{
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    "next": null,
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    "results": [
        {
            "id": 30386,
            "url": "https://svs.gsfc.nasa.gov/30386/",
            "result_type": "Hyperwall Visual",
            "release_date": "2013-10-24T12:00:00-04:00",
            "title": "Monthly Cloud Particle Radius (Terra/MODIS)",
            "description": "To better understand the role of clouds in the Earth's climate system, scientists need two important measurements: cloud optical thickness and cloud particle size. The size of cloud particles is important. In general, smaller particles produce brighter, more reflective clouds, which bounce more sunlight back into space and cool the planet. By carefully quantifying how much shortwave infrared sunlight clouds absorb, scientists can determine the size of the individual particles within clouds. Clouds with larger particles absorb more shortwave infrared light and, conversely, clouds with smaller particles absorb less shortwave infrared light. These maps show monthly cloud particle radius from January 2005 to the present, produced using data from the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument onboard NASA’s Terra satellite. White shades show where there are smaller cloud particles (between 4 and 11 micrometers in radius), while purple shades show where there are larger cloud particles (between 33 and 40 micrometers). || ",
            "hits": 17
        },
        {
            "id": 30399,
            "url": "https://svs.gsfc.nasa.gov/30399/",
            "result_type": "Hyperwall Visual",
            "release_date": "2013-10-24T12:00:00-04:00",
            "title": "Monthly Cloud Particle Radius (Aqua/MODIS)",
            "description": "To better understand the role of clouds in the Earth's climate system, scientists need two important measurements: cloud optical thickness and cloud particle size. The size of cloud particles is important. In general, smaller particles produce brighter, more reflective clouds, which bounce more sunlight back into space and cool the planet. By carefully quantifying how much shortwave infrared sunlight clouds absorb, scientists can determine the size of the individual particles within clouds. Clouds with larger particles absorb more shortwave infrared light and, conversely, clouds with smaller particles absorb less shortwave infrared light. These maps show monthly cloud particle radius from July 2002 to the present, produced using data from the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument onboard NASA’s Aqua satellite. White shades show where there are smaller cloud particles (between 4 and 11 micrometers in radius), while purple shades show where there are larger cloud particles (between 33 and 40 micrometers). || ",
            "hits": 32
        },
        {
            "id": 30400,
            "url": "https://svs.gsfc.nasa.gov/30400/",
            "result_type": "Hyperwall Visual",
            "release_date": "2013-10-24T12:00:00-04:00",
            "title": "Monthly Cloud Water Content (Aqua/MODIS)",
            "description": "Have you ever wondered how much water is in clouds? These maps show monthly cloud water content from July 2002 to the present, produced using data from the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument onboard NASA’s Aqua satellite. Cloud water content is a measure of how many grams of water per square meter you would get if you drained all the water out of the clouds into a flat layer on the ground. Light pink to white shades show areas of clouds with as much as 1000 grams of water per square meter; pink shades show areas with about 500 grams of water per square meter, and dark purple shows areas with little or no cloud water content. In short, the more water in a cloud, the more it reflects sunlight back to space and the more it cools Earth's surface. Cloud water content as well as cloud particle size are also important for global studies of precipitation. || ",
            "hits": 174
        }
    ]
}