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        {
            "id": 14634,
            "url": "https://svs.gsfc.nasa.gov/14634/",
            "result_type": "Produced Video",
            "release_date": "2024-07-25T14:00:00-04:00",
            "title": "Fermi Finds Novel Feature in BOAT Gamma-Ray Burst",
            "description": "The brightest gamma-ray burst yet recorded gave scientists a new high-energy feature to study. Learn what NASA’s Fermi mission saw, and what this feature may be telling us about the burst’s light-speed jets. Credit: NASA's Goddard Space Flight CenterMusic: “Tides,” Jon Cotton [PRS] and Ben Niblett [PRS], Universal Production MusicWatch this video on the NASA Goddard YouTube channel.Complete transcript available. || Distant_GRB_still.jpg (3840x2160) [2.5 MB] || 14634_Fermi_GRB_Emission_Line_Under100.mp4 (1920x1080) [90.7 MB] || 14634_Fermi_GRB_Emission_Line_Best.mp4 (1920x1080) [422.0 MB] || 14634FermiGRBEmissionLine_Captions.en_US.srt [4.4 KB] || 14634FermiGRBEmissionLine_Captions.en_US.vtt [4.2 KB] || 14634_Fermi_GRB_Emission_Line_ProRes_1920x1080_2997.mov (1920x1080) [2.8 GB] || ",
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        },
        {
            "id": 13710,
            "url": "https://svs.gsfc.nasa.gov/13710/",
            "result_type": "Produced Video",
            "release_date": "2020-10-05T13:00:00-04:00",
            "title": "TESS's Northern Sky Vista",
            "description": "NASA’s Transiting Exoplanet Survey Satellite (TESS) spent nearly a year imaging the northern sky in its search for worlds beyond our solar system. Explore this panorama to see what TESS has found so far.Credit: NASA's Goddard Space Flight CenterMusic: \"Strolling\" from Above and Below. Written and produced by Lars LeonhardWatch this video on the NASA Goddard YouTube channel.Complete transcript available. || TESS_Northern_and_Southern_Still.jpg (1920x1080) [699.1 KB] || 13710_TESS_Northern_Tour_Best_1080.webm (1920x1080) [33.4 MB] || 13710_TESS_Northern_Tour_1080.mp4 (1920x1080) [423.5 MB] || 13710_TESS_Northern_Tour_SRT_Captions.en_US.srt [4.9 KB] || 13710_TESS_Northern_Tour_SRT_Captions.en_US.vtt [4.9 KB] || 13710_TESS_Northern_Tour_Best_1080.mp4 (1920x1080) [1.1 GB] || 13710_TESS_Northern_Tour_ProRes_1920x1080_2997.mov (1920x1080) [4.0 GB] || ",
            "hits": 59
        },
        {
            "id": 13285,
            "url": "https://svs.gsfc.nasa.gov/13285/",
            "result_type": "Produced Video",
            "release_date": "2019-11-05T13:00:00-05:00",
            "title": "TESS's Southern Sky Panorama",
            "description": "NASA’s Transiting Exoplanet Survey Satellite (TESS) spent a year imaging the southern sky in its search for worlds beyond our solar system. Dive into a mosaic of these images to see what TESS has found so far. Credit: NASA's Goddard Space Flight CenterMusic: “Phenomenon\" from Above and Below Written and produced by Lars LeonhardWatch this video on the NASA Goddard YouTube channel.Complete transcript available. || Southern_Sky_Still.jpg (1920x1080) [892.0 KB] || Southern_Sky_Still_print.jpg (1024x576) [222.5 KB] || Southern_Sky_Still_searchweb.png (320x180) [66.5 KB] || Southern_Sky_Still_thm.png (80x40) [5.0 KB] || 13285_TESS_SouthernSky_Small_720.webm (1280x720) [26.3 MB] || 13285_TESS_SouthernSky_Small_720.mp4 (1280x720) [250.7 MB] || 13285_TESS_SouthernSky_1080.mp4 (1920x1080) [492.4 MB] || 13285_TESS_SouthernSky_SRT_Captions.en_US.srt [4.3 KB] || 13285_TESS_SouthernSky_SRT_Captions.en_US.vtt [4.3 KB] || 13285_TESS_SouthernSky_Best_1080.mp4 (1920x1080) [1.2 GB] || 13285_TESS_SouthernSky_ProRes_1920x1080_30.mov (1920x1080) [3.5 GB] || tesss-southern-sky-panorama-movie.hwshow || 07a_tess_coverage.hwshow [190 bytes] || ",
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        },
        {
            "id": 4428,
            "url": "https://svs.gsfc.nasa.gov/4428/",
            "result_type": "Visualization",
            "release_date": "2016-02-19T00:00:00-05:00",
