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    "results": [
        {
            "id": 5583,
            "url": "https://svs.gsfc.nasa.gov/5583/",
            "result_type": "Visualization",
            "release_date": "2025-09-17T13:00:00-04:00",
            "title": "Arctic Sea Ice Minimum 2025",
            "description": "Animation of Arctic sea ice from its maximum extent, March 22 2025, to its minimum, September 10, 2025, 4K version || sea_ice_2025_min_2160p60.2820_print.jpg (1024x576) [154.9 KB] || sea_ice_2025_min_2160p60.2820_searchweb.png (320x180) [74.1 KB] || sea_ice_2025_min_2160p60.2820_thm.png (80x40) [6.0 KB] || 3840x2160_16x9_60p (3840x2160) [3200 Item(s)] || sea_ice_2025_min_2160p60_p60.mp4 (3840x2160) [107.4 MB] || sea_ice_2025_min_2160p60_p60.mp4.hwshow [194 bytes] || ",
            "hits": 787
        },
        {
            "id": 5382,
            "url": "https://svs.gsfc.nasa.gov/5382/",
            "result_type": "Visualization",
            "release_date": "2024-09-24T13:00:00-04:00",
            "title": "Arctic Sea Ice Minimum 2024",
            "description": "Animation of Arctic sea ice maximum extent, March 14 2024, to its minimum, September 11, 2024 || sea_ice_2024_min_2160p60.2608_print.jpg (1024x576) [152.6 KB] || sea_ice_2024_min_2160p60.2608_searchweb.png (320x180) [74.6 KB] || sea_ice_2024_min_2160p60.2608_thm.png (80x40) [6.0 KB] || sea_ice_2024_min_1080p60.mp4 (1920x1080) [38.2 MB] || sea_ice_min_2024 [0 Item(s)] || sea_ice_2024_min_2160p60.mp4 (3840x2160) [106.6 MB] || antarctic_arctic_seaice_comp_5x3.hwshow || ",
            "hits": 329
        },
        {
            "id": 5162,
            "url": "https://svs.gsfc.nasa.gov/5162/",
            "result_type": "Visualization",
            "release_date": "2023-09-25T13:00:00-04:00",
            "title": "Arctic Sea Ice Minimum 2023",
            "description": "Animation of Arctic sea ice maximum extent, March 6 2023, to its minimum, September 19, 2023 || arctic_sea_ice_2023_min_2160p60.2820_print.jpg (1024x576) [138.6 KB] || arctic_sea_ice_min_2023 (3840x2160) [0 Item(s)] || arctic_sea_ice_2023_min_2160p60_p60.mp4 (3840x2160) [107.4 MB] || ",
            "hits": 160
        },
        {
            "id": 5030,
            "url": "https://svs.gsfc.nasa.gov/5030/",
            "result_type": "Visualization",
            "release_date": "2022-09-22T13:00:00-04:00",
            "title": "Arctic Sea Ice Minimum 2022",
            "description": "Arctic Sea Ice Minimum 2022, Animation || sea_ice_2022_min_1080p60.03100_print.jpg (1024x576) [125.6 KB] || sea_ice_2022_min_1080p60.03100_searchweb.png (180x320) [71.7 KB] || sea_ice_2022_min_1080p60.03100_thm.png (80x40) [6.2 KB] || full (1920x1080) [0 Item(s)] || sea_ice_2022_min_1080p60.mp4 (1920x1080) [31.1 MB] || sea_ice_2022_min_1080p60.webm (1920x1080) [7.1 MB] || sea_ice_2022_min_1080p60.hwshow [89 bytes] || ",
            "hits": 97
        },
        {
            "id": 13474,
            "url": "https://svs.gsfc.nasa.gov/13474/",
            "result_type": "Produced Video",
            "release_date": "2019-12-09T15:00:00-05:00",
            "title": "Operation IceBridge - Western Greenland",
            "description": "NASA’s Operation IceBridge images Earth’s polar ice in unprecedented detail to better understand processes that connect the polar regions with the global climate system. IceBridge utilizes a highly specialized fleet of research aircraft and the most sophisticated suite of innovative science instruments ever assembled to characterize annual changes in thickness of sea ice, glaciers, and ice sheets. In addition, IceBridge collects critical data used to predict the response of earth’s polar ice to climate change and resulting sea-level rise.In 2019, IceBridge was based out of Kangerlussuaq in western Greenland, surveying both sea ice and land ice. Flight lines include survey lines over the Jakobshavn and Kangerlussuaq glaciers, as well as surveyed several IceSat2 ground tracks in southern Greenland. The flights also revealed a startling amount of early spring melt ponds on Greenland's ice sheet. || ",
