Morphometric Characterization of the Pindar Basin, Garhwal Himalaya, Uttarakhand

Morphometric analysis is a vital tool for understanding river basins' hydrological and geomorphological characteristics, which aids in effective watershed management and sustainable development. This study focuses on the Pindar Basin in Uttarakhand, India, a key tributary of the Alaknanda River in the central Himalayas. Utilizing Advanced Land Observing Satellite (ALOS) PALSAR Digital Elevation Model (DEM) data along with topographical maps, we computed Drainage Network, Basin Geometry, Drainage Texture, and Relief morphometric parameters to assess the basin's geomorphic behavior. The analysis includes detailed calculations of stream order, stream length, bifurcation ratio, channel length, valley length, channel index, and valley index under drainage network parameters. Basin Geometry includes basin length, area, perimeter, form factor, elongation ratio, and circularity ratio, providing insights into the basin’s shape, flow efficiency, and potential for surface runoff. Drainage Texture analysis includes drainage density, stream frequency, drainage pattern, drainage texture, and infiltration number. Relief parameters, including basin relief, relief ratio, and ruggedness number, were used to evaluate the elevation variations and landscape ruggedness. Results reveal that the Pindar Basin exhibits a dendritic drainage pattern, characteristic of regions with uniform lithology and moderate-to-steep slopes. The relatively high drainage density and moderate bifurcation ratio indicate moderate permeability and a mature stage of basin development. The Hypsometric integral of 0.49 indicates a transitional stage between youth and maturity, with active erosion and modest relief. Relief characteristics suggest a highly rugged terrain, highlighting the basin's susceptibility to soil erosion and potential flash floods. This comprehensive morphometric assessment offers a foundation for understanding the basin's hydrological response and provides critical insights for regional watershed management and disaster risk mitigation in this environmentally sensitive Himalayan region.

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2024-12-30
DOI
https://doi.org/10.5281/zenodo.15574948
Primary Topic
Groundwater and Watershed Analysis
Type
article
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article

Morphometric Characterization of the Pindar Basin, Garhwal Himalaya, Uttarakhand

Zenodo (CERN European Organization for Nuclear Research)
Groundwater and Watershed Analysis
article

Morphometric Characterization of the Pindar Basin, Garhwal Himalaya, Uttarakhand

article en

Abstract

Morphometric analysis is a vital tool for understanding river basins' hydrological and geomorphological characteristics, which aids in effective watershed management and sustainable development. This study focuses on the Pindar Basin in Uttarakhand, India, a key tributary of the Alaknanda River in the central Himalayas. Utilizing Advanced Land Observing Satellite (ALOS) PALSAR Digital Elevation Model (DEM) data along with topographical maps, we computed Drainage Network, Basin Geometry, Drainage Texture, and Relief morphometric parameters to assess the basin's geomorphic behavior. The analysis includes detailed calculations of stream order, stream length, bifurcation ratio, channel length, valley length, channel index, and valley index under drainage network parameters. Basin Geometry includes basin length, area, perimeter, form factor, elongation ratio, and circularity ratio, providing insights into the basin’s shape, flow efficiency, and potential for surface runoff. Drainage Texture analysis includes drainage density, stream frequency, drainage pattern, drainage texture, and infiltration number. Relief parameters, including basin relief, relief ratio, and ruggedness number, were used to evaluate the elevation variations and landscape ruggedness. Results reveal that the Pindar Basin exhibits a dendritic drainage pattern, characteristic of regions with uniform lithology and moderate-to-steep slopes. The relatively high drainage density and moderate bifurcation ratio indicate moderate permeability and a mature stage of basin development. The Hypsometric integral of 0.49 indicates a transitional stage between youth and maturity, with active erosion and modest relief. Relief characteristics suggest a highly rugged terrain, highlighting the basin's susceptibility to soil erosion and potential flash floods. This comprehensive morphometric assessment offers a foundation for understanding the basin's hydrological response and provides critical insights for regional watershed management and disaster risk mitigation in this environmentally sensitive Himalayan region.

Zenodo (CERN European Organization for Nuclear Research)
Openalex Percentile: Top 72%
Groundwater and Watershed Analysis
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