            "title": "2012 Mediterranean Drought",
            "description": "Print resolution image showing less than normal ground water saturation throughout the Mediteranean region on January 15, 2012. This image includes the date and colorbar overlay. || grace_med_comp.3666_print.jpg (1024x576) [172.1 KB] || grace_med_comp.3666_searchweb.png (320x180) [88.0 KB] || grace_med_comp.3666_thm.png (80x40) [13.9 KB] || grace_med_comp.3666.tif (3840x2160) [74.7 MB] || ",
            "hits": 23
        },
        {
            "id": 4413,
            "url": "https://svs.gsfc.nasa.gov/4413/",
            "result_type": "Visualization",
            "release_date": "2016-01-07T00:00:00-05:00",
            "title": "Sea Surface Temperature Anomaly and Terrestrial Water Storage Anomaly Comparison",
            "description": "Animation showing Sea Surface Temperature Anomaly (SSTA) and Terrestrial Water Storage Anomaly (TWSA) data from 2002 to 2015 simultaneously. For SSTA data, blues indicate temperatures lower than normal and reds are areas warmer than normal. With this data we can see the comings and goings of El Niño and La Niña across the years. For the TWSA data, browns indicate areas with less ground water than normal and greens are areas with more ground water than normal, which correlates to droughts and floods in these various regions. Furthermore, terrestrial areas that show significant amounts of low water storage are much more sensitive to wildfires. || grace_w_ssta_rob2.4991_print.jpg (1024x576) [133.2 KB] || grace_w_ssta_rob2.4991_searchweb.png (180x320) [91.1 KB] || grace_w_ssta_rob2.4991_thm.png (80x40) [7.7 KB] || grace_w_ssta_rob2_2x_1080p30.mp4 (1920x1080) [41.8 MB] || composite (1920x1080) [0 Item(s)] || robinson_projection (1920x1080) [0 Item(s)] || dates (1920x1080) [0 Item(s)] || grace_w_ssta_rob2_2x_1080p30.webm (1920x1080) [9.8 MB] || ",
            "hits": 28
        },
        {
            "id": 4415,
            "url": "https://svs.gsfc.nasa.gov/4415/",
            "result_type": "Visualization",
            "release_date": "2016-01-06T00:00:00-05:00",
            "title": "Terrestrial Water Storage Anomaly 2002 - 2015",
            "description": "Animation showing Terrestrial Water Storage Anomaly (TWSA) data from 2002 to 2015. Browns indicate areas with less ground water than normal and greens are areas with more ground water than normal, which correlates to droughts and floods in these various regions.This video is also available on our YouTube channel. || grace_anom_comp_v2.4991_print.jpg (1024x576) [124.4 KB] || grace_anom_comp_v2.4991_searchweb.png (320x180) [70.7 KB] || grace_anom_comp_v2.4991_thm.png (80x40) [6.3 KB] || grace_anom_comp_v2_2x_1080p30.mp4 (1920x1080) [25.8 MB] || grace_anom_comp_v2_2x_1080p30.webm (1920x1080) [8.7 MB] || composite (1920x1080) [0 Item(s)] || robinson_projection (1920x1080) [0 Item(s)] || dates (1920x1080) [0 Item(s)] || grace_anom_comp_v2_2x_1080p30.mp4.hwshow [195 bytes] || ",
            "hits": 47
        },
        {
            "id": 30697,
            "url": "https://svs.gsfc.nasa.gov/30697/",
            "result_type": "Hyperwall Visual",
            "release_date": "2015-10-23T00:00:00-04:00",
            "title": "Ocean Alkalinity",
            "description": "To document effects of ocean acidification it is important to have an understanding of the processes and parameters that influence alkalinity. Alkalinity is a measure of the ability of seawater to neutralize acids. This visualization shows monthly surface total alkalinity (TA) from August 2011 to May 2015 as derived using data from NASA’s Aquarius mission. Utilization of Aquarius data allows unprecedented global mapping of surface TA as it correlates strongly with salinity and to a lesser extent with temperature.For the first time, Aquarius data are allowing scientists to observe changes in surface alkalinity over time. For example, they have found that the Northern Hemisphere has more spatial and monthly variability in total alkalinity and salinity, while less variability in Southern Ocean alkalinity is due to less salinity variability and upwelling of waters enriched in alkalinity. Increasing surface TA in subtropical regions from increasing salinity and temperature causes the saturation states of calcite and aragonite to decrease, i.e., enhanced dissolution. Thus, based on increasing TA in the subtropical regions over the past few decades, it is expected that it is becoming more difficult for calcifying organisms to make their shells. || ",
