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    "results": [
        {
            "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": 30368,
            "url": "https://svs.gsfc.nasa.gov/30368/",
            "result_type": "Hyperwall Visual",
            "release_date": "2013-10-23T12:00:00-04:00",
            "title": "Monthly Outgoing Longwave Radiation",
            "description": "Light energy travels in waves, but not all the waves are the same. The kind of light our eyes can see is only a tiny part of the energy that exists in the universe. Other kinds of energy are invisible, like the energy that makes our hands feel warm when we hold them over a fire, or the energy that cooks our food in the microwave. When Earth absorbs sunlight, it heats up. The heat, or \"outgoing longwave radiation,\" radiates back into space. Satellites measure this radiation as it leaves the top of Earth's atmosphere. The hotter a place is, the more energy it radiates. These maps show monthly outgoing longwave radiation from July 2006 to the present, from the Fast Longwave And Shortwave Radiative Fluxes, or FLASHFlux, Time Interpolation and Spatial Averaging (TISA) data product. The product contains daily observations collected by the Clouds and the Earth's Radiant Energy System (CERES) sensors on NASA's Aqua and Terra satellites. The colors show the amount of outgoing longwave radiation leaving Earth's atmosphere (in Watts per square meter). Bright yellow and orange indicate greater heat emission, purple and blue indicate intermediate emissions, and white shows little or no heat emission. || ",
            "hits": 115
        },
        {
            "id": 3176,
            "url": "https://svs.gsfc.nasa.gov/3176/",
            "result_type": "Visualization",
            "release_date": "2005-06-21T00:00:00-04:00",
            "title": "Outgoing Longwave Flux Compared to Clouds (WMS)",
            "description": "The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere. As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights. The amount of reflection and absorption is critical to the climate. An instrument named CERES orbits the Earth every 99 minutes and measures the reflected solar energy. This animation shows the outgoing thermal radiation measured by CERES during 29 orbits on June 20 and 21 of 2003 over global infrared cloud images. Thermal radiation is longwave radiation and depends on the temperature of the earth, with the most intense radiation coming from the warmest regions and the least from cold clouds in the atmosphere. Although cold clouds and the cold Antarctic night regions can be seen in this data, the Earth radiates pretty uniformly in the longwave bands because the atmosphere distributes the heat of the sun to the whole planet. || ",
            "hits": 37
        },
        {
            "id": 3155,
            "url": "https://svs.gsfc.nasa.gov/3155/",
            "result_type": "Visualization",
            "release_date": "2005-05-27T12:00:00-04:00",
            "title": "Urban Signatures: Thermal Radiation (WMS)",
            "description": "Big cities influence the environment around them. For example, urban areas are typically warmer than their surroundings. Cities are strikingly visible in computer models that simulate the Earth's land surface. This visualization shows outgoing thermal radiation predicted by the Land Information System (LIS) for a day in June 2001. Cities are warmer, so they emit more longwave (infrared) radiation. Only part of the global computation is shown, focusing on the highly urbanized northeast corridor in the United States, including the cities of Boston, New York, Philadelphia, Baltimore, and Washington. || ",
            "hits": 34
        },
        {
            "id": 3091,
            "url": "https://svs.gsfc.nasa.gov/3091/",
            "result_type": "Visualization",
            "release_date": "2005-02-01T12:00:00-05:00",
            "title": "Average Clear-sky Outgoing Longwave Flux (WMS)",
