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Read Full Article (file size: 1836275 bytes) Cited by
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 113,
D16S32,
doi:10.1029/2007JD008863,
2008
Assimilated ozone from EOS-Aura: Evaluation of the tropopause region and tropospheric columns
Ivanka Stajner
Science Applications International Corporation, Beltsville, Maryland, USA Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Krzysztof Wargan
Science Applications International Corporation, Beltsville, Maryland, USA Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Steven Pawson
Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Hiroo Hayashi
Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA Goddard Earth Sciences and Technology Center, University of Maryland, Baltimore County, Baltimore, Maryland, USA
Lang-Ping Chang
Science Applications International Corporation, Beltsville, Maryland, USA Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Rynda C. Hudman
Atmospheric Chemistry Modeling Group, Harvard University, Cambridge, Massachusetts, USA
Lucien Froidevaux
Jet Propulsion Laboratory, Pasadena, California, USA
Nathaniel Livesey
Jet Propulsion Laboratory, Pasadena, California, USA
Pieternel F. Levelt
Royal Dutch Meteorological Institute, De Bilt, Netherlands
Anne M. Thompson
Department of Meteorology, Pennsylvania State University, University Park, Pennsylvania, USA
David W. Tarasick
Air Quality Research Division, Environment Canada, Downsview, Ontario, Canada
René Stübi
Aerological Station Payerne, MeteoSwiss, Payerne, Switzerland
Signe Bech Andersen
Danish Meteorological Institute, Copenhagen, Denmark
Margarita Yela
Instituto Nacional de Tecnica Aeroespacial, Madrid, Spain
Gert König-Langlo
Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
F. J. Schmidlin
NASA GSFC, Wallops Flight Facility, Wallops Island, Virginia, USA
Jacquelyn C. Witte
Science Systems and Applications Inc., Lanham, Maryland, USA
Abstract
Retrievals from the Microwave Limb Sounder (MLS) and the Ozone Monitoring Instrument (OMI) on EOS-Aura were included in the
Goddard Earth Observing System version 4 (GEOS-4) ozone data assimilation system. The distribution and daily to seasonal evolution
of ozone in the stratosphere and troposphere during 2005 are investigated. In the lower stratosphere, where dynamical processes
dominate, comparisons with independent ozonesonde and Measurement of Ozone and Water Vapour by Airbus In-Service Aircraft
(MOZAIC) data indicate mean agreement within 10%. In the troposphere, OMI and MLS provide constraints on the ozone column,
but the ozone profile shape results from the parameterized ozone chemistry and the resolved and parameterized transport. Assimilation
of OMI and MLS data improves tropospheric column estimates in the Atlantic region but leads to an overestimation in the tropical
Pacific and an underestimation in the northern high and middle latitudes in winter and spring. Transport and data biases are
considered in order to understand these discrepancies. Comparisons of assimilated tropospheric ozone columns with ozonesonde
data reveal root-mean-square (RMS) differences of 2.9–7.2 Dobson units (DU), which are smaller than the model-sonde RMS differences
of 3.2–8.7 DU. Four different definitions of the tropopause using temperature lapse rate, potential vorticity (PV), and isentropic
surfaces or ozone isosurfaces are compared with respect to their global impact on the estimated tropospheric ozone column.
The largest sensitivity in the tropospheric ozone column is found near the subtropical jet, where the ozone- or PV-determined
tropopause typically lies below the lapse rate tropopause.
Received 20
April
2007;
accepted 17
January
2008;
published 29
May
2008.
Keywords: ozone assimilation;
lower stratosphere;
troposphere.
Index Terms: 3315 Atmospheric Processes: Data assimilation; 3334 Atmospheric Processes: Middle atmosphere dynamics (0341, 0342); 3360 Atmospheric Processes: Remote sensing; 3362 Atmospheric Processes: Stratosphere/troposphere interactions; 0368 Atmospheric Composition and Structure: Troposphere: constituent transport and chemistry.
Read Full Article (file size: 1836275 bytes) Cited by
Citation: Stajner, I., et al.
(2008),
Assimilated ozone from EOS-Aura: Evaluation of the tropopause region and tropospheric columns,
J. Geophys. Res.,
113,
D16S32,
doi:10.1029/2007JD008863.
Copyright 2008 by the American Geophysical Union.
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