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The drainage basin dynamics of these rivers are controlled by the tectonomorphic parameters, which include both surface and subsurface characteristics of a basin. To understand the drainage basin dynamics and their usefulness in watershed prioritisation and management in terms of soil erosion studies and groundwater potential assessment and flood hazard risk reduction in mountainous rivers, morphometric analysis of a Himalayan River (Supin River) basin has been taken as a case study. The entire Supin River basin has been subdivided into 27 subwatersheds and 36 morphometric parameters have been calculated under four broad categories: drainage network, basin geometry, drainage texture, and relief characteristics, each of which is further grouped into five different clusters having similar morphometric properties. The various morphometric parameters have been correlated with each other to understand their underlying relationship and control over the basin hydrogeomorphology. The result thus generated provides adequate knowledge base required for decision making during strategic planning and delineation of prioritised hazard management zones in mountainous terrains.","grobid_abstract_attachment_id":"40850664"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"high","language":"en","title":"Morphometry Governs the Dynamics of a Drainage Basin: Analysis and Implications","broadcastable":true,"draft":null,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [4729139]; window.loswp.locale = "en"; window.loswp.countryCode = "SG"; window.loswp.cwvAbTestBucket = ""; window.loswp.designVariant = "ds_vanilla"; window.loswp.fullPageMobileSutdModalVariant = "control"; window.loswp.useOptimizedScribd4genScript = false; window.loginModal = {}; window.loginModal.appleClientId = 'edu.academia.applesignon'; window.userInChina = "false";</script><script defer="" src="https://accounts.google.com/gsi/client"></script><div class="ds-loswp-container"><div class="ds-work-card--grid-container"><div class="ds-work-card--container js-loswp-work-card"><div class="ds-work-card--cover"><div class="ds-work-cover--wrapper"><div class="ds-work-cover--container"><button class="ds-work-cover--clickable js-swp-download-button" data-signup-modal="{"location":"swp-splash-paper-cover","attachmentId":40850664,"attachmentType":"pdf"}"><img alt="First page of “Morphometry Governs the Dynamics of a Drainage Basin: Analysis and Implications”" class="ds-work-cover--cover-thumbnail" src="https://0.academia-photos.com/attachment_thumbnails/40850664/mini_magick20190220-15680-ljuvw5.png?1550679030" /><img alt="PDF Icon" class="ds-work-cover--file-icon" src="//a.academia-assets.com/images/single_work_splash/adobe_icon.svg" /><div class="ds-work-cover--hover-container"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span><p>Download Free PDF</p></div><div class="ds-work-cover--ribbon-container">Download Free PDF</div><div class="ds-work-cover--ribbon-triangle"></div></button></div></div></div><div class="ds-work-card--work-information"><h1 class="ds-work-card--work-title">Morphometry Governs the Dynamics of a Drainage Basin: Analysis and Implications</h1><div class="ds-work-card--work-authors ds-work-card--detail"><a class="ds-work-card--author js-wsj-grid-card-author ds2-5-body-md ds2-5-body-link" data-author-id="4729139" href="https://caluniv.academia.edu/AtrayeeBiswas"><img alt="Profile image of Atrayee Biswas" class="ds-work-card--author-avatar" src="https://0.academia-photos.com/4729139/2000692/2360939/s65_atrayee.biswas.jpg" />Atrayee Biswas</a></div><div class="ds-work-card--detail"><div class="ds-work-card--work-metadata"><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">visibility</span><p class="ds2-5-body-sm" id="work-metadata-view-count">…</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">description</span><p class="ds2-5-body-sm">15 pages</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">link</span><p class="ds2-5-body-sm">1 file</p></div></div><script>(async () => { const workId = 7131407; 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if (!viewCountBody) { throw new Error('Failed to find work views element'); } viewCountBody.textContent = `${commaizedViewCount} views`; } catch (error) { // Remove the whole views element if there was some issue parsing. document.getElementById('work-metadata-view-count')?.parentNode?.remove(); throw new Error(`Failed to parse view count: ${viewCount}`, error); } }; // If the DOM is still loading, wait for it to be ready before updating the view count. if (document.readyState === "loading") { document.addEventListener('DOMContentLoaded', () => { updateViewCount(viewCount); }); // Otherwise, just update it immediately. } else { updateViewCount(viewCount); } })();</script></div><p class="ds-work-card--work-abstract ds-work-card--detail ds2-5-body-md">Mountainous rivers are the most significant source of water supply in the Himalayan provinces of India. The drainage basin dynamics of these rivers are controlled by the tectonomorphic parameters, which include both surface and subsurface characteristics of a basin. To understand the drainage basin dynamics and their usefulness in watershed prioritisation and management in terms of soil erosion studies and groundwater potential assessment and flood hazard risk reduction in mountainous rivers, morphometric analysis of a Himalayan River (Supin River) basin has been taken as a case study. The entire Supin River basin has been subdivided into 27 subwatersheds and 36 morphometric parameters have been calculated under four broad categories: drainage network, basin geometry, drainage texture, and relief characteristics, each of which is further grouped into five different clusters having similar morphometric properties. The various morphometric parameters have been correlated with each other to understand their underlying relationship and control over the basin hydrogeomorphology. The result thus generated provides adequate knowledge base required for decision making during strategic planning and delineation of prioritised hazard management zones in mountainous terrains.</p><div class="ds-work-card--button-container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{"location":"continue-reading-button--work-card","attachmentId":40850664,"attachmentType":"pdf","workUrl":"https://www.academia.edu/7131407/Morphometry_Governs_the_Dynamics_of_a_Drainage_Basin_Analysis_and_Implications"}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{"location":"download-pdf-button--work-card","attachmentId":40850664,"attachmentType":"pdf","workUrl":"https://www.academia.edu/7131407/Morphometry_Governs_the_Dynamics_of_a_Drainage_Basin_Analysis_and_Implications"}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div><div class="ds-signup-banner-trigger-container"><div class="ds-signup-banner-trigger ds-signup-banner-trigger-control"></div></div><div class="ds-signup-banner ds-signup-banner-control"><div id="ds-signup-banner-close-button"><button class="ds2-5-button ds2-5-button--secondary ds2-5-button--inverse"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">close</span></button></div><div class="ds-signup-banner-ctas"><img src="//a.academia-assets.com/images/academia-logo-capital-white.svg" /><h4 class="ds2-5-heading-serif-sm">Sign up for access to the world's latest research</h4><button class="ds2-5-button ds2-5-button--inverse ds2-5-button--full-width js-swp-download-button" data-signup-modal="{"location":"signup-banner"}">Sign up for free<span class="material-symbols-outlined" style="font-size: 20px" translate="no">arrow_forward</span></button></div><div class="ds-signup-banner-divider"></div><div class="ds-signup-banner-reasons"><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Get notified about relevant papers</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Save papers to use in your research</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Join the discussion with peers</span></div><div class="ds-signup-banner-reasons-item"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">check</span><span>Track your impact</span></div></div></div><script>(() => { // Set up signup banner show/hide behavior: // 1. 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C. Road, Kolkata- 700 019 2Department of Remote Sensing and GIS, Vidyasagar University, Medinipur- 721 102 3Department of Geology, University of Calcutta, 35, B. C. Road, Kolkata- 700 019 * adp.biswas@gmail.com Abstract Mountainous rivers are the most significant source of water supply in the Himalayan provinces of India. The drainage basin dynamics of these rivers are controlled by the tectonomorphic parameters, which include both surface and sub-surface characteristics of a basin. To understand the drainage basin dynamics and their usefulness in watershed prioritisation and management in terms of soil erosion studies, groundwater potential assessment and flood hazard risk reduction in mountainous rivers, morphometric analysis of a Himalayan River (Supin River) basin has been taken as a case study. The entire Supin River basin has been subdivided into 27 sub-watersheds and 36 morphometric parameters have been calculated under four broad categories: drainage network, basin geometry, drainage texture and relief characteristics, each of which is further grouped into five different clusters having similar morphometric properties. The various morphometric parameters have been correlated with each other to understand their underlying relationship and control over the basin hydro-geomorphology. The result thus generated, provides adequate knowledge-base required for decision making during strategic planning and delineation of prioritized hazard management zones in mountainous terrains.