            "hits": 18
        },
        {
            "id": 13434,
            "url": "https://svs.gsfc.nasa.gov/13434/",
            "result_type": "Produced Video",
            "release_date": "2019-12-09T14:00:00-05:00",
            "title": "Operation IceBridge - Thule, Greenland Landscape",
            "description": "Thule, Greenland has been one of the major hubs of Operation IceBridge since the mission began in 2009. The Thule Air Base, located 750 miles north of the Arctic circle, has been a critical hub of IceBridge Arctic flights during the course of the mission. || ",
            "hits": 67
        },
        {
            "id": 13471,
            "url": "https://svs.gsfc.nasa.gov/13471/",
            "result_type": "Produced Video",
            "release_date": "2019-12-09T14:00:00-05:00",
            "title": "Operation IceBridge - Icebergs",
            "description": "Icebergs start as land ice—snow that has accumulated on land and, over the course of many years, has been compacted into ice. When this glacial ice flows downstream and reaches the sea, cracks in the ice are widened as warm water and air melt the ice from below and above, respectively. When these cracks become large enough, pieces break off like fingernail clippings and drift into the water as icebergs. || ",
            "hits": 25
        },
        {
            "id": 13475,
            "url": "https://svs.gsfc.nasa.gov/13475/",
            "result_type": "Produced Video",
            "release_date": "2019-12-09T14:00:00-05:00",
            "title": "Operation IceBridge - Greenland Sea Ice",
            "description": "Arctic sea ice occupies an ocean basin mostly enclosed by land. Because there is no landmass at the North Pole, sea ice extends all the way to the pole, making the ice subject to the most extreme oscillations between wintertime darkness and summertime sunlight. Likewise, because the ocean basin is surrounded by land, ice has less freedom of movement to drift into lower latitudes and melt.Arctic sea ice generally reaches its maximum extent each March and its minimum extent each September. || ",
            "hits": 33
        },
        {
            "id": 13478,
            "url": "https://svs.gsfc.nasa.gov/13478/",
            "result_type": "Produced Video",
            "release_date": "2019-12-09T14:00:00-05:00",
            "title": "Operation IceBridge - Thule Ice Sheet Scenics",
            "description": "Frozen sea ice outside of the Thule Air Base in Greenland provided project scientists a chance to get up close to locked icebergs and other features. || ",
            "hits": 31
        },
        {
            "id": 13309,
            "url": "https://svs.gsfc.nasa.gov/13309/",
            "result_type": "Produced Video",
            "release_date": "2019-09-23T13:00:00-04:00",
            "title": "Arctic Sea Ice Reaches 2019 Minimum Extent",
            "description": "Music: Hiraeth by Anthony Edwin Phillips [PRS], James Edward CollinsComplete transcript available. || Arctic_Min_2019_Thumbnail_LKW.png (1920x1080) [2.2 MB] || Arctic_Min_2019_Thumbnail_LKW_print.jpg (1024x576) [102.3 KB] || Arctic_Min_2019_Thumbnail_LKW_searchweb.png (320x180) [88.1 KB] || Arctic_Min_2019_Thumbnail_LKW_thm.png (80x40) [6.9 KB] || Arctic_Min_2019_LKW.mov (1920x1080) [3.8 GB] || Arctic_Min_2019_LKW.webm (1920x1080) [19.9 MB] || Arctic_Min_2019_LKW.mp4 (1920x1080) [182.4 MB] || Arctic_Min_2019_LKW.en_US.srt [3.4 KB] || Arctic_Min_2019_LKW.en_US.vtt [3.3 KB] || ",
