DC pole | Wartość | Język |
dc.contributor.author | Falarz, Małgorzata | - |
dc.date.accessioned | 2019-05-13T08:06:24Z | - |
dc.date.available | 2019-05-13T08:06:24Z | - |
dc.date.issued | 2013 | - |
dc.identifier.citation | Theoretical and Applied Climatology, Vol. 111, no. 1 (2013), s. 21-28 | pl_PL |
dc.identifier.issn | 0177-798X | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/9096 | - |
dc.description.abstract | The seasonal stability of snow cover (ISS) was
defined as a percentage ratio of the real and the potential
snow cover duration in a winter season. Main results of the
study are as follows: (1) alternately occurring periods of
high and low values of the index of snow cover stability
did not appeared simultaneously in mountainous and nonmountainous
areas; (2) in the majority of Poland area both
zonal and meridional components of the atmospheric circulation
influence the ISS; however, in south the meridional
air flow reveals the stronger impact, mostly due to the
intensification of the southern advection by the foehn effect;
and (3) changes of two or three indices describing atmospheric
circulation explain up to 50 % of the ISS in Poland.
The diminishing stability of snow cover in Poland corresponds
with an increasing intensity of the advection from
the western sector in winter in the second half of the twentieth
century in Europe. | pl_PL |
dc.language.iso | en | pl_PL |
dc.rights | Uznanie autorstwa 3.0 Polska | * |
dc.rights.uri | http://creativecommons.org/licenses/by/3.0/pl/ | * |
dc.subject | snow cover | pl_PL |
dc.subject | snow | pl_PL |
dc.subject | snow water equivalent | pl_PL |
dc.title | Seasonal stability of snow cover in Poland in relation to the atmospheric circulation | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.relation.journal | Theoretical and Applied Climatology | pl_PL |
dc.identifier.doi | 10.1007/s00704-012-0642-x | - |
Pojawia się w kolekcji: | Artykuły (WNP)
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