Planet floating above the horizon. This breathtaking color image would later become known as the iconic Earthrise photograph. The visualization uses data collected by NASA's Terra satellite and Lunar Reconnaissance Orbiter to re-create this historic moment in space exploration. || ",
            "hits": 230
        },
        {
            "id": 10961,
            "url": "https://svs.gsfc.nasa.gov/10961/",
            "result_type": "Produced Video",
            "release_date": "2012-04-19T00:00:00-04:00",
            "title": "NASA's Lunar Reconnaissance Orbiter Brings \"Earthrise\" to Everyone",
            "description": "On December 24, 1968, Apollo 8 Commander Frank Borman and crew members William A. Anders and James A. Lovell, Jr. became the first humans to photograph the Earth rising over the moon. Now, the rest of us can see what it was like in a new NASA visualization that draws on richly detailed maps of the moon's surface made from data gathered by NASA's Lunar Reconnaissance Orbiter!The narration in this visualization comes from the original audio recording of the Apollo 8 astronauts. The flight time has been compressed for effect. The Earth in this visualization is not an exact duplication of what the astronauts saw but a mosaic of more recent images taken by Earth-observing satellites. Representative clouds were then layered on top of the mosaic. || ",
            "hits": 281
        },
        {
            "id": 10948,
            "url": "https://svs.gsfc.nasa.gov/10948/",
            "result_type": "Produced Video",
            "release_date": "2012-04-05T00:00:00-04:00",
            "title": "Shrinking, Growing Moon",
            "description": "Ever since getting whacked by asteroids and cooked by heat radiating from unstable elements during its violent formation, the moon has cooled. Many things shrink as they cool and the moon is no exception. But tiny valleys discovered in new images from NASA's Lunar Reconnaissance Orbiter (LRO) indicate that the forces causing the moon to shrink were accompanied in some places by other forces acting to pull it apart. This tectonic tug-of-war taking place on the supposedly inert lunar surface surprised scientists. Not only that, it suggests the moon never completely melted in its early stages of evolution—unlike Earth and the other rocky planets—and instead was covered by an expansive ocean of molten rock. Watch the videos below to see evidence of these lunar valleys, called graben, and to learn more about the moon's fascinating geologic past. || ",
            "hits": 248
        },
        {
            "id": 3917,
            "url": "https://svs.gsfc.nasa.gov/3917/",
            "result_type": "Visualization",
            "release_date": "2012-03-15T00:00:00-04:00",
            "title": "Hyperwall: Three Moon Sites",
            "description": "Using elevation data returned by Lunar Reconnaissance Orbiter (LRO), these hyperwall-resolution animations visit three prominent features on the Moon's near side. || ",
            "hits": 137
        },
        {
            "id": 10931,
            "url": "https://svs.gsfc.nasa.gov/10931/",
            "result_type": "Produced Video",
            "release_date": "2012-03-15T00:00:00-04:00",
            "title": "Moon Struck",
            "description": "Long before the first humans gazed up into the velvety blackness of the night sky, the moon was young and fresh-faced. These were the early days, before the patchwork of inky stains called the Man in the Moon, before the brilliant starburst patterns called ray craters decorated the surface, before a colossal crash turned one-fifth of its real estate into the South Pole-Aitken basin. Fast-forward to the present, and the moon's once smooth contour appears flawed and disfigured, punished by explosive volcanic eruptions and raining interstellar objects that bombarded its surface over eons. In the visualizations below, see some of the clearest views of the moon yet, courtesy of NASA's Lunar Reconnaissance Orbiter, and witness a recreation of the destructive, 4.5-billion-year evolution of Earth's natural satellite. || ",
            "hits": 117
        },
        {
            "id": 3909,
            "url": "https://svs.gsfc.nasa.gov/3909/",
            "result_type": "Visualization",
