Global air-sea surface carbon dioxide transfer velocity and flux estimated using 17 a altimeter data and a new algorithm
Yu Tan1,2,3,5,6; He Yijun3; Yan Xiaohai4
刊名ACTA OCEANOLOGICA SINICA
2013-10-01
卷号32期号:10页码:24-33
关键词altimeter remote sensing sea surface carbon dioxide transfer velocity carbon dioxide flux
ISSN号0253-505X
通讯作者He, YJ
中文摘要The global distributions of the air-seaCO(2) transfer velocity and flux are retrieved from TOPEX/Poseidon and Jason altimeter data from October 1992 to December 2009 using a combined algorithm. The 17 a average global, area-weighted, Schmidt number-corrected mean gas transfer velocity is 21.26 cm/h, and the full exploration of the uncertainty of this estimate awaits further data. The average total CO2 flux (calculated by carbon) from atmosphere to ocean during the 17 a was 2.58 Pg/a. The highest transfer velocity is in the circumpolar current area, because of constant high wind speeds and currents there. This results in strongCO(2) fluxes. CO2 fluxes are strong but opposite direction in the equatorial east Pacific Ocean, because the air-sea CO2 partial pressure difference is the largest in the global oceans. The results differ from the previous studies calculated using the wind speed. It is demonstrated that the air-sea transfer velocity is very important for estimating air-sea CO2 flux. It is critical to have an accurate estimation for improving calculation of CO2 flux within climate change studies.
英文摘要The global distributions of the air-seaCO(2) transfer velocity and flux are retrieved from TOPEX/Poseidon and Jason altimeter data from October 1992 to December 2009 using a combined algorithm. The 17 a average global, area-weighted, Schmidt number-corrected mean gas transfer velocity is 21.26 cm/h, and the full exploration of the uncertainty of this estimate awaits further data. The average total CO2 flux (calculated by carbon) from atmosphere to ocean during the 17 a was 2.58 Pg/a. The highest transfer velocity is in the circumpolar current area, because of constant high wind speeds and currents there. This results in strongCO(2) fluxes. CO2 fluxes are strong but opposite direction in the equatorial east Pacific Ocean, because the air-sea CO2 partial pressure difference is the largest in the global oceans. The results differ from the previous studies calculated using the wind speed. It is demonstrated that the air-sea transfer velocity is very important for estimating air-sea CO2 flux. It is critical to have an accurate estimation for improving calculation of CO2 flux within climate change studies.
学科主题Oceanography
WOS标题词Science & Technology ; Physical Sciences
类目[WOS]Oceanography
研究领域[WOS]Oceanography
关键词[WOS]GAS TRANSFER VELOCITY ; CO2 TRANSFER VELOCITY ; WIND-SPEED ; SATELLITE ALTIMETERS ; TIME-SERIES ; WAVE PERIOD ; IN-SITU ; OCEAN ; EXCHANGE ; PARAMETERIZATION
收录类别SCI
原文出处10.1007/s13131-013-0362-9
语种英语
WOS记录号WOS:000325965500005
公开日期2014-07-17
内容类型期刊论文
源URL[http://ir.qdio.ac.cn/handle/337002/16410]  
专题海洋研究所_海洋环流与波动重点实验室
作者单位1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing 210044, Jiangsu, Peoples R China
4.Univ Delaware, Ctr Remote Sensing, Newark, DE 19716 USA
5.Chinese Acad Sci, Inst Oceanol, Chinese Acad Sci Ocean Circulat & Waves KLOCAW, Key Lab, Qingdao 266071, Peoples R China
6.Shanghai Ocean Univ, Coll Marine Sci, Shanghai 201306, Peoples R China
推荐引用方式
GB/T 7714
Yu Tan,He Yijun,Yan Xiaohai. Global air-sea surface carbon dioxide transfer velocity and flux estimated using 17 a altimeter data and a new algorithm[J]. ACTA OCEANOLOGICA SINICA,2013,32(10):24-33.
APA Yu Tan,He Yijun,&Yan Xiaohai.(2013).Global air-sea surface carbon dioxide transfer velocity and flux estimated using 17 a altimeter data and a new algorithm.ACTA OCEANOLOGICA SINICA,32(10),24-33.
MLA Yu Tan,et al."Global air-sea surface carbon dioxide transfer velocity and flux estimated using 17 a altimeter data and a new algorithm".ACTA OCEANOLOGICA SINICA 32.10(2013):24-33.
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