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    "funding_sources": [
        "ESE Informal Education"
    ],
    "credits": [
        {
            "role": "Animator",
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                    "name": "Lori Perkins",
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        {
            "name": "L1B Global Elevation Data (GLA06)",
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            "name": "MODIS Mosaic of Antarctica (MOA) Image Map",
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            "type": "Mosaic",
            "organizations": [
                "National Snow and Ice Data Center (NSIDC) and the University of New Hampshire"
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            "description": "Staff from the National Snow and Ice Data Center (NSIDC) and the University of New Hampshire have assembled two digital image maps of surface morphology and optical snow grain size that cover the Antarctic continent and its surrounding islands. The MODIS Mosaic of Antarctica (MOA) image maps are derived from composites of 260 MODIS (Moderate-resolution Imaging Spectroradiometer) orbit swaths acquired between 20 November 2003 and 29 February 2004. The MOA provides a cloud-free view of the ice sheet, ice shelves, and land surfaces, and a quantitative measure of optical snow grain size for snow- or ice-covered areas. All land areas larger than a few hundred meters that are south of 60° S are included in the mosaic, as well as persistent fast ice regions and some grounded icebergs present near the coast in the 2003-2004 austral summer. The MOA surface morphology image map is derived from digitally processed MODIS Band 1 data. The optical snow grain size image is compiled using a normalized ratio of atmospherically corrected, calibrated band radiance data from Bands 1 and 2.",
            "credit": "",
            "url": "http://nsidc.org/data/nsidc-0280.html",
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        "Cryosphere",
        "Earth Science",
        "Glaciers/Ice Sheets"
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    "related": [
        {
            "id": 10723,
            "url": "https://svs.gsfc.nasa.gov/10723/",
            "page_type": "Produced Video",
            "title": "Base Camp: West Antarctica",
            "description": "Stretching off the edge of the continent, 1,400 miles west of Antarctica's McMurdo Station, is Pine Island Glacier (PIG)—a massive river of ice 190 miles wide and 30 miles long that satellite measurements reveal is rapidly shrinking in size. Much of the glacier rests on a bed below sea level and global sea levels could increase by three feet or more if the glacier melted completely. The rate of ice loss on the glacier has increased rapidly in recent years, and scientists believe shifting warm water rising from the adjacent deep ocean and circulating in the surrounding Amundsen Sea are rapidly melting the underside of the glacier's floating edge—the ice shelf. To be certain requires measurements taken beneath this floating ice. That's where NASA polar scientist Robert Bindschadler comes in. In 2008, Bindschadler led an expedition to the remote ice shelf by plane, but the dangers of landing on the crevassed surface prevented his team from collecting data. This fall Bindschadler will return via helicopter. The plan on arrival: drill 1,640 feet below the surface and deploy a specially designed instrument that will start continuous measurements of the shifting ocean waters beneath the glacier. || ",
            "release_date": "2011-02-14T00:00:00-05:00",
            "update_date": "2023-05-03T13:53:52.980779-04:00",
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                "media_type": "Image",
                "alt_text": "Polar scientists will return to Antarctica in fall 2011 to monitor one of the world's fastest moving glaciers.",
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                "pixels": 589824
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    ],
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