Εμφάνιση απλής εγγραφής

dc.contributor.author Δρακόπουλος, Πάνος el
dc.contributor.author Marsden, Richard F. en
dc.date.accessioned 2015-01-25T20:52:44Z
dc.date.available 2015-01-25T20:52:44Z
dc.date.issued 2015-01-25
dc.identifier.uri http://hdl.handle.net/11400/4727
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 Coastal Ocean Dynamics Experiment (CODE)
dc.subject Island Coastal Current Experiment
dc.subject Vancouver Island (B.C.)
dc.subject Spectral analysis
dc.subject Tides
dc.subject Βανκούβερ
dc.subject Φασματική ανάλυση
dc.subject Παλίρροιες
dc.title The internal tide off the west coast of Vancouver island en
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/sh2006001521
heal.keywordURI http://id.loc.gov/authorities/subjects/sh2001008907
heal.keywordURI http://id.loc.gov/authorities/subjects/sh85135283
heal.identifier.secondary doi.org/10.1175/1520-0485(1993)023<0758:TITOTW>2.0.CO;2
heal.language en
heal.access free
heal.recordProvider Τ.Ε.Ι. Αθήνας, Σχολή Επαγγελμάτων Υγείας & Πρόνοιας, Τμήμα Οπτικής & Οπτομετρίας el
heal.publicationDate 1992-06-22
heal.bibliographicCitation Drakopoulos, P.G.and Marsden, R.F. (1993). The internal tide off the west coast of Vancouver Island . Journal of Physical Oceanography 23(4), 22/06/1992, pp. 758-775. Available from: http://journals.ametsoc.org/doi/abs/10.1175/1520-0485(1993)023%3C0758%3ATITOTW%3E2.0.CO%3B2 en
heal.abstract Using data from the Coastal Ocean Dynamics Experiment ( CODE ) and the Island Coastal Current Experiment, the internal ride offthe west coast ofthe Vancouver Island was studied. Although the semidiurnal barotropic velocity field in the area was weak, the baroclinic field was found to be relatively strong with speeds up to five times greater. The intermittent nature of the baroclinic field was resolved by estimating the M2 tidal harmonic coefficients every 24 hours in l5-day overlaping intervals. These time-evolving coefficients were then analyzed using spectral analysis methods. For most ofthe area under investigation, the internal tide was generated mainly at the shelf break and was found to propagate cross-shore. Off Estevan point, where the bottom contour is regular, the beam structure was identified and traced to distances 40 km from the generation region on the slope. The downward-propagating beam was found to follow the seasonal variation ofthe characteristic prop- agation paths. An empirical orthogonal function analysis revealed a highly coherent baroclinic field (787o of the M2 variance). The predictions of an internal tide model were found to be in good agreement with the experimental results on the slope. The interaction of a cyclonic eddy, present in the area during August 1980, with the internal tide was also addresse. en
heal.journalName Journal of Physical Oceanography en
heal.journalType peer-reviewed
heal.fullTextAvailability true
heal.dateCreated 1991-03-18


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Εμφάνιση απλής εγγραφής

Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες Εκτός από όπου ορίζεται κάτι διαφορετικό, αυτή η άδεια περιγράφεται ως Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες