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Zastosuj identyfikator do podlinkowania lub zacytowania tej pozycji: http://hdl.handle.net/20.500.12128/10500
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dc.contributor.authorŁupikasza, Ewa-
dc.contributor.authorNiedźwiedź, Tadeusz-
dc.date.accessioned2019-08-05T07:22:33Z-
dc.date.available2019-08-05T07:22:33Z-
dc.date.issued2013-
dc.identifier.citationBulletin of Geography. Physical Geography Series, 2013, vol. 6, iss. 1, p. 81-97pl_PL
dc.identifier.issn2080-7686-
dc.identifier.issn2300-8490-
dc.identifier.urihttp://hdl.handle.net/20.500.12128/10500-
dc.description.abstractThe paper aims to present research into both the long-term variability in the ice days in Svalbard representing the Atlantic sector of the Arctic, and their relations to atmospheric circulation. Ice days are defined as days with a daily maximum temperature below 0°C (Tmax<0°C). They are considered to be amongst the most important indices of current climate change. All the available data on daily maximum air temperature from three Norwegian stations (Svalbard Airport (Svalbard Lufthavn), Bjørnøya and Hopen) and from the Polish Polar Station in Hornsund (SW Spitsbergen) have been employed. The relevance of atmospheric circulation to the frequency of the occurrence of ice days was evaluated by calculating the Spearman correlation coefficients between the frequency of ice days and three regional circulation indices: zonal westerly circulation index (W), meridional southerly circulation index (S) and index of cyclonicity (C). At all the stations the number of ice days exhibited significant decreasing trends in the period of 1979-2012.pl_PL
dc.language.isoenpl_PL
dc.rightsUznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/pl/*
dc.subjectMaximum air temperaturepl_PL
dc.subjectIce dayspl_PL
dc.subjectCirculation indicespl_PL
dc.subjectSvalbardpl_PL
dc.subjectArcticpl_PL
dc.titleFrequency of Ice Days at Selected Meteorological Stations in Svalbardpl_PL
dc.typeinfo:eu-repo/semantics/articlepl_PL
dc.identifier.doi10.2478/bgeo-2013-0005-
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