| DOI: | 10.1007/s00382-017-3647-4
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| Scopus记录号: | 2-s2.0-85016053936
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| 论文题名: | Control of the South Atlantic Convergence Zone by extratropical thermal forcing |
| 作者: | Talento S.; Barreiro M.
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| 刊名: | Climate Dynamics
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| ISSN: | 9307575
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| 出版年: | 2018
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| 卷: | 50, 期:2018-03-04 | | 起始页码: | 885
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| 结束页码: | 900
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| 语种: | 英语
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| 英文关键词: | Extratropical forcing
; SACZ
; Slab ocean model
; Tropical sea surface temperatures
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| Scopus关键词: | air-sea interaction
; atmospheric forcing
; atmospheric general circulation model
; boundary condition
; cooling
; extratropical environment
; Northern Hemisphere
; sea surface temperature
; Southern Hemisphere
; Walker circulation
; warming
; Africa
; Atlantic Ocean
; Atlantic Ocean (South)
; Equus asinus
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| 英文摘要: | The response of the South Atlantic Convergence Zone (SACZ) to an extratropical thermal forcing is investigated in a series of simulations performed with an atmospheric general circulation model coupled to a slab ocean model. Three sets of experiments are performed, varying the extratropical forcing. In the first the forcing consists of warming of the Northern Hemisphere (NH) and cooling of the Southern Hemisphere, with zero global average. In the second and third experiments, the former forcing is divided into its northern and southern components to asses their relative roles in affecting the SACZ. In all the cases realistic surface boundary conditions are implemented. We found that during its peak in austral summer the SACZ weakens in response to the extratropical forcing and that such weakening is mostly due to the NH component of the forcing. We found that 75% of the SACZ signal in response to the forcing is linked to the generation of a secondary tropical convergence zone in the Atlantic Ocean around 20°N–30°N, which generates an anomalous Hadley circulation with subsidence over the SACZ. This mechanism appears to be dependent on the upper level changes and tropical ocean response, as it weakens significantly when the simulation is repeated not allowing the tropical sea surface temperatures to change in response to the forcing. The remaining 25% of the signal can be explained through the development of a Walker-type of circulation between western tropical Africa and the SACZ, being this mechanism dependent on the African land surface temperature reaction to the remote forcing. © 2017, Springer-Verlag Berlin Heidelberg. |
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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/109456
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| Appears in Collections: | 影响、适应和脆弱性
气候变化事实与影响
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作者单位: | Department of Atmospheric Sciencies, Institute of Physics, School of Sciences, Universidad de la República, Montevideo, 11400, Uruguay
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| Recommended Citation: | |
Talento S.,Barreiro M.. Control of the South Atlantic Convergence Zone by extratropical thermal forcing[J]. Climate Dynamics,2018-01-01,50(2018-03-04)
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