            "hits": 102
        },
        {
            "id": 4616,
            "url": "https://svs.gsfc.nasa.gov/4616/",
            "result_type": "Visualization",
            "release_date": "2018-03-13T00:00:00-04:00",
            "title": "Disappearing Ice",
            "description": "This visualization begins by showing the dynamic beauty of the Arctic sea ice as it responds to winds and ocean currents.  Research into the behavior of the Arctic sea ice for the last 30 years has led to a deeper understanding of how this ice survives from year to year.  In the animation that follows,  age of the sea ice is visible, showing the younger ice in darker shades of blue and the oldest ice in brighter white.  This visual representation of the ice age clearly shows how the quantity of older and thicker ice has changed between 1984 and 2016.Complete transcript available.This video is also available on our YouTube channel. || Arctic_Sea_Ice_Age.6140_print.jpg (1024x576) [145.3 KB] || Arctic_Sea_Ice_Age.6140_searchweb.png (320x180) [69.8 KB] || Arctic_Sea_Ice_Age.6140_thm.png (80x40) [6.0 KB] || Arctic_Sea_Ice_Age_rev1_1080p30_wAudio.webm (1920x1080) [27.2 MB] || Arctic_Sea_Ice_Age_rev1_1080p30_wAudio.mp4 (1920x1080) [183.5 MB] || SeaIceAge_comp_final (3840x2160) [0 Item(s)] || a004616_captions.en_US.srt [3.9 KB] || a004616_captions.en_US.vtt [3.9 KB] || Disappearing_Ice.aif [38.1 MB] || Arctic_Sea_Ice_Age_rev1.2160p30_wAudio.mp4 (3840x2160) [258.5 MB] || Arctic_Sea_Ice_Age_YTube.2160p30_wAudio.mp4 (3840x2160) [978.3 MB] || Final_seaIceAge_Prores_withAudio.mov (3840x2160) [14.3 GB] || Arctic_Sea_Ice_Age_rev1_1080p30_wAudio.mp4.hwshow [204 bytes] || ",
            "hits": 326
        },
        {
            "id": 12421,
            "url": "https://svs.gsfc.nasa.gov/12421/",
            "result_type": "Produced Video",
            "release_date": "2016-11-14T12:30:00-05:00",
            "title": "Warm Winter Cyclone Damaged Arctic Sea Ice Pack",
            "description": "A large cyclone that crossed the Arctic in December 2015 brought so much heat and humidity to this otherwise frigid environment that it thinned and shrunk the sea ice cover during a time when the ice should have been growing.The visualization elements are available here. || ",
            "hits": 22
        },
        {
            "id": 4520,
            "url": "https://svs.gsfc.nasa.gov/4520/",
            "result_type": "Visualization",
            "release_date": "2016-11-10T00:00:00-05:00",
            "title": "Early 2016 Winter Storm Melts Arctic Sea Ice",
            "description": "This visualization starts with a global view of the Western hemisphere. The viewer then moves in over the arctic on December 27, 2015. Winds and air temperature fade in as time moves forward. A low pressure system then moves in pushing warm air ahead of it. The warm air moves over the Arctic sea ice, contributing to dramatic melting of the sea ice concentration in this region. || arctic_cyclone_comp7.0710_print.jpg (1024x576) [214.4 KB] || arctic_cyclone_comp7.0710_searchweb.png (320x180) [121.2 KB] || arctic_cyclone_comp7.0710_thm.png (80x40) [7.4 KB] || arctic_cyclone_comp7_1080p30.mp4 (1920x1080) [45.6 MB] || arctic_cyclone_comp7_720p30.mp4 (1280x720) [28.2 MB] || comp (1920x1080) [128.0 KB] || date_overlay (1920x1080) [128.0 KB] || low_pressure_overlay (1920x1080) [128.0 KB] || wind_overlay (1920x1080) [64.0 KB] || temperature_overlay (1920x1080) [128.0 KB] || country_names_overlay (1920x1080) [64.0 KB] || earth_with_sea_ice_background (1920x1080) [64.0 KB] || arctic_cyclone_comp7_1080p30.webm (1920x1080) [4.9 MB] || arctic_cyclone_comp7_360p30.mp4 (640x360) [11.1 MB] || ",
            "hits": 28
        },
        {
            "id": 4245,
            "url": "https://svs.gsfc.nasa.gov/4245/",
