{
    "count": 9,
    "next": null,
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    "results": [
        {
            "id": 12355,
            "url": "https://svs.gsfc.nasa.gov/12355/",
            "result_type": "Produced Video",
            "release_date": "2017-05-18T11:00:00-04:00",
            "title": "ATom Postcard - Azore Islands to Kangerlussuaq",
            "description": "Atmospheric scientists Bernadett Weinzierl of the University of Vienna, Paul Newman of Goddard Space Flight Center, and Róisín Commane of Harvard University sent back a video postcard from the last three legs of the Atmospheric Tomography, or ATom mission. Departing Ascension Island in the tropics, the science team traveled up the Atlantic to Terceira Island in the Azores off the coast of Portugal, and then back to the Arctic by way of Kangerlussuaq, Greenland. Finally the team crossed North America to return home to Palmdale, California. || Screen_Shot_2016-08-31_at_11.31.03_AM.png (1911x1072) [1.9 MB] || Screen_Shot_2016-08-31_at_11.31.03_AM_print.jpg (1024x574) [126.6 KB] || Screen_Shot_2016-08-31_at_11.31.03_AM_searchweb.png (320x180) [88.1 KB] || Screen_Shot_2016-08-31_at_11.31.03_AM_thm.png (80x40) [7.1 KB] || ATom_Postcard_-_Azores_to_Kangerlussuaq.webm (1920x1080) [37.1 MB] || ATom_Postcard_-_Azores_to_Kangerlussuaq.en_US.srt [6.6 KB] || ATom_Postcard_-_Azores_to_Kangerlussuaq.en_US.vtt [6.3 KB] || ATom_Postcard_-_Azores_to_Kangerlussuaq.mp4 (1920x1080) [520.1 MB] || ATom_Postcard_-_Azores_to_Kangerlussuaq.mov (1920x1080) [8.8 GB] || ",
            "hits": 21
        },
        {
            "id": 12354,
            "url": "https://svs.gsfc.nasa.gov/12354/",
            "result_type": "Produced Video",
            "release_date": "2016-08-29T22:00:00-04:00",
            "title": "ATom Postcard - Punta Arenas to Ascension Island",
            "description": "Postcard #3Atmospheric scientist Róisín Commane and Principal Investigator Steven Wofsy both of Harvard University sent back a video postcard from the Atlantic legs of the Atmospheric Tomography, or ATom mission. The science team left Christchurch New Zealand and traveled past Antarctica to Punta Arenas, Chile at the bottom of the world. Then they went up the Atlantic Ocean to Ascension Island, just south of the equator. || Screen_Shot_2016-08-29_at_2.44.38_AM_print.jpg (1024x574) [143.5 KB] || Screen_Shot_2016-08-29_at_2.44.38_AM.png (2154x1209) [3.4 MB] || Screen_Shot_2016-08-29_at_2.44.38_AM_searchweb.png (320x180) [98.6 KB] || Screen_Shot_2016-08-29_at_2.44.38_AM_thm.png (80x40) [7.1 KB] || ATom_Postcard_3_-_Punta_Arenas_to_Ascension.webm (1920x1080) [23.2 MB] || ATom_Postcard_3_-_Punta_Arenas_to_Ascension.en_US.srt [4.2 KB] || ATom_Postcard_3_-_Punta_Arenas_to_Ascension.en_US.vtt [4.0 KB] || ATom_Postcard_3_-_Punta_Arenas_to_Ascension.mov (1920x1080) [5.5 GB] || ",
            "hits": 16
        },
        {
            "id": 12342,
            "url": "https://svs.gsfc.nasa.gov/12342/",
            "result_type": "Produced Video",
            "release_date": "2016-08-16T18:00:00-04:00",
            "title": "ATom Postcard - Samoa to New Zealand",
            "description": "Principal Investigator Steven Wofsy of Harvard University and atmospheric scientist Paul Newman of NASA’s Goddard Space Flight Center sent back a video postcard of the second two legs of the Atmospheric Tomography, or ATom mission. They and the science team traversed the tropical Pacific from Kona, Hawaii to Pago Pago, American Samoa, and then to Christchurch, New Zealand. || Screen_Shot_2016-08-16_at_6.11.17_PM_print.jpg (1024x574) [203.0 KB] || Screen_Shot_2016-08-16_at_6.11.17_PM.png (2305x1293) [4.5 MB] || Screen_Shot_2016-08-16_at_6.11.17_PM_searchweb.png (320x180) [124.7 KB] || Screen_Shot_2016-08-16_at_6.11.17_PM_thm.png (80x40) [8.3 KB] || Samoa_to_New_Zealand.webm (1280x720) [24.5 MB] || Samoa_to_New_Zealand.en_US.srt [4.7 KB] || Samoa_to_New_Zealand.en_US.vtt [4.5 KB] || Samoa_to_New_Zealand.mp4 (1280x720) [245.1 MB] || Samoa_to_New_Zeland.mov (1280x720) [3.1 GB] || ",
            "hits": 21
        },
        {
            "id": 12337,
            "url": "https://svs.gsfc.nasa.gov/12337/",
            "result_type": "Produced Video",
            "release_date": "2016-08-10T15:00:00-04:00",
            "title": "ATom Mission Postcard - Palmdale to Kona",
