Articles | Volume 23, issue 24
https://doi.org/10.5194/acp-23-15589-2023
https://doi.org/10.5194/acp-23-15589-2023
Research article
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20 Dec 2023
Research article | Highlight paper |  | 20 Dec 2023

Drivers controlling black carbon temporal variability in the lower troposphere of the European Arctic

Stefania Gilardoni, Dominic Heslin-Rees, Mauro Mazzola, Vito Vitale, Michael Sprenger, and Radovan Krejci

Data sets

Equivalent black carbon from aerosol absorption coefficient M. Mazzola and S. Gilardoni https://data.iadc.cnr.it/erddap/tabledap/ebc_2010_2020.html

Climate Change Tower Meteorological Data A. P. Viola, M. Mazzola, and V. Vitale https://data.iadc.cnr.it/erddap/tabledap/cct_meteo_d2.html

EGUsphere-2023-1376 Equivalent Black Carbon Data S. Gilardoni https://data.iadc.cnr.it/erddap/tabledap/gilardoni_acp_ebc_2023.html

EGUsphere-2023-1376 Meteo Data S. Gilardoni https://data.iadc.cnr.it/erddap/tabledap/gilardoni_acp_met_2023.html

Video supplement

Drivers controlling black carbon variability in the Arctic S. Gilardoni https://doi.org/10.5446/63516

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Executive editor
Black carbon is a key source of uncertainty in regional climate predictions through aerosol-radiation interactions, cloud modifications and enhanced snow melt, and the arctic is particularly sensitive to these effects. Understanding the influence of continental emissions on arctic aerosols is crucial in earth system science, and this influence can be expected to evolve with changes to the atmospheric circulation in response to climate change. This paper uses a machine learning approach to study the factors controlling observations of black carbon in the arctic and quantitatively links these to meteorological processes and trends. This phenomenological assessment will facilitate predictions in the long range transport of black carbon transport under various climate change scenarios.
Short summary
Models still fail in reproducing black carbon (BC) temporal variability in the Arctic. Analysis of equivalent BC concentrations in the European Arctic shows that BC seasonal variability is modulated by the efficiency of removal by precipitation during transport towards high latitudes. Short-term variability is controlled by synoptic-scale circulation patterns. The advection of warm air from lower latitudes is an effective pollution transport pathway during summer.
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