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Tidal residual currents and sediment transport through multiple tidal inlets
- Date Issued:
- 1993
Title: | Tidal residual currents and sediment transport through multiple tidal inlets. |
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Name(s): |
Liu, James T., creator Aubrey, David G., creator Harbor Branch Oceanographic Institute |
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Type of Resource: | text | |
Genre: | Article | |
Issuance: | single unit | |
Date Issued: | 1993 | |
Publisher: | American Geophysical Union | |
Extent: | 46 p. | |
Physical Description: | ||
Language(s): | English | |
Identifier: | 3172972 (digitool), FADT3172972 (IID), fau:5715 (fedora), 10.1029/CE044 (doi) | |
Note(s): |
The combined influence of the tidal phase, amplitude, and mean sea-level differences on the generation of tidal residual currents in a channel is complex and non-linear, and can be predicted properly only by non-linear numerical models. The sediment transport patterns in a tidal channel that connects two bodies of water having different tidal characteristics can be attributed to residual currents that is primarily caused by the mean sea-level difference, and to a minor degree, by the tidal amplitude and phase differences between the two ends of the channel. Multiple inlets at Chatham, Massachusetts, are used as a case study. An edited version of this paper was published by AGU.This publication may be cited as: Liu, J. T. & Aubrey, D. G., (1993). Tidal residual currents and sediment transport through multiple tidal inlets. In D. G. Aubrey & G. S. Giese (Eds.), Formation and Evolution of Multiple Tidal Inlets, Coastal Estuarine Studies, 44, (pp. 113-157), doi:10.1029/CE044 Florida Atlantic University. Harbor Branch Oceanographic Institute contribution #756. |
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Subject(s): |
Tidal currents Sediment transport Tides Inlets Estuarine oceanography |
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Persistent Link to This Record: | http://purl.flvc.org/FCLA/DT/3172972 | |
Links: | http://dx.doi.org/10.1029/CE044 | |
Restrictions on Access: | ©1993 American Geophysical Union | |
Host Institution: | FAU |