Snow water equivalent variability and forecast in Lithuania
Atmosphere circulation is the most important modulator of snow cover parameters. This study deals with the relation between the dominant Northern Hemisphere circulation mode, called the Artic Oscillation (AO), and the spatial distribution of the snow water equivalent (SWE) within the territory of Li...
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ftlithuaniansrc:oai:elaba:3100547 2023-05-15T15:45:41+02:00 Snow water equivalent variability and forecast in Lithuania Rimkus, Egidijus Stankūnavičius, Gintautas 2002 http://vu.lvb.lt/VU:ELABAPDB3100547&prefLang=en_US eng eng http://vu.lvb.lt/VU:ELABAPDB3100547&prefLang=en_US Boreal environment research : an international interdisciplinary journal, Helsinki : Finnish Environment Institute, 2002, vol. 7, no 4, p. 457-462 ISSN 1239-6095 info:eu-repo/semantics/article 2002 ftlithuaniansrc 2021-12-02T00:12:53Z Atmosphere circulation is the most important modulator of snow cover parameters. This study deals with the relation between the dominant Northern Hemisphere circulation mode, called the Artic Oscillation (AO), and the spatial distribution of the snow water equivalent (SWE) within the territory of Lithuania. The results indicate an inverse relation between the extreme AO phase and the SWE. However, the largest spatial differences are seen in the positive AO phase. Article in Journal/Newspaper Boreal Environment Research LSRC VL (Lithuanian Social Research Centre Virtual Library) |
institution |
Open Polar |
collection |
LSRC VL (Lithuanian Social Research Centre Virtual Library) |
op_collection_id |
ftlithuaniansrc |
language |
English |
description |
Atmosphere circulation is the most important modulator of snow cover parameters. This study deals with the relation between the dominant Northern Hemisphere circulation mode, called the Artic Oscillation (AO), and the spatial distribution of the snow water equivalent (SWE) within the territory of Lithuania. The results indicate an inverse relation between the extreme AO phase and the SWE. However, the largest spatial differences are seen in the positive AO phase. |
format |
Article in Journal/Newspaper |
author |
Rimkus, Egidijus Stankūnavičius, Gintautas |
spellingShingle |
Rimkus, Egidijus Stankūnavičius, Gintautas Snow water equivalent variability and forecast in Lithuania |
author_facet |
Rimkus, Egidijus Stankūnavičius, Gintautas |
author_sort |
Rimkus, Egidijus |
title |
Snow water equivalent variability and forecast in Lithuania |
title_short |
Snow water equivalent variability and forecast in Lithuania |
title_full |
Snow water equivalent variability and forecast in Lithuania |
title_fullStr |
Snow water equivalent variability and forecast in Lithuania |
title_full_unstemmed |
Snow water equivalent variability and forecast in Lithuania |
title_sort |
snow water equivalent variability and forecast in lithuania |
publishDate |
2002 |
url |
http://vu.lvb.lt/VU:ELABAPDB3100547&prefLang=en_US |
genre |
Boreal Environment Research |
genre_facet |
Boreal Environment Research |
op_source |
Boreal environment research : an international interdisciplinary journal, Helsinki : Finnish Environment Institute, 2002, vol. 7, no 4, p. 457-462 ISSN 1239-6095 |
op_relation |
http://vu.lvb.lt/VU:ELABAPDB3100547&prefLang=en_US |
_version_ |
1766380204233588736 |