EGU22-10292
https://doi.org/10.5194/egusphere-egu22-10292
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

How do the local meteorology and turbulence influence the nitrogen dioxide concentration in Madrid?

Carlos Yagüe1, Carlos Román-Cascón1, Pablo Ortiz1, Mariano Sastre1, Gregorio Maqueda1, Encarna Serrano1, Begoña Artíñano2, Francisco Javier Gómez-Moreno2, Elías Díaz-Ramiro2, Elisabeth Alonso2, Javier Fernández2, Rafael Borge3, Adolfo Narros3, José María Cordero3, Ana María García4, and Andrés Núñez4
Carlos Yagüe et al.
  • 1Departamento de Física de la Tierra y Astrofísica. Universidad Complutense de Madrid. 28040 Madrid, Spain (carlos@ucm.es)
  • 2Department of Environment, CIEMAT, 28040 Madrid, Spain
  • 3Department of Chemical and Environmental Engineering, Technical University of Madrid (UPM), 28006 Madrid, Spain
  • 4Department of Applied Physics and Material Engineering. Technical University of Madrid (UPM), 28006 Madrid, Spain

The pollutant concentration close to the surface at specific sites of a city depends on multiple factors. However, disentangling the relative importance of them using observational data is not an easy task. To deepen into these relationships, in this study we use intensive and multiple data from several urban field campaigns that were developed in the city of Madrid (Spain) during 2020 and 2021 under the framework of the AIRTEC-CM (*) research project (Urban Air Quality and Climate Change Integral Assessment).
Among the most typical pollutants in cities, the nitrogen dioxide (NO2) is of crucial importance due to its negative impacts on human health. The diurnal cycle of this pollutant is closely related to the anthropogenic emissions in the area and to the local meteorology, as well as to the turbulent transfers in the atmospheric boundary layer. In this work, we analyse the relation between the NOconcentration and different meteorological variables, including some turbulent parameters calculated from sonic anemometers: turbulent kinetic energy (TKE) and friction velocity (U*). In this sense, we have distinguished those situations where the turbulent parameters are more valuable (have better correlation) than the wind speed, which is the meteorological variable typically used to be correlated with the pollutant concentration.
The analysis of the data clearly reveals how the highest NO2 concentrations are associated with fair-weather (stable) synoptic conditions, as it is already known and expected. However, the detailed analysis of the diurnal cycle in these periods also highlights how the stability favours the appearance of mesoscale diurnal winds (mountain breezes) in the city, increasing the turbulence close to the surface and favouring the pollutants dispersion. This is of key importance because in some cases these processes are not correctly simulated by numerical models, which could lead to wrong predictions (overestimation) of the pollutant’s concentrations at specific hours. Specifically, the evening transition and the following hours during stable conditions are the most difficult periods, displaying the highest and quicker variability in NO2 concentration: very high concentration during calm periods in the transition followed by a rapid cleaning of the air a few hours later due to the breeze appearance.

 

(*) AIRTEC-CM research project (S2018/EMT-4329) is funded by The Regional Government of Madrid (Spain).

How to cite: Yagüe, C., Román-Cascón, C., Ortiz, P., Sastre, M., Maqueda, G., Serrano, E., Artíñano, B., Gómez-Moreno, F. J., Díaz-Ramiro, E., Alonso, E., Fernández, J., Borge, R., Narros, A., Cordero, J. M., García, A. M., and Núñez, A.: How do the local meteorology and turbulence influence the nitrogen dioxide concentration in Madrid?, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-10292, https://doi.org/10.5194/egusphere-egu22-10292, 2022.