scholarly journals Quantitative Analysis of a River Basin - A GIS-based Approach

2021 ◽  
Vol 12 (3) ◽  
pp. 3429-3436
Author(s):  
Ketan A.Salunke Et.al
Keyword(s):  
River Basin ◽  
Drainage Density ◽  
High Permeability ◽  
Bifurcation Ratio ◽  
Stream Frequency ◽  
Large Databases ◽  
Structural Deformations ◽  
Seventh Order ◽  
Geomorphological Parameters ◽  
The Mean

The river basin plays a fundamental role in planning the management of natural resources. The hydrological behavior of the basin depends on the geomorphological parameters of the hydrographic basin. In the present study, a morphometric analysis was performed to determine the linear, areal and relief parameters of the Panzara River, the main tributary of the Tapi River, using the Geographic Information System tool. The river basin is of seventh order, showing a dendritic pattern of drainage that indicates the homogeneity in the texture of the basin. The drainage density in the area is 2.56 and the mean bifurcation ratio 5.065 indicates the less impact of structural deformations on the basin. The stream frequency of the basin is 3.20 showing low relief and high permeability. The present study reveals that the applications of GIS techniques are reliable, take less time and are competent to manage large databases for management of river basins.

Morphometric and Sinuosity Analysis of Tlawng River Basin: A Geographic Information System Approach

2021 ◽  
Vol 5 (1) ◽  
pp. 22-32
Author(s):  
David Lalramchulloa ◽  
Ch Udaya Bhaskra Rao ◽  
P. Rinawma
Keyword(s):  
River Basin ◽  
Drainage Density ◽  
Alluvial Plain ◽  
Morphometric Parameters ◽  
Positive Relation ◽  
Vegetative Cover ◽  
Bifurcation Ratio ◽  
Sinuosity Index ◽  
Stream Frequency ◽  
And Behavior

Channel plan-form patterns of river Tlawng has been studied which shows that there is variation in the sinuosity index. This variation is a sign of changing characteristics and behavior of the river. The average sinuosity of the river is 1.41. The sinuosity index is higher in the lower course of the river as it flows through alluvial plain. GIS techniques have been used for studying morphometric parameters. There are 6736 streams in the Tlawng river basin which shows that the topography is still undergoing erosion as the number of stream is high (Zaidi, 2011). The river has low bifurcation ratio which indicates less possibilities of flooding. The drainage density indicates the higher permeable subsoil and moderate to thick vegetative cover. The stream frequency value of the Tlawng river basin is 1.30 streams / km2 which shows a positive relation with drainage density.

scholarly journals GIS-Based Approach in Drainage Morphometric Analysis of Bharathapuzha River Basin, India

2019 ◽  
pp. 1-12 ◽  
Author(s):  
M. Dhanusree ◽  
G. Bhaskaran
Keyword(s):  
River Basin ◽  
Morphometric Analysis ◽  
Structural Control ◽  
Resource Planning ◽  
Drainage Density ◽  
Stream Order ◽  
Elongation Ratio ◽  
Stream Length ◽  
Bifurcation Ratio ◽  
Stream Frequency

Aims: The paper aims to study about the river basin morphometry namely the physical, linear and aerial parameters for the basin. Study Design: The Study has been carried out with the help of Geospatial techniques and statistical formulas. Place and Duration of Study: Bharathapuzha river basin, Kerala, India between January 2018 to July 2018. Methodology: The Study of River morphometry of Bharathapuzha River basin has been done with the help of SRTM satellite data. The downloaded data has been analyzed with the help of ARC GIS Software. The morphometric analysis has been carried out by dividing the basin into nine watersheds based on Water shed Atlas of India Prepared by Soil and Land Use board of           India. Relief, Linear and areal parameters of the basin is calculated with the help of statistical formulas. Results: Based on the analysis it is noted that there is not much difference in morphometric values except in some watersheds. Watershed number 5A2B5, 5A2B6 and 5A2B7 has highest drainage density, stream frequency, relief, relief ratio, ruggedness number, stream length ratio and lowest bifurcation ratio. These watersheds are characterized by highest surface runoff and erosion. The values of form factor, circulatory ratio and elongation ratio suggests that most of the watersheds are elongated and has high basin relief. The maximum stream order frequency is observed in case of first order streams and then for second order streams. Hence it is noted that there is decrease in stream frequency as stream order increases. Conclusion: The mean bifurcation ratio of the Bharathapuza basin is 1.52 which indicates the whole basin is less effected by structural control. This present study is valuable for the erosion control, watershed management, land and water resource planning and future prospective related to runoff study.

