Evaluation of stratosphere - troposphere exchange and the hydroxyl radical distribution in 3-dimensional global atmospheric models using observations of cosmogenic 14CO

Patrick Jöckel1, Carl A.M. Brenninkmeijer1, Mark G. Lawrence1, Adriaan B. M. Jeuken2,3, and Peter F. J. van Velthoven2

1Max Planck Institute for Chemistry, Atmospheric Chemistry Division, Mainz, Germany
2Royal Netherlands Meteorological Institute (KNMI), Section of Atmospheric Composition, De Bilt, The Netherlands
3now at Institute for Inland Water Management and Waste Water Treatment, Lelystad, The Netherlands

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. D20, 4446, doi:10.1029/2001JD001324, 2002

Abstract. A new method for the quantitative evaluation of global atmospheric transport and the hydroxyl radical (OH)-based oxidation in three-dimensional (3-D) atmospheric chemistry transport models (CTMs) and general circulation models (GCMs) is developed. The method is based on a cosmogenic 14CO climatology that has been previously derived from a large number of 14CO observations. Using 14CO measurements to constrain model OH distributions and the simulated stratosphere–troposphere exchange (STE) provides a challenging test for 3-D atmospheric models. Here, the evaluation method is applied to the CTMs MATCH and TM3. Whereas MATCH overestimates the STE in both hemispheres, TM3 does reproduce the STE in the Southern Hemisphere (SH) but underestimates it in the Northern Hemisphere (NH). The STE phase in MATCH is 1 month too early, whereas no significant phase shift for TM3 is revealed. These characteristic deficiencies in both models were consistently determined, i.e., with the same boundary conditions (OH distribution and 14CO source distribution). The robustness of the results is tested by various sensitivity studies, involving the 14CO source distribution and strength, the tropospheric OH distribution, the stratospheric OH abundance, and the applied numerical advection scheme. Consistency is further checked by comparison of the model simulated vertical 14CO profiles to 14CO observations from a number of aircraft campaigns. The 14CO simulations do not support an interhemispheric asymmetry in the OH abundance with an on average higher concentration in the SH.

