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Impact of Atmospheric Circulation on the Occurrence of Very Strong and Extreme Cold Stress in Poland Cover

Impact of Atmospheric Circulation on the Occurrence of Very Strong and Extreme Cold Stress in Poland

Quaestiones Geographicae
Volume 41 (2022): Issue 3 (September 2022)
By: Małgorzata Owczarek and  Arkadiusz M. Tomczyk  
Open Access
|Aug 2022

Figures & Tables

Fig. 1

Location of meteorological stations.
Location of meteorological stations.

Fig. 2

Mean frequency of occurrence (%) of very strong and extreme cold stress according to the UTCI in Poland in the period November to March (A) and January (B), 1966/67 to 2018/19. UTCI, Universal Thermal Climate Index.
Mean frequency of occurrence (%) of very strong and extreme cold stress according to the UTCI in Poland in the period November to March (A) and January (B), 1966/67 to 2018/19. UTCI, Universal Thermal Climate Index.

Fig. 3

Multiannual variability of seasonal (November–March) number of days with very strong or extreme cold stress according to UTCI in Suwałki (A) and Warszawa (B), 1966/67 to 2018/19. Solid lines represent respective trends. UTCI, Universal Thermal Climate Index.
Multiannual variability of seasonal (November–March) number of days with very strong or extreme cold stress according to UTCI in Suwałki (A) and Warszawa (B), 1966/67 to 2018/19. Solid lines represent respective trends. UTCI, Universal Thermal Climate Index.

Fig. 4

Mean SLP [in hPa] (colour scale) and z500 hPa [in gpm] (dotted line) (A) anomalies of SLP [in hPa] (colour scale) and z500 hPa [in m] (dotted line) (B) and anomalies of T850 [in °C] (C) for days with very strong and extreme cold stress. SLP, sea level pressure.
Mean SLP [in hPa] (colour scale) and z500 hPa [in gpm] (dotted line) (A) anomalies of SLP [in hPa] (colour scale) and z500 hPa [in m] (dotted line) (B) and anomalies of T850 [in °C] (C) for days with very strong and extreme cold stress. SLP, sea level pressure.

Fig. 5

Mean SLP [in hPa] (colour scale) and z500 hPa [in gpm] (dotted line) (left column); SLP [in hPa] (colour scale) and z500 hPa anomalies [in m] (dotted line) (middle column); and anomalies of T850 [in °C] (right column) for the designated circulation types. SLP, sea level pressure.
Mean SLP [in hPa] (colour scale) and z500 hPa [in gpm] (dotted line) (left column); SLP [in hPa] (colour scale) and z500 hPa anomalies [in m] (dotted line) (middle column); and anomalies of T850 [in °C] (right column) for the designated circulation types. SLP, sea level pressure.

Fig. 6

UTCI values (°C) in Poland on selected days: 31 December 1978 (A) and 30 January 2014 (B). UTCI, Universal Thermal Climate Index.
UTCI values (°C) in Poland on selected days: 31 December 1978 (A) and 30 January 2014 (B). UTCI, Universal Thermal Climate Index.

Fig. 7

Mean SLP [in hPa] (colour scale) and z500 hPa [in gpm] (dotted line) (top row); SLP [in hPa] (colour scale) and z500 hPa anomalies [in m] (dotted line) (middle row); and anomalies of T850 [in °C] (bottom row) for the selected days. SLP, sea level pressure.
Mean SLP [in hPa] (colour scale) and z500 hPa [in gpm] (dotted line) (top row); SLP [in hPa] (colour scale) and z500 hPa anomalies [in m] (dotted line) (middle row); and anomalies of T850 [in °C] (bottom row) for the selected days. SLP, sea level pressure.

Selected characteristics of the number of days with very strong and extreme cold stress according to UTCI in Poland, 1966/67 to 2018/19: their maximum number and trend coefficient_ Statistically significant (at 0_05 level) trend values are in bold_

StationMaximum number of days and season of their occurrenceTrend (days· decade−1)
Białystok42 1971/72−3.53
Bielsko-Biała17 1967/68−0.91
Borucino48 1969/70−2.33
Chojnice7 1978/79 1986/870.00
Elbląg19 1969/70−0.34
Gdańsk15 1978/790.00
Gorzów Wlkp.13 1978/79−0.57
Hel16 1978/79−0.29
Jelenia Góra10 1975/76−0.36
Kalisz15 1986/870.00
Katowice6 1978/79−0.31
Kielce12 1984/85−0.24
Kłodzko9 1969/70, 1977/78, 1983/84, 1984/85−0.34
Kołobrzeg8 1978/79−0.53
Koszalin9 1978/79−0.59
Kraków14 1968/690.00
Lesko15 1978/79−1.43
Lublin13 1986/870.00
Łeba19 1978/79 1986/870.00
Łódź16 1969/70−0.99
Mikołajki47 1971/72−4.62
Mława28 1971/72−1.67
Olsztyn12 1969/700.00
Opole5 1978/79−0.31
Poznań14 1978/79−0.49
Racibórz10 1986/870.00
Rzeszów21 1968/69−0.35
Siedlce17 1986/87−0.81
Słubice6 1978/79−0.29
Suwałki34 1978/79−4.00
Świnoujście16 1986/87−0.53
Szczecin11 1978/790.00
Terespol20 1968/69−0.59
Toruń9 1978/79−0.53
Ustka10 2010/110.00
Warszawa19 1969/70, 1986/87−0.67
Włodawa21 1978/79−0.48
Wrocław9 1978/79−0.38
Zakopane4 1967/68−0.18
Zielona Góra9 1978/79−0.33
DOI: https://doi.org/10.2478/quageo-2022-0028 | Journal eISSN: 2081-6383 | Journal ISSN: 2082-2103
Journal RSS Feed
Language: English
Page range: 111 - 126
Submitted on: May 3, 2022
|
Published on: Aug 31, 2022
Published by: Adam Mickiewicz University
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year
Keywords:
bioclimatology,
UTCI,
atmospheric circulation,
cold stress,
winter,
Poland
Related subjects:
Geosciences,
Geography

© 2022 Małgorzata Owczarek, Arkadiusz M. Tomczyk, published by Adam Mickiewicz University
This work is licensed under the Creative Commons Attribution 4.0 License.

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