Large scale moisture flux characteristics of the mediterranean basin and their relationships with drier and wetter climate conditions

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dc.authorid0000-0003-1714-1240
dc.authorid0000-0002-7662-3250
dc.authorscopusid36005636900
dc.authorscopusid6602448770
dc.authorscopusid7410338331
dc.authorscopusid7006309552
dc.authorscopusid57203672349
dc.authorwosidSahin, Sinan/ABA-6198-2020
dc.authorwosidHannah, David M./B-9221-2015
dc.contributor.authorŞahin, Sinan
dc.contributor.authorTürkeş, Murat
dc.contributor.authorWang, Sheng-Hung
dc.contributor.authorHannah, David
dc.contributor.authorEastwood, Warren
dc.date.accessioned2022-05-11T14:26:37Z
dc.date.available2022-05-11T14:26:37Z
dc.date.issued2015
dc.departmentFakülteler, Çorlu Mühendislik Fakültesi, İnşaat Mühendisliği Bölümü
dc.description.abstractLarge scale moisture flux analysis was carried out for the Mediterranean Basin in order to increase our understanding of the larger scale atmospheric controls on moisture flux convergence that are related to drier and wetter conditions. The seasonal moisture budget (precipitation minus evaporation) was calculated using the National Centers for Environmental Prediction-National Center for Atmospheric Research reanalysis data for the period 1949-2012. Results of the analysis show that the displacements of prevailing atmospheric action centres located over the subtropical mid-east Atlantic (i.e. Azores high) and the north-east Atlantic (i.e. sub-polar or Iceland low) to the north and to south, respectively, generally determine the wet or dry conditions over the Mediterranean Basin. In winter, the eddy fluxes originating from the mid-Atlantic propagate over Europe providing wet conditions in western and central Europe. The contribution of eddies to the moisture budget weaken in summer for the Mediterranean Basin, because of weaker and less frequent frontal activities in general.
dc.identifier.doi10.1007/s00382-015-2545-x
dc.identifier.endpage3401
dc.identifier.issn0930-7575
dc.identifier.issn1432-0894
dc.identifier.issue45637en_US
dc.identifier.scopus2-s2.0-84947487435
dc.identifier.scopusqualityQ1
dc.identifier.startpage3381
dc.identifier.urihttps://doi.org/10.1007/s00382-015-2545-x
dc.identifier.urihttps://hdl.handle.net/20.500.11776/6521
dc.identifier.volume45
dc.identifier.wosWOS:000365418900026
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthorŞahin, Sinan
dc.language.isoen
dc.publisherSpringer
dc.relation.ispartofClimate Dynamics
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectAtmospheric moisture budget
dc.subjectConvergence
dc.subjectWet and dry, drought
dc.subjectTeleconnections
dc.subjectMediterranean basin
dc.subjectNorth-Atlantic Oscillation
dc.subjectGeopotential Height Fields
dc.subjectWater-Budget
dc.subjectNcep-Ncar
dc.subjectPrecipitation
dc.subjectVariability
dc.subjectSummer
dc.subjectTurkey
dc.subjectSea
dc.subjectTemperature
dc.titleLarge scale moisture flux characteristics of the mediterranean basin and their relationships with drier and wetter climate conditions
dc.typeArticle

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