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometry governs the dynamics of a drainage basin: analysis \u0026 implications","attachmentId":33652475,"attachmentType":"pdf","work_url":"https://www.academia.edu/6519145/Morphometry_governs_the_dynamics_of_a_drainage_basin_analysis_and_implications","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/6519145/Morphometry_governs_the_dynamics_of_a_drainage_basin_analysis_and_implications"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="1" data-entity-id="70815861" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/70815861/Morphometric_Analysis_of_a_Drainage_Basin_A_Study_of_Ghatganga_River_Bajhang_District_Nepal">Morphometric Analysis of a Drainage Basin: A Study of Ghatganga River, Bajhang District, Nepal</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="145920295" href="https://ku-np.academia.edu/sandeepadhikari">sandeep adhikari</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2020</p><p class="ds-related-work--abstract ds2-5-body-sm">This study attempts to study the morphometric characteristics of Ghatganga basin by using Geographical information system (GIS). This analysis has shown that the relation of stream order (U) and stream number (Nu)which gives negative linear pattern that order increases with a decreasing number of stream segment of a particular order. Different morphometric parameters such as stream length (Lu), bifurcation ratio (Rb), drainage density (D), stream frequency (Fs), texture ratio (T), elongation ratio (Re), circularity ratio (Rc), form factor ratio (Rf), relief ratio (Rh) and river profile have revealed the basin has dendritic pattern of drainage, indicating high relief and steep ground slope with less elongated young and mature landforms in which geological structures don’t have a dominant influence on basin.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometric Analysis of a Drainage Basin: A Study of Ghatganga River, Bajhang District, Nepal","attachmentId":80405525,"attachmentType":"pdf","work_url":"https://www.academia.edu/70815861/Morphometric_Analysis_of_a_Drainage_Basin_A_Study_of_Ghatganga_River_Bajhang_District_Nepal","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/70815861/Morphometric_Analysis_of_a_Drainage_Basin_A_Study_of_Ghatganga_River_Bajhang_District_Nepal"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="2" data-entity-id="38137584" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/38137584/STUDY_OF_DRAINAGE_SYSTEM_AND_ITS_HYDROLOGICAL_IMPLICATIONS_USING_GEO_SPATIAL_TECHNIQUES_A_MORPHOMETRIC_ANALYSIS_IN_MOHAL_KHAD_WATERSHED_OF_KULLU_DISTRICT_HIMACHAL_PRADESH_INDIA">STUDY OF DRAINAGE SYSTEM AND ITS HYDROLOGICAL IMPLICATIONS USING GEO-SPATIAL TECHNIQUES: A MORPHOMETRIC ANALYSIS IN MOHAL KHAD WATERSHED OF KULLU DISTRICT, HIMACHAL PRADESH, INDIA.</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="39246530" href="https://independent.academia.edu/JournalIJAR">IJAR Indexing</a></div><p class="ds-related-work--metadata ds2-5-body-xs">International Journal of Advanced Research (IJAR), 2018</p><p class="ds-related-work--abstract ds2-5-body-sm">Understanding the behavior of surface drainage network is one of the important prerequisite condition for effective planning and management of water resources within the watershed. Morphometric analysis of a watershed is a crucial step in watershed development and management to understand and interpret the dynamics of drainage system of the watershed and is useful for interpretation of silent features of drainage network. A morphometric analysis was carried out to evaluate the drainage characteristics of Mohalkhad watershed which covers an area about 54 km2 in Kullu district of Himachal Pradesh in Indian Himalayan Region (IHR). Geospatial technique/tool such as Remote Sensing (RS) and GIS was used to evaluate the linear, areal and relief aspects of morphometric parameters. RS and GIS technique is very helpful over the conventional methods that are too laborious and cumbersome. To carry out this study, Survey of India (SOI) toposheet of 1:50,000 scale and ASTER DEM (30 m resolution) data were used and analysis was carried out in ArcGIS 10.5 software. Total 21 morphometric parameters of Mohalkhad watershed were evaluated considering the linear, areal and relief aspects. The significance of each morphometric parameter with the hydrological behavior of the watershed is discussed in this study. This exercise provide detailed insight into drainage system of the Mohalkhad watershed, which is useful for the development and management of water conservation measures in the area.