| DOI: | 10.1175/JCLI-D-14-00481.1
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| Scopus记录号: | 2-s2.0-84942055314
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| 论文题名: | Climate-driven variability in the Southern Ocean carbonate system |
| 作者: | Conrad C.J.; Lovenduski N.S.
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| 刊名: | Journal of Climate
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| ISSN: | 8948755
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| 出版年: | 2015
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| 卷: | 28, 期:13 | | 起始页码: | 5335
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| 结束页码: | 5350
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| 语种: | 英语
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| Scopus关键词: | Acidification
; Advection
; Carbon
; Carbonation
; Climatology
; Dissolved inorganic carbon
; Interannual variability
; Ocean acidifications
; Ocean general circulation models
; Pre-industrial levels
; Seasonal and interannual variability
; Southern Annular Mode
; Surface carbonates
; Oceanography
; acidification
; advection
; air-sea interaction
; annual variation
; carbon dioxide
; El Nino-Southern Oscillation
; oceanic general circulation model
; seasonal variation
; Pacific Ocean
; Pacific Ocean (South)
; Southern Ocean
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| 英文摘要: | Seasonal and interannual variability in the Southern Ocean carbonate system is investigated using output from a historically forced (1948- 2007) ocean general circulation model with embedded biogeochemistry. Atmospheric CO2 is fixed at preindustrial levels to investigate carbonate system variability in the absence of an anthropogenic CO2 perturbation. It is found that nearly a quarter of interannual variability in Southern Ocean Pacific sector surface carbonate ion concentration ([CO2- 3 ]) can be explained by variability in ENSO, with Pacific sector surface [CO2- 3 ] decreasing by 0.43 mmolm-3 per standard deviation decrease in the ENSO-3.4 index. ENSO-related variability in vertical advection of dissolved inorganic carbon (DIC) drives this relationship between ENSO and surface [CO2- 3 ]. It is also found that positive phases of the southern annular mode (SAM) are associated with decreased Southern Ocean surface [CO2- 3 ], an association driven by SAM-related variability in vertical advection of DIC. Despite the influence of the SAM on interannual variability in surface [CO2- 3 ], only 4.5% of the trend in natural Southern Ocean surface [CO2- 3 ] exhibits linear congruence with the trend in wind stress. Given this, the authors predict that the positive trend in the SAM will not have a substantial impact on ocean acidification. Last, ENSO is found to alter the wintertime minimum in surface [CO2- 3 ]. Assuming a business-as-usual acidification rate of 0.5mmol CO2- 3 m-3 yr-1, exacerbation of the wintertime minimum during La Niña conditions may advance the date of aragonite undersaturation within the central Pacific sector of the Southern Ocean by as much as 8 yr. © 2015 American Meteorological Society. |
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| 资源类型: | 期刊论文
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| 标识符: | http://119.78.100.158/handle/2HF3EXSE/50756
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| Appears in Collections: | 气候变化事实与影响
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作者单位: | Department of Atmospheric and Oceanic Sciences, Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, United States
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| Recommended Citation: | |
Conrad C.J.,Lovenduski N.S.. Climate-driven variability in the Southern Ocean carbonate system[J]. Journal of Climate,2015-01-01,28(13)
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