Interannual sea level variability in the Mediterranean sea and its relation to local meteorological factors.

dc.contributor.author	Δρακόπουλος, Πάνος	el
dc.contributor.author	Λασκαράτος, Αλέξανδρος	el
dc.date.accessioned	2015-01-23T16:06:30Z
dc.date.issued	2015-01-23
dc.identifier.uri	http://hdl.handle.net/11400/4622
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	Wind
dc.subject	Time-series analysis--Congresses
dc.subject	Αλληλεπίδραση ωκεανού-ατμόσφαιρας
dc.subject	Άνεμος
dc.subject	Χρονοσειρά
dc.title	Interannual sea level variability in the Mediterranean sea and its relation to local meteorological factors.	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/sh2010116556
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. and Lascaratos, A.(1998). Interannual sea level variability in the Mediterranean sea and its relation to local meteorological factors. Rapp. Comm. Int. Mer Medit. 35. pp. 136-137.	en
heal.abstract	The response of the sea level in the Mediterranean to local meteorological forcing for time scales larger than the seasonal is examined. Multiple regression has indicated that the average sea level response to local air pressure is —0.8 cm/mb (15% of variability), and decreases toward the Eastern Mediterranean with no significant frequency dependence. The response to local wind stress is responsible for no more than 2% of the sea level variance and for most stations maximum response is in a cross shore direction. The annual cycle has amplitude ~5 cm (25% of variance) and peaks in October. According to these findings, almost 60% of variance cannot be explained by local meteorology.	en
heal.fullTextAvailability	true
heal.conferenceName	Rapp. Comm. Int. Mer Medit.35.	en
heal.conferenceItemType	full paper