scholarly journals Inventário de movimentos de massa na bacia hidrográfica do rio Mascarada/RS

2021 ◽  
Vol 43 ◽  
pp. e31
Author(s):  
Gabriel Lopes Cardozo ◽  
Franciele Zanandrea ◽  
Gean Paulo Michel ◽  
Masato Kobiyama
Keyword(s):  
River Basin ◽  
Mass Movement ◽  
Drainage Density ◽  
Mass Movements ◽  
Shape Parameters ◽  
Watershed Dynamics ◽  
Geomorphological Parameters ◽  
Area Of Influence ◽  
The Moment ◽  
Natural Disaster Management

Mass movements inventories play a key role to the understanding of watershed dynamics. The alteration of this dynamics occurs in the moment of failure and after it due the erosion when precipitation hits the uncovered soil at the mass movement scars. Thus, this paper has characterized these mass movements, which are classified as landslides, occurred in Mascarada´s river basin through different geomorphological parameters, as slope and curvature, and comparing shape parameters against different methodologies to determine the evaluation area. The proposed shape parameters Percentage of affected area (PAA), Drainage density of scars (Ddc) and Density of scars (Dcic) were evaluated against total area of Mascarada´s river basin, against two sub-basins and against a proposed “Area of influence”. 407 scars were mapped with an area of 2,2 km², a mean slope of 36,1° and all scars are in convergent areas. The evaluation of shape forms showed that “area of influence” improved the understanding of this mass movements magnitude. Thus, the elaboration of mass movement inventories with reliable methodologies can provide important information for the natural disaster management.

scholarly journals Prioritization of sub-catchments of a river basin using DEM and Fuzzy VIKOR

2018 ◽  
Vol 1 (1) ◽  
pp. 1-11 ◽  
Author(s):  
K. Srinivasa Raju ◽  
D. Nagesh Kumar ◽  
Anmol Jalali
Keyword(s):  
Drainage Density ◽  
Entropy Method ◽  
Membership Functions ◽  
Elongation Ratio ◽  
Bifurcation Ratio ◽  
Individual Values ◽  
Fuzzy Vikor ◽  
Stream Frequency ◽  
Digital Elevation ◽  
Triangular Membership Function

Abstract Fuzzy VIKOR, a decision making technique, is applied to prioritize 224 sub-catchments of Mahanadi Basin, India. Seven geomorphology based criteria viz., drainage density, bifurcation ratio, stream frequency, texture ratio, form factor, elongation ratio and circulatory ratio are estimated from five digital elevation models (DEMs). Triangular membership functions were formulated for each criterion for each sub-catchment which are based on individual values obtained from individual DEM's. Entropy method is employed for estimation of weights of criteria and a similar mechanism is followed while formulating triangular membership function for weights. Eight groups are formulated with a number of sub-catchments in each group as 5, 26, 69, 65, 29, 11, 12, 7 for taking up conservation measures. Effect of varying strategy weight, (ν) on the ranking pattern is also studied and found that ν value effects ranking pattern significantly.

Morphometric Analysis of a Drainage Basin: A Study of Ghatganga River, Bajhang District, Nepal

2020 ◽  
Vol 7 ◽  
pp. 127-144
Author(s):  
Sandeep Adhikari
Keyword(s):  
Drainage Basin ◽  
Drainage Density ◽  
Geographical Information ◽  
Elongation Ratio ◽  
Stream Length ◽  
Bifurcation Ratio ◽  
Linear Pattern ◽  
Stream Frequency ◽  
Dominant Influence ◽  
Relief Ratio

This study attempts to study the morphometric characteristics of the 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 a 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 a 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 the basin.

scholarly journals Flash Flood Risk Estimation of Wadi Qena Watershed, Egypt Using GIS Based Morphometric Analysis

2018 ◽  
pp. 36-45 ◽  
Author(s):  
Wael M. Elsadek ◽  
Mona G. Ibrahim ◽  
Wael E. Mahmod
Keyword(s):  
Flash Flood ◽  
Risk Estimation ◽  
Eastern Desert ◽  
Drainage Density ◽  
Bifurcation Ratio ◽  
Flash Flooding ◽  
Hazard Degree ◽  
Stream Frequency ◽  
Flooding Risk ◽  
The Relationship

