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        {
            "id": 13761,
            "url": "https://svs.gsfc.nasa.gov/13761/",
            "result_type": "Produced Video",
            "release_date": "2020-11-05T11:00:00-05:00",
            "title": "Rising Waters: Out-of-Balance Ice Sheets",
            "description": "Music: \"Marimba Rhythms\" via Universal Production MusicComplete transcript available. || Anatomy_Glacier_Thumbnail.png (1280x720) [1.2 MB] || Anatomy_Glacier_Thumbnail_print.jpg (1024x576) [91.9 KB] || Anatomy_Glacier_Thumbnail_searchweb.png (320x180) [79.1 KB] || Anatomy_Glacier_Thumbnail_thm.png (80x40) [6.0 KB] || Anatomy_Glacier_FINAL.mov (1280x720) [1.4 GB] || Anatomy_Glacier_FINAL.mp4 (1920x1080) [197.9 MB] || Anatomy_Glacier_FINAL.webm (1920x1080) [22.6 MB] || Anatomy_Glacier_FINAL.en_US.srt [3.8 KB] || Anatomy_Glacier_FINAL.en_US.vtt [3.8 KB] || ",
            "hits": 223
        },
        {
            "id": 13679,
            "url": "https://svs.gsfc.nasa.gov/13679/",
            "result_type": "Produced Video",
            "release_date": "2020-08-05T11:00:00-04:00",
            "title": "Greenland's Extreme Melt, One Year Later",
            "description": "Last spring, NASA's Operation IceBridge flew over one of Greenland's earliest melt seasons on record. This year, the melt is progressing more typically, despite warm temperatures in the Arctic. Brooke Medley reflects on the differences between 2019 and 2020 melt in Greenland. || ",
            "hits": 22
        },
        {
            "id": 12977,
            "url": "https://svs.gsfc.nasa.gov/12977/",
            "result_type": "Produced Video",
            "release_date": "2018-09-26T13:00:00-04:00",
            "title": "Mass Balance of Ice Sheets",
            "description": "AntarcticaMusic: \"Distant Echoes,\" Adam Salkeld, Atmosphere Music Ltd. PRS; \"Evolution of Life,\" David Stephen Goldsmith, Atmosphere Music Ltd. PRSComplete transcript available. || antarc_thumb_print.jpg (1024x576) [113.1 KB] || antarc_thumb_searchweb.png (180x320) [88.3 KB] || antarc_thumb_thm.png (80x40) [6.3 KB] || Antarctica_Brunt.mov (1920x1080) [4.1 GB] || Antarctica_Brunt_facebook_720.mp4 (1280x720) [424.3 MB] || Antarctica_Brunt_twitter_720.mp4 (1280x720) [77.5 MB] || Antarctica_Brunt_youtube_1080.mp4 (1920x1080) [571.8 MB] || Antarctica_Brunt_youtube_720.mp4 (1280x720) [552.4 MB] || Antarctica_Brunt_facebook_720.webm (1280x720) [32.9 MB] || Antarctica_icesheet.en_US.srt [6.0 KB] || Antarctica_icesheet.en_US.vtt [6.0 KB] || ",
            "hits": 43
        },
        {
            "id": 12867,
            "url": "https://svs.gsfc.nasa.gov/12867/",
            "result_type": "Produced Video",
            "release_date": "2018-07-19T15:00:00-04:00",
            "title": "Why Won't it Melt? How NASA's Solar Probe will Survive the Sun",
            "description": "Music credit: Cheeky Chappy [Main Track] by Jimmy Kaleth, Ross Andrew McLean from www.killertracks.com This music requires a license for use.Watch this video on the NASA Goddard YouTube channel.Complete transcript available. || meltthumb.jpg (1920x1080) [311.2 KB] || meltthumb_searchweb.png (320x180) [76.6 KB] || meltthumb_thm.png (80x40) [5.4 KB] || 12867WhyWontItMeltV8.mov (1920x1080) [5.4 GB] || 12867WhyWontItMeltV8.webm (1920x1080) [23.3 MB] || 12867WhyWontItMeltV8_appletv.m4v (1280x720) [148.8 MB] || 12867WhyWontItMeltV8_youtube_1080.mp4 (1920x1080) [443.5 MB] || 12867WhyWontItMeltV8_youtube_hq.mov (1920x1080) [1.3 GB] || 12867WhyWontItMeltV8_appletv_subtitles.m4v (1280x720) [148.9 MB] || 12867WhyWontItMeltV8.en_US.srt [4.2 KB] || 12867WhyWontItMeltV8.en_US.vtt [4.2 KB] || 12867WhyWontItMeltV8_ipod_sm.mp4 (320x240) [38.2 MB] || ",
            "hits": 136
        },
        {
            "id": 11991,
            "url": "https://svs.gsfc.nasa.gov/11991/",
            "result_type": "Produced Video",
            "release_date": "2015-09-16T17:00:00-04:00",
            "title": "Ask A Climate Scientist - Thinning Ice Sheets",
            "description": "Dr. Kelly Brunt explains that Greenland's ice sheet is thinning, and while it is still over 10,000 feet thick, the melt water is contributing to sea level rise.For complete transcript, click here. || G2013-077_AACS_Thinning_Ice.jpg (1280x720) [96.0 KB] || poster-G2013-077_AACS_Thinning_Ice_searchweb.png (320x180) [79.8 KB] || G2013-077_AACS_Thinning_Ice_thm.png (80x40) [7.1 KB] || G2013-077_AACS_Thinning_Ice_youtube_hq.mov (1280x720) [235.9 MB] || G2013-077_AACS_Thinning_Ice_appletv.m4v (1280x720) [70.2 MB] || G2013-077_AACS_Thinning_Ice.mpeg (1280x720) [488.6 MB] || G2013-077_AACS_Thinning_Ice_prores.mov (1280x720) [2.0 GB] || G2013-077_AACS_Thinning_Ice_HD.wmv (1280x720) [21.5 MB] || G2013-077_AACS_Thinning_Ice.webm (960x540) [58.2 MB] || G2013-077_AACS_Thinning_Ice_appletv_subtitles.m4v (1280x720) [70.3 MB] || G2013-077_AACS_Thinning_Ice.en_US.srt [2.4 KB] || G2013-077_AACS_Thinning_Ice.en_US.vtt [2.5 KB] || G2013-077_AACS_Thinning_Ice_ipod_sm.mp4 (320x240) [24.3 MB] || ",
            "hits": 129
        },
        {
            "id": 11973,
            "url": "https://svs.gsfc.nasa.gov/11973/",
            "result_type": "Produced Video",
            "release_date": "2015-08-17T18:00:00-04:00",
            "title": "Lakes On A Glacier",
            "description": "A view of Greenland's ice sheet from the NASA/USGS Landsat 8 satellite, narrated by Dr. Allen Pope.  The data enables Dr. Pope to measure the depth of the lakes that form on the surface every summer as the snow and ice melts.  The data in this image are from July 12, 2014, and shows the area just south of the Jakobshavn Glacier.For complete transcript, click here.Watch this video on the NASA Goddard YouTube channel. || G2015-056_Lakes_On_A_Glacier-print.jpg (1024x576) [430.4 KB] || G2015-056_Lakes_On_A_Glacier_MASTER_youtube_hq_searchweb.png (180x320) [71.3 KB] || G2015-056_Lakes_On_A_Glacier_MASTER_youtube_hq_thm.png (80x40) [4.8 KB] || G2015-056_Lakes_On_A_Glacier_MASTER_youtube_1920.mp4 (1920x1080) [132.4 MB] || G2015-056_Lakes_On_A_Glacier_MASTER_youtube_hq.mov (1280x720) [391.1 MB] || G2015-056_Lakes_On_A_Glacier_MASTER_appletv.m4v (1280x720) [78.9 MB] || G2015-056_Lakes_On_A_Glacier_MASTER.mpeg (1280x720) [560.6 MB] || G2015-056_Lakes_On_A_Glacier_MASTER_1280x720.wmv (1280x720) [80.6 MB] || G2015-056_Lakes_On_A_Glacier_MASTER_prores.mov (1280x720) [2.3 GB] || G2015-056_Lakes_On_A_Glacier_MASTER_prores-1920.mov (1920x1080) [4.3 GB] || G2015-056_Lakes_On_A_Glacier_MASTER.webm (960x540) [67.1 MB] || G2015-056_Lakes_On_A_Glacier_MASTER_appletv_subtitles.m4v (1280x720) [79.0 MB] || G2015-056_Lakes_On_A_Glacier-captions.en_US.srt [3.0 KB] || G2015-056_Lakes_On_A_Glacier-captions.en_US.vtt [3.0 KB] || G2015-056_Lakes_On_A_Glacier_MASTER_ipod_sm.mp4 (320x240) [28.0 MB] || ",
            "hits": 29
        },
        {
            "id": 11900,
            "url": "https://svs.gsfc.nasa.gov/11900/",
            "result_type": "Produced Video",
            "release_date": "2015-07-21T13:00:00-04:00",
            "title": "Instagram: Scientists Link Earlier Melting Of Snow To Dark Aerosols",
            "description": "Tiny particles suspended in the air, known as aerosols, can darken snow and ice causing it to absorb more of the sun’s energy. But until recently, scientists rarely considered the effect of all three major types of light-absorbing aerosols together in climate models.In a new study, NASA scientists used a climate model to examine the impact of this snow-darkening phenomenon on Northern Hemisphere snowpacks, including how it affects snow amount and heating on the ground in spring.The study looked at three types of light-absorbing aerosols – dust, black carbon and organic carbon. Black carbon and organic carbon are produced from the burning of fossil fuels, like coal and oil, as well as biofuels and biomass, such as forests.With their snow darkening effect added to NASA’s GEOS-5 climate model, scientists analyzed results from 2002 to 2011, and compared them to model runs done without the aerosols on snow. They found that the aerosols indeed played a role in absorbing more of the sun’s energy. Over broad places in the Northern Hemisphere, the darkened snow caused some surface temperatures to be up to 10 degrees Fahrenheit warmer than it would be if the snow were pristine. As a result, warmer, snow-darkened areas had less snow in spring than they would have had under pristine snow conditions.According to the study, dust’s snow darkening effect significantly contributed to surface warming in Central Asia and the western Himalayas. Black carbon’s snow darkening effect had a larger impact primarily in Europe, the eastern Himalayas and East Asia. It had a smaller impact in North America. Organic carbon’s snow darkening effect was relatively lower but present in regions such as southeastern Siberia, northeastern East Asia and western Canada.