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Spatio-Temporal Variability of Winter Monsoon over the Indochina Peninsula

机译:印度支那半岛冬季季风的时空变化

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摘要

In this study, the spatial patterns and their interannual variability of wintertime low-level winds over the Indochina Peninsula (IDP) were studied by using the analysis of the empirical orthogonal function for complex numbers. The leading mode accounts for 46.6% of the total variance. The composite and regressed patterns of wind components show dominant northeasterly wind over the IDP, which are related to the East Asia winter monsoon (EAWM) circulation and connected to the cyclonic circulation near Borneo. The correlations between the EAWM indices and the leading principal component (PC) suggest the plausible connections between the low-level wind over the IDP and EAWM predominantly via the wind circulation. We also performed correlation analysis on the relationship between leading mode and sea surface temperature anomalies (SSTAs). The result indicates that there is a linkage between the northeasterly wind over the IDP and EAWM and with SSTAs in the Pacific Ocean. This study provides useful information and a mechanism related to the monsoon variability over the IDP.
机译:在这项研究中,通过使用经验数正交函数的分析,研究了印度支那半岛(IDP)冬季低空风的空间格局及其年际变化。领先模式占总方差的46.6%。风分量的复合和回归模式显示了IDP上的东北风为主,这与东亚冬季风(EAWM)循环有关,并与婆罗洲附近的气旋循环有关。 EAWM指数与主要主成分(PC)之间的相关性表明,IDP上的低水平风与EAWM之间主要通过风环流建立了合理的联系。我们还对超前模式与海表温度异常(SSTA)之间的关系进行了相关分析。结果表明,在IDP和EAWM上空的东北风与太平洋上的SSTA之间存在联系。这项研究提供了有用的信息和与IDP季风变化有关的机制。

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