IOCAS-IR  > 海洋环流与波动重点实验室
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; He, YJ
2013-10-01
发表期刊ACTA OCEANOLOGICA SINICA
ISSN0253-505X
卷号32期号:10页码:24-33
文章类型Article
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.; 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.
关键词Altimeter Remote Sensing Sea Surface Carbon Dioxide Transfer Velocity Carbon Dioxide Flux
学科领域Oceanography
DOI10.1007/s13131-013-0362-9
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收录类别SCI
语种英语
WOS研究方向Oceanography
WOS类目Oceanography
WOS记录号WOS:000325965500005
WOS关键词GAS TRANSFER VELOCITY ; CO2 TRANSFER VELOCITY ; WIND-SPEED ; SATELLITE ALTIMETERS ; TIME-SERIES ; WAVE PERIOD ; IN-SITU ; OCEAN ; EXCHANGE ; PARAMETERIZATION
WOS标题词Science & Technology ; Physical Sciences
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被引频次:1[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/16410
专题海洋环流与波动重点实验室
通讯作者He, YJ
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
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Yu Tan,He Yijun,Yan Xiaohai,et al. 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,&He, YJ.(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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