Sensitivity of chemical tracers to meteorological parameters in the MOZART‐3 chemical transport model
Author(s) -
Kinnison D. E.,
Brasseur G. P.,
Walters S.,
Garcia R. R.,
Marsh D. R.,
Sassi F.,
Harvey V. L.,
Randall C. E.,
Emmons L.,
Lamarque J. F.,
Hess P.,
Orlando J. J.,
Tie X. X.,
Randel W.,
Pan L. L.,
Gettelman A.,
Granier C.,
Diehl T.,
Niemeier U.,
Simmons A. J.
Publication year - 2007
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2006jd007879
Subject(s) - environmental science , stratosphere , atmospheric sciences , ozone , chemical transport model , troposphere , mozart , atmosphere (unit) , climatology , water vapor , wind speed , meteorology , geology , physics
The Model for Ozone and Related Chemical Tracers, version 3 (MOZART‐3), which represents the chemical and physical processes from the troposphere through the lower mesosphere, was used to evaluate the representation of long‐lived tracers and ozone using three different meteorological fields. The meteorological fields are based on (1) the Whole Atmosphere Community Climate Model, version 1b (WACCM1b), (2) the European Centre for Medium‐Range Weather Forecasts (ECMWF) operational analysis, and (3) a new reanalysis for year 2000 from ECMWF called EXP471. Model‐derived tracers (methane, water vapor, and total inorganic nitrogen) and ozone are compared to data climatologies from satellites. Model mean age of air was also derived and compared to in situ CO 2 and SF 6 data. A detailed analysis of the chemical fields simulated by MOZART‐3 shows that even though the general features characterizing the three dynamical sets are rather similar, slight differences in winds and temperature can produce substantial differences in the calculated distributions of chemical tracers. The MOZART‐3 simulations that use meteorological fields from WACCM1b and ECMWF EXP471 represented best the distribution of long‐lived tracers and mean age of air in the stratosphere. There was a significant improvement using the ECMWF EXP471 reanalysis data product over the ECMWF operational data product. The effect of the quasi‐biennial oscillation circulation on long‐lived tracers and ozone is examined.
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