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        {
            "id": 3264,
            "url": "https://svs.gsfc.nasa.gov/3264/",
            "result_type": "Visualization",
            "release_date": "2005-10-30T12:00:00-05:00",
            "title": "Smithsonian Exhibit:  Antarctic Ozone Sequence 1979 through 2004",
            "description": "NASA has been monitoring the status of the ozone layer through satellite observations since the 1970s, beginning with the TOMS sensors on the Nimbus satellites. The latest-generation ozone-monitoring technology, the Ozone Monitoring Instrument (OMI), is flying onboard NASA's Aura satellite. The ozone hole is not technically a 'hole' where no ozone is present, but is actually a region of exceptionally depleted ozone in the stratosphere over the Antarctic.  The ozone hole begins to grow in August and reaches its largest area in depth in the middle of September to early October period. In the early years (before 1984) the hole was small because chlorine and bromine levels over Antarctica were low. Year-to-year variations in area and depth are caused by year-to-year variations in temperature. Colder conditions result in a larger area and lower ozone values in the center of the hole.  This animation shows total ozone in the Antarctic region along with the maximum ozone depth and size since the earliest measurements of Earth Probe instrument on the TOMS satellite.  This animation was created for an exhibit at the Smithsonium Museum. Data dropouts have been removed for the following times:  1998/12/14-31, 2002/08/03-11, 2003/11/28-2003/12/02.  The minimum ozone recorded is 82.0 du  on September 26, 2003.  The maximum area of 29 million square kilometers (11.4 million square miles) occurred on September 9, 2000. || ",
            "hits": 50
        },
        {
            "id": 3169,
            "url": "https://svs.gsfc.nasa.gov/3169/",
            "result_type": "Visualization",
            "release_date": "2005-06-01T12:00:00-04:00",
            "title": "Sulfur Dioxide from the Mount Pinatubo Volcanic Eruption, 1991 (WMS)",
            "description": "This animation shows levels of sulfur dioxide in the atmosphere after the volcanic eruption of Mt. Pinatubo in the Philippines.This product is available through our Web Map Service. || background-bluemarble-equatorial.png (1024x256) [226.3 KB] || pinatubo_so2-thm.png (80x40) [3.9 KB] || pinatubo_so2-pre.png (320x160) [39.3 KB] || pinatubo_so2-pre_searchweb.png (320x180) [39.6 KB] || pinatubo_so2.webmhd.webm (960x540) [173.9 KB] || 1024x256 (1024x256) [4.0 KB] || pinatubo_so2.m2v (1024x256) [4.8 MB] || a003169_pinatubo_so2.mp4 (640x160) [987.3 KB] || ",
            "hits": 95
        },
        {
            "id": 3126,
            "url": "https://svs.gsfc.nasa.gov/3126/",
            "result_type": "Visualization",
            "release_date": "2005-03-08T12:00:00-05:00",
            "title": "Daily Erythemal Index (UV exposure) for 2000-2001 (WMS)",
            "description": "The Erythemal Index is a measure of ultraviolet (UV) radiation at ground level on the Earth. (The word 'erythema' means an abnormal redness of the skin, such as is caused by spending too much time in the sun—a sunburn is damage to your skin cells caused by UV radiation.) Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can affect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 20
        },
        {
            "id": 3114,
            "url": "https://svs.gsfc.nasa.gov/3114/",
            "result_type": "Visualization",
            "release_date": "2005-03-07T12:00:00-05:00",
            "title": "Daily Erythemal Index (UV exposure) Measurements for 2000-2001 (WMS)",
            "description": "The Erythemal Index is a measure of ultraviolet (UV) radiation at ground level on the Earth. (The word 'erythema' means an abnormal redness of the skin, such as is caused by spending too much time in the sun—a sunburn is damage to your skin cells caused by UV radiation.) Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can affect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 44
        },
        {
            "id": 3124,
            "url": "https://svs.gsfc.nasa.gov/3124/",
            "result_type": "Visualization",
            "release_date": "2005-03-07T12:00:00-05:00",
            "title": "Monthly Average Erythemal Index (UV exposure) for 2000-2001 (WMS)",
