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Characteristics of Arabian Sea mini warm pool and Indian summer monsoon

机译:阿拉伯海迷你温水游泳池和印度夏季风的特征

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Arabian Sea Mini Warm Pool (ASMWP) is a part of the Indian Ocean Warm Pool and formed in the eastern Arabian Sea prior to the onset of the summer monsoon season. This warm pool attained its maximum intensity during the pre-monsoon season and dissipated with the commencement of summer monsoon. The main focus of the present work was on the triggering of the dissipation of this warm pool and its relation to the onset of summer monsoon over Kerala. This phenomenon was studied utilizing NCEP/NCAR (National Center for Envi-ronmental Prediction/National Center for Atmospheric and Research) re-analysis data, TRMM Micro wave Imager (TMI) and observational data. To define the ASMWP, sea surface temperature exceeding 30.25℃ was taken as the criteria. The warm pool attained its maximum dimension and intensity nearly 2 weeks prior to the onset of summer monsoon over Kerala. Interestingly, the warm pool started its dissipation immediately after attaining its maximum core temperature. This information can be included in the present numerical models to enhance the prediction capa-bility. It was also found that the extent and intensity of the ASMWP varied depending on the type of monsoon i.e., excess, normal, and deficient monsoon. Maximum core temperature and wide coverage of the warm pool observed during the excess monsoon years compared to normal and deficient monsoon years. The study also revealed a strong relationship between the salinity in the eastern Arabian Sea and the nature of the monsoon.
机译:阿拉伯海迷你暖池(ASMWP)是印度洋暖池的一部分,在夏季风开始之前在阿拉伯海东部形成。这个暖池在季风前季节达到最大强度,并随着夏季季风的开始消散。当前工作的主要重点是引发这个暖池的消散及其与喀拉拉邦夏季风爆发的关系。利用NCEP / NCAR(国家环境预测中心/国家大气与研究中心)再分析数据,TRMM微波成像仪(TMI)和观测数据对这种现象进行了研究。为了定义ASMWP,以海面温度超过30.25℃为标准。在喀拉拉邦夏季风开始之前的近两周,暖池达到了最大尺寸和强度。有趣的是,温池在达到最高核心温度后立即开始其消散。该信息可以被包括在当前数值模型中以增强预测能力。还发现,ASMWP的程度和强度随季风的类型而变化,即季风过量,正常和不足。与正常季风季和不足季风季相比,季风季过高时观测到的最高核心温度和暖池的广泛覆盖。该研究还揭示了阿拉伯海东部的盐度与季风的性质之间的密切关系。

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