Występowanie pokrywy śnieżnej w różnych masach powietrza na przykładzie Legnicy i Zamościa
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Date
2005
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Wydawnictwo Poznańskiego Towarzystwa Przyjaciół Nauk
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Abstract
The 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.
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Citation
Badania Fizjograficzne, Seria A, Tom 56, 2005, s. 7-14
Seria
Seria A - Geografia Fizyczna Tom 56;
ISBN
83-7063-456-7
ISSN
0067-2807