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        {
            "id": 4204,
            "url": "https://svs.gsfc.nasa.gov/4204/",
            "page_type": "Visualization",
            "title": "Small Multiples of NSIDC North Pole Sea Ice Extent",
            "description": "This is a still image generated from  National Snow and Ice Data Center (NSIDC) north pole sea ice extent images.  These images are arranged in a grid pattern with the years across the top from 1979 to 2014 and the months running down the image from January to December.By glancing at the image, the viewer can quickly see the periods during the year when north pole sea ice extent is at minimum and maximum.  It is also easy to see how the sea ice has changed over the years.  There is no data for December 1987 and January 1988; these dates are left black. || ",
            "release_date": "2014-09-09T00:00:00-04:00",
            "update_date": "2023-05-03T13:50:35.809624-04:00",
            "main_image": {
                "id": 452314,
                "url": "https://svs.gsfc.nasa.gov/vis/a000000/a004200/a004204/arctic_ice_extent_12264x6016_print.jpg",
                "filename": "arctic_ice_extent_12264x6016_print.jpg",
                "media_type": "Image",
                "alt_text": "Monthly sea ice extent arranged in a grid pattern with years running horizontally from 1979 to 2014 and months running vertically from January through December",
                "width": 1024,
                "height": 502,
                "pixels": 514048
            }
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        {
            "id": 11634,
            "url": "https://svs.gsfc.nasa.gov/11634/",
            "page_type": "Produced Video",
            "title": "A Selective History of Arctic Sea Ice Observations",
            "description": "Arctic sea ice has been been the last frontier of the North for thousands of years, turning back seafarers, testing the mettle of explorers, and providing a way of life for people circling the top of the world. This animated timeline provides a quick (and highly selective) ride from the days of early Greek exploration to the dawn of the Space Age to the advanced capabilities we have today. || ",
            "release_date": "2014-09-03T09:00:00-04:00",
            "update_date": "2023-05-03T13:50:37.564919-04:00",
            "main_image": {
                "id": 452290,
                "url": "https://svs.gsfc.nasa.gov/vis/a010000/a011600/a011634/history_sea_ice_part_1_youtube_hq_print.jpg",
                "filename": "history_sea_ice_part_1_youtube_hq_print.jpg",
                "media_type": "Image",
                "alt_text": "For complete transcript, click here.",
                "width": 1024,
                "height": 576,
                "pixels": 589824
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        },
        {
            "id": 3592,
            "url": "https://svs.gsfc.nasa.gov/3592/",
            "page_type": "Visualization",
            "title": "Fall Arctic Sea Ice Thickness Declining Rapidly",
            "description": "Using five years of data from NASA's Ice, Cloud and land Elevation Satellite (ICESat), a team of NASA and university scientists made the first basin-wide estimate of the thickness and volume of the Arctic Ocean ice cover between 2003 and 2008. The scientists found that younger, thinner ice has replaced older, thicker ice as the dominant type over the past five years. Until recently, the majority of Arctic ice survived at least one summer and often several. That balance has now flipped. Seasonal ice, or ice that melts and re-freezes every year, now comprises about 70 percent of the Arctic sea ice in wintertime, up from 40 to 50 percent in the 1980s and 1990s. Thicker ice - surviving two or more years - now comprises just 10 percent of ice cover, down from 30 to 40 percent in years past.Sea ice thickness has been hard to measure directly so scientists have typically used estimates of ice age to approximate thickness. With ICESat, NASA scientists were for the first time able to monitor the ice thickness and volume changes over the entire Arctic Ocean. The Arctic ice cap grows each winter as the sun sets for several months and intense cold sets in. The total volume of winter Arctic ice is equal to the volume of fresh water in Lake Superior and Lake Michigan combined. Some of that ice is naturally pushed out of the Arctic by winds, while much of it melts in place. But not all of the ice in the Arctic melts each summer, and the thicker, older ice that survives one or more summers is more likely to persist through the next summer. This older, thicker ice is declining thinner ice that is more vulnerable to summer melt. Seasonal sea ice usually reaches about 2 meters (6 feet) in thickness, while ice that has lasted through more than one summer averages 3 meters (9 feet), though it can grow much thicker in some locations near the coast. From 2003 to 2008, multi-year ice has thinned by an average of 60 centimeters (2 feet). The total ice volume in winter has decreased by 6,300 cubic kilometers, or 40 percent. The maximum extent of multi-year ice is now one-third of what it was in the 1990s. || ",
            "release_date": "2009-04-05T00:00:00-04:00",
            "update_date": "2023-05-03T13:54:51.195937-04:00",
            "main_image": {
                "id": 499048,
                "url": "https://svs.gsfc.nasa.gov/vis/a000000/a003500/a003592/2008fall.jpg",
                "filename": "2008fall.jpg",
                "media_type": "Image",
                "alt_text": "This sequence shows Arctic sea ice thickness derived from fall campaigns from the ICESat satellite. While the sea ice extent might look similar from year to year this thickness data shows dramatic thinning especially near the North Pole (shown in dark blue). This image was generated with data acquired between Oct 4 - Oct 19, 2008.",
                "width": 3840,
                "height": 2160,
                "pixels": 8294400
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