            "release_date": "2012-03-14T11:00:00-04:00",
            "title": "Tour of the Moon: Additional Footage",
            "description": "This is additional footage produced for the narrated version of Tour of the Moon. It supplements the visualizations in entry 3874. || ",
            "hits": 92
        },
        {
            "id": 10929,
            "url": "https://svs.gsfc.nasa.gov/10929/",
            "result_type": "Produced Video",
            "release_date": "2012-03-14T10:00:00-04:00",
            "title": "A Narrated Tour of the Moon",
            "description": "Although the moon has remained largely unchanged during human history, our understanding of it and how it has evolved over time has evolved dramatically. Thanks to new measurements, we have new and unprecedented views of its surface, along with new insight into how it and other rocky planets in our solar system came to look the way they do. See some of the sights and learn more about the moon here! || ",
            "hits": 75
        },
        {
            "id": 10930,
            "url": "https://svs.gsfc.nasa.gov/10930/",
            "result_type": "Produced Video",
            "release_date": "2012-03-14T10:00:00-04:00",
            "title": "Evolution of the Moon",
            "description": "From year to year, the moon never seems to change. Craters and other formations appear to be permanent now, but the moon didn't always look like this. Thanks to NASA's Lunar Reconnaissance Orbiter, we now have a better look at some of the moon's history. Learn more in this video!This entry contains the Evolution of the Moon video in mutliple formats, including stereoscopic 3D in both side-by-side and individual left/right channel versions. It also includes a narrated and non-narrated version. Each individual video is labeled to make it easier to find the version that works for you! || ",
            "hits": 137
        },
        {
            "id": 10915,
            "url": "https://svs.gsfc.nasa.gov/10915/",
            "result_type": "Produced Video",
            "release_date": "2012-02-20T11:00:00-05:00",
            "title": "NASA Spacecraft Reveals Recent Geological Activity on the Moon",
            "description": "New images acquired by NASA's Lunar Reconnaissance Orbiter (LRO) spacecraft show that the moon's crust is being slightly stretched, forming small valleys - at least in some small areas. High-resolution images obtained by the Lunar Reconnaissance Orbiter Camera (LROC) provide evidence that these valleys are very young, suggesting the moon has experienced relatively recent geologic activity. || ",
            "hits": 55
        },
        {
            "id": 3894,
            "url": "https://svs.gsfc.nasa.gov/3894/",
            "result_type": "Visualization",
            "release_date": "2012-01-01T00:00:00-05:00",
            "title": "Moon Phase and Libration, 2012",
            "description": " || The data in the table for the entire year can be downloaded as a JSON file or as a text file. || moon.0001.jpg (730x730) [67.4 KB] || moon.0001.tif (1920x1080) [1.1 MB] || ",
            "hits": 535
        },
        {
            "id": 10836,
            "url": "https://svs.gsfc.nasa.gov/10836/",
            "result_type": "Produced Video",
            "release_date": "2011-10-20T00:00:00-04:00",
            "title": "Moon Wobble",
            "description": "From Earth we only see one face of the moon. But it's not always the exact same face. The moon rotates once on its own axis during each 27-day journey around the Earth. But as the moon makes its elliptical orbit, its velocity varies and alters that synchronicity, causing our perspective of the \"light side\" to appear at slightly different angles throughout any given month. In short, the moon wobbles. At least, it does to our eyes. A casual glance skyward won't reveal this, but when a full month of lunar views gets compressed into 12 seconds, as in the visualization below, it's impossible to miss. This rocking like a ship at sea is called libration, from the Latin for balance scale. Instead of just one side, we actually see about 59 percent of the lunar surface over the course of an orbit. The sped up view also reveals how the apparent size of the moon changes in the sky depending on where it is in its elliptical orbit. Its farthest point, the apogee, and nearest point, perigee, differ by more than 10 percent. Watch in the visualization below just how much the moon's face, from a Northern Hemisphere perspective, has wobbled throughout this year. || ",
