{
    "count": 44,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 14445,
            "url": "https://svs.gsfc.nasa.gov/14445/",
            "result_type": "Produced Video",
            "release_date": "2023-10-25T15:00:00-04:00",
            "title": "Atmospheric Gravity Waves Imagery",
            "description": "Atmospheric gravity waves are similar to what happens when you drop a stone into a calm pond, but they roll through the air and cloud tops instead of water. Just like waves form in the ocean or a lake when water is disturbed, waves also form in the atmosphere when air is disturbed. They form when air is forced upward by hills or mountains into a layer of stable air in the atmosphere. Gravity causes the air to fall back down, and it begins to oscillate, creating a ripple effect. Wind flowing over the Rocky Mountains, for example, can create gravity waves that are felt as turbulence on an airplane. || ",
            "hits": 543
        },
        {
            "id": 31139,
            "url": "https://svs.gsfc.nasa.gov/31139/",
            "result_type": "Hyperwall Visual",
            "release_date": "2020-05-08T00:00:00-04:00",
            "title": "Earth: A System of Systems (updated)",
            "description": "All six time-synchronous datasets, individually and then layered two at a time || layered_pairs_1080p.00001_print.jpg (1024x576) [59.0 KB] || layered_pairs_1080p.00001_searchweb.png (320x180) [42.0 KB] || layered_pairs_1080p.00001_thm.png (80x40) [3.8 KB] || layered_pairs_720p.mp4 (1280x720) [83.6 MB] || layered_pairs_1080p.webm (1920x1080) [28.6 MB] || layered_pairs_1080p.mp4 (1920x1080) [157.7 MB] || layered_pairs_2160p.mp4 (3840x2160) [432.6 MB] || A_System_of_Systems_Updated_-_30701.pptx [436.3 MB] || ",
            "hits": 73
        },
        {
            "id": 4782,
            "url": "https://svs.gsfc.nasa.gov/4782/",
            "result_type": "Visualization",
            "release_date": "2020-03-04T00:00:00-05:00",
            "title": "Vegetation Index Anomalies and Rift Valley fever (RVF) outbreaks in South Africa region: 2008-2011",
            "description": "This visualization with corresponding data dashboard shows the relationship between vegetation index anomalies and outbreaks of Rift Valley fever (RVF) during 2008 and 2011 in the South Africa region. The sequence starts in 2007 looking at the entire continent of Africa and zooms in the region of South Africa to take a closer look at the patterns between ENSO events (El Niño and La Niña), above normal vegetaion over land (green) and RVF outbreak locations (orange pins). || NDVI_RVF_SAfrica_Composite_3840x2160_2657_print.jpg (1024x576) [102.7 KB] || NDVI_RVF_SAfrica_Composite_3840x2160_2657_searchweb.png (320x180) [57.8 KB] || NDVI_RVF_SAfrica_Composite_3840x2160_2657_thm.png (80x40) [5.0 KB] || NDVI_RVF_SAfrica_Composite_1920x1080p30.mp4 (1920x1080) [35.6 MB] || NDVI_RVF_SAfrica_Composite_1920x1080p30.webm (1920x1080) [7.1 MB] || Composite (3840x2160) [0 Item(s)] || Composite (3840x2160) [0 Item(s)] || NDVI_RVF_SAfrica_Composite_3840x2160_p30.mp4 (3840x2160) [72.6 MB] || NDVI_RVF_SAfrica_Composite_3840x2160_2657.tif (3840x2160) [31.6 MB] || ",
            "hits": 38
        },
        {
            "id": 4783,
            "url": "https://svs.gsfc.nasa.gov/4783/",
            "result_type": "Visualization",
            "release_date": "2020-02-27T00:00:00-05:00",
            "title": "Precipitation Anomaly and Rift Valley fever (RVF) outbreaks in South Africa: 2008-2011",
            "description": "This visualization with corresponding data dashboard shows the relationship between precipitation anomalies and outbreaks of Rift Valley fever (RVF) during 2008 and 2011 in the South Africa region. The sequence starts in 2007 looking at the entire continent of Africa and zooms in the region of South Africa to take a closer look at the patterns between ENSO events (El Niño and La Niña), above normal precipitation over land (blue) and RVF outbreak locations (orange pins). || PrecipRVF_SAfrica_Composite_3840x2160_3422_print.jpg (1024x576) [97.8 KB] || PrecipRVF_SAfrica_Composite_3840x2160_3422_searchweb.png (320x180) [57.6 KB] || PrecipRVF_SAfrica_Composite_3840x2160_3422_thm.png (80x40) [5.2 KB] || PrecipRVF_SAfrica_Composite_1920x1080p30.mp4 (1920x1080) [31.5 MB] || Composite (3840x2160) [0 Item(s)] || Composite (3840x2160) [0 Item(s)] || PrecipRVF_SAfrica_Composite_3840x2160_p30.mp4 (3840x2160) [68.2 MB] || PrecipRVF_SAfrica_Composite_3840x2160_3422.tif (3840x2160) [4.0 MB] || PrecipRVF_SAfrica_Composite_3840x2160_p30.webm (3840x2160) [14.1 MB] || ",
            "hits": 26
        },
        {
            "id": 4724,
            "url": "https://svs.gsfc.nasa.gov/4724/",
            "result_type": "Visualization",
            "release_date": "2020-02-21T00:00:00-05:00",
            "title": "Vegetation index anomalies and Rift Valley fever (RVF) outbreaks in Africa and Middle East during 2000-2018",
            "description": "Data visualization featuring vegetation index anomalies over Africa and Middle East and locations of Rift Valley Fever (RVF) outbreaks (orange pins) during the period of 2000-2018. Frames are provided in 4K resolution. || Africa_NDVIRVF_2000_2018_3840x2160_2430_print.jpg (1024x576) [78.8 KB] || Africa_NDVIRVF_2000_2018_3840x2160_2430_searchweb.png (320x180) [48.8 KB] || Africa_NDVIRVF_2000_2018_3840x2160_2430_thm.png (80x40) [4.4 KB] || Africa_NDVIRVFComposite_2000_2018_3840x2160_1080p30.mp4 (1920x1080) [88.7 MB] || Africa_NDVIRVFComposite_2000_2018_3840x2160_1080p30.webm (1920x1080) [25.5 MB] || Africa_NDVIRVF_2000_2018_Composite (3840x2160) [0 Item(s)] || Africa_NDVIRVF_2000_2018_3840x2160_2430.tif (3840x2160) [6.0 MB] || Africa_NDVIRVFComposite_2000_2018_3840x2160_p30.mp4 (3840x2160) [283.2 MB] || ",
            "hits": 37
        },
        {
            "id": 4747,
            "url": "https://svs.gsfc.nasa.gov/4747/",
            "result_type": "Visualization",
            "release_date": "2020-02-21T00:00:00-05:00",
            "title": "Vegetation index anomalies and Rift Valley fever (RVF) outbreaks in South Africa during 2009-2011",
            "description": "This visualization shows the relationship between vegetation index anomalies (Normalized Difference Vegetation Index - NDVI) data and outbreak locations of Rift Valley fever (RVf) during 2008 and 2011. The sequence starts in 2007 looking at the entire continent of Africa and zooms in the region of South Africa slowly to take a closer look at the above normal vegetation (green) and RVF outbreak locations (orange pins). Frames are provided in 4K resolution. || SAfrica_NDVIRVFwDates_3840x2160_1263_print.jpg (1024x576) [86.2 KB] || SAfrica_NDVIRVFwDates_3840x2160_1263_searchweb.png (320x180) [56.0 KB] || SAfrica_NDVIRVFwDates_3840x2160_1263_thm.png (80x40) [4.5 KB] || SAfrica_NDVIRVFComposite_1080p30.mp4 (1920x1080) [31.6 MB] || SAfrica_NDVIRVFComposite_1080p30.webm (1920x1080) [7.0 MB] || Composite (3840x2160) [0 Item(s)] || SAfrica_NDVIRVFwDates_3840x2160_1263.tif (3840x2160) [7.6 MB] || SAfrica_NDVIRVFComposite_3840x2160_p30.mp4 (3840x2160) [96.4 MB] || ",
            "hits": 35
        },
        {
            "id": 4784,
            "url": "https://svs.gsfc.nasa.gov/4784/",
            "result_type": "Visualization",
