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

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:	[Graduate Institute of Astronomy] journal & Dissertation

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