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1958-2006年河西走廊极端天气气候事件变化特征
引用本文:曹玲,李岩瑛,刘明春,窦永祥,杨晓玲.1958-2006年河西走廊极端天气气候事件变化特征[J].干旱区研究,2009,26(5).
作者姓名:曹玲  李岩瑛  刘明春  窦永祥  杨晓玲
作者单位:1. 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;甘肃省武威市气象局,甘肃武威,733000
2. 甘肃省张掖市气象局,甘肃张掖,734000
3. 甘肃省武威市气象局,甘肃武威,733000
基金项目:甘肃省气象局第四批“十人计划”;;公益性行业(气象)科研专项“西北地区旱作农业对气候变暖的响应特征及其预警和应对技术研究”(GYHY200806021)
摘    要:利用1958-2006年甘肃河西走廊18个观测站大雨、干旱、≥35℃高温、≤-20℃低温、霜冻、大风、沙尘暴、雷暴、冰雹等极端天气气候事件的年发生日数资料,采用多项式法、线性倾向、M ann-Kendall法、滑动t检验及Morlet小波等统计学方法诊断分析其变化特征。结果表明:近49年来,河西走廊大风、沙尘暴、低温、霜冻、雷暴和冰雹呈显著减少趋势,高温呈显著增多趋势,其中大风、沙尘暴、高温和霜冻分别于1996,1989,1996年和1998年前后发生突变;大雨和干旱频数总体变化不显著。20世纪90年代初,低温和霜冻由多趋少,高温、大雨和干旱由少趋多,与河西走廊突变增暖时间基本吻合。干旱和高温存在长期性变化周期,沙尘暴、雷暴存在阶段性变化周期,其余极端天气周期变化不明显。

关 键 词:极端天气  气候趋势  气候变暖  河西走廊  甘肃  

Change Characteristics of Extreme Weather and Climatic Events over the Hexi Corridor during the Period of 1958 -2006
CAO Ling,LI Yan-ying,LIU Ming-chun,DOU Yong-xiang,YANG Xiao-ling.Change Characteristics of Extreme Weather and Climatic Events over the Hexi Corridor during the Period of 1958 -2006[J].Arid Zone Research,2009,26(5).
Authors:CAO Ling  LI Yan-ying  LIU Ming-chun  DOU Yong-xiang  YANG Xiao-ling
Institution:1.Lanzhou Institute of Arid Meteorology;China Meteorological Administration;Gansu Province Key Laboratory of Arid Climate Change and Disaster Reduction;Key Open Laboratory of Arid Climate Change and Disaster Reduction;Lanzhou 730020;China;2.Wuwei Meteorological Bureau;Wuwei 733000;Gansu Province;3.Zhangye Meteorological Bureau;Zhangye 734000;China
Abstract:This paper analyzes the change characteristics of extreme weather and climate events, such as heavy rain, drought, high temperature ≥35 ℃, low temperature≤ -20℃ , frost, gale, sandstorm, thunderstorm and hail over the Hexi Corridor using the data of annual occurring days of extreme weather and climate events from 18 meteorological stations in the corridor during the period of 1958 -2006 and the statistical methods, such as polynomial , linear trend, Mann-Kendall test, Moving T-test and Morlet wavelet analysis. The results show that the annual days of occurring some extreme weather events, such as gale, sandstorm, low temperature ≤ -20℃, frost, thunderstorm and hail, over the Hexi Corridor in recent 49 years have been significantly decreased, but the annual days of occurring high temperature ≥35 ℃ have been obviously increased. Of which the abrupt change of occurrence of gale, sandstorm, high temperature ≥35 ℃ and frost occurred around 1996, 1989, 1996 and 1998 respectively. Generally, the change of the frequencies of heavy rain and drought is not so obvious. In the early 1990s, the annual days of occurring low temperature ≤ -20 ℃ and frost were decreased, but those of high temperature ≥35 ℃ , heavy rain and drought were increased, and these trends met the abrupt warming in the Hexi Corridor. There is a long-term periodical change in high temperature and drought but a staggered one in sandstorm and thunderstorm, and the periodical change of other extreme weather and climate events is not so obvious.
Keywords:Hexi corridor  extreme weather  climatic trend  climate warming  Gansu    
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