Analyses of sea level fluctuations in Thermaicos Gulf and Salonica Bay, northwestern Aegean Sea
Analyses of sea level fluctuations in Thermaicos Gulf and Salonica Bay, northwestern Aegean Sea
Short period (2·4 to 2·7 h) and long period (several days) oscillations of non-tidal origin have been identified in the analysis of a short series of sea level records from stations in Salonica Bay and Thermaicos Gulf.
Oscillations of short period can be attributed to seiche-like motions; those of long period correspond with variations in barometric pressure. The harmonic constituents are generally indicative of a standing tidal wave over the whole of the area.
325-334
Wilding, Amanda
d41bdddc-943f-46c7-973d-91814c7109df
Collins, Michael
3b70278b-0004-45e0-b3c9-0debdf0a9351
Ferentinos, George
abacdc6a-8c4d-41c4-9a21-ce4eee70802d
March 1980
Wilding, Amanda
d41bdddc-943f-46c7-973d-91814c7109df
Collins, Michael
3b70278b-0004-45e0-b3c9-0debdf0a9351
Ferentinos, George
abacdc6a-8c4d-41c4-9a21-ce4eee70802d
Wilding, Amanda, Collins, Michael and Ferentinos, George
(1980)
Analyses of sea level fluctuations in Thermaicos Gulf and Salonica Bay, northwestern Aegean Sea.
Estuarine, Coastal and Shelf Science, 10 (3), .
(doi:10.1016/S0302-3524(80)80105-8).
Abstract
Short period (2·4 to 2·7 h) and long period (several days) oscillations of non-tidal origin have been identified in the analysis of a short series of sea level records from stations in Salonica Bay and Thermaicos Gulf.
Oscillations of short period can be attributed to seiche-like motions; those of long period correspond with variations in barometric pressure. The harmonic constituents are generally indicative of a standing tidal wave over the whole of the area.
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Published date: March 1980
Identifiers
Local EPrints ID: 72311
URI: http://eprints.soton.ac.uk/id/eprint/72311
ISSN: 0272-7714
PURE UUID: 04f5459f-975c-4ae3-bbf0-e414328477e0
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Date deposited: 05 Feb 2010
Last modified: 13 Mar 2024 21:23
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Contributors
Author:
Amanda Wilding
Author:
Michael Collins
Author:
George Ferentinos
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