Cyclops project

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