{
    "count": 2,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 4688,
            "url": "https://svs.gsfc.nasa.gov/4688/",
            "result_type": "Visualization",
            "release_date": "2019-03-25T12:00:00-04:00",
            "title": "Jakobshavn's Interrupted Thinning Explained",
            "description": "This visualization shows a variety of data from the oceans and ice to help explain why the Jakobshavn glacier grew thicker and advanced between 2016 and 2017.This video is also available on our YouTube channel. || Jakob_comp_final.3462_print.jpg (1024x576) [311.2 KB] || Jakob_comp_final_1080p30.webmhd.webm (1080x606) [30.5 MB] || Jakobshavn_1080p30.webm (1920x1080) [15.9 MB] || final_composite (1920x1080) [0 Item(s)] || Jakobshavn_720p30.mp4 (1280x720) [110.0 MB] || Jakobshavn_1080p30.mp4 (1920x1080) [201.3 MB] || Jakobshavn_youtube_1080p.mp4 (1920x1080) [241.5 MB] || captions_silent.26988.en_US.srt [43 bytes] || captions_silent.26988.en_US.vtt [56 bytes] || Jakobshavn_1080p30.mp4.hwshow [184 bytes] || ",
            "hits": 46
        },
        {
            "id": 4691,
            "url": "https://svs.gsfc.nasa.gov/4691/",
            "result_type": "Visualization",
            "release_date": "2019-02-11T11:00:00-05:00",
            "title": "A possible second large subglacial impact crater in northwest Greenland",
            "description": "As this visualization draws near to the northwest coast of Greenland where the Hiawatha Glacier is located, the ice sheet is cut away to show the topography of Greenland's bedrock lying beneath the ice sheet at 20x vertical exaggeration. The Hiawatha crater is clearly visible in the topography. Farther inland another, subtler circular depression can be seen. The edge picks of this depression are shown as vertical bars, while potential central peaks are marked by orange pyramids. As we rotate around the depression, the location of the best-fit circle to the edge picks appears and that circle's center is marked with an \"X\". This circle matches well with both the edge of the bedrock depression and also the residual slope of the ice surface as it flows over this depression (not shown), strongly supporting the inference that this depression is another large impact crater.This video is also available on our YouTube channel. || C2_Crater_4k.1524_print.jpg (1024x576) [111.8 KB] || C2_Crater_4k.1524_searchweb.png (320x180) [88.0 KB] || C2_Crater_4k.1524_thm.png (80x40) [7.2 KB] || C2_Crater_4k_1080p30_low.mp4 (1920x1080) [23.1 MB] || C2_Crater_4k_1080p30.mp4 (1920x1080) [47.8 MB] || C2_Crater_4k_1080p30.webmhd.webm (1080x606) [11.6 MB] || C2_Crater_4k_2160p30_low.mp4 (3840x2160) [48.2 MB] || C2_Crater_4k_2160p30.mp4 (3840x2160) [85.9 MB] || 3840x2160_16x9_30p (3840x2160) [0 Item(s)] || captions_silent.24907.en_US.srt [43 bytes] || captions_silent.24907.en_US.vtt [56 bytes] || C2_Crater_4K_YouTube.mp4 (3840x2160) [245.6 MB] || C2_Crater_4K_ProRes.mov (3840x2160) [3.4 GB] || C2_Crater_4k_1080p30_low.mp4.hwshow [190 bytes] || ",
            "hits": 26
        }
    ]
}