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中国沙漠 ›› 2013, Vol. 33 ›› Issue (6): 1874-1883.DOI: 10.7522/j.issn.1000-694X.2013.00043

• 天气与气候 • 上一篇    下一篇

中国西北地区降水异常的气候分析

陈志昆1,2, 张书余3, 雒佳丽1, 李照荣4   

  1. 1.兰州大学 半干旱气候变化教育部重点实验室, 甘肃 兰州 730020;
    2.国家海洋环境预报中心, 北京 100081;
    3.中国气象局兰州干旱气象研究所 甘肃省干旱气候变化与减灾重点实验室/中国气象局干旱气候变化与减灾重点开放实验室, 甘肃 兰州 730020;
    4.兰州中心气象台, 甘肃 兰州 730020
  • 收稿日期:2012-08-12 修回日期:2012-10-08 出版日期:2013-11-20 发布日期:2012-10-08

A Climatic Analysis on the Precipitation Features and Anomaly in Northwest China

CHEN Zhi-kun1,2, ZHANG Shu-yu3, LUO Jia-li1, LI Zhao-rong4   

  1. 1.Ministry of Education Key Laboratory of Semi-Arid Climate Change, Lanzhou University, Lanzhou 730020, China;
    2.National Marine Environmental Forecasting Center, Beijing 100081, China;
    3.Gansu Key Laboratory of Arid Climatic Change and Reducing Disaster/Key Open Laboratory of Arid Climatic Change and Disaster Reduction of China Meteorological Administration, Institute of Arid Meteorology, China Meteorological Administration, Lanzhou 730020, China;
    4.Lanzhou Central Meteorological Observatory, Lanzhou 730020, China
  • Received:2012-08-12 Revised:2012-10-08 Online:2013-11-20 Published:2012-10-08

摘要:

利用中国西北地区128个气象站1971—2009年逐月的降水资料,用经验正交函数(EOF)、旋转经验正交函数(REOF)、小波分析以及突变分析等方法对西北地区降水的空间异常特征和时间变化规律进行了诊断分析。结果表明:西北地区降水类型可分为降水一致型、东-西型、以及南-北型,并且重要程度依次递减;整个西北地区可以分为6个降水区域,分别为高原东北侧区、北疆区、渭河流域区、高原区、河西走廊区、南疆区;尽管在1971—1909年近40年中西北地区整体呈现出少雨、多雨交替的波动变化特征,却未有明显的变干或变湿的倾向,但是各个异常区的气候变化呈现出了不同的趋势倾向;每个降水异常区域都有明显的周期性和年际、年代际变化特征,普遍存在3~5年左右的短周期和10年、20年左右的长周期,各个异常区所盛行的主要周期以及同一异常区在不同年代所盛行的主要周期均有所差异。

关键词: 西北地区, 降水异常, 经验正交函数, 旋转经验正交函数, 小波分析, 突变分析

Abstract:

With EOF, REOF,Wavelet analysis and catastrophe analysis methods, we studied the spatial anomaly features and time evolution rule of precipitation in northwest China using the precipitation data collected in 128 observational stations during in 1971-2009. The results showed that, the first three loading vector field could reveal the most anomaly structures of precipitation in northwest China; the anomaly pattern could be summered as even in the whole area, varying from south to north, and vaarying from east to west; the first seven rotated loading vector fields could repersent six principal precipitation anomaly areas, northeast Qinghai-Tibet Plateau, Weihe River basin, Qinghai plateau, northern Xinjiang, southern Xinjiang and Hexi corridor; the northwest China saw a fluctuations in precipitation in recent 40 years, and no obvious long-term trend was found although some short-term dryer-wetter conversions existed; different anomaly regions showed different trends; the precipitation in northwest China had about 3-5 years, 10 years, and 20 years periodic variations; there existed different prevailing periods among different areas and different prevailing times within one area.

Key words: northwest china, precipitation anomaly, empirical orthogonal function, rotated empirical orthogonal function, wavelet analysis, catastrophe analysis

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