{
    "count": 4,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 3175,
            "url": "https://svs.gsfc.nasa.gov/3175/",
            "result_type": "Visualization",
            "release_date": "2005-06-21T00:00:00-04:00",
            "title": "Outgoing Shortwave Flux 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 reflected solar radiation measured by CERES during 29 orbits on June 20 and 21 of 2003 over infrared cloud images for the same period. Reflected solar radiation is shortwave radiation, and the most intense reflection comes from clouds. || ",
            "hits": 22
        },
        {
            "id": 3096,
            "url": "https://svs.gsfc.nasa.gov/3096/",
            "result_type": "Visualization",
            "release_date": "2005-02-01T12:00:00-05:00",
            "title": "Average Clear-sky Outgoing Shortwave Flux (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 average amount of reflection and absorption is critical to the climate, because the absorbed energy heats up the Earth until it is radiated away as thermal radiation.  This animation shows the monthly average clear-sky outgoing shortwave radiation from July, 2002 through June, 2004 as measured by the CERES instrument.  This is the sunlight that is directly reflected back into space by ice, desert, and other physical areas on the Earth when the sky is cloud-free.  The ice sheets can be clearly seen to reflect the most sunlight, with desert areas next.  Oceans absorb the most sunlight, more than the vegetated land areas such as the tropical rain forest and temperate forests and plains. || ",
            "hits": 17
        },
        {
            "id": 3097,
            "url": "https://svs.gsfc.nasa.gov/3097/",
            "result_type": "Visualization",
            "release_date": "2005-02-01T12:00:00-05:00",
            "title": "Average Total-sky Outgoing Shortwave Flux (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 average amount of reflection and absorption is critical to the climate, because the absorbed energy heats up the Earth until it is radiated away as thermal radiation.  This animation shows the monthly average outgoing shortwave radiation from July, 2002 through June, 2004 as measured by the CERES instrument.  This is the sunlight that is directly reflected back into space by clouds, ice, desert, and other physical areas on the Earth.  Although clouds are very reflective, they come and going during the month, so more reflection is seen on average from ice sheets, which change very little during a monthly period.  Note that the cloud-free parts of the ocean are relatively dark, indicating that oceans absorb more sunlight than they reflect. || ",
            "hits": 14
        },
        {
            "id": 3108,
            "url": "https://svs.gsfc.nasa.gov/3108/",
            "result_type": "Visualization",
            "release_date": "2005-02-01T12:00:00-05:00",
            "title": "Instantaneous Outgoing Shortwave Flux (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 reflected solar radiation measured by CERES during 29 orbits on June 20 and 21 of 2003.  Reflected solar radiation is shortwave radiation, and the most intense reflection comes from clouds, followed by ice.  Land reflects only a small amount of radiation, but ocean reflects the least, which is the reason that the sun heats the oceans so effectively.  Of course, there is no reflected solar radiation in regions of night. || ",
            "hits": 13
        }
    ]
}