Overtide Generation in Small Inlet-Bay Systems
Publication: Journal of Waterway, Port, Coastal, and Ocean Engineering
Volume 145, Issue 5
Abstract
The generation of shallow water tides (overtides) may influence shoaling processes in shallow embayments and harbors. A simplified, conceptual model is developed to simulate the generation of overtides and tidal asymmetries in small inlet/bay systems. The model’s formulation assumes a weakly nonlinear, pumping-mode response and includes effects of four generating mechanisms: quadratic bottom friction (QB), elevation-effect of friction (EEF), nonlinear continuity (NC), and advective acceleration (AA). QB generates primarily odd harmonics, including a second overtide component (M6) that reduces/distorts peak flood/ebb currents symmetrically. The first overtide component (M4) is generated primarily by NC, EEF, and AA. NC, AA, and QB mechanisms are associated with flood-dominant distortion patterns, whereas the EEF mechanism is associated with a shift toward ebb dominance in the special case in which NC contributions are reduced (e.g., large basin tidal flats) and AA is small. Solutions for the M4 tide indicate phase-locking, and distortion patterns consistent with previous studies. A maximum flood-dominant response can occur when the ocean forcing frequency is half the Helmholtz frequency, which is a condition that may cause flood shoals to develop.
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Acknowledgments
The authors would like to acknowledge the cited studies by Dr. Bruce Parker that inspired and enabled this paper. Also, we would like to thank the reviewers for their thoughtful comments.
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© 2019 American Society of Civil Engineers.
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Received: May 22, 2018
Accepted: Feb 6, 2019
Published online: Jul 9, 2019
Published in print: Sep 1, 2019
Discussion open until: Dec 9, 2019
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