Impact of Atmospheric Circulation on the Occurrence of Very Strong and Extreme Cold Stress in Poland
31 ago 2022
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Publicado en línea: 31 ago 2022
Páginas: 111 - 126
Recibido: 03 may 2022
DOI: https://doi.org/10.2478/quageo-2022-0028
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© 2022 Małgorzata Owczarek et al., published by Sciendo
This work is licensed under the Creative Commons Attribution 4.0 International License.
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![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.](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/647351144e662f30ba539ed7/j_quageo-2022-0028_fig_004.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20250912%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20250912T142921Z&X-Amz-Expires=3600&X-Amz-Signature=111e23e1e34a7364b8eba44b5e0947c30d820e79710882e12b3a777e6174ccd5&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
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![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.](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/647351144e662f30ba539ed7/j_quageo-2022-0028_fig_005.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20250912%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20250912T142921Z&X-Amz-Expires=3600&X-Amz-Signature=4ddc4cb9dd3c4c5329c49f84c950462d1aaaaa7bd8549f06d7473e256aa24910&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
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![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.](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/647351144e662f30ba539ed7/j_quageo-2022-0028_fig_007.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20250912%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20250912T142921Z&X-Amz-Expires=3600&X-Amz-Signature=1de5eff0004e444828c2f8bf18df7514038a095372df62c2daf65c9a29863ba2&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
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_
Station | Maximum number of days and season of their occurrence | Trend (days· decade−1) |
---|---|---|
Białystok | 42 1971/72 | |
Bielsko-Biała | 17 1967/68 | |
Borucino | 48 1969/70 | |
Chojnice | 7 1978/79 1986/87 | 0.00 |
Elbląg | 19 1969/70 | −0.34 |
Gdańsk | 15 1978/79 | 0.00 |
Gorzów Wlkp. | 13 1978/79 | −0.57 |
Hel | 16 1978/79 | |
Jelenia Góra | 10 1975/76 | |
Kalisz | 15 1986/87 | 0.00 |
Katowice | 6 1978/79 | |
Kielce | 12 1984/85 | |
Kłodzko | 9 1969/70, 1977/78, 1983/84, 1984/85 | |
Kołobrzeg | 8 1978/79 | −0.53 |
Koszalin | 9 1978/79 | −0.59 |
Kraków | 14 1968/69 | 0.00 |
Lesko | 15 1978/79 | |
Lublin | 13 1986/87 | 0.00 |
Łeba | 19 1978/79 1986/87 | 0.00 |
Łódź | 16 1969/70 | |
Mikołajki | 47 1971/72 | |
Mława | 28 1971/72 | |
Olsztyn | 12 1969/70 | 0.00 |
Opole | 5 1978/79 | −0.31 |
Poznań | 14 1978/79 | |
Racibórz | 10 1986/87 | 0.00 |
Rzeszów | 21 1968/69 | −0.35 |
Siedlce | 17 1986/87 | |
Słubice | 6 1978/79 | −0.29 |
Suwałki | 34 1978/79 | |
Świnoujście | 16 1986/87 | |
Szczecin | 11 1978/79 | 0.00 |
Terespol | 20 1968/69 | |
Toruń | 9 1978/79 | −0.53 |
Ustka | 10 2010/11 | 0.00 |
Warszawa | 19 1969/70, 1986/87 | |
Włodawa | 21 1978/79 | −0.48 |
Wrocław | 9 1978/79 | |
Zakopane | 4 1967/68 | −0.18 |
Zielona Góra | 9 1978/79 | −0.33 |