Articles | Volume 21, issue 15
https://doi.org/10.5194/acp-21-12113-2021
https://doi.org/10.5194/acp-21-12113-2021
Measurement report
 | 
13 Aug 2021
Measurement report |  | 13 Aug 2021

Measurement report: Effect of wind shear on PM10 concentration vertical structure in the urban boundary layer in a complex terrain

Piotr Sekuła, Anita Bokwa, Jakub Bartyzel, Bogdan Bochenek, Łukasz Chmura, Michał Gałkowski, and Mirosław Zimnoch

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Cited articles

ACCORD: A Consortium for COnvection-scale modelling Research and Development, Meteorological model ALADIN, available at: http://www.umr-cnrm.fr/accord, last access: 21 April 2021. 
Benard, P., Vivoda, J., Masek, J., Smolikova, P., Yessad, K., Smith, C., Brozkova, R., and Geleyn, J. F.: Dynamical kernel of the Aladin-NH spectral limited-area model: Revised formulation and sensitivity experiments, Q. J. Roy. Meteor. Soc., 136, 155–169, https://doi.org/10.1002/qj.522, 2010. 
Bochenek, B. Sekuła, P., Jerczyński, M., Kolonko, M., Szczęch-Gajewska, M., Woyciechowska, J., and Stachura, G.: ALADIN in Poland, 30th ALADIN Wk and HIRLAM ASM 2020, Ljubljana, Slovenia,available at: http://www.umr-cnrm.fr/aladin/IMG/pdf/poster_poland.pdf (last access: 21 April 2021), 30 March–3 April 2020. 
Bokwa, A.: Miejska wyspa ciepła na tle naturalnego zróżnicowania termicznego obszaru położonego we wklęsłej formie terenu (na przykładzie Krakowa) [Urban heat island against the background of natural thermal diversity of the area located in a concave terrain (on the example of Kraków city)], Prace Geograficzne IGiGP UJ, 122, 111–132, 2009. 
Bokwa, A.: Wieloletnie zmiany struktury mezoklimatu miasta na przykładzie Krakowa [Long-term changes in the structure mesoclimate of the city on the example of Kraków city], IGiGP UJ, Kraków, 296 pp., 2010. 
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Short summary
The wind shear generated on a local scale by the diversified relief’s impact can be a factor which significantly modifies the spatial pattern of PM10 concentration. The vertical profile of PM10 over a city located in a large valley during the events with high surface-level PM10 concentrations may show a sudden decrease with height not only due to the increase in wind speed, but also due to the change in wind direction alone. Vertical aerosanitary urban zones can be distinguished.
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