A preliminary study on the internal tides of the gulfs of Patras and Korinthos, Greece.

dc.contributor.author	Δρακόπουλος, Πάνος	el
dc.contributor.author	Λασκαράτος, Αλέξανδρος	el
dc.date.accessioned	2015-01-25T19:30:46Z
dc.date.available	2015-01-25T19:30:46Z
dc.date.issued	2015-01-25
dc.identifier.uri	http://hdl.handle.net/11400/4719
dc.rights	Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/us/	*
dc.subject	Tides
dc.subject	Greek Mainland
dc.subject	Submarine topography
dc.subject	Ocean wave power
dc.subject	Παλίρροιες
dc.subject	Ελληνική ηπειρωτική
dc.subject	Υποθαλάσσια τοπογραφία
dc.subject	Κύματα ωκεανού
dc.title	A preliminary study on the internal tides of the gulfs of Patras and Korinthos, Greece.	el
heal.type	journalArticle
heal.classification	Ophthalmology
heal.classification	Optics
heal.classification	Οφθαλμολογία
heal.classification	Οπτική
heal.classificationURI	http://skos.um.es/unescothes/C02842
heal.classificationURI	http://skos.um.es/unescothes/C02847
heal.classificationURI	N/A-Οφθαλμολογία
heal.classificationURI	N/A-Οπτική
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh85135283
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh85129498
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh85093907
heal.identifier.secondary	doi:10.1016/S0278-4343(98)00052-1
heal.language	en
heal.access	campus
heal.recordProvider	Τ.Ε.Ι. Αθήνας, Σχολή Επαγγελμάτων Υγείας & Πρόνοιας, Τμήμα Οπτικής & Οπτομετρίας	el
heal.publicationDate	1998-04-21
heal.bibliographicCitation	Drakopoulos, P.G. and Lascaratos, A. (1998). A preliminary study on the internal tides of the gulfs of Patras and Korinthos, Greece . Continental Shelf Research 18(12), 21/04/1998, pp. 1517-1529. Available from: http://www.sciencedirect.com/science/article/pii/S0278434398000521 [Accessed 15/04/1999].	en
heal.abstract	The semi-diurnal baroclinic tide in the semi-closed channel which lies between the Greek Mainland and Peloponnesus has been investigated. It appears to be generated in the centre of the channel, where a bottom step topography exists. At a location 8km away from the source, its amplitude reaches 3m during spring tides. Modal decomposition of the baroclinic tide indicated that the ﬁrst mode accounts for 80% of the energy while almost all of the energy is accounted for by the ﬁrst three vertical modes. During the observational period several upwellingevents occurred.These eventscaused baroclinictidal energyto disappearthrough the weakening of the stratiﬁcation within 10—20h. The higher modes dissipated much faster than the ﬁrst mode which continued to gain energy until the isopycnal tilt reached a maximum. The availableset of data indicatesthat thebaroclinic oscillationsmaynot bean internalKelvin-type wave.	en
heal.journalName	Continental Shelf Research.	en
heal.journalType	peer-reviewed
heal.fullTextAvailability	true
heal.dateCreated	1995-03-21