Authors :
Ibtisam Marei; Bouroj Al-Shabe
Volume/Issue :
Volume 9 - 2024, Issue 10 - October
Google Scholar :
https://tinyurl.com/rjpeesut
Scribd :
https://tinyurl.com/4c8py4jz
DOI :
https://doi.org/10.38124/ijisrt/IJISRT24OCT003
Note : A published paper may take 4-5 working days from the publication date to appear in PlumX Metrics, Semantic Scholar, and ResearchGate.
Abstract :
The study aimed to Analyse the Hydrometric
Characteristics of Wadi Rajil basin and assess the flood
hazards in the basin using Remote Sensing and
Geographic Information Systems Techniques. The study
used Models of Digital Visualizations of the basin and
processed them using ARC GIS 10.5 and ARC HYDRO
TOOLS. The result was that the Hypsometric Coefficient
reached (21.4%) of the valley area that was exposed to
erosion and (78.6%) of it is still waiting for its turn to
erosion, indicating that the valley has reached the stage of
youth. The analysis of Hot Spots in the GIS program
resulted in negative values for internal Drainage Basins
greater than -0.5 extending to the northern and
northwestern parts of the basin. It also showed that the
flow coefficient exceeds the internal Drainage Coefficient
or Leakage. As for the positive values, they are distributed
in the southern and southeastern parts, where the (Hot)
values prevail and where the leakage coefficient exceeds
the Flow Coefficient. We find that the Hot Spots are
concentrated in the southeastern parts, which are mostly
extended. The Rift and thus the most suitable areas for
Groundwater Charging through it.
Keywords :
Morphometric Analysis, Hypsometric Coefficient, Pedestrian, GIS, Drainage Coefficient.
References :
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The study aimed to Analyse the Hydrometric
Characteristics of Wadi Rajil basin and assess the flood
hazards in the basin using Remote Sensing and
Geographic Information Systems Techniques. The study
used Models of Digital Visualizations of the basin and
processed them using ARC GIS 10.5 and ARC HYDRO
TOOLS. The result was that the Hypsometric Coefficient
reached (21.4%) of the valley area that was exposed to
erosion and (78.6%) of it is still waiting for its turn to
erosion, indicating that the valley has reached the stage of
youth. The analysis of Hot Spots in the GIS program
resulted in negative values for internal Drainage Basins
greater than -0.5 extending to the northern and
northwestern parts of the basin. It also showed that the
flow coefficient exceeds the internal Drainage Coefficient
or Leakage. As for the positive values, they are distributed
in the southern and southeastern parts, where the (Hot)
values prevail and where the leakage coefficient exceeds
the Flow Coefficient. We find that the Hot Spots are
concentrated in the southeastern parts, which are mostly
extended. The Rift and thus the most suitable areas for
Groundwater Charging through it.
Keywords :
Morphometric Analysis, Hypsometric Coefficient, Pedestrian, GIS, Drainage Coefficient.