dc.contributor.author | Δρακόπουλος, Πάνος | el |
dc.contributor.author | Λασκαράτος, Αλέξανδρος | el |
dc.date.accessioned | 2015-01-25T18:38:52Z | |
dc.date.available | 2015-01-25T18:38:52Z | |
dc.date.issued | 2015-01-25 | |
dc.identifier.uri | http://hdl.handle.net/11400/4716 | |
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 | Mediterranean Sea | |
dc.subject | Princeton Ocean Model (POM) | |
dc.subject | Regional basin | |
dc.subject | Μεσόγειος Θάλασσα | |
dc.subject | Περιφερειακή λεκάνη | |
dc.title | Modelling the Mediterranean Sea | en |
heal.type | journalArticle | |
heal.secondaryTitle | climatological forcing. | 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://id.loc.gov/authorities/subjects/sh85083236 | |
heal.identifier.secondary | doi:10.1016/S0924-7963(98)00080-3 | |
heal.language | en | |
heal.access | campus | |
heal.recordProvider | Τ.Ε.Ι. Αθήνας, Σχολή Επαγγελμάτων Υγείας & Πρόνοιας, Τμήμα Οπτικής & Οπτομετρίας | el |
heal.publicationDate | 1997-08-26 | |
heal.bibliographicCitation | Drakopoulos, P.G. and Lascaratos, A. (1999). Modelling the Mediterranean Sea: climatological forcing . Journal of Marine Systems 20(1-4), 26/08/1997, pp. 157-173. Available from: http://www.sciencedirect.com/science/article/pii/S0924796398000803 [Accessed 18/0/1999] | en |
heal.abstract | Within the framework of a Mediterranean model evaluation experiment, a Princeton Ocean Model POM of the Mediterranean has been developed in University of Athens. In this paper, the results of the coarse resolution version Ž. y1 1r48=1r48 are presented. SST and SSS were restored to monthly climatology with a time constant 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 Ž. known features have been modelled 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.journalName | Journal of Marine Systems | en |
heal.journalType | peer-reviewed | |
heal.fullTextAvailability | true |
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