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Spatial and temporal variations of annual precipitation during 1960-2010 in China

机译:1960-2010年中国年降水量的时空变化

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摘要

China is situated in the East Asian Monsoon zone, and the heterogeneity of the temporal and spatial characteristics of precipitation might result in serious flood and drought disasters. Based on precipitation data from 1840 stations across China, the empirical orthogonal function (EOF) analysis and the rotated empirical orthogonal function (REOF) analysis were used to analyze the spatiotemporal characteristics of precipitation variations in China in 1960-2010. Results showed that: (1) precipitation in the East China witnessed changes in the late 1970s, from the late 1980s to early 1990s, and in the early 21st Century respectively, featuring the recurrent south-north shifts of the rainbelt in both directions. Precipitation in Northwest China experienced an abrupt change in the mid-1980s, showing that the western part of Northwest China became wet from the previous dry conditions, whereas the eastern part of the region became dry from the previous wet conditions. However, precipitation in Northeast China underwent abrupt changes in early 1980s and late 1990s respectively, when precipitation changed from near normal in the previous period to more than normal in early 1980s and from more to less than normal in late 1990s. Evident phases in changes in precipitation had been detected over Southwest China, showing that the precipitation changes over both western and northeastern parts of this region were almost opposite; (2) decadal changes of precipitation in East China were closely correlated with the East Asian summer monsoon and the atmospheric circulation, while as important external forcing factors, the Pacific SST and snow cover on the Tibetan Plateau also had indirect impacts on the precipitation in the region through their influences on the East Asian summer monsoon and the atmospheric circulation. (C) 2014 Elsevier Ltd and INQUA. All rights reserved.
机译:中国位于东亚季风区,降水时空特征的异质性可能导致严重的水旱灾害。基于中国1840个站点​​的降水资料,运用经验正交函数(EOF)分析和旋转经验正交函数(REOF)分析来分析1960-2010年中国降水变化的时空特征。结果表明:(1)1970年代末期,1980年代末至1990年代初以及21世纪初,华东地区的降水分别发生了变化,其特征是雨带从北向北反复发生。中国西北地区的降水在1980年代中期经历了突然的变化,这表明西北地区的西部由于先前的干燥条件而变得潮湿,而该地区的东部由于先前的潮湿条件而变得干燥。但是,东北地区的降水分别在1980年代初和1990年代末发生了突然的变化,当时降水从前期的近乎正常变化到1980年代初的多于正常水平,而在1990年代末则从多于正常变化。在中国西南地区已发现降水变化的明显阶段,这表明该地区西部和东北部的降水变化几乎相反。 (2)华东地区降水的年代际变化与东亚夏季风和大气环流密切相关,而作为重要的外部强迫因素,青藏高原的太平洋海温和积雪也间接影响了该地区的降水。区域对东亚夏季风和大气环流的影响。 (C)2014 Elsevier Ltd和INQUA。版权所有。

著录项

  • 来源
    《Quaternary International》 |2015年第4期|5-13|共9页
  • 作者单位

    China Meteorol Adm, Natl Climate Ctr, Lab Climate Studies, Beijing 100081, Peoples R China.;

    China Meteorol Adm, Natl Climate Ctr, Lab Climate Studies, Beijing 100081, Peoples R China.;

    Chinese Acad Forestry, Inst Desertificat Studies, Beijing 100091, Peoples R China.;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Precipitation; Spatial pattern; Temporal variation;

    机译:降水;空间格局;时空变化;

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