西北地区不同流域内循环降水率的模拟

黑河流域 内循环降水率 数值模拟
高艳红 2009-01 项目
【英文摘要】Water recycling is a quantitative index for impact of land surface on atmosphere water cycle. While, large uncertanty and disputed exist in this issue by now, especially in Northwest China, where the inner land watershed formed along the unique topography. How much in deed the water recycling in the inner basin is still a key question worthwhile. Several reanalyzed soil moisture data sets for the Heihe River Basin will be assessed based on the remote sensing data and field observations in the first place, And, the best one will be selected as the initializatyion and lower boundary condition for mesoscale atmosphere numerical modeling. The high resolution hydrology-atmospheric coupling model enhanced by Gao et al. will be used, in which the land surface water cycle is included and sutable for complex topography like Qilian Mountain. The spatial distribution of evaporation and precipitation ratio will be modleded through numerical simulation. Finally, the water recycling for the Heihe River Basin will be quanlitatively estimated through the comparison with the sensitive experiments.
【中文摘要】内循环降水率是陆面对大气降水影响的定量指标。目前,对于内循环降水率还存在很大争议,尤其是在我国西北地区,独特的地形造就了独特的内陆河流域,该区域内循环降水率究竟有多大还是一个非常值得深入研究的问题。本项目拟对照卫星遥感资料以及野外观测数据,选取较符合黑河流域土壤湿度实际分布的再分析资料,为中尺度数值模拟提供较为准确的土壤湿度初、边值条件;利用高艳红等发展的耦合了陆面水循环过程、适合复杂地形的高分辨率的水文-大气耦合模式,通过数值模拟手段,模拟黑河流域蒸发量和降水率的空间分布特征;通过与敏感性试验模拟结果的对比,初步估算黑河流域的内循环降水率。