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One-dimensional hydrodynamic modeling of GLOF and impact on hydropower projects in Dhauliganga River using remote sensing and GIS applications

机译:利用遥感和GIS应用对GLOF的一维水动力模型及其对道里甘加河水电项目的影响

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This study presents the one-dimensional hydrodynamic modeling for the Glacier Lake Outburst Flood (GLOF) simulation for the six hydroelectric (HE) power projects in Dhauliganga River of Alaknanda Basin. ArcGIS and HEC-GeoRAS extension is used for the whole river GIS database creation. Elevation values and cross-sections were taken from digital elevation models. The initial flow hydrographs were used as upstream boundary condition in MIKE11. The land use/land cover map and Manning's N values for roughness were prepared using LANDSAT TM and CARTOSAT-1 and verified by the field observation. Cross-sections were also modified after identifying the actual cross-sections width and depth. Subsequently, simulation has been carried out by using MIKE11 HD model at different sections of the river stretch. Calibration is done for the period of June 1, 2001, to May 31, 2002, and validated for the year of 2005 with about 95 % accuracy of observed data. In this study, results have been carried out by 100-year flood ordinates and considering the redistribution of lateral flow from five catchments of Alaknanda Basin. The GLOF peaks for the breach parameters are 1394.28, 1552.04 and 1898.04 m(3)/s for breach width 40, 60 and 80 m, respectively, just the downstream of the lake site. It is inferred from the study that the GLOF for 80 m breach width gives the peak flood of 1575 m(3)/s at the project site 1 for first scenario and 3500 m(3)/s at the site 6 for second scenario. The maximum simulated water levels and depth for the Central Water Commission gauging site at Joshimath are 1381.49 and 4.329 m, respectively, for 100-year-plus GLOF event. This information is critical for the project design discharge calculations.
机译:这项研究为阿拉克南达盆地道里甘加河的六个水力发电项目提供了一维水动力模型,用于模拟冰川湖爆发洪水(GLOF)。 ArcGIS和HEC-GeoRAS扩展用于整个河流GIS数据库的创建。高程值和横截面取自数字高程模型。初始流量水线图被用作MIKE11中的上游边界条件。使用LANDSAT TM和CARTOSAT-1编制土地使用/土地覆盖图和Manning的粗糙度N值,并通过现场观察进行验证。在确定实际横截面的宽度和深度后,还对横截面进行了修改。随后,通过使用MIKE11 HD模型在河段的不同部分进行了模拟。校准在2001年6月1日至2002年5月31日期间进行,并在2005年进行了验证,所测数据的准确性约为95%。在这项研究中,结果由100年的洪水纵坐标进行,并考虑了阿拉克南达盆地5个流域的侧向流量的重新分配。仅在湖泊站点的下游,对于突破宽度40、60和80 m,突破参数的GLOF峰值分别为1394.28、1552.04和1898.04 m(3)/ s。从研究中可以得出,对于第一种情况,在80 m的裂口宽度处的GLOF给出的洪峰峰值为1575 m(3)/ s,对于第二种情况,在站点6处为3500 m(3)/ s。对于100年以上的GLOF事件,位于Joshimath的中央水委员会测量场的最大模拟水位和深度分别为1381.49和4.329 m。此信息对于项目设计排放量的计算至关重要。

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