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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