Horizontal Precipitation Gradients in Alpine Valleys of Northwestern Slovenia

Mountain landscapes are the areas characteristic for a great spatial variability of precipitation amounts. On the windward sides of orographic barriers there is intense rising of air, and on the lee sides air descends. The intensity of the two processes is manifested in great differences in precipit...

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Main Authors: Matej Ogrin, Erika Kozamernik
Format: Article
Language:English
Published: Znanstvena založba Filozofske fakultete Univerze v Ljubljani (Ljubljana University Press, Faculty of Arts) 2018-12-01
Series:Dela
Subjects:
Online Access:https://revije.ff.uni-lj.si/Dela/article/view/8097
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spelling doaj-bf29d780e5ff47d6917c2161775115972020-11-24T22:01:43ZengZnanstvena založba Filozofske fakultete Univerze v Ljubljani (Ljubljana University Press, Faculty of Arts)Dela0354-05961854-10892018-12-014953610.4312/dela.49.5-368097Horizontal Precipitation Gradients in Alpine Valleys of Northwestern SloveniaMatej Ogrin0Erika KozamernikUniversity of Ljubljana, Faculty of ArtsMountain landscapes are the areas characteristic for a great spatial variability of precipitation amounts. On the windward sides of orographic barriers there is intense rising of air, and on the lee sides air descends. The intensity of the two processes is manifested in great differences in precipitation amounts at short distances. Although the network of precipitation stations is the densest in the Alps of all mountain regions in the world, precipitation regime at the micro level continues to be poorly known at many a place. Precipitation stations in mountainous landscapes are the most numerous in lower-lying and settled areas, whereas they are rather few in the high-lying areas. Also the accuracy of measurements is problematic in the mountains. As a result, the information on precipitation regime is inadequate right in the areas with the largest precipitation amounts. This means that the estimation of water balance is inadequate, and it is difficult to forecast the precipitation-related processes, such as torrential floods, landslides, avalanches, and the like. The present paper deals with horizontal precipitation gradients in the Alpine valleys of Planica, Krnica and the stream Beli potok which are all situated in the north-western part of the Slovenian section of the Julian Alps.https://revije.ff.uni-lj.si/Dela/article/view/8097mountain climate, precipitation gradients, Julian Alps, orographic precipitation, Alpine valleys
collection DOAJ
language English
format Article
sources DOAJ
author Matej Ogrin
Erika Kozamernik
spellingShingle Matej Ogrin
Erika Kozamernik
Horizontal Precipitation Gradients in Alpine Valleys of Northwestern Slovenia
Dela
mountain climate, precipitation gradients, Julian Alps, orographic precipitation, Alpine valleys
author_facet Matej Ogrin
Erika Kozamernik
author_sort Matej Ogrin
title Horizontal Precipitation Gradients in Alpine Valleys of Northwestern Slovenia
title_short Horizontal Precipitation Gradients in Alpine Valleys of Northwestern Slovenia
title_full Horizontal Precipitation Gradients in Alpine Valleys of Northwestern Slovenia
title_fullStr Horizontal Precipitation Gradients in Alpine Valleys of Northwestern Slovenia
title_full_unstemmed Horizontal Precipitation Gradients in Alpine Valleys of Northwestern Slovenia
title_sort horizontal precipitation gradients in alpine valleys of northwestern slovenia
publisher Znanstvena založba Filozofske fakultete Univerze v Ljubljani (Ljubljana University Press, Faculty of Arts)
series Dela
issn 0354-0596
1854-1089
publishDate 2018-12-01
description Mountain landscapes are the areas characteristic for a great spatial variability of precipitation amounts. On the windward sides of orographic barriers there is intense rising of air, and on the lee sides air descends. The intensity of the two processes is manifested in great differences in precipitation amounts at short distances. Although the network of precipitation stations is the densest in the Alps of all mountain regions in the world, precipitation regime at the micro level continues to be poorly known at many a place. Precipitation stations in mountainous landscapes are the most numerous in lower-lying and settled areas, whereas they are rather few in the high-lying areas. Also the accuracy of measurements is problematic in the mountains. As a result, the information on precipitation regime is inadequate right in the areas with the largest precipitation amounts. This means that the estimation of water balance is inadequate, and it is difficult to forecast the precipitation-related processes, such as torrential floods, landslides, avalanches, and the like. The present paper deals with horizontal precipitation gradients in the Alpine valleys of Planica, Krnica and the stream Beli potok which are all situated in the north-western part of the Slovenian section of the Julian Alps.
topic mountain climate, precipitation gradients, Julian Alps, orographic precipitation, Alpine valleys
url https://revije.ff.uni-lj.si/Dela/article/view/8097
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AT erikakozamernik horizontalprecipitationgradientsinalpinevalleysofnorthwesternslovenia
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