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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fttriple:oai:gotriple.eu:oai:doaj.org/article:49cb5992333a4d42a44b0f4d063f08ac 2023-05-15T16:11:48+02:00 The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) Kyösti Laaksonen 1977-01-01 https://doaj.org/article/49cb5992333a4d42a44b0f4d063f08ac en eng Geographical Society of Finland 1798-5617 https://doaj.org/article/49cb5992333a4d42a44b0f4d063f08ac undefined Fennia: International Journal of Geography, Vol 151, Iss 1 (1977) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1977 fttriple 2023-01-22T19:27:36Z 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 Unknown |
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language |
English |
topic |
geo envir |
spellingShingle |
geo envir Kyösti Laaksonen The influence of sea areas upon mean air temperatures in Fennoscandia (1921-1950) |
topic_facet |
geo envir |
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 |
Kyösti Laaksonen |
author_facet |
Kyösti Laaksonen |
author_sort |
Kyösti Laaksonen |
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://doaj.org/article/49cb5992333a4d42a44b0f4d063f08ac |
genre |
Fennoscandia Sea ice |
genre_facet |
Fennoscandia Sea ice |
op_source |
Fennia: International Journal of Geography, Vol 151, Iss 1 (1977) |
op_relation |
1798-5617 https://doaj.org/article/49cb5992333a4d42a44b0f4d063f08ac |
op_rights |
undefined |
_version_ |
1765996987530870784 |