Abstract

Larson et al. (1987) proposed a closed-form solution to describe the development of river delta coastlines owing to sediment supply from the river. This solution is for a beach of infinite extent adjacent to the river mouth. However, in reality, the beach length is always finite due to the existence of man-made structures or headlands. It is, therefore, useful to derive a new analytical solution to gain a better understanding of beach behavior under the effect of boundaries.

Highlights

  • Larson et al (1987) proposed a closed-form solution to describe the development of river delta coastlines owing to sediment supply from the river

  • Characteristic differences between the new analytical solution and the solution provided by Larson et al (1987) for the formation of river delta shorelines will be discussed

  • There has not been any analytical solution for the development of a river delta coastline with a finite length, there is a comparable study about the heat conduction in a medium between two insulated boundaries (Myers, 1971)

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Summary

INTRODUCTION

Larson et al (1987) proposed a closed-form solution to describe the development of river delta coastlines owing to sediment supply from the river. This solution is for a beach of infinite extent adjacent to the river mouth. It is, useful to derive a new analytical solution to gain a better understanding of beach behavior under the effect of boundaries

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