塔什库尔干河谷降水年际异常的水汽输送特征OA
Characteristics of water vapor transport associated with interannual precipitation anomalies in the Taxkorgan Valley
塔什库尔干河谷流域作为高寒山区典型代表流域,其降水是影响帕米尔高原东部水文循环和水资源变化的关键因素,但目前对其降水年际异常变化及水汽输送路径定量特征认识不足.因此,以气象观测资料、GDAS、ERA5再分析数据为基础,分析2013-2023年降水年际异常变化特征,采用HYSPLIT拉格朗日后向轨迹模型进行水汽输送路径定量模拟,并结合欧拉方法研究水汽通量和风场特征,定量揭示塔什库尔干河谷流域水汽输送路径特征,探讨降水异常年的水汽输送成因,结果表明:(1)在平均态上,降水的水汽主要来源于西风带输送,其中大西洋水汽占比14.41%,地中海一带水汽占比39.13%,陆源水汽占比46.46%.(2)从冷季到暖季,西风带上的水汽通道由南到北逐渐北移,西风带海源水汽占比逐渐减小,局地循环水汽补充逐渐增加;夏季有来自印度洋的水汽绕过青藏高原到达塔什库尔干河谷.(3)塔什库尔干河谷流域有效降水与西风带水汽通道稳定性呈显著正相关.降水异常多年的西风带南压,水汽通道稳定且集中;降水异常少年西风带波动加剧,水汽通道分散且较短,难以形成持续水汽通路.研究成果揭示了塔什库尔干河谷降水年际异常的水汽输送特征及其原因,为理解降水异常机理及预报预测提供科学依据.
Precipitation in the Taxkorgan Valley,a representative high-altitude cold mountainous region,is a criti-cal driver of the hydrological cycle and water resource dynamics in the eastern Pamir Plateau.However,the quan-titative characteristics of its moisture transport pathways and the mechanisms governing interannual precipitation anomalies remain poorly understood.Using meteorological observations alongside GDAS and ERA5 reanalysis datasets,this study analyzes interannual precipitation anomalies from 2013 to 2023.The HYSPLIT Lagrangian backward trajectory was employed to quantitatively simulate moisture transport pathways.By integrating Euleri-an methods to analyze water vapor fluxes and wind fields,we elucidated moisture transport characteristics and at-mospheric drivers during anomalous precipitation years.The results indicate the following.(1)In the climatologi-cal mean state,precipitation moisture is primarily transported by westerly winds:14.41%from the Atlantic Ocean,39.13%from the Mediterranean region,and 46.46%from terrestrial sources.(2)During the transition from cold to warm seasons,the westerly moisture transport corridor shifts northward.This shift leads to a de-creased proportion of marine moisture from the westerlies and an increased contribution from local moisture recy-cling.Notably,during summer,Indian Ocean moisture bypasses the Qinghai-Xizang Plateau to reach the basin.(3)Effective precipitation in the basin exhibits a significant positive correlation with the stability of the westerlies moisture transport corridor.During anomalously wet years,a southward shift of the westerlies establishes stable and concentrated moisture pathways.Conversely,during anomalously dry years,intensified westerly fluctuations lead to dispersed and truncated trajectories,hindering the formation of sustained moisture conduits.These find-ings clarify the moisture transport mechanisms driving interannual precipitation anomalies in the Taxkorgan Val-ley,providing a scientific basis for regional precipitation forecasting and climate prediction.
李晗薇;姚俊强;刘精;张载勇;高紫璇;孙英玮
中国气象局气象干部培训学院新疆分院,新疆 乌鲁木齐 830013中国气象局乌鲁木齐沙漠气象研究所,新疆 乌鲁木齐 830002新疆维吾尔自治区气候中心,新疆 乌鲁木齐 830002中国气象局气象干部培训学院新疆分院,新疆 乌鲁木齐 830013莱斯特大学物理和天文学院,英国 莱斯特 LE1 7RH中国气象局气象干部培训学院新疆分院,新疆 乌鲁木齐 830013
塔什库尔干河谷降水异常水汽输送特征HYSPLIT大气降水
Taxkorgan Valleyprecipitation anomaliescharacteristics of water vapor transportHYSPLITatmo-spheric precipitation
《干旱区研究》 2026 (10)
2098-2112,15
国家自然科学基金(42571051,42171038)中国气象局气象干部培训学院科研项目(2024CMATCQN13)新疆气象局引导性计划项目(YD2024045,YD2026021)中国气象科学研究院科技发展基金项目(2021KJ034)
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