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Incorporating rainfall intensity into daily rainfall records for simulating runoff and infiltration into soil profiles

机译:将降雨强度纳入日常降雨记录中,以模拟径流和土壤剖面入渗

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摘要

Hydrological modelling often implies the use of rainfall data. Its quality and resolution directly affect the accuracy of the simulation results. This study illustrates that a simple approach of incorporating rainfall intensity information in daily rainfall records significantly improves the simulation of surface runoff and rainfall infiltration into soil profiles. The procedure is developed using a frequency analysis on rainfall data of the Royal Meteorological Institute of Belgium, collected with a resolution of 10 min and for a consecutive period of 61 years. The frequency analysis of the data allowed the incorporation of rainfall intensity information into daily rainfall records. To test the effect of this approach the surface runoff and water flow into three different soil types was simulated using the HYDRUS-1D model for a typical dry, normal and wet year. The simulation results whereby the observed 10-min rainfall data was used as input were considered as the reference. Comparative analysis revealed that the simulations using the 10 min rainfall data deducted from the incorporation of rainfall intensity into daily rainfall records, deviate a maximum 1·2% from the reference and produce much better results than the Soil Conservation Service (SCS) runoff curve-number method because rainfall intensity is considered in the procedure presented. The SCS curve-number method typical overestimates surface runoff during periods of low rainfall intensity (winter) and underestimate runoff during periods of high rainfall intensities (summer). Copyright © 2002 John Wiley & Sons, Ltd.
机译:水文建模通常意味着使用降雨数据。它的质量和分辨率直接影响仿真结果的准确性。这项研究表明,将降雨强度信息纳入每日降雨记录中的简单方法可以显着改善地表径流和降雨入渗到土壤剖面中的模拟。该程序是通过对比利时皇家气象学院的降雨数据进行频率分析而开发的,分辨率为10分钟,连续61年。数据的频率分析允许将降雨强度信息纳入每日降雨记录。为了测试这种方法的效果,使用HYDRUS-1D模型模拟了典型的干旱,正常和湿润年份的地表径流和流入三种不同土壤类型的水。以观测到的10分钟降雨数据作为输入的模拟结果被视为参考。对比分析显示,使用从降雨强度纳入每日降雨记录中扣除的10分钟降雨数据得出的模拟结果,与参考值相比最大偏离了1·2%,并且比土壤保护局(SCS)径流曲线产生了更好的结果-数法,因为在介绍的程序中考虑了降雨强度。 SCS曲线数法通常会高估低降雨强度(冬季)期间的地表径流,而会高估降雨强度(夏季)期间的地表径流。版权所有©2002 John Wiley&Sons,Ltd.

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  • 作者

    Mertens J.; Raes D.; Feyen J.;

  • 作者单位

    Laboratory of Soil and Water Faculty of Agricultural and Applied Biological Sciences Katholieke Universiteit Leuven Vital Decosterstraat 102 B‐3000 Leuven Belgium. Laboratory of Soil and Water Faculty of Agricultural and Applied Biological Sciences Katholieke Universiteit Vital Decosterstraat 102 B‐3000 Leuven Belgium.;

    Laboratory of Soil and Water Faculty of Agricultural and Applied Biological Sciences Katholieke Universiteit Leuven Vital Decosterstraat 102 B‐3000 Leuven Belgium;

    Laboratory of Soil and Water Faculty of Agricultural and Applied Biological Sciences Katholieke Universiteit Leuven Vital Decosterstraat 102 B‐3000 Leuven Belgium;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    hydrology; rainfall intensity; daily rainfall records; runoff; disaggregation;

    机译:水文;降雨强度;日降水记录;径流;分解;

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