The importance of water accumulation of snow cover measurements in mountainous regions of Slovenia

Snow cover is a frequent phenomenon in Slovenia and even in the lowlands of the interior regions, it can last for several weeks. The properties of snow and winter weather after the snow cover has formed, determine the load of snow upon houses, trees and other objects. Water accumulation of snow cove...

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Main Authors: Matej Ogrin, Jaka Ortar
Format: Article
Language:English
Published: ZRC SAZU, Založba ZRC 2007-12-01
Series:Acta Geographica Slovenica
Subjects:
Online Access:https://ojs.zrc-sazu.si/ags/article/view/1246
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author Matej Ogrin
Jaka Ortar
author_facet Matej Ogrin
Jaka Ortar
author_sort Matej Ogrin
collection DOAJ
description Snow cover is a frequent phenomenon in Slovenia and even in the lowlands of the interior regions, it can last for several weeks. The properties of snow and winter weather after the snow cover has formed, determine the load of snow upon houses, trees and other objects. Water accumulation of snow cover (WASC) gives us the amount of water in snow and therefore also the weight of snow. Deep snow cover can soak its own melting water from the surface, so WASC does not decrease as fast as one would conclude from the intensity of melting. WASC is also a good indicator of winter precipitation where precipitation stations are rare and precipitation gradients are big. The researches carried out in the winter 2005/2006 showed that precipitation in the central part of the Bohinj ridge in the Slovenian Julian Alps, was about 50% higher than at its northern edge, where the meteorological station Vogel is located.
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spelling doaj.art-cb597785008548fa9477bd8fd2ae1e9b2022-12-22T04:39:00ZengZRC SAZU, Založba ZRCActa Geographica Slovenica1581-66131581-83142007-12-01471477110.3986/AGS47103975The importance of water accumulation of snow cover measurements in mountainous regions of SloveniaMatej OgrinJaka OrtarSnow cover is a frequent phenomenon in Slovenia and even in the lowlands of the interior regions, it can last for several weeks. The properties of snow and winter weather after the snow cover has formed, determine the load of snow upon houses, trees and other objects. Water accumulation of snow cover (WASC) gives us the amount of water in snow and therefore also the weight of snow. Deep snow cover can soak its own melting water from the surface, so WASC does not decrease as fast as one would conclude from the intensity of melting. WASC is also a good indicator of winter precipitation where precipitation stations are rare and precipitation gradients are big. The researches carried out in the winter 2005/2006 showed that precipitation in the central part of the Bohinj ridge in the Slovenian Julian Alps, was about 50% higher than at its northern edge, where the meteorological station Vogel is located.https://ojs.zrc-sazu.si/ags/article/view/1246snow coverwater accumulation of snow coverweight of snowupper sava valleybohinj ridge
spellingShingle Matej Ogrin
Jaka Ortar
The importance of water accumulation of snow cover measurements in mountainous regions of Slovenia
Acta Geographica Slovenica
snow cover
water accumulation of snow cover
weight of snow
upper sava valley
bohinj ridge
title The importance of water accumulation of snow cover measurements in mountainous regions of Slovenia
title_full The importance of water accumulation of snow cover measurements in mountainous regions of Slovenia
title_fullStr The importance of water accumulation of snow cover measurements in mountainous regions of Slovenia
title_full_unstemmed The importance of water accumulation of snow cover measurements in mountainous regions of Slovenia
title_short The importance of water accumulation of snow cover measurements in mountainous regions of Slovenia
title_sort importance of water accumulation of snow cover measurements in mountainous regions of slovenia
topic snow cover
water accumulation of snow cover
weight of snow
upper sava valley
bohinj ridge
url https://ojs.zrc-sazu.si/ags/article/view/1246
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