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dc.creatorBurić, Dragan
dc.creatorDragojlović, Jovan
dc.creatorPenjišević-Sočanac, Ivana
dc.creatorLuković, Jelena
dc.creatorDoderović, Miroslav
dc.date.accessioned2021-09-24T15:42:14Z
dc.date.available2021-09-24T15:42:14Z
dc.date.issued2019
dc.identifier.issn1610-2002
dc.identifier.urihttps://gery.gef.bg.ac.rs/handle/123456789/963
dc.description.abstractPrevious research conducted in Montenegro suggested an increase in maximum and minimum daily temperatures in the last decades, followed by growth of extreme events frequency. This study examines the relationship between temperature and atmospheric circulation fields in Montenegro using 9 WMO-CCL/CLIVAR extreme climatic indices. The data on atmospheric circulation refers to 11 teleconnection patterns analyzed by seasonal timescales. The assessment of the impact of certain teleconnection patterns has shown a significant connection to extreme events in Montenegro. Calculated results showed the strongest impact of EA, MO, WeMO, EAWR and AO during the winter season, while the weaker impact was calculated for NAO and SCAND. The best impact is obtained for EA and AO during spring, while summer temperature variations are connected to EA, AMO, EAWR, SCAND and NAO. The autumn season showed strong connection with EA, SCAND, AMO, EAWR, MO and AO.en
dc.publisherSpringer
dc.rightsrestrictedAccess
dc.sourceClimate Change Management
dc.subjectAtmospheric oscillationen
dc.subjectExtremesen
dc.subjectMontenegroen
dc.subjectTemperatureen
dc.titleRelationship Between Atmospheric Circulation and Temperature Extremes in Montenegro in the Period 1951–2010en
dc.typebookPart
dc.rights.licenseARR
dcterms.abstractЛуковић, Јелена; Пењишевић-Сочанац, Ивана; Додеровић, Мирослав; Драгојловић, Јован; Бурић, Драган;
dc.citation.spage29
dc.citation.epage42
dc.citation.other: 29-42
dc.identifier.doi10.1007/978-3-030-03383-5_3
dc.identifier.scopus2-s2.0-85071426915
dc.identifier.rcubhttps://hdl.handle.net/21.15107/rcub_gery_963
dc.type.versionpublishedVersion


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