Abstract
Linear and nonlinear aspects of the development of morphodynamical features of fluvial and coastal environments are reviewed. It is emphasized that, in spite of the as yet incomplete understanding of the mechanics of sediment transport, some essential mechanisms operating in morphodynamics have been recently clarified by employing classical tools of linear and weakly nonlinear stability theory.
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Seminara, G. Stability and Morphodynamics. Meccanica 33, 59–99 (1998). https://doi.org/10.1023/A:1004225516566
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DOI: https://doi.org/10.1023/A:1004225516566