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        {
            "id": 12794,
            "url": "https://svs.gsfc.nasa.gov/12794/",
            "result_type": "Produced Video",
            "release_date": "2017-12-12T00:00:00-05:00",
            "title": "A Summer ABoVE the Warming Arctic",
            "description": "Scientists with NASA's Arctic Boreal Vulnerability Experiment - ABoVE - are studying how the Arctic region responds to climate change. Looking at everything from thawing permafrost underground to wildfires, the researchers are working to create a comprehensive picture of the warming Arctic.This summer, the team brought a fleet of planes to fly over Alaska and Canada and gather data to complement measurements taken from the ground. The ABoVE campaign is designed to last for ten years. || ",
            "hits": 32
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        {
            "id": 12044,
            "url": "https://svs.gsfc.nasa.gov/12044/",
            "result_type": "Produced Video",
            "release_date": "2015-11-12T11:00:00-05:00",
            "title": "Carbon and Climate Briefing - November 12, 2015",
            "description": "Carbon_and_Climate_HD.jpg (1280x720) [722.5 KB] || Carbon_and_Climate_HD_searchweb.png (320x180) [100.9 KB] || Carbon_and_Climate_HD_thm.png (80x40) [7.8 KB] || ",
            "hits": 82
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        {
            "id": 12056,
            "url": "https://svs.gsfc.nasa.gov/12056/",
            "result_type": "Produced Video",
            "release_date": "2015-11-12T11:00:00-05:00",
            "title": "Carbon Dioxide Sources From a High-Resolution Climate Model",
            "description": "Animation of carbon dioxide released from two different sources: fires (biomass burning) and massive urban centers known as megacities.  The animation covers a five day period in June 2006.  The model is based on real emission data and is then set to run so that scientists can observe how the greenhouse gas behaves once it has been emitted. || tagged_co2_global_loop_appletv_print.jpg (1024x576) [102.9 KB] || tagged_co2_global_loop_appletv_searchweb.png (320x180) [75.4 KB] || tagged_co2_global_loop_appletv_thm.png (80x40) [6.0 KB] || tagged_co2_global_loop_appletv.m4v (1280x720) [25.1 MB] || tagged_co2_global_loop_youtube_hq.mov (1920x1080) [80.0 MB] || tagged_co2_global_loop.webm (960x540) [14.5 MB] || tagged_co2_global_loop_ipod_sm.mp4 (320x240) [7.8 MB] || tagged_co2_global_loop.mpeg (1280x720) [172.7 MB] || tagged_co2_global_loop_prores.mov (1280x720) [707.1 MB] || ",
            "hits": 40
        },
        {
            "id": 30515,
            "url": "https://svs.gsfc.nasa.gov/30515/",
            "result_type": "Hyperwall Visual",
            "release_date": "2014-06-30T13:00:00-04:00",
            "title": "Simulated Atmospheric Carbon Concentrations",
            "description": "Carbon exists in many forms—e.g., carbon dioxide (CO2), carbon monoxide (CO)—and continually cycles through Earth’s atmosphere, ocean, and terrestrial ecosystems. This visualization, created using data from the 7-km GEOS-5 Nature Run model, shows average column concentrations of atmospheric CO2 (colored shades) and CO (white shades underneath) from January 1, 2006 to December 31, 2006.CO2 variations are largely controlled by fossil fuel emissions and seasonal fluxes of carbon between the atmosphere and land biosphere. For example, dark red and pink shades represent regions where CO2 concentrations are enhanced by carbon sources, mainly from human activities. During Northern Hemisphere spring and summer months, plants absorb a substantial amount of CO2 through photosynthesis, thus removing CO2 from the atmosphere. Atmospheric CO, a pollutant harmful to human health, is produced mainly from fossil fuel combustion and biomass burning. Here, high concentrations of CO (white) are mainly from fire activity in Africa, South America, and Australia. Scientists use model output data such as these to help answer important questions about Earth’s climate and to help design future satellite missions.These model simulations use fossil fuel emissions estimates provided by the Emissions Database for Global Atmospheric Research (EDGAR). NASA’s Quick Fire Emissions Dataset (QFED) estimates fire emissions using MODIS fire radiative power observations. Additional, observationally constrained estimates of CO2 flux between the atmosphere and land and ocean carbon reservoirs were produced as part of NASA’s Carbon Monitoring System Flux Pilot Project (http://carbon.nasa.gov/cgi-bin/cms/inv_pgp.pl?pgid=581). Land biosphere fluxes come from the Carnegie-Ames-Stanford Approach Global Fire Emissions Database (CASA-GFED) model which incorporates MODIS vegetation classification and AVHRR Normalized Difference Vegetation Index (NDVI) data. Ocean fluxes are produced by the NASA Ocean Biogeochemical Model (NOBM) which incorporates MODIS chlorophyll observations. || ",
