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首页> 外文期刊>Mausam: Journal of the Meteorological Department of India >Spatial patterns of northeast monsoon rainfall over sub-regions of southern peninsular India and Sri Lanka as revealed through empirical orthogonal function analysis
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Spatial patterns of northeast monsoon rainfall over sub-regions of southern peninsular India and Sri Lanka as revealed through empirical orthogonal function analysis

机译:通过经验正交函数分析揭示印度南部半岛和斯里兰卡南部次区域东北季风降雨的空间格局

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The spatial variability of northeast monsoon (NEM) rainfall of peninsular India and Sri Lanka is studied using Empirical Orthogonal Function (EOF) analysis based on monthly / seasonal rainfall data for the months of October, November, December, January and for the season October-December (OND) for the 107 year period of 1900-2006 over nine sub-regions defined for the study based on climatology and geography. Monthly / seasonal rainfall series over these nine sub-regions are subjected to EOF analysis and 2-3 significant Principal Components (PCs) are identified for each case. Each PC is then linked to physical modes known to be associated with NEM using correlation and compositing techniques. For the OND season and for all the four individual months, the first PC explaining maximum variance of 49-64% in the spatial rainfall distribution is identified with the overall NEM strength. The second and the third PCs are identified with rainfall due to passage of synoptic scale systems such as cyclones and depressions (explaining 11-20% variation) and southwest monsoon (SWM) rainfall prior to onset of NEM in October (15% variance explained). PCs representing NEM strength and SWM contribution exhibit contrasting nature of relation with the major climate index Southern Oscillation Index. Relation between the PCs and important regional circulation features,viz., the subtropical ridge at 200 hPa level and the equatorial trough at 850 hPa are used to delineate the PCs associated with SWM and NEM rainfall during October. The study also reveals that the sub-region of north coastal Andhra Pradesh is not benefitted by the over NEM strength but, receives rainfall due to passage of cyclonic disturbances and SWM prior to NEM onset.
机译:基于经验正交函数(EOF)分析,基于10月,11月,12月,1月和10月的季节/月份的每月/季节性降雨数据,研究了印度半岛和斯里兰卡半岛东北季风(NEM)降雨的空间变异性。 1900-2006年的107年期间的12月(OND),该9个分区是根据气候和地理条件进行研究的。对这9个子区域的月/季降雨序列进行了EOF分析,并为每种情况确定了2-3个重要的主成分(PC)。然后,使用相关和合成技术将每个PC链接到已知与NEM相关联的物理模式。对于OND季节和所有四个月,第一台PC解释了NEM的总体强度,该PC解释了空间降雨分布中最大变化49​​-64%。由于天气尺度系统(如旋风和低压(解释为11-20%的变化)和西南季风(SWM))在10月NEM发生之前的降雨通过,因此确定了第二和第三台PC具有降雨。 。代表NEM强度和SWM贡献的PC与主要气候指数Southern Oscillation Index的关系具有相反的性质。 PCs与重要的区域环流特征之间的关系,即200hPa的亚热带海脊和850hPa的赤道,被用来描绘与10月SWM和NEM降雨有关的PCs。这项研究还表明,北部沿海安得拉邦的部分地区并非受益于NEM强度过高,而是由于在NEM发生之前通过了旋风扰动和SWM而获得降雨。

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