首页> 外文期刊>Arabian journal of geosciences >Rainfall-runoff modelling of Doddahalla watershed-an application of HEC-HMS and SCN-CN in ungauged agricultural watershed
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Rainfall-runoff modelling of Doddahalla watershed-an application of HEC-HMS and SCN-CN in ungauged agricultural watershed

机译:Doddahalla流域降雨径流模拟——HEC-HMS和SCN-CN在未开垦农业流域中的应用

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The scarcity of reliable rainfall-runoff recorded data in Doddahalla watershed is a serious problem for the analysis of the hydrology of watersheds. Sustainable management of the available water in this area is only possible when there was sound information on the rainfall-runoff and other hydrological determinants that influence the water resource. Considering the current problem rainfall-runoff. simulation is carried out using the HEC-HMS hydrological simulation model with integrated use of remote sensing and GIS. Tropical Rainfall Measuring Mission 3 hourly and Indian Meteorological Department daily rainfall datasets are utilised. Cartosat-1 CartoDEM (30 m) was used to delineate the sub-watershed and generate the stream network. Geospatial Hydrologic Modeling Extension (HEC-GeoHMS), along with ArcHydro extension in ArcGIS 9.3 utilised to create the input file for use in HEC-HMS. Indian Remote Sensing Satellite Linear Imaging and Self Scanning sensors (LISS-III, 24 m) and Survey of India (SOI) toposheet are used to prepare the soil and land use map. All the data are georectified and reprojected to Geographic Coordinate System-World Geodetic System 1984 (GCS WGS) Universal Transverse Mercator (UTM) zone 43 North for the easy handling in GIS environment. SCS-CN loss model and SCS unit hydrograph as a transform method was applied to simulate the excess storm water to direct runoff in the watershed. The Muskingum-Cunge model used as channel routing. The model is validated by using field observation data and discharge data from the neighbouring Hoovinahole watershed. The results of simulated and observed stream flow show greater confidence and the reliability of the model. Similar procedure and calibration parameters applied to the ungauged Doddahalla watershed for estimating the rainfallrunoff. The research result gives a general idea regarding the stream flow, peak flow and velocity of the peak flow. The present study concludes that the stimulated result can be useful for the water and land resource planning and management practice in the Doddahalla watershed. The models can be best utilised in ungauged watershed and water scarce region where the monitored data are limited, and runoff estimation is mandatory to sustain the water resources.
机译:道达哈拉(Doddahalla)流域缺乏可靠的降雨径流记录数据,这对于分析流域的水文学来说是一个严重的问题。只有掌握了有关降雨径流和其他影响水资源的水文决定因素的可靠信息,才有可能对该地区的可用水进行可持续管理。考虑当前的降雨径流问题。使用结合了遥感和GIS的HEC-HMS水文模拟模型进行模拟。利用每小时3小时的热带雨量测量任务和印度气象部门的每日雨量数据集。 Cartosat-1 CartoDEM(30 m)被用来描绘子流域并产生河流网络。地理空间水文建模扩展(HEC-GeoHMS)与ArcGIS 9.3中的ArcHydro扩展一起用于创建用于HEC-HMS的输入文件。印度遥感卫星线性成像和自扫描传感器(LISS-III,24 m)和印度调查(SOI)地形表用于准备土壤和土地利用图。所有数据都经过地理校正,然后重新投影到1984年的世界地理坐标系(GCS WGS)和北纬43度的通用横轴墨卡托(UTM)区,以便在GIS环境中轻松处理。应用SCS-CN损失模型和SCS单位水位图作为转换方法,模拟了多余的雨水来引导流域内的径流。 Muskingum-Cunge模型用作通道路由。通过使用现场观测数据和邻近的Hoovinahole流域的流量数据对模型进行验证。模拟和观察到的水流的结果显示出更大的置信度和模型的可靠性。将类似的过程和校准参数应用于未覆盖的Doddahalla流域,以估算降雨径流。研究结果给出了关于流量,峰值流量和峰值流量速度的总体思路。本研究得出的结论是,激发的结果对于Doddahalla流域的水土资源规划和管理实践可能是有用的。该模型可以最好地用于监测数据有限的非流域和缺水地区,并且径流估算对于维持水资源是必不可少的。

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