{
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    "results": [
        {
            "id": 3970,
            "url": "https://svs.gsfc.nasa.gov/3970/",
            "result_type": "Visualization",
            "release_date": "2012-08-04T15:00:00-04:00",
            "title": "Summer Temperature Anomalies for the Northern Hemisphere, 1955-2011",
            "description": "This visualization shows a flat map of the Earth with summertime temperature anomalies for the Northern Hemisphere. This analysis compares observed seasonal mean temperatures (June-July-August) to the seasonal mean temperatures during a base period from 1951 to 1980.The colors correspond to statistical standard deviations from the seasonal mean of the base period. The hot anomalies are defined as \"hot\" (orange); \"very hot\" (red); and \"extremely hot\" (bown). The cold anomalies are defined as \"cold\" (light blue); \"very cold\" (dark blue); and \"extremely cold\" (purple). Regions in white fall within the normal category.The visualization shows the increasing occurrence, in particular, of \"extremely hot\" temperatures since 2000. While these temperatures were experienced by less than 1 percent of land areas during the base period, about 10 percent of land areas have experienced these summer temperatures since 2000. These extreme heat events include the heat waves in Europe in 2003, Russia in 2010, and Texas and Oklahoma in 2011.No data is shown below the equator because this only uses Northern Hemisphere June-July-August temperature data. The visualization shows the data for 1955, 1965, 1975 and then 1985-2011. || ",
            "hits": 27
        },
        {
            "id": 3975,
            "url": "https://svs.gsfc.nasa.gov/3975/",
            "result_type": "Visualization",
            "release_date": "2012-08-04T15:00:00-04:00",
            "title": "Shifting Distribution of Northern Hemisphere Summer Temperature Anomalies, 1951-2011",
            "description": "This bell curve graph shows how the distribution of Northern Hemisphere summer temperature anomalies has shifted toward an increase in hot summers. The seasonal mean temperature for the entire base period of 1951-1980 is plotted at the top of the bell curve. Decreasing in frequency to the right are what are defined as \"hot\" anomalies (between 1 and 2 standard deviations from the norm), \"very hot\" anomalies (between 2 and 3 standard deviations) and \"extremely hot\" anomalies (greater than 3 standard deviations). The anomalies fall off to the left in mirror-image categories of \"cold, \"very cold\" and \"extremely cold.\" The range between the .43 and -.43 standard deviation marks represent \"normal\" temperatures. As the graph moves forward in time, the bell curve shifts to the right, representing an increase in the frequency of the various hot anomalies. It also gets wider and shorter, representing a wider range of temperature extremes. As the graph moves beyond 1980, the temperatures are still compared to the seasonal mean of the 1951-1980 base period, so that as it reaches the 21st century, there is a far greater frequency of temperatures that once fell 3 standard deviations beyond the mean.  As the graphic indicates, each bell curve shown through the time series represents the distribution of anomalies over an 11-year period. || ",
            "hits": 50
        }
    ]
}