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        {
            "id": 4484,
            "url": "https://svs.gsfc.nasa.gov/4484/",
            "result_type": "Visualization",
            "release_date": "2016-08-16T00:00:00-04:00",
            "title": "Global Fires 2015-2016 Visualizations",
            "description": "Global Fires 2015-2016, with Dates and Colorbar || global_fires_statelines_0000_print.jpg (1024x576) [73.9 KB] || global_fires_statelines_0000_searchweb.png (320x180) [41.4 KB] || global_fires_statelines_0000_thm.png (80x40) [4.6 KB] || global_fires_statelines (1920x1080) [0 Item(s)] || global_fires_statelines_1080p30.mp4 (1920x1080) [8.5 MB] || global_fires_statelines_1080p30.webm (1920x1080) [2.3 MB] || global_fires_statelines_1080p30.mp4.hwshow [197 bytes] || ",
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        {
            "id": 12330,
            "url": "https://svs.gsfc.nasa.gov/12330/",
            "result_type": "Produced Video",
            "release_date": "2016-07-29T05:00:00-04:00",
            "title": "NASA Sees Intense Fires Around The World",
            "description": "This year’s wildfire season is off to a blazing start. The United States had an early start to the season, with more than 29,000 wildfires burning more than 2.6 million acres of land. The driest season in 14 years has left the southern Amazon primed for heavy wildfire activity as well. The expected wildfire surge in the Amazon this summer is the result of El Niño, a warming of waters in the Pacific Ocean that had major impacts on weather across the United States the first half of 2016. While El Niño has officially ended, we’re still feeling effects through increased wildfire activity. In some parts of the U.S., the fire season is now on average 78 days longer than it was in 1970, according to the U.S. Department of Agriculture. NASA scientists are able to monitor these wildfires better than ever before, providing valuable information that fire managers can use to prepare the public. Using data collected by satellites, planes and on the ground, NASA is tracking wildfires around the world and keeping an eye on the hot, dry conditions that contribute to larger fires. || ",
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        },
        {
            "id": 12325,
            "url": "https://svs.gsfc.nasa.gov/12325/",
            "result_type": "Produced Video",
            "release_date": "2016-07-25T12:00:00-04:00",
            "title": "Wildfires Live Shot July 2016",
            "description": "B-roll that goes along with the following questions:Wildfires have been raging in parts of the US this year. Can you show us the view from space?It’s been an active year around the globe for wildfires. How do fires on the other side of the world affect us?El Nino has dried out the Amazon this year, making it vulnerable to wildfires. What impacts could this have on the Summer Olympics?NASA is doing groundbreaking research around the world to study wildfires. What are we learning?Where can we learn more?Click for NASA's FIRES webpage.Find the latest on Twitter @NASAEarth || 008_B-Roll.00001_print.jpg (1024x576) [85.5 KB] || 008_B-Roll.00001_searchweb.png (320x180) [46.0 KB] || 008_B-Roll.00001_thm.png (80x40) [5.2 KB] || 008_B-Roll.mov (1280x720) [4.3 GB] || 008_B-Roll.mp4 (1280x720) [452.4 MB] || 008_B-Roll.webm (1280x720) [30.5 MB] || ",
            "hits": 26
        },
        {
            "id": 4413,
            "url": "https://svs.gsfc.nasa.gov/4413/",
            "result_type": "Visualization",
            "release_date": "2016-01-07T00:00:00-05:00",
            "title": "Sea Surface Temperature Anomaly and Terrestrial Water Storage Anomaly Comparison",
            "description": "Animation showing Sea Surface Temperature Anomaly (SSTA) and Terrestrial Water Storage Anomaly (TWSA) data from 2002 to 2015 simultaneously. For SSTA data, blues indicate temperatures lower than normal and reds are areas warmer than normal. With this data we can see the comings and goings of El Niño and La Niña across the years. For the TWSA data, browns indicate areas with less ground water than normal and greens are areas with more ground water than normal, which correlates to droughts and floods in these various regions. Furthermore, terrestrial areas that show significant amounts of low water storage are much more sensitive to wildfires. || grace_w_ssta_rob2.4991_print.jpg (1024x576) [133.2 KB] || grace_w_ssta_rob2.4991_searchweb.png (180x320) [91.1 KB] || grace_w_ssta_rob2.4991_thm.png (80x40) [7.7 KB] || grace_w_ssta_rob2_2x_1080p30.mp4 (1920x1080) [41.8 MB] || composite (1920x1080) [0 Item(s)] || robinson_projection (1920x1080) [0 Item(s)] || dates (1920x1080) [0 Item(s)] || grace_w_ssta_rob2_2x_1080p30.webm (1920x1080) [9.8 MB] || ",
            "hits": 16
        },
        {
            "id": 4415,
            "url": "https://svs.gsfc.nasa.gov/4415/",
            "result_type": "Visualization",
            "release_date": "2016-01-06T00:00:00-05:00",
            "title": "Terrestrial Water Storage Anomaly 2002 - 2015",
            "description": "Animation showing Terrestrial Water Storage Anomaly (TWSA) data from 2002 to 2015. Browns indicate areas with less ground water than normal and greens are areas with more ground water than normal, which correlates to droughts and floods in these various regions.This video is also available on our YouTube channel. || grace_anom_comp_v2.4991_print.jpg (1024x576) [124.4 KB] || grace_anom_comp_v2.4991_searchweb.png (320x180) [70.7 KB] || grace_anom_comp_v2.4991_thm.png (80x40) [6.3 KB] || grace_anom_comp_v2_2x_1080p30.mp4 (1920x1080) [25.8 MB] || grace_anom_comp_v2_2x_1080p30.webm (1920x1080) [8.7 MB] || composite (1920x1080) [0 Item(s)] || robinson_projection (1920x1080) [0 Item(s)] || dates (1920x1080) [0 Item(s)] || grace_anom_comp_v2_2x_1080p30.mp4.hwshow [195 bytes] || ",
