Hydrological Analysis of Wadi Arab Valley Dam by Integrate Soil Conservation Service and Geographic Information Systems
			
	
 
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				1
				Faculty of Sciences, Department of Geology, Université Ibn Tofail, Kénitra 14000, Morocco
				 
			 
						
				2
				Department of Geographic Information Systems and Remote Sensing,Faculty of Earth and Environmental Sciences, Al Al-Bayt University, Mafraq, Jordan
				 
			 
										
				
				
		
		 
			
			
		
		
		
		
		
		
	
							
										    		
    			 
    			
    				    					Autor do korespondencji
    					    				    				
    					Majed  Ibrahim   
    					Department of Geographic Information Systems and Remote Sensing,Faculty of Earth and Environmental Sciences, Al Al-Bayt University, Mafraq, Jordan
    				
 
    			
				 
    			 
    		 		
			
																	 
		
	 
		
 
 
Ecol. Eng. Environ. Technol. 2024; 12:165-179
		
 
 
SŁOWA KLUCZOWE
DZIEDZINY
STRESZCZENIE
This study aims to estimate the runoff volume by analyzing satellite data and Digital Elevation Model (DEM) data utilizing a set of software tools such as (ArcHydro Tool, ArcGIS) to excerpt hydrological and morphological characteristics of Wadi Al Arab Dam basin with an area of 266 km² in Jordan. Natural data “soil and land use” were analyzed and defined by the curve number (CN) method with Geographic Information Systems (GIS). The novelty of this study lies in the application of high-resolution DEMs combined with advanced GIS techniques to achieve more precise elevation mapping and hydrological flow assessments, which were previously less accurate in similar studies. Moreover, it highlights runoff concentration time and the minimal dissection of the basin, providing a better understanding of flood potential and geomorphological traits in arid regions. This fills a gap in quantifying basin hydrodynamics compared to previous studies. Results found that the total CN for the basin was 86.5. The drainage density of the basin was found to be 4.39×10⁻⁵ m/m², indicating less impact from erosion factors and less dissection. The concentration time of the basin was approximately 65.69 minutes, increasing the possibility of high flood potential due to the short distance traveled by the runoff. The relief ratio was found to be low at 0.018, indicating minimal dissection and runoff in the basin. We recommended the urgent adoption of high-accuracy digital data sources due to the precision they offer when conducting quantitative measurements.