Global aerosol modeling with MADE3 (v3.0) in EMAC (based on v2.53): model description and evaluation
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Published:2019-02-01
Issue:1
Volume:12
Page:541-579
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ISSN:1991-9603
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Container-title:Geoscientific Model Development
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language:en
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Short-container-title:Geosci. Model Dev.
Author:
Kaiser J. Christopher, Hendricks Johannes, Righi MattiaORCID, Jöckel PatrickORCID, Tost HolgerORCID, Kandler Konrad, Weinzierl BernadettORCID, Sauer DanielORCID, Heimerl Katharina, Schwarz Joshua P.ORCID, Perring Anne E., Popp Thomas
Abstract
Abstract. Recently, the aerosol microphysics submodel MADE3 (Modal Aerosol Dynamics
model for Europe, adapted for global applications, third generation) was
introduced as a successor to MADE and MADE-in. It includes nine aerosol
species and nine lognormal modes to represent aerosol particles of three
different mixing states throughout the aerosol size spectrum. Here, we
describe the implementation of the most recent version of MADE3 into the
ECHAM/MESSy Atmospheric Chemistry (EMAC) general circulation model, including
a detailed evaluation of a 10-year aerosol simulation with MADE3 as part of
EMAC. We compare simulation output to station network measurements of near-surface
aerosol component mass concentrations, to airborne measurements of aerosol
mass mixing ratio and number concentration vertical profiles, to ground-based
and airborne measurements of particle size distributions, and to station
network and satellite measurements of aerosol optical depth. Furthermore, we
describe and apply a new evaluation method, which allows a comparison of model
output to size-resolved electron microscopy measurements of particle
composition. Although there are indications that fine-mode particle deposition
may be underestimated by the model, we obtained satisfactory agreement with
the observations. Remaining deviations are of similar size to those identified
in other global aerosol model studies. Thus, MADE3 can be considered ready for application within EMAC. Due to its
detailed representation of aerosol mixing state, it is especially useful for
simulating wet and dry removal of aerosol particles, aerosol-induced
formation of cloud droplets and ice crystals as well as aerosol–radiation
interactions. Besides studies on these fundamental processes, we also plan to
use MADE3 for a reassessment of the climate effects of anthropogenic aerosol
perturbations.
Publisher
Copernicus GmbH
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