Flash flooding is one of the periodic geohazards in the eastern desert of Egypt where many parts of Upper Egypt, Sinai, and Red Sea areas were hit by severe flash floods, for example in 1976, 1982, 1996 and January 2010. The hazard degree for each sub-basin was determined using the approach developed by El-Shamy for assessing susceptibility of sub-basins to flash flooding risk. To identify at-risk sub-basins, two different methods were applied. The first method is based on the relationship between the drainage density and bifurcation ratio, and the second one uses the relationship between drainage frequency and bifurcation ratio. The three morphometric parameters (the bifurcation ratio, drainage density, and stream frequency) were extracted and calculated for each sub-basin of the watershed. Based on the final hazard degree resulting from the two methods, a detailed hazard degree map was extracted for all sub-basins. The results illustrate that there are no sub-basins with low risk of flooding. The sub-basins with the highest hazard degree are concentrated in the middle of the watershed although they have smaller areas compared with the surrounding sub-basins. The sub-basins located at the boundary of the watershed have an intermediate risk of flooding and moderate potential for groundwater recharge. This constructed map can be used as a basic data for assessment of flood mitigation and planning.

scholarly journals GIS & Remote Sensing Based Morphometric Parameters and Topographic Changes of the Lower Orashi River in Niger Delta

2021 ◽  
Vol 5 (1) ◽  
Author(s):  
Desmond Eteh ◽  
Edirin Akpofure ◽  
Solomon Otobo
Keyword(s):  
Remote Sensing ◽  
River Basin ◽  
Drainage Density ◽  
Morphometric Parameters ◽  
Watershed Hydrology ◽  
Drainage Pattern ◽  
Total Size ◽  
Stream Frequency ◽  
Drainage Texture ◽  
Remote Sensing Techniques

In watershed hydrology, the morphometric features of a river basin are vital to examine the lower Orashi River basin morphological and hydrological aspects, as well as its flood potential, based on their morphometric characteristics using remotely sensed SRTM data that was analyzed with ArcGIS software. The areal, linear, and relief aspects of the Orashi River basin were examined as morphometric parameters. The lower Orashi river basin, according to the findings, has a total size of 625.61 km2 and a perimeter of 307.98 km, with a 5th order river network based on Strahler categorization and a dendritic drainage pattern. Because of low drainage density, the drainage texture is very fine, the relief is low, and the slope is very low. Bifurcation ratio, circularity ratio, drainage density aspect ratio, form factor, and stream frequency values indicate that the basin is less elongated and would produce surface runoff for a longer period, while topographic changes show that the river is decreasing with depth in the land area at about the same elevation as a result of sand deposited due to lack of maintenance by dredging, which implies that the basin is morphometrically elevated and sensitive to erosion and flooding. To understand geohydrological features and to plan and manage watersheds, morphometric analysis based on geographic information systems and remote sensing techniques is beneficial.

How landscape and climate affect the spatial variability of the Italian rainfall extremes? Some initial clues based on I2-RED

2021 ◽  
Author(s):  
Paola Mazzoglio ◽  
Ilaria Butera ◽  
Pierluigi Claps
Keyword(s):  
Spatial Variability ◽  
Linear Regression Analysis ◽  
Alpine Region ◽  
Annual Rainfall ◽  
Mean Values ◽  
Rainfall Extremes ◽  
Geomorphological Parameters ◽  
The Mean ◽  
The Relationship ◽  
Italian Territory

