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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 109,
D23201,
doi:10.1029/2004JD004735,
2004
Comparison of aerosol chemistry transport model simulations with lidar and Sun photometer observations at a site near Paris
A. Hodzic
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Palaiseau, France
H. Chepfer
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Palaiseau, France
R. Vautard
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Palaiseau, France
P. Chazette
Laboratoire des Sciences du Climat et de l'Environnement, Institut Pierre-Simon Laplace, Gif sur Yvette, France
M. Beekmann
Service d'Aéronomie, Institut Pierre-Simon Laplace, Paris, France
B. Bessagnet
Institut National de l'Environnement Industriel et des Risques, Verneuil en Halatte, France
B. Chatenet
Laboratoire Interuniversitaire des Systèmes Atmosphériques, Créteil, France
J. Cuesta
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Palaiseau, France
P. Drobinski
Service d'Aéronomie, Institut Pierre-Simon Laplace, Paris, France
P. Goloub
Laboratoire d'Optique Atmosphérique, Lille, France
M. Haeffelin
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Palaiseau, France
Y. Morille
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Palaiseau, France
Abstract
The ability of the aerosol chemistry transport model CHIMERE to simulate the vertical aerosol concentration profiles at a
site near the city of Paris is evaluated using routine elastic backscatter lidar and Sun photometer measurements. The comparisons
of model aerosols with measurements are carried out over a full year time period between October 2002 and September 2003.
The methodology we propose here is new: From the model concentration outputs (optical properties varying with chemical composition
and mass vertical distribution) we simulate the lidar backscattering profiles and compare them with the observed ones. The
comparisons demonstrate the ability of the model to reproduce correctly the aerosol vertical distributions and their temporal
variability. However, the aerosol load within the boundary layer is generally underestimated by the model, in particular during
the afternoon hours and the summertime period. Several sensitivity tests indicate that this underestimation may have two origins:
the lack of secondary organic and, to a lesser extent, mineral aerosols inside the model. The second deficiency is due to
the absence of erosion/resuspension of soil material in the primary aerosol sources considered here; the first deficiency
is probably due to incomplete knowledge about the formation of organic species in a photochemically active atmosphere. The
results also show that the particles ranging from 0.08 to 1.25 μm in radius represent more than 89% of the volume backscattering
at 532 nm, while the coarse particles are not efficient in terms of optical properties. The missing aerosol mass must therefore
be found within the accumulation mode.
Received 4
March
2004;
accepted 29
June
2004;
published 1
December
2004.
Keywords: aerosol modeling;
aerosol optical properties;
lidar profile;
model validation;
vertical distribution of aerosols.
Index Terms: 0305 Atmospheric Composition and Structure: Aerosols and particles (0345, 4801); 0345 Atmospheric Composition and Structure: Pollution—urban and regional (0305); 0394 Atmospheric Composition and Structure: Instruments and techniques.
Read Full Article (file size: 871886 bytes) Cited by
Citation: Hodzic, A., et al.
(2004),
Comparison of aerosol chemistry transport model simulations with lidar and Sun photometer observations at a site near Paris,
J. Geophys. Res.,
109,
D23201,
doi:10.1029/2004JD004735.
Copyright 2004 by the American Geophysical Union.
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