{
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    "next": null,
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    "results": [
        {
            "id": 31223,
            "url": "https://svs.gsfc.nasa.gov/31223/",
            "result_type": "Hyperwall Visual",
            "release_date": "2023-04-03T00:00:00-04:00",
            "title": "A Daily View of Earth",
            "description": "A year-long true color global animation of MODIS corrected reflectance. || MODIS_combined_CorrRefl_TrueColor_2023-02-20_print.jpg (1024x576) [276.9 KB] || MODIS_combined_CorrRefl_TrueColor_2023-02-20_searchweb.png (320x180) [127.8 KB] || MODIS_combined_CorrRefl_TrueColor_2023-02-20_thm.png (80x40) [19.9 KB] || modis_truecolor_labeled_2022-2023_1080p10.webm (1920x1080) [8.7 MB] || MODIS_combined_CorrRefl_TrueColor_2023-02-20.tif (3840x2160) [14.0 MB] || modis_truecolor_labeled (3840x2160) [32.0 KB] || modis_truecolor_labeled_2022-2023_1080p10.mp4 (1920x1080) [176.9 MB] || modis_truecolor_labeled_2022-2023_2160p10.mp4 (3840x2160) [799.1 MB] || modis_truecolor_labeled_2022-2023_1080p10.hwshow [123 bytes] || modis_truecolor_labeled_2022-2023_2160p10.hwshow [123 bytes] || ",
            "hits": 195
        },
        {
            "id": 10389,
            "url": "https://svs.gsfc.nasa.gov/10389/",
            "result_type": "Produced Video",
            "release_date": "2009-02-19T00:00:00-05:00",
            "title": "Aerosols Absorb; Aerosols Reflect",
            "description": "Some aerosol particles primarily reflect solar radiation and cool the atmosphere, and others can also absorb radiation and warm the surrounding air. When aerosols heat the atmosphere, they create an unstable environment where clouds can't thrive. The suppression of clouds leads to further warming of the atmosphere by solar radiation. Aerosols are a complex but critical piece of the climate puzzle, and researchers are still working to understand the role of these curious particles. || ",
            "hits": 182
        },
        {
            "id": 3179,
            "url": "https://svs.gsfc.nasa.gov/3179/",
            "result_type": "Visualization",
            "release_date": "2005-06-21T00:00:00-04:00",
            "title": "Scene Identification Compared to Clouds (WMS)",
            "description": "The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere. As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights. The amount of reflection and absorption is critical to the climate. An instrument named CERES orbits the Earth every 99 minutes and measures the reflected solar energy. This animation shows the scene identification as measured by CERES during 29 orbits on June 20 and 21 of 2003. By comparing the incoming solar radiation with the outgoing reflected and thermal radiation, it is possible to identify the type of area being viewed, whether it be land, clouds, ocean, or ice. This scene identification is used together with the radiation flux measurements to build up a complete picture of the Earth's energy budget over time. || ",
            "hits": 10
        },
        {
            "id": 3104,
            "url": "https://svs.gsfc.nasa.gov/3104/",
            "result_type": "Visualization",
            "release_date": "2005-02-01T12:00:00-05:00",
            "title": "Instantaneous Scene Identification (WMS)",
            "description": "The Earth's climate is determined by energy transfer from the sun to the Earth's land, oceans, and atmosphere. As the Earth rotates, the sun lights up only part of the Earth at a time, and some of that incoming solar energy is reflected and some is absorbed, depending on type of area it lights. The amount of reflection and absorption is critical to th e climate. An instrument named CERES orbits the Earth every 99 minutes and measures the reflected solar energy. This animation shows the scene identification as measured by CERES during 29 orbits on June 20 and 21 of 2003. By comparing the incoming solar radiation with the outgoing reflected and thermal radiation, it is possible to identify the type of area being viewed, whether it be land, clouds, ocean, or ice. This scene identification is used together with the radiation flux measurements to build up a complete picture of the Earth's energy budget over time. || ",
            "hits": 19
        },
        {
            "id": 20023,
            "url": "https://svs.gsfc.nasa.gov/20023/",
            "result_type": "Animation",
            "release_date": "2004-02-09T12:00:00-05:00",
            "title": "Ice Albedo: Black Soot and Snow",
            "description": "Black soot may contribute to melting glaciers and other ice on the planet and eventually a warmer Earth. Traveling potentially thousands of miles from its sources on air currents, this pollution eventually settles out of the air, onto land and into the oceans. On ice and snow, it darkens normally bright surfaces. Just as a white shirt keeps a person cooler in the summer than a black shirt, the vast stretches of polar ice covering much of the planet's top and bottom reflect large amounts of solar radiation falling on the planet's surface, helping regulate Earth's temperature. Soot lowers this albedo, or reflectivity, and the ice retains more heat, leading to increased melting.Soot-darkened ice retains more light, contributing to the process. As light is absorbed, the environment is heated, thus intensifying a feedback loop: a warmer planet yields more ice melting and thus an even warmer planet. || ",
            "hits": 249
        },
        {
            "id": 20022,
            "url": "https://svs.gsfc.nasa.gov/20022/",
            "result_type": "Animation",
            "release_date": "2004-02-05T12:00:00-05:00",
            "title": "Ice Albedo: Bright White Reflects Light",
            "description": "This animation provides a close perspective of the relationship between ice and solar reflectivity. As glaciers, the polar caps, and icebergs (shown here) melt, less sunlight gets reflected into space. Instead, the oceans and land absorb the light, thus raising the overall temperature and adding energy to a vicious circle. || ",
            "hits": 561
        }
    ]
}