{
    "count": 5,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 3672,
            "url": "https://svs.gsfc.nasa.gov/3672/",
            "result_type": "Visualization",
            "release_date": "2010-01-05T00:00:00-05:00",
            "title": "28 Year Arctic Temperature Trend",
            "description": "Scientists who study the Arctic region consider this area to be an early indicator of global warming, because changes in this area are amplified by the high albedo of the snow and ice. This animation depicts the 28-year surface temperature trend over the Arctic region determined from data collected between August 1981 and July 2009. The warming and cooling regions are shown in steps of .02 degrees Kelvin per year from the regions of greatest change to the areas of least change. Blue hues indicate cooling regions; red hues depict warming. The neutral region of -.02 to +.02 is shown in white. Light regions indicate less change while darker regions indicate more. The temperature scale used ranges from -0.42 to +0.42 degrees Kelvin, although the minimum data value is -0.1825 degrees Kelvin per year while the maximum value is 0.4185. || ",
            "hits": 114
        },
        {
            "id": 3676,
            "url": "https://svs.gsfc.nasa.gov/3676/",
            "result_type": "Visualization",
            "release_date": "2010-01-05T00:00:00-05:00",
            "title": "28 Year Arctic Winter Seasonal Temperature Trend",
            "description": "The Arctic region has been an area of scientific interest because it is expected that global warming signals will be amplified in the region because of ice-albedo feedback effect. Such effect is associated with the high albedo of snow and sea ice covered areas compared to that of ice free ocean and land areas. This animation depicts the 28-year winter seasonal surface temperature trend over the Arctic region determined from data collected during the months of December, January and February between 1981 and 2009. In this animation, the warming and cooling regions are revealed in steps of .02 degrees change per year starting with the regions of greatest change and progressing to the areas of least change. Blue hues indicate cooling regions while red hues depict warming. The neutral region of -.01 to +.01 degrees is shown in white. Brighter regions indicate greater temperature change while light regions indicate less. On the left side, the colarbar shows cooling temperatures ranging from -0.42 to zero degrees Kelvin, while the colorbar on the right shows warming temperatures ranging from zero to +0.42 degrees Kelvin per year. A moving bar beside each colorbar indicates the range of data values being displayed. || ",
            "hits": 89
        },
        {
            "id": 3677,
            "url": "https://svs.gsfc.nasa.gov/3677/",
            "result_type": "Visualization",
            "release_date": "2010-01-05T00:00:00-05:00",
            "title": "28 Year Arctic Spring Seasonal Temperature Trend",
            "description": "The Arctic region has been an area of scientific interest because it is expected that global warming signals will be amplified in the region because of ice-albedo feedback effect. Such effect is associated with the high albedo of snow and sea ice covered areas compared to that of ice free ocean and land areas. This animation depicts the 28-year spring seasonal surface temperature trend over the Arctic region determined from data collected during the months of March, April and May between 1982 and 2009.In this animation, the warming and cooling regions are revealed in steps of .02 degrees change per year starting with the regions of greatest change and progressing to the areas of least change. Blue hues indicate cooling regions while red hues depict warming. The neutral region of -.01 to +.01 degrees is shown in white. Brighter regions indicate greater temperature change while light regions indicate less. On the left side, the colarbar shows cooling temperatures ranging from -0.42 to zero degrees Kelvin, while the colorbar on the right shows warming temperatures ranging from zero to +0.42 degrees per year. An animated bar beside each colorbar brackets the range of data values being displayed. || ",
            "hits": 26
        },
        {
            "id": 3678,
            "url": "https://svs.gsfc.nasa.gov/3678/",
            "result_type": "Visualization",
            "release_date": "2010-01-05T00:00:00-05:00",
            "title": "28 Year Arctic Summer Seasonal Temperature Trend",
            "description": "The Arctic region has been an area of scientific interest because it is expected that global warming signals will be amplified in the region because of ice-albedo feedback effect. Such effect is associated with the high albedo of snow and sea ice covered areas compared to that of ice free ocean and land areas. This animation depicts the 28-year summer seasonal surface temperature trend over the Arctic region determined from data collected during the months of June, July and August between 1982 and 2009.In this animation, the warming and cooling regions are revealed in steps of .02 degrees change per year starting with the regions of greatest change and progressing to the areas of least change. Blue hues indicate cooling regions while red hues depict warming. The neutral region of -.01 to +.01 degrees is shown in white. Brighter regions indicate greater temperature change while light regions indicate less. On the left side, the colarbar shows cooling temperatures ranging from -0.42 to zero degrees Kelvin, while the colorbar on the right shows warming temperatures ranging from zero to +0.42 degrees per year. An animated bar beside each colorbar brackets the range of data values being displayed. || ",
            "hits": 44
        },
        {
            "id": 3679,
            "url": "https://svs.gsfc.nasa.gov/3679/",
            "result_type": "Visualization",
            "release_date": "2010-01-05T00:00:00-05:00",
            "title": "28 Year Arctic Autumn Seasonal Temperature Trend",
            "description": "The Arctic region has been an area of scientific interest because it is expected that global warming signals will be amplified in the region because of ice-albedo feedback effect. Such effect is associated with the high albedo of snow and sea ice covered areas compared to that of ice free ocean and land areas. This animation depicts the 28-year autumn seasonal surface temperature trend over the Arctic region determined from data collected during the months of September, October and November between 1981 and 2008.In this animation, the warming and cooling regions are revealed in steps of .02 degrees change per year starting with the regions of greatest change and progressing to the areas of least change. Blue hues indicate cooling regions while red hues depict warming. The neutral region of -.01 to +.01 degrees is shown in white. Brighter regions indicate greater temperature change while light regions indicate less. On the left side, the colarbar shows cooling temperatures ranging from -0.42 to zero degrees Kelvin, while the colorbar on the right shows warming temperatures ranging from zero to +0.42 degrees per year. An animated bar beside each colorbar brackets the range of data values being displayed. || ",
            "hits": 31
        }
    ]
}