Propagation characteristics from meteorological drought to agricultural drought over the Heihe River Basin, Northwest China

In the context of global warming,drought events occur frequently.In order to better understanding the process and mechanism of drought occurrence and evolution,scholars have dedicated much attention on drought propagation,mainly focusing on drought propagation time and propagation probability.However,there are relatively few studies on the sensitivities of drought propagation to seasons and drought levels.Therefore,we took the Heihe River Basin(HRB)of Northwest China as the case study area to quantify the propagation time and propagation probability from meteorological drought to agricultural drought during the period of 1981–2020,and subsequently explore their sensitivities to seasons(irrigation and non-irrigation seasons)and drought levels.The correlation coefficient method and Copula-based interval conditional probability model were employed to determine the drought propagation time and propagation probability.The results determined the average drought propagation time as 8 months in the whole basin,which was reduced by 2 months(i.e.,6 months)on average during the irrigation season and prolonged by 2 months(i.e.,10 months)during the non-irrigation season.Propagation probability was sensitive to both seasons and drought levels,and the sensitivities had noticeable spatial differences in the whole basin.The propagation probability of agricultural drought at different levels generally increased with the meteorological drought levels for the upstream,midstream,and southern downstream regions of the HRB.Lesser agricultural droughts were more likely to be triggered during the irrigation season,while severer agricultural droughts were occurred mostly during the non-irrigation season.The research results are helpful to understand the characteristics of drought propagation and provide a scientific basis for the prevention and control of droughts.This study is of great significance for the rational planning of local water resources and maintaining good ecological environment in the HRB.

1961—2016年北京地区旱涝中心的演变特征

受气候变化影响,北京地区旱涝事件的时空变异性增强。为全面评估北京地区旱涝严重区域的演变特征,通过融合历时、强度、烈度、峰值、频率等多个旱涝特征,采用熵权法构建了归一化旱涝综合特征指标,并通过Kmeans算法识别了旱涝中心。结果表明:归一化旱涝综合特征指标能全面地反映出该地区的旱涝状况;1961—2016年北京地区南部偏旱,昌平、海淀、房山区旱情较为突出,北部偏涝,密云区雨涝较为严重;20世纪60—90年代旱涝交替,整体偏涝,21世纪00—10年代整体偏旱;对于高等级及以上旱涝中心,干旱中心多分布于平原区,雨涝中心多分布于西南部和东北部山区;整体上,干旱中心的重心有向北迁移的趋势,雨涝中心的重心有向东迁移的趋势。