            "hits": 841
        },
        {
            "id": 10818,
            "url": "https://svs.gsfc.nasa.gov/10818/",
            "result_type": "Produced Video",
            "release_date": "2011-09-06T10:00:00-04:00",
            "title": "New LRO Images Offer Sharper Views of Apollo 12, 14, and 17 Sites",
            "description": "NASA's Lunar Reconnaissance Orbiter (LRO) has captured the sharpest images ever taken from space of the Apollo 12, 14 and 17 sites, revealing the twists and turns of the paths made when the astronauts explored these areas. || ",
            "hits": 1141
        },
        {
            "id": 3836,
            "url": "https://svs.gsfc.nasa.gov/3836/",
            "result_type": "Visualization",
            "release_date": "2011-06-29T13:00:00-04:00",
            "title": "LRO at the June 15, 2011 Lunar Eclipse: View from the Moon",
            "description": "For Lunar Reconnaissance Orbiter (LRO), the lunar eclipse on June 15, 2011 is likely to be the longest and darkest of its life. This matters because LRO relies on sunlight to power its systems and instruments. Although it spends half of every orbit on the night side of the Moon, each night side pass lasts only an hour. For the June 15 eclipse, LRO will be in the dark for more than twice as long.During a previous total eclipse, LRO hibernated, turning off all of its instruments to conserve its battery power until the Moon emerged from the Earth's shadow. For the June 15 event, LRO will leave on the Diviner Lunar Radiometry Experiment. Diviner will measure the cooling of the Moon's surface during the eclipse. This unique temperature record is expected to reveal information about the roughness and composition of the swath of lunar surface visible to Diviner's sensors during the eclipse.The visualization archived on this page shows the view of the eclipse from the Moon, looking back toward the Earth and the Sun. On the Moon, this event is a solar eclipse. As the Sun disappears behind the Earth, the umbral shadow sweeps across the lunar landscape, and as our eyes adjust to the darkness, the stars come out, and the lunar surface looks a dull red. The atmosphere of the Earth lights up as a red ring around the planet, the sunrises and sunsets all around the edge of the globe lending their faint light to the Moon while the Sun is otherwise blocked. At the start of the eclipse, Australia is facing us, but over time, the Moon sets in eastern Australia while southern Africa rotates into view. LRO streaks through the frame several times on its orbit 50 kilometers above the Moon's surface.Other visualizations in this series depict the view of the eclipsealong the shadow line, with the figures of the umbra, penumbra, and lunar and solar pathsthrough a telescope on Earthflying above LRO as Diviner takes temperature measurementsA narrated piece that uses these visualizations is available in entry #10794. For an explanation of lunar eclipses, visit entry #10787. || ",
            "hits": 124
        },
        {
            "id": 3810,
            "url": "https://svs.gsfc.nasa.gov/3810/",
            "result_type": "Visualization",
            "release_date": "2011-06-13T09:00:00-04:00",
            "title": "Moon Phase and Libration, 2011",
            "description": " || The data in the table for the entire year can be downloaded as a JSON file or as a text file. || moon.0001.jpg (730x730) [36.2 KB] || moon.0001.tif (1920x1080) [852.2 KB] || ",
            "hits": 578
        },
        {
            "id": 3833,
            "url": "https://svs.gsfc.nasa.gov/3833/",
            "result_type": "Visualization",
            "release_date": "2011-06-13T00:00:00-04:00",
            "title": "LRO at the June 15, 2011 Lunar Eclipse: Shadow View",
