Atmospheric composition in the Eastern Mediterranean

Influence of biomass burning during summertime using the WRF-Chem model

Journal article (2016)

Authors

E. Bossioli National Technical University of Athens

M. Tombrou National Technical University of Athens

Nikolaos Mihalopoulos University of Crete

C. J. Percival The University of Manchester

J. Kalogiros National Observatory of Athens

J. Allan The University of Manchester

A. Bacak The University of Manchester

S. Bezantakos The Cyprus Institute

G. Biskos Atmospheric Remote Sensing - , The Cyprus Institute, Energy Environment and Water Research Center

H. Coe The University of Manchester

B. T. Jones The University of Manchester

G. Kouvarakis University of Crete

Research Group

Atmospheric Remote Sensing () (TU Delft)

Aerosols Eastern Mediterranean Gases Biomass burning WRF-Chem Biogenic emissions

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Published Date

01-05-2016

Language

English

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Faculty

Civil Engineering & Geosciences

Department

Geoscience and Remote Sensing

Research Group

Atmospheric Remote Sensing

Abstract

The composition of the atmosphere over the Aegean Sea (AS) during an 'Etesian' outbreak under the influence of biomass burning (BB) activity is investigated. Simulations with the fully coupled WRF-Chem model during the Aegean-GAME campaign (29/8-9/9/2011) are used to examine the BB effect over the region. Two distinct Etesian flow patterns characterized by different transport conditions are analysed. The influence of the off-line calculated BB emissions on the atmospheric chemical composition over the AS under these conditions is estimated. In addition, sensitivity runs are used to examine the influence of the biogenic emissions calculated on-line and the realistic representation of the stratosphere-troposphere exchange processes are investigated through the time-varying chemical boundary conditions from the MOZART global chemical transport model. The horizontal and vertical distributions of gaseous and aerosol species are simulated under long-range transport conditions and interpreted in relation to the evolution of the Planetary Boundary Layer (PBL). In the case of a weaker synoptic system (medium-range transport conditions), even a small variability of meteorological parameters in limited areas become critical for the spatial distribution of gases and aerosols. The BB activity increases O₃, PM_2.5 and organic matter concentrations up to 5.5 ppb, 5.8 μg m^-3 and 3.3 μg m^-3, respectively. The spatial extent of the simulated BB plumes is further examined by comparison with airborne measurements of hydrogen cyanide (HCN). The estimated effect of biogenic emissions on O₃ and PM_2.5 concentrations is either positive or negative (±6 ppb for O₃ and up to ± 1 μg m^-3 for PM_2.5) depending on the emission algorithm employed. The realistic representation of the chemical boundary conditions reproduces an observed layer rich in O₃ above 4 km, but also increases O₃ concentrations inside the PBL by up to 40%.