Research Article

Morphometric Analysis to Infer Hydrological Behaviour of Lidder Watershed, Western Himalaya, India

Table 5

Showing bifurcation ratios, drainage density, and stream frequency of the subwatersheds.

SubwatershedBifurcation ratio Mean bifurcation ratio Drainage density Stream frequencyDrainage intensity
I/IIII/IIIIII/IVIV/V

WS13.834.003.003.612.115.932.82
WS24.894.502.003.802.435.152.12
WS33.565.074.673.004.082.365.632.39
WS44.086.502.004.192.355.782.46
WS52.384.002.002.792.487.022.83
WS62.465.007.004.822.646.522.47
WS72.068.836.002.004.722.967.042.38
WS82.129.205.002.004.582.987.982.68
WS91.9410.714.205.005.622.697.822.91
WS101.7314.143.502.005.342.496.702.69
WS114.005.002.003.671.864.522.44
WS123.5317.0010.262.958.192.78
WS134.2114.009.113.017.052.34
WS143.336.004.671.764.122.35
WS153.945.673.004.202.215.642.55
WS163.905.004.452.326.152.65
WS173.003.001.183.472.94