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            "url": "https://svs.gsfc.nasa.gov/2980/",
            "result_type": "Visualization",
            "release_date": "2004-09-03T12:00:00-04:00",
            "title": "Ground Level UV Exposure",
            "description": "A large ozone hole means more ultraviolet exposure. TOMS tracks solar ultraviolet (UV-B radiation) measured at 290-320 nanometer wavelengths. Loss of stratospheric ozone has been linked to skin cancer in humans. Increased UV-B exposures for Southern continents can seriously impact phytoplankton and other species. Red is for high UV exposure and blue is for low UV exposure. || ",
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            "url": "https://svs.gsfc.nasa.gov/2216/",
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            "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. || ",
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            "result_type": "Visualization",
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            "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. || ",
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            "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. || ",
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            "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. || ",
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            "url": "https://svs.gsfc.nasa.gov/2228/",
            "result_type": "Visualization",
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            "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. || ",
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            "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. || ",
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            "url": "https://svs.gsfc.nasa.gov/2256/",
            "result_type": "Visualization",
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            "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. || ",
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            "url": "https://svs.gsfc.nasa.gov/2196/",
            "result_type": "Visualization",
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            "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. || ",
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            "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. || ",
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            "url": "https://svs.gsfc.nasa.gov/2198/",
            "result_type": "Visualization",
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            "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. || ",
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            "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)",
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            "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. || ",
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            "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. || ",
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}