River meanders and vorticity theorem

Eos, Earth and Space Science News
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Abstract

The serpentine windings of rivers, which in certain reaches attain a remarkable symmetry and are then called meanders, must represent one aspect of the tendency for establishment of quasi-equilibrium in natural streams. With the increase in knowledge of the interaction of forces operating in rivers, this tendency toward equilibrium has assumed a greater significance.

Suggested Citation

Leopold, L.B., 1953, River meanders and vorticity theorem: Eos, Earth and Space Science News, v. 34, no. 6, p. 955-959, https://doi.org/10.1029/TR034i006p00955.

Publication type Article
Publication Subtype Journal Article
Title River meanders and vorticity theorem
Series title Eos, Earth and Space Science News
DOI 10.1029/TR034i006p00955
Volume 34
Issue 6
Publication Date August 18, 2014
Year Published 1953
Language English
Publisher AGU Publications
Description 5 p.
First page 955
Last page 959
Additional publication details