            "release_date": "2020-02-21T00:00:00-05:00",
            "title": "ENSO Teleconnections and Rift Valley fever (RVF) Outbreaks",
            "description": "During the 2008-2011 period, ENSO events brought changes to weather conditions across the globe that triggered infectious disease outbreaks, such as mosquito-borne Rift Valley fever (RVF) in South Africa. This visualization with corresponding data dashboard shows how Sea Surface Temperature (SST) anomalies in the equatorial Pacific Ocean (left) gave rise to Precipitation (center) and Vegetation (right) Index Anomalies in South Africa. During La Niña events, Southern Africa receives persistent and above normal rainfall, which floods habitats of RVF mosquito vectors triggering hatching of RVF virus infected eggs. The above-normal rainfall is followed by an increase in vegetation creating appropriate habitats for the mosquito vectors setting the stage for RVF outbreak activity, which in simple terms means an uptick in mosquito populations that cause infections of domestic livestock and human populations with the RVF virus. However, in rare cases there is a departure from this canonical response, as we can observe in 2009-2010, when a mild El Niño event resulted in above normal vegetaton and a large RVF outbreak in  South Africa. || ENSO_TeleconnectionsRVF_2008_2011_3840x2160_2960_print.jpg (1024x576) [107.8 KB] || ENSO_TeleconnectionsRVF_2008_2011_3840x2160_3525_searchweb.png (320x180) [63.0 KB] || ENSO_TeleconnectionsRVF_2008_2011_3840x2160_3525_thm.png (80x40) [6.5 KB] || ENSO_Teleconnections (1920x1080) [0 Item(s)] || SST_Precip_NDVI_Dashboard_2008_2011_1920x1080_p30.mp4 (1920x1080) [22.7 MB] || ENSO_Teleconnections (3840x2160) [0 Item(s)] || ENSO_Teleconnections (3840x2160) [0 Item(s)] || ENSO_TeleconnectionsRVF_2008_2011_3840x2160_p30.mp4 (3840x2160) [56.0 MB] || ENSO_TeleconnectionsRVF_2008_2011_3840x2160_p30.webm (3840x2160) [10.2 MB] || ENSO_TeleconnectionsRVF_2008_2011_3840x2160_2960.tif (3840x2160) [3.4 MB] || ENSO_TeleconnectionsRVF_2008_2011_3840x2160_3525.tif (3840x2160) [3.4 MB] || ",
            "hits": 32
        },
        {
            "id": 40411,
            "url": "https://svs.gsfc.nasa.gov/gallery/podaacanimation/",
            "result_type": "Gallery",
            "release_date": "2020-02-14T00:00:00-05:00",
            "title": "PODAAC animation",
            "description": "Animations created by the Physical Oceanography DAAC.",
            "hits": 2
        },
        {
            "id": 4654,
            "url": "https://svs.gsfc.nasa.gov/4654/",
            "result_type": "Visualization",
            "release_date": "2018-12-14T12:00:00-05:00",
            "title": "Evolution of the Meteorological Observing System in the MERRA-2 Reanalysis",
            "description": "Meteorological Observing Systems, 1980 and 2018. Data is revealed within a moving 1.5 hour window centered on the time shown. || gmao_HW.00300_print.jpg (1024x345) [102.7 KB] || gmao_HW.00300_searchweb.png (320x180) [93.0 KB] || gmao_HW.00300_thm.png (80x40) [6.4 KB] || gmao_HW_1920_648p30.webm (1920x648) [11.9 MB] || gmao_HW_1920_648p30.mp4 (1920x648) [134.3 MB] || 9600x3240_80x27_30p (9600x3240) [0 Item(s)] || ",
            "hits": 75
        },
        {
            "id": 30942,
            "url": "https://svs.gsfc.nasa.gov/30942/",
            "result_type": "Hyperwall Visual",
            "release_date": "2018-05-03T00:00:00-04:00",
            "title": "The first Ice, Cloud, and land Elevation Satellite (ICESat)",
            "description": "ICESat launch animation and sensor operation || VTS_01_1_trim_00561.jpg (1280x720) [131.3 KB] || VTS_01_1_trim_720p.mp4 (1280x720) [61.6 MB] || VTS_01_1_trim.webm (720x480) [29.8 MB] || ",
            "hits": 89
        },
        {
            "id": 4600,
            "url": "https://svs.gsfc.nasa.gov/4600/",
            "result_type": "Visualization",
            "release_date": "2018-01-31T00:00:00-05:00",
            "title": "Sixty Years of Earth Observations: from Explorer-1 (1958) to CYGNSS (2017)",
            "description": "Earth observing spacecraft from Explorer-1 to CYGNSSThis video is also available on our YouTube channel. || explorer1_68_1920x1080.09999_print.jpg (1024x576) [149.7 KB] || explorer1_68_1920x1080.09999_searchweb.png (320x180) [76.7 KB] || explorer1_68_1920x1080.09999_thm.png (80x40) [5.8 KB] || explorer1_68_1920x1080_p60.mp4 (1920x1080) [73.6 MB] || firsts (1920x1080) [0 Item(s)] || explorer1_68_1920x1080_p30.webm (1920x1080) [35.9 MB] || explorer1_68_1920x1080_p30.mp4 (1920x1080) [124.5 MB] || explorer1_68_1920x1080.1080p30.mp4 (1920x1080) [128.5 MB] || 9600x3240_16x9_30p (9600x3240) [0 Item(s)] || 3840x2160_16x9_60p (3840x2160) [0 Item(s)] || explorer1_68_3840x2160_p30.mp4 (3840x2160) [461.5 MB] || ",
            "hits": 135
        },
        {
            "id": 12704,
            "url": "https://svs.gsfc.nasa.gov/12704/",
            "result_type": "Produced Video",
            "release_date": "2017-08-31T12:00:00-04:00",
            "title": "NASA Eclipse Imagery",
            "description": "As millions of people across the United States experienced a total eclipse as the umbra, or Moon’s shadow passed over them, only six people witnessed the umbra from space. Viewing the eclipse from orbit were NASA’s Randy Bresnik, Jack Fischer and Peggy Whitson, ESA (European Space Agency’s) Paolo Nespoli, and Roscosmos’ Commander Fyodor Yurchikhin and Sergey Ryazanskiy. The space station crossed the path of the eclipse three times as it orbited above the continental United States at an altitude of 250 miles. Credit: NASA || iss052e056122.jpg (4928x3280) [844.0 KB] || ",
            "hits": 497
        },
        {
            "id": 30893,
            "url": "https://svs.gsfc.nasa.gov/30893/",
            "result_type": "Hyperwall Visual",
            "release_date": "2017-08-31T00:00:00-04:00",
            "title": "2017 Eclipse Image Collection",
            "description": "This image is a composite photograph that shows the progression of the total solar eclipse over Madras, Oregon.http://earthobservatory.nasa.gov/NaturalHazards/view.php?id=90796 || eclipsecomposite_pho_lrg.jpg (2231x1487) [541.4 KB] || eclipsecomposite_pho_lrg_searchweb.png (320x180) [47.2 KB] || eclipsecomposite_pho_lrg_thm.png (80x40) [3.3 KB] || 2017-eclipse-images-7.hwshow [293 bytes] || ",
            "hits": 211
        },
        {
            "id": 12698,
            "url": "https://svs.gsfc.nasa.gov/12698/",
            "result_type": "Produced Video",
            "release_date": "2017-08-30T10:00:00-04:00",
            "title": "What Spacecraft Saw During the 2017 Solar Eclipse",
            "description": "On Aug. 21, 2017, a solar eclipse passed over North America. People throughout the continent experienced a partial solar eclipse, and a total solar eclipse passed over a narrow swath of land stretching from Oregon to South Carolina, called the path of totality. NASA and its partner’s satellites had a unique vantage point to watch the eclipse. Several Sun-watching satellites were in a position to see the Moon cross in front of the Sun, while many Earth-observing satellites – and NASA’s Lunar Reconnaissance Orbiter, which typically images the Moon’s landscape – captured images of the Moon’s shadow on Earth’s surface. See more and download content at https://go.nasa.gov/2x7b8kf || ",
