{
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    "next": null,
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    "results": [
        {
            "id": 30548,
            "url": "https://svs.gsfc.nasa.gov/30548/",
            "result_type": "Hyperwall Visual",
            "release_date": "2014-11-18T00:00:00-05:00",
            "title": "Montage of early data from Aura's Microwave Limb Sounder",
            "description": "Montage of six measurements made by MLS || montage_early_data_aura_microwave_limb_sounder_print.jpg (1024x576) [59.6 KB] || montage_early_data_aura_microwave_limb_sounder_web.png (320x180) [40.8 KB] || montage_early_data_aura_microwave_limb_sounder_web.jpg (320x180) [11.6 KB] || montage_early_data_aura_microwave_limb_sounder_searchweb.png (180x320) [40.8 KB] || montage_early_data_aura_microwave_limb_sounder_thm.png (80x40) [4.4 KB] || mls_montage_720p.webm (1280x720) [1.3 MB] || mls_montage_720p.mp4 (1280x720) [1.3 MB] || mls_montage_1080p.mp4 (1920x1080) [2.3 MB] || montage_early_data_aura_microwave_limb_sounder.tif (5760x3240) [19.2 MB] || mls_montage_360p.mp4 (640x360) [523.1 KB] || mls_montage_2304p.mp4 (4096x2304) [6.4 MB] || Montage_early_data_Aura_Microwave_Limb_S.pptx [1.9 MB] || Montage_early_data_Aura_Microwave_Limb_S.key [4.3 MB] || ",
            "hits": 19
        },
        {
            "id": 3088,
            "url": "https://svs.gsfc.nasa.gov/3088/",
            "result_type": "Visualization",
            "release_date": "2005-01-27T12:00:00-05:00",
            "title": "Chlorine Monoxide from new Microwave Limb Sounder on Aura (WMS)",
            "description": "Chlorine monoxide (ClO) in the atmosphere as measured by the Microwave Limb Sounder (MLS) instrument on NASA's Aura satellite. MLS can simultaneously measure several trace gases and ozone-destroying chemicals in the upper troposphere and photosphere. In this series of animations we present chlorine monoxide (ClO), hydrogen chloride (HCl), nitric acid (HNO3), ozone (O3), water vapor (H2O) and temperature measurements. These are 'first light' data taken when the MLS was operated for the first time. ClO is a temporary byproduct of the chemical reaction sequence by which chlorine from chlorofluorocarbons (CFCs) destroys ozone. || ",
            "hits": 24
        },
        {
            "id": 3056,
            "url": "https://svs.gsfc.nasa.gov/3056/",
            "result_type": "Visualization",
            "release_date": "2004-12-14T12:00:00-05:00",
            "title": "New Data from Aura's Microwave Limb Sounder (MLS) Chlorine Monoxide",
            "description": "The Microwave Limb Sounder (MLS) measures the chemistry of the lower stratosphere and upper troposphere. Measuring concentration of chlorine monoxide and other chemicals. Chlorine monoxide (CIO) is formed by the photolysis of CFCs in the stratosphere and the subsequent destruction of an ozone molecule, these radicals can act as a catalyst in the destruction of ozone while not being destroyed themselves. || ",
            "hits": 39
        },
        {
            "id": 3062,
            "url": "https://svs.gsfc.nasa.gov/3062/",
            "result_type": "Visualization",
            "release_date": "2004-12-14T12:00:00-05:00",
            "title": "The Microwave Limb Sounder Observes the Lower Stratosphere and Upper Troposphere",
            "description": "MLS measures lower stratospheric temperature and concentrations of H2O, O3, ClO, BrO, HCl, OH, HO2, HNO3, HCN, and N2O, for their effects on (and diagnoses of) ozone depletion, transformations of greenhouse gases, and radiative forcing of climate change. || ",
            "hits": 61
        },
        {
            "id": 837,
            "url": "https://svs.gsfc.nasa.gov/837/",
            "result_type": "Visualization",
            "release_date": "1999-04-09T12:00:00-04:00",
            "title": "Ozone and Chlorine Monoxide over Antarctica from MLS (1/12/93 - 9/17/93)",
            "description": "The  Microwave Limb Sounder (MLS) measures microwave emission from ozone and chlorine monoxide, a major ozone destroying radical.  Right after UARS was launched, MLS began to measure large concentrations of chlorine monoxide over the south pole.  These dramatic images clearly showed the extent of the south polar ozone destruction and confirmed the connection between man-made chlorine and the formation to  the Antarctic ozone hole. Why is so much  chlorine monoxide found over the Antarctic?  UARS measurements have confirmed that CFCs enter the stratosphere in the tropics.  As they rise above the ozone layer, ultraviolet molecules release chlorine, which then can react with methane to form hydrogen chloride.  Chlorine can also react with ozone forming the radical chlorine monoxide.  Chlorine monoxide then combines with the radical nitrogen dioxide to form stable chlorine nitrate.  Chlorine nitrate and hydrogen chloride are called reservoir gases for the chlorine radical.  These reservoir gases usually contain more than ninety percent of the chlorine in the lower stratosphere. || ",
            "hits": 61
        },
        {
            "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": 54
        }
    ]
}