Uneingeschränkter Zugang

The Role of Increased Sunshine in Shaping Air Temperature Rise in Kraków (1951–2020)

Andrzej A. Marsz

Andrzej A. Marsz

Polish Geophysical Society, Baltic BranchGdynia, Poland
Orcid-Profil
Suche nach diesem Autor auf
Sciendo|Google Scholar
Marsz, Andrzej A.
, 
Dorota Matuszko

Dorota Matuszko

Institute of Geography and Spatial Management, Jagiellonian UniversityKraków, Poland
Orcid-Profil
Suche nach diesem Autor auf
Sciendo|Google Scholar
Matuszko, Dorota
 und 
Anna Styszyńska

Anna Styszyńska

Association of Polish ClimatologistsWarszawa, Poland
Orcid-Profil
Suche nach diesem Autor auf
Sciendo|Google Scholar
Styszyńska, Anna
  
28. Juli 2025
The Role of Increased Sunshine in Shaping Air Temperature Rise in Kraków (1951–2020)'s Cover Image
Über diesen Artikel
Vorheriger Artikel
Nächster Artikel
Zitieren
COVER HERUNTERLADEN
Online veröffentlicht: 28. Juli 2025
Eingereicht: 04. März 2025
DOI: https://doi.org/10.14746/quageo-2025-0024
Schlüsselwörter
© 2025 Andrzej A. Marsz et al., published by Sciendo
This work is licensed under the Creative Commons Attribution 4.0 International License.

Fig. 1.

Course of average annual air temperature (°C) and annual totals of sunshine duration (SD in hours) in Kraków (1951–2020).
Course of average annual air temperature (°C) and annual totals of sunshine duration (SD in hours) in Kraków (1951–2020).

Fig. 2.

Ranges of variability of annual air temperature (°C) and annual sums of sunshine duration (SD in hours) in Kraków in the years 1951–1988 and 1988–2020.
Ranges of variability of annual air temperature (°C) and annual sums of sunshine duration (SD in hours) in Kraków in the years 1951–1988 and 1988–2020.

Fig. 3.

Course of annual cloudiness values (oktas) in Kraków in the period 1951–2020, and ranges of its variability in periods 1951–1988 and 1988–2020.
Course of annual cloudiness values (oktas) in Kraków in the period 1951–2020, and ranges of its variability in periods 1951–1988 and 1988–2020.

Fig. 4.

Ranges of variability in the number of days with observations of frontal clouds (As, Ns, St) and clouds occurring in unstable weather conditions in Kraków during the periods 1951–1988 and 1988–2020.
Ranges of variability in the number of days with observations of frontal clouds (As, Ns, St) and clouds occurring in unstable weather conditions in Kraków during the periods 1951–1988 and 1988–2020.

Fig. 5.

The course of the observed mean annual air temperature (°C) in Kraków (Obs) and the estimated air temperature based on sunshine duration (est) from 1951 to 2020. The trend values are marked in boxes (with the standard error of estimation values in parentheses).
The course of the observed mean annual air temperature (°C) in Kraków (Obs) and the estimated air temperature based on sunshine duration (est) from 1951 to 2020. The trend values are marked in boxes (with the standard error of estimation values in parentheses).

Fig. 6.

The course of the North Atlantic Oscillation principal components (NAO PC) DJFM Hurrell index from 1951 to 2020 and the ranges of its variability in the periods 1951–1988 and 1988–2020.
The course of the North Atlantic Oscillation principal components (NAO PC) DJFM Hurrell index from 1951 to 2020 and the ranges of its variability in the periods 1951–1988 and 1988–2020.

Fig. 7.

Course of the observed mean annual air temperature (°C) in Kraków (Obs) and the estimated (est) from the course of two variables: sunshine duration (SD) and North Atlantic Oscillation (NAO) in the years 1951–2020. The trend values are marked in the boxes (with standard error of estimation values in parentheses).
Course of the observed mean annual air temperature (°C) in Kraków (Obs) and the estimated (est) from the course of two variables: sunshine duration (SD) and North Atlantic Oscillation (NAO) in the years 1951–2020. The trend values are marked in the boxes (with standard error of estimation values in parentheses).

