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Hydrological Modeling of Large Drainage Basins Using a GIS-Based Hybrid Atmospheric and Terrestrial Water Balance (HATWAB) Model

机译:基于GIS的大气和陆地水平衡混合模型的大型流域水文模拟。

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摘要

A Hydrological model is proposed to study the spatial and temporal variability of the water budget components of large drainage basin systems from atmospheric and terrestrial water balances. In order to understand the water balances that include, surface runoff, actual evapotranspiration and soil moisture, a GIS-based simple water balance model which is referred as Hydrological Model from Hybrid Atmospheric and Terrestrial Water Balances with acronym HATWAB is presented. The spatio-temporal climatology database was created from a network of climate stations from CL1MWAT data base to reconstruct the monthly primary inputs to HATWAB model, rainfall and potential evapotranspiration. The modeling principles and HATWAB model are demonstrated using the Limpopo and Congo basins in Africa. The model was used to simulate water balance components by taking rainfall-runoff processes in the basin including soil-texture controlled moisture in the terrestrial system, and the vertical integrated moisture convergence that accounts for the net water vapor flux from the basins in order to close the hydrologic water budget.
机译:提出了一种水文模型,从大气和陆地水平衡的角度研究大型流域系统水平衡要素的时空变化。为了了解包括地表径流,实际蒸散量和土壤湿度在内的水平衡,提出了一种基于GIS的简单水平衡模型,该模型被称为“大气和陆地混合水平衡”的水文模型,缩写为HATWAB。时空气候学数据库是从CL1MWAT数据库的气候站网络创建的,用于重建HATWAB模型的每月主要输入,降雨和潜在的蒸散量。使用非洲的林波波和刚果盆地论证了建模原理和HATWAB模型。该模型用于模拟流域的水平衡要素,包括盆地中的降雨径流过程,包括地面系统中土壤质地受控的水分,以及垂直积分的水分收敛,该因子考虑了来自盆地的净水蒸气通量,以实现封闭。水文用水预算。

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