            "hits": 59
        },
        {
            "id": 11668,
            "url": "https://svs.gsfc.nasa.gov/11668/",
            "result_type": "Produced Video",
            "release_date": "2014-10-23T07:00:00-04:00",
            "title": "Vital Signs: Taking the Pulse of Our Planet",
            "description": "Our planet is a beautiful and awesome place. In a new video, join NASA scientists on a 40-minute visual tour of Earth from space, presented at the IMAX Theater at National Air and Space Museum in Washington, D.C. on September 10. “Vital Signs: Taking the Pulse of Our Planet\" was the theme for NASA’s Goddard Space Flight Center's fifteenth installment of its annual lecture and reception sponsored by the Maryland Space Business Roundtable. Earth is a complex, dynamic system we do not yet fully understand. Like the human body, the Earth system comprises diverse components that interact in complex ways.On this global tour, scientists lead the viewer through Earth’s water cycle, forests and frozen regions as seen through the eyes of NASA’s Earth observing satellite fleet. They share a story of how we can make life better today and into the future.NASA's Earth science program aims to develop a greater understanding of Earth's system and its response to natural or human-induced changes, and to improve predictions of climate, weather and natural disasters. || ",
            "hits": 32
        },
        {
            "id": 4205,
            "url": "https://svs.gsfc.nasa.gov/4205/",
            "result_type": "Visualization",
            "release_date": "2014-09-24T09:00:00-04:00",
            "title": "Earth Science Heads-up Display",
            "description": "On September 10, 2014, NASA's Earth Observing System (EOS) was celebrated in an evening event at the Smithsonian National Air and Space Museum in Washington DC.  The title of this event was \"Vital Signs: Taking the Pulse of Our Planet\", and the speakers at this event included several Earth Scientists from Goddard Space Flight Center.  This animation was used in the beginning of the event to illustrate the interconnectedness of the many Earth-based data sets that NASA has produced over the last decade or so.  The animation simulates a view of the Earth from the International Space Station, over which interconnected data sets are displayed as if on a head-up display. || ",
            "hits": 38
        },
        {
            "id": 30486,
            "url": "https://svs.gsfc.nasa.gov/30486/",
            "result_type": "Hyperwall Visual",
            "release_date": "2014-02-28T00:00:00-05:00",
            "title": "Sea Surface Temperature in the Eastern Pacific",
            "description": "This animation from Jan 2011 to Dec 2013 shows high resolution sea surface temperature (SST) in the Eastern Pacific off Central America. Clearly visible off the Central American Coast are the cooling events associated with the winds that blow through the mountain gaps in Central America. The cooling events can form cold eddies and domes, such as off the coast of Costa Rica. The MUR SST dataset combines data from the Advanced Very High Resolution Radiometer (AVHRR), Moderate Resolution Imaging Spectroradiometer (MODIS), and Advanced Microwave Scanning Radiometer for EOS (AMSR-E) instruments, and currently the NAVY Windsat Satellite. More details of the MUR data set may be found at PO.DAAC. || ",
            "hits": 35
        },
        {
            "id": 30487,
            "url": "https://svs.gsfc.nasa.gov/30487/",
            "result_type": "Hyperwall Visual",
            "release_date": "2014-02-28T00:00:00-05:00",
            "title": "Sea Surface Temperature and the Agulhas Current",
            "description": "This animation from Jan 2011 to Dec 2013 shows high resolution sea surface temperature (SST) in the Agulhas Retroflection off South Africa. Clearly visible in the Agulhas animation are the eddies that form as a result of the retroflection of the current. These eddies can shed or spin off the main current and travel into the South Atlantic. The MUR SST dataset combines data from the Advanced Very High Resolution Radiometer (AVHRR), Moderate Resolution Imaging Spectroradiometer (MODIS), and Advanced Microwave Scanning Radiometer for EOS (AMSR-E) instruments, and currently the NAVY Windsat Satellite. More details of the MUR data set may be found at PO.DAAC || ",
            "hits": 21
        },
        {
            "id": 3925,
            "url": "https://svs.gsfc.nasa.gov/3925/",
            "result_type": "Visualization",
            "release_date": "2012-07-22T00:00:00-04:00",
            "title": "NPP Ceres Shortwave Radiation",
            "description": "The CERES experiment is one of the highest priority scientific satellite instruments developed for NASA's Earth Observing System (EOS). The doors are open on NASA's Suomi NPP satellite and the newest version of the Clouds and the Earth's Radiant Energy System (CERES) instrument is scanning Earth for the first time, helping to assure continued availability of measurements of the energy leaving the Earth-atmosphere system.CERES products include both solar-reflected and Earth-emitted radiation from the top of the atmosphere to the Earth's surface. Cloud properties are determined using simultaneous measurements by other EOS and NPP instruments such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Visible and Infrared Sounder (VIRS). Analyses using CERES data, build upon the foundation laid by previous missions such as NASA Earth Radiation Budget Experiment (ERBE), leading to a better understanding of the role of clouds and the energy cycle in global climate change. The sun's radiant energy is the fuel that drives Earth's climate engine. The Earth-atmosphere system constantly tries to maintain a balance between the energy that reaches the Earth from the sun and the energy that flows from Earth back out to space. Energy received from the sun is mostly in the visible (or shortwave) part of the electromagnetic spectrum. About 30% of the solar energy that comes to Earth is reflected back to space. The ratio of reflected-to-incoming energy is called \"albedo\" from the Latin word meaning whiteness. The solar radiation absorbed by the Earth causes the planet to heat up until it is radiating (or emitting) as much energy back into space as it absorbs from the sun. The Earth's thermal emitted radiation is mostly in the infrared (or longwave part of the spectrum. The balance between incoming and outgoing energy is called the Earth's radiation budget. This global view shows CERES top-of-atmosphere (TOA) shortwave radiation from Jan 26 and 27, 2012. Thick cloud cover tends to reflect a large amount of incoming solar energy back to space (blue/green/white image). For more information on the Clouds and Earth's Radiant Energy System (CERES) see http://ceres.larc.nasa.gov || ",
            "hits": 73
        },
        {
            "id": 3926,
            "url": "https://svs.gsfc.nasa.gov/3926/",
            "result_type": "Visualization",
            "release_date": "2012-07-22T00:00:00-04:00",
            "title": "NPP Ceres Longwave Radiation",
