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近56a武汉市降水气候变化特征分析
引用本文:张意林,覃军,陈正洪.近56a武汉市降水气候变化特征分析[J].湖北气象,2008,27(3):253-257.
作者姓名:张意林  覃军  陈正洪
作者单位:[1]中国地质大学,武汉430074 [2]武汉区域气候中心,武汉430074
基金项目:中国气象局气候变化专项基金,武汉区域气象中心重点科技项目
摘    要:以武汉市1951—2006年逐日降水资料为基础,采用累积距平、线性趋势、移动T检验、5%分位数、小波分析等方法,分析了近56a来武汉市降水气候变化特征。结果表明:(1)近56年来,武汉市年降水量、降水强度呈增加趋势,而降水日数呈减少趋势;(2)除春季外,其它季节以及汛期、梅雨期、伏旱期等时段的降水量均有所增加;降水日数在春、秋季、汛期呈下降趋势,其余时段则为增加趋势;降水强度在夏季、伏早期呈减小趋势,其余时段均为增大趋势;(3)梅雨期、年的降水量变化较为一致,其周期性变化明显,主要表现为10a年代际周期,突变点约在1979年;(4)1960、1970年代暴雨日数较少,在1979年前后突变增多后,进人多暴雨阶段;(5)历年最大日降水量、5%分位数极端降水强度、暴雨平均强度变化略有减少趋势但不显著,而大暴雨平均强度减弱趋势明显。

关 键 词:武汉市  降水  气候变化  趋势  极端值  突变

Analysis on the Change Characteristics of Precipitation in the Latest 56 Years in Wuhan
ZHANG Yi-lin,QIN Jun,CHEN Zheng-hong.Analysis on the Change Characteristics of Precipitation in the Latest 56 Years in Wuhan[J].Meteorology Journal of Hubei,2008,27(3):253-257.
Authors:ZHANG Yi-lin  QIN Jun  CHEN Zheng-hong
Institution:ZHANG Yi-lin, QIN Jun, CHEN Zheng-hong ( 1. China University of Geosciences, Wuhan 430074 ;2. Wuhan Regional Climate Center, Wuhan 430074)
Abstract:Based on the data of daily rainfall from 1951 to 2006 in Wuhan, several methods such as linear tendency, cumulative distance, analysis of little wave and Moving-T-Test (M33) are adopted to analyze the rainfall climate change. The results show: (1) in the latest 56 years in Wuhan, the rainfall and rain intensity are increasing and the number of raining day is decreasing; (2) except the spring, the rainfall in the flood season, and hot-drought season is increasing; the number of raining day is decreasing in spring, autumn and the flood season and increasing in the other spells; the rain intensity is decreasing in summer especially the hot-drought season; (3) there are increasing trend of the rainfall and the number of raining day both in the flood season and the total year with a obvious period of ten years; (4) there is a abrupt increasing change for the number of heavy rain day near 1979 with the less number of heavy rain day in 1960s and 1970s and more in 1980s and 2000s; (5) all indexes of the extreme precipitation including the yearly maximum rainfall, 5% value of daily rainfall, the number of raining day and the average rain intensity show a little decreasing tendency, but the average intensity of the torrential rain (daily rainfall ≥ 100 mm) is decreasing obviously.
Keywords:Rainfall  Climate changes  Tendency  Extremes  Abrupt change
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