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Wave ‘set-down’ and set-Up

Bowen, A. J., Inman, D. L., Simmons, V. P.·1968·Journal of Geophysical Research

Abstract

‘Set-down’ and set-up, the negative and positive changes in mean water level due to the presence of a train of surface waves, was measured in a wave channel. Well outside the break point the experimental results are in good agreement with the theoretical relationship determined by Longuet-Higgins and Stewart. Near the break point, where the wave height is greater than predicted by first-order wave theory, the measured ‘set-down’ was consistently less than theory would predict from the deep water wave height. Inside the break point the bore height was found to be a linear function of the mean water depth. In this region, the gradient of the set-up, , was related to the beach slope tan β and the mean ratio of wave height to water depth by the equation .

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Metadata

Authors
Bowen, A. J., Inman, D. L., & Simmons, V. P.
Venue
Journal of Geophysical Research
Published
1968-04-15
Volume
73
Issue
8
Pages
2569-2577
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2143407072
Cited by
427
References
0
FWCI
19.40
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Wave ‘set-down’ and set-Up. https://app.cochat.ai/papers/10.1029/jb073i008p02569
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Bowen, A. J., Inman, D. L., & Simmons, V. P. (1968). Wave ‘set-down’ and set-Up. Journal of Geophysical Research. https://doi.org/10.1029/jb073i008p02569

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