globalchange  > 气候减缓与适应
DOI: 10.1002/grl.50697
论文题名:
Second peak in the far eastern Pacific sea surface temperature anomaly following strong El Niño events
作者: Kim W.; Cai W.
刊名: Geophysical Research Letters
ISSN: 0094-8598
EISSN: 1944-8329
出版年: 2013
卷: 40, 期:17
起始页码: 4751
结束页码: 4755
语种: 英语
英文关键词: eastern Pacific SST ; strong El Niño ; thermocline feedback ; zonal SPCZ
Scopus关键词: Atmosphere-ocean interactions ; Eastern equatorial Pacific ; Eastern pacific ; Latent heat release ; Sea surface temperature anomalies ; Short-wave radiation ; South pacific convergence zones ; zonal SPCZ ; Atmospheric temperature ; Stream flow ; Wind stress ; Oceanography ; convergence ; El Nino ; oceanic circulation ; sea surface temperature ; shortwave radiation ; temperature anomaly ; thermocline ; upwelling ; westerly ; wind stress ; Pacific Ocean ; Pacific Ocean (East) ; Pacific Ocean (Equatorial) ; Pacific Ocean (South)
英文摘要: The eastern Pacific sea surface temperature anomaly (SSTa) associated with El Niño usually peaks in December, January, and February, and decays in the ensuing months; sometimes, however, after a strong El Niño, a second peak in SSTa is observed in the far eastern equatorial Pacific. It is found that an enhanced westerly wind stress anomaly over the equatorial Pacific basin, usually associated with a meridional swing of South Pacific Convergence Zone (SPCZ), precedes the occurrence of the second peak. As the equatorial thermocline slope balances with the zonally integrated zonal-wind stress, the westerly wind stress anomaly induces deepened thermocline and suppresses upwelling in the eastern Pacific for the double-peak cases. On the other hand, enhanced latent heat release and reduced shortwave radiation cause a pause in warming between the two peaks. As a result, a strong El Niño, usually accompanied by a zonal SPCZ, exhibits distinct double-peak characteristics. Key Points There is a second peak after strong El Nino The second peak is generated by anomalous ocean circulation There exists a pause between the peaks due to atmosphere-ocean interaction ©2013. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84883566422&doi=10.1002%2fgrl.50697&partnerID=40&md5=1cb14074d0a734a6a77c6818799b2f19
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/5862
Appears in Collections:气候减缓与适应

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作者单位: CSIRO Marine and Atmospheric Research, Aspendale, VIC 3195, Australia

Recommended Citation:
Kim W.,Cai W.. Second peak in the far eastern Pacific sea surface temperature anomaly following strong El Niño events[J]. Geophysical Research Letters,2013-01-01,40(17).
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