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Impacts of the Kuroshio intrusion entering the Luzon Strait on the local atmosphere by satellite observations

机译:卫星观测黑潮入侵吕宋海峡对当地大气的影响

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The Kuroshio is the western boundary current of the North Pacific Ocean. Kuroshio intrudes into the north of South China Sea (SCS) through the Luzon Strait. The intruded Kuroshio often forms an anticyclonic current loop north of the Luzon Strait. Previous studies confirmed co-variability of sea surface temperature (SST) influence on the local atmosphere. In this study, by using satellite data and numerical modeling, the impact of Kuroshio intrusion (KI) entering north Luzon Strait on the local atmosphere is investigated. First, satellite data analysis shows that KI causing increased local sea surface temperature and enhanced intensity of wind speed and rainfall off southwestern Taiwan during easterly winds (from November to April). Moreover, based on vertical velocity (w) of atmosphere derived from reanalysis data, the result shows that higher local SST (associated with KI) triggering enhanced wind speed and rainfall by enhancing lower atmosphere vertical motion and thus decreasing vertical wind shear, which leads to intensify of vertical mixing.
机译:黑潮是北太平洋的西部边界流。黑潮通过吕宋海峡侵入南海北部。入侵的黑潮经常在吕宋海峡以北形成反气旋电流回路。先前的研究证实了海面温度(SST)对当地大气影响的协变性。在这项研究中,通过使用卫星数据和数值模拟,研究了进入吕宋海峡北部的黑潮入侵(KI)对当地大气的影响。首先,卫星数据分析显示,KI在东风(11月至4月)期间导致台湾西南部海域局部海表温度升高以及风速和降雨强度增强。此外,根据从重新分析数据得出的大气垂直速度(w),结果表明,较高的局部SST(与KI关联)通过增强较低的大气垂直运动并因此减小垂直风切变来触发增强的风速和降雨。加强垂直混合。

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