            "description": "The Erythemal Index is a measure of ultraviolet (UV) radiation at ground level on the Earth. (The word 'erythema' means an abnormal redness of the skin, such as is caused by spending too much time in the sun—a sunburn is damage to your skin cells caused by UV radiation.) Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can affect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 24
        },
        {
            "id": 2284,
            "url": "https://svs.gsfc.nasa.gov/2284/",
            "result_type": "Visualization",
            "release_date": "2001-11-12T12:00:00-05:00",
            "title": "Total Ozone from Earth Probe TOMS: 7/26/1996-11/4/2001",
            "description": "This animation shows the total ozone as measured by Earth Probe TOMS since the earliest measurements by that instrument.  Days for which the instrument collected little or no data are skipped. || ",
            "hits": 14
        },
        {
            "id": 2216,
            "url": "https://svs.gsfc.nasa.gov/2216/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Daily Erythemal Index over the United States for July 2001",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 14
        },
        {
            "id": 2217,
            "url": "https://svs.gsfc.nasa.gov/2217/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Daily Erythemal Index over the United States for July 2001 (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 11
        },
        {
            "id": 2218,
            "url": "https://svs.gsfc.nasa.gov/2218/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Zoom to North America (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 5
        },
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            "id": 2219,
            "url": "https://svs.gsfc.nasa.gov/2219/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Slow Zoom to North America (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 7
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            "id": 2220,
            "url": "https://svs.gsfc.nasa.gov/2220/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Rotating Globe (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 12
        },
        {
            "id": 2221,
            "url": "https://svs.gsfc.nasa.gov/2221/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Slow Rotating Globe (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 8
        },
        {
            "id": 2222,
            "url": "https://svs.gsfc.nasa.gov/2222/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Full Earth",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 10
        },
        {
            "id": 2223,
            "url": "https://svs.gsfc.nasa.gov/2223/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Full Earth (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 11
        },
        {
            "id": 2224,
            "url": "https://svs.gsfc.nasa.gov/2224/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: North and South America",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 6
        },
        {
            "id": 2225,
            "url": "https://svs.gsfc.nasa.gov/2225/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: North and South America (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 12
        },
        {
            "id": 2226,
            "url": "https://svs.gsfc.nasa.gov/2226/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Europe and Africa",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 7
        },
        {
            "id": 2227,
            "url": "https://svs.gsfc.nasa.gov/2227/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Europe and Africa (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 11
        },
        {
            "id": 2228,
            "url": "https://svs.gsfc.nasa.gov/2228/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Australia and Asia",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 14
        },
        {
            "id": 2229,
            "url": "https://svs.gsfc.nasa.gov/2229/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Australia and Asia (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 10
        },
        {
            "id": 2256,
            "url": "https://svs.gsfc.nasa.gov/2256/",
            "result_type": "Visualization",
            "release_date": "2001-08-08T12:00:00-04:00",
            "title": "Erythemal Index for August 2000 through July 2001: Rotating Globe",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 5
        },
        {
            "id": 2196,
            "url": "https://svs.gsfc.nasa.gov/2196/",
            "result_type": "Visualization",
            "release_date": "2001-07-02T12:00:00-04:00",
