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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 108, NO. D8,
8372,
doi:10.1029/2002JD002665,
2003
Budget of tropospheric ozone during TOPSE from two chemical transport models
L. K. Emmons
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
P. Hess
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
A. Klonecki
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
X. Tie
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
L. Horowitz
Geophysical Fluid Dynamics Laboratory, National Oceanic and Atmospheric Administration,
Princeton,
New Jersey,
USA
J.-F. Lamarque
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
D. Kinnison
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
G. Brasseur
Max Planck Institute for Meteorology,
Hamburg,
Germany
E. Atlas
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
E. Browell
Atmospheric Sciences,
NASA Langley Research Center,
Hampton,
Virginia,
USA
C. Cantrell
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
F. Eisele
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
R. L. Mauldin
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
J. Merrill
Graduate School of Oceanography, Center for Atmospheric Chemistry Studies,
University of Rhode Island,
Narragansett,
Rhode Island,
USA
B. Ridley
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
R. Shetter
Atmospheric Chemistry Division, National Center for Atmospheric Research,
Boulder,
Colorado,
USA
Abstract
The tropospheric ozone budget during the Tropospheric Ozone Production about the Spring Equinox (TOPSE) campaign has been
studied using two chemical transport models (CTMs): HANK and the Model of Ozone and Related chemical Tracers, version 2 (MOZART-2).
The two models have similar chemical schemes but use different meteorological fields, with HANK using MM5 (Pennsylvania State
University, National Center for Atmospheric Research Mesoscale Modeling System) and MOZART-2 driven by European Centre for
Medium-Range Weather Forecasts (ECMWF) fields. Both models simulate ozone in good agreement with the observations but underestimate
NOx. The models indicate that in the troposphere, averaged over the northern middle and high latitudes, chemical production of
ozone drives the increase of ozone seen in the spring. Both ozone gross chemical production and loss increase greatly over
the spring months. The in situ production is much larger than the net stratospheric input, and the deposition and horizontal
fluxes are relatively small in comparison to chemical destruction. The net production depends sensitively on the concentrations
of H2O, HO2 and NO, which differ slightly in the two models. Both models underestimate the chemical production calculated in a steady
state model using TOPSE measurements, but the chemical loss rates agree well. Measures of the stratospheric influence on tropospheric
ozone in relation to in situ ozone production are discussed. Two different estimates of the stratospheric fraction of O3 in the Northern Hemisphere troposphere indicate it decreases from 30–50% in February to 15–30% in June. A sensitivity study
of the effect of a perturbation in the vertical flux on tropospheric ozone indicates the contribution from the stratosphere
is approximately 15%.
Published 26
April
2003.
Index Terms: 0368 Atmospheric Composition and Structure: Troposphere—constituent transport and chemistry; 0365 Atmospheric Composition and Structure: Troposphere—composition and chemistry; 0322 Atmospheric Composition and Structure: Constituent sources and sinks.
Read Full Article (file size: 13456660 bytes) Cited by
Citation: Emmons, L. K., et al.
(2003),
Budget of tropospheric ozone during TOPSE from two chemical transport models,
J. Geophys. Res.,
108(D8),
8372,
doi:10.1029/2002JD002665.
Copyright 2003 by the American Geophysical Union.
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