            "description": "The CERES experiment is one of the highest priority scientific satellite instruments developed for NASA's Earth Observing System (EOS). The doors are open on NASA's Suomi NPP satellite and the newest version of the Clouds and the Earth's Radiant Energy System (CERES) instrument is scanning Earth for the first time, helping to assure continued availability of measurements of the energy leaving the Earth-atmosphere system.CERES products include both solar-reflected and Earth-emitted radiation from the top of the atmosphere to the Earth's surface. Cloud properties are determined using simultaneous measurements by other EOS and NPP instruments such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Visible and Infrared Sounder (VIRS). Analyses using CERES data, build upon the foundation laid by previous missions such as NASA Earth Radiation Budget Experiment (ERBE), leading to a better understanding of the role of clouds and the energy cycle in global climate change.The sun's radiant energy is the fuel that drives Earth's climate engine. The Earth-atmosphere system constantly tries to maintain a balance between the energy that reaches the Earth from the sun and the energy that flows from Earth back out to space. Energy received from the sun is mostly in the visible (or shortwave) part of the electromagnetic spectrum. About 30% of the solar energy that comes to Earth is reflected back to space. The ratio of reflected-to-incoming energy is called \"albedo\" from the Latin word meaning whiteness. The solar radiation absorbed by the Earth causes the planet to heat up until it is radiating (or emitting) as much energy back into space as it absorbs from the sun. The Earth's thermal emitted radiation is mostly in the infrared (or longwave part of the spectrum. The balance between incoming and outgoing energy is called the Earth's radiation budget.This global view shows CERES top-of-atmosphere (TOA) longwave radiation from Jan 26 and 27, 2012. Heat energy radiated from Earth (in watts per square meter) is shown in shades of yellow, red, blue and white. The brightest-yellow areas are the hottest and are emitting the most energy out to space, while the dark blue areas and the bright white clouds are much colder, emitting the least energy. Increasing temperature, decreasing water vapor, and decreasing clouds will all tend to increase the ability of Earth to shed heat out to space.For more information on the Clouds and Earth's Radiant Energy System (CERES) see  http://ceres.larc.nasa.gov || ",
            "hits": 79
        },
        {
            "id": 10893,
            "url": "https://svs.gsfc.nasa.gov/10893/",
            "result_type": "Produced Video",
            "release_date": "2012-01-12T11:00:00-05:00",
            "title": "Aqua Podcast Series",
            "description": "This page will soon feature six videos about the Aqua satellite mission, starting with an introductory video, followed by weekly additions of videos highlighting the AIRS, AMSR-E, MODIS, and CERES instruments, and concluding with a video featuring applications of Aqua data. || ",
            "hits": 15
        },
        {
            "id": 10742,
            "url": "https://svs.gsfc.nasa.gov/10742/",
            "result_type": "Produced Video",
            "release_date": "2011-08-25T12:00:00-04:00",
            "title": "NPP Resource Reel",
            "description": "The NPOESS Preparatory Project (NPP) represents a critical first step in building the next-generation weather satellite system. Goddard Space Flight Center is leading NASA's effort to launch a satellite that will carry the first of the new sensors developed for this next-generation system, previously called the National Polar-orbiting Operational Environmental Satellite System (NPOESS) and now the Joint Polar Satellite System (JPSS). || ",
            "hits": 39
        },
        {
            "id": 3719,
            "url": "https://svs.gsfc.nasa.gov/3719/",
            "result_type": "Visualization",
            "release_date": "2010-06-24T00:00:00-04:00",
            "title": "MERRA Specific Humidity",
            "description": "Retrospective-analyses (or reanalyses) have been a critical tool in studying weather and climate variability for the last 15 years. Reanalyses blend the continuity and breadth of output data of a numerical model with the constraint of vast quantities of observational data. The result is a long-term continuous data record. The Modern Era Retrospective-analysis for Research and Applications was developed to support NASA's Earth science objectives, by applying the state-of-the-art GMAO data assimilation system that includes many modern observing systems (such as EOS) in a climate framework.The MERRA time period covers the modern era of remotely sensed data, from 1979 through the present, and the special focus of the atmospheric assimilation is the hydrological cycle.The time period covered by the visualization is the months of May, June, and July of 1988 and 1993, two years with contrasting extreme weather events during the summer: a drought through the midwestern states of the US in 1988, and heavy rains and flooding through the same region in 1993.This visualization shows the specific humidity dataset produced by MERRA, up to a geopotential height of 20 km. The height coordinate is greatly exaggerated. Both opacity and color are driven by the data value.This animation was created as part of a presentation for the Nasa Center for Climate Simulation (NCCS) hyperwall display. This is a set of tiled high definition displays consisting of 5 displays across by 3 displays down. The full resolution of all combined displays is 6840 pixels accross by 2304 pixels down. For the full presentation, see the link below. || ",
            "hits": 9
        },
        {
            "id": 3732,
            "url": "https://svs.gsfc.nasa.gov/3732/",
            "result_type": "Visualization",
            "release_date": "2010-06-24T00:00:00-04:00",
            "title": "MERRA Relative Humidity",
            "description": "Retrospective-analyses (or reanalyses) have been a critical tool in studying weather and climate variability for the last 15 years. Reanalyses blend the continuity and breadth of output data of a numerical model with the constraint of vast quantities of observational data. The result is a long-term continuous data record. The Modern Era Retrospective-analysis for Research and Applications was developed to support NASA's Earth science objectives, by applying the state-of-the-art GMAO data assimilation system that includes many modern observing systems (such as EOS) in a climate framework.The MERRA time period covers the modern era of remotely sensed data, from 1979 through the present, and the special focus of the atmospheric assimilation is the hydrological cycle.The time period covered by the visualization is the months of May, June, and July of 1988 and 1993, two years with contrasting extreme weather events during the summer: a drought through the midwestern states of the US in 1988, and heavy rains and flooding through the same region in 1993.This visualization shows the relative humidity dataset produced by MERRA, up to a geopotential height of 20 km. The height coordinate is greatly exaggerated. Both opacity and color are driven by the data value.This animation was created as part of a presentation for the Nasa Center for Climate Simulation (NCCS) hyperwall display. This is a set of tiled high definition displays consisting of 5 displays across by 3 displays down. The full resolution of all combined displays is 6840 pixels accross by 2304 pixels down. For the full presentation, see the link below. || ",
