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        {
            "id": 4256,
            "url": "https://svs.gsfc.nasa.gov/4256/",
            "result_type": "Visualization",
            "release_date": "2015-03-16T10:00:00-04:00",
            "title": "The Winter of 2013 – 2014: A Cold, Snowy and Icy Winter in North America",
            "description": "This animation shows the snow cover over North America during the 2013-2014 winter as well as the ice concentration over the Great Lakes.  The date and a graph showing the percent of ice cover over the Great Lakes and Lake Superior is shown on this version. || GreatLakes_ice_2014-15_30p.02845_print.jpg (1024x576) [134.0 KB] || GreatLakes_ice_2014-15_30p.02845_searchweb.png (320x180) [90.3 KB] || GreatLakes_ice_2014-15_30p.02845_thm.png (80x40) [6.6 KB] || GreatLakes_Ice_2013-2014_720.mp4 (1280x720) [42.1 MB] || GreatLakes_Ice_2013-2014_1080.mp4 (1920x1080) [74.5 MB] || GreatLakes_ice_withOlay (1920x1080) [0 Item(s)] || GreatLakes_ice_withOlay (1920x1080) [0 Item(s)] || GreatLakes_Ice_2013-2014_720.webm (1280x720) [27.5 MB] || GreatLakes_Ice_2013-2014_4256.key [45.7 MB] || GreatLakes_Ice_2013-2014_4256.pptx [43.1 MB] || ",
            "hits": 44
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        {
            "id": 3853,
            "url": "https://svs.gsfc.nasa.gov/3853/",
            "result_type": "Visualization",
            "release_date": "2011-10-24T00:00:00-04:00",
            "title": "AMSR-E Arctic Sea Ice",
            "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.In this animation, the Arctic sea ice and seasonal land cover change progress through time, from September 4, 2009 through January 30, 2011. Over the water, Arctic sea ice changes from day to day showing a running 3-day average 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 miniimum 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. || ",
            "hits": 27
        },
        {
            "id": 3854,
            "url": "https://svs.gsfc.nasa.gov/3854/",
            "result_type": "Visualization",
            "release_date": "2011-10-24T00:00:00-04:00",
            "title": "AMSR-E Antarctic Sea Ice",
            "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.In this animation, the Antarctic sea ice progresses through time from May 26, 2009 through July 31, 2010. Over the water, Arctic sea ice changes from day to day showing a running 3-day average 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 minimum of the AMSR-E 89 GHz brightness temperature. Over the Antarctic continent, the LIMA data shown here uses the pan-chromatic band and has a resolution of 240 meters per pixel. The Landsat Image Mosaic of Antarctica (LIMA) is a data product funded by the National Science Foundation (NSF) and jointly produced by the U.S. Geological Survey (USGS), the British Antarctic Survey (BAS), and the National Aeronautics and Space Administration (NASA). || ",
            "hits": 47
        },
        {
            "id": 3824,
            "url": "https://svs.gsfc.nasa.gov/3824/",
            "result_type": "Visualization",
            "release_date": "2011-03-29T00:00:00-04:00",
            "title": "AMSR-E Arctic Sea Ice: September 2010 to March 2011",
            "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.In this animation, the Arctic sea ice and seasonal land cover change progress through time, from the 2010 minimum which occurred on September 17 through March 16, 2011. 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. || ",
            "hits": 17
        },
        {
            "id": 3767,
            "url": "https://svs.gsfc.nasa.gov/3767/",
            "result_type": "Visualization",
            "release_date": "2010-09-29T00:00:00-04:00",
            "title": "Arctic Sea Ice Minimum Extent for 2010",
            "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.In this animation, the Arctic sea ice and seasonal land cover change progress through time, from March 31, 2010 when sea ice in the Arctic was at its maximum extent, through September 19, 2010, when it was at its minimum. 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. || ",
            "hits": 39
        },
        {
            "id": 3698,
            "url": "https://svs.gsfc.nasa.gov/3698/",
            "result_type": "Visualization",
            "release_date": "2010-03-29T00:00:00-04:00",
            "title": "AMSR-E Arctic Sea Ice: September 2009 to March 2010",
            "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.In this animation, the Arctic sea ice and seasonal land cover change progress through time, from September 1, 2009 when sea ice in the Arctic was near its minimum extent, through March 30, 2010. The animation plays at a rate of six frames per day or ten days per second. 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. || ",
            "hits": 26
        },
        {
            "id": 3571,
            "url": "https://svs.gsfc.nasa.gov/3571/",
            "result_type": "Visualization",
            "release_date": "2008-12-18T00:00:00-05:00",
            "title": "AMSR-E Arctic Sea Ice: 2005 to 2008",
            "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.In this animation, the globe slowly rotates one full rotation while the Arctic sea ice and seasonal land cover change throughout the years. The animation begins on September 21, 2005 when sea ice in the Arctic was at its minimum extent, and continues through September 20, 2008. This time period repeats twice during the animation, playing at a rate of one frame per day. Over the terrain, monthly data from the seasonal Blue Marble Next Generation fades slowly from month to month. Over the water, Arctic sea ice changes from day to day. This is a modification of animation ID  #3404 : Global Rotation showing Seasonal Landcover and Arctic Sea Ice, which only covered a one-year time period.For a 3D stereo version of this visualization, please visit animation entry:  #3578: AMSR-E Arctic Sea Ice: 2005 to 2008 - Stereoscopic Version || ",
            "hits": 36
        },
        {
            "id": 3578,
            "url": "https://svs.gsfc.nasa.gov/3578/",
            "result_type": "Visualization",
            "release_date": "2008-12-18T00:00:00-05:00",
            "title": "AMSR-E Arctic Sea Ice: 2005 to 2008 - Stereoscopic Version",
            "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.In this animation, the globe slowly rotates one full rotation while the Arctic sea ice and seasonal land cover change throughout the years. The animation begins on September 21, 2005 when sea ice in the Arctic was at its minimum extent, and continues through September 20, 2008. This time period repeats twice during the animation, playing at a rate of one frame per day. Over the terrain, monthly data from the seasonal Blue Marble Next Generation fades slowly from month to month. Over the water, Arctic sea ice changes from day to day. This visualization is a stereoscopic version of animation entry:  #3571: AMSR-E Arctic Sea Ice: 2005 to 2008In this page the visualization content is offered in two different modes to accomodate stereoscopic systems, such as: Left and Right Eye separate and Left and Right Eye side-by-side combined on the same frame. || ",
            "hits": 52
        }
    ]
}