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dc.contributor.authorBartzokas, A.en
dc.contributor.authorGanas, I. S.en
dc.date.accessioned2015-11-24T18:35:11Z-
dc.date.available2015-11-24T18:35:11Z-
dc.identifier.issn0899-8418-
dc.identifier.urihttps://olympias.lib.uoi.gr/jspui/handle/123456789/17057-
dc.rightsDefault Licence-
dc.subjectmediterraneanen
dc.subjectsea-surface temperatureen
dc.subjectprincipal components factor analysisen
dc.subjectprincipal component analysisen
dc.subjectlevel pressureen
dc.subjectunited-statesen
dc.subjectheight fielden
dc.subjectvariabilityen
dc.subjectrotationen
dc.subjectfrequencyen
dc.titleSpatial and Temporal Sea-Surface Temperature Covariances in the Mediterraneanen
heal.typejournalArticle-
heal.type.enJournal articleen
heal.type.elΆρθρο Περιοδικούel
heal.identifier.secondary<Go to ISI>://A1994NE12100005-
heal.identifier.secondaryhttp://onlinelibrary.wiley.com/store/10.1002/joc.3370140206/asset/3370140206_ftp.pdf?v=1&t=h0xitl6b&s=89d648a381a61dc044a3c648af90a80afeeb5daa-
heal.languageen-
heal.accesscampus-
heal.recordProviderΠανεπιστήμιο Ιωαννίνων. Σχολή Επιστημών και Τεχνολογιών. Τμήμα Βιολογικών Εφαρμογών και Τεχνολογιώνel
heal.publicationDate1994-
heal.abstractUsing sea-surface temperature data for the, post-war period, the Mediterranean Sea is divided objectively (principal components factor analysis) into subareas with similar covariances. This division is not the same in every season of the year. In summer, two subareas are found, the west and the east. In spring and autumn three, and in winter four significant subareas denote physical oceanographic and meteorological processes. The scores of the analyses show clearly the minimum of the late 1970s and then the warming of recent years somewhat delayed in the eastern Mediterranean.en
heal.journalNameInternational Journal of Climatologyen
heal.journalTypepeer reviewed-
heal.fullTextAvailabilityTRUE-
Appears in Collections:Άρθρα σε επιστημονικά περιοδικά ( Ανοικτά)

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