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DOI | 10.1073/pnas.1908670117 |
Timing and magnitude of southern ocean sea ice/carbon cycle feedbacks | |
Stein K.; Timmermann A.; Kwon E.Y.; Friedrich T. | |
发表日期 | 2020 |
ISSN | 0027-8424 |
起始页码 | 4498 |
结束页码 | 4504 |
卷号 | 117期号:9 |
英文摘要 | The Southern Ocean (SO) played a prominent role in the exchange of carbon between ocean and atmosphere on glacial timescales through its regulation of deep ocean ventilation. Previous studies indicated that SO sea ice could dynamically link several processes of carbon sequestration, but these studies relied on models with simplified ocean and sea ice dynamics or snapshot simulations with general circulation models. Here, we use a transient run of an intermediate complexity climate model, covering the past eight glacial cycles, to investigate the orbital-scale dynamics of deep ocean ventilation changes due to SO sea ice. Cold climates increase sea ice cover, sea ice export, and Antarctic Bottom Water formation, which are accompanied by increased SO upwelling, stronger poleward export of Circumpolar Deep Water, and a reduction of the atmospheric exposure time of surface waters by a factor of 10. Moreover, increased brine formation around Antarctica enhances deep ocean stratification, which could act to decrease vertical mixing by a factor of four compared with the current climate. Sensitivity tests with a steady-state carbon cycle model indicate that the two mechanisms combined can reduce atmospheric carbon by 40 ppm, with ocean stratification acting early within a glacial cycle to amplify the carbon cycle response. © 2020 National Academy of Sciences. All rights reserved. |
英文关键词 | Carbon cycle; Glacial cycles; Sea ice; Southern Ocean |
语种 | 英语 |
scopus关键词 | ice; surface water; air conditioning; Article; atmosphere; biogeochemistry; carbon cycle; cold climate; concentration (parameter); environmental exposure; priority journal; sea ice; simulation; Southern Ocean; steady state |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/160312 |
作者单位 | Stein, K., Center for Climate Physics, Institute for Basic Science, Busan, 46241, South Korea, Pusan National University, Busan, 46241, South Korea; Timmermann, A., Center for Climate Physics, Institute for Basic Science, Busan, 46241, South Korea, Pusan National University, Busan, 46241, South Korea; Kwon, E.Y., Center for Climate Physics, Institute for Basic Science, Busan, 46241, South Korea, Pusan National University, Busan, 46241, South Korea; Friedrich, T., Department of Oceanography, University of Hawai'i at Mānoa, Honolulu, HI 96822, United States |
推荐引用方式 GB/T 7714 | Stein K.,Timmermann A.,Kwon E.Y.,et al. Timing and magnitude of southern ocean sea ice/carbon cycle feedbacks[J],2020,117(9). |
APA | Stein K.,Timmermann A.,Kwon E.Y.,&Friedrich T..(2020).Timing and magnitude of southern ocean sea ice/carbon cycle feedbacks.Proceedings of the National Academy of Sciences of the United States of America,117(9). |
MLA | Stein K.,et al."Timing and magnitude of southern ocean sea ice/carbon cycle feedbacks".Proceedings of the National Academy of Sciences of the United States of America 117.9(2020). |
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