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Development of the WEP-L distributed hydrological model and dynamic assessment of water resources in the Yellow River basin

机译:黄河流域WEP-L分布式水文模型的建立与水资源动态评价。

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Dynamic assessment of water resources becomes desirable to reflect water resources variations in the basins under strong human impacts. A physically based distributed hydrological model, WEP-L, which couples simulations of natural hydrological processes and water use processes, is developed for the purpose. Concepts of special water resources (i.e., surface water resources and groundwater resources) and genera[ water resources (i.e., the special water resources plus the precipitation directly utilized by ecosystem) are proposed, and an approach for dynamic assessment of water resources is suggested. Basin subdivision, classification of [and covers, and deduction of water use spatial/temporal distributions in the Yellow River basin are carried out with the aid of remote sensing (RS) data and geographic information system (GIS) techniques. The basin is subdivided into 8485 sub-watersheds and 38,720 contour bands, and the WEP-L model is verified by comparing simulated and observed discharges at main gage stations. Lastly, continuous simulations of 45 years (1956-2000) in variable time steps (from 1 h to 1 day) are performed for various [and cover and water use conditions, and water resources assessment results under present condition of land cover and water use are compared with those under historical condition of [and cover and water use. The study results reveal that: (1) the surface water resources reduced, but the groundwater resources non-overlapped with the surface water resources increased under the impact of human activities in the Yellow River basin; and (2) the special water resources reduced, but the general water resources increased accompanied with increase of the precipitation directly utilized by ecosystem in the basin. (c) 2006 Elseiver B.V. All rights reserved.
机译:为了反映人类强烈影响下流域水资源的变化,需要对水资源进行动态评估。为此,开发了基于物理的分布式水文模型WEP-L,该模型结合了自然水文过程和用水过程的模拟。提出了特殊水资源(地表水资源和地下水资源)和一般水资源(即特殊水资源加上生态系统直接利用的降水量)的概念,并提出了一种动态评估水资源的方法。借助遥感(RS)数据和地理信息系统(GIS)技术,对黄河流域进行了流域细分,[和覆盖物分类以及推断用水量的时空分布]。该流域被细分为8485个子流域和38,720个等高带,并通过比较主要测站的模拟流量和观测流量来验证WEP-L模型。最后,针对各种[以及覆盖和水的使用条件,以及在当前土地覆盖和水的使用条件下的水资源评估结果],以可变的时间步长(从1 h到1天)进行了45年(1956-2000)的连续模拟。将其与[以及覆盖和用水的历史条件下的那些]进行比较。研究结果表明:(1)在黄河流域人为活动的影响下,地表水资源减少,但不与地表水资源重叠的地下水资源增加; (2)特殊水资源减少,但一般水资源增加,流域生态系统直接利用的降水量增加。 (c)2006 Elseiver B.V.保留所有权利。

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