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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Teleconnections between tropical-extratropical oceans and the daily intensity of extreme rainfall over Argentina
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Teleconnections between tropical-extratropical oceans and the daily intensity of extreme rainfall over Argentina

机译:热带—热带海洋之间的遥相关和阿根廷上空的每日极端降雨强度

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摘要

A Singular value decomposition (SVD) analysis was performed jointly on the daily intensity of extreme rainfall (DIER) over Argentina and the sea surface temperature (SST) of all the oceans from 17.5°N to 90°S in order to identify the large-scale variability of the SSTs related to extreme rainfall, in the period 1962-2005. The main objective of the article is to objectively recognize regions of the tropical and subtropical oceans that could be related with the extreme rainfall over Argentina. Spring is the season that is best represented by the first mode, accounting for up to 45% of the covariance between the DIER and SST. The first SVD mode of spring, summer and autumn presents a pattern of SST relating to the El Ni?o-Southern Oscillations (ENSO) phenomena with an enhanced DIER in different zones of centre and east of Argentina. In the second SVD mode of spring and summer, the SST patterns show cold conditions in the tropical and subtropical Atlantic and near Indonesia with an enhancement of the DIER in the centre and east of Argentina. These modes show a significant decadal variability. In the third SVD mode of spring and summer, the SST patterns present warm and cold conditions in the Indian Ocean and the centre and western Pacific Ocean (PO) with decreased rainfall in the northern and eastern portion of Argentina, respectively. This mode shows a significant period of temporal variability of around 14 years. The third mode of autumn presents warm conditions in the tropical Atlantic and the southwest PO with a low DIER in the centre and east of Argentina. This mode also presents temporal variability of around 14 years. The correlation between each mode derived from analysis of SVD and climate indices related with SST were computed.
机译:对阿根廷上空的极端降雨(DIER)的日强度和从17.5°N到90°S的所有海洋的海面温度(SST)共同进行了奇异值分解(SVD)分析,以便识别出1962-2005年期间与极端降雨有关的SST的尺度变化。本文的主要目的是客观地认识可能与阿根廷上空的极端降雨有关的热带和亚热带海洋区域。春天是第一种模式最能代表的季节,占DIER和SST之间协方差的45%。春季,夏季和秋季的第一个SVD模式呈现出与厄尔尼诺-南方涛动(ENSO)现象有关的SST模式,并在阿根廷中部和东部的不同区域增强了DIER。在春季和夏季的第二种SVD模式下,SST模式显示出热带和亚热带大西洋以及印度尼西亚附近的寒冷状况,而阿根廷中部和东部的DIER增强。这些模式显示出明显的年代际变化。在春季和夏季的第三种SVD模式下,SST模式在印度洋和中部和西太平洋(PO)呈现温暖和寒冷的状况,而阿根廷北部和东部分别出现降雨减少。这种模式显示出大约14年的显着时间变化。秋季的第三种模式在热带大西洋和西南PO表现为温暖的条件,阿根廷中部和东部的DIER较低。这种模式还表现出约14年的时间变异性。计算了从SVD分析得出的每种模式与与SST相关的气候指数之间的相关性。

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