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Spatiotemporal evolution characteristics of precipitation in Tarim River Basin during 1960–2009

机译:1960 - 2009年塔里木河流域降水的时空演变特征

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Using U.S. NCEP / NCAR monthly mean reanalysis data (2.5°×2.5°) and daily precipitation data at 26 weather stations in Tarim River Basin from 1960 to 2009, spatiotemporal evolution characteristics of precipitation over Tarim River Basin (TRB) were analyzed. The results show that: 1) The spatial distribution of precipitation in TRB was in contrast with that in China, showing a gradual increase trend from southeast to northwest with some variation in different seasons and the year with more (less) rainfall; 2)The annual change in precipitation over mountains, plains and five sub-regions were likely consistent, and the decadal mutation of precipitation in around 1987 and 2003 appeared at almost all regions; 3)During the period of 1978 to 2003 in which global warming was the most significant, precipitation over mountain showed an clear increasing trend, while the precipitation over plain showed decreasing trend. It can be believed that the complexity of spatiotemporal distribution of precipitation over TRB implied a variety of precipitation mechanisms in this area, and the warm and wet evidence in western Tianshan Mountains may be the signal that global warming is accelerating the local water cycle.
机译:从1960年到2009年,使用美国NCEP / NCAR每月平均再分析数据(2.5°×2.5°)和塔里木河流域的26个气象站的每日降水数据,分析了塔里木河流域(TRB)降水的时空演化特征。结果表明:1)TRB中降水的空间分布与中国相比,逐渐增加了西北地区的逐步增加趋势,在不同季节和年度的变化中,更多(更少)降雨量; 2)山脉,平原和五个子地区降水的年度变化可能是一致的,1987年左右的降水突变在几乎所有地区出现; 3)在1978年至2003年期间,全球变暖是最重要的,山区的降水显示出明显的趋势,而过度降水表现出降低趋势。可以据信,在TRB上降水的时空分布的复杂性隐含着各种沉淀机制在这一领域,西天山山脉的温暖和潮湿的证据可能是全球变暖正在加速当地水循环的信号。

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