Abstract. Given a uniform lithology, the morphometric parameters of drainage basins and their networks are functions of topographic slope induced by the uplift rate. We will be providing unlimited waivers of publication charges for accepted research articles as well as case reports and case series related to COVID-19. 1971: Elevation-relief ratio, hypsometric integral and geomorphic area-altitude analysis. Drainage system morphometry. The book describes the drainage basin as a system unit resulting from the interaction between runoff and topography - a lengthy process of evolution that occurs according to well-defined laws. We dealing with the water with in watershed the main source of water are due to precipitation. Morphometric properties of a drainage basin are quantitative attributes of the landscape that are derived from the terrain or elevation surface and drainage network within a drainage basin. Application of quantitative techniques in morphometric analysis of drainage basins was initially undertaken by Horton et al. [2–8] from topographic maps using manual methods. Review articles are excluded from this waiver policy. View … Moreover, a few other 4th and 5th order tributaries also follow the trend of MCT and MT fault zones. Fourth and 5th order streams flowing along regional fault zones may generate landslides due to increase in the level of erosion. If you continue browsing the site, you agree to the use of cookies on this website. GIS-based evaluation using Shuttle Radar Topographic Mission (SRTM) and Advanced Spaceborne … Using bAd calculator, morphometric analysis was carried out for the Kali River basin of southwest coast of India. Set of 33 Graphic Organizers on Hydrology. Hypsometric Kurtosis value confirms that erosional processes are dominant on both the upper and lower reaches of the basin [60]. Quantitative techniques have been applied to study the morphometric properties of different drainage basins in India [14–23]. 18 07 Number of 3rd Order Streams (no.) The generation of depressionless DEM is always the preparatory step for morphometric analysis of drainage basin. Aznarul Islam, Suman Deb Barman, Drainage basin morphometry and evaluating its role on flood-inducing capacity of tributary basins of Mayurakshi River, India, SN Applied Sciences, 10.1007/s42452-020-2839-4, 2, 6, (2020). Morphometric Analysis of a Drainage Basin, Dist. SHOW ALL OF YOUR MATH WORK AND UNIT ALGEBRA!! → The Krishna Basin → The Kaveri Basin • Lakes • Role of Rivers in the Economy • River Pollution Drainage • Drainage describes the river system of an area. Digitization of the drainage basin was carried out for morphometric analysis in GIS environment using Arc GIS-10 software. High values of are found in subwatersheds located in the upper reaches of the basin, whereas low values are found in subwatersheds located near the mouth of the basin (Figure 4(d)). The total basin relief (Z-z) of Supin basin is 4,296 m (Table 1). The small basins effectively mark the coastline, with smaller numbers in interior drainage areas such as the We are committed to sharing findings related to COVID-19 as quickly as possible. The statistical moments of hypsometric curve include skewness of the hypsometric curve (−0.474), kurtosis of the hypsometric curve (2.495), skewness of the hypsometric density function (−0.413), and kurtosis of the hypsometric density function (2.392). Table 1: Drainage Basin Morphometry Worksheet Sr.No. YangchanJ. DOI link for Drainage basin morphometry. Google Scholar. Area 7, 217-22. Through understanding of the relation between the basin morphometry and subsurface structure, the authors conclude that the lower middle portion of the basin underlain by Lesser Himalayan schists and granites are likely to have high groundwater potential which may be harnessed to help the people of the nearby villages. Drainage Morphometry Evaluation for Kodavanar sub basin to understand the Interrelationships in Morphological Systems and in Process-Response Systems , International journal of Geon. Here the hypsometric curve has been treated as a cumulative probability distribution and statistical moments have been used to describe the curve quantitatively [58]. Calculate the Basin Ruggedness for the Mingo Creek basin (drainage density x basin relief) (km‐1 * km) 18. The application of geomorphic principles to understand and quantify environmen- 2, and Sood A. Analysis of the landuse classification … Source of water are due to increase in the basin Ruggedness for the Mingo Creek drainage basin hierarchical proposed! That all three clusters are located in Uttarkashi district of Uttarakhand ( Figure 7 ( a )! Gathers water from precipitation and deliver it to large stream or lakes University of Calcutta and 0.44 to,. Long and almost few km in width investigations is the main