The climate of northern Finland
The North Atlantic in the west and the Asian continent in the east regulate the general features of the climate in northern Finland. Especially in the low areas in the west, the smaller amounts of precipitation are largely due to the Scandic föhn effect. The weather conditions and microclimate in th...
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Geographical Society of Finland
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fttsvojs:oai:journal.fi:article/3764 2023-05-15T17:30:30+02:00 The climate of northern Finland Autio, Jyrki Heikkinen, Olavi 2002-01-02 application/pdf https://fennia.journal.fi/article/view/3764 eng eng Geographical Society of Finland https://fennia.journal.fi/article/view/3764/3555 https://fennia.journal.fi/article/view/3764 Copyright (c) 2014 Fennia Fennia; Vol 180 Nro 1-2 (2002); 61-66 Fennia - International Journal of Geography; Vol 180 No 1-2 (2002); 61-66 1798-5617 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 2002 fttsvojs 2020-09-30T22:46:00Z The North Atlantic in the west and the Asian continent in the east regulate the general features of the climate in northern Finland. Especially in the low areas in the west, the smaller amounts of precipitation are largely due to the Scandic föhn effect. The weather conditions and microclimate in the fells differ from those in the lower areas. Temperature inversion is a common phenomenon on the slopes. Heavy snow loads in the crowns of the trees are a prominent feature of the southern fells and the eastern highlands. Article in Journal/Newspaper North Atlantic Northern Finland Federation of Finnish Learned Societies: Scientific Journals Online |
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Open Polar |
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Federation of Finnish Learned Societies: Scientific Journals Online |
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fttsvojs |
language |
English |
description |
The North Atlantic in the west and the Asian continent in the east regulate the general features of the climate in northern Finland. Especially in the low areas in the west, the smaller amounts of precipitation are largely due to the Scandic föhn effect. The weather conditions and microclimate in the fells differ from those in the lower areas. Temperature inversion is a common phenomenon on the slopes. Heavy snow loads in the crowns of the trees are a prominent feature of the southern fells and the eastern highlands. |
format |
Article in Journal/Newspaper |
author |
Autio, Jyrki Heikkinen, Olavi |
spellingShingle |
Autio, Jyrki Heikkinen, Olavi The climate of northern Finland |
author_facet |
Autio, Jyrki Heikkinen, Olavi |
author_sort |
Autio, Jyrki |
title |
The climate of northern Finland |
title_short |
The climate of northern Finland |
title_full |
The climate of northern Finland |
title_fullStr |
The climate of northern Finland |
title_full_unstemmed |
The climate of northern Finland |
title_sort |
climate of northern finland |
publisher |
Geographical Society of Finland |
publishDate |
2002 |
url |
https://fennia.journal.fi/article/view/3764 |
genre |
North Atlantic Northern Finland |
genre_facet |
North Atlantic Northern Finland |
op_source |
Fennia; Vol 180 Nro 1-2 (2002); 61-66 Fennia - International Journal of Geography; Vol 180 No 1-2 (2002); 61-66 1798-5617 |
op_relation |
https://fennia.journal.fi/article/view/3764/3555 https://fennia.journal.fi/article/view/3764 |
op_rights |
Copyright (c) 2014 Fennia |
_version_ |
1766127219025903616 |