            "description": "For Lunar Reconnaissance Orbiter (LRO), the lunar eclipse on June 15, 2011 is likely to be the longest and darkest of its life. This matters because LRO relies on sunlight to power its systems and instruments. Although it spends half of every orbit on the night side of the Moon, each night side pass lasts only an hour. For the June 15 eclipse, LRO will be in the dark for more than twice as long.During a previous total eclipse, LRO hibernated, turning off all of its instruments to conserve its battery power until the Moon emerged from the Earth's shadow. For the June 15 event, LRO will leave on the Diviner Lunar Radiometry Experiment. Diviner will measure the cooling of the Moon's surface during the eclipse. This unique temperature record is expected to reveal information about the roughness and composition of the swath of lunar surface visible to Diviner's sensors during the eclipse.The visualization archived on this page shows the view of the eclipse along the axis of the Earth's shadow, with the figures of the umbra, penumbra, and lunar and solar paths in the background. This is the view typically used in eclipse diagrams like those produced by Fred Espenak for the NASA Eclipse site.Other visualizations in this series depict the view of the eclipsefrom the Moon, where the event is a solar eclipsethrough a telescope on Earthflying above LRO as Diviner takes temperature measurementsA narrated piece that uses these visualizations is available in entry #10794. For an explanation of lunar eclipses, visit entry #10787. || ",
            "hits": 32
        },
        {
            "id": 3834,
            "url": "https://svs.gsfc.nasa.gov/3834/",
            "result_type": "Visualization",
            "release_date": "2011-06-13T00:00:00-04:00",
            "title": "LRO at the June 15, 2011 Lunar Eclipse: Earth View",
            "description": "For Lunar Reconnaissance Orbiter (LRO), the lunar eclipse on June 15, 2011 is likely to be the longest and darkest of its life. This matters because LRO relies on sunlight to power its systems and instruments. Although it spends half of every orbit on the night side of the Moon, each night side pass lasts only an hour. For the June 15 eclipse, LRO will be in the dark for more than twice as long.During a previous total eclipse, LRO hibernated, turning off all of its instruments to conserve its battery power until the Moon emerged from the Earth's shadow. For the June 15 event, LRO will leave on the Diviner Lunar Radiometry Experiment. Diviner will measure the cooling of the Moon's surface during the eclipse. This unique temperature record is expected to reveal information about the roughness and composition of the swath of lunar surface visible to Diviner's sensors during the eclipse.The visualization archived on this page shows the eclipse as it might appear through a telescope on Earth (except that you can't see LRO in such a telescope). Celestial north is up. As the Moon enters the umbra (the part of the shadow in which the Sun is completely blocked by the Earth), the shadowed side of the Moon appears black while the sunlit side remains bright. Only when the Moon is almost completely within the umbra is it possible to see the faint red glow of the shadowed side, some 10,000 times fainter than the sunlit Moon. The redness is sunlight filtered and refracted by Earth's atmosphere. The same effect reddens sunrises and sunsets on Earth.Other visualizations in this series depict the view of the eclipsefrom the Moon, where the event is a solar eclipsealong the shadow line, with the figures of the umbra, penumbra, and lunar and solar pathsflying above LRO as Diviner takes temperature measurementsA narrated piece that uses these visualizations is available in entry #10794. For an explanation of lunar eclipses, visit entry #10787. || ",
            "hits": 38
        },
        {
            "id": 3835,
            "url": "https://svs.gsfc.nasa.gov/3835/",
            "result_type": "Visualization",
            "release_date": "2011-06-13T00:00:00-04:00",
            "title": "LRO's Diviner during the June 15, 2011 Lunar Eclipse",
            "description": "For Lunar Reconnaissance Orbiter (LRO), the lunar eclipse on June 15, 2011 is likely to be the longest and darkest of its life. This matters because LRO relies on sunlight to power its systems and instruments. Although it spends half of every orbit on the night side of the Moon, each night side pass lasts only an hour. For the June 15 eclipse, LRO will be in the dark for more than twice as long.During a previous total eclipse, LRO hibernated, turning off all of its instruments to conserve its battery power until the Moon emerged from the Earth's shadow. For the June 15 event, LRO will leave on the Diviner Lunar Radiometry Experiment. Diviner will measure the cooling of the Moon's surface during the eclipse. This unique temperature record is expected to reveal information about the roughness and composition of the swath of lunar surface visible to Diviner's sensors during the eclipse.The visualization archived on this page shows LRO flying over the lunar surface during the darkest part of the eclipse, with Diviner measuring temperatures along a swath about 3.5 kilometers wide. LRO will pass this part of the surface again during the eclipse, and it will tilt a bit so that Diviner can point at the same strip of lunar surface. The difference between the two temperature readings gives the rate of cooling at each point along the swath.Other visualizations in this series depict the view of the eclipsefrom the Moon, where the event is a solar eclipsealong the shadow line, with the figures of the umbra, penumbra, and lunar and solar pathsthrough a telescope on EarthA narrated piece that uses these visualizations is in entry #10794. For an explanation of lunar eclipses, visit entry #10787. || ",
            "hits": 86
        },
        {
            "id": 10787,
            "url": "https://svs.gsfc.nasa.gov/10787/",
            "result_type": "Produced Video",
            "release_date": "2011-06-08T00:00:00-04:00",
            "title": "Lunar Eclipse Essentials",
            "description": "When the moon passes through the Earth's shadow, it causes the moon to look very unusual for a short period of time. This event is called a lunar eclipse, and it occurs roughly twice a year. Learn more about how lunar eclipses work in this video!These videos and animations are available in both standard formats as well as stereoscopic 3D for those who can view it. We've included left and right eye clips, a side-by-side version, and an anaglyph (red/blue) version of the narrated video, and left and right eye clips for each of the animations. The labels next to each link will help you pick! || ",
            "hits": 212
        },
        {
            "id": 10743,
            "url": "https://svs.gsfc.nasa.gov/10743/",
            "result_type": "Produced Video",
            "release_date": "2011-03-31T00:00:00-04:00",
            "title": "LEND: The Lunar Neutron Counter",
            "description": "How would you find out where to look for water on the Moon? NASA's Lunar Reconnaissance Orbiter has a unique answer: Count the neutrons coming from the Moon! By measuring the relative amounts of slow and fast neutrons coming from soil on the Moon, scientists think they can estimate the amount of hydrogen. And it's believed that where there's hydrogen, there might also be water! Find out more about LEND by watching this video. || ",
            "hits": 27
        },
        {
            "id": 10697,
            "url": "https://svs.gsfc.nasa.gov/10697/",
            "result_type": "Produced Video",
            "release_date": "2010-12-17T08:00:00-05:00",
            "title": "LOLA AGU Presentation Support",
            "description": "NASA's Lunar Reconnaissance Orbiter is allowing researchers to create the most precise and complete elevation map to date of the moon's complex, heavily cratered landscape. || ",
            "hits": 54
        },
        {
            "id": 10684,
            "url": "https://svs.gsfc.nasa.gov/10684/",
            "result_type": "Produced Video",
            "release_date": "2010-10-21T13:55:00-04:00",
            "title": "LRO Supports LCROSS - Quicktime and Windows Media versions",
            "description": "This video shows how the LEND instrument was used to help locate an ideal impact site for the LCROSS spacecraft. It also shows the DIVINER instrument taking measurements after the LCROSS impact. || lro_over_lcross_ipod_lg.00252_print.jpg (1024x576) [129.9 KB] || lro_over_lcross_ipod_lg_web.png (320x180) [241.8 KB] || lro_over_lcross_ipod_lg_thm.png (80x40) [14.5 KB] || lro_over_lcross_appletv.m4v (960x540) [17.3 MB] || lro_over_lcross_prores.mov (1280x720) [251.4 MB] || lro_over_lcross_wmv.wmv (1280x720) [16.3 MB] || lro_over_lcross_youtube_hq.mov (1280x720) [18.5 MB] || lro_over_lcross_appletv.webmhd.webm (960x540) [6.5 MB] || lro_over_lcross_ipod_lg.m4v (640x360) [5.5 MB] || lro_over_lcross_nasaportal.mov (640x360) [13.5 MB] || lro_over_lcross_nasacast.mp4 (320x240) [2.7 MB] || lro_over_lcross_svs.mpg (512x288) [4.1 MB] || ",
            "hits": 18
        },
        {
            "id": 10686,
            "url": "https://svs.gsfc.nasa.gov/10686/",
            "result_type": "Produced Video",
            "release_date": "2010-10-21T13:55:00-04:00",
            "title": "LRO Observes the LCROSS Impact",
            "description": "NASA scientists have revealed the lunar soil inside shadowy craters is rich in useful materials, that the moon is chemically active, and that it also has a water cycle. The Lunar Reconnaissance Orbiter, by observing the impact of the LCROSS spacecraft, helped contribute to these new findings. || ",
            "hits": 58
        },
        {
            "id": 10595,
            "url": "https://svs.gsfc.nasa.gov/10595/",
            "result_type": "Produced Video",
            "release_date": "2010-06-23T00:00:00-04:00",
            "title": "Ten Cool Things Seen in the First Year of LRO",
            "description": "Having officially reached lunar orbit on June 23nd, 2009, the Lunar Reconnaissance Orbiter (LRO) has now marked one full year on its mission to scout the moon. Maps and datasets collected by LRO's state-of-the-art instruments will form the foundation for all future lunar exploration plans, as well as be critical to scientists working to better understand the moon and its environment. In only the first year of the mission, LRO has gathered more digital information than any previous planetary mission in history. To celebrate one year in orbit, here are ten cool things already observed by LRO. Note that the stories here are just a small sample of what the LRO team has released and barely touch on the major scientific accomplishments of the mission. If you like these, visit the official LRO web site at www.nasa.gov/LRO to find out even more! || ",
            "hits": 242
        },
        {
            "id": 10528,
            "url": "https://svs.gsfc.nasa.gov/10528/",
            "result_type": "Produced Video",
            "release_date": "2009-09-17T00:00:00-04:00",
            "title": "LRO Early Results Press Conference",
            "description": "NASA showcased new images from the Lunar Reconnaissance Orbiter's seven instruments and provided updates about the topography of the moon's south pole during a news conference on September 17. NASA also provided an update about the spacecraft's status and mission plans. The briefing took place at NASA's Goddard Space Flight Center in Greenbelt, Md. (no transcript available) || LRO_1stResults_PressConf_ipod.00002_print.jpg (1024x576) [115.7 KB] || LRO_1stResults_PressConf_ipod_web.png (320x180) [138.1 KB] || LRO_1stResults_PressConf_ipod_thm.png (80x40) [16.1 KB] || LRO_1stResults_PC_appleTV.webmhd.webm (960x540) [499.4 MB] || LRO_1stResults_PC_appleTV.m4v (960x540) [1.4 GB] || LRO_1stResults_PressConf_ipod.m4v (640x360) [586.3 MB] || ",
            "hits": 11
        },
        {
            "id": 10479,
            "url": "https://svs.gsfc.nasa.gov/10479/",
            "result_type": "Produced Video",
            "release_date": "2009-09-11T00:00:00-04:00",
            "title": "A Tour of the LRO Instrument Suite",
            "description": "Lunar Reconnaissance Orbiter Project Scientist Rich Vondrak explains the LRO suite of instruments and how each will greatly benefit our understanding of the Moon.For complete transcript, click here. || LRO_vondrak_ipod.02402_print.jpg (1024x576) [90.1 KB] || LRO_vondrak_ipod_web.png (320x180) [177.9 KB] || LRO_vondrak_ipod_thm.png (80x40) [16.3 KB] || LRO_vondrak_ipod.webmhd.webm (960x540) [46.3 MB] || LRO_vondrak_ipod.m4v (640x360) [70.8 MB] || LRO_vondrak.wmv (320x236) [37.5 MB] || LRO_vondrak_nasacast.mp4 (320x176) [21.6 MB] || ",
            "hits": 9
        },
        {
            "id": 3620,
            "url": "https://svs.gsfc.nasa.gov/3620/",
            "result_type": "Visualization",
            "release_date": "2009-07-16T00:00:00-04:00",
            "title": "Apollo Landing Sites, with Shadows",
            "description": "The six Apollo lunar landing sites are all relatively near the equator on the side of the Moon that faces the Earth. Left behind at each site is the lower half of the Lunar Module, called the descent stage. It carried most of the astronauts' supplies and served as the launchpad for their return trip to the Command and Service Module in orbit around the Moon.LROC, the Lunar Reconnaissance Orbiter Camera, will have a number of opportunities to photograph the Apollo landing sites. Despite the excellent half-meter resolution of LROC's narrow angle cameras, the LM descent stage at each site can fill only a few pixels of these images. If photographed when the Sun is low in the lunar sky, however, the long shadow formed by the descent stage is easily discernable.This brief animation shows the locations of the Apollo landing sites, with lengthening shadows as each site approaches lunar nightfall. The lighting simulates the angle of the Sun during the second week of July, 2009, when LROC took its first images of the sites. The gold LM markers are about 20,000 times actual size. || ",
            "hits": 429
        },
        {
            "id": 10447,
            "url": "https://svs.gsfc.nasa.gov/10447/",
            "result_type": "Produced Video",
            "release_date": "2009-07-07T00:00:00-04:00",
            "title": "Flyover of the First Images from the Lunar Reconnaissance Orbiter Camera",
            "description": "A starkly beautiful region a few kilometers east of Hell E crater, which is located on the floor of the ancient Imbrian-aged Deslandres impact structure in the lunar highlands south of Mare Nubium. Numerous small, secondary craters can be identified, including several small crater chains. Also identifiable are distinctive lineations made readily apparent by the extreme lighting, representing ejecta from a nearby impact. The NAC image shown here has not been calibrated and the pixel values were stretched to enhance contrast. Image width is 3.5 km x 70 km; north is down. || ",
            "hits": 22
        },
        {
            "id": 10444,
            "url": "https://svs.gsfc.nasa.gov/10444/",
            "result_type": "Produced Video",
            "release_date": "2009-06-23T00:00:00-04:00",
            "title": "LRO Enters Lunar Orbit (full live event)",
            "description": "This entry is the full one hour program that was produced live during the orbit insertion event. To see just a short portion of highlights from the event, see entry #10445 || ",
            "hits": 39
        },
        {
            "id": 10438,
            "url": "https://svs.gsfc.nasa.gov/10438/",
            "result_type": "Produced Video",
            "release_date": "2009-05-21T00:00:00-04:00",
            "title": "LRO: Mapping Our Future",
            "description": "The Lunar Reconnaissance Orbiter (LRO) is the first mission in NASA's planned return to the moon. LRO is an unmanned mission to create the comprehensive atlas of the moon's features and resources necessary to design all future lunar exploration efforts. LRO focuses on the selection of safe landing sites, identification of lunar resources and the study of how lunar radiation will affect humans.For complete transcript, click here. || LRO_MappingOurFuture_ipod.00905_print.jpg (1024x576) [30.4 KB] || LRO_MappingOurFuture_ipod_web.png (320x180) [33.3 KB] || LRO_MappingOurFuture_ipod_thm.png (80x40) [3.6 KB] || LRO_MappingOurFuture_AppleTV.webmhd.webm (960x540) [84.8 MB] || LRO_MappingOurFuture_YouTube.mov (1280x720) [100.5 MB] || LRO_MappingOurFuture_fullres.mov (1280x720) [192.6 MB] || LRO_MappingOurFuture_AppleTV.m4v (960x540) [210.6 MB] || LRO_MappingOurFuture_ipod.m4v (640x360) [67.2 MB] || GSFC_20090521_LRO_m10438_Mapping1a.en_US.srt [7.5 KB] || GSFC_20090521_LRO_m10438_Mapping1a.en_US.vtt [7.5 KB] || LRO_MappingOurFuture_320x240.mp4 (320x240) [16.6 MB] || LRO_MappingOurFuture_portal.wmv (346x260) [48.7 MB] || LRO_MappingOurFuture_svs.mpg (512x288) [54.2 MB] || ",
            "hits": 147
        },
        {
            "id": 10249,
            "url": "https://svs.gsfc.nasa.gov/10249/",
