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1951~2009年东亚地区日降水趋势特征分析
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国家公益性行业专项GYHY201206012


Changes in Daily Precipitation over East Asia during 1951-2009
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    摘要:

    研究大陆或次大陆尺度日降水长期趋势变化规律,对于检测、理解区域气候和陆地水循环对全球气候变暖的响应特征十分重要。利用美国国家气候资料中心(NCDC)和中国基准气候站、基本气象站网降水观测资料,在对该站点资料进行基本质量控制基础上,选取东亚地区619个站1951~2009年日降水数据,按照百分位阈值对降水进行分级,共分为弱、中、强、极强4个级别,用经纬度网格面积加权平均方法构建区域平均的时间序列,分析了各类降水事件长期变化趋势的时空特征。结果表明:东亚地区近59年平均总降水量表现出不显著下降趋势,降水日数没有出现趋势性变化,平均日降水强度略有减小;区域平均的年降水量、降水日数和日降水强度在中国北方大部、蒙古东部、俄罗斯远东地区南部和日本列岛多呈减少趋势,而在俄罗斯中西伯利亚南部、朝鲜半岛南部和中国长江中下游流域一般表现为增加。从季节上看,近59年东亚区域平均的冬、春季降水量、降水日数和日降水强度均呈增加趋势,而夏、秋季一般呈减少趋势,仅夏季日降水强度略有增加。降水的年内分配出现均匀化趋势。从不同级别降水事件看,近59年来东亚区域平均的各级别降水量均为下降趋势,中降水、强降水和极强降水日数也呈现下降趋势,弱降水日数表现出较明显增加;仅有全区秋季强降水量、日数减少趋势和冬季中降水量、日数增加趋势通过了显著性水平检验。分析还发现,近30年(1980~2009年)东亚地区日降水趋势变化出现了新的特征,主要表现为大部分地区降水日数呈现增加,日降水强度减少,45°N以南多数台站降水量也增加,全区降水有向非极端化方向发展趋势。

    Abstract:

    Atmospheric precipitation is a critical component of the terrestrial water cycle. For detecting and understanding the response of the water cycle to global warming at the regional scale, it is important to analyze the temporal and spatial variations in daily precipitation at the continental or subcontinental scale. In this study, daily precipitation data from the US National Climate Data Center (NCDC) and the China National Reference Climate and Basic Meteorological Stations for the period of 1951-2009 were used to analyze the long-term variations in precipitation over East Asia (25°N-55°N, 105°E-145°E). After basic quality control, 619 stations were chosen. Based on the percentile thresholds, the daily rainfall was classified into light, moderate, intense, and very intense. The regional average time series were obtained by the method of the area-weighted average for the grids. The spatial and temporal patterns of the long-term changes in all kinds of precipitation events were also analyzed.
    The results showed that the average regional precipitation and precipitation intensity decreased during the last 59 years (1951-2009), whereas the rainy days exhibited no prominent trend. In most of northern China, eastern Mongolia, southern Russian-Far East, and most of Japan, the amount, frequency, and intensity of annual precipitation generally decreased. However, the southern part of Middle Siberia, the Korean Peninsula, and the Yangtze River basin witnessed increasing trends of the precipitation index series. The amount, frequency, and intensity of seasonal precipitation increased in winter and spring, and decreased in the summer and autumn except for the summer precipitation intensity. The annual seasonal precipitation variability in the last decade was gentler than the previous.
    The regional average precipitation decreased in all categories in 1951-2009. The moderate precipitation decreased faster than the precipitation frequency, whereas the intense and very intense precipitation decreased slightly slower than the precipitation frequency. The moderate, intense, and very intense precipitation frequencies decreased during the last 59 years, and only the light precipitation frequency increased. Note that for the last 30 years (1980-2009), the overall precipitation intensity decreased, whereas the overall precipitation frequency increased for most areas in the study region. Most of the stations south of the 45°N latitude recorded increased annual precipitation; however, the daily precipitation intensity was less extreme.

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战云健,任国玉,任玉玉,李娇.2013.1951~2009年东亚地区日降水趋势特征分析[J].气候与环境研究,18(6):767-780. ZHAN Yunjian, REN Guoyu, REN Yuyu, LI Jiao.2013. Changes in Daily Precipitation over East Asia during 1951-2009[J]. Climatic and Environmental Research (in Chinese],18(6):767-780.

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  • 收稿日期:2012-08-27
  • 最后修改日期:2013-04-27
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  • 在线发布日期: 2013-11-20
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