“As we add more of these aerosols to the mix, we are potentially increasing our overall impact on Earth’s climate,” said research scientist Teppei Yasunari at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.Research: Impact of snow darkening via dust, black carbon, and organic carbon on boreal spring climate in the Earth systemJournal: Geophysical Research: Atmospheres, June 15, 2015.Link to paper: http://onlinelibrary.wiley.com/doi/10.1002/2014JD022977/fullHere is the YouTube video. || ",
            "hits": 152
        },
        {
            "id": 11818,
            "url": "https://svs.gsfc.nasa.gov/11818/",
            "result_type": "Produced Video",
            "release_date": "2015-03-23T11:00:00-04:00",
            "title": "Wyoming Snowmelt 2013",
            "description": "Images from NASA/USGS Landsat satellites show the snowcover in Wyoming's Fremont Lake Basin throughout 2013.  NASA scientists have used Landsat data from 1972-2013 to determine that the snow is melting 16 days earlier. || Wyoming_Snowmelt_2013_nasaportal_print.jpg (1024x576) [212.1 KB] || Wyoming_Snowmelt_2013_nasaportal_searchweb.png (320x180) [143.5 KB] || Wyoming_Snowmelt_2013_nasaportal_web.png (320x180) [143.5 KB] || Wyoming_Snowmelt_2013_nasaportal_thm.png (80x40) [8.7 KB] || Wyoming_Snowmelt_2013_youtube_hq.mov (1920x1080) [15.1 MB] || Wyoming_Snowmelt_2013_appletv.m4v (960x540) [6.1 MB] || Wyoming_Snowmelt_2013_prores.mov (1280x720) [234.7 MB] || Wyoming_Snowmelt_2013_1280x720.wmv (1280x720) [6.9 MB] || Wyoming_Snowmelt_2013_appletv.webm (960x540) [1.5 MB] || Wyoming_Snowmelt_2013_nasaportal.mov (640x360) [4.5 MB] || Wyoming_Snowmelt_2013_ipod_lg.m4v (640x360) [2.3 MB] || GSFC_20150323_Wyoming_m11818_Snowmelt.en_US.vtt [64 bytes] || Wyoming_Snowmelt_2013_ipod_sm.mp4 (320x240) [1.0 MB] || ",
            "hits": 138
        },
        {
            "id": 4247,
            "url": "https://svs.gsfc.nasa.gov/4247/",
            "result_type": "Visualization",
            "release_date": "2014-12-17T00:00:00-05:00",
            "title": "Greenland Survey Areas",
            "description": "This animation starts with an overview of the Earth looking down upon North America. It then zooms into Greenland taking up most of the frame, and slowly dissolves in the research areas of interest. This animation ends where the following 4 animations pick up, so they can be composited together, if desired. || greenland_all_locs.jpg (1920x1080) [356.3 KB] || greenland_slow.1339_print.jpg (1024x576) [107.2 KB] || greenland_slow.1339_searchweb.png (320x180) [72.8 KB] || greenland_slow.1339_thm.png (80x40) [5.7 KB] || greenland_zoom_in_1080.mp4 (1920x1080) [5.2 MB] || Zoom_in (1920x1080) [32.0 KB] || greenland_zoom_in_1080.webm (1920x1080) [1.3 MB] || ",
            "hits": 20
        },
        {
            "id": 3053,
            "url": "https://svs.gsfc.nasa.gov/3053/",
            "result_type": "Visualization",
            "release_date": "2004-12-01T12:00:00-05:00",
            "title": "Jakobshavn Glacier Calving Front Recession (2001-2003)",
            "description": "Jakobshavn Isbrae holds the record as Greenland's fastest moving glacier and major contributor to the mass balance of the continental ice sheet. Starting in late 2000, following a period of slowing down in the mid 1990s, the glacier showed significant acceleration and nearly doubled its discharge of ice. The following imagery from the Landsat satellite shows the retreat of Jakobshavn's calving front from 2001 to 2003. || ",
            "hits": 154
        },
        {
            "id": 20022,
            "url": "https://svs.gsfc.nasa.gov/20022/",
            "result_type": "Animation",
            "release_date": "2004-02-05T12:00:00-05:00",
            "title": "Ice Albedo: Bright White Reflects Light",
            "description": "This animation provides a close perspective of the relationship between ice and solar reflectivity. As glaciers, the polar caps, and icebergs (shown here) melt, less sunlight gets reflected into space. Instead, the oceans and land absorb the light, thus raising the overall temperature and adding energy to a vicious circle. || ",
            "hits": 430
        }
    ]
}