<p>The intensity and the spatial distribution of precipitation depths are known to be highly dependent on relief and geomorphological parameters. Complex environments like mountainous regions are prone to intense and frequent precipitation events, especially if located near the coastline. Although the link between the mean annual rainfall and geomorphological parameters has received substantial attention, few literature studies investigate the relationship between the sub-daily maximum annual rainfall depth and geographical or morphological landscape features.<br>In this study, the mean of the rainfall extremes in Italy, recently revised in the so-called I<sup>2</sup>-RED dataset, are investigated in their spatial variability in comparison with some landscape and also some broad climatic characteristics. The database includes all sub-daily rainfall extremes recorded in Italy from 1916 until 2019 and this analysis considers their mean values (from 1 to 24 hours) in stations with at least 10 years of records, involving more than 3700 stations.<br>The geo-morpho-climatic factors considered range from latitude, longitude and minimum distance from the coastline on the geographic side, to elevation, slope, openness and obstruction morphological indices, and also include an often-neglected robust climatological information, as the local mean annual rainfall.<br>Obtained results highlight that the relationship between the annual maximum rainfall depths and the hydro-geomorphological parameters is not univocal over the entire Italian territory and over different time intervals. Considering the whole of Italy, the highest correlation is reached between the mean values of the 24-hours records and the mean annual precipitation (correlation coefficient greater than 0.75). This predominance remains also in sub-areas of the Italian territory (i.e., the Alpine region, the Apennines or the coastal areas) but correlation decreases as the time interval decreases, except for the Alpine region (0.73 for the 1-hour maximum). The other geomorphological parameters seem to act in conjunction, making it difficult to evaluate, with a simple linear regression analysis, their impact. As an example, the absolute value of the correlation coefficient between the elevation and the 1-hour extremes is greater than 0.35 for the Italian and the Alpine regions, while for the 24-hours interval it is greater than 0.35 over the coastal areas.<br>To further investigate the spatial variability of the relationship between rainfall and elevation, a spatial linear regression analysis has been undertaken. Local linear relationships have been fitted in circles centered on any of the 0.5-km size pixels in Italy, with 1 to 30 km radius and at least 5 stations included. Results indicate the need of more comprehensive terrain analysis to better understand the causes of local increasing or decreasing relations, poorly described in the available literature.</p>

scholarly journals Features of the Spring Flood Formation in the Arpa River Basin

2021 ◽  
pp. 126-152
Author(s):  
Keyword(s):  
River Basin ◽  
Weighted Average ◽  
Close Correlation ◽  
Annual Runoff ◽  
Average Height ◽  
Spring Flood ◽  
Correlation Relationship ◽  
Catchment Areas ◽  
The Mean ◽  
Maximum Runoff

The article considers main physical and geographical factors affecting the runoff, spring flood of rivers in the Arpa River basin, and analyzes the regularities of their spacetime distribution. The authors have obtained correlation relationship between the values of the flood runoff layer, the mean module maximum runoff and weighted average height of the catchment area of the Arpa River, between the mean annual maximum runoff module for the period floods and catchment areas of rivers. These dependencies can be used for preliminary estimates of the spring flood runoff of unexplored rivers of the territory under consideration. A close correlation between the values of the annual runoff and the runoff of the spring flood in the section of the Arpa River – Dzhermuk has been also revealed. It can be used for forecasting the annual flow.

scholarly journals Hydrological response of hydrographic sub-basins in the Piracicaba River Basin - Southeast Region of Brazil

2022 ◽  
Vol 34 (1) ◽  
Author(s):  
Ana Claudia Pereira Carvalho ◽  
Reinaldo Lorandi ◽  
José Augusto Di Lollo ◽  
Eduardo Goulart Collares ◽  
Luiz Eduardo Moschini
Keyword(s):  
River Basin ◽  
Drainage Density ◽  
Environmental Data ◽  
Low Flow ◽  
Infiltration Capacity ◽  
Infiltration Process ◽  
Human Needs ◽  
Runoff Potential ◽  
Water Response ◽  
Piracicaba River

Use of water for several human needs, associated with climate change, indicates the need understand the response of watersheds, in order to provide adequate water resources planning and management. This study was carried out in two pairs of hydrographic watersheds, in the Piracicaba River Basin, southeast of Brazil, analyzing water response, integrating in-situ collected precipitation and flow data, natural environment attributes, and anthropic environmental data. To support the analysis, Surface Runoff Potential Charts (SRPC). The evaluation of the physical characteristics of the sub watersheds (SW(A) and SW(B)) shows that these areas present very low to low potential, indicating greater infiltration capacity. The use and coverage of the soil partially justifies the flow changes in pair 1, since SW(A) has a larger extent of agricultural areas that can use irrigation. SW(B), even with a greater variety of crops, has a smaller cultivated area and tends to demand less water. At pair 2, the low runoff potential is mainly due to the predominance of flat relief in the sub-basins. The soils that compose them present a higher fraction of silt and clay, with thicknesses > 5m in SW(C) and varying from 0.5m, reaching depths above 5m in SW(D), however, the physical properties of these soils do not provide a low flow rate, but associated with the low slope of the land, the geological characteristics and low drainage density are configured in regions where the flow flows more slowly, contributing to the evaporation and infiltration process. The use and coverage of the soil also partially justifies the flow oscillations, due to anthropic activities in SW(C) and SW(D), such as irrigation and spraying of citrus, fertirrigation of sugarcane, irrigation of seedling nurseries, directly interfering with the availability of surface water.

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