Fig. 8.

Course of the observed mean annual air temperature (°C) in Kraków (Obs) and the estimated (Est) from the course of radiative forcing in the years 1951–2020.
Course of the observed mean annual air temperature (°C) in Kraków (Obs) and the estimated (Est) from the course of radiative forcing in the years 1951–2020.

Fig. 9.

The course of the observed annual average air temperature (°C) in Kraków (Obs) and the estimated (est) temperature based on the course of three variables: sunshine duration (SD), North Atlantic Oscillation (NAO), and △F from 1951 to 2020.
The course of the observed annual average air temperature (°C) in Kraków (Obs) and the estimated (est) temperature based on the course of three variables: sunshine duration (SD), North Atlantic Oscillation (NAO), and △F from 1951 to 2020.

Fig. 10.

Course of the observed average annual air temperature (°C) in Kraków (Obs) and the estimated temperature (Est) based on the course of two variables sunshine duration (SD) and North Atlantic Oscillation (NAO) and three variables (SD, NAO, and △F) in the years 1951–2020. Trend lines are marked. The differences between the observed temperature trend and the estimated temperature trend based on three variables are so small (0.001°C · year−1) that they overlap in the graphical representation
Course of the observed average annual air temperature (°C) in Kraków (Obs) and the estimated temperature (Est) based on the course of two variables sunshine duration (SD) and North Atlantic Oscillation (NAO) and three variables (SD, NAO, and △F) in the years 1951–2020. Trend lines are marked. The differences between the observed temperature trend and the estimated temperature trend based on three variables are so small (0.001°C · year−1) that they overlap in the graphical representation

Correlation coefficients (r) and their statistical significance (p) between monthly and annual air temperature and the annual sunshine duration (SD) in Kraków, the North Atlantic Oscillation PC DJFM Hurrell index (NAO), and radiative forcing (△F) during the years 1951–2020 (bold values are significant in level p < 0_05)_

Month SD NAO ΔF
R p r p r p
I 0.35 0.003 0.51 0.000 0.24 0.045
II 0.22 0.074 0.40 0.001 0.28 0.020
III 0.26 0.027 0.54 0.000 0.33 0.006
IV 0.51 0.000 0.24 0.043 0.43 0.000
V 0.29 0.014 0.07 0.593 0.36 0.002
VI 0.63 0.000 0.13 0.292 0.45 0.000
VII 0.59 0.000 0.19 0.112 0.45 0.000
VIII 0.68 0.000 0.28 0.019 0.55 0.000
IX 0.49 0.000 0.18 0.130 0.21 0.074
X 0.16 0.187 0.08 0.526 0.16 0.175
XI 0.29 0.014 –0.16 0.176 0.20 0.105
XII 0.25 0.036 0.18 0.145 0.17 0.154
year 0.76 0.000 0.54 0.000 0.64 0.000

Correlation coefficients (r) and their statistical significance (p) between the annual frequency of cloud types and annual sunshine duration (SD), average annual air temperature (T), and cloudiness (N) in Kraków in the years 1951–2020 (bold values are significant in level p < 0_05)_

Element Cloud genera Cloudless sky
Ci Cc Cs Ac As Ns Sc St Cu Cb
SD r 0.61 0.62 0.10 0.01 –0.45 –0.37 0.25 –0.41 0.59 0.14 –0.03
p 0.000 0.000 0.395 0.942 0.000 0.002 0.040 0.000 0.000 0.264 0.800
T r 0.49 0.40 0.01 0.08 –0.53 –0.46 0.38 –0.55 0.52 0.30 –0.17
p 0.000 0.001 0.913 0.491 0.000 0.000 0.001 0.000 0.000 0.012 0.149
N r –0.02 0.16 0.48 0.01 0.58 0.60 –0.09 0.64 –0.04 –0.48 –0.52
p 0.851 0.190 0.000 0.966 0.000 0.000 0.456 0.000 0.735 0.000 0.000
Sprache:
Englisch
Zeitrahmen der Veröffentlichung:
4 Hefte pro Jahr
Fachgebiete der Zeitschrift:
Geowissenschaften, Geografie
Zeitschrift RSS Feed