            "result_type": "Produced Video",
            "release_date": "2009-05-14T00:00:00-04:00",
            "title": "LRO L-14 Press Conference Supporting Videos",
            "description": "LRO From Launch to OrbitThis video starts with LRO launch animation, shows the spacecraft's path to orbit, and ends with the spacecraft animated over the lunar surface. || LRO_L14_LaunchtoOrbit_50sec_ipod00702_print.jpg (1024x576) [91.7 KB] || LRO_L14_LaunchtoOrbit_50sec_ipod_web.png (320x180) [156.1 KB] || LRO_L14_LaunchtoOrbit_50sec_fullres.webmhd.webm (960x540) [11.4 MB] || LRO_L14_LaunchtoOrbit_50sec_fullres.mov (1280x720) [30.0 MB] || LRO_L14_LaunchtoOrbit_50sec_ipod.m4v (640x360) [8.8 MB] || LRO_L14_LaunchtoOrbit_50sec_svs.mpg (512x288) [7.6 MB] || LRO_L14_LaunchtoOrbit_50sec_portal.wmv (346x260) [7.1 MB] || LRO_L14_LaunchtoOrbit_50sec_fullres.mov.hwshow [218 bytes] || ",
            "hits": 14
        },
        {
            "id": 3577,
            "url": "https://svs.gsfc.nasa.gov/3577/",
            "result_type": "Visualization",
            "release_date": "2009-05-12T00:00:00-04:00",
            "title": "Permanent Shadows on the Moon",
            "description": "As the Earth and Moon orbit around the Sun, there are places on the Moon that never receive direct sunlight. Most of these permanently shadowed regions are at the lunar poles. This animation approximates the permanently shadowned regions pertaining to the Moon's south pole by maintaining a maximum sun angle to the surface of 1.5 degrees. These permanently shadowed areas are of interest because they could hold water ice. (NOTE: South Pole Digital Elevation Maps [DEM] based on publically released JAXA/Selene data.) || ",
            "hits": 412
        },
        {
            "id": 3576,
            "url": "https://svs.gsfc.nasa.gov/3576/",
            "result_type": "Visualization",
            "release_date": "2009-05-08T00:00:00-04:00",
            "title": "LRO Ground Track",
            "description": "A satellite's ground track shows the path of its orbit on the surface of the parent body. Lunar Reconnaissance Orbiter will be placed in a nearly circular polar orbit about 50 kilometers (31 miles) above the surface of the Moon, completing each orbit in a little less than two hours. The orientation of this orbit remains fixed in space, relative to the stars, while the Moon slowly rotates beneath it as they travel together around the Earth, allowing LRO to scan the entire surface of the Moon every two weeks.As this animation shows, the density of the ground coverage provided by a polar orbit is greatest at the poles. For the Moon, this is also where a great deal of current interest lies, since permanently shadowed areas at the poles may harbor water ice. This is also where some high-altitude areas are in gentle but perennial sunlight, providing the lighting and power supply for extended human exploration.The animation depicts LRO's ground track over a period of seven days (89 orbits). The elevation map comprises low-resolution data from a number of sources, including the Clementine and JAXA/SELENE spacecraft, combined with high-resolution insets for the regions near the poles. The surface color is derived from photographs taken by Clementine. || ",
            "hits": 207
        },
        {
            "id": 10378,
            "url": "https://svs.gsfc.nasa.gov/10378/",
            "result_type": "Produced Video",
            "release_date": "2009-03-24T00:00:00-04:00",
            "title": "LRO Interview: Rich Vondrak, Project Scientist",
            "description": "Rich Vondrak is the Project Scientist for the Lunar Reconnaissance Orbiter (LRO) mission. The following soundbites from Vondrak give information about the LRO mission's objectives and importance. || Vondrak_01_intro_640x360.04097_print.jpg (1024x576) [58.3 KB] || Vondrak_01_intro_640x360_web.png (320x180) [170.3 KB] || Vondrak_01_intro_640x360_thm.png (80x40) [16.3 KB] || LRO_invu_Vondrak_fullres.webmhd.webm (960x540) [47.8 MB] || LRO_invu_Vondrak_fullres.mov (1280x720) [142.0 MB] || LRO_invu_Vondrak_prores.mov (1280x720) [3.6 GB] || LRO_invu_Vondrak_ipod.m4v (640x360) [42.6 MB] || LRO_invu_Vondrak_svs.mpg (512x288) [34.1 MB] || ",
            "hits": 17
        }
    ]
}