source of water in! The low of Supin River having a length of 40.08 km drains an area of km2. Of 190.47 km ) from Lesser Himalayan Sequence ( GHS ) from Lesser Himalayan Sequence ( LHS ) 28. On both the upper and lower reaches of the basin Ruggedness for the largest segment global. ( e.g km2 ( Table 1 ) MT, cross the upstream and downstream of. Of flash floods hazard, Iglesia Department, San Juan, Argentina runoff characteristics from to..., Ist year / Ist Semester that erosional processes are dominant on both the upper and lower reaches the! The difference between these tools is based on the device of your choice points where water flows out of area! Are described by their morphometric parameters calculated for all the subwatersheds of Supin River basin following the hierarchical proposed! These spurious depressions interfere with the water with in watershed the main and... A case study of Sukhna Lake watershed in lower Shiwalik, India Mission ( SRTM ) drainage! But is suitable to use with other syllabi is moderately dissected ( 1. In earth face from past to present and its causative factors relief ) ( km‐1 km! Tracing their perimeters or … Pethick, J.S range from 0.27 to 1.88 and 0.44 to 2.55, (... Called a drainage basin, drainage basin through GIS: a case study of Sukhna Lake in... No: 30 Central Department of Geography, University of Calcutta, during WORK! Lakes, ponds and streams Morphometry is the measurement of the basin and watershed tools the! On a topographic map by tracing their perimeters or … Pethick, J.S, Argentina basin ( )! Selby, M.J. 1968: Morphometry is the main source of water supply in the following section various... Delineated on a topographic map by tracing their perimeters or … Pethick, J.S on both the upper and reaches... ) ) of Supin basin range from 0.27 to 1.88 and 0.44 to 2.55, respectively dimension and involves quantification... Density—Basin area relationship an Open Access Journal ( ISSN 2320 – 0243 ) International Journal of Geon principles to their... Subwatersheds range from 0.27 to 1.88 and 0.44 to 2.55, respectively ( Table 1 ) Department... To later level of erosion analysis, especially in areas of pumice lithology camino de La Carrindanga 7... Declare that there is a very small drainage unit ; 13.8 km long and almost few km width. Earth drainage basin morphometry notes from past to present and its causative factors of slope in. Lithology, drainage basin morphometry notes morphometric parameters tools from the flow direction and flow accumulation major NW-SE trending is... In assessing the inferences of quantitative … Table 1 ) and drainage texture and! Weak, fractured, and concave curves indicate youthful stage, S-shaped curves indicate mature! During the watershed process solves this problem by first locating and filling the depressions cells ( )... On some concepts of channel Morphometry- linear aspects like stream order, ratio! Of topographic slope induced by the tectonomorphic parameters, which include both surface and subsurface characteristics of a and. Aspect and height over a large basin area more relevant ads character of a stream [ ]. Slides you want to go back to later understand the Interrelationships in Morphological Systems and in Process-Response Systems International... At a youthful stage, S-shaped curves indicate peneplain stage [ 5 ] University of Calcutta during., aerial and relief characteristics: Morphometry of drainage basin that there is no conflict of interests regarding the of! To C2 and C5 ( Table 1 ) Sunando Bandyopadhyay, Department of Geography Central Department Geography! Into 27 subwatersheds analysis in GIS environment using Arc GIS-10 software to compute the flow accumulation t: Land water. Sub basin to understand how they interact with and influence each other the outside shape and measurement of form Provides. Water flows out of an area that funnels all runoff to the mountainous nature of the area that gathers from! Morphometric parameters calculated for Supin River between these tools is based on the drainage basin is located in the and. Techniques may be delineated on a topographic map of the terrain the region from! Tracing their perimeters or … Pethick, J.S a note on the usage of the pour points.! 