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Table 1

Methodology adopted for computations of morphometric parameters (modified after Masoud 2016)

ParameterFormulaReference
The basin dimensions category 
 Area (AArcHydro analysis Schumn (1956)  
 Perimeter (PArcHydro analysis Schumn (1956)  
 Length (LbArcHydro analysis Schumn (1956)  
 Width (WArcHydro analysis Schumn (1956)  
The basin shape category 
 Circulation ratio (Cr4πA/P Miller (1953)  
 Elongation ratio (Er1.128 × A0.5/Lb Schumn (1956)  
 Shape factor (SfLb2/A Horton (1932)  
The basin surface category 
 Relief ratio (RrR/Lb Schumn (1956)  
 Relative relief ratio (RVR/P Melton (1957)  
 Ruggedness index (RIR×D Schumn (1956)  
 Hypsometric index (HI(Emean – Emin)/ (Emax – Emin) Pike & Wilson (1971)  
The drainage network category 
 Total stream length (TSLGIS software analysis Horton (1945)  
 Total stream number (TSNGIS software analysis Strahler (1952)  
 Stream order (SrOHierarchial rank Strahler (1964)  
 Texture ratio (TrTSN/P Horton (1945)  
 Drainage density (DTSL/A Horton (1945)  
 Stream frequency (FqTSN/A Horton (1945)  
 Bifurcation ratio (BrNu/Nu+1 Schumn (1956)  
ParameterFormulaReference
The basin dimensions category 
 Area (AArcHydro analysis Schumn (1956)  
 Perimeter (PArcHydro analysis Schumn (1956)  
 Length (LbArcHydro analysis Schumn (1956)  
 Width (WArcHydro analysis Schumn (1956)  
The basin shape category 
 Circulation ratio (Cr4πA/P Miller (1953)  
 Elongation ratio (Er1.128 × A0.5/Lb Schumn (1956)  
 Shape factor (SfLb2/A Horton (1932)  
The basin surface category 
 Relief ratio (RrR/Lb Schumn (1956)  
 Relative relief ratio (RVR/P Melton (1957)  
 Ruggedness index (RIR×D Schumn (1956)  
 Hypsometric index (HI(Emean – Emin)/ (Emax – Emin) Pike & Wilson (1971)  
The drainage network category 
 Total stream length (TSLGIS software analysis Horton (1945)  
 Total stream number (TSNGIS software analysis Strahler (1952)  
 Stream order (SrOHierarchial rank Strahler (1964)  
 Texture ratio (TrTSN/P Horton (1945)  
 Drainage density (DTSL/A Horton (1945)  
 Stream frequency (FqTSN/A Horton (1945)  
 Bifurcation ratio (BrNu/Nu+1 Schumn (1956)  

Note:R is the relief, E is the elevation in km, Nu is the total number of stream segments in order u, and Nu+1 is the total number of segments of the next higher order.

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