2023
DOI: 10.3390/su16010023
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Morpho-Hydrological Analysis and Preliminary Flash Flood Hazard Mapping of Neom City, Northwestern Saudi Arabia, Using Geospatial Techniques

Bashar Bashir,
Abdullah Alsalman

Abstract: Neom city is a unique cross-border city connecting Saudi Arabia, Jordan, and Egypt. Although Neom city is of great and critical importance for Saudi Arabia, few hydrological, natural hazard, and geomorphological studies have been undertaken on this region. This work aims to investigate the hydro-geomorphological characteristics and assess the flash flood hazards in Neom city by investigating several valuable morphometric parameters. The Shutter Radar Topography Mission (SRTM) digital elevation model and hydrol… Show more

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Cited by 9 publications
(1 citation statement)
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“…When rivers and streams flow across rocks and soils of varying strengths, erosional processes adjust to the terrain, resulting in topographic evolution [19]. Several studies have successfully used this useful measure to examine various topographic stream gradients along channels and rivers in different basins to determine the relationship between the erosional strength of rocks and relative tectonic activity [5,18,27,28]. The SL index can be calculated as follows: SL = (∆H/∆L) × L where ∆H/∆L provides signals about the stream slope of the basin reach of the mean basin, and the symbol L represents the length from the reach midpoint to the basin divide.…”
Section: Stream Length Gradient (Sl)mentioning
confidence: 99%
“…When rivers and streams flow across rocks and soils of varying strengths, erosional processes adjust to the terrain, resulting in topographic evolution [19]. Several studies have successfully used this useful measure to examine various topographic stream gradients along channels and rivers in different basins to determine the relationship between the erosional strength of rocks and relative tectonic activity [5,18,27,28]. The SL index can be calculated as follows: SL = (∆H/∆L) × L where ∆H/∆L provides signals about the stream slope of the basin reach of the mean basin, and the symbol L represents the length from the reach midpoint to the basin divide.…”
Section: Stream Length Gradient (Sl)mentioning
confidence: 99%