The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950)
Individual maritimity maps were constructed for each month in the year on the basis of regression analysis. The pattern of the residuals obtained provides indications of the additional influence of factors such as sea water temperature, sea ice, warm and cold advection, cloud cover, snow cover and t...
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Geographical Society of Finland
1977
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fttsvojs:oai:journal.fi:article/9222 2023-05-15T16:11:48+02:00 The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) Laaksonen, Kyösti 1977-01-01 https://fennia.journal.fi/article/view/9222 en eng Geographical Society of Finland https://fennia.journal.fi/article/view/9222 Copyright (c) 2014 Fennia Fennia; Vol 151 Nro 1 (1977) Fennia - International Journal of Geography; Vol 151 No 1 (1977) 1798-5617 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 1977 fttsvojs 2020-09-30T22:46:18Z Individual maritimity maps were constructed for each month in the year on the basis of regression analysis. The pattern of the residuals obtained provides indications of the additional influence of factors such as sea water temperature, sea ice, warm and cold advection, cloud cover, snow cover and the major regional climatic factor, the Kölen mountain range, enabling these to be taken into account in the construction of the maritimity maps. The results enable an examination to be made of both the long‑range effects of the Atlantic Ocean and the inland sea area and also the local effects of individual seas. Substantial seasonal fluctuations are to be observed in the regional distribution of maritimity and continentality. Article in Journal/Newspaper Fennoscandia Sea ice Federation of Finnish Learned Societies: Scientific Journals Online |
institution |
Open Polar |
collection |
Federation of Finnish Learned Societies: Scientific Journals Online |
op_collection_id |
fttsvojs |
language |
English |
description |
Individual maritimity maps were constructed for each month in the year on the basis of regression analysis. The pattern of the residuals obtained provides indications of the additional influence of factors such as sea water temperature, sea ice, warm and cold advection, cloud cover, snow cover and the major regional climatic factor, the Kölen mountain range, enabling these to be taken into account in the construction of the maritimity maps. The results enable an examination to be made of both the long‑range effects of the Atlantic Ocean and the inland sea area and also the local effects of individual seas. Substantial seasonal fluctuations are to be observed in the regional distribution of maritimity and continentality. |
format |
Article in Journal/Newspaper |
author |
Laaksonen, Kyösti |
spellingShingle |
Laaksonen, Kyösti The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) |
author_facet |
Laaksonen, Kyösti |
author_sort |
Laaksonen, Kyösti |
title |
The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) |
title_short |
The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) |
title_full |
The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) |
title_fullStr |
The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) |
title_full_unstemmed |
The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) |
title_sort |
influence of sea areas upon mean air temperatures in fennoscandia (1921-1950) |
publisher |
Geographical Society of Finland |
publishDate |
1977 |
url |
https://fennia.journal.fi/article/view/9222 |
genre |
Fennoscandia Sea ice |
genre_facet |
Fennoscandia Sea ice |
op_source |
Fennia; Vol 151 Nro 1 (1977) Fennia - International Journal of Geography; Vol 151 No 1 (1977) 1798-5617 |
op_relation |
https://fennia.journal.fi/article/view/9222 |
op_rights |
Copyright (c) 2014 Fennia |
_version_ |
1765996990189010944 |