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    "results": [
        {
            "id": 3684,
            "url": "https://svs.gsfc.nasa.gov/3684/",
            "result_type": "Visualization",
            "release_date": "2010-03-03T00:00:00-05:00",
            "title": "Five-Year Average Global Temperature Anomalies from 1881 to 2009 for Science On a Sphere",
            "description": "Each year, scientists at NASA Goddard Institute for Space Studies analyze global temperature data. The past year, 2009, tied as the second warmest year in the 130 years of global instrumental temperature records, in the surface temperature analysis of the NASA Goddard Institute for Space Studies (GISS). The Southern Hemisphere set a record as the warmest year for that half of the world. Global mean temperature, was 0.57°C (1.0°F) warmer than climatology (the 1951-1980 base period). Southern Hemisphere mean temperature was 0.49°C (0.88°F) warmer than in the period of climatology. The global record warm year, in the period of near-global instrumental measurements (since the late 1800s), was 2005. This color-coded map displays a long term progression of changing global surface temperatures, from 1881 to 2009. Dark red indicates the greatest warming and dark blue indicates the greatest cooling. For more information on the data used to generate these images, please see http://data.giss.nasa.gov/gistemp. || ",
            "hits": 91
        },
        {
            "id": 3674,
            "url": "https://svs.gsfc.nasa.gov/3674/",
            "result_type": "Visualization",
            "release_date": "2010-01-27T13:00:00-05:00",
            "title": "Five-Year Average Global Temperature Anomalies from 1881 to 2009",
            "description": "Each year, scientists at NASA Goddard Institute for Space Studies analyze global temperature data. The past year, 2009, tied as the second warmest year in the 130 years of global instrumental temperature records, in the surface temperature analysis of the NASA Goddard Institute for Space Studies (GISS). The Southern Hemisphere set a record as the warmest year for that half of the world. Global mean temperature, was 0.57°C (1.0°F) warmer than climatology (the 1951-1980 base period). Southern Hemisphere mean temperature was 0.49°C (0.88°F) warmer than in the period of climatology. The global record warm year, in the period of near-global instrumental measurements (since the late 1800s), was 2005. This color-coded map displays a long term progression of changing global surface temperatures, from 1881 to 2009. Dark red indicates the greatest warming and dark blue indicates the greatest cooling. For more information on the data used to generate these images, please see http://giss.nasa.gov/gistemp/ || ",
            "hits": 29
        },
        {
            "id": 3675,
            "url": "https://svs.gsfc.nasa.gov/3675/",
            "result_type": "Visualization",
            "release_date": "2010-01-26T14:00:00-05:00",
            "title": "Ten-Year Average Global Temperature Anomaly Image from 2000 to 2009",
            "description": "There is a high degree of interannual (year-to-year) and decadal variability in both global and hemispheric temperatures. Underlying this variability, however, is a long-term warming trend that has become strong and persistent over the past three decades. The long-term trends are more apparent when temperature is averaged over several years. This image represents the 10 year average temperatures anomaly data from 2000 through 2009. || ",
            "hits": 44
        },
        {
            "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": 88
        },
        {
            "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": 93
        },
        {
            "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": 18
        },
        {
            "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": 56
        },
        {
            "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": 34
        },
        {
            "id": 3506,
            "url": "https://svs.gsfc.nasa.gov/3506/",
            "result_type": "Visualization",
            "release_date": "2008-04-23T00:00:00-04:00",
            "title": "Surface Temperature of the Greenland Ice Sheet During the Summer of 2005",
            "description": "The surface temperature of the Greenland Ice Sheet is a sensitive indicator of surface melt extent, frequency, timing and duration. The daily clear-sky surface temperature of the Greenland Ice Sheet was measured using MODIS-derived land surface temperature (LST) data-product maps. For this animation, an 8-day moving average of clear-sky surface temperature was generated from May 1 through September 1, 2005. Coldest temperatures are shown here in violet and blue, while warmer temperatures nearing the melting point of zero degrees centigrade are shown in orange and red. The summer season is repeated two times in this animation. || ",
            "hits": 39
        },
        {
            "id": 3036,
            "url": "https://svs.gsfc.nasa.gov/3036/",
            "result_type": "Visualization",
            "release_date": "2005-01-12T12:00:00-05:00",
            "title": "Daily Sea Ice Surface Temperature 2002-2003 (WMS)",
            "description": "This animation shows the daily sea ice surface temperature over the northern hemisphere from September 2002 through May 2003. The sea ice surface temperature was measured by the MODIS instrument on the Aqua satellite. Since this instrument cannot take measurements through clouds or in the dark, in dark or cloud-covered regions or areas with suspect data quality, the prior day's value is retained until a valid data reading is obtained. The color of the sea ice indicates the sea ice surface temperature. || ",
            "hits": 7
        },
        {
            "id": 3037,
            "url": "https://svs.gsfc.nasa.gov/3037/",
            "result_type": "Visualization",
            "release_date": "2005-01-11T12:00:00-05:00",
            "title": "Sea Ice Surface Temperature with Regions of No Data Indicated (WMS)",
            "description": "This animation shows the daily sea ice surface temperature over the northern hemisphere from September 2002 through May 2003. The sea ice surface temperature was measured by the MODIS instrument on the Aqua satellite. Since this instrument cannot take measurements through clouds, in cloud-covered regions or areas with suspect data quality, the prior day's value is retained until a valid data reading is obtained. The satellite instruments are also unable to collect data in the dark, so the region around the pole is shown here with a gray cap that grows and shrinks, indicating the region in polar darkness. The color of the sea ice indicates the sea ice surface temperature. || ",
            "hits": 9
        },
        {
            "id": 3047,
            "url": "https://svs.gsfc.nasa.gov/3047/",
            "result_type": "Visualization",
            "release_date": "2004-12-13T12:00:00-05:00",
            "title": "22-Year Arctic Surface Temperature Trend",
            "description": "This image shows the 22-year surface temperature trend over the Arctic region.  Blue hues indicate areas that are cooling; gold hues depict areas that are warming.  Lighter colors indicate less change while darker colors indicate more. The temperature scale steps from zero degrees Celsius in increments of .02 degrees. (See color bar below)  The data ranges from -0.162 to +0.487 degrees Celsius. || ",
            "hits": 18
        },
        {
            "id": 2567,
            "url": "https://svs.gsfc.nasa.gov/2567/",
            "result_type": "Visualization",
            "release_date": "2002-10-09T12:00:00-04:00",
            "title": "Land Surface Temperature",
            "description": "The average temperature of the land is one component of a model used to predict the areas where mosquitos will flourish and where they will not. Satellite remote sensing can help construct maps of the average land surface temperature. These images were created in support of a story describing how NASA is assisting the CDC and EPA in tracking the spread of West Nile Virus. || ",
            "hits": 23
        }
    ]
}