塔里木盆地荒漠区各季节可降水量数据集（1979-2017年）

基于空中水资源基本理论，将大气中由特殊的边界层形成的次生环流锁定且具备发生相变转化为云和降水潜力的水物质定义为有效水汽，然后基于水汽辐合区开发有效水汽识别算法，并对区域可开发空中水资源（即有效水汽）的总量和空中水资源降水潜力进行评估。

Based on the fundamental theory of atmospheric water resources, water substances in the atmosphere that are locked by the secondary circulation generated by a special boundary layer and have the potential to undergo phase transitions into clouds and precipitation are defined as effective water vapor. Subsequently, an effective water vapor recognition algorithm is developed based on water vapor convergence zones, and assessments are carried out for both the total amount of developable regional atmospheric water resources (i.e., effective water vapor) and the precipitation potential of atmospheric water resources.

搜集汇总

背景与挑战

背景概述

该数据集提供了1979年至2017年塔里木盆地荒漠区各季节的可降水量数据，基于ERA-Interim再分析资料通过水汽识别算法计算得出，旨在评估区域空中水资源潜力和支持水资源管理研究。数据以年分辨率呈现，格式为Excel，适用于气候和水文分析。