            "description": "The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere.  As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights.  The average amount of reflection and absorption is critical to the climate, because the absorbed energy heats up the Earth until it is radiated away as thermal radiation.   This animation shows the monthly average clear-sky outgoing longwave radiation from July, 2002 through June, 2004 as measured by the CERES instrument.  This is the thermal radiation given off by the warm Earth when the sky is cloud free.  The Earth's rotation and the movement of warm air from the equator to the poles make the Earth roughly uniformin temperature.  The most visible features are the cold poles in winter and the significant regions of snow coverage in the northern hemisphere, also in winter. || ",
            "hits": 24
        },
        {
            "id": 3092,
            "url": "https://svs.gsfc.nasa.gov/3092/",
            "result_type": "Visualization",
            "release_date": "2005-02-01T12:00:00-05:00",
            "title": "Average Total-sky Outgoing Longwave Flux (WMS)",
            "description": "The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere.  As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights.  The average amount of reflection and absorption is critical to the climate, because the absorbed energy heats up the Earth until it is radiated away as thermal radiation.  This animation shows the monthly average outgoing longwave radiation from July, 2002 through June, 2004 as measured by the CERES instrument.  This is the thermal radiation given off by the warm Earth.  The Earth's rotation and the movement of warm air from the equator to the poles make the Earth roughly  uniform in temperature.  The most visible features are the cold poles in winter and the cold clouds along the equator which trap the outgoing thermal radiation. || ",
            "hits": 26
        },
        {
            "id": 3107,
            "url": "https://svs.gsfc.nasa.gov/3107/",
            "result_type": "Visualization",
            "release_date": "2005-02-01T12:00:00-05:00",
            "title": "Instantaneous Outgoing Longwave Flux (WMS)",
            "description": "The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere.  As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights. The amount of reflection and absorption is critical to the climate.  An instrument named CERES orbits the Earth every 99 minutes and measures the reflected solar energy.  This animation shows the outgoing thermal radiation measured by CERES during 29 orbits on June 20 and 21 of 2003.  Thermal radiation is longwave radiation and depends on the temperature of the earth, with the most intense radiation coming from the warmest regions and the least from cold clouds in the atmosphere.  Although cold clouds and the cold Antarctic night regions can be seen in this data, the Earth radiates pretty uniformly in the longwave bands because the atmosphere distributes the heat of the sun to the whole planet. || ",
            "hits": 7
        },
        {
            "id": 2157,
            "url": "https://svs.gsfc.nasa.gov/2157/",
            "result_type": "Visualization",
            "release_date": "2001-06-20T12:00:00-04:00",
            "title": "One Year of Terra/CERES Data (Outgoing Longwave Radiation) Daily Data",
            "description": "This animation displays one year of Outgoing Longwave Radiation (OLR) Terra/CERES data (March 1, 2000 to May 25, 2001) at one day resolution. The data are 2.5 degree resolution. || Movie at one frame per day of Terra-CERES OLR data. || a002157.00005_print.png (720x480) [513.3 KB] || a002157_pre.jpg (320x242) [10.1 KB] || a002157.webmhd.webm (960x540) [22.4 MB] || a002157.dv (720x480) [432.9 MB] || a002157.mpg (352x240) [16.4 MB] || ",
            "hits": 14
        },
        {
            "id": 2159,
            "url": "https://svs.gsfc.nasa.gov/2159/",
            "result_type": "Visualization",
            "release_date": "2001-06-20T12:00:00-04:00",
            "title": "14-Day Boxcar Averaged Terra/CERES Data (Outgoing Longwave Radiation)",
            "description": "This animation displays one year of Outgoing Longwave Radiation (OLR) Terra/CERES data (March 1, 2000 to May 25, 2001) with a 14-day boxcar average. Endpoints have the average re-weighted for the smaller amount of data. The data are 2.5 degree resolution. || ",
            "hits": 7
        },
        {
            "id": 2167,
            "url": "https://svs.gsfc.nasa.gov/2167/",
            "result_type": "Visualization",
            "release_date": "2001-06-20T12:00:00-04:00",
