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The spatial distribution of precipitation over the West Qinling region, China, AD 1470-2000

机译:西秦岭地区的降水空间分布,公元1470-2000年

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摘要

The West Qinling Mountains form part of the climatic barrier that separates southern and northern China, and are located at the edge of the region dominated by the Asian summer monsoon. To investigate the spatial distribution of regional hydroclimatic variability in the West Qinling region, the annually resolved spatial field of rainy season (May-June-July-August-September, MJJAS) precipitation anomalies from AD 1470 to 2000 was reconstructed using 39 tree-ring chronologies, as well as 28 dryness/wetness indices derived from historical documentary data. The results indicate that the El Nifio-Southern Oscillation (ENSO) and the Tropospheric Biennial Oscillation (TBO) may jointly affect the spatial pattern of precipitation over the West Qinling Mountains at inter-annual timescales. The drought in the 1990s was found to exceed the amplitude and duration of all other periods of drought that have occurred since AD 1470 in this region. The new precipitation field reconstruction assesses the spatial pattern of historical hydroclimatic variability in the West Qinling region and provides an opportunity to test the performance of climate models in simulating regional precipitation variability and change. (C) 2015 Elsevier B.V. All rights reserved.
机译:西秦岭山脉是分隔中国南部和北部的气候屏障的一部分,位于亚洲夏季风主导的区域边缘。为了调查西秦岭地区区域水文气候变化的空间分布,使用39个年轮树重建了公元1470年至2000年雨季(5月,6月,7月,8月,9月,MJJAS)的年降水空间异常。从历史文献数据中得出的时间顺序以及28个干/湿指数。结果表明,厄尔尼诺—南部涛动(ENSO)和对流层两年一次涛动(TBO)可能在年际尺度上共同影响西秦岭山脉的降水空间格局。发现1990年代的干旱超过了自公元1470年以来该地区发生的所有其他干旱时期的幅度和持续时间。新的降水场重建评估了西秦岭地区历史水文气候变化的空间格局,并提供了一个机会来测试气候模型在模拟区域降水变化和变化方面的性能。 (C)2015 Elsevier B.V.保留所有权利。

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