{
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    "results": [
        {
            "id": 108,
            "url": "https://svs.gsfc.nasa.gov/108/",
            "result_type": "Visualization",
            "release_date": "1996-03-22T12:00:00-05:00",
            "title": "Assimilation of N2O in the Upper Atmosphere Using a Kalman Filter: N2O Mixing Ratio",
            "description": "This series of animations shows assimilation of N2O in the upper atmosphere using observations from the Cryogenic Limb Etalon Spectrometer (CLAES) on the Upper Atmosphere Research Satellite (UARS). Winds were provided by the Goddard EOS Data Assimilation System (GEOS-DAS). Flow is at the 850K isentropic level. N2O mixing ratio is expressed in parts per billion volume (ppbv). || ",
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            "url": "https://svs.gsfc.nasa.gov/1394/",
            "result_type": "Visualization",
            "release_date": "1996-03-22T12:00:00-05:00",
            "title": "Assimilation of N2O in the Upper Atmosphere Using a Kalman Filter: Error Correlation",
            "description": "This series of animations shows assimilation of N2O in the upper atmosphere using observations from the Cryogenic Limb Etalon Spectrometer (CLAES) on the Upper Atmosphere Research Satellite (UARS). Winds were provided by the Goddard EOS Data Assimilation System (GEOS-DAS). Flow is at the 850K isentropic level. N2O mixing ratio is expressed in parts per billion volume (ppbv). || ",
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