Articles | Volume 26, issue 17
https://doi.org/10.5194/acp-26-12729-2026
https://doi.org/10.5194/acp-26-12729-2026
Research article
 | 
09 Sep 2026
Research article |  | 09 Sep 2026

Numerical study of a Saharan dust plume impact on radiation, urban climate and thermal comfort in the Paris region during an heatwave event

Jérémy Bernard, Tim Nagel, Valéry Masson, Aude Lemonsu, Jean Wurtz, Pierre Tulet, and Quentin Rodier

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Cited articles

Bangert, M., Nenes, A., Vogel, B., Vogel, H., Barahona, D., Karydis, V. A., Kumar, P., Kottmeier, C., and Blahak, U.: Saharan dust event impacts on cloud formation and radiation over Western Europe, Atmos. Chem. Phys., 12, 4045–4063, https://doi.org/10.5194/acp-12-4045-2012, 2012. a
Basart, S., Nickovic, S., Terradellas, E., Cuevas, E., García-Pando, C. P., García-Castrillo, G., Werner, E., and Benincasa, F.: The WMO SDS-WAS Regional Center for Northern Africa, Middle East and Europe, E3S Web of Conferences, 99, 04008, https://doi.org/10.1051/e3sconf/20199904008, 2019. a
Bernstein, D. N., Neelin, J. D., Li, Q. B., and Chen, D.: Could aerosol emissions be used for regional heat wave mitigation?, Atmos. Chem. Phys., 13, 6373–6390, https://doi.org/10.5194/acp-13-6373-2013, 2013. a
Boone, A., Samuelsson, P., Gollvik, S., Napoly, A., Jarlan, L., Brun, E., and Decharme, B.: The interactions between soil–biosphere–atmosphere land surface model with a multi-energy balance (ISBA-MEB) option in SURFEXv8 – Part 1: Model description, Geosci. Model Dev., 10, 843–872, https://doi.org/10.5194/gmd-10-843-2017, 2017. a
Bröde, P., Fiala, D., Błażejczyk, K., Holmér, I., Jendritzky, G., Kampmann, B., Tinz, B., and Havenith, G.: Deriving the operational procedure for the Universal Thermal Climate Index (UTCI), Int. J. Biometeorol., 56, 481–494, https://doi.org/10.1007/s00484-011-0454-1, 2012. a, b
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Short summary
Cities are particularly vulnerable to heat-waves because of their dense population combined with an amplification of the heat hazard caused by the urban heat island phenomenon. Heat event are sometimes associated with aerosol plume in the atmosphere, which affect the thermal comfort. This study shows that aerosol plumes can result in a heat stress reduction of up to 1 °C in sunny areas in cities while no difference in the shade of suburban areas.
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