{
    "count": 6,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 2389,
            "url": "https://svs.gsfc.nasa.gov/2389/",
            "result_type": "Visualization",
            "release_date": "2002-03-04T12:00:00-05:00",
            "title": "Mount Pinatubo Particle Model",
            "description": "The global impact of the June 1991 Mount Pinatubo eruption in the Philippines can be seen in this particle model. Immediately following the eruption large amounts of sulfur dioxide and dust spread through the earth's atmosphere. The colors in this animation reflect the atmospheric height of the particles. Red is high and blue is closer to the earth's surface. || ",
            "hits": 80
        },
        {
            "id": 2181,
            "url": "https://svs.gsfc.nasa.gov/2181/",
            "result_type": "Visualization",
            "release_date": "2001-06-12T12:00:00-04:00",
            "title": "Sulfur Dioxide Emission from Mt Pinatubo Eruption, June 1991",
            "description": "This animation shows sulfur dioxide in the stratosphere during the Mt. Pinatubo eruption and for a few weeks after the eruption.  Stratospheric SO2 dissipates rather quickly compared to volcanic ash and stratoshperic H2SO4. || Sulfur dioxide emission for the two weeks following the Mt. Pinatubo eruption. || so2pinatubo_pre.jpg (320x266) [7.8 KB] || preview_made_from_dv.00120_print.png (320x240) [95.7 KB] || so2pinatubo.webmhd.webm (960x540) [340.6 KB] || so2pinatubo.mpg (320x240) [1.1 MB] || ",
            "hits": 27
        },
        {
            "id": 2182,
            "url": "https://svs.gsfc.nasa.gov/2182/",
            "result_type": "Visualization",
            "release_date": "2001-06-12T12:00:00-04:00",
            "title": "Sulfur Dioxide emission from Mt Pinatubo Eruption June 1991 with dates",
            "description": "This animation shows sulfur dioxide in the stratosphere during the Mt. Pinatubo Eruption and for a few weeks after the eruption.  Stratospheric SO2 dissipates rather quickly compared to volcanic ash and stratoshperic H2SO4. || ",
            "hits": 148
        },
        {
            "id": 2183,
            "url": "https://svs.gsfc.nasa.gov/2183/",
            "result_type": "Visualization",
            "release_date": "2001-06-12T12:00:00-04:00",
            "title": "Mt. Pinatubo Eruption on June 15, 1991",
            "description": "The second-largest volcanic eruption of the 20th century, and by far the largest eruption to affect a densely populated area, occurred at Mount Pinatubo in the Philippines on June 15, 1991. The eruption produced high-speed avalanches of hot ash and gas, giant mudflows, and a cloud of volcanic ash hundreds of miles across. This animation shows the ozone measurements around Mt Pinatubo reacting to the eruption. That \"hole\" in the days immediately following the eruption of Pinatubo is due to interference by sulfur dioxide with the retrieval algorithm. There are high amounts of volcanic SO2 in the initial plume from the eruption. These measurements make it look like there was an ozone hole when there was not. Ozone really did decrease in the equatorial zone after the volcanic cloud spread throughout the equatorial zone over the next year or so. Plots of global average ozone show a clear minimum in the two years after the eruption. But that \"hole\" on June 20th for instance is sulfur dioxide, not an ozone hole. || ",
            "hits": 172
        },
        {
            "id": 2193,
            "url": "https://svs.gsfc.nasa.gov/2193/",
            "result_type": "Visualization",
            "release_date": "2001-06-12T12:00:00-04:00",
            "title": "Mt. Pinatubo 10th Anniversary Perspective",
            "description": "This recent false color Landsat-7 image, from January 2001, shows Mt. Pinatubo as it stands today. The caldera is seen in the middle of the image, underneath clouds.Ten years after the blast, vegetation is re-growing on the slopes of the mountain (in green.) Streams of mud, called lahars, (resulting from ash from the eruption mixing with water- seen as the lighter sediment) continue to flow down the sides of the mountains, as well as channels of water (darker streams).  However, as vegetation grows back, the ash becomes more stabilized and less likely to form the destructive lahars. || ",
            "hits": 54
        },
        {
            "id": 2194,
            "url": "https://svs.gsfc.nasa.gov/2194/",
            "result_type": "Visualization",
            "release_date": "2001-06-12T12:00:00-04:00",
            "title": "Mt. Pinatubo 10th Anniversary Perspective (Stills)",
            "description": "This recent false color Landsat-7 image, from January 2001, shows Mt. Pinatubo as it stands today. The caldera is seen in the middle of the image, underneath clouds. Ten years after the blast, vegetation is re-growing on the slopes of the mountain (in green). Streams of mud, called lahars, (resulting from ash from the eruption mixing with water- seen as the lighter sediment) continue to flow down the sides of the mountains, as well as channels of water (darker streams). However, as vegetation grows back, the ash becomes more stabilized and less likely to form the destructive lahars. || ",
            "hits": 30
        }
    ]
}