Changes in surface wind directions in Estonia during 1966–2008 and their relationships with large-scale atmospheric circulation

Changes in the percentages of eight main surface wind directions at 14 meteorological stations in Estonia, Northeast Europe, were studied during 1966–2008. Long-term changes in wind directions are related to variations in the large-scale atmospheric circulation but partly also to changes in the surr...

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Main Authors: Jaak Jaagus, Ain Kull
Format: Article
Language:English
Published: Estonian Academy Publishers 2011-11-01
Series:Estonian Journal of Earth Sciences
Subjects:
Online Access:http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_4/earth-2011-4-220-231.pdf
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spelling doaj-97c7aca1b0614552a7dac018f82dd2f82020-11-25T00:46:01ZengEstonian Academy PublishersEstonian Journal of Earth Sciences1736-47282011-11-0160422023110.3176/earth.2011.4.03Changes in surface wind directions in Estonia during 1966–2008 and their relationships with large-scale atmospheric circulationJaak JaagusAin KullChanges in the percentages of eight main surface wind directions at 14 meteorological stations in Estonia, Northeast Europe, were studied during 1966–2008. Long-term changes in wind directions are related to variations in the large-scale atmospheric circulation but partly also to changes in the surroundings of the stations and in wind obstacles. Significant alterations in wind directions were determined, and found to be the strongest in the winter season. The percentages of W and SW winds have clear positive trends, while SE, E and NE winds are characterized by negative tendencies in winter. In conclusion, wind directions have probably been shifted from east to west. Differences in trends between the stations are explained by changes in wind obstacles around the stations. The trends in wind roses in Estonia were caused by the intensification of the westerly circulation over the Atlantic/European sector during the winter season.http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_4/earth-2011-4-220-231.pdfwind directionsclimate changeatmospheric circulationwind roseEstonia.
collection DOAJ
language English
format Article
sources DOAJ
author Jaak Jaagus
Ain Kull
spellingShingle Jaak Jaagus
Ain Kull
Changes in surface wind directions in Estonia during 1966–2008 and their relationships with large-scale atmospheric circulation
Estonian Journal of Earth Sciences
wind directions
climate change
atmospheric circulation
wind rose
Estonia.
author_facet Jaak Jaagus
Ain Kull
author_sort Jaak Jaagus
title Changes in surface wind directions in Estonia during 1966–2008 and their relationships with large-scale atmospheric circulation
title_short Changes in surface wind directions in Estonia during 1966–2008 and their relationships with large-scale atmospheric circulation
title_full Changes in surface wind directions in Estonia during 1966–2008 and their relationships with large-scale atmospheric circulation
title_fullStr Changes in surface wind directions in Estonia during 1966–2008 and their relationships with large-scale atmospheric circulation
title_full_unstemmed Changes in surface wind directions in Estonia during 1966–2008 and their relationships with large-scale atmospheric circulation
title_sort changes in surface wind directions in estonia during 1966–2008 and their relationships with large-scale atmospheric circulation
publisher Estonian Academy Publishers
series Estonian Journal of Earth Sciences
issn 1736-4728
publishDate 2011-11-01
description Changes in the percentages of eight main surface wind directions at 14 meteorological stations in Estonia, Northeast Europe, were studied during 1966–2008. Long-term changes in wind directions are related to variations in the large-scale atmospheric circulation but partly also to changes in the surroundings of the stations and in wind obstacles. Significant alterations in wind directions were determined, and found to be the strongest in the winter season. The percentages of W and SW winds have clear positive trends, while SE, E and NE winds are characterized by negative tendencies in winter. In conclusion, wind directions have probably been shifted from east to west. Differences in trends between the stations are explained by changes in wind obstacles around the stations. The trends in wind roses in Estonia were caused by the intensification of the westerly circulation over the Atlantic/European sector during the winter season.
topic wind directions
climate change
atmospheric circulation
wind rose
Estonia.
url http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2011/issue_4/earth-2011-4-220-231.pdf
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