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    "title": "Ice Flow toward the Petermann Glacier, Greenland",
    "description": "Greenland looks like a big pile of snow seen from space using a regular camera. But satellite radar interferometry helps us detect the motion of ice beneath the snow. Ice starts flowing from the flanks of topographic divides in the interior of the island, and increases in speed toward the coastline where it is channelized along a set of narrow, powerful outlet glaciers. In the east, these glaciers make their sinuous way through complex terrain at low speed. They form long floating extensions that deform slowly in the cold north. As we move toward sectors of higher snowfall in the northwest and centre west, ice flow speeds increase by nearly a factor 10, with many, smaller glaciers flowing straight down to the coastline at several kilometers per year.This complete description of ice motion was only made possible from the coordinated effort of four space agencies: the Japanese Space Agency, the Canadian Space Agency, the European Space Agency, and NASA's Jet Propulsion Laboratory. The data will help scientists improve their understanding of the dynamics of ice in Greenland and in projecting how the Greenland Ice Sheet will respond to climate change in the decades and centuries to come. || ",
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            "description": "Greenland looks like a big pile of snow seen from space using a regular camera. But satellite radar interferometry helps us detect the motion of ice beneath the snow. Ice starts flowing from the flanks of topographic divides in the interior of the island, and increases in speed toward the coastline where it is channelized along a set of narrow, powerful outlet glaciers. In the east, these glaciers make their sinuous way through complex terrain at low speed. They form long floating extensions that deform slowly in the cold north. As we move toward sectors of higher snowfall in the northwest and centre west, ice flow speeds increase by nearly a factor 10, with many, smaller glaciers flowing straight down to the coastline at several kilometers per year.<p><p>This complete description of ice motion was only made possible from the coordinated effort of four space agencies: the Japanese Space Agency, the Canadian Space Agency, the European Space Agency, and NASA's Jet Propulsion Laboratory. The data will help scientists improve their understanding of the dynamics of ice in Greenland and in projecting how the Greenland Ice Sheet will respond to climate change in the decades and centuries to come.",
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        "Earth Science",
        "Glacier Motion/Ice Sheet Motion",
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        {
            "id": 11153,
            "url": "https://svs.gsfc.nasa.gov/11153/",
            "page_type": "Produced Video",
            "title": "Iceberg Maker",
            "description": "Petermann Glacier has earned a reputation in recent years for birthing \"ice islands\"—icebergs so big they get their own designation. Petermann's ice tongue, the portion of the glacier connected to land but still floating, snakes through a fjord for more than 40 miles, making it the largest of its kind north of the equator. Stressed by ice flow behind it, grinding against a rocky coastline, the front of this tongue has set free island-sized icebergs in the summers of both 2010 and 2012. While this shedding of ice is a normal process, NASA scientists are keeping close watch on how Greenland's ice responds to warming air and ocean temperatures, as the ice sheet has shown rapid changes in the past decade. Watch the visualization to see a sped-up animation of how Petermann Glacier empties ice from Greenland's interior to open water. || ",
            "release_date": "2013-01-08T00:00:00-05:00",
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                "media_type": "Image",
                "alt_text": "Flowing toward the rocky strait that separates Greenland and Canada is the Northern Hemisphere's largest floating glacier.",
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