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A Study on Distribution Characteristics of Heavy Precipitation in the Regions Supplied with Electric Power in Central and Eastern Tibet*

机译:中部和东藏电力中沉降沉淀的分布特性研究 *

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摘要

Spatial and temporal distribution characteristics, precipitation concentration degree and concentration period distribution characteristics of heavy precipitation in Tibet Plateau region are analyzed with statistical methods, e.g. wavelet analysis, EOF analysis and precipitation concentration degree, etc. on the basis of daily precipitation data of 39 meteorological observation stations in Tibet region from 1980 to 2012, and analysis results show that the spatial distribution of precipitation in Tibet region is seriously uneven, showing the distribution characteristics of low precipitation in the west and north and high precipitation in the east and south, and several heavy precipitation centers exist simultaneously; the frequency of heavy precipitation in Tibet shows an upward trend (up to 0.28 time/10a), and has a 11-year significant period; the precipitation concentration degree is 0.2-0.9, showing a gradual progressive increase trend from south to north; the precipitation is mainly concentrated between the 32nd Climate and the 45th Climate, that is, between early May and mid-August every year, in which the the precipitation is highly concentrated in the regions along Yarlung Zangbo River, and the precipitation concentration period in eastern Tibet region changes obviously, and Shigatse region, regions from eastern Nagchu to northern Nyingchi, and Yajiang valley are the main regions where precipitation concentration degree changes abnormally, and these regions are the key regions of power interconnection project in central and eastern Tibet, the study of which plays a science and technology support role in the operation and maintenance of power grid project.
机译:用统计方法分析了西藏高原地区重沉淀的沉淀浓度度和浓度周期分布特征,统计方法分析了统计方法。小波分析,EOF分析和降水浓度等等基于1980年至2012年的西藏地区的39个气象观测站的日降水数据,分析结果表明,西藏地区降水的空间分布严重不均匀,显示西部和南部低降水量的分布特性及东南和高沉淀,同时存在几种重沉淀中心;西藏重沉淀的频率显示出上升趋势(高达0.28次/ 10A),并具有11年的重要期限;沉淀浓度程度为0.2-0.9,显示南北朝向北方的逐步逐步增加趋势;沉淀主要集中在第32个气候和第45届气候之间,即每年5月早期和8月中旬之间,其中沉淀在雅隆Zangbo河的地区高度集中,以及东部的降水集中期西藏地区显而易见,南宫东部地区的地区到南美洲北部,雅江谷和雅江谷是沉淀浓度程度异常变化的主要区域,这一区域是中部和西藏东部的电力互联项目的关键区域,这项研究其中在电网项目的运行和维护中发挥了科技支持作用。

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