首页|1961-2012年辽宁省不同级别降水事件变化特征

1961-2012年辽宁省不同级别降水事件变化特征

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利用1961—2012年辽宁省52个气象站降水资料,采用线性倾向估计、趋势分析及 Mann-Kendell 等方法,分析了辽宁省降水量、降水日数及降水强度的变化特征。结果表明:辽宁省降水量和降水日数最高值均出现在7月,降水强度最高值出现在8月。年降水量呈减少的趋势(3.47 mm/10 a),冬季和春季降水量呈增加的趋势,夏季和秋季降水量呈减少的趋势,年降水量减少主要是由于夏季小雨降水量的减少引起的。年降水日数呈显著减少的趋势(2.93 d/10 a),春季降水日数增加,夏季和秋季降水日数减少,冬季降水日数无明显变化,年降水日数的减少主要是由于夏季小雨日数的减少引起的。年降水强度呈显著增加的趋势(0.22(mm·d -1)/10 a),四季降水强度均呈增加的趋势,年降水强度的增加主要是由于秋季小雨降水强度的增加引起的。辽宁省降水量由西北向东南递增,凤城地区降水量减少速率最大,为28.40 mm/10 a;年降水日数呈东多西少的分布,新宾地区降水日数减少最明显,减少速率为9.9 d/10 a;年降水强度高值区位于辽宁东部地区,东港地区降水强度增加最大,为0.80(mm·d -1)/10 a。年降水量与年降水日数的空间分布和长期变化趋势较相似,而其与年降水强度的长期变化趋势相反。年降水量和年降水强度无明显的突变,年降水日数的突变年份为1981年。
Characteristics of precipitation events of different levels in Liaoning province from 1961 to 2012
Based on precipitation data from 52 weather stations from 1961 to 2012 in Liaoning province,character-istics of precipitation,number of rain day and rain intensity in Liaoning province were analyzed by methods of a linear trend estimate,a trend analysis and a Mann-Kendall and so on.The results show that the maximums of pre-cipitation and number of rain day both occur in July,while the maximium of rain intensity is in August.Annual precipitation both are in a decreasing trend (3.47 mm/10 a),so is summer and autumn precipitation.However, winter and spring precipitation both are in increasing trends.The number of annual rain day is also in a decreasing trend (2.93 mm/10 a)because of decreasing in light rain day in summer.The number of rain day in spring is in an increasing trend,while that in summer and autumn is in a decreasing trend.There is not significant change for the number of winter rain day.Rain intensity is in a signigicant increasing tendency (0.22 mm·d -1 per ten years) because of increasing in light rain intensity in autumn,so is seasonal rain intensity.Precipitation increases from northwest to southeast in Liaoning province.The maximum decreasing rate occurs in Fengcheng with 28.4 mm per decade.Annual rain day is more in east than in west.The maximum decreasing rate is in Xinbin with 9.9 days per decade.Annual rain intensity is higher in the east of Liaoning province,especially in Donggang with increasing rate of 0.8 mm·d -1 per decade.Spatial distribution and long changing tendency of annual precipitation are similar to those of rain day,while it is an opposite changing tendency with rain intensity.Annual rain day has an abrupt change in 1981,while annual precipitation and rain intensity have no obvious abrupt changes.

PrecipitationRain dayRain intensityAbrupt change

周晓宇、敖雪、赵春雨、崔妍、王颖、刘鸣彦、张新宜、王涛

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沈阳区域气候中心,辽宁 沈阳 110166

黄石市气象局,湖北 黄石 435002

降水量 降水日数 降水强度 突变

公益性行业(气象)科研专项中国气象局气候变化专项中国气象局气候变化专项

GYHY201206012CCSF201338CCSF201321

2015

气象与环境学报
中国气象局沈阳大气环境研究所

气象与环境学报

CSTPCD
影响因子:1.433
ISSN:1673-503X
年,卷(期):2015.(5)
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