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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://repozitorij.uni-lj.si/IzpisGradiva.php?id=164777"><dc:title>Latent cooling of atmosphere as an indicator of lowered snow line</dc:title><dc:creator>Strle,	Danijela	(Avtor)
	</dc:creator><dc:creator>Ogrin,	Matej	(Avtor)
	</dc:creator><dc:subject>geography</dc:subject><dc:subject>snow line</dc:subject><dc:subject>lowered snow line</dc:subject><dc:subject>mountain climate</dc:subject><dc:subject>local climate</dc:subject><dc:subject>snow precipitation</dc:subject><dc:subject>Planica (Slovenia)</dc:subject><dc:subject>Vrata (Slovenia)</dc:subject><dc:description>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.</dc:description><dc:date>2021</dc:date><dc:date>2024-11-12 09:29:26</dc:date><dc:type>Neznano</dc:type><dc:identifier>164777</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
