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    "results": [
        {
            "id": 5509,
            "url": "https://svs.gsfc.nasa.gov/5509/",
            "result_type": "Visualization",
            "release_date": "2025-04-25T07:00:59-04:00",
            "title": "Airborne Aerosol Wind Profiler (AWP) Measurements",
            "description": "This is a visualization of Aerosol Wind Profiler (AWP) data aboard the NASA Gulfstream-III for a flight on 15 October 2024 that originated from NASA/Langley Research Center (LaRC) in Hampton, Virginia.",
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        {
            "id": 3783,
            "url": "https://svs.gsfc.nasa.gov/3783/",
            "result_type": "Visualization",
            "release_date": "2010-10-21T00:00:00-04:00",
            "title": "Iceland's Eyjafjallajökull Volcanic Ash Plume May 6-8, 2010 - Stereoscopic Version",
            "description": "During April and May, 2010, the Eyjafjallajökull volcano on Iceland's southern coast erupted, creating an expansive ash cloud that disrupted air traffic throughout Europe and across the Atlantic. This animation shows the flow of this ash cloud for three days in early May on an hourly basis as sensed from a geostationary satellite. The ash cloud heights were determined using an approach developed by NOAA/NESDIS/STAR for the next generation of Geostationary Operational Environmental Satellite (GOES-R). Data from EUMETSAT's Spinning Enhanced Visible and Infrared Imager (SEVIRI) was used as a proxy for GOES-R Advanced Baseline Imager (ABI) data. This data is shown intersecting with the CALIPSO Parallel Attenuated Backscatter curtain on May 6th. In this page the visualization content is offered in two different modes to accommodate stereoscopic systems as: Left and Right Eye separate and Left and Right Eye side-by-side combined on the same frame. || ",
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        {
            "id": 3365,
            "url": "https://svs.gsfc.nasa.gov/3365/",
            "result_type": "Visualization",
            "release_date": "2006-08-03T00:00:00-04:00",
            "title": "CALIPSO  Profile over China",
            "description": "Aerosols, small particles in the atmosphere, can be produced from natural sources, such as volcanos and dust storms, or from human activity, such as pollution from manufacturing and automobiles.   Aerosols remain in the atmosphere for long periods and travel across the globe propelled by winds.  They also affect weather and climate by reflecting or absorbing sunlight and by altering chemical reactions within the atmosphere.  The CALIOP lidar onboard the CALIPSO satellite enables scientists to collect aerosol data on slices or 'curtains' through the atmosphere.  In these images looking eastward across China over the Yellow Sea and the Korean Peninsula, slices of total attenuated backscatter show the geographic location and altitude of both aerosols and subvisible clouds in the upper troposphere.  The curtain shown here extends from sea level to a height of 20 km.  Both the height of the curtain and the terrain are exaggerated by 6x.  The near-vertical line indicates 40 degree North latitude, while the horizontal line marks 120 degree east longitude. || ",
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        {
            "id": 3366,
            "url": "https://svs.gsfc.nasa.gov/3366/",
            "result_type": "Visualization",
            "release_date": "2006-08-03T00:00:00-04:00",
            "title": "CALIPSO Profile over China, India and Bhutan",
            "description": "Aerosols, small particles in the atmosphere, can be produced from natural sources, such as volcanos and dust storms, or from human activity, such as pollution from manufacturing and automobiles. Aerosols remain in the atmosphere for long periods and travel across the globe propelled by winds. They also affect weather and climate by reflecting or absorbing sunlight and by altering chemical reactions within the atmosphere. The CALIOP lidar onboard the CALIPSO satellite enables scientists to collect aerosol data on slices or 'curtains' through the atmosphere. In these images looking east across India over the Himalayan Mountains and Bangladesh, slices of total attenuated backscatter show the geographic location and altitude of both aerosols and subvisible clouds in the upper troposphere. The curtain shown here extends from sea level to a height of 20 km. Both the height of the curtain and the terrain are exaggerated by 6x. || ",
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