            "hits": 73
        },
        {
            "id": 3579,
            "url": "https://svs.gsfc.nasa.gov/3579/",
            "result_type": "Visualization",
            "release_date": "2009-02-05T00:00:00-05:00",
            "title": "Sea Ice over the Arctic and Antarctic designed for Science On a Sphere (SOS) and WMS",
            "description": "Sea ice is frozen seawater floating on the surface of the ocean, typically averaging a few meters in thickness. Some sea ice is semi-permanent, persisting from year to year, and some is seasonal, melting and refreezing from season to season. This animation shows how the seasonal global sea ice has changed from day to day since 2002, when the Aqua satellite was launched. The AMSR-E instrument on the Aqua satellite acquires high resolution measurements of the 89 GHz brightness temperature and sea ice concentration near the poles. This sensor is able to observe the entire polar region every day, even through clouds and snowfall, because it is not very sensitive to atmospheric effects. The false color of the sea ice, derived from the AMSR-E 6.25 km 89 GHz brightness temperature, highlights the fissures or divergence areas in the sea ice cover by warm brightness temperatures (in blue) while cold brightness temperatures, shown in brighter white, represent consolidated sea ice. The sea ice edge identifies areas containing at least 15% ice concentration in the three-day moving average of the AMSR-E 12.5 km sea ice concentration data.This sequence shows the daily global sea ice over both the Arctic and Antarctic on a Cartesian grid from June 21, 2002 through December 31, 2008 at a frame rate of four frames per day. On days when data is not available, the prior or following day's data is used. Periods when data was absent for several consecutive days include: 2002/07/29 through 2002/08/08, 2002/09/11 through 2002/09/20, and 2003/10/29 through 2003/11/03. || ",
            "hits": 25
        },
        {
            "id": 3564,
            "url": "https://svs.gsfc.nasa.gov/3564/",
            "result_type": "Visualization",
            "release_date": "2008-01-06T00:00:00-05:00",
            "title": "Sea Ice over the Arctic and Antarctic designed for Science On a Sphere (SOS) and WMS",
            "description": "Sea ice is frozen seawater floating on the surface of the ocean, typically averaging a few meters in thickness. Some sea ice is semi-permanent, persisting from year to year, and some is seasonal, melting and refreezing from season to season. This animation shows how the seasonal global sea ice has changed from day to day in both the northern and southern hemisphere since 2002, when the Aqua satellite was launched.This series shows the daily global sea ice over both the Arctic and Antarctic from June 21, 2002 through September 22, 2008. Global data from the AMSR-E instrument on the Aqua satellite is shown on a Cartesian grid. The sea ice extent is derived from the daily AMSR-E 12.5 km sea ice concentration where the ice concentration is above 15%. || ",
            "hits": 27
        },
        {
            "id": 20016,
            "url": "https://svs.gsfc.nasa.gov/20016/",
            "result_type": "Animation",
            "release_date": "2003-12-09T12:00:00-05:00",
            "title": "Aqua Mission Science Objectives",
