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

NCU Institutional Repository > 理學院 > 天文研究所 > 期刊論文 > Item 987654321/33811

請使用永久網址來引用或連結此文件: http://ir.lib.ncu.edu.tw/handle/987654321/33811

題名:	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
作者:	Liang,Mao-Chang;Blake,Geoffrey A.;Yung,Yuk L.
貢獻者:	天文研究所
關鍵詞:	ABSORPTION CROSS-SECTION;OXYGEN ISOTOPIC FRACTIONATION;GLOBAL 3-DIMENSIONAL MODEL;CARBON-DIOXIDE;NITROUS-OXIDE;TEMPERATURE-DEPENDENCE;STRATOSPHERIC CO2;MEAN AGES;OZONE;PHOTODISSOCIATION
日期:	2008
上傳時間:	2010-07-07 11:49:23 (UTC+8)
出版者:	中央大學
摘要:	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
關聯:	JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES????
顯示於類別:	[天文研究所] 期刊論文

文件中的檔案:

檔案	描述	大小	格式	瀏覽次數
index.html		0Kb	HTML	489	檢視/開啟

在NCUIR中所有的資料項目都受到原著作權保護.

社群 sharing