热带印度洋SST海盆模态的“充电/放电”作用——对夏季南亚高压的影响

杨建玲; 刘秦玉

热带印度洋SST海盆模态的“充电/放电”作用——对夏季南亚高压的影响

中国海洋大学物理海洋实验室, 海洋大气相互作用与气候实验室, 山东, 青岛, 266100

基金项目: 国家自然科学基金项目(40676010)

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出版历程
- 收稿日期: 2007-06-28
- 修回日期: 2007-10-10

The "charge/discharge" roles of the basin-wide mode of the Indian Ocean SST anomaly——influence on the South Asian High in summer

Physical Oceanography Laboratory, and Ocean-Atmosphere Interaction and Climate Laboratory, Ocean University of China, Qingdao 266103, China

摘要

摘要: 根据观测资料和海气耦合模式初值试验结果,通过比较分析热带太平洋SST主模态(ENSO模)和热带印度洋SST主模态(海盆模)对夏季南亚高压的影响,揭示了印度洋海盆模的"充电/放电"作用:赤道中东太平洋海温异常首先对印度洋进行"充电",形成热带印度洋SST对太平洋EN-SO的响应模态——海盆模。该模态在ENSO发生翌年春季达到峰值位相,而且有很好的持续性,可以从春季持续到夏季,该暖(冷)模态可以引起大气的"Matsuno-Gillpattern"响应,并通过亚洲夏季平均西南季风的异常水汽输送等使得夏季南亚高压偏强(弱),即为"放电"过程。而赤道中东太平洋海温异常对夏季南亚高压的直接影响并不显著,并指出了夏季南亚高压和超前3~12个月Nio3指数之间高的显著正相关关系只是一个表象,并不是太平洋海温异常对南亚高压的直接影响结果,而是通过印度洋海盆模态的"充电/放电"作用引起的。
- 印度洋 /
- 海盆模态 /
- 充电/放电 /
- 南亚高压
Abstract: Based on observational dat a and ocean-atmosphere coupled model experiments,by analyzing the influence of the sea surface temperature(SST)anomaly main mode of the tropical Pacific ENSO and the Indian Ocean basin-wide mode(IOBM)on the South Asian High(SAH)in boreal summer,the "charge/discharge" roles of the IOBM are revealed:Firstly,the SST anomaly in the mid-east equatorial of the Pacific charges to the Indian Ocean and induces the IOBM. Being the responding mode of the Pacific ENSO, the IOBM reaches its peak phase in the next spring of the ENSO developing year and can persist from the spring to the summer. Then,the warm(cool)SST anomaly of IOBM in the spring and the summer can in turn influence the atmospheric circulation and make SAH in summer stronger(weaker)through atmos-pheric response of "Matsuno-Gill pattern" and water vapor transportation ano maly by mean south west wind of Asian summer monsoon circulation,this process is called "discharge"1. While the direct influence of the SST anomaly of the mid-east equat orial Pacific on SAH in summer is not significant,and it is pointed out that the high positive sig nificant correlation between the SAH in summer and the leading 3~12 months Niño 3 index is only a superficies,and not the result from the direct influence of the ENSO but from the "charge/discharge" role of the Indian Ocean.
- the Indian Ocean /
- basin-wide mode /
- charge/discharge /
- the South Asian High

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参考文献(21)

张琼,钱永甫.南亚高压的年际和年代际变化[J].大气科学,2000,124(11):67-78.

刘屹岷,吴国雄,刘辉,等.空间非均匀加热对副热带高压形成和变异的影响:Ⅲ.凝结潜热加热与南哑高压及西太平洋副高[J].气象学报,1999,57(5):525-538.

LI Chong-yin,MU Ming-quan.The influence of the Indian Ocean dipole on atmospheric circulation and climate[J].Adv Atmos Sci,2001,18(5):831-843.

杨辉,李崇银.热带太平洋-印度洋海温异常综合模对南亚高压的影响[J].大气科学2005,29(1):99-110.

SAJI N H,GOSWAMI B N,VINAYACHANDRAN P N,et al.A dipole mode in the tropical Indian Ocean[J].Nature,1999,401:360-363.

SAJI N H,YAMAGATA T.Possible impacts of Indian ℃ ean dipole mode events on global climate[J].Clim Res,2003,25:151-169.

GUAN Z,ASHOK K,YAMAGATA T.Summer-time response of the tropical atmosphere to the Indian Ocean dipole sea surface temperature anomalies[J].J Meteorol Soc Jpn,2003,81:531-561.

ANNAMALAI H,LIU Ping,XIE Shang-ping.Southwest Indian Ocean SST variability:Its local effect and remote influence on Asian monsoons[J].J Climate,2005,18:4150-4167.

KLEIN S A,SODE B J,LAU N-C.Remote sea surface temperature variations during ENSO:Evidence for a tropical atmospheric bridge[J].J Climate,1999,12,917-932.

XIE S-P,ANNAMALAI H,SCHOTT F,et al.Structure and Mechanisms of south Indian Ocean climate variability[J].J Climate,2002,15:864-878.

ANNAMALAI H.Raghu Mutugrdde,role of Indian Ocean in regional climate variability[J].Earth's Climate:The Ocean-atmosphere interaction.Geophysical Monograph,2004,147:213-246.

RASMUSSON E M,CARPENTER T H.Variations in tropical sea surface temperature and sea surface wind fields associated with the Southern Oscillation/El Niño[J].Mon Wea Rev,1982,110:354-384.

WANG Bin,WU Reng-guang,LI Tim.Atmosphere-warm Ocean interaction and its impacts on Asian-Australian monsoon variation[J].J Climate,2003,15:1195-1211.

谭言科,张人禾,何金海,等.热带印度洋海温的年际变化与ENSO[J].大气科学,2004,62(6):831-840.

HOREL J D,WALLACE J M.Planetary-scale atmospheric phenomena associated with the Southern Oscillation[J].Mon Weather Rev,1981,109:813-829.

YANG Jian-ling,LIU Qin-yu,XIE Shang-ping,et al.Impact of the Indian Ocean SST basin mode on the Asian summer monsoon[J].Geophys Res Lett,2007,34,L02708,doi: 10.1029/2006GL028571.

MATSUNO T.Quasi-geostrophic motions in the equatorial area[J].J Meteor Soc Japan,1966,44:26-43.

GILL A E.Some simple solutions for heat-induced tropical circulation[J].Quart J Roy Meteor Soe,1980,106:447-462.

RODWELL M J,BRIA J H.Monsoons and the dynamics of deserts[J].Q J R Meteorol SOc,1996,122:1385-1404.

CHIANG J C H,SOBEL A H.Tropical tropospheric temperature variations caused by ENSO and their influence on the remote tropical climate[J].J Clim,2002,15:2616-2631.

YULAEVA E,WALLACE J M.Sensitivity of seasonal dimate forecasts to persisted SST anomalies[J].J Clim,1994,7:1719-1736.

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