A note on processes influencing the mixed layer depth in the North Western Aegean Sea

dc.contributor.author	Sultan, Selman A.R.	en
dc.contributor.author	James, Alec E.	en
dc.contributor.author	Collins, Michael B.	en
dc.date.accessioned	2016-01-25T08:03:00Z
dc.date.issued	2016-01-25
dc.identifier.uri	http://hdl.handle.net/123456789/324
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	Water masses	en
dc.subject	Thermocline	en
dc.subject	Mixed layer depth	en
dc.title	A note on processes influencing the mixed layer depth in the North Western Aegean Sea	en
heal.type	journalArticle
heal.classification	Ωκεανογραφία	el
heal.classification	Physical Oceanography	en
heal.classificationURI	N/A-Ωκεανογραφία
heal.classificationURI	N/A-Physical Oceanography
heal.keywordURI	N/A-Water masses
heal.keywordURI	N/A-Thermocline
heal.keywordURI	N/A-Mixed layer depth
heal.contributorName	Sultan, Selman A.R.	en
heal.contributorName	James, Alec E.	en
heal.contributorName	Collins, Michael B.	en
heal.identifier.secondary	thalassographica vol.6 ,5-18 (1984)
heal.dateAvailable	2016-01-25T08:08:00Z
heal.language	el
heal.language	en
heal.access	free
heal.recordProvider	Department of Oceanography,University College,Singleton park	en
heal.publicationDate	1984-12
heal.bibliographicCitation	Selman A.R. Sultan, Alec E. James, Michael B. Collins (1984).A note on processes influencing the mixed layer depth in the North Western Aegean Sea.Thalassographica, 7: 5-18 .	en
heal.abstract	Physical oceanographic observations in the N.W. Aegean Sea have defined a surface mixed, isothermal layer above the main thermocline. The observations were made both before and after the passage of a severe storm through the area. The area is divided into three main oceanographic regions, based on water mass characteristics. The response and recovery of the surface layers to the storm, in each of the regions, is examined. In the more exposed areas of the N.W. Aegean Sea, there is a linear response between wind speed and the depth of the mixed layer; this is typical for both predictions and observations in open ocean areas elsewhere. In enclosed areas of the Sea, freshwater inputs and water circulation patterns further influence the development of the surface mixed layer and the wind effect is not as clear.	en
heal.publisher	ΙΩΚΑΕ	el
heal.publisher	IOFR	en
heal.journalName	Θαλασσογραφικά	el
heal.journalName	Thalassographica	en
heal.journalType	peer-reviewed
heal.fullTextAvailability	true
heal.coverage.spatial	Aegean sea	el
heal.coverage.spatial	Αιγαίο Πέλαγος	el