            "description": "The Water Cycle  - Water falling from summer storm clouds onto a field of wheat today will someday fall again somewhere else. This is the essence of the water cycle.  The first step in the cycle is evaporation. Heated by sunlight, liquid water turns to vapor and enters the atmosphere. Another source of atmospheric water vapor is the respiratory process of plants.  Vapor leaves plants through tiny pores called stomata. This process is called transpiration. As moist air ascends into the atmosphere and encounters lower atmospheric pressure, the invisible water vapor transforms back into liquid water, and we see the next phase in the water cycle: condensation. Droplets of water coalesce from traces of vapor, and as they gain size by joining with other droplets, they yield the next part of the water cycle. This is called precipitation. The cycle is endless. As it's name suggests, the Aqua project will be intensely involved in studying the water cycle in its many forms.Evaporation - Depending on total ambient temperature, relative humidity, wind speed, and water temperature, some molecules of water are almost always passing from liquid to gaseous state at the surface. This is called evaporation. Evaporation is what puts moisture into the air, pulling water off the surface of lakes and streams and topsoil. Not only does water vapor enter the atmosphere, but also evaporating water pulls heat away from the surface. That heat will get redistributed to a different part of the atmosphere when the recently liberated water vapor re-condenses.Transpiration - Related to evaporation, this is the respiratory equivalent of breathing in plants. Transpiration is how plants lose water to the surrounding air. While some water directly evaporates through the walls of cells on the surface of plants, the majority of water lost happens through intercellular structures called stomata. These are like tiny pores. Transpiration helps pull nutrients from plant roots up to leaves. It's a natural process that's heavily influenced by ambient temperature, humidity, and other factors. Additionally, transpiration also helps properly circulate carbon dioxide and oxygen, diffusing the first into plant cells for growth, and carrying the second away from cells as waste gas.Condensation - The process that describes the change in physical state of a gas to a liquid is called condensation. Generally this is a phenomenon brought about by either of two processes: cooling of air to its dewpoint, or the addition of enough water vapor to bring the air to the point of saturation. But as that moisture either reaches high enough altitudes so that the air containing it is chilled by lower temperatures found there, or affected by increasing humidity from dynamic meteorological conditions, it condenses. The water molecules start moving more slowly, and the state of matter begins to change, as water molecules start hooking up. Gas becomes a liquid. Condensation can take many forms without necessarily falling from the sky. Dew, fog, mist, and clouds are all examples of condensed water.Precipitation - Simply speaking, precipitation is a function of water changing its material state from vapor to a liquid or a solid. But more specifically, two fundamental steps must take place for water to fall from the sky. The first is that basic precipitation components must develop. These include ice crystals that form around various minute particles in the atmosphere such as dust or salts. The second step is for those ice crystals or condensed droplets to grow. Because of their increasing size, larger droplets or ice crystals are more apt to collide with other particles of water, and thus more likely to fall or 'precipitate' out of a cloud. || ",
            "hits": 386
        },
        {
            "id": 2796,
            "url": "https://svs.gsfc.nasa.gov/2796/",
            "result_type": "Visualization",
            "release_date": "2003-09-08T12:00:00-04:00",
            "title": "Hubble Space Telescope: Image Deblurring with a Parallel Comptuer",
            "description": "This is the star system is known as R-Aquarii, this system is comprised of a hot star orbiting a mass losing giant star. || ",
            "hits": 65
        }
    ]
}