{
    "count": 7,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 579,
            "url": "https://svs.gsfc.nasa.gov/579/",
            "result_type": "Visualization",
            "release_date": "1999-04-09T12:00:00-04:00",
            "title": "UARS: The Upper Atmosphere Research Satellite",
            "description": "This video summarizes science and data obtained by the Upper Atmosphere Research Satellite (UARS) mission.  UARS was launched in 1991 to study ozone depletion and the processes that control the stratospheric ozone layer.  Although the mission was intended to last only 18 months, UARS continued to operate 7.5 years after launch with 8 of the 10 instruments at the time this video was made. UARS has been one of the most successful NASA satellite programs. The spacecraft was developed and is managed by NASA's Goddard Space Flight Center. || ",
            "hits": 59
        },
        {
            "id": 810,
            "url": "https://svs.gsfc.nasa.gov/810/",
            "result_type": "Visualization",
            "release_date": "1999-04-09T12:00:00-04:00",
            "title": "Viewing the ISAMS and CLAES Instruments on UARS",
            "description": "Key to understanding the chlorine chemistry in the polar stratosphere is the measurement of polar stratospheric clouds, chlorine monoxide, and the reservoir gas chlorine nitrate.  Polar stratospheric clouds  are seen by the  Improved Stratospheric and Mesospheric Sounder, ISAMS, and chlorine nitrate has been measured by the Cryogen Limb Array Etalon Spectrometer, CLAES.  Both ISAMS and CLAES make measurements by looking at  infrared emission from cloud particles and trace gases. || ",
            "hits": 45
        },
        {
            "id": 829,
            "url": "https://svs.gsfc.nasa.gov/829/",
            "result_type": "Visualization",
            "release_date": "1999-04-09T12:00:00-04:00",
            "title": "CLAES Measurements of CFC-12 in the Stratosphere",
            "description": "CLAES made the first global measurements of CFCs in the stratosphere.  CFCs enter the stratosphere through upwelling in the tropics.  The CFCs decrease with height as they are broken down by UV radiation.  CFCs are the major source of stratospheric chlorine.  Red indicates large amounts of CFC-12. || ",
            "hits": 100
        },
        {
            "id": 838,
            "url": "https://svs.gsfc.nasa.gov/838/",
            "result_type": "Visualization",
            "release_date": "1999-04-09T12:00:00-04:00",
            "title": "Chlorine Nitrate over the Arctic from CLAES (2/12/93 - 3/16/93)",
            "description": "Key to understanding the chlorine chemistry in the polar stratosphere is the measurement of polar stratospheric clouds, chlorine monoxide, and the reservoir gas chlorine nitrate.  Chlorine nitrate has been measured by the Cryogen Limb Array Etalon Spectrometer, CLAES.  CLAES makes measurements by looking at infrared emission from cloud particles and trace gases.  CLAES measurements help to show that the polar stratospheric clouds which form in the cold Arctic stratosphere have converted most  of the chlorine nitrate into the radical chlorine monoxide. In 1992, UARS measurements showed conclusively that an an Arctic ozone hole is beginning to form. || ",
            "hits": 44
        },
        {
            "id": 839,
            "url": "https://svs.gsfc.nasa.gov/839/",
            "result_type": "Visualization",
            "release_date": "1999-04-09T12:00:00-04:00",
            "title": "Chlorine Nitrate from CLAES and Chlorine Monoxide from MLS over the Arctic (2/12/93 - 3/10/93)",
            "description": "Key to understanding the chlorine chemistry in the polar stratosphere is the measurement of polar stratospheric clouds, chlorine monoxide, and the reservoir gas chlorine nitrate. Chlorine nitrate has been measured by CLAES and chlorine monoxide by MLS. The CLAES and MLS measurements together help to show that the polar stratospheric clouds which form in the cold Arctic stratosphere have converted most of the chlorine nitrate into the radical chlorine monoxide. In 1992, UARS measurements showed conclusively that an an Arctic ozone hole is beginning to form. || ",
            "hits": 60
        },
        {
            "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). || ",
            "hits": 16
        },
        {
            "id": 1394,
            "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). || ",
            "hits": 12
        }
    ]
}