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Hydrometric Implications of Morphometry and Geology: A Study of Lower Ramganga Catchment


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1 Department of Geography, Kumaon University Campus, Almora (UP) 263 601, India
     

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Total stream length (ΣL) and relief ratio (Rr) are the most significant morphometric parameters, which have been used to define allometric change of hydrometric parameters i.e. stream discharge (Q) and silt delivery (S) as: Q = a+b (ΣL) and S = a b (Rr). The allometric models are largely controlled by bedrock lithologies. The lower Ramganga catchment in the central. U.P. Himalaya was employed as a natural laboratory for the above investigation.
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  • Hydrometric Implications of Morphometry and Geology: A Study of Lower Ramganga Catchment

Abstract Views: 179  |  PDF Views: 2

Authors

J. S. Jawat
Department of Geography, Kumaon University Campus, Almora (UP) 263 601, India

Abstract


Total stream length (ΣL) and relief ratio (Rr) are the most significant morphometric parameters, which have been used to define allometric change of hydrometric parameters i.e. stream discharge (Q) and silt delivery (S) as: Q = a+b (ΣL) and S = a b (Rr). The allometric models are largely controlled by bedrock lithologies. The lower Ramganga catchment in the central. U.P. Himalaya was employed as a natural laboratory for the above investigation.