            "hits": 35
        },
        {
            "id": 3733,
            "url": "https://svs.gsfc.nasa.gov/3733/",
            "result_type": "Visualization",
            "release_date": "2010-06-24T00:00:00-04:00",
            "title": "MERRA Wind",
            "description": "Retrospective-analyses (or reanalyses) have been a critical tool in studying weather and climate variability for the last 15 years. Reanalyses blend the continuity and breadth of output data of a numerical model with the constraint of vast quantities of observational data. The result is a long-term continuous data record. The Modern Era Retrospective-analysis for Research and Applications was developed to support NASA's Earth science objectives, by applying the state-of-the-art GMAO data assimilation system that includes many modern observing systems (such as EOS) in a climate framework.The MERRA time period covers the modern era of remotely sensed data, from 1979 through the present, and the special focus of the atmospheric assimilation is the hydrological cycle.The time period covered by the visualization is the months of May, June, and July of 1988 and 1993, two years with contrasting extreme weather events during the summer: a drought through the midwestern states of the US in 1988, and heavy rains and flooding through the same region in 1993.This visualization shows the combined U and V components of wind at three different pressure levels: 850 mb, 500 mb, and 300 mb. The pressure coordinate is greatly exaggerated.This animation was created as part of a presentation for the Nasa Center for Climate Simulation (NCCS) hyperwall display. This is a set of tiled high definition displays consisting of 5 displays across by 3 displays down. The full resolution of all combined displays is 6840 pixels accross by 2304 pixels down. For the full presentation, see the link below. || ",
            "hits": 43
        },
        {
            "id": 3734,
            "url": "https://svs.gsfc.nasa.gov/3734/",
            "result_type": "Visualization",
            "release_date": "2010-06-24T00:00:00-04:00",
            "title": "MERRA Combined Liquid Water and Ice Mixing Ratios",
            "description": "Retrospective-analyses (or reanalyses) have been a critical tool in studying weather and climate variability for the last 15 years. Reanalyses blend the continuity and breadth of output data of a numerical model with the constraint of vast quantities of observational data. The result is a long-term continuous data record. The Modern Era Retrospective-analysis for Research and Applications was developed to support NASA's Earth science objectives, by applying the state-of-the-art GMAO data assimilation system that includes many modern observing systems (such as EOS) in a climate framework.The MERRA time period covers the modern era of remotely sensed data, from 1979 through the present, and the special focus of the atmospheric assimilation is the hydrological cycle.The time period covered by the visualization is the months of May, June, and July of 1988 and 1993, two years with contrasting extreme weather events during the summer: a drought through the midwestern states of the US in 1988, and heavy rains and flooding through the same region in 1993.This visualization shows the combined liquid water and ice mixing ratio dataset produced by MERRA, roughly corresponding to cloud cover, up to an geopotential height of 20 km. The height coordinate is greatly exaggerated. Both opacity and color are driven by the data value.This animation was created as part of a presentation for the NASA Center for Climate Simulation (NCCS) hyperwall display. This is a set of tiled high definition displays consisting of 5 displays across by 3 displays down. The full resolution of all combined displays is 6840 pixels accross by 2304 pixels down. For the full presentation, see the link below. || ",
            "hits": 16
        },
        {
            "id": 3735,
            "url": "https://svs.gsfc.nasa.gov/3735/",
            "result_type": "Visualization",
            "release_date": "2010-06-24T00:00:00-04:00",
            "title": "MERRA Rate of Total Precipitation, 1988, 1993",
            "description": "Retrospective-analyses (or reanalyses) have been a critical tool in studying weather and climate variability for the last 15 years. Reanalyses blend the continuity and breadth of output data of a numerical model with the constraint of vast quantities of observational data. The result is a long-term continuous data record. The Modern Era Retrospective-analysis for Research and Applications was developed to support NASA's Earth science objectives, by applying the state-of-the-art GMAO data assimilation system that includes many modern observing systems (such as EOS) in a climate framework.The MERRA time period covers the modern era of remotely sensed data, from 1979 through the present, and the special focus of the atmospheric assimilation is the hydrological cycle.The time period covered by the visualization is the months of May, June, and July of 1988 and 1993, two years with contrasting extreme weather events during the summer: a drought through the midwestern states of the US in 1988, and heavy rains and flooding through the same region in 1993.This visualization shows the total precipitation rate dataset produced by MERRA.This animation was created as part of a presentation for the NASA Center for Climate Simulation (NCCS) hyperwall display. This is a set of tiled high definition displays consisting of 5 displays across by 3 displays down. The full resolution of all combined displays is 6840 pixels accross by 2304 pixels down. For the full presentation, see the link below. || ",
            "hits": 10
        },
        {
            "id": 3710,
            "url": "https://svs.gsfc.nasa.gov/3710/",
            "result_type": "Visualization",
            "release_date": "2010-05-01T00:00:00-04:00",
            "title": "Five Spheres - Cryosphere",
            "description": "Sea ice is frozen seawater floating on the surface of the ocean. Some sea ice is semi-permanent, persisting from year to year, and some is seasonal, melting and refreezing from season to season. The sea ice cover reaches its minimum extent at the end of each summer and the remaining ice is called the perennial ice cover. The Advanced Microwave Scanning Radiometer - Earth Observing System (AMSR-E) instrument on the NASA Earth Observing System (EOS) Aqua satellite, provides data mapped to a polar stereographic grid at 12.5 km spatial resolution. This satellite data can be used to monitor the health of the cryosphere from space. This animation of sea ice changes in the Arctic is match framed to animation entries 3707, 3708, 3709, and 3711. Over the water, Arctic sea ice changes from day to day showing a running 3-day maximum sea ice concentration in the region where the concentration is greater than 15%. The blueish white color of the sea ice is derived from a 3-day running maximum of the AMSR-E 89 GHz brightness temperature. Over the terrain, monthly data from the seasonal Blue Marble Next Generation fades slowly from month to month.For more information about sea ice see http://nsidc.org/data/amsre or http://modis-snow-ice.gsfc.nasa.gov. || ",
