中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Cross-Shelf Carbon Transport in the East China Sea and Its Future Trend Under Global Warming

文献类型:期刊论文

作者Hao, Jiajia2,4,5; Yuan, Dongliang1,2,4,5,11; He, Lei9,10; Yuan, Huamao2,8,11; Su, Jian7; Pohlmann, Thomas3; Ran, Xiangbin6
刊名JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
出版日期2024
卷号129期号:1页码:19
ISSN号2169-9275
关键词cross-shelf transport carbon transport East China Sea global warming
DOI10.1029/2022JC019403
通讯作者Yuan, Dongliang(dyuan@fio.org.cn) ; He, Lei(helei23@mail.sysu.edu.cn)
英文摘要The cross-shelf carbon transports across a section along the 100 m isobath from Taiwan to Cheju are estimated based on carbon concentration observations and ocean currents simulated by a regionally zoomed ocean-atmosphere coupled model. Results show that the net cross-shelf particulate organic carbon, dissolved organic carbon, and dissolved inorganic carbon transports are in the offshore direction at 1.81 +/- 0.22, 51.8 +/- 2.85, and 783 +/- 58.9 TgC yr-1, respectively, which are high in spring and summer and low in winter and fall following the seasonality of the offshore volume transport. The carbon is transported into the East China Sea (ECS) mainly by the Taiwan Warm Current and the Yellow Sea Warm Current, whereas they are carried out of the ECS mainly by the East China Sea Current extension and the recirculation north of Taiwan. Assuming steady biological activity, future net total organic carbon transports are projected to increase by 5%similar to 19% offshore at the end of the 21st century, with the maximum increase in winter, in a high greenhouse gas emission scenario of RCP8.5. The increased carbon transports are due to the increased offshore volume transport, transferring more carbon-rich coastal water away from the shelf in the warming future than at present. The results quantify cross-shelf carbon burial in the ECS in the background of global warming. Carbon transport due to water exchange between the continental shelf and the open ocean is one of the most important components of the world ocean carbon budgets. In this study, the cross-shelf carbon transport in the East China Sea (ECS) is estimated based on in situ carbon concentration observations and simulated ocean currents by an ocean-atmosphere coupled model. The use of the simulated currents is to avoid a bogus volume surplus in the estimates of the carbon transports. The offshore and the onshore volume transports, with significantly different carbon concentrations, are found to have a strong seasonal cycle and increase in the background of global warming, both of which are much larger than their difference, a.k.a. the net volume transport. As a result, the net cross-shelf carbon transports are in the offshore direction and are high in spring and summer and low in winter and fall. The organic carbon transports are projected to increase due to the ongoing global warming. These changes in the carbon burial need to be considered when assessing the impact of human activities and warming on the global carbon cycle. Our work would provide scientific evidence for increasing carbon sinks in the ECS in the warming future. Carbon transports across the ECS shelf were estimated based on carbon concentration observations and simulated currentsOffshore carbon transports are found induced by the ECSC from the inner shelf to the shelf breakThe organic carbon transports are projected to increase with the global warming at the end of the 21st century
WOS关键词YELLOW SEA ; ORGANIC-CARBON ; CO2 FLUXES ; MATTER ; DISTRIBUTIONS ; VARIABILITY ; CIRCULATION ; IMPACTS ; EDDIES ; TAIWAN
资助项目CAS ; NSFC[42149902] ; NSFC[92258301] ; NSFC[2020YFA0608800] ; National Key R&D Program of China[NORC2011-06] ; The Taishan Scholar Program ; The Kunpeng Outstanding Scholar Project of the FIO/MNR of China ; NSFC Open Research Cruise[NORC2013-02] ; NSFC Open Research Cruise[NORC2014-02] ; CODC, IOCAS ; [41576016]
WOS研究方向Oceanography
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:001149698000001
源URL[http://ir.qdio.ac.cn/handle/337002/184320]  
专题海洋研究所_海洋环流与波动重点实验室
海洋研究所_海洋生态与环境科学重点实验室
通讯作者Yuan, Dongliang; He, Lei
作者单位1.Minist Nat Resources, Inst Oceanog 1, Key Lab Marine Sci & Numer Modeling, Shandong Key Lab Marine Sci & Numer Modeling, Qingdao, Peoples R China
2.Laoshan Lab, Qingdao, Peoples R China
3.Univ Hamburg, Inst Oceanog, Ctr Earth Syst Res & Sustainabil, Hamburg, Germany
4.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
5.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China
6.Minist Nat Resources, Inst Oceanog 1, Res Ctr Marine Ecol, Qingdao, Peoples R China
7.Danish Meteorol Inst, Copenhagen, Denmark
8.Chinese Acad Sci, Inst Oceanol, Ctr Ocean Mega Sci, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China
9.Guangdong Prov Key Lab Marine Resources & Coastal, Zhuhai, Peoples R China
10.Sun Yat Sen Univ, Sch Marine Sci, Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai, Peoples R China
推荐引用方式
GB/T 7714
Hao, Jiajia,Yuan, Dongliang,He, Lei,et al. Cross-Shelf Carbon Transport in the East China Sea and Its Future Trend Under Global Warming[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2024,129(1):19.
APA Hao, Jiajia.,Yuan, Dongliang.,He, Lei.,Yuan, Huamao.,Su, Jian.,...&Ran, Xiangbin.(2024).Cross-Shelf Carbon Transport in the East China Sea and Its Future Trend Under Global Warming.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,129(1),19.
MLA Hao, Jiajia,et al."Cross-Shelf Carbon Transport in the East China Sea and Its Future Trend Under Global Warming".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 129.1(2024):19.

入库方式: OAI收割

来源:海洋研究所

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