            "hits": 59
        },
        {
            "id": 11899,
            "url": "https://svs.gsfc.nasa.gov/11899/",
            "result_type": "Produced Video",
            "release_date": "2015-07-21T13:00:00-04:00",
            "title": "Scientists Link Earlier Melting Of Snow To Dark Aerosols",
            "description": "Tiny particles suspended in the air, known as aerosols, can darken snow and ice causing it to absorb more of the sun’s energy. But until recently, scientists rarely considered the effect of all three major types of light-absorbing aerosols together in climate models.In a new study, NASA scientists used a climate model to examine the impact of this snow-darkening phenomenon on Northern Hemisphere snowpacks, including how it affects snow amount and heating on the ground in spring.The study looked at three types of light-absorbing aerosols – dust, black carbon and organic carbon. Black carbon and organic carbon are produced from the burning of fossil fuels, like coal and oil, as well as biofuels and biomass, such as forests.With their snow darkening effect added to NASA’s GEOS-5 climate model, scientists analyzed results from 2002 to 2011, and compared them to model runs done without the aerosols on snow. They found that the aerosols indeed played a role in absorbing more of the sun’s energy. Over broad places in the Northern Hemisphere, the darkened snow caused some surface temperatures to be up to 10 degrees Fahrenheit warmer than it would be if the snow were pristine. As a result, warmer, snow-darkened areas had less snow in spring than they would have had under pristine snow conditions.According to the study, dust’s snow darkening effect significantly contributed to surface warming in Central Asia and the western Himalayas. Black carbon’s snow darkening effect had a larger impact primarily in Europe, the eastern Himalayas and East Asia. It had a smaller impact in North America. Organic carbon’s snow darkening effect was relatively lower but present in regions such as southeastern Siberia, northeastern East Asia and western Canada.“As we add more of these aerosols to the mix, we are potentially increasing our overall impact on Earth’s climate,” said research scientist Teppei Yasunari at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.Research: Impact of snow darkening via dust, black carbon, and organic carbon on boreal spring climate in the Earth systemJournal: Geophysical Research: Atmospheres, June 15, 2015.Link to paper: http://onlinelibrary.wiley.com/doi/10.1002/2014JD022977/fullHere is the YouTube video. || ",
            "hits": 73
        },
        {
            "id": 11900,
            "url": "https://svs.gsfc.nasa.gov/11900/",
            "result_type": "Produced Video",
            "release_date": "2015-07-21T13:00:00-04:00",
            "title": "Instagram: Scientists Link Earlier Melting Of Snow To Dark Aerosols",
            "description": "Tiny particles suspended in the air, known as aerosols, can darken snow and ice causing it to absorb more of the sun’s energy. But until recently, scientists rarely considered the effect of all three major types of light-absorbing aerosols together in climate models.In a new study, NASA scientists used a climate model to examine the impact of this snow-darkening phenomenon on Northern Hemisphere snowpacks, including how it affects snow amount and heating on the ground in spring.The study looked at three types of light-absorbing aerosols – dust, black carbon and organic carbon. Black carbon and organic carbon are produced from the burning of fossil fuels, like coal and oil, as well as biofuels and biomass, such as forests.With their snow darkening effect added to NASA’s GEOS-5 climate model, scientists analyzed results from 2002 to 2011, and compared them to model runs done without the aerosols on snow. They found that the aerosols indeed played a role in absorbing more of the sun’s energy. Over broad places in the Northern Hemisphere, the darkened snow caused some surface temperatures to be up to 10 degrees Fahrenheit warmer than it would be if the snow were pristine. As a result, warmer, snow-darkened areas had less snow in spring than they would have had under pristine snow conditions.According to the study, dust’s snow darkening effect significantly contributed to surface warming in Central Asia and the western Himalayas. Black carbon’s snow darkening effect had a larger impact primarily in Europe, the eastern Himalayas and East Asia. It had a smaller impact in North America. Organic carbon’s snow darkening effect was relatively lower but present in regions such as southeastern Siberia, northeastern East Asia and western Canada.“As we add more of these aerosols to the mix, we are potentially increasing our overall impact on Earth’s climate,” said research scientist Teppei Yasunari at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.Research: Impact of snow darkening via dust, black carbon, and organic carbon on boreal spring climate in the Earth systemJournal: Geophysical Research: Atmospheres, June 15, 2015.Link to paper: http://onlinelibrary.wiley.com/doi/10.1002/2014JD022977/fullHere is the YouTube video. || ",
            "hits": 35
        }
    ]
}