globalchange  > 气候变化事实与影响
DOI: 10.1002/2016GB005476
Scopus记录号: 2-s2.0-85001052404
论文题名:
Anthropogenic carbon in the ocean—Surface to interior connections
作者: Groeskamp S; , Lenton A; , Matear R; , Sloyan B; M; , Langlais C
刊名: Global Biogeochemical Cycles
ISSN: 8866236
出版年: 2016
卷: 30, 期:11
起始页码: 1682
结束页码: 1698
语种: 英语
英文关键词: anthropogenic carbon ; circulation ; climate ; stream function
Scopus关键词: air-sea interaction ; Antarctic Intermediate Water ; carbon ; carbon cycle ; carbon sequestration ; circumpolar current ; coordinate ; deep water ; human activity ; oceanic circulation ; spatial distribution ; thermocline
英文摘要: Quantifying the surface to interior transport of anthropogenic carbon (CA) is critical for projecting future carbon uptake and for improved understanding of the role of the oceans in the global carbon cycle. Here we develop and apply a diagnostic tool that provides a volumetric stream function in (CA,σ0) coordinates to calculate the total diapycnal CA transport in the ocean, where σ0 is the surface referenced potential density anomaly. We combine this with air-sea fluxes of CA to infer the internal ocean mixing of CA to obtain a closed globally integrated budget analyses of the ocean's CA transport. This diagnostic separates the contribution from the mean flow, seasonal cycles, trend, surface fluxes, and mixing in the distribution and the accumulation of CA in the ocean. We find that the redistribution of CA from the surface to the interior of the ocean is due to an interplay between circulation and mixing. The circulation component is dominated by the mean flow; however, effects due to seasonal cycles are significant for the CA redistribution. The two most important pathways for CA subduction are through the transformation of thermocline water (TW) into subantarctic mode water and by transformation of Circumpolar Deep Water (CDW) into lighter Antarctic Intermediate Water. The results suggest that an accurate representation of intermediate and mode water formation, deep water formation, and spatial and temporal distribution of ocean mixing in ocean models is essential to simulate and project the oceanic uptake of CA. �2016. American Geophysical Union. All Rights Reserved.
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被引频次[WOS]:16   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/77798
Appears in Collections:气候变化事实与影响

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作者单位: Lamont-Doherty Earth Observatory, Columbia University, New York, NY, United States; CSIRO Oceans and Atmospheres, Hobart, TAS, Australia; Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, TAS, Australia

Recommended Citation:
Groeskamp S,, Lenton A,, Matear R,et al. Anthropogenic carbon in the ocean—Surface to interior connections[J]. Global Biogeochemical Cycles,2016-01-01,30(11)
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