Atmospheric Chemistry and Physics Discussions
www.atmos-chem-phys-discuss.net
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9
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2009
10.5194/acpd-9-5505-2009
http://www.atmos-chem-phys-discuss.net/9/5505/2009/
http://www.atmos-chem-phys-discuss.net/9/5505/2009/acpd-9-5505-2009.html
http://www.atmos-chem-phys-discuss.net/9/5505/2009/acpd-9-5505-2009.pdf
5505
5547
2009-03-02
Accurate satellite-derived estimates of the tropospheric ozone impact on the global radiation budget
J. Joiner
joanna.joiner@nasa.gov
M. R. Schoeberl
A. P. Vasilkov
L. Oreopoulos
S. Platnick
N. J. Livesey
P. F. Levelt
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Science Systems and Applications Inc., Lanham, MD, USA
Jet Propulsion Laboratory, Pasadena, CA, USA
Royal Netherlands Meteorological Institute (KNMI), de Bilt, The Netherlands
Estimates of the radiative forcing due to anthropogenically-produced
tropospheric O<sub>3</sub> are derived primarily from models. Here, we
use tropospheric ozone and cloud data from several instruments in the
A-train constellation of satellites as well as information from the
GEOS-5 Data Assimilation System to accurately estimate the radiative
effect of tropospheric O<sub>3</sub> for January and July 2005. Since we
cannot distinguish between natural and anthropogenic sources with the
satellite data, our derived radiative effect reflects the unadjusted
(instantaneous) effect of the total tropospheric O<sub>3</sub> rather
than the anthropogenic component. We improve upon previous estimates
of tropospheric ozone mixing ratios from a residual approach using the
NASA Earth Observing System (EOS) Aura Ozone Monitoring Instrument
(OMI) and Microwave Limb Sounder (MLS) by incorporating cloud pressure
information from OMI. We focus specifically on the magnitude and
spatial structure of the cloud effect on both the short- and long-wave
radiative budget. The estimates presented here can be used to evaluate
the various aspects of model-generated radiative forcing. For example,
our derived cloud impact is to reduce the radiative effect of
tropospheric ozone by ~16%. This is centered within the
published range of model-produced cloud effect on instantaneous
radiative forcing.
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