首页|期刊导航|人民长江|1901~2022年长江流域降水年内分配时空演变规律

1901~2022年长江流域降水年内分配时空演变规律OA

Spatiotemporal evolution of intra-annual precipitation distribution in Changjiang River Basin from 1901 to 2022

中文摘要英文摘要

为评估长时间降水序列在时空维度的变化态势及其对旱涝灾害的影响,采用降水集中指数(PCI)、季节降水集中指数(SPCI)和降水异常指数(RAI)等分析长江流域1901~2022 年间降水年内分配的时空演变以及旱涝变化特征.结果表明:① 1901~2022 年,长江流域多年平均 PCI 为 11~26,表明降水年内分配处于中度集中到异常集中水平;空间上,PCI 值呈现出西北高、东南低的分布格局.② 在整个研究时段内,PCI 的年际变化整体呈增大趋势(0.029/10 a),表明降水年内集中度增强;不同时段内(1901~1960 年和1961~2022 年)PCI 值年际变化趋势存在明显差异,这种差异反映出降水变化在时间维度上的复杂性.③ RAI 分析表明,1901~2022 年长江流域整体呈现湿润化趋势(0.021/10 a);但在不同时间段和不同区域差异显著,部分地区经历了从干旱到湿润的转变,而部分地区则由湿润逐渐转向干旱;这种干湿状态的转变体现了流域气候的多样性和动态性.④ 突变分析表明,在不同研究时段内 PCI 与 SPCI 发生突变的时间不一致,但在1950 年代和1990 年代前后,二者均发生了突变.1901~2022 年长江流域 PCI 经历了3 次突变(1953、1988 年和2002 年);而春、秋和冬季发生突变的时间较早(1931、1920 年和1937 年),春、夏和冬季则在1953 年和1989 年左右再次发生突变.研究成果揭示了长江流域降水模式的转变,其时空演变特征可为旱涝灾害预测提供科学依据,有助于理解区域气候对全球变化的响应机制.

To assess the long-term spatiotemporal evolution of precipitation and its impacts on drought and flood disasters,this study employs the Precipitation Concentration Index(PCI),Seasonal Precipitation Concentration Index(SPCI),and Rainfall A-nomaly Index(RAI)to characterize the intra-annual precipitation distribution and associated drought-flood variations in the Changjiang River Basin from 1901 to 2022.The main findings are as follows:① Over the study period,the multi-year average PCI ranges from 11 to 26 across the basin,indicating a moderate to exceptionally concentrated intra-annual precipitation regime.Spatially,PCI values exhibit a northwest-high,southeast-low pattern.② On an interannual timescale,PCI shows an overall in-creasing trend(0.029 per decade),suggesting a strengthening of intra-annual precipitation concentration.Notably,the trend dif-fers markedly between the sub-periods 1901~1960 and 1961~2022,highlighting the temporal complexity of precipitation chan-ges.③ RAI analysis reveals a general wetting trend across the Changjiang River Basin(0.021 per decade)from 1901 to 2022.However,pronounced variations exist among different sub-periods and sub-regions.Some areas have transitioned from dry to wet conditions,whereas others have shifted from wet to dry,reflecting the diversity and dynamic nature of the basin's climate.④Abrupt change analysis shows that while the timing of abrupt changes in PCI and SPCI varies across study sub-periods,both in-dices experienced abrupt changes around the 1950s and 1990s.For the entire 1901~2022 period,PCI experienced three abrupt changes(in 1953,1988,and 2002).Abrupt changes in spring,autumn,and winter occurred earlier(1931,1920,and 1937,re-spectively),whereas another cluster of abrupt changes occurred around 1953 and 1989 in spring,summer,and winter.These find-ings reveal a shift in the precipitation regime of the Changjiang River Basin.The identified spatiotemporal evolution characteristics provide a scientific basis for predicting drought and flood disasters and contribute to a better understanding of regional climate re-sponses to global change.

张克新;汪田归;刘云龙;彭娇婷

贵州财经大学 管理科学与工程学院,贵州 贵阳 550025贵州财经大学 管理科学与工程学院,贵州 贵阳 550025贵州财经大学 管理科学与工程学院,贵州 贵阳 550025贵州财经大学 管理科学与工程学院,贵州 贵阳 550025

天文与地球科学

降水集中指数降水异常指数时空演变旱涝变化长江流域

Precipitation Concentration IndexRainfall Anomaly Indexspatiotemporal evolutiondrought-flood changesChangjiang River Basin

《人民长江》 2026 (6)

39-48,10

国家自然科学基金项目(42163001)贵州省科技计划项目(黔科合基础-zk[2022]一般023)

10.16232/j.cnki.1001-4179.2026.06.005

评论