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Comparison of two distributed hydrological model for soil moisture simulation

机译:两分布水分模拟对土壤水分模拟的比较

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Soil moisture is one of the most important factors for hydrology research and agriculture management. But it is measured only at limited locations and temporal periods due to the limitations of technology and economy. Distributed hydrological model can simulate the variation and spatial distribution of soil moisture conveniently. This paper compared the simulation results of two different distributed hydrological models and the results show that simulated soil moisture is perfect and the spatial distribution have a tight relationship with the land cover and soil type in AFFDEF model, but in WATLAC model it is different. In WATLAC model results, soil water content changed with groundwater head, but the soil moisture are changed periodic in every year, and maybe it is the results of temperature effect in AFFDEF model results.
机译:土壤水分是水文研究和农业管理最重要的因素之一。但由于技术和经济的局限性,它仅在有限地点和时间时段测量。分布式水文模型可以方便地模拟土壤水分的变化和空间分布。本文比较了两种不同分布式水文模型的仿真结果,结果表明,模拟土壤水分是完美的,空间分布与Affdef模型的陆地覆盖和土壤类型紧密关系,但在Watlac模型中它是不同的。在Watlac模型的结果中,土壤水含量随地下水的变化,但土壤水分在每年都发生变化,也可能是弥漫模型的温度效应的结果。

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