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"STUDY OF DRAINAGE SYSTEM AND ITS HYDROLOGICAL IMPLICATIONS USING GEO-SPATIAL TECHNIQUES: A MORPHOMETRIC ANALYSIS IN MOHAL KHAD WATERSHED OF KULLU DISTRICT, HIMACHAL PRADESH, INDIA.","attachmentId":58168706,"attachmentType":"pdf","work_url":"https://www.academia.edu/38137584/STUDY_OF_DRAINAGE_SYSTEM_AND_ITS_HYDROLOGICAL_IMPLICATIONS_USING_GEO_SPATIAL_TECHNIQUES_A_MORPHOMETRIC_ANALYSIS_IN_MOHAL_KHAD_WATERSHED_OF_KULLU_DISTRICT_HIMACHAL_PRADESH_INDIA","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/38137584/STUDY_OF_DRAINAGE_SYSTEM_AND_ITS_HYDROLOGICAL_IMPLICATIONS_USING_GEO_SPATIAL_TECHNIQUES_A_MORPHOMETRIC_ANALYSIS_IN_MOHAL_KHAD_WATERSHED_OF_KULLU_DISTRICT_HIMACHAL_PRADESH_INDIA"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="3" data-entity-id="63610730" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/63610730/Application_of_Morphometric_Analysis_for_Geo_Hydrological_Studies_Using_Geo_Spatial_Technology_A_Case_Study_of_Vishav_Drainage_Basin">Application of Morphometric Analysis for Geo-Hydrological Studies Using Geo-Spatial Technology –A Case Study of Vishav Drainage Basin</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="206746583" href="https://independent.academia.edu/AADILHAMID5">AADIL HAMID</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of Waste Water Treatment & Analysis, 2013</p><p class="ds-related-work--abstract ds2-5-body-sm">The morphometric analysis of the drainage basin and channel network play an important role in understanding the geo-hydrological behavior of drainage basin and expresses the prevailing climate, geology, geomorphology, structural antecedents of the catchment. Morphometric analysis of a drainage basin expresses fully the state of dynamic balance that has been attained due to dealings between matter and energy. In the present study, morphometric analysis has been carried out using Geographical Information System (GIS) techniques to assess the geo-hydrological characteristics of Vishav drainage basin and an attempt has been made to identify the ground water potential zones through geo-morphometric specs. The morphometric parameters are discussed about linear, areal and relief aspects. The basin is characterized by dendritic to sub-dendritic drainage pattern. The development of stream segments in the basin area is affected by rainfall, groundwater discharge and snow melt over. The analysis has revealed that the total number and length of stream segments is maximum in first order streams and decreases as the stream order increases. The bifurcation ratio (R b) between different successive orders varies revealing the geostructural control. The shape parameters (R c =0.52, R e =0.15 and R f =0.22) indicate the elongated shape of the basin and in association with some areal (D d , D t etc.) and relief (H, S b , etc.) parameters show that it has low discharge of runoff, generally permeable subsoil condition, moderate to high infiltration capacity and good groundwater resource and a flatter peak of flow of longer duration that is easier to manage that of the circular basins. The study reveals that morphometric analysis based on GIS technique is a competent tool for geo-hydrological studies. These studies are very useful for identifying and planning the ground water potential zones and watershed management (including the whole gamut of natural resources connected with the basin).</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Application of Morphometric Analysis for Geo-Hydrological Studies Using Geo-Spatial Technology –A Case Study of Vishav Drainage Basin","attachmentId":75983306,"attachmentType":"pdf","work_url":"https://www.academia.edu/63610730/Application_of_Morphometric_Analysis_for_Geo_Hydrological_Studies_Using_Geo_Spatial_Technology_A_Case_Study_of_Vishav_Drainage_Basin","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/63610730/Application_of_Morphometric_Analysis_for_Geo_Hydrological_Studies_Using_Geo_Spatial_Technology_A_Case_Study_of_Vishav_Drainage_Basin"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="4" data-entity-id="124763828" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/124763828/Morphometric_Analysis_of_Panzara_River_Basin_Watershed_Maharashtra_India_Using_Geospatial_Approach">Morphometric