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@ARTICLE{SchroedterHomscheidt:17059,
author = {Schroedter-Homscheidt, M. and Elbern, H. and Holzer-Popp,
T.},
title = {{O}bservation operator for the assimilation of aerosol type
resolving satellite measurements into a chemical transport
model},
journal = {Atmospheric chemistry and physics},
volume = {10},
issn = {1680-7316},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {PreJuSER-17059},
pages = {10435 - 10452},
year = {2010},
note = {Record converted from VDB: 12.11.2012},
abstract = {Modelling of aerosol particles with chemical transport
models is still based mainly on static emission databases
while episodic emissions cannot be treated sufficiently. To
overcome this situation, a coupling of chemical mass
concentration modelling with satellite-based measurements
relying on physical and optical principles has been
developed. This study deals with the observation operator
for a component-wise assimilation of satellite measurements.
It treats aerosol particles classified into water soluble,
water insoluble, soot, sea salt and mineral dust containing
aerosol particles in the atmospheric boundary layer as
separately assimilated aerosol components. It builds on a
mapping of aerosol classes used both in observation and
model space taking their optical and chemical properties
into account. Refractive indices for primary organic carbon
particles, anthropogenic particles, and secondary organic
species have been defined based on a literature review.
Together with a treatment of different size distributions in
observations and model state, this allows transforming the
background from mass concentrations into aerosol optical
depths. A two-dimensional, variational assimilation is
applied for component-wise aerosol optical depths. Error
covariance matrices are defined based on a validation
against AERONET sun photometer measurements. Analysis fields
are assessed threefold: (1) through validation against
AERONET especially in Saharan dust outbreak situations, (2)
through comparison with the British Black Smoke and Sulphur
Dioxide Network for soot-containing particles, and (3)
through comparison with measurements of the water soluble
components SO4, NH4, and NO3 conducted by the EMEP (European
Monitoring and Evaluation Programme) network. Separately,
for the water soluble, the soot and the mineral dust aerosol
components a bias reduction and subsequent a root mean
square error reduction is observed in the analysis for a
test period from July to November 2003. Additionally,
examples of an improved analysis during wildfire and dust
outbreak situations are shown.},
keywords = {J (WoSType)},
cin = {IEK-8},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000284210400018},
doi = {10.5194/acp-10-10435-2010},
url = {https://juser.fz-juelich.de/record/17059},
}