            "title": "Erythemal Index 2000: Push-in to the United States",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 9
        },
        {
            "id": 2197,
            "url": "https://svs.gsfc.nasa.gov/2197/",
            "result_type": "Visualization",
            "release_date": "2001-07-02T12:00:00-04:00",
            "title": "Erythemal Index 2000: Push-in to the United States (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 13
        },
        {
            "id": 2198,
            "url": "https://svs.gsfc.nasa.gov/2198/",
            "result_type": "Visualization",
            "release_date": "2001-07-02T12:00:00-04:00",
            "title": "Erythemal Index 2000: Full Globe Loop",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 25
        },
        {
            "id": 2199,
            "url": "https://svs.gsfc.nasa.gov/2199/",
            "result_type": "Visualization",
            "release_date": "2001-07-02T12:00:00-04:00",
            "title": "Erythemal Index 2000: Full Globe Loop (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 9
        },
        {
            "id": 2200,
            "url": "https://svs.gsfc.nasa.gov/2200/",
            "result_type": "Visualization",
            "release_date": "2001-07-02T12:00:00-04:00",
            "title": "Erythemal Index 2000: United States Loop",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 12
        },
        {
            "id": 2201,
            "url": "https://svs.gsfc.nasa.gov/2201/",
            "result_type": "Visualization",
            "release_date": "2001-07-02T12:00:00-04:00",
            "title": "Erythemal Index 2000: United States Loop (With Dates)",
            "description": "The Erythemal Index is a measure of ultraviolet radiation (UV) at ground level on the Earth. UV exists to the left of the visible spectrum and is divided into three components (UV-A, UV-B and UV-C). UV-B (290-320 wavelengths) is the most dangerous form of UV radiation that can reach ground level. Atmospheric ozone shields life at the surface from most of the harmful components of solar radiation. Chemical processes in the atmosphere can effect the level of protection provided by the ozone in the upper atmosphere. This thinning of the atmospheric ozone in the stratosphere leads to elevated levels of UV-B at ground level and increases the risks of DNA damage in living organisms. || ",
            "hits": 14
        },
        {
            "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": 33
        },
        {
            "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": 80
        },
        {
            "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": 289
        },
        {
            "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": 44
        },
        {
            "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": 34
        },
        {
            "id": 2164,
            "url": "https://svs.gsfc.nasa.gov/2164/",
            "result_type": "Visualization",
            "release_date": "2001-01-01T12:00:00-05:00",
            "title": "EP TOMS Ozone: Southern Hemisphere (1/4/99 - 12/31/00)",
            "description": "This animation was created for an exhibit at the National Space Centre in Leicester, England.Note that there are no frames in the animation for November 17, 1999, and November 18, 1999, since Earth Probe TOMS data is incomplete for those days. || ",
            "hits": 10
        },
        {
            "id": 2165,
            "url": "https://svs.gsfc.nasa.gov/2165/",
            "result_type": "Visualization",
            "release_date": "2001-01-01T12:00:00-05:00",
            "title": "EP TOMS Ozone: Northern Hemisphere (1/1/00 - 12/31/00)",
            "description": "This animation was created for an exhibit at the National Space Centre in Leicester, England. || ",
            "hits": 10
        },
        {
            "id": 2166,
            "url": "https://svs.gsfc.nasa.gov/2166/",
            "result_type": "Visualization",
            "release_date": "2001-01-01T12:00:00-05:00",
            "title": "EP TOMS Ozone (7/26/96 - 12/4/00)",
            "description": "This animation shows the total ozone as measured by Earth Probe TOMS since the earliest measurements by that instrument.Days on which no data was taken appear as blank. || ",
            "hits": 15
        },
        {
            "id": 129,
            "url": "https://svs.gsfc.nasa.gov/129/",
            "result_type": "Visualization",
            "release_date": "1998-01-01T12:00:00-05:00",
