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Typhoon-Induced SST Cooling and Rainfall Variations: The Case of Typhoon CHAN-HOM and Nangka

机译:台风引起的海表温度降温和降雨变化:以CHAN-HOM和南卡台风为例

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This paper focuses on the investigation of sea surface temperature (SST) and the rainfall variations due to typhoon CHAN-HOM and Nangka occurred in 2015 over Northwest Pacific Ocean (NPO). On 7-13 July, the SST cooling area occurred mainly in the middle of the two typhoons track, the maximum SST decline reached more than 4℃?during typhoon CHAN-HOM and Nangka passage. Due to the collective effe ct of typhoon CHAN-HOM and Nangka, the SST cooling phenomenon maintained for about 15 days. Typhoon CHAN- HOM and Nangka produced heavy rainfall and the maximum daily rainfall was 120 mm (8 July) and 130 mm (11 July). In a1, c area, the average temperature and rainfall basically showed a positive correlation with correlation coefficient of 0.54, while on area a2, the correlation coefficient was?﹣0.6.
机译:本文的重点是调查2015年西北太平洋(NPO)上发生的海表温度(SST)以及台风CHAN-HOM和Nangka造成的降雨变化。 7月7日至13日,SST降温区主要发生在两个台风轨道的中部,在CHAN-HOM和Nangka台风期间,最大SST降幅达到4℃以上。由于CHAN-HOM台风和Nangka的共同作用,SST冷却现象保持了约15天。 CHANHOM台风和Nangka产生了大雨,最大日降雨量分别为120 mm(7月8日)和130 mm(7月11日)。在a1,c区域,平均气温与降雨量基本呈正相关,相关系数为0.54,而在a2区域,相关系数为?﹣0.6。

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