Articles | Volume 15, issue 14
Atmos. Chem. Phys., 15, 8401–8421, 2015
https://doi.org/10.5194/acp-15-8401-2015

Special issue: CHemistry and AeRosols Mediterranean EXperiments (ChArMEx)...

Atmos. Chem. Phys., 15, 8401–8421, 2015
https://doi.org/10.5194/acp-15-8401-2015
Research article
28 Jul 2015
Research article | 28 Jul 2015

Aerosol chemistry above an extended archipelago of the eastern Mediterranean basin during strong northern winds

E. Athanasopoulou et al.

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Cited articles

Anagnostopoulou, C., Zanis, P., Katragkou, E., Tegoulias, I., and Tolika, K.: Recent past and future patterns of the Etesian winds based on regional scale climate model simulations, Clim. Dynam., 42, 1819–1836, https://doi.org/10.1007/s00382-013-1936-0, 2014.
Astitha, M. and Kallos, C.: Gas-phase and aerosol chemistry interactions in South Europe and the Mediterranean región, Environ. Fluid Mech., 9, 3–22, https://doi.org/10.1007/s10652-008-9110-7, 2008.
Athanasopoulou, E., Tombrou, M., Pandis, S. N., and Russell, A. G.: The role of sea-salt emissions and heterogeneous chemistry in the air quality of polluted coastal areas, Atmos. Chem. Phys., 8, 5755–5769, https://doi.org/10.5194/acp-8-5755-2008, 2008.
Athanasopoulou, E., Tombrou, M., Russell, A. G., Karanasiou, A., Eleftheriadis, K., and Dandou, A.: Implementation of road and soil dust emission parameterizations in the aerosol model CAMx: Applications over the greater Athens urban area affected by natural sources, J. Geophys. Res.-Atmos., 115, D17301, https://doi.org/10.1029/2009JD013207, 2010.
Athanasopoulou, E., Vogel, H., Vogel, B., Tsimpidi, A. P., Pandis, S. N., Knote, C., and Fountoukis, C.: Modeling the meteorological and chemical effects of secondary organic aerosols during an EUCAARI campaign, Atmos. Chem. Phys., 13, 625–645, https://doi.org/10.5194/acp-13-625-2013, 2013.
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Short summary
A model system is evaluated versus ground and airborne aerosol measurements, towards the identification of its competencies and deficiencies over the eastern Mediterranean (EM) during summer. Secondary organic aerosol (OA) formation is investigated towards improving OA behaviour. Biomass burning is a significant particle source, largely explaining OA underestimation (ca. 50%). More than 70% of the aerosol mass over the EM is related to trans-boundary transport during strong northeastern winds.
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