Kontynentalizm termiczny w Europie

dc.contributor.authorWitek, Michał
dc.contributor.authorBednorz, Ewa
dc.contributor.authorForycka-Ławniczak, Hanna
dc.date.accessioned2017-09-25T13:05:19Z
dc.date.available2017-09-25T13:05:19Z
dc.date.issued2015
dc.description.abstractFive indices of thermal continentality were computed for 84 stations in Europe and shown in the maps. The thermal continentality in Europe is spatially variable and increases eastward and southward from the northwestern shores towards Asia. Continental features are distinct in the interior of the Iberian Peninsula and in the northeastern part of the Scandinavian Peninsula, despite their small distance from the Atlantic Ocean. Most continentality indices (Chromow’s, Ewert’s, Conrad’s, Johansson-Ringleb’s) reveal a similar spatial pattern of thermal continentality in Europe, and they allow the continent to be divided into a western and eastern part along meridian 20–25°E. Marsz’s index, which takes into consideration the level of oceanity, indicates a narrow zone along the northwestern shore as oceanic and the remaining part of Europe as continental.pl_PL
dc.description.articlenumber13pl_PL
dc.description.journaltitleBadania Fizjograficznepl_PL
dc.description.pageof171pl_PL
dc.description.pageto182pl_PL
dc.description.tome6pl_PL
dc.identifier.citationBadania Fizjograficzne, Seria A, Tom 66, 2015, s. 171-182pl_PL
dc.identifier.doihttps://doi.org/10.14746/bfg.2015.6.13
dc.identifier.issn2081-6014
dc.identifier.urihttp://hdl.handle.net/10593/19321
dc.language.isopolpl_PL
dc.publisherWydawnictwo Poznańskiego Towarzystwa Przyjaciół Naukpl_PL
dc.relation.ispartofseriesSeria A - Geografia Fizyczna Tom 66;
dc.rightsinfo:eu-repo/semantics/openAccesspl_PL
dc.subjectEuropepl_PL
dc.subjectclimatepl_PL
dc.subjectthermal continentalitypl_PL
dc.subjectindicespl_PL
dc.titleKontynentalizm termiczny w Europiepl_PL
dc.typeArtykułpl_PL

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Uniwersytet im. Adama Mickiewicza w Poznaniu
Biblioteka Uniwersytetu im. Adama Mickiewicza w Poznaniu
Ministerstwo Nauki i Szkolnictwa Wyższego