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Principal Component Analysis to study spatial variability of errors in the INSAT derived quantitative precipitation estimates over Indian monsoon region

机译:主成分分析,研究印度季风区域INSAT定量降水估计中误差的空间变异性

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In this paper, Principal Component Analysis has been applied to investigate the spatial variability of errors in the INSAT derived quantitative precipitation estimates (QPE) over the Indian monsoon region, using daily rainfall analysis (at the same resolution) for the period from 1 June to 30 August of summer monsoon 2001. The study shows that the QPE errors have certain spatial variability. The orographic rainfall is significantly underestimated along the Western Ghats and along the foothills of the Himalayas, where the root mean square errors are also very large. Otherwise, the performance of the QPE is reasonably good over the rest of the region. The first principal component, which explains about 5.1% of the variance, corresponds to the onset phase of the monsoon during June, when strong positive loadings dominate over the southern parts of the country. The second principal component explaining about 4.2% of the variance, has strong positive loading in the intermittent presence of the monsoon low pressure system over the east central parts of the country. The third principal component which explains 3.3% of the variance is associated with the monsoon trough at the normal position, and the fourth principal component which explains 3.1% of the variance is associated with the monsoon trough at the southern position.
机译:本文采用主成分分析法,利用6月1日至6月1日的每日降水量分析(以相同的分辨率)研究了印度季风区INSAT导出的定量降水量估计值(QPE)中误差的空间变异性。 2001年夏季季风的8月30日。研究表明QPE误差具有一定的空间变异性。西高止山脉和喜马拉雅山的山麓地带的地形降雨被大大低估了,那里的均方根误差也很大。否则,QPE在该地区其他地区的表现相当不错。第一个主要成分解释了大约5.1%的方差,对应于6月的季风爆发期,当时该国南部地区出现了强烈的正向负荷。第二个主要成分解释了约4.2%的方差,在该国中部东部季风低压系统的间歇性存在下具有强大的正负荷。解释方差3.3%的第三主成分与正常位置的季风槽有关,解释方差3.1%的第四主成分与南部位置的季风槽有关。

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