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Hydromorphological analysis of Upper Tapi River Sub-basin, India, using QSWAT model

机译:使用QSwat模型的上塔基河盆地盆地的水样分析

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Morphometric parameters of a drainage basin are quantitative attributes of the landscape that are derived from the elevation surface and drainage network. The drainage characteristics of Upper Tapi River Sub-basin, India, were analysed by SRTM DEM using GIS tools, and the hydrologic parameters were calculated using QSWAT model. The QSWAT model was calibrated for the period 1991-2005 including 3-year warm-up period (1988-1990) with Sequential Uncertainty Fitting (SUFI-2) algorithm in SWAT Calibration and Uncertainty Program and validated for the period 2006-2013. The model performance is evaluated based on R-2 (0.75), ENS (0.75) and PBIAS (1.1) values, which indicate very good agreement between observed and simulated discharge. The study area has been subdivided into 14 sub-watersheds, and 22 morphometric parameters have been calculated under three broad categories, viz. linear, aerial, and relief characteristics. The various morphometric and hydrologic parameters have been correlated with each other to understand their underlying relationship and control over the basin hydro-geomorphology. The R-2 values for drainage density (D-d), sediment yield and evapotranspiration vary from 0.30 to 0.40. Similarly, the R-2 values for stream frequency (F-s) and potential evapotranspiration, base flow, deep percolation, water yield were 0.93. 0.79, 0.75 and 0.81, respectively. The relationships among infiltration number (I-f), potential evapotranspiration, base flow, and sediment yield show the R-2 values as 0.57, 0.48, and 0.70. Therefore, integration of morphometric parameters, GIS and QSWAT model have been done in this study to overcome the challenge of scarcity of observed data.
机译:排水盆地的形态测量参数是景观的定量属性,其源自仰角和排水网络。使用GIS工具通过SRTM DEM分析了印度上塔基河子盆地的排水特性,使用QSWAT模型计算了水文参数。 QSWAT模型在1991 - 2005年期间校准,包括3年的预热期(1988-1990),在SWAT校准和不确定性计划中具有连续的不确定性拟合(SUFI-2)算法,并在2006 - 2013年期间验证。基于R-2(0.75),ENS(0.75)和PBIAS(1.1)值进行评估模型性能,这表明观察和模拟放电之间非常良好的一致性。该研究区已被细分为14个次流域,并且在三个广泛类别,viz下计算了22个形态学参数。线性,空中和浮雕特性。各种形态学和水文参数彼此相关,以了解他们的潜在关系和控制盆地水力正面。排水密度(D-D)的R-2值,沉积物产量和蒸发散,0.30至0.40。类似地,流频率(F-S)的R-2值和电位蒸散蒸腾,碱流动,深渗透,水产率为0.93。 0.79,0.75和0.81分别。渗透数(I-F),电位蒸发,碱流和沉积物的关系显示R-2值为0.57,0.48和0.70。因此,已经在本研究中完成了形态学参数,GIS和QSWAT模型的整合,以克服观察到的数据稀缺的挑战。

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