{
    "count": 4,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 30190,
            "url": "https://svs.gsfc.nasa.gov/30190/",
            "result_type": "Hyperwall Visual",
            "release_date": "2013-10-17T12:00:00-04:00",
            "title": "Saharan Dust over the Atlantic",
            "description": "Easterly winds carry Saharan dust from Africa high above the North Atlantic Ocean. At left, a natural color image captured by NASA’s Aqua satellite shows the dust as it travels offshore on September 21, 2009. The dust plume is shaped by the wind, forming waves near the surface immediately offshore. An even higher, thinner tan cloud veils the surface-level dust. Dust has infiltrated into different heights of the atmosphere. Differences in wind direction at various heights in the atmosphere create the “X” near the center of the dust plume.In certain atmospheric conditions, dust from the Sahara Desert is transported clear around the globe. In fact, many scientists use space-based multi-angle imaging to track the journey of dust. Having the capability to track dust from space, provides even greater opportunities for understanding atmospheric circulation patterns at a global scale. || ",
            "hits": 25
        },
        {
            "id": 30192,
            "url": "https://svs.gsfc.nasa.gov/30192/",
            "result_type": "Hyperwall Visual",
            "release_date": "2013-10-17T12:00:00-04:00",
            "title": "Using MISR to View Dust",
            "description": "On October 18, 2002, a large dust plume extended across countries bordering the eastern Mediterranean Sea. Information on the horizontal and vertical extent of the dust are provided by these views from the Multi-angle Imaging SpectroRadiometer (MISR). The left-hand panel portrays the scene as viewed by the instrument's vertical-viewing (nadir) camera. Here only some of the dust over eastern Syria and southeastern Turkey can be discerned. The dust is much more obvious in the center panel, which is a view from MISR's most steeply forward-looking camera. The right-hand panel is an elevation field derived from automated MISR stereoscopic processing, in which the heights of clouds and certain parts of the dust plume are retrieved. Clouds within the image area are situated between about 2 and 5.5 kilometers above sea level, and the dust is located below most of the cloud, at heights of about 1.5 kilometers or less. || ",
            "hits": 22
        },
        {
            "id": 30193,
            "url": "https://svs.gsfc.nasa.gov/30193/",
            "result_type": "Hyperwall Visual",
            "release_date": "2013-10-17T12:00:00-04:00",
            "title": "Dust Storm in the Middle East",
            "description": "Dust from Syria and Iraq blows toward the northwest across Turkey and the easternmost Black Sea on July 30, 2011, when the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite acquired this natural-color image. Dust forms a giant arc extending from northern Iraq across Turkey and the easternmost Black Sea. The northeastern tip of the dust plume appears to push into western Georgia. || ",
            "hits": 37
        },
        {
            "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. || ",
            "hits": 71
        }
    ]
}