Long‐term occurrence, variability and tracks of deep cyclones over Krakow (Central Europe) during the period 1900–2010
Abstract This article discusses patterns in the long‐term and seasonal occurrence of deep cyclones over Krakow. This study analysed the frequency of occurrence of air pressure values equal to or lower than the 1st percentile (equivalent to ≤995.3 hPa) of all air pressure values recorded at 12:00 UTC...
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crwiley:10.1002/joc.3459 2024-06-02T08:12:21+00:00 Long‐term occurrence, variability and tracks of deep cyclones over Krakow (Central Europe) during the period 1900–2010 Bielec‐Bąkowska, Zuzanna Piotrowicz, Katarzyna 2012 http://dx.doi.org/10.1002/joc.3459 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3459 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3459 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 33, issue 3, page 677-689 ISSN 0899-8418 1097-0088 journal-article 2012 crwiley https://doi.org/10.1002/joc.3459 2024-05-03T11:10:54Z Abstract This article discusses patterns in the long‐term and seasonal occurrence of deep cyclones over Krakow. This study analysed the frequency of occurrence of air pressure values equal to or lower than the 1st percentile (equivalent to ≤995.3 hPa) of all air pressure values recorded at 12:00 UTC over a period of 110 years (1900/1901–2009/2010). Special attention was devoted to the tracks of deep cyclones. No distinct changes were found in the frequency of occurrence of deep cyclones during the study period. Overall the frequency peaked in December, but in recent years there has been an increase in frequency towards the end of winter and beginning of spring. A similar general lack of noticeable change in the number of days with deep cyclones can also be found in specific tracks. There were minor increases in the frequency of occurrence of cyclones from the Norwegian Sea (T1), the Atlantic (T3), Bay of Biscay (T6) and the Mediterranean (T7) after 1950. The study also found confirmation of the theory that cyclone tracks had shortened at their northeastern extremities. Copyright © 2012 Royal Meteorological Society Article in Journal/Newspaper Norwegian Sea Wiley Online Library Norwegian Sea International Journal of Climatology 33 3 677 689 |
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Open Polar |
collection |
Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract This article discusses patterns in the long‐term and seasonal occurrence of deep cyclones over Krakow. This study analysed the frequency of occurrence of air pressure values equal to or lower than the 1st percentile (equivalent to ≤995.3 hPa) of all air pressure values recorded at 12:00 UTC over a period of 110 years (1900/1901–2009/2010). Special attention was devoted to the tracks of deep cyclones. No distinct changes were found in the frequency of occurrence of deep cyclones during the study period. Overall the frequency peaked in December, but in recent years there has been an increase in frequency towards the end of winter and beginning of spring. A similar general lack of noticeable change in the number of days with deep cyclones can also be found in specific tracks. There were minor increases in the frequency of occurrence of cyclones from the Norwegian Sea (T1), the Atlantic (T3), Bay of Biscay (T6) and the Mediterranean (T7) after 1950. The study also found confirmation of the theory that cyclone tracks had shortened at their northeastern extremities. Copyright © 2012 Royal Meteorological Society |
format |
Article in Journal/Newspaper |
author |
Bielec‐Bąkowska, Zuzanna Piotrowicz, Katarzyna |
spellingShingle |
Bielec‐Bąkowska, Zuzanna Piotrowicz, Katarzyna Long‐term occurrence, variability and tracks of deep cyclones over Krakow (Central Europe) during the period 1900–2010 |
author_facet |
Bielec‐Bąkowska, Zuzanna Piotrowicz, Katarzyna |
author_sort |
Bielec‐Bąkowska, Zuzanna |
title |
Long‐term occurrence, variability and tracks of deep cyclones over Krakow (Central Europe) during the period 1900–2010 |
title_short |
Long‐term occurrence, variability and tracks of deep cyclones over Krakow (Central Europe) during the period 1900–2010 |
title_full |
Long‐term occurrence, variability and tracks of deep cyclones over Krakow (Central Europe) during the period 1900–2010 |
title_fullStr |
Long‐term occurrence, variability and tracks of deep cyclones over Krakow (Central Europe) during the period 1900–2010 |
title_full_unstemmed |
Long‐term occurrence, variability and tracks of deep cyclones over Krakow (Central Europe) during the period 1900–2010 |
title_sort |
long‐term occurrence, variability and tracks of deep cyclones over krakow (central europe) during the period 1900–2010 |
publisher |
Wiley |
publishDate |
2012 |
url |
http://dx.doi.org/10.1002/joc.3459 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3459 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3459 |
geographic |
Norwegian Sea |
geographic_facet |
Norwegian Sea |
genre |
Norwegian Sea |
genre_facet |
Norwegian Sea |
op_source |
International Journal of Climatology volume 33, issue 3, page 677-689 ISSN 0899-8418 1097-0088 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/joc.3459 |
container_title |
International Journal of Climatology |
container_volume |
33 |
container_issue |
3 |
container_start_page |
677 |
op_container_end_page |
689 |
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1800758753727873024 |