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首页> 外文期刊>Journal of water and climate change >Assessment of variability in runoff coefficients and their linkages with physiographic and climatic characteristics of two contrasting catchments
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Assessment of variability in runoff coefficients and their linkages with physiographic and climatic characteristics of two contrasting catchments

机译:评估两个相反集水区径流系数的变化及其与地貌和气候特征的联系

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In the present study, long-term spatio-temporal variability in runoff coefficient (C) for different drainage areas of Upper Tapi basin, India, is analysed. The Upper Tapi basin is divided into two sub-catchments, Burhanpur and Purna, which are contrasting in nature in terms of their physiographic and climatic characteristics. The digital filter algorithm has been used to separate the base flow from observed streamflow for respective drainage areas. The sensitivity of the parameters involved in base flow separation is assessed by incorporating the hydrological and hydrogeological properties of individual drainage areas. The C values are then computed at different temporal scales, namely, daily, monthly, seasonal and annual, for different drainage areas. The effects of physiographic features such as topography, geology, soil type, and land use; and climatic features such as rainfall, temperature, and evapotranspiration, on the variability of C values are further investigated. The analyses reveal that Burhanpur sub-catchment (C = 0.39) yields higher C value compared to Puma sub-catchment (C = 0.11) at annual time scale. The C values clearly highlight the diversity in response of both sub-catchments, due to their distinct physiographic and climatic characteristics, and enabled us to study the variability in annual water balance of the basin.
机译:在本研究中,分析了印度上塔皮盆地不同流域的径流系数(C)的长期时空变化。塔皮河上游盆地分为两个子汇水区,布尔汉普尔河和普尔纳河,在自然地理和气候特征方面形成鲜明对比。数字过滤器算法已用于将基本流量与相应排水区域的观测流量分开。通过合并各个流域的水文和水文地质特性,可以评估与基本流分离有关的参数的敏感性。然后,针对不同的流域,在不同的时间尺度上(即每天,每月,季节性和年度)计算C值。地形,地质,土壤类型和土地利用等地貌特征的影响;以及气候特征,如降雨,温度和蒸散量,对C值的变化性进行了进一步研究。分析表明,在每年的时间尺度上,Burhanpur子集水区(C = 0.39)比Puma子集水区(C = 0.11)产生更高的C值。由于C和C的独特的地理和气候特征,它们的C值清楚地突出了这两个子汇水区响应的多样性,并使我们能够研究流域年度水平衡的变化。

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