Buoyancy fluxes in the Aegean Sea

dc.contributor.author	Δρακόπουλος, Πάνος	el
dc.contributor.author	Πούλος, Σεραφείμ	el
dc.contributor.author	Λασκαράτος, Αλέξανδρος	el
dc.date.accessioned	2015-01-23T15:54:35Z
dc.date.issued	2015-01-23
dc.identifier.uri	http://hdl.handle.net/11400/4619
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	Ocean-atmosphere interaction
dc.subject	River input
dc.subject	Aegean Sea
dc.subject	Αέρας-θάλασσα, αλληλεπιδράσεις
dc.subject	Είσοδος ποταμού
dc.subject	Αιγαίο
dc.title	Buoyancy fluxes in the Aegean Sea	en
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://id.loc.gov/authorities/subjects/sh85093878
heal.keywordURI	http://id.loc.gov/authorities/subjects/sh85001234
heal.identifier.secondary	ISSN: 0373-434X
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	1998
heal.bibliographicCitation	Drakopoulos, P.G., Poulos, S. and Lascaratos, A.(1998). Buoyancy fluxes in the Aegean Sea. Rapp. Comm. Int. Mer Medit. 35. pp. 134-135.	en
heal.abstract	Recent observations have shown that outflowing Aegean waters have replaced about 20% of the deep and bottom waters of the eastern Mediterranean basin. This indicates changes in the hydrology of water masses in the Aegean Sea and the corresponding thermohaline circulation. In this work we estimate the driving mechanism of the thermohaline circulation, the buoyancy fluxes using 45 years of COADS data. The long term buoyancy loss is estimated to be about 5xl0'6 kg nr1 S'-\ However for certain periods lasting a few years the flux reverses sign and there is buoyancy gain . The reversal of sign is expected to lead in changes of the thermohaline circulation in the basin.	en
heal.fullTextAvailability	true
heal.conferenceName	Rapp. Comm. Int. Mer Medit.35.	el
heal.conferenceItemType	full paper