            "title": "Visualization of 3D Ozone Data: Nimbus-7 SBUV",
            "description": "An animation which first shows the height structure of Nimbus-7 SBUV ozone profile measurements, then an animation of the three dimension structure of atmospheric ozone using a cut-away surface and a series of isosurfaces at various ozone values.  Data in this animation comes from the first week of October, 1985. || a000129.00095_print.png (720x480) [496.8 KB] || a000129_thm.png (80x40) [4.9 KB] || a000129_pre.jpg (320x238) [6.9 KB] || a000129_pre_searchweb.jpg (320x180) [43.6 KB] || a000129.webmhd.webm (960x540) [5.8 MB] || a000129.mp4 (640x480) [13.8 MB] || a000129.dv (720x480) [245.4 MB] || a000129.mpg (352x240) [9.2 MB] || ",
            "hits": 39
        },
        {
            "id": 130,
            "url": "https://svs.gsfc.nasa.gov/130/",
            "result_type": "Visualization",
            "release_date": "1998-01-01T12:00:00-05:00",
            "title": "SBUV Daily Profile Ozone: June 1985 - November 1985",
            "description": "Daily ozone height profiles as measured by the Nimbus-7 SBUV from June 1, 1985 through November 30, 1985 || a000130.00095_print.png (720x480) [432.3 KB] || a000130_thm.png (80x40) [4.9 KB] || a000130_pre.jpg (320x238) [6.5 KB] || a000130_pre_searchweb.jpg (320x180) [43.4 KB] || a000130.webmhd.webm (960x540) [5.4 MB] || a000130.dv (720x480) [315.4 MB] || a000130.mp4 (640x480) [17.3 MB] || a000130.mpg (352x240) [12.2 MB] || ",
            "hits": 23
        },
        {
            "id": 131,
            "url": "https://svs.gsfc.nasa.gov/131/",
            "result_type": "Visualization",
            "release_date": "1998-01-01T12:00:00-05:00",
            "title": "SBUV 2-Day Running Average Profile and Total Ozone: June 1985 - November 1985",
            "description": "2-day running averages of ozone height profiles and total ozone as measured by the Nimbus-7 SBUV from June 1, 1985 through November 30, 1985 || a000131.00095_print.png (720x480) [480.8 KB] || a000131_thm.png (80x40) [5.6 KB] || a000131_pre.jpg (320x238) [8.6 KB] || a000131_pre_searchweb.jpg (320x180) [60.4 KB] || a000131.webmhd.webm (960x540) [8.7 MB] || a000131.dv (720x480) [313.7 MB] || a000131.mp4 (640x480) [17.2 MB] || a000131.mpg (352x240) [12.3 MB] || ",
            "hits": 38
        },
        {
            "id": 36,
            "url": "https://svs.gsfc.nasa.gov/36/",
            "result_type": "Visualization",
            "release_date": "1994-10-03T12:00:00-04:00",
            "title": "1992 Daily Ozone from Nimbus-7",
            "description": "In this animation of total ozone, the luminance values of the colors bounding areas of missing data are used in interpolating over these regions.  The missing data are mapped to the grayscale portion of the color map. || ",
            "hits": 47
        },
        {
            "id": 37,
            "url": "https://svs.gsfc.nasa.gov/37/",
            "result_type": "Visualization",
            "release_date": "1994-10-03T12:00:00-04:00",
            "title": "1993 Daily Ozone from Nimbus-7",
            "description": "In this animation of total ozone, the luminance values of the colors bounding areas of missing data are used in interpolating over these regions.  The missing data are mapped to the grayscale portion of the color map. || ",
            "hits": 10
        },
        {
            "id": 38,
            "url": "https://svs.gsfc.nasa.gov/38/",
            "result_type": "Visualization",
            "release_date": "1994-10-03T12:00:00-04:00",
            "title": "1993 Daily Ozone from Meteor-3",
            "description": "In this animation of total ozone, the luminance values of the colors bounding areas of missing data are used in interpolating over these regions.  The missing data are mapped to the grayscale portion of the color map. || ",
            "hits": 14
        },
        {
            "id": 74,
            "url": "https://svs.gsfc.nasa.gov/74/",
            "result_type": "Visualization",
            "release_date": "1994-03-13T12:00:00-05:00",
            "title": "Mt. Pinatubo Aerosols",
            "description": "Global aerosol data in the period around the Mt. Pinatubo eruption || a000074.00005_web.png (720x480) [470.6 KB] || a000074_thm.png (80x40) [4.7 KB] || a000074_pre.jpg (320x238) [7.9 KB] || a000074_pre_searchweb.jpg (320x180) [37.5 KB] || a000074.webmhd.webm (960x540) [2.9 MB] || a000074.dv (720x480) [66.3 MB] || a000074.mp4 (640x480) [3.7 MB] || a000074.mpg (352x240) [2.4 MB] || ",
            "hits": 67
        }
    ]
}