            "hits": 36
        },
        {
            "id": 40068,
            "url": "https://svs.gsfc.nasa.gov/gallery/project-videos/",
            "result_type": "Gallery",
            "release_date": "2010-03-08T00:00:00-05:00",
            "title": "Project Videos",
            "description": "No description available.",
            "hits": 88
        },
        {
            "id": 3619,
            "url": "https://svs.gsfc.nasa.gov/3619/",
            "result_type": "Visualization",
            "release_date": "2009-09-01T18:00:00-04:00",
            "title": "A Tour of the Cryosphere 2009",
            "description": "The cryosphere consists of those parts of the Earth's surface where water is found in solid form, including areas of snow, sea ice, glaciers, permafrost, ice sheets, and icebergs. In these regions, surface temperatures remain below freezing for a portion of each year. Since ice and snow exist relatively close to their melting point, they frequently change from solid to liquid and back again due to fluctuations in surface temperature. Although direct measurements of the cryosphere can be difficult to obtain due to the remote locations of many of these areas, using satellite observations scientists monitor changes in the global and regional climate by observing how regions of the Earth's cryosphere shrink and expand.This animation portrays fluctuations in the cryosphere through observations collected from a variety of satellite-based sensors. The animation begins in Antarctica, showing some unique features of the Antarctic landscape found nowhere else on earth. Ice shelves, ice streams, glaciers, and the formation of massive icebergs can be seen clearly in the flyover of the Landsat Image Mosaic of Antarctica. A time series shows the movement of iceberg B15A, an iceberg 295 kilometers in length which broke off of the Ross Ice Shelf in 2000. Moving farther along the coastline, a time series of the Larsen ice shelf shows the collapse of over 3,200 square kilometers ice since January 2002. As we depart from the Antarctic, we see the seasonal change of sea ice and how it nearly doubles the apparent area of the continent during the winter.From Antarctica, the animation travels over South America showing glacier locations on this mostly tropical continent. We then move further north to observe daily changes in snow cover over the North American continent. The clouds show winter storms moving across the United States and Canada, leaving trails of snow cover behind. In a close-up view of the western US, we compare the difference in land cover between two years: 2003 when the region received a normal amount of snow and 2002 when little snow was accumulated. The difference in the surrounding vegetation due to the lack of spring melt water from the mountain snow pack is evident.As the animation moves from the western US to the Arctic region, the areas affected by permafrost are visible. As time marches forward from March to September, the daily snow and sea ice recede and reveal the vast areas of permafrost surrounding the Arctic Ocean.The animation shows a one-year cycle of Arctic sea ice followed by the mean September minimum sea ice for each year from 1979 through 2008. The superimposed graph of the area of Arctic sea ice at this minimum clearly shows the dramatic decrease in Artic sea ice over the last few years.While moving from the Arctic to Greenland, the animation shows the constant motion of the Arctic polar ice using daily measures of sea ice activity. Sea ice flows from the Arctic into Baffin Bay as the seasonal ice expands southward. As we draw close to the Greenland coast, the animation shows the recent changes in the Jakobshavn glacier. Although Jakobshavn receded only slightly from 1964 to 2001, the animation shows significant recession from 2001 through 2009. As the animation pulls out from Jakobshavn, the effect of the increased flow rate of Greenland costal glaciers is shown by the thinning ice shelf regions near the Greenland coast.This animation shows a wealth of data collected from satellite observations of the cryosphere and the impact that recent cryospheric changes are making on our planet.For more information on the data sets used in this visualization, visit NASA's EOS DAAC website.Note: This animation is an update of the animation 'A Short Tour of the Cryosphere', which is itself an abridged version of the animation 'A Tour of the Cryosphere'. The popularity of the earlier animations and their continuing relevance prompted us to update the datasets in parts of the animation and to remake it in high definition. In certain cases, our experiences in using the earlier work have led us to tweak the presentation of some of the material to make it clearer. Our thanks to Dr. Robert Bindschadler for suggesting and supporting this remake. || ",
            "hits": 45
        },
        {
            "id": 3355,
            "url": "https://svs.gsfc.nasa.gov/3355/",
            "result_type": "Visualization",
            "release_date": "2006-05-20T23:55:00-04:00",
            "title": "A Short Tour of the Cryosphere",
            "description": "A newer version of this animation is available here.This narrated, 5-minute animation shows a wealth of data collected from satellite observations of the cryosphere and the impact that recent cryospheric changes are making on our planet. This is a shorter version of a narrated, 7 1/2 minute animation entitled  'A Tour of the Cryosphere'.See the above link for a detailed description of the full animation.Two sections have been removed from the original animation: one showing a flyby of the South Pole station and glaciers feeding the Ross Ice Shelf and one showing solar data related to the Earth's energy balance.For more information on the data sets used in this visualization, visit NASA's EOS DAAC website. || ",
            "hits": 25
        },
        {
            "id": 3181,
            "url": "https://svs.gsfc.nasa.gov/3181/",
            "result_type": "Visualization",
            "release_date": "2005-12-04T23:55:00-05:00",
            "title": "A Tour of the Cryosphere",
