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- W2079264185 abstract "A river network model with a variable exponent of drainage basin is presented. The river network model is an extended version of the Scheidegger river model to take into account a flow-dependent meandering. The scaling behaviour of river-size distribution, the scaling of drainage basin and the multifractal structure of flow (channel discharge) distribution are investigated by computer simulation. It is shown that the exponent of drainage basin changes continuously from 1.5 (the value of the Scheidegger river) to 1 (the value of a linear river) with increasing exponent gamma of flow-dependent meandering, and the exponent of cumulative river-size distribution changes from 0.33 to 0.0. It is found that the partition function Z(q) identical to Sigma iIiq of flow distribution scales as Z(q) approximately=Lzeta (q) where Ii is the flow (channel discharge) of water passing over the site i within the river network and the summation ranges over all sites. The multiscaling exponent zeta (q) of flow distribution changes with the exponent gamma of flow-dependent meandering. The dependence of f- alpha spectra on values of gamma are discussed." @default.
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- W2079264185 date "1993-09-07" @default.
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- W2079264185 title "Scaling and multifractality in a river network model with flow-dependent meandering" @default.
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- W2079264185 doi "https://doi.org/10.1088/0305-4470/26/17/032" @default.
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