            "description": "Principal Investigator Steven Wofsy of Harvard University and atomsperhic scientist Paul Newman of NASA’s Goddard Space Flight Center sent back a video postcard of the first two legs of the Atmospheric Tomography, or ATom mission. The science team first traveled from Palmdale California to Anchorage Alaksa by way of the North Pole, and one their second leg flew south to Kona, Hawaii. || Screen_Shot_2016-08-10_at_3.27.23_PM.png (1911x1069) [3.1 MB] || Screen_Shot_2016-08-10_at_3.27.23_PM_print.jpg (1024x572) [177.1 KB] || Screen_Shot_2016-08-10_at_3.27.23_PM_searchweb.png (320x180) [111.1 KB] || Screen_Shot_2016-08-10_at_3.27.23_PM_thm.png (80x40) [7.7 KB] || ATom_Final.webm (1920x1080) [19.0 MB] || Atom_Final.en_US.srt [3.4 KB] || Atom_Final.en_US.vtt [3.2 KB] || ATom_Final.mov (1920x1080) [4.6 GB] || ATom_Final.mp4 (1920x1080) [170.2 MB] || ",
            "hits": 15
        },
        {
            "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": 62
        },
        {
            "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": 24
        },
        {
            "id": 3665,
            "url": "https://svs.gsfc.nasa.gov/3665/",
            "result_type": "Visualization",
            "release_date": "2009-12-13T00:00:00-05:00",
            "title": "Global Transport of Black Carbon",
            "description": "Tiny air pollution particles commonly called soot, but also known as black carbon, are in the air and on the move throughout our planet. Black carbon enters the air when fossil fuels and biofuels, such as coal, wood, and diesel are burned. Since black carbon readily absorbs heat from sunlight, the particles can affect Earth's climate, especially on a regional scale. Though global distribution of soot remains difficult to measure, NASA researchers use satellite data and computer models to better understand how these short-lived particles influence Earth's climate, cryosphere, and clouds. This scientific data visualization uses data from the GEOS5 GOCART climate model to show black carbon's atmospheric concentration from August to November in 2009.A flat map version of this animation is available.This visualziation was created in support of a presentation at the Fall 2009 American Geophysical Union (AGU) conference in San Fransisco, CA. || ",
            "hits": 69
        },
        {
            "id": 3668,
            "url": "https://svs.gsfc.nasa.gov/3668/",
            "result_type": "Visualization",
            "release_date": "2009-12-13T00:00:00-05:00",
            "title": "Atmospheric Black Carbon Density",
            "description": "Black carbon, or soot, is formed from the burning of fossil fuels and biomass and lingers in the atmosphere for days or weeks before being deposited on the land or ocean. The transport and deposition of black carbon has become an important topic related to climate change since it can absorb sunlight and cause an increase in temperature on ice surfaces or in the atmosphere. The movement of black carbon in the atmosphere can be simulated by including existing black carbon data sets in a global model of the atmosphere. This animation shows the simulation of over three months of atmospheric black carbon production and movement from the Goddard Chemistry Aerosol and Transport (GOCART) model, which is driven by output of the GEOS5 global atmosphere simulation. Note the production of black carbon from industrialization in China and biomass burning in Africa, as well as the movement of black carbon across the oceans of the world. || ",
            "hits": 54
        },
        {
            "id": 10525,
            "url": "https://svs.gsfc.nasa.gov/10525/",
            "result_type": "Produced Video",
            "release_date": "2009-11-04T00:00:00-05:00",
            "title": "Hello Crud",
            "description": "This segment provides an introduction to aerosols- their varied sources, brief lifetimes, and erratic behavior.  Glory's APS will help researchers determine the global distribution of aerosol particles.  This unique instrument will unravel the microphysical properties of aerosols, and will shed light on the chemical composition of natural and anthropogenic aerosols and clouds. For complete transcript, click here. || Hello_Crud__512x288.00727_print.jpg (1024x576) [58.9 KB] || Hello_Crud__512x288_web.png (320x180) [160.9 KB] || Hello_Crud__512x288_thm.png (80x40) [15.7 KB] || Hello_Crud_960x720_AppleTV.webmhd.webm (960x540) [66.8 MB] || Hello_Crud_1280x720_ProRes.mov (1280x720) [4.6 GB] || Hello_Crud_1280x720_H264.mov (1280x720) [128.2 MB] || Hello_Crud_960x720_AppleTV.m4v (960x540) [160.6 MB] || Hello_Crud__640x480_ipod.m4v (640x360) [52.5 MB] || Hello_Crud__512x288.mpg (512x288) [37.2 MB] || Hello_Crud_320x240.mp4 (320x180) [22.3 MB] || Hello_Crud.wmv (320x180) [32.7 MB] || ",
            "hits": 11
        }
    ]
}