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            "id": 14013,
            "url": "https://svs.gsfc.nasa.gov/14013/",
            "result_type": "Produced Video",
            "release_date": "2022-01-19T00:00:00-05:00",
            "title": "Elements of Webb: Super Black Ep11",
            "description": "Elements of Webb EP11:  Super Black || SuperBlack_-_Dark.jpg (1920x1080) [1015.6 KB] || SuperBlack_-_Dark_print.jpg (1024x576) [430.6 KB] || SuperBlack_-_Dark_searchweb.png (320x180) [97.2 KB] || SuperBlack_-_Dark_web.png (320x180) [97.2 KB] || SuperBlack_-_Dark_thm.png (80x40) [7.7 KB] || 11-Elements_-_SuperBlack_draft_2.mp4 (1920x1080) [224.9 MB] || 11-Elements_-_SuperBlack_ProRes.mov (1920x1080) [3.1 GB] || 11-Elements_-_SuperBlack_draft_2.webm (1920x1080) [24.2 MB] || 11-Elements_-_SuperBlack.en_US.srt [3.9 KB] || 11-Elements_-_SuperBlack.en_US.vtt [3.9 KB] || ",
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            "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. || ",
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            "url": "https://svs.gsfc.nasa.gov/20023/",
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            "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. || ",
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            "url": "https://svs.gsfc.nasa.gov/20020/",
            "result_type": "Animation",
            "release_date": "2003-12-12T12:00:00-05:00",
            "title": "Ice Albedo-Close Up",
            "description": "This  is a conceptual animation showing how melting ice on land and at sea, can affect  the surrounding ocean water, changing both the chemistry and relative sea level. || ",
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            "url": "https://svs.gsfc.nasa.gov/20021/",
            "result_type": "Animation",
            "release_date": "2003-12-12T12:00:00-05:00",
            "title": "Ice Albedo - Global View",
            "description": "This is a conceptual animation showing how polar ice reflects light from the sun. As this ice begins to melt, less sunlight gets reflected into space. It is instead absorbed into the oceans and land, raising the overall temperature, and fueling further melting. || ",
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