中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Summer sst anomalies in the indian ocean and the seasonal timing of enso decay phase

文献类型:期刊论文

作者Ren, Rongcai1,2,3; Sun, Shuyue1,4; Yang, Yang1,4; Li, Qian1
刊名Climate dynamics
出版日期2016-09-01
卷号47期号:5-6页码:1827-1844
关键词Sst anomalies Summer indian ocean Seasonal timing of enso decay phase
ISSN号0930-7575
DOI10.1007/s00382-015-2935-0
通讯作者Ren, rongcai(rrc@lasg.iap.ac.cn)
英文摘要Enso affects the tropical indian ocean (tio) sst in winter-spring in enso decay years through an enso-induced 'atmospheric-bridge' and subsequent air-sea coupling processes. the interdecadal delay of el nio decay phase has been related to a warming change in the summer tio since 1970s. a physical linkage between the summer sst anomalies over the tio and the timing of enso decay phase is however still unclear. this study uses multi-source data to distinguish 'later-decay' from 'normal-decay' el nio/la nia events, and performs diagnostic analysis of the changes in various thermodynamic and dynamic processes due to later-decay enso for quantifying the partial contribution by each of these processes to the summer sst changes over the tio. the results show that, at both the interannual and interdecadal timescales, the significant warmer and colder sst anomalies in the spring tio in later-decay el nio and la nia years respectively can persist into summer. most of the enso-induced atmospheric-bridge-related processes contribute positively to the tio sst changes in summer due to later-decay of enso, as they do in spring during normal-delay enso year. the exceptions are the surface wind-evaporation-mechanism and sensible heat-flux anomalies in summer, which always contribute negatively to the summer sst anomalies over most parts of the tio. the negative contributions from these two processes in summer exist no matter whether there is a weakening or strengthening surface wind due to later-decay of enso events. generally, the presence of five later-decay el nio events after the 1970s is mainly responsible for the observed interdecadal summer tio warming in recent decades.
WOS关键词SEA-SURFACE TEMPERATURE ; INDO-WESTERN PACIFIC ; INDIVIDUAL FEEDBACK PROCESSES ; NINO-SOUTHERN OSCILLATION ; EL-NINO ; ATMOSPHERIC BRIDGE ; TROPICAL PACIFIC ; INTERANNUAL VARIABILITY ; INTERDECADAL CHANGE ; CLIMATE SYSTEM
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000382112000029
出版者SPRINGER
URI标识http://www.irgrid.ac.cn/handle/1471x/2376243
专题中国科学院大学
通讯作者Ren, Rongcai
作者单位1.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, POB 9804, Beijing 100029, Peoples R China
2.Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing, Jiangsu, Peoples R China
3.Nanjing Univ Informat Sci & Technol, KLME, Nanjing, Jiangsu, Peoples R China
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Ren, Rongcai,Sun, Shuyue,Yang, Yang,et al. Summer sst anomalies in the indian ocean and the seasonal timing of enso decay phase[J]. Climate dynamics,2016,47(5-6):1827-1844.
APA Ren, Rongcai,Sun, Shuyue,Yang, Yang,&Li, Qian.(2016).Summer sst anomalies in the indian ocean and the seasonal timing of enso decay phase.Climate dynamics,47(5-6),1827-1844.
MLA Ren, Rongcai,et al."Summer sst anomalies in the indian ocean and the seasonal timing of enso decay phase".Climate dynamics 47.5-6(2016):1827-1844.

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来源:中国科学院大学

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