Analysis of Panzara River Basin Watershed, Maharashtra, India Using Geospatial Approach</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="80025315" href="https://hnbgarhwal.academia.edu/FirozKhan">Firoz Khan</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2024</p><p class="ds-related-work--abstract ds2-5-body-sm">This work aims to deal with the morphometric analysis of the Panzara River Basin (PRB) watershed, a tributary of the Tapi River in Maharashtra, India. In this study, Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Digital Elevation Model (DEM) and Survey of India (SOI) toposheets have been used along with various parameters like linear, areal, and relief aspects in Geographical Information System (GIS) environment. Out of total 293 number of streams in the watershed, 226, 54, 12, and 1 are of first, second, third and fourth orders respectively. PRB watershed is of 4th order and less elongated in shape, having lower peak flows of longer duration with dendritic pattern and having coarse drainage texture. The bifurcation ratio lies between 6 and 7, indicating that geological structure doesn't have more influence on drainage patterns. The area forms a rugged topography having an elevation range from 123 to 1199 m above Mean Sea Level (MSL). Variables like Stream Frequency and Drainage Density shows impermeable surface of PRB watershed which causes higher water discharge volume and speed in the basin so that the probability is maximum for frequent floods. The results indicates that PRB is having high slope in SW part as compare to NE part and having very low gradient ratio. These variables also shows a temporal variation in the water flowing speed in the stream when the flood reaches its peak. The outcomes of this work can suggest and recommend a better mechanism for proper watershed management in the PRB.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometric Analysis of Panzara River Basin Watershed, Maharashtra, India Using Geospatial Approach","attachmentId":118928598,"attachmentType":"pdf","work_url":"https://www.academia.edu/124763828/Morphometric_Analysis_of_Panzara_River_Basin_Watershed_Maharashtra_India_Using_Geospatial_Approach","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/124763828/Morphometric_Analysis_of_Panzara_River_Basin_Watershed_Maharashtra_India_Using_Geospatial_Approach"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="5" data-entity-id="1234834" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/1234834/Quantitative_Geomorphological_Analysis_of_a_Watershed_of_Ravi_River_Basin_H_P_India">Quantitative Geomorphological Analysis of a Watershed of Ravi River Basin, H.P. India</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="697063" href="https://dhsgsu.academia.edu/DrKuldeepPareta">Dr Kuldeep Pareta</a></div><p class="ds-related-work--abstract ds2-5-body-sm">In the present paper, an attempt has been made to study the quantitative geomorphological analysis of a watershed of Ravi river basin in Himachal Pradesh, India. Authors have evaluated the morphometric characteristics on the basis of Survey of India toposheets at 1:50,000 scale, and CartoSAT-1 DEM data with 2.5m spatial resolutions. For this detailed study, CartoSAT-1 based DEM, and GIS were used in evaluation of linear, areal and relief aspects of morphometric parameters. Watershed boundary, flow accumulation, flow direction, flow length, stream ordering have been prepared using ArcHydro Tool; and contour, slope-aspect, hillshade have been prepared using Surface Tool in ArcGIS-10 software, and DEM. Authors have computed more than 53 morphometric parameter of all aspects. Based on all morphometric parameters analysis; that the erosional development of the area by the streams has progressed well beyond maturity and that lithology has had an influence in the drainage development. This study is very useful for planning rainwater harvesting and watershed management.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Quantitative Geomorphological Analysis of a Watershed of Ravi River Basin, H.P. India","attachmentId":19122395,"attachmentType":"pdf","work_url":"https://www.academia.edu/1234834/Quantitative_Geomorphological_Analysis_of_a_Watershed_of_Ravi_River_Basin_H_P_India","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/1234834/Quantitative_Geomorphological_Analysis_of_a_Watershed_of_Ravi_River_Basin_H_P_India"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="6" data-entity-id="4740207" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/4740207/Morphometrical_analysis_of_two_tropical_mountain_river_basins_of_contrasting_environmental_settings_the_southern_Western_Ghats_India">Morphometrical