EGU25-3488, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-3488
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 01 May, 10:45–12:30 (CEST), Display time Thursday, 01 May, 08:30–12:30
 
Hall X5, X5.94
Environmental factors affecting fog formation
Iva Hunova1,2, Marek Brabec3,4, Marek Malý3,4, Jan Geletič3, Alexandru Dumitrescu5, and Anna Valeriánová1
Iva Hunova et al.
  • 1Czech Hydrometeorological Institute, Ambient Air Quality Department, Prague, Czech Republic (iva.hunova@chmi.cz)
  • 2Charles University, Prague, Czech Republic
  • 3Institute of Computer Science, Academy of Sciences of the Czech Republic, Prague, Czech Republic
  • 4National Institute of Public Health, Prague, Czech Republic
  • 5Meteo Romania (National Meteorological Administration), Bucharest, Romania

Fog is an important phenomenon related to both atmospheric physics and chemistry, and has a significant impact on our environment. Although the meteorological factors relevant to fog formation have been extensively studied, other factors remain unexplored. Here we summarise our recent results from several studies (Hůnová et al., 2018, 2021 a, 2021 b, 2022), where we examined observed and measured long-term data from the Czech Republic (1989–2015) and Romania (1981–2017). Our focus was on the environmental factors that drive fog formation. Specifically, we examined the effects of terrain, water and forests (for Romania), and ambient air pollution (for the Czech Republic). The long-term empirical data   were analysed using advanced statistical modelling GAM (generalised additive model). In terms of terrain, apart from altitude, slope and landform appeared to have a strong influence on fog formation. Forests have a significant effect on fog formation, the most significant being the forest area within 3 km of the the fog observation point, with coniferous and broad leave trees having different effects. Not surprisingly, the presence of water body in the vicinity of a fog site affects fog formation, but less so than altitude or seasonality. Freshwater and seawater show clear differences in both the seasonal profile and frequency of fog. Ambient air pollution, indicated by the daily mean concentrations of  sulphur dioxide and nitrogen oxides, was the most important explanatory variable (apart from relative humidity) in modelling the probability of fog at three Centre European sites reflecting different environments (urban, rural and mountain).

References:

Hůnová I., Brabec M., Geletič J., Malý M., Dumitrescu A., 2021 a. Statistical analysis of the effects of forests on fog. STOTEN, https://doi.org/10.1016/j.scitotenv.2021.146675.

Hůnová I., Brabec M., Geletič J., Malý M., Dumitrescu A., 2022. Local fresh- and sea-water effects on fog occurrence. STOTEN, https://doi.org/10.1016/j.scitotenv.2021.150799.

Hůnová I., Brabec M., Malý M., Dumitrescu A., Geletič J., 2021 b. Terrain and its effects on fog occurrence. STOTEN, https://doi.org/10.1016/j.scitotenv.2020.144359.

Hůnová I., Brabec M., Malý M., Valeriánová A., 2018. Revisiting fog as an important constituent of the atmosphere.  STOTEN, https://doi.org/10.1016/j.scitotenv.2018.04.322.

 

Acknowledgements:

We are grateful to the Czech Hydrometeorological Institute and Meteo Romania for providing the input data. Our study was supported by the Technological Agency of the Czech Republic (TAČR) through the project SS02030031 ARAMIS, by the Czech Hydrometeorological Institute research project ʽDlouhodobá koncepce rozvoje výzkumné organizace (DKRVO) Český hydrometeorologický ústav’ financed by the Czech Ministry of the Environment, and by the long-term strategic development financing of the Institute of Computer Science (Czech Republic RVO 67985807).

How to cite: Hunova, I., Brabec, M., Malý, M., Geletič, J., Dumitrescu, A., and Valeriánová, A.: Environmental factors affecting fog formation, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-3488, https://doi.org/10.5194/egusphere-egu25-3488, 2025.