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Linear aspects include stream number, stream order, stream length, mean stream length, stream length ratio and bifurcation ratio.
The stream length and mean stream length of various orders has been calculated from Horton's law of stream length method.
// loop to find expected stream length at.
Higher stream length ratio indicates high erosion activity.
Stream length Length of stream Horton (1945) 3.
Similarly, the stream length is calculated in GIS platform.
This experiment was conducted for stream length with 1000 points.
Horton's law (1945) of stream length states that mean stream length segments of each of the successive orders of a basin tends to approximate a direct geomorphic series with stream length towards higher order of streams.
The mean stream length is directly related to mean annual runoff; therefore, the highest mean stream length has relatively high mean annual rainfall runoff and relatively low mean annual rainfall runoff in less mean stream length.
Horton's law (1945) of stream length points out that mean stream length segments of each of the successive orders of a basin tends to approximate a direct geometric series with stream length increasing towards higher order of streams.
Stream length ratio RL = Lu/Lu − 1, where, Lu = total stream length of order "u", Lu − 1 = the total stream length of its next lower order Horton (1945) 5.
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