{
    "count": 2,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 20011,
            "url": "https://svs.gsfc.nasa.gov/20011/",
            "result_type": "Animation",
            "release_date": "2003-12-09T12:00:00-05:00",
            "title": "Pollution Reduces Winter Precipitation",
            "description": "In winter, moist air flows off the ocean and rises over the hills downwind of  a coastal city, dropping its rain and snow mainly as it ascends the hills.  As pollution from the city is pushed into the clouds by the hills downwind of the city, it interferes with droplet formation in the clouds as observed by NASA's satellites.  The smaller cloud droplets convert more slowly into precipitation.  Instead of precipitating, much of the water in the clouds evaporates, reducing the net rainfall downwind of the urban area by up to 15% to 25% on a seasonal basis.  First is the unpolluted case. || ",
            "hits": 54
        },
        {
            "id": 20012,
            "url": "https://svs.gsfc.nasa.gov/20012/",
            "result_type": "Animation",
            "release_date": "2003-12-09T12:00:00-05:00",
            "title": "Pollution Increases Summer Precipitation",
            "description": "In summer, weaker winds move the clouds more slowly.  Heat absorbed by the city and pollution's interference with raindrop formation interact to cause the clouds to intensify before producing precipitation.  The onset of rainfall from a cloud leads eventually to its demise by cooling off the air near the ground.  the air pollution delays the onset of precipitation, so that the intense storm clouds can build higher and larger before they start precipitating and subsequently dissipating.  Therefore, these larger and more intense thunderstorm clouds produce eventually heavier rainfall on the city and the downwind areas.  First is the unpolluted, then the polluted case. || ",
            "hits": 61
        }
    ]
}