            "title": "Terra/CERES on the American Southwest: May 2001",
            "description": "Terra/CERES views the American southwest during the heatwave of May 2001.  The animation is generated for outgoing longwave radiation (heat). || Movie of the American Southwest during a heatwave.  April-May 2001. || a002167.00005_print.png (720x480) [580.5 KB] || a002167_pre.jpg (320x242) [8.7 KB] || a002167.webmhd.webm (960x540) [1.9 MB] || a002167.dv (720x480) [55.5 MB] || a002167.mpg (352x240) [1.9 MB] || ",
            "hits": 7
        },
        {
            "id": 2169,
            "url": "https://svs.gsfc.nasa.gov/2169/",
            "result_type": "Visualization",
            "release_date": "2001-06-20T12:00:00-04:00",
            "title": "Terra/CERES Views the Americas in Outgoing Longwave Radiation - Daily Data",
            "description": "Terra/CERES views the Americas in Outgoing Longwave Radiation (March 1, 2000 to May 25, 2001). These are daily data. || Movie of the Americas in OLR. || a002169.00005_print.png (720x480) [621.3 KB] || a002169_pre.jpg (320x242) [9.1 KB] || a002169.webmhd.webm (960x540) [22.3 MB] || a002169.dv (720x480) [432.7 MB] || a002169.mpg (352x240) [16.4 MB] || ",
            "hits": 8
        },
        {
            "id": 2170,
            "url": "https://svs.gsfc.nasa.gov/2170/",
            "result_type": "Visualization",
            "release_date": "2001-06-20T12:00:00-04:00",
            "title": "Terra/CERES Outgoing Longwave and Reflected Solar Radiation: Boxcar Averaged",
            "description": "Terra/CERES views the world in outgoing longwave radiation (left) and reflected solar radiation (right). This is a 14-day boxcar averaged datas ets from March 1, 2001 to May 25, 2001. || Side-by-side Earth views of 14-day boxcar averaged OLR & RSR data. || a002170.00005_print.png (720x480) [424.9 KB] || a002170_pre.jpg (320x240) [7.0 KB] || a002170.webmhd.webm (960x540) [2.5 MB] || a002170.dv (720x480) [72.0 MB] || a002170.mpg (320x240) [2.1 MB] || ",
            "hits": 13
        },
        {
            "id": 2171,
            "url": "https://svs.gsfc.nasa.gov/2171/",
            "result_type": "Visualization",
            "release_date": "2001-06-20T12:00:00-04:00",
            "title": "Terra/CERES Outgoing Longwave and Reflected Solar Radiation: Daily Data",
            "description": "Terra/CERES views the world in outgoing longwave radiation (left) and reflected solar radiation (right). This is daily data from March 1, 2000 to May 25, 2001. || Synchronized, side-by-side views of the Earth in RSR & OLR. || a002171.00005_print.png (720x480) [451.5 KB] || a002171_pre.jpg (320x238) [7.8 KB] || a002171.webmhd.webm (960x540) [24.2 MB] || a002171.dv (720x480) [432.9 MB] || a002171.mpg (352x240) [16.4 MB] || ",
            "hits": 8
        },
        {
            "id": 2173,
            "url": "https://svs.gsfc.nasa.gov/2173/",
            "result_type": "Visualization",
            "release_date": "2001-06-20T12:00:00-04:00",
            "title": "Terra/CERES Views the World in Outgoing Longwave Radiation - Daily data",
            "description": "Terra/CERES views the world in outgoing longwave radiation. These are daily data from March 1, 2000 to May 25, 2001. || Movie of daily OLR data on a spinning Earth. || a002173.00005_print.png (720x480) [430.1 KB] || a002173_pre.jpg (320x242) [6.6 KB] || a002173.webmhd.webm (960x540) [19.8 MB] || a002173.dv (720x480) [433.0 MB] || a002173.mpg (352x240) [16.5 MB] || ",
            "hits": 18
        },
        {
            "id": 2174,
            "url": "https://svs.gsfc.nasa.gov/2174/",
            "result_type": "Visualization",
            "release_date": "2001-06-20T12:00:00-04:00",
            "title": "Terra/CERES Views the Pakistan Heat Wave: May 2001",
            "description": "Terra/CERES views the Pakistan heat wave. || Movie of OLR changes in May 2001 near Pakistan. || a002174.00005_print.png (720x480) [630.4 KB] || a002174_pre.jpg (320x242) [9.8 KB] || a002174.webmhd.webm (960x540) [2.4 MB] || a002174.dv (720x480) [55.5 MB] || a002174.mpg (352x240) [1.5 MB] || May 5, 2001 || PakistanOLR3445.jpg (2560x1920) [420.0 KB] || PakistanOLR3445_web.jpg (320x240) [14.8 KB] || PakistanOLR3445.tif (2560x1920) [2.9 MB] || ",
            "hits": 14
        }
    ]
}