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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:利用美国NCEP / NCAR的1960年至2009年月平均再分析数据(2.5°×2.5°)和塔里木河流域26个气象站的每日降水数据,分析了塔里木河流域(TRB)降水的时空演变特征。结果表明:1)TRB的降水空间分布与中国相反,从东南向西北呈逐渐增加的趋势,不同季节和年份降水量较多(较少); 2)山区,平原和五个次区域的年降水量变化可能是一致的,1987年和2003年左右降水的年代际突变几乎出现在所有区域。 3)1978年至2003年是全球变暖最严重的时期,山区降水明显增加,而平原降水减少。可以相信,TRB降水时空分布的复杂性暗示了该地区的各种降水机制,而天山西部的湿热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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