Striking a Balance between Conservation and Development: A Geospatial Approach to Watershed Prioritisation in the Himalayan Basin

Parvaiz Ahmad Ganie, Ravindra Posti, Vidya Shree Bharti, Vinay Kumar Sehgal, Debajit Sarma, Pramod Kumar Pandey
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Abstract

This study was undertaken in the Himalayan basin, in the river Lohawati, Uttarakhand, to study its hydro-morphological characteristics and prioritise the watersheds using geospatial tools. Advanced Spaceborne Thermal Emission and Reflection (ASTER-30 m) data and the Survey of India’s topographic sheets were used to analyse the study area comprehensively. Nine watersheds were identified within the basin in order to calculate the hydro-morphological characteristics in terms of basic, shape, texture, and relief aspects. The basin was identified as being elongated, with a total drainage area of 337.48 km2. The interaction between the terrain, rock formations, and precipitation levels produced a branching structure in the areas drainage system that ranged from dendritic to sub-dendritic. The basin had been classified as a fifth-order basin, comprising a network of 500 stream segments spanning a total length of 492.41 km. In each of the watersheds, the primary streams are of the first order, followed by those of the second order, and so forth. The physiography and lithology of the basin have a significant influence on this pattern. The calculated elongation ratio, circulatory ratio, form factor, shape index, and shape factor ranged from 0.57 to 0.80, 0.35 to 0.64, 0.26 to 0.50, 1.98 to 3.89, and 0.57 to 1.77, respectively. These values indicate that watersheds are elongated, suggesting moderate lag times. The parameters, including drainage density (0.98 to 1.62), stream frequency (1.07 to 1.59), infiltration number (1.04 to 2.59), drainage texture (0.67 to 2.82), and drainage intensity (0.93 to 1.12), pointed towards the coarser drainage texture, higher infiltration, and minimal runoff characteristics of the basin. In light of the relief characteristics of the basin, a higher basin relief, relief ratio, and relative relief were observed for the watersheds, indicating the possibility of higher erosion and deforestation rates. Using the Weighted Sum Analysis (WSA) method, the computed factors were utilised to rank the watersheds based on their potential for erosion. Based on the WSA approach, watersheds were classified into high-, moderate-, and low-prioritisation zones. This further indicates that 36.14% (121.95 km2) of watersheds are in the high-priority zone, and that 48.84% (164.91 km2) and 15.00% (50.62 km2) of watersheds are in the moderate- and low-priority zones, respectively. The WSA is a practical strategy to prioritise watersheds when making appropriate decisions.
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在保护与发展之间取得平衡:喜马拉雅盆地流域优先排序的地理空间方法
本研究在喜马拉雅盆地进行,在北阿坎德邦的洛哈瓦蒂河,研究其水文形态特征,并使用地理空间工具对流域进行优先排序。先进星载热发射和反射(ASTER-30 m)数据和印度地形调查数据被用于全面分析研究区域。在流域内确定了9个流域,从基本、形状、纹理和地形等方面计算了流域的水文形态特征。流域为狭长型,流域总面积为337.48 km2。地形、岩层和降水水平之间的相互作用在该地区的排水系统中形成了树枝状到亚树枝状的分支结构。该盆地被划分为第五级盆地,由500个河段组成,全长492.41公里。在每一个流域,主要的河流是一级,其次是二级,依此类推。盆地的地形和岩性对这一格局有重要影响。伸长率、循环率、形状因子、形状指数和形状因子的计算范围分别为0.57 ~ 0.80、0.35 ~ 0.64、0.26 ~ 0.50、1.98 ~ 3.89和0.57 ~ 1.77。这些值表明分水岭被拉长,表明延迟时间适中。流域排水密度(0.98 ~ 1.62)、径流频次(1.07 ~ 1.59)、入渗数(1.04 ~ 2.59)、排水质地(0.67 ~ 2.82)、排水强度(0.93 ~ 1.12)等参数均显示流域排水质地较粗、入渗较高、径流较少的特征。根据流域起伏特征,流域起伏度、起伏比和相对起伏度较高,表明流域侵蚀率和毁林率可能较高。利用加权和分析(WSA)方法,利用计算得到的因子对流域的侵蚀潜力进行排序。基于WSA方法,流域被划分为高优先区、中等优先区和低优先区。高优先区占36.14% (121.95 km2),中低优先区占48.84% (164.91 km2),低优先区占15.00% (50.62 km2)。WSA是一种实用的策略,可以在做出适当决策时优先考虑流域。
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