            "hits": 89
        },
        {
            "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": 70
        },
        {
            "id": 10494,
            "url": "https://svs.gsfc.nasa.gov/10494/",
            "result_type": "Produced Video",
            "release_date": "2009-10-09T00:00:00-04:00",
            "title": "The Carbon Cycle",
            "description": "Carbon is the basic building block of life, and these unique atoms are found everywhere on Earth. Carbon makes up Earth's plants and animals, and is also stored in the ocean, the atmosphere, and the crust of the planet. A carbon atom could spend millions of years moving through Earth in a complex cycle. This conceptual animation provides an illustration of the various parts of the Carbon cycle. Purple arrows indicate the uptake of Carbon; yellow arrows indicate the release of Carbon. On land, plants remove carbon from the atmosphere through photosynthesis. Animals eat plants and either breath out the carbon, or it moves up the food chain. When plants and animals die and decay, they transfer carbon back to the soil. Moving offshore, the ocean takes up carbon through physical and biological processes. At the ocean's surface, carbon dioxide from the atmosphere dissolves into the water. Tiny marine plants called phytoplankton use this carbon dioxide for photosynthesis. Phytoplankton are the base of the marine food web. After animals eat the plants, they breathe out the carbon or pass it up the food chain. Sometimes phytoplankton die, decompose, and are recycled in the surface waters. Phytoplankton can also sink to the bottom of the ocean, where they become buried in marine sediment. Over long time scales, this process has made the ocean floor the largest reservoir of carbon on the planet. In a process called upwelling, currents bring cold water containing carbon up to the surface. As the water warms, the carbon is then be released as a gas back into the atmosphere, continuing the carbon cycle.  Carbon is found in the atmosphere as Carbon dioxide, which is a greenhouse gas. Greenhouse gases act like a blanket, and trap heat in the atmosphere. In the past two centuries, humans have increased atmospheric carbon dioxide by more than 30%, by burning fossil-fuels and cutting down forests. || ",
            "hits": 305
        },
        {
            "id": 20006,
            "url": "https://svs.gsfc.nasa.gov/20006/",
            "result_type": "Animation",
            "release_date": "2003-11-05T12:00:00-05:00",
            "title": "Carbon Cycle",
            "description": "The Carbon  Cycle - The carbon cycle on land, acted out here show a tree  taking in carbon dioxide from the atmosphere, and combined with water  and nutrients from the soil, growing. In the fall and winter, parts  of the growth die off and release some carbon back into the system.  At some point, the tree is no longer able to take in carbon and  begins to die. When that happens, all the carbon absorbed in its body  is released back into the cycle as it decomposes. Fire can accelerate  this, sending plumes of carbon-laden aerosols into the atmosphere, as  well as leaving carbon-rich ash deposits on the ground for further  decomposition and recycling. || ",
            "hits": 31
        },
        {
            "id": 20007,
            "url": "https://svs.gsfc.nasa.gov/20007/",
            "result_type": "Animation",
            "release_date": "2003-11-05T12:00:00-05:00",
            "title": "Carbon Cycle",
            "description": "Carbon And The Ocean — The Slow Cycle - The oceans are vast, and their processes as complex as their waters are deep.Phytoplankton absorbs carbon dioxide from the atmosphere and nutrient rich waters and grows in wide colonies called blooms. These blooms are highly dependent on surrounding environmental conditions.As phytoplankton grows, it forms the foundation for the food chain, thus passing carbon up to higher life forms. But just as on land, links in the ocean's chain of life also break, and stored carbon settles out of the top layers of water. A portion of it gets swept back to the surface as upwellings, only to begin again, but a major portion sinks to the bottom, becoming what oceanographers call 'marine snow.' This decomposing biological matter literally precipitates through the water and builds up on the ocean bottom, essentially sequestered from the rest of the Earth for geologically long periods of time. || ",
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        }
    ]
}