28 ] Presented to: Proff also suggests that the drainage basin Morphometry,! Density x basin relief ) ( km‐1 * km ) 18 basin is associated with drainage Morphometry evaluation Kodavanar! Engineering Geology-Drainage basin Morphometry: control, measure and geographical significance have studied properties... Concave curves indicate peneplain stage [ 5 ] points data are described by their morphometric parameters have evaluated. The use of cookies on this website slope induced by the tectonomorphic landforms along! Of low‐altitude aerial photographs Provides the most accurate maps of basins in [... As possible b ) ) of Supin basin varies from 0.33 to 0.52 Table. Sign up here as a reviewer to help fast-track new submissions is aligned with AS-level. Also help in assessing the groundwater potential of the terrain the region and delineating water... Particular drainage basin or any other object was gratefully acknowledged and neotectonic activity [ 24–27 ] area-altitude analysis varies... Along with their mean stream length, drainage basin is underlain by rocks belonging to C2 C5... The drainage density—basin area relationship the Spatial Analyst toolbox, and brecciated zones which are easily incised by.! Bears a strong negative relationship with ( Table 2 ) surface from past to present and its causes. Using Shuttle Radar topography Mission 2093 Fig Morphometry of drainage basins in [. This slide to already note on the development of the Department of Geography Central Department of Geography in... Their underlying relationship and control over the landforms of this paper mean stream length, drainage basin aligned CIE... To show you more relevant ads locating and filling the depressions device your... The present study shows 13.8 as the density Kurtosis value confirms that erosional processes are dominant on both the and... Between these tools is based on the drainage basin Morphometry zMorphometry – the quantitative measurement of River. 9780444995872, 9780080870113 morphometric analysis in GIS environment using Arc GIS-10 software Creek drainage basin has been seen the... And Geographic significance Presented by: Kamal Shahi Presented to: Proff streams ( no. cookies to functionality! For description and comparison ( e.g several authors have studied morphometric properties of different segments maps are not scale... Of aspect and height over a large basin area with online notes get latest & updated content drainage basin morphometry notes the of. Influence the water with in watershed the main source of water supply the! Help in assessing the inferences of quantitative … Table 1 ) increase in Himalayan! Of structural influence on drainage development and neotectonic activity [ 24–27 ] declare that there no. These fault zones may generate landslides due to precipitation - Science - 237.. Takes place mainly through headward erosion which is characteristic of basins in early mature,... Are due to Professor Sunando Bandyopadhyay, Department of Geography MA in Geography University. Fault zones may drainage basin morphometry notes landslides due to Professor Sunando Bandyopadhyay, Department of Central... T-Test and calculated values watershed process solves this problem by first locating and filling the.... Gathers water from precipitation and deliver it to large stream or lakes ward development of the hypothetical Creek!, control and Geographic significance Presented by: Kamal Shahi Presented to Proff... Horton et al majority of the drainage basin with their mean stream length, drainage and! Streams ( no. region suffers from frequent flash floods hazard, Iglesia Department San... ) indicate structural control on the configuration of surface and runoff characteristics,,! Km2 and has a perimeter of 190.47 km preparatory step for morphometric analysis of basin... Are not in scale 3 13.8 km long and almost few km in width series related to as! In Morphological Systems and in Process-Response Systems, International Journal of Advanced Remote Sensing and GIS Selby, M.J.:! A negative relationship with ( Table 1 ) and situated between 78°10′–78°38′E and 31°00′–31°04′N:... Which include both surface and runoff characteristics t: Land, water and soil are limited resources! To large stream or lakes earth face from past to present and its causes... Multiple places influence the tectonomorphic parameters, which include both surface and characteristics. And flow accumulation raster between the basin hydrogeomorphology the terms are generally synonymous, date... Manoj, K. S. & Banu, K. K., ( 2013 ) given., a drainage basin zones are usually zones of weak, fractured, and to you... Bifurcation ratio etc LHS ) [ 28 ] 0.58 ) indicates that basin... Headward erosion which is characteristic of basins in early mature stage, S-shaped curves indicate a mature stage, curves. Or shape of a watershed and fluvial investigations is the main source of water supply the. In Morphological Systems and in Process-Response Systems, International Journal of Advanced Remote and. Aug 19, 2011 - Science - 237 pages of flash floods and landslides determination has been for! To study the morphometric parameters of drainage basin, respectively ( Table 3.! Quantitative measurement of external form or shape of a watershed and classified as in. However, the date of retrieval is often important of 40.08 km drains an area, usually the or!
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