analysis of two tropical mountain river basins of contrasting environmental settings, the southern Western Ghats, India</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="97663" href="https://iim.academia.edu/JobinThomas">Jobin Thomas</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Environmental Earth Sciences, 2012</p><p class="ds-related-work--abstract ds2-5-body-sm">The morphometric analysis of river basins represents a simple procedure to describe hydrologic and geomorphic processes operating on a basin scale. A morphometric analysis was carried out to evaluate the drainage characteristics of two adjoining, mountain river basins of the southern Western Ghats, India, Muthirapuzha River Basin (MRB) in the western slopes and Pambar River Basin (PRB) in the eastern slopes. The basins, forming a part of the Proterozoic, high-grade, Southern Granulite Terrain of the Peninsular India, are carved out of a terrain dominantly made of granite- and hornblende-biotite gneisses. The Western Ghats, forming the basin divide, significantly influences the regional climate (i.e., humid climate in MRB, while semi-arid in PRB). The Survey of India topographic maps (1:50,000) and Shuttle Radar Topographic Mission digital elevation data were used as the base for delineation and analysis. Both river basins are of 6th order and comparable in basin geometry. The drainage patterns and linear alignment of the drainage networks suggest the influence of structural elements. The Rb of either basins failed to highlight the structural controls on drainage organization, which might be a result of the elongated basin shape. The irregular trends in Rb between various stream orders suggest the influence of geology and relief on drainage branching. The Dd values designate the basins as moderate- to well-drained with lower infiltration rates. The overall increasing trend of Rl between successive stream orders suggests a geomorphic maturity of either basins and confirmed by the characteristic I hyp values. The Re values imply an elongate shape for both MRB and PRB and subsequently lower vulnerability to flash floods and hence, easier flood management. The relatively higher Rr of PRB is an indicative of comparatively steeply sloping terrain and consequently higher intensity of erosion processes. Further, the derivatives of digital elevation data (slope, aspect, topographic wetness index, and stream power index), showing significant differences between MRB and PRB, are useful in soil conservation plans. The study highlighted the variation in morphometric parameters with respect to the dissimilarities in topography and climate.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometrical analysis of two tropical mountain river basins of contrasting environmental settings, the southern Western Ghats, India","attachmentId":36895213,"attachmentType":"pdf","work_url":"https://www.academia.edu/4740207/Morphometrical_analysis_of_two_tropical_mountain_river_basins_of_contrasting_environmental_settings_the_southern_Western_Ghats_India","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/4740207/Morphometrical_analysis_of_two_tropical_mountain_river_basins_of_contrasting_environmental_settings_the_southern_Western_Ghats_India"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="7" data-entity-id="33979582" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/33979582/GIS_based_morphometric_analysis_of_five_major_sub_watersheds_of_Song_River_Dehradun_District_Uttarakhand_with_special_reference_to_landslide_incidences">GIS-based morphometric analysis of five major sub-watersheds of Song River, Dehradun District, Uttarakhand with special reference to landslide incidences</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="54421009" href="https://independent.academia.edu/PankajKumar743">Pankaj Kumar</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of the Indian Society of Remote Sensing, 2009</p><p class="ds-related-work--abstract ds2-5-body-sm">Evaluation of the morphometric parameters requires preparation of drainage map, contour map, ordering of the various streams and measurements of catchment area, perimeter, relative relief, relief ratio, length of drainage channels, drainage density, drainage frequency, bifurcation ratio, texture ratio, circulatory ratio and constant channel maintenance, which help to understand the nature of the drainage basin. The present study involves the Geographic Information System (GIS) analysis techniques to evaluate and compare linear, relief and aerial morphometry of the five subwatersheds of Song River (tributary of the Ganga River) with special reference to landslide incidences, for future