A numerical model of the seasonal general circulation in the Mediterranean sea.

dc.contributor.author	Δρακόπουλος, Πάνος	el
dc.contributor.author	Λασκαράτος, Αλέξανδρος	el
dc.date.accessioned	2015-01-23T16:34:13Z
dc.date.issued	2015-01-23
dc.identifier.uri	http://hdl.handle.net/11400/4626
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	Princeton Ocean Model
dc.subject	Oceanographic measurement
dc.subject	Deep-sea temperature
dc.subject	Mediterranean Sea
dc.subject	Μεσόγειος θάλασσα
dc.subject	Θάλασσα επιφανειακή θερμοκρασία
dc.subject	Αλατότητα
dc.title	A numerical model of the seasonal general circulation in the Mediterranean sea.	en
dc.title	Αριθμητικό ομοίωμα της εποχικής γενικής κυκλοφορίας της Μεσογείου.	el
heal.type	conferenceItem
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://skos.um.es/unescothes/C02812
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh85036384
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh85083236
heal.dateAvailable	10000-01-01
heal.language	el
heal.language	en
heal.access	forever
heal.recordProvider	Τ.Ε.Ι. Αθήνας, Σχολή Επαγγελμάτων Υγείας & Πρόνοιας, Τμήμα Οπτικής & Οπτομετρίας	el
heal.publicationDate	1998-04-15
heal.bibliographicCitation	Drakopoulos, P.G. and Lascaratos, A. (1997). A numerical model of the seasonal general circulation in the Mediterranean sea. 5th National Symposium on Oceanography and Fisheries, Kavala, Greece. 15-18/04/1997, pp. 335-338.	en
heal.abstract	A Princeton Ocean Model (POM) of the Mediterranean Sea has been developed in University of Athens. In this paper the results of the climatological run at a horizontal resolution of 0.25 x 0.25 deg. are presented. Sea Surface Temperature (SST) and Sea Surface Salinity (SSS) were restored to monthly climatology with a restoring coefficient of 1 m/day. The seasonal variability of the general circulation was found to be in a good agreement with the observed patterns and some known features have been observed for the first time. The implied surface fluxes (heat loss and salt gain) were too weak and resulted in absence of deep water formation.	en
heal.fullTextAvailability	true
heal.conferenceName	5th National Symposium on Oceanography and Fisheries, Kavala, Greece.	en
heal.conferenceItemType	full paper