Winter thermal extremes in Poland and their circulation conditions
The study’s objective was to determine the spatial and temporal variability of occurrence of extremely warm days in winter in Poland in 1966/67–2020/21, and to determine the effect of atmospheric circulation on their occurrence. An extremely warm day is defined as a day with a maximum daily air temp...
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Adam Mickiewicz University Poznan
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ftamickiewiczojs:oai:ojs.pressto.amu.edu.pl:article/39026 2023-09-05T13:21:28+02:00 Winter thermal extremes in Poland and their circulation conditions Zimowe ekstrema termiczne w Polsce i ich cyrkulacyjne uwarunkowania Tomczyk, Arkadiusz M. Miś, Filip 2023-08-02 application/pdf http://pressto.amu.edu.pl/index.php/bfg/article/view/39026 pol pol Adam Mickiewicz University Poznan http://pressto.amu.edu.pl/index.php/bfg/article/view/39026/33187 http://pressto.amu.edu.pl/index.php/bfg/article/view/39026 Prawa autorskie (c) 2022 Prof. UAM dr hab. Arkadiusz M. Tomczyk, Filip Miś http://creativecommons.org/licenses/by-nc-nd/4.0 Badania Fizjograficzne Seria A - Geografia Fizyczna; Tom 13 Nr A 73 (2022); 193-205 2081-6014 air temperature warm days NOA SCAND winter Poland info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Artykuł naukowy 2023 ftamickiewiczojs 2023-08-21T23:06:20Z The study’s objective was to determine the spatial and temporal variability of occurrence of extremely warm days in winter in Poland in 1966/67–2020/21, and to determine the effect of atmospheric circulation on their occurrence. An extremely warm day is defined as a day with a maximum daily air temperature equal to or higher than the value of the 95. percentile. The effect of atmospheric circulation on the occurrence of the analyzed days was determined on the basis on two teleconnection patterns, namely the North Atlantic Oscillation (NAO) and Scandinavia (SCAND). The progressing warming translated into increasingly frequent occurrence of extremely warm days. In terms of the abundance of such days, the following winters stood out in the entire multiannual period: 1989/90, 2015/16, 2006/07, and 2001/02. The study’s objective was to determine the spatial and temporal variability of occurrence of extremely warm days in winter in Poland in 1966/67–2020/21, and to determine the effect of atmospheric circulation on their occurrence. An extremely warm day is defined as a day with a maximum daily air temperature equal to or higher than the value of the 95. percentile. The effect of atmospheric circulation on the occurrence of the analyzed days was determined on the basis on two teleconnection patterns, namely the North Atlantic Oscillation (NAO) and Scandinavia (SCAND). The progressing warming translated into increasingly frequent occurrence of extremely warm days. In terms of the abundance of such days, the following winters stood out in the entire multiannual period: 1989/90, 2015/16, 2006/07, and 2001/02. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Adam Mickiewicz University in Poznań: PRESSto |
institution |
Open Polar |
collection |
Adam Mickiewicz University in Poznań: PRESSto |
op_collection_id |
ftamickiewiczojs |
language |
Polish |
topic |
air temperature warm days NOA SCAND winter Poland |
spellingShingle |
air temperature warm days NOA SCAND winter Poland Tomczyk, Arkadiusz M. Miś, Filip Winter thermal extremes in Poland and their circulation conditions |
topic_facet |
air temperature warm days NOA SCAND winter Poland |
description |
The study’s objective was to determine the spatial and temporal variability of occurrence of extremely warm days in winter in Poland in 1966/67–2020/21, and to determine the effect of atmospheric circulation on their occurrence. An extremely warm day is defined as a day with a maximum daily air temperature equal to or higher than the value of the 95. percentile. The effect of atmospheric circulation on the occurrence of the analyzed days was determined on the basis on two teleconnection patterns, namely the North Atlantic Oscillation (NAO) and Scandinavia (SCAND). The progressing warming translated into increasingly frequent occurrence of extremely warm days. In terms of the abundance of such days, the following winters stood out in the entire multiannual period: 1989/90, 2015/16, 2006/07, and 2001/02. The study’s objective was to determine the spatial and temporal variability of occurrence of extremely warm days in winter in Poland in 1966/67–2020/21, and to determine the effect of atmospheric circulation on their occurrence. An extremely warm day is defined as a day with a maximum daily air temperature equal to or higher than the value of the 95. percentile. The effect of atmospheric circulation on the occurrence of the analyzed days was determined on the basis on two teleconnection patterns, namely the North Atlantic Oscillation (NAO) and Scandinavia (SCAND). The progressing warming translated into increasingly frequent occurrence of extremely warm days. In terms of the abundance of such days, the following winters stood out in the entire multiannual period: 1989/90, 2015/16, 2006/07, and 2001/02. |
format |
Article in Journal/Newspaper |
author |
Tomczyk, Arkadiusz M. Miś, Filip |
author_facet |
Tomczyk, Arkadiusz M. Miś, Filip |
author_sort |
Tomczyk, Arkadiusz M. |
title |
Winter thermal extremes in Poland and their circulation conditions |
title_short |
Winter thermal extremes in Poland and their circulation conditions |
title_full |
Winter thermal extremes in Poland and their circulation conditions |
title_fullStr |
Winter thermal extremes in Poland and their circulation conditions |
title_full_unstemmed |
Winter thermal extremes in Poland and their circulation conditions |
title_sort |
winter thermal extremes in poland and their circulation conditions |
publisher |
Adam Mickiewicz University Poznan |
publishDate |
2023 |
url |
http://pressto.amu.edu.pl/index.php/bfg/article/view/39026 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
Badania Fizjograficzne Seria A - Geografia Fizyczna; Tom 13 Nr A 73 (2022); 193-205 2081-6014 |
op_relation |
http://pressto.amu.edu.pl/index.php/bfg/article/view/39026/33187 http://pressto.amu.edu.pl/index.php/bfg/article/view/39026 |
op_rights |
Prawa autorskie (c) 2022 Prof. UAM dr hab. Arkadiusz M. Tomczyk, Filip Miś http://creativecommons.org/licenses/by-nc-nd/4.0 |
_version_ |
1776202079137693696 |