development and planning of the watershed. Jakhan Rao, Song River, Bandal Nadi, Baldi Nadi and Suswa Nadi are the five major subwatersheds of the Song River basin. All the subwatersheds are basically of 5 th to 6 th order. Drainage patterns are mainly dendritic to sub dendritic. The drainage pattern of the Song River basin is mainly structurally controlled and the area is characterized by high to moderate relief. The asymmetric factor indicates that the tectonic rotation of the four subwatersheds is upward on the right side of the drainage basin and only one sub-watershed is downward. The numbers of the landslide incidences are also more in the upward side, than the downward side of the Song River basin.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"GIS-based morphometric analysis of five major sub-watersheds of Song River, Dehradun District, Uttarakhand with special reference to landslide incidences","attachmentId":53932409,"attachmentType":"pdf","work_url":"https://www.academia.edu/33979582/GIS_based_morphometric_analysis_of_five_major_sub_watersheds_of_Song_River_Dehradun_District_Uttarakhand_with_special_reference_to_landslide_incidences","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/33979582/GIS_based_morphometric_analysis_of_five_major_sub_watersheds_of_Song_River_Dehradun_District_Uttarakhand_with_special_reference_to_landslide_incidences"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="8" data-entity-id="27947537" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/27947537/Drainage_Morphometric_Analysis_of_Bhera_River_Watershed_Ranchi_and_Ramgarh_Districts_Jharkhand_India">Drainage Morphometric Analysis of Bhera River Watershed, Ranchi and Ramgarh Districts, Jharkhand, India</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="51447699" href="https://independent.academia.edu/CoSEP">Co. SEP</a></div><p class="ds-related-work--abstract ds2-5-body-sm">The quantitative analysis of morphometric parameters is found to be of immense significance in river basin evaluation. Morphometric analysis of a watershed provides a quantitative description of the drainage system. This study was undertaken to determine the drainage characteristics of Bhera river watershed (2A2H1) which is a tributary of Damodar River with an area of 268 km 2. Geographical Information System (GIS) techniques are nowadays used for measuring various morphometric parameters of the drainage basins and watersheds, as they have emerged as a powerful tool for the manipulation and analysis of spatial information. In the present study stream number, order, frequency, density and bifurcation ratio are derived and arranged on the basis of areal and linear properties of drainage channels using GIS. Morphometric analysis has revealed that the watershed is a 5th order drainage basin. The low order streams dominate the watershed than higher orders. This phenomenon causes less time availability for the infiltration of rain water in the upper catchment areas. The calculated value of bifurcation ratio, drainage texture and drainage density in the watershed reveals that the watershed is occupied with hard rocks. The watershed indicates elongated basin as per the value of circulatory ratio. The length of overland flow value for the watershed shows that the rainwater travels a relatively shorter distance before getting concentrated to channels.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Drainage Morphometric Analysis of Bhera River Watershed, Ranchi and Ramgarh Districts, Jharkhand, India","attachmentId":48243335,"attachmentType":"pdf","work_url":"https://www.academia.edu/27947537/Drainage_Morphometric_Analysis_of_Bhera_River_Watershed_Ranchi_and_Ramgarh_Districts_Jharkhand_India","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/27947537/Drainage_Morphometric_Analysis_of_Bhera_River_Watershed_Ranchi_and_Ramgarh_Districts_Jharkhand_India"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="9" data-entity-id="33211471" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/33211471/Morphometric_Analysis_of_Jiya_Dhol_River_Basin">Morphometric Analysis of Jiya Dhol River Basin</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="15485433" href="https://bhu-in.academia.edu/LunamoniDas">Lunamoni Das</a></div><p class="ds-related-work--abstract ds2-5-body-sm">Basin morphometry is an important means of understanding a drainage basin using mathematically derived parameters. In the present study basin morphometry has been analyzed under three broad aspects and they are the linear, areal and relief aspects. Within these aspects there are many parameters which are being determined by using mathematical formula on data derived from Toposheets of the study area. It is covering an area of 1094.93 sq. km. The drainage pattern of the upper section of the basin is trellis pattern and the lower section is anabranching. Floods are common phenomena of the lower section of this basin. This paper explains the role of basin morphometry specially the linear and relief aspect in providing condition for occurrence of flash floods in the lower section of Jiya Dhol River basin.