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Impact of the Indo-Western Pacific Ocean Capacitor mode on South Asian summer monsoon rainfall

机译:印度西太平洋电容器模式对南亚夏季季风降雨的影响

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The influence of Indo-Western Pacific Ocean Capacitor (IPOC) mode on South Asian summer monsoon rainfall variability is investigated in the present study. It is found from the observations that the IPOC mode induces a tripole pattern in precipitation anomalies over the South Asian region. Strong positive precipitation anomalies over some parts of western Ghats and Sundarbans and Bangladesh region separated by negative precipitation anomalies over the monsoon trough region are found to be the main characteristic features closely associated with the IPOC mode. It is noted that anomalous western north Pacific (WNP) anticyclone and tropical Indian Ocean (TIO) warming maintain a tripole precipitation pattern over the South Asian region. Anomalous low level convergence in the northern flank of WNP anticyclone and orographic lift cause enhanced rainfall over the Sundarbans and Bangladesh region. Meanwhile, westward propagating atmospheric cold Rossby wave as a response to suppressed convection over the WNP region induced moisture divergence and downward motion play important role in maintaining negative rainfall anomalies over the monsoon trough. At the same time, TIO SST warming supported by easterly wind anomalies associated with WNP anticyclone has contributed to the enhanced rainfall over parts of eastern Arabian Sea and western Ghats. Coupled General Circulation Model sensitivity experiments are performed to investigate individual and combined impact of the TIO warming and WNP circulation on south Asian summer monsoon rainfall variability associated with IPOC mode. The model experiments revealed that WNP anticyclone influences the rainfall over the monsoon trough region and Sundarbans-Bangladesh region. Further the moisture convergence induced by local SST warming is mainly helping to sustain enhanced Western Ghats rainfall. Sub-seasonal variability of ISM rainfall associated with the IPOC modes is also discussed. This study advocates the importance of IPOC mode in exerting strong impact on regional summer rainfall variability over the Indian/South Asian summer monsoon region on the interannual time scale. Thus, it is important to consider the possible roles of TIO warming and WNP circulation in predicting the South Asian summer monsoon rainfall.
机译:印度西太平洋电容器(IPOC)模式对南亚夏季季风降雨变异的影响研究。从观察结果中发现了IPOC模式在南亚地区的降水异常中引起了普遍模式。发现季船坞止音站和阳光和阳光区和孟加拉国在季风槽区域上分离的孟加拉国和孟加拉国区域的强烈的正降水异常被发现是与IPOC模式密切相关的主要特征。人指出,异常西北太平洋(WNP)抗气旋和热带印度洋(TIO)加热维持南亚地区的黎翼降水模式。 WNP北侧侧翼的异常低水平收敛性和地形升降机造成阳光银行和孟加拉国地区的降雨。同时,向西传播大气冷罗斯比波作为对WNP区域诱导的水分分歧和向下运动的反应,在维持季风槽上的负降雨异常方面发挥着重要作用。与此同时,由与WNP抗气旋有关的东风异常支持的TiO SST变暖有助于增加东部阿拉伯海和西部止步区的地区的增强降雨。耦合的一般循环模型敏感性实验是调查TIO变暖和WNP循环对与IPOC模式相关的南亚夏季季风降雨变异性的个体和综合影响。模型实验表明,WNP抗气旋区影响了季风槽地区和Sundarbans-Bangladesh地区的降雨。此外,局部SST变暖引起的水分收敛主要有助于维持增强的西巨头降雨。还讨论了与IPOC模式相关的ISM降雨的次季节变化。本研究主张了IPOC模式对印度/南亚夏季季风地区在年夏季季风地区的施加强劲影响方面对年夏季季风地区的强劲影响。因此,重要的是要考虑TIO变暖和WNP循环在预测南亚夏季季风降雨中的可能作用。

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