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    Please use this identifier to cite or link to this item: http://ir.lib.ncu.edu.tw/handle/987654321/33811


    Title: Seasonal cycle of (COO)-O-16-O-16, (COO)-O-16-O-17, and (COO)-O-16-O-18 in the middle atmosphere: Implications for mesospheric dynamics and biogeochemical sources and sinks of CO2
    Authors: Liang,Mao-Chang;Blake,Geoffrey A.;Yung,Yuk L.
    Contributors: 天文研究所
    Keywords: ABSORPTION CROSS-SECTION;OXYGEN ISOTOPIC FRACTIONATION;GLOBAL 3-DIMENSIONAL MODEL;CARBON-DIOXIDE;NITROUS-OXIDE;TEMPERATURE-DEPENDENCE;STRATOSPHERIC CO2;MEAN AGES;OZONE;PHOTODISSOCIATION
    Date: 2008
    Issue Date: 2010-07-07 11:49:23 (UTC+8)
    Publisher: 中央大學
    Abstract: The isotopic anomaly of oxygen in atmospheric CO2 is caused by exchange reactions with isotopically anomalous O(D-1) in the middle atmosphere. In the stratosphere, the major source of O(D-1) is O-3 photolysis; O-3 is known to possess mass-independent isot
    Relation: JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES????
    Appears in Collections:[天文研究所] 期刊論文

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