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The stream orders are classified up to seventh orders in the Kanhar basin.
Each distribution of the terrestrial runoff was calculated by multiplying the runoffs by the stream orders at each grid, normalized to the maximum orders in each watershed.
The stream order is the first step in drainage basin, which is based on the hierarchic ranking of streams and determines the stream orders.
The stream orders were extracted from Cartosat-I DEM (10 m) and updated from SOI toposheet of 1 50,000 following a system introduced by Horton (1945) but later modified by Strahler (1952).
Channel frequency density serves as a tool in establishing the erosional processes operating over an area; to be more specific, the same in relation to the stream orders and their characteristics provides data which can throw light even on the sequences of relief developments and the degree of ruggedness in the area (Singh 1980).
Similar(55)
The stream order of data stream (s_{mathcal {A}}) is (|mathcal {A}|).
The stream ordering of the watershed suggested that the Makhawan watershed is of fifth order.
In general, it is observed that the mean stream length increases with the stream order.
The stream order defined in Section 4.2 is applied to the generalized RS.
It is the number of stream segments of various orders and is inversely proportional to the stream order.
The total length of stream segment is higher in first order streams and decreases as the stream order increases, pursuing the Horton's (1945) law of stream length.
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