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Five different types of lowered snow line in alpine valleys
ID
Strle, Danijela
(
Avtor
),
ID
Ogrin, Matej
(
Avtor
)
URL - Izvorni URL, za dostop obiščite
https://link.springer.com/article/10.1007/s11629-020-6237-6
Opis: Dostopno s plačilom
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(6,93 MB)
MD5: C68DE73768FE5794942936BEDB094C13
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Izvleček
The snow line for the same precipitation event in alpine valleys can vary greatly from valley to valley, even when the valleys are close together. Often this is not due to a difference in air mass, but to a different interaction of topography and topography-related meteorological conditions. By knowing the causes of a lowered snow line, we can better understand the differences in snow cover in alpine valleys at the same elevation over short distances or the differences in snow cover between alpine valleys and areas outside the valleys. As different types of lowered snow line respond differently to climate change, we can also understand future changes in snow conditions in alpine valleys. To better understand the process, we observed the temperature conditions during winter precipitation events on the territory of Eastern Julian Alps (Slovenia) over a period of two years, focusing on the height of the zero isotherm. Depending on atmospheric conditions, especially changes in the temperature profile and precipitation intensity during precipitation events, five causes of lowered snow line have been identified. These types can occur individually, but during multi-day snowfall events they occur frequently or in combination.
Jezik:
Angleški jezik
Ključne besede:
climatogeography
,
snow
,
local climate
,
mountain climate
,
Slovenia
,
Julian Alps
Tipologija:
1.01 - Izvirni znanstveni članek
Organizacija:
FF - Filozofska fakulteta
Datum objave:
01.01.2022
Leto izida:
2022
Št. strani:
Str. 73-84
Številčenje:
Vol. 19, issue 1
PID:
20.500.12556/RUL-164655
UDK:
551.585.7(497.4)
ISSN pri članku:
1993-0321
DOI:
10.1007/s11629-020-6237-6
COBISS.SI-ID:
93190659
Datum objave v RUL:
06.11.2024
Število ogledov:
78
Število prenosov:
17
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Objavi na:
Gradivo je del revije
Naslov:
Journal of mountain science
Skrajšan naslov:
J. mt. sci.
Založnik:
Science Press, Springer
ISSN:
1993-0321
COBISS.SI-ID:
515419673
Sekundarni jezik
Jezik:
Slovenski jezik
Ključne besede:
klimatogeografija
,
padavine
,
lokalno podnebje
,
gorsko podnebje
,
Slovenija
,
Julijske Alpe
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