Relationship between cross-equatorial flows over the Bay of Bengal and Australia in boreal summer:Role of tropical diabatic heating  

作　　者：Xuelei Jiang Yuanyuan Guo Zhiping Wen 

机构地区：[1]Department of Atmospheric and Oceanic Sciences&Institute of Atmospheric Sciences,Fudan University,Shanghai,China [2]Innovation Center of Ocean and Atmosphere System,Zhuhai Fudan Innovation Research Institute,Zhuhai,China [3]Jiangsu Collaborative Innovation Center for Climate Change,Nanjing,China

出　　处：《Atmospheric and Oceanic Science Letters》2022年第2期1-6,共6页大气和海洋科学快报（英文版）

基　　金：jointly supported by the National Key Research and Development Program of China[grant number 2016YFA0600601];the National Natural Science Foundation of China[grant numbers 42030601 and 41875087]。

摘　　要：The interannual variability of cross-equatorial flows(CEFs)over the Asian–Australian monsoon(AAM)region during boreal summer was analyzed by applying the empirical orthogonal function(EOF)method to the meridional wind at 925 h Pa.The first mode(EOF1)exhibits an in-phase relationship among different CEF channels over the AAM region,which has received much attention owing to its tight linkage with ENSO.By contrast,the second mode(EOF2)possesses an out-of-phase relationship between the Bay of Bengal(BOB)CEF(90°E)and Australian CEF,among which the New Guinea CEF near 150°E shows the most significant opposite correlation with the BOB CEF.Observational and numerical model results suggest that the equatorially asymmetric heat source(sink)over the western(eastern)Maritime Continent,closely associated with the in-situ sea surface temperature anomaly,can induce cross-equatorial northerly(southerly)flow into the heating hemisphere,which dominates the out-of-phase relationship between the BOB and New Guinea CEFs.Furthermore,an equatorially symmetric heating over the central Pacific may indirectly change the CEFs by modulating the zonal atmospheric circulation near the Maritime Continent.本文通过对1979–2017年夏季925 h Pa经向风异常进行经验正交函数(EOF)分解,研究了亚澳季风区内越赤道气流的年际变化特征.结果表明,越赤道气流的第一模态表现为亚澳季风区内不同通道间的同相变化,即一致加强或减弱;第二模态表现为孟加拉湾和澳大利亚越赤道气流的反相变化,其中新几内亚和孟加拉湾越赤道气流的反相变化最显著.该反相模态分别对应着赤道以南地区海洋性大陆东西两侧的海温异常,其纬向偶极型的空间分布直接导致海洋性大陆西部(东部)出现沿赤道非对称的异常热汇(热源),它可以激发跨越赤道的南风(北风)异常,从而有利于该反相模态的出现.

关 键 词：Cross-equatorial flow Equatorially asymmetric diabatic heating Linear baroclinic model 

分 类 号：P43[天文地球—大气科学及气象学]