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dc.contributor.author Ζωδιάτης, Γιώργος el
dc.contributor.author Δρακόπουλος, Πάνος el
dc.contributor.author Brenner, Steve en
dc.contributor.author Groom, Steve en
dc.date.accessioned 2015-01-22T16:49:33Z
dc.date.issued 2015-01-22
dc.identifier.uri http://hdl.handle.net/11400/4555
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.source ΤΕΙ Αθήνας el
dc.subject Eastern Mediterranean
dc.subject Levantine Basin
dc.subject CYCLOPS project
dc.subject General Circulation Models
dc.subject Warm core mesoscale eddies
dc.subject Satellite imagery
dc.subject Ανατολική Μεσόγειος
dc.subject Γενική Κυκλοφορία
dc.subject Δορυφορικές εικόνες
dc.title Cyclops project en
heal.type book
heal.secondaryTitle the hydrodynamics of the warm core eddy south of Cyprus, SE Levantine Basin en
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://lod.nal.usda.gov/13661
heal.identifier.secondary ISBN 975-288-451-2
heal.dateAvailable 10000-01-01
heal.language en
heal.access forever
heal.recordProvider Τ.Ε.Ι. Αθήνας, Σχολή Επαγγελμάτων Υγείας & Πρόνοιας, Τμήμα Οπτικής & Οπτομετρίας el
heal.publicationDate 2003
heal.bibliographicCitation Zodiatis, G., Drakopoulos, P., Brenner, S. and Groom, S. (2003). Cyclops project: the hydrodynamics of the warm core eddy south of Cyprus, SE Levantine Basin. Yilmaz, Aysen. pp 18-23. en
heal.abstract The Levantine Basin circulation pattern as obtained during April-May and August 2001, within the frame of the EU CYCLOPS project, showed that the dominant flow feature in the region south of Cyprus is the warm core eddy, known as the Cyprus eddy. Its centre was found to be located about 80 km west of its previous location during the 80s and late 90s, and the eddy was quite strong with geostrophic currents around the rim as high as 30-40 cm/s in the near surface layers. The salinity and temperature signals of the eddy were discernible down to 350 m. The computed geostrophic velocities of the eddy were comparable to the values estimated from the displacement of a subsurface buoy deployed by the PML group during the May 2001 CYCLOPS cruise. The post cruise model simulations also showed similar velocity values in the jet. en
heal.publisher Yilmaz, Aysen el
heal.fullTextAvailability true


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Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες Except where otherwise noted, this item's license is described as Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες