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A test of the statistical theory of meander formation

A test of the statistical theory of meander formation The statistical theory of meander formation ascribes the meandering of stream channels to the hypothesis that a river has a Gaussian probability to deviate by an angle dΦ in progressing an elemental distance ds along its course. This paper aims at checking this hypothesis. Taking three cases, the Salt Fork Vermilion River in Illinois, the Assiniboine River in Canada, and, as an interesting comparison, a ‘river’ (Hadley Rill) on the Moon, it was indeed possible to show that the probability in question is Gaussian, using pertinent statistical tests. Our study can therefore be said to confirm to this extent the probabilistic view of meander development. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Water Resources Research Wiley

A test of the statistical theory of meander formation

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References (7)

Publisher
Wiley
Copyright
Copyright © 1968 by the American Geophysical Union.
ISSN
0043-1397
eISSN
1944-7973
DOI
10.1029/WR004i002p00317
Publisher site
See Article on Publisher Site

Abstract

The statistical theory of meander formation ascribes the meandering of stream channels to the hypothesis that a river has a Gaussian probability to deviate by an angle dΦ in progressing an elemental distance ds along its course. This paper aims at checking this hypothesis. Taking three cases, the Salt Fork Vermilion River in Illinois, the Assiniboine River in Canada, and, as an interesting comparison, a ‘river’ (Hadley Rill) on the Moon, it was indeed possible to show that the probability in question is Gaussian, using pertinent statistical tests. Our study can therefore be said to confirm to this extent the probabilistic view of meander development.

Journal

Water Resources ResearchWiley

Published: Apr 1, 1968

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