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Long-term hydrologic simulation using SCS-CN-based improved soil moisture accounting procedure

机译:使用基于SCS-CN的改良土壤水分核算程序进行长期水文模拟

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The Soil Conservation Service Curve Number (SCS-CN) method is widely used in determination of direct surface run-offnin long-term (continuous) hydrologic simulation models. Of late, Michel et al. (2005) reviewed the soil moisture accountingn(SMA) procedure that lies behind the original SCS-CN method and pointed out severe structural inconsistencies in the treatmentnof antecedent condition and, in turn, proposed a sounder methodology. However, this method still needs refinement in thendefinition of initial moisture level (V0) to make it usable in field. Thus, in the present study, the Michel et al. (2005) modelnis modified to avoid the unrealistic sudden jump in V0 by incorporating conceptual SMA procedure and variation of dailynCN based on antecedent moisture amount instead of antecedent moisture condition. When applied to 17 watersheds fromndifferent agro-climatic regions of India, the proposed model simulates daily stream flows better than those due to Michelnet al. model. The proposed model performed better in high run-off producing (wet) watersheds than in low run-off producingn(dry) watersheds, and the base flow was more and less significant in high and low run-off producing watersheds, respectively,nwhereas the evapotranspiration showed a reverse trend. Copyright  2010 John Wiley & Sons, Ltd.
机译:水土保持服务曲线号(SCS-CN)方法广泛用于确定长期(连续)水文模拟模型的直接表面径流。最近,米歇尔等。 (2005年)回顾了原始SCS-CN方法背后的土壤湿度核算程序,并指出了在处理前期条件时存在严重的结构不一致之处,进而提出了一种更合理的方法。但是,在定义初始湿度水平(V0)使其可在现场使用时,仍然需要完善此方法。因此,在本研究中,Michel等人。 (2005年)模型修改,通过结合概念上的SMA程序和基于前含水量而不是前含水量条件的daynCN的变化来避免V0突然跳升。当应用于来自印度不同农业气候地区的17个流域时,所提出的模型比Michelnet等人更好地模拟了日流量。模型。所提出的模型在高径流产生(湿)流域中的表现要好于低径流产生(干)流域,并且在高径流产生流域和低径流产生流域中,基本流量分别变得越来越不重要。蒸散量呈相反趋势。版权所有©2010 John Wiley&Sons,Ltd.

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