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黄河流域1960-2022年干湿格局变化特征OACSTPCD

Spatiotemporal changes in precipitation and drying-wetting patterns in the Yellow River Basin

中文摘要英文摘要

[目的]研究黄河流域降水时空变化,分析气候变化情况下黄河流域降水及干湿格局变化特征.[方法]收集黄河流域 1960-2022年 51 个气象站点降水数据,通过回归分析、相关分析、频率百分数法、Mann-Kendall非参数检验法,探究 1960-2022 年黄河流域降水、干湿期特征时空变化规律及相关性.[结果]①1960-2022 年,黄河流域年降水量变化不显著,但降水频率下降(-1.95%/10 a),强度上升(2.67%/10 a),且均通过显著性检验(P<0.05),年降水频率在 1978年发生突变,年降水强度在 1990年发生突变,自 1990年开始,年降水频率显著减少,强度显著增加.流域上游变湿,中、下游变干,流域整体来看,微降水、小降水、中等强度降水减少,强降水、极端降水增加,在流域上、中、下游微降水普遍减少,极端降水普遍增加;②黄河流域及流域上、中游发生干旱的风险增加,干旱强度下降,流域下游发生干旱风险及强度均呈增加趋势.降水在湿期分配更加集中,流域发生干旱和洪涝风险共存;③年降水量变化主要由高强度降水事件变化引起,年降水频率变化主要受低强度降水事件影响.湿日在年内的分配情况主要受低强度降水事件影响,湿期降水量变化主要是受高强度降水事件影响.[结论]在气候变化背景下,黄河流域发生干旱和洪涝灾害的风险共存,直接原因是低强度降水事件减少导致较短干期合并成较长干期,流域发生干旱风险增加.降水强度增加,降水在湿期更加集中导致流域发生洪涝风险增加.

[Background and Objective]The Yellow River Basin is the second largest river basin in China.Over the past 60 years,precipitation patterns in the basin have undergone both spatial and temporal changes due to the impact of climate change.This paper analyzes the precipitation characteristics and spatiotemporal alterations in dry-wet patterns in the basin.[Method]The study was based on meteorological data measured from 1960 to 2022 at weather stations across the basin.Spatiotemporal changes in precipitation,dry and wet spells were analyzed using regression analysis,correlation analysis,frequency percentage method,and the Mann-Kendall nonparametric statistical method.[Result]① No significant change in total annual precipitation was identified in the basin from 1960 to 2022.However,a notable decrease in annual precipitation events(-1.95%per decade)and a significant increase in average precipitation intensity(+2.67%per decade)were observed.A sudden change in annual precipitation frequency occurred in 1978,while a shift in precipitation intensity happened in 1990.Since 1990,annual precipitation frequency has decreased markedly,while precipitation intensity has increased significantly.Regionally,the upper basin has become wetter,while the middle and lower reaches of the basin have become drier.Across the basin,light,moderate and medium-intensive rainfall events have declined,while heavy and extreme rainfall events have increased.Extreme rainfall event have become increasingly common,particularly in the middle and lower reaches of the basin.② The risk of drought has increased in the upper and middle reaches of the basin,although drought intensity has decreased.Meanwhile,the likelihood and severity of drought in the lower reach has risen.Wet spells have shown heightened precipitation intensity during the wet season,corresponding to an increase in extreme precipitation events across the basin.The coexistence of drought and flooding highlights vulnerability of the basin to extreme weather events.③ Changes in annual precipitation are primarily driven by intensive precipitation events,while changes in precipitation frequency ware influenced by low-intensive precipitation events.The distribution of wet days is affected by low-intensive precipitation,whereas wet-season precipitation is driven by high-intensive precipitation events.[Conclusion]In the context of climate change,the Yellow River Basin is increasingly vulnerable to both droughts and floods.The reduction in low-intensive precipitation events has prolonged dry periods,increasing drought risk.Simultaneously,the increase in precipitation intensity and extreme events during wet seasons raises flood risk.These findings underscore the urgent need for developing integrated water resource managements and new strategies to mitigate the impact of climate change.

马洁;廉陆鹞;刘原峰;苏鹏海;杨茹珍

甘肃省水利水电勘测设计研究院有限责任公司,兰州 730000甘肃省水土保持科学研究所,兰州 730000甘肃地质工程有限责任公司,兰州 730000

大气科学

黄河流域降水干期湿期极端降水

the Yellow River Basinprecipitationdry spellswet spellsextreme precipitation

《灌溉排水学报》 2024 (012)

65-73 / 9

甘肃省科技计划资助-青年科技基金项目(23JRRA1267)

10.13522/j.cnki.ggps.2024209

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