            "description": "A new HD version of this animation is available here.Click here to go to the media download section.The cryosphere consists of those parts of the Earth's surface where water is found in solid form, including areas of snow, sea ice, glaciers, permafrost, ice sheets, and icebergs. In these regions, surface temperatures remain below freezing for a portion of each year. Since ice and snow exist relatively close to their melting point, they frequently change from solid to liquid and back again due to fluctuations in surface temperature. Although direct measurements of the cryosphere can be difficult to obtain due to the remote locations of many of these areas, using satellite observations scientists monitor changes in the global and regional climate by observing how regions of the Earth's cryosphere shrink and expand.This animation portrays fluctuations in the cryosphere through observations collected from a variety of satellite-based sensors. The animation begins in Antarctica, showing ice thickness ranging from 2.7 to 4.8 kilometers thick along with swaths of polar stratospheric clouds. In a tour of this frozen continent, the animation shows some unique features of the Antarctic landscape found nowhere else on earth. Ice shelves, ice streams, glaciers, and the formation of massive icebergs can be seen. A time series shows the movement of iceberg B15A, an iceberg 295 kilometers in length which broke off of the Ross Ice Shelf in 2000. Moving farther along the coastline, a time series of the Larsen ice shelf shows the collapse of over 3,200 square kilometers ice since January 2002. As we depart from the Antarctic, we see the seasonal change of sea ice and how it nearly doubles the size of the continent during the winter.From Antarctica, the animation travels over South America showing areas of permafrost over this mostly tropical continent. We then move further north to observe daily changes in snow cover over the North American continent. The clouds show winter storms moving across the United States and Canada, leaving trails of snow cover behind. In a close-up view of the western US, we compare the difference in land cover between two years: 2003 when the region received a normal amount of snow and 2002 when little snow was accumulated. The difference in the surrounding vegetation due to the lack of spring melt water from the mountain snow pack is evident.As the animation moves from the western US to the Arctic region, the areas effected by permafrost are visible. In December, we see how the incoming solar radiation primarily heats the Southern Hemisphere. As time marches forward from December to June, the daily snow and sea ice recede as the incoming solar radiation moves northward to warm the Northern Hemisphere.Using satellite swaths that wrap the globe, the animation shows three types of instantaneous measurements of solar radiation observed on June 20, 2003: shortwave (reflected) radiation, longwave (thermal) radiation and net flux (showing areas of heating and cooling). Correlation between reflected radiation and clouds are evident. When the animation fades to show the monthly global average net flux, we see that the polar regions serve to cool the global climate by radiating solar energy back into space throughout the year.The animation shows a one-year cycle of the monthly average Arctic sea ice concentration followed by the mean September minimum sea ice for each year from 1979 through 2004. A red outline indicates the mean sea ice extent for September over 22 years, from 1979 to 2002. The minimum Arctic sea ice animation clearly shows how over the last 5 years the quantity of polar ice has decreased by 10 - 14% from the 22 year average.While moving from the Arctic to Greenland, the animation shows the constant motion of the Arctic polar ice using daily measures of sea ice activity. Sea ice flows from the Arctic into Baffin Bay as the seasonal ice expands southward. As we draw close to the Greenland coast, the animation shows the recent changes in the Jakobshavn glacier. Although Jakobshavn receded only slightly from 1042 to 2001, the animation shows significant recession over the past three years, from 2002 through 2004.This animation shows a wealth of data collected from satellite observations of the cryosphere and the impact that recent cryospheric changes are making on our planet.For more information on the data sets used in this visualization, visit NASA's EOS DAAC website. || ",
            "hits": 104
        },
        {
            "id": 3180,
            "url": "https://svs.gsfc.nasa.gov/3180/",
            "result_type": "Visualization",
            "release_date": "2005-07-31T00:00:00-04:00",
            "title": "MODIS Daily Global Snow Cover and Sea Ice Surface Temperature as seen in the SIGGRAPH 2005 Electronic Theater",
            "description": "This animation showing snow cover and sea ice surface temperature in the Northern Hemisphere portrays data collected from daily MODIS satellite images acquired during the winter of 2002-2003. Darkness increases with the onset of autumn, reaching a maximum at the Winter Solstice on December 21st. Thereafter, the circle of darkness shrinks as the period of daylight increases. Daily changes in sea ice are shown as ice surface temperature, which is related to the air temperature and the concentration of the sea ice. Sea ice surface temperatures range from about -40 to -2 degrees Celsius. Here, ice surface temperatures are depicted by colors, described by a color bar shown below. The snow tracks of several winter storms across the United States can be clearly seen. With an albedo of up to 80 percent or more, snow-covered terrain reflects most of the incoming solar radiation back into space, cooling the lower atmosphere. When snow cover melts, the albedo drops suddenly to less than about 30 percent, allowing the ground to absorb more solar radiation, heating the Earth's surface and lower atmosphere. Rapid changes in albedo, resultingfrom snowfall and snow melt, cause significant changes in the regional energy balance. This animation was accepted into the prestigious 2005 SIGGRAPH Electronic Theater, where it was shown during the annual conference from July 31 through August 4, 2005 in Los Angeles, CA. For more information on the data sets used in this visualization, visit NASA's EOS DAAC website. || ",
            "hits": 21
        },
        {
            "id": 3062,
            "url": "https://svs.gsfc.nasa.gov/3062/",
            "result_type": "Visualization",
            "release_date": "2004-12-14T12:00:00-05:00",
            "title": "The Microwave Limb Sounder Observes the Lower Stratosphere and Upper Troposphere",
            "description": "MLS measures lower stratospheric temperature and concentrations of H2O, O3, ClO, BrO, HCl, OH, HO2, HNO3, HCN, and N2O, for their effects on (and diagnoses of) ozone depletion, transformations of greenhouse gases, and radiative forcing of climate change. || ",
            "hits": 16
        },
        {
            "id": 2900,
            "url": "https://svs.gsfc.nasa.gov/2900/",
            "result_type": "Visualization",
            "release_date": "2004-02-12T12:00:00-05:00",
            "title": "Global Atmospheric Carbon Monoxide in 2000 (WMS)",
            "description": "This visualization shows global carbon monoxide concentrations at the 500 millibar altitude in the atmosphere from March 1, 2000 through December 31, 2000. Areas in red have 200 parts per billion of carbon monoxide or more at that altitude (around 5,500 meters), while areas in blue are 50 parts per billion or less. Carbon monoxide is an atmospheric pollutant and the highest concentrations come from grassland and forest fires in Africa and South America, although there is evidence that industrial sources may also be a factor. Atmospheric circulation rapidly moves the carbon monoxide to other parts of the world once it has reached this altitude. This data was measured by the MOPITT instrument on the Terra satellite. || ",
            "hits": 25
        },
        {
            "id": 2436,
