Evangeliou+et+al_Atmos+Chem+Phys_2018.pdf (8.357Mb)

Using prior as well as posterior emissions, the simulated BC concentrations were compared to observed concentrations at all inversion and independent sites, and ECLIPSEv6 stood

BC concentrations from MERRA-2 (left axis) since 2015 in the most highly affected European 25. countries (France, Italy, Germany, Spain and UK), Scandinavia and Europe from

The Bayesian inversion framework FLEXINVERT + de- scribed in detail in Thompson and Stohl (2014) was used to optimize emissions of BC before (January to mid- March 2020) and during

Change in daily maximum near-surface ozone (ppbv) due to forest fire emissions (REF-NF and GF-NF) calculated by WRF-Chem using FINN emissions (left), WRF-Chem using GFED

Sensitivity of posterior total emissions to (a) different prior emissions (six different previously published assessments), (b) using different injection altitudes in the prior

The error bars show the calculated observation uncertainty used in the inversions (observations = black, background = green, S1 prior.. = blue, S1 posterior

As an example of the importance of northern hemispheric biomass burning emissions for the air over Greenland, we present time series of surface BC concentrations in north-

Seasonality of aerosol optical properties – includ- ing the aerosol light-scattering coefficient, absorption coef- ficient, single-scattering albedo, scattering Ångström expo- nent,