Występowanie pokrywy śnieżnej w różnych masach powietrza na przykładzie Legnicy i Zamościa

dc.contributor.authorBednorz, Ewa
dc.contributor.authorWięcław, Mirosław
dc.date.accessioned2017-01-23T08:41:10Z
dc.date.available2017-01-23T08:41:10Z
dc.date.issued2005
dc.description.abstractThe relationships between the kind of air masses and snow cover occurrence in two stations: Legnica and Zamość were investigated, using daily snow cover depths and daily calendar of air masses for the years 1971-2000. The frequency of the days with snow cover in the different air masses was counted and furthermore, air masses favourable to increases and decreases in snow cover depth were singled out. Snow cover appears most often in arctic and polar-continental air masses. Arctic air is favourable to snowfalls, which lead to increases in the snow cover depth, while polar-continental air guaranties snow sustainment. Polarmaritime air which is the most frequent in Poland during the wintertime can also bring snowfalls, but in this air masses snow does not last long, because polar-maritime air is the most favourable to decreases in snow cover depth.pl_PL
dc.identifier.citationBadania Fizjograficzne, Seria A, Tom 56, 2005, s. 7-14pl_PL
dc.identifier.isbn83-7063-456-7
dc.identifier.issn0067-2807
dc.identifier.urihttp://hdl.handle.net/10593/17375
dc.language.isopolpl_PL
dc.publisherWydawnictwo Poznańskiego Towarzystwa Przyjaciół Naukpl_PL
dc.relation.ispartofseriesSeria A - Geografia Fizyczna Tom 56;
dc.rightsinfo:eu-repo/semantics/openAccesspl_PL
dc.titleWystępowanie pokrywy śnieżnej w różnych masach powietrza na przykładzie Legnicy i Zamościapl_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