首页> 外文期刊>Advances in Meteorology >Connection between Two Leading Modes of Autumn Rainfall Interannual Variability in Southeast China and Two Types of ENSO-Like SSTA
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Connection between Two Leading Modes of Autumn Rainfall Interannual Variability in Southeast China and Two Types of ENSO-Like SSTA

机译:东南秋天降雨际变化两种领先模式的联系及两种类型的enso样式SSTA

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The interannual variability of autumn rainfall in Southeast China (SEC) is significant, with two major modes, namely, monopole and dipole modes. It is found that the monopole mode is closely related to EP ENSO-like sea surface temperature anomaly (SSTA), and the dipole mode is related to CP ENSO-like SSTA. During the warm phase of EP ENSO-like SSTA, an anomalous anti-Walker circulation emerges in the tropical Pacific, with an anomalous subsiding during 110°E–120°E and an anomalous ascending branch in SEC. These two branches of anomalous current are in the same longitude and form a closed meridional circulation. Besides, there also exists an anticyclone anomaly in the Northwest Pacific (NWP), transporting water vapor into SEC. These circulation configurations induced by the warm phase of EP ENSO-like SSTA are consistent with those of monopole mode positive anomaly year. The good correspondence between EP ENSO warm event and the positive monopole mode also helps to support the corresponding relationship between the EP ENSO-like SSTA and monopole mode of SEC autumn rainfall. After the diagnosis of the perturbation omega equation, the anomalous subsiding branch over SEC, as the key link of EP ENSO-like warm phase SSTA exerting impact on the monopole mode during positive anomaly year, is mainly related with the anomalous relative vorticity advection transported by basic zonal wind and temperature advection transported by meridional wind anomaly. As for the dipole mode, it is related to the CP ENSO-like SSTA, but the corresponding relationship is weaker than that of the monopole mode and EP ENSO-like SSTA. In special, during the warm phase of CP ENSO-like SSTA, an anomalous cyclone appears in the NWP and prevailing sinking motion over SEC, both of which favors the appearance of positive anomaly of the dipole mode. Specially, the local anomalous vertical motion mainly depends on anomalous relative vorticity transported by basic meridional wind. Generally speaking, the monopole (dipole) mode is closely associated with the EP (CP) ENSO-like SSTA, demonstrating some correspondence.
机译:中国东南部秋天降雨的际变化(秒)是重要的,两种主要模式,即单极和偶极模式。发现单极模式与EP ENSO样的海表面温度异常(SSTA)密切相关,偶极模式与CP ENSO样SSTA有关。在EP ENSO-SSTA的温暖阶段,热带太平洋中出现的异常防河流循环,在110°E-120°E期间具有异常子定位和SEC的异常升序分支。这两个异常电流的分支处于相同的经度,形成闭合的化学循环。此外,西北太平洋(NWP)还存在一类抗气旋异常,将水蒸气运送到秒中。通过EP Enso-lims SSTA的温暖阶段诱导的这些循环配置与单极模式阳性异常年份的温度一致。 EP ENSO温暖事件与正单极模式之间的良好对应关系还有助于支持EP ENSO样SSTA与SEC秋季降雨的单极模式之间的相应关系。在诊断扰动OMEGA方程后,SEC的异常子定位分支,作为EP ENSO的温度SSTA对阳性异常年内对单极模式的影响的关键联系,主要与运输的异常相对涡流平流有关子午类异常运输的基本区域风和温度平流。至于偶极模式,它与CP ENSO样SSTA有关,但相应的关系比单极模式和EP ENSO类似SSTA的关系较弱。在特殊的是,在CP Enso样SSTA的温暖阶段,在NWP中出现异常旋风,并在SEC中占上风沉降运动,这两者都有助于偶极模式的正异常的外观。特别地,局部异常垂直运动主要取决于基本经络传输的异常相对涡度。一般而言,单极(偶极)模式与EP(CP)类似的SSTA密切相关,展示了一些对应关系。

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