{
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    "results": [
        {
            "id": 3182,
            "url": "https://svs.gsfc.nasa.gov/3182/",
            "result_type": "Visualization",
            "release_date": "2005-07-27T11:00:00-04:00",
            "title": "Global Atmospheric Sea Level Pressure during Hurricane Frances (WMS)",
            "description": "The weight of the Earth's atmosphere exerts pressure on the surface of the Earth.  This pressure varies from place-to-place due the variations in the Earth's surface since higher altitudes have less atmosphere above them than lower altitudes.  Atmospheric pressure also varies from time-to-time due to the uneven heating of the atmosphere by the sun and the rotation of the Earth, causing weather.  In order to see the changes in pressure which affect the weather, the variation due to altitude is removed from the surface pressure, creating a quantity called sea level pressure.  This animation shows the atmospheric sea level pressure for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean.  The sharp, moving low pressures areas for Frances and Songda can be clearly seen in the oceans.  Even with the direct effect of altitude removed, cold high-altitude regions such as the South Pole and the Himalayan Plateau still exhibit lower-than-normal pressures, probably due to the interaction of cold air over those regions with the warmer air in the surrounding regions. || ",
            "hits": 65
        },
        {
            "id": 3199,
            "url": "https://svs.gsfc.nasa.gov/3199/",
            "result_type": "Visualization",
            "release_date": "2005-07-27T11:00:00-04:00",
            "title": "Global Surface Latent Heat Flux during Hurricane Frances (WMS)",
            "description": "As the Sun's energy reaches the Earth, it is either reflected, absorbed by the clouds, or absorbed by the Earth's surface.  The part absorbed by the surface heats the Earth, which causes surface water to evaporate to the air, particularly over oceans or moist land.  Similarly, a cold surface causes water to condense from the air onto the land or ocean.  Latent heat flux is the amount of energy moving from the surface to the air due to evaporation (positive values) or from the air to the land due to condensation (negative values).  This animation shows the latent heat flux for the whole globe from September 1, 2004, through September 5, 2004, during the period of Hurricane Frances in the western Atlantic Ocean and Typhoon Songda in the western Pacific Ocean.  The animation clearly shows the evaporation over land only during the heat of the day, while the evaporation over the ocean is continuous throughout the day.  The highest positive latent heat flux occurs during hurricanes and typhoons, as these events are powered by the movement of heat energy from the warm ocean to the atmosphere, seen here in Hurricane Frances and Typhoon Songda.  Significant negative latent heat flux is somewhat rare and occurs over the ocean only during certain configurations of air and surface conditions. || ",
            "hits": 160
        }
    ]
}