            "url": "https://svs.gsfc.nasa.gov/2436/",
            "result_type": "Visualization",
            "release_date": "2002-04-30T12:00:00-04:00",
            "title": "Great Zoom out of Mongu, Africa (EOS Land Validation Site)",
            "description": "Using data from different spacecraft and some powerful computer technology, visualizers at the Goddard Space Flight Center present you with a collection of American cities in a way you have never seen them before. Starting with our camera high above the Earth, we rush in towards the surface at what would be an impossible speed for any known vehicle. Passing though layers of atmosphere, the colors of our destinations shimmer with their own unique  characteristics, and suddenly we find ourselves floating in virtual space just above the ground. || ",
            "hits": 7
        },
        {
            "id": 2437,
            "url": "https://svs.gsfc.nasa.gov/2437/",
            "result_type": "Visualization",
            "release_date": "2002-04-30T12:00:00-04:00",
            "title": "Great Zoom into Mongu, Africa (EOS Land Validation Site)",
            "description": "Using data from different spacecraft and some powerful computer technology, visualizers at the Goddard Space Flight Center present you with a collection of American cities in a way you have never seen them before. Starting with our camera high above the Earth, we rush in towards the surface at what would be an impossible speed for any known vehicle. Passing though layers of atmosphere, the colors of our destinations shimmer with their own unique characteristics, and suddenly we find ourselves floating in virtual space just above the ground. || ",
            "hits": 3
        },
        {
            "id": 2438,
            "url": "https://svs.gsfc.nasa.gov/2438/",
            "result_type": "Visualization",
            "release_date": "2002-04-30T12:00:00-04:00",
            "title": "Great Zoom out of Sabie River, Africa (EOS Land Validation Site)",
            "description": "Using data from different spacecraft and some powerful computer technology, visualizers at the Goddard Space Flight Center present you with a collection of American cities in a way you have never seen them before. Starting with our camera high above the Earth, we rush in towards the surface at what would be an impossible speed for any known vehicle. Passing though layers of atmosphere, the colors of our destinations shimmer with their own unique characteristics, and suddenly we find ourselves floating in virtual space just above the ground. || ",
            "hits": 4
        },
        {
            "id": 2439,
            "url": "https://svs.gsfc.nasa.gov/2439/",
            "result_type": "Visualization",
            "release_date": "2002-04-30T12:00:00-04:00",
            "title": "Great Zoom into Sabie River, Africa (EOS Land Validation Site)",
            "description": "Using data from different spacecraft and some powerful computer technology, visualizers at the Goddard Space Flight Center present you with a collection of American cities in a way you have never seen them before. Starting with our camera high above the Earth, we rush in towards the surface at what would be an impossible speed for any known vehicle. Passing though layers of atmosphere, the colors of our destinations shimmer with their own unique characteristics, and suddenly we find ourselves floating in virtual space just above the ground. || ",
            "hits": 4
        },
        {
            "id": 2331,
            "url": "https://svs.gsfc.nasa.gov/2331/",
            "result_type": "Visualization",
            "release_date": "2001-12-01T12:00:00-05:00",
            "title": "Great Zoom into Beltsville, MD: Beltsville Agricultural Research Center",
            "description": "Using data from different spacecraft and some powerful computer technology, visualizers at the Goddard Space Flight Center present you with a collection of American cities in a way you have never seen them before. Starting with our camera high above the Earth, we rush in towards the surface at what would be an impossible speed for any known vehicle. Passing though layers of atmosphere, the colors of our destinations shimmer with their own unique characteristics, and suddenly we find ourselves floating in virtual space just above the ground. || ",
            "hits": 9
        },
        {
            "id": 562,
            "url": "https://svs.gsfc.nasa.gov/562/",
            "result_type": "Visualization",
            "release_date": "1999-02-02T12:00:00-05:00",
            "title": "EOS NPOESS the Bridge Mission",
            "description": "A Dynamic proposal between the National Aeronautics and Space Administration and the National Polar Orbiting Environmental Satellite System Integrated Program Office.  A project to bridge or link between the operations of the Earth Observing System AM-1 and the PM-1 Spacecraft and the National Polar Orbiting Environmental Satellite System Spacecraft (NPOESS) || ",
            "hits": 45
        },
        {
            "id": 183,
            "url": "https://svs.gsfc.nasa.gov/183/",
            "result_type": "Visualization",
            "release_date": "1998-01-01T12:00:00-05:00",
            "title": "EOS - AM1 Beauty Shot",
            "description": "AM1 orbiting the Earth || a000183.00095_print.png (720x480) [219.7 KB] || a000183_pre.jpg (320x242) [3.8 KB] || a000183.webmhd.webm (960x540) [793.1 KB] || a000183.dv (720x480) [38.2 MB] || a000183.mp4 (640x480) [2.2 MB] || a000183.mpg (352x240) [1.4 MB] || AM1 spacecraft with Earth globe in the background || EOS_AM1.gif (1280x960) [286.8 KB] || EOS_AM1_web.jpg (320x240) [11.1 KB] || EOS_AM1_thm.png (80x40) [3.6 KB] || EOS_AM1_web_searchweb.jpg (320x180) [74.6 KB] || ",
            "hits": 66
        },
        {
            "id": 108,
            "url": "https://svs.gsfc.nasa.gov/108/",
            "result_type": "Visualization",
            "release_date": "1996-03-22T12:00:00-05:00",
            "title": "Assimilation of N2O in the Upper Atmosphere Using a Kalman Filter: N2O Mixing Ratio",
            "description": "This series of animations shows assimilation of N2O in the upper atmosphere using observations from the Cryogenic Limb Etalon Spectrometer (CLAES) on the Upper Atmosphere Research Satellite (UARS). Winds were provided by the Goddard EOS Data Assimilation System (GEOS-DAS). Flow is at the 850K isentropic level. N2O mixing ratio is expressed in parts per billion volume (ppbv). || ",
            "hits": 25
        },
        {
            "id": 1394,
            "url": "https://svs.gsfc.nasa.gov/1394/",
            "result_type": "Visualization",
            "release_date": "1996-03-22T12:00:00-05:00",
            "title": "Assimilation of N2O in the Upper Atmosphere Using a Kalman Filter: Error Correlation",
            "description": "This series of animations shows assimilation of N2O in the upper atmosphere using observations from the Cryogenic Limb Etalon Spectrometer (CLAES) on the Upper Atmosphere Research Satellite (UARS). Winds were provided by the Goddard EOS Data Assimilation System (GEOS-DAS). Flow is at the 850K isentropic level. N2O mixing ratio is expressed in parts per billion volume (ppbv). || ",
            "hits": 8
        }
    ]
}