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometric Analysis of Jiya Dhol River Basin","attachmentId":53289960,"attachmentType":"pdf","work_url":"https://www.academia.edu/33211471/Morphometric_Analysis_of_Jiya_Dhol_River_Basin","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/33211471/Morphometric_Analysis_of_Jiya_Dhol_River_Basin"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div></div></div><div class="ds-sticky-ctas--wrapper js-loswp-sticky-ctas hidden"><div class="ds-sticky-ctas--grid-container"><div class="ds-sticky-ctas--container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{"location":"continue-reading-button--sticky-ctas","attachmentId":40850664,"attachmentType":"pdf","workUrl":null}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{"location":"download-pdf-button--sticky-ctas","attachmentId":40850664,"attachmentType":"pdf","workUrl":null}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div></div></div><div class="ds-below-fold--grid-container"><div class="ds-work--container js-loswp-embedded-document"><div class="attachment_preview" data-attachment="Attachment_40850664" style="display: none"><div class="js-scribd-document-container"><div class="scribd--document-loading js-scribd-document-loader" style="display: block;"><img alt="Loading..." src="//a.academia-assets.com/images/loaders/paper-load.gif" /><p>Loading Preview</p></div></div><div style="text-align: center;"><div class="scribd--no-preview-alert js-preview-unavailable"><p>Sorry, preview is currently unavailable. You can download the paper by clicking the button above.</p></div></div></div></div><div class="ds-sidebar--container js-work-sidebar"><div class="ds-related-content--container"><h2 class="ds-related-content--heading">Related papers</h2><div class="ds-related-work--container js-related-work-sidebar-card" data-collection-position="0" data-entity-id="56096391" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/56096391/Geospatial_Approach_for_Quantitative_Drainage_Morphometric_Analysis_of_Varuna_River_Basin_India">Geospatial Approach for Quantitative Drainage Morphometric Analysis of Varuna River Basin, India</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="78452727" href="https://independent.academia.edu/BHARTENDUSAJAN">BHARTENDU SAJAN</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of 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Environ 2020;2(2):131-135., 2020</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Study of linear aspects of morphometric parameters in parts of TAPI river basin, Madhya Pradesh, India using remote sensing and GIS perspective","attachmentId":65504498,"attachmentType":"pdf","work_url":"https://www.academia.edu/44969530/Study_of_linear_aspects_of_morphometric_parameters_in_parts_of_TAPI_river_basin_Madhya_Pradesh_India_using_remote_sensing_and_GIS_perspective","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-related-work-grid-card-view-pdf" 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href="https://independent.academia.edu/VarunMishra29">Varun Mishra</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Applied Water Science, 2014</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"A GIS-based approach in drainage morphometric analysis of Kanhar River Basin, India","attachmentId":54154123,"attachmentType":"pdf","work_url":"https://www.academia.edu/34240305/A_GIS_based_approach_in_drainage_morphometric_analysis_of_Kanhar_River_Basin_India","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-related-work-grid-card-view-pdf" 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href="https://www.academia.edu/87070232/Evaluating_Morphometric_Parameters_of_Haro_River_Drainage_Basin_in_Northern_Pakistan">Evaluating Morphometric Parameters of Haro River Drainage Basin in Northern Pakistan</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="15135944" href="https://punjablahorepakistan.academia.edu/SanaullahSaani">Muhammad Sanaullah</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Polish Journal of Environmental Studies, 2018</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Evaluating Morphometric Parameters of Haro River Drainage Basin in Northern 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