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Latent cooling of atmosphere as an indicator of lowered snow line : Case study from Planica and Vrata valleys
ID Strle, Danijela (Author), ID Ogrin, Matej (Author)

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Abstract
A lowered snow line in Alpine valleys as a local weather phenomenon often varies from onevalley to another. The relief morphology of the valleys and the intensity of precipitation play a crucial rolein the variation. In Slovenia certain valleys are more susceptible to this phenomenon than others, one suchexample being the Planica Valley. This paper examines the occurrence of a lowered snow line in the PlanicaValley and the Vrata Valley during the winter seasons of 2015/2016 and 2016/2017. Precipitation eventsaccompanying the occurrence of a lowered snow line were analyzed, and data on temperature and pre-cipitation were included in the analysis. Results showed a striking degree of congruence of the phenomenonin both valleys.

Language:English
Keywords:geography, snow line, lowered snow line, mountain climate, local climate, snow precipitation, Planica (Slovenia), Vrata (Slovenia)
Typology:1.01 - Original Scientific Article
Organization:FF - Faculty of Arts
Publication date:01.01.2021
Year:2021
Number of pages:Str. 7-23
Numbering:61, št. 1
PID:20.500.12556/RUL-164777 This link opens in a new window
UDC:911.2:551.578.4:551.524(234.323.6)
ISSN on article:1581-6613
DOI:10.3986/AGS.8573 This link opens in a new window
COBISS.SI-ID:72512515 This link opens in a new window
Publication date in RUL:12.11.2024
Views:47
Downloads:187
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Record is a part of a journal

Title:Acta geographica Slovenica
Shortened title:Acta geogr. Slov.
Publisher:Geografski inštitut Antona Melika ZRC SAZU, Založba ZRC, Slovenska akademija znanosti in umetnosti
ISSN:1581-6613
COBISS.SI-ID:124775936 This link opens in a new window

Secondary language

Language:Slovenian
Title:Latentno ohlajanje ozračja kot pokazatelj znižane meje sneženja : Študija primera izdolin Planica in Vrata
Abstract:
Znižana meja sneženja se, kot lokalni vremenski pojav, v alpskih dolinah ne pojavlja pov-sod v enaki meri. Ključno vlogo imata zaprtost dolinskega reliefa ter intenziteta padavin. Splošno znanov Sloveniji je, da so nekatere doline, kot na primer dolina Planice za ta pojav zelo dovzetne, druge pa manj.V nekaterih dolinah je pojav manj poznan zgolj zaradi tega, ker so neposeljene in pozimi tudi neoblju-dene. Prispevek govori o analizi pojava znižane meje sneženja v dolini Planice in dolini Vrata v dveh zimskihsezonah 2015/2016 in 2016/2017. Analizirani so bili padavinski dogodki s pojavom znižane meje sneženja,v analizo pa smo vključili temperaturne podatke ter podatke o padavinah. Rezultati so pokazali presenetljivoujemanje pojava v obeh dolinah.

Keywords:geografija, meja sneženja, znižana meja sneženja, gorsko podnebje, lokalno podnebje, sneg, Planica (Slovenija), Vrata (Slovenija

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