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Changes in Precipitation and Drought Extremes over the Past Half Century in China

机译:近半个世纪以来中国降水和极端干旱的变化

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Changes in climate extremes have become a hot issue in the research field of climate change recently. Many studies have reported that climate extremes have occurred more frequently and with increasing intensity in recent decades. In this study, thresholds of precipitation and drought extremes were determined by the cumulative distribution function, and their spatiotemporal changes over the past half-century in China were analyzed by relative change rate. The results show that: (1) precipitation extremes increased in all regions except North China, while increasing trends of drought extremes were detected in all regions except Northwest China and the Qing–Tibet Plateau; (2) the maximum change rates in frequency of precipitation extremes were found in Northwest China and the Qing–Tibet Plateau, with values of 16.13% and 8.12%, and the maximum change rates in frequency of drought extremes were in Southwest and Southeast China, whose increases in intensity of drought extremes were also the maximum; (3) variation in precipitation extremes showed a relatively mixed pattern with higher heterogeneity compared to that of drought extremes; and (4) changes in precipitation and drought extremes relate to mid-intensity, lower-intensity, and annual precipitation.
机译:极端气候的变化最近已经成为气候变化研究领域中的热点问题。许多研究报告说,近几十年来,气候极端事件的发生频率越来越高,强度也越来越大。在这项研究中,通过累积分布函数确定了降水和极端干旱的阈值,并通过相对变化率分析了过去半个世纪以来它们的时空变化。结果表明:(1)除华北以外的所有地区的极端降水都增加,而除西北地区和青藏高原以外的所有地区都出现了极端干旱的趋势; (2)西北和青藏高原的极端降水发生频率最大变化率分别为16.13%和8.12%,而极端干旱的最大发生频率变化率在西南和东南地区,其极端干旱强度的增加也是最大的; (3)与干旱极端相比,极端降水的变化表现出相对混合的格局,具有更高的非均质性; (4)降水和极端干旱的变化与中强度,低强度和年降水量有关。

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