            "result_type": "Visualization",
            "release_date": "2014-12-17T13:00:00-05:00",
            "title": "Link between Sea-Ice Fraction and Absorbed Solar Radiation over the Arctic Ocean",
            "description": "NASA satellite instruments have observed a marked increase in solar radiation absorbed in the Arctic since the year 2000 – a trend that aligns with the drastic decrease in Arctic sea ice during the same period.  This visual shows the Arctic Sea Ice Change and the corresponding Absorbed Solar Radiation Change during June, July, and August from 2000 through 2014.This video is also available on our YouTube channel. || seaice_solarAbsorption_0344_print.jpg (1024x576) [117.1 KB] || SeaIceSolarAbsorptionChange.webm (1920x1080) [1.2 MB] || 1920x1080_16x9_60p (1920x1080) [0 Item(s)] || SeaIceSolarAbsorptionChange.mp4 (1920x1080) [12.1 MB] || composite (1920x1080) [0 Item(s)] || source (1920x1080) [0 Item(s)] || SeaIceSolarAbsorptionChange.m4v (640x360) [2.1 MB] || ",
            "hits": 159
        },
        {
            "id": 11653,
            "url": "https://svs.gsfc.nasa.gov/11653/",
            "result_type": "Produced Video",
            "release_date": "2014-09-22T06:00:00-04:00",
            "title": "Instagram: Arctic Sea Ice Minimum 2014",
            "description": "Sea ice acts as an air conditioner for the planet, reflecting energy from the Sun. On September 17, the Arctic sea ice reached its minimum extent for 2014. At 1.94 million square miles (5.02 million square kilometers), it’s the sixth lowest extent of the satellite record.  With warmer temperatures and thinner, less resilient ice, the Arctic sea ice is on a downward trend. || ",
            "hits": 27
        },
        {
            "id": 11654,
            "url": "https://svs.gsfc.nasa.gov/11654/",
            "result_type": "Produced Video",
            "release_date": "2014-09-22T06:00:00-04:00",
            "title": "Arctic Sea Ice Reaches 2014 Minimum Extent",
            "description": "Sea ice acts as an air conditioner for the planet, reflecting energy from the Sun. On September 17, the Arctic Sea ice reached its minimum extent for 2014  — at 1.94 million square miles (5.02 million square kilometers), it’s the sixth lowest extent of the satellite record.  With warmer temperatures and thinner, less resilient ice, the Arctic sea ice is on a downward trend.Here is the YouTube video. || ",
            "hits": 32
        },
        {
            "id": 11627,
            "url": "https://svs.gsfc.nasa.gov/11627/",
            "result_type": "Produced Video",
            "release_date": "2014-08-22T14:55:00-04:00",
            "title": "Arctic Sea Ice Live Shot 2014",
            "description": "Canned Interviews and B-roll for Arctic Sea Ice 2014 live shot campaign. || ",
            "hits": 20
        },
        {
            "id": 3592,
            "url": "https://svs.gsfc.nasa.gov/3592/",
            "result_type": "Visualization",
            "release_date": "2009-04-05T00:00:00-04:00",
            "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. || ",
            "hits": 47
        },
        {
            "id": 3589,
            "url": "https://svs.gsfc.nasa.gov/3589/",
            "result_type": "Visualization",
            "release_date": "2009-03-05T00:00:00-05:00",
            "title": "Winter 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. || ",
            "hits": 246
        },
        {
            "id": 3593,
            "url": "https://svs.gsfc.nasa.gov/3593/",
            "result_type": "Visualization",
            "release_date": "2009-03-05T00:00:00-05:00",
            "title": "Fall and Winter 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. || ",
            "hits": 146
        }
    ]
}