1 Evidence of trends in near-surface wind speeds over the Baltic

Annual mean wind speeds over the Baltic significantly increased over the period 1953-1999 with the majority of the increase being associated with increases in the upper quartile of the wind speed distribution and the winter season. Trends in annual and seasonal mean wind speeds are greatest in relat...

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Main Authors: S. C. Pryor, R. J. Barthelmie, J. Schoof
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.866
http://www.risoe.dk/vea/projects/endow/papers/pryoretal_trends.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.490.866 2023-05-15T17:34:53+02:00 1 Evidence of trends in near-surface wind speeds over the Baltic S. C. Pryor R. J. Barthelmie J. Schoof The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.866 http://www.risoe.dk/vea/projects/endow/papers/pryoretal_trends.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.866 http://www.risoe.dk/vea/projects/endow/papers/pryoretal_trends.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.risoe.dk/vea/projects/endow/papers/pryoretal_trends.pdf Near-surface flow Baltic basin Trend analysis General Circulation Models text ftciteseerx 2016-01-08T08:30:20Z Annual mean wind speeds over the Baltic significantly increased over the period 1953-1999 with the majority of the increase being associated with increases in the upper quartile of the wind speed distribution and the winter season. Trends in annual and seasonal mean wind speeds are greatest in relative and absolute sense in the south-west of the Baltic basin where they are in excess of 0.25 m s-1 per decade for the annual mean. The majority of the increase in winter wind speeds is attributable to an increase in the frequency of westerly anticyclonic, westerly cyclonic and north-westerly cyclonic circulation types (defined by the Grosswetterlagen catalogue) which are in turn related to the recent prevalence of positive phase North Atlantic Oscillation. To address whether these trends will be maintained in the future we provide a highly provisional first prognosis for wind speeds during 2000-2030 based on simulations from the HadCM3 GCM. The results indicate that the first decades of the twenty-first century will be very similar to the 1990s with respect to the flow regime but that 2010’s may be characterized by slightly lower wind speeds. These results are highly preliminary because, as demonstrated, this GCM appears to underestimate wind speeds in the west of the Baltic, and slightly overestimate wind speeds in the northeast of the domain. Further evaluation of GCM simulations and use of downscaling techniques are advocated to provide more robust wind speed prognoses. Text North Atlantic North Atlantic oscillation Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Near-surface flow
Baltic basin
Trend analysis
General Circulation Models
spellingShingle Near-surface flow
Baltic basin
Trend analysis
General Circulation Models
S. C. Pryor
R. J. Barthelmie
J. Schoof
1 Evidence of trends in near-surface wind speeds over the Baltic
topic_facet Near-surface flow
Baltic basin
Trend analysis
General Circulation Models
description Annual mean wind speeds over the Baltic significantly increased over the period 1953-1999 with the majority of the increase being associated with increases in the upper quartile of the wind speed distribution and the winter season. Trends in annual and seasonal mean wind speeds are greatest in relative and absolute sense in the south-west of the Baltic basin where they are in excess of 0.25 m s-1 per decade for the annual mean. The majority of the increase in winter wind speeds is attributable to an increase in the frequency of westerly anticyclonic, westerly cyclonic and north-westerly cyclonic circulation types (defined by the Grosswetterlagen catalogue) which are in turn related to the recent prevalence of positive phase North Atlantic Oscillation. To address whether these trends will be maintained in the future we provide a highly provisional first prognosis for wind speeds during 2000-2030 based on simulations from the HadCM3 GCM. The results indicate that the first decades of the twenty-first century will be very similar to the 1990s with respect to the flow regime but that 2010’s may be characterized by slightly lower wind speeds. These results are highly preliminary because, as demonstrated, this GCM appears to underestimate wind speeds in the west of the Baltic, and slightly overestimate wind speeds in the northeast of the domain. Further evaluation of GCM simulations and use of downscaling techniques are advocated to provide more robust wind speed prognoses.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author S. C. Pryor
R. J. Barthelmie
J. Schoof
author_facet S. C. Pryor
R. J. Barthelmie
J. Schoof
author_sort S. C. Pryor
title 1 Evidence of trends in near-surface wind speeds over the Baltic
title_short 1 Evidence of trends in near-surface wind speeds over the Baltic
title_full 1 Evidence of trends in near-surface wind speeds over the Baltic
title_fullStr 1 Evidence of trends in near-surface wind speeds over the Baltic
title_full_unstemmed 1 Evidence of trends in near-surface wind speeds over the Baltic
title_sort 1 evidence of trends in near-surface wind speeds over the baltic
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.866
http://www.risoe.dk/vea/projects/endow/papers/pryoretal_trends.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source http://www.risoe.dk/vea/projects/endow/papers/pryoretal_trends.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.866
http://www.risoe.dk/vea/projects/endow/papers/pryoretal_trends.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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