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The effect of hyperpycnal water on tidal exchange
- Date Issued:
- 1996
Title: | The effect of hyperpycnal water on tidal exchange. |
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Name(s): | Smith, Ned P., creator | |
Type of Resource: | text | |
Genre: | Article | |
Issuance: | single unit | |
Date Issued: | 1996 | |
Publisher: | American Geophysical Union | |
Extent: | 11 p. | |
Physical Description: | ||
Language(s): | English | |
Identifier: | 3172981 (digitool), FADT3172981 (IID), fau:5719 (fedora), 10.1029/CE053 (doi) | |
Note(s): |
Current meter and hydrographic data from a tidal channel connecting the western side of Exuma Sound with the eastern margin of Great Bahama Bank are used to investigate the efficiency of tidal exchanges. The density of water leaving the bank is usually higher than the density of water arriving on the flood tide. Data from near the shelf break confirm that density currents cascade down the narrow shelf. An edited version of this paper was published by AGU. This publication may be cited as: Smith, N. P. (1996). The effect of hyperpycnal water on tidal exchange. In D. G. Aubrey & C. T. Friedrichs (Eds.), Buoyancy Effects on Coastal and Estuarine Dynamics, Coastal Estuarine Studies, 53, (pp. 107-116). doi:10.1029/CE053 Florida Atlantic University. Harbor Branch Oceanographic Institute contribution #1135. |
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Subject(s): |
Hydrology Tides Sediment transport Salinity Temperature |
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Persistent Link to This Record: | http://purl.flvc.org/FCLA/DT/3172981 | |
Links: | http://dx.doi.org/10.1029/CE053 | |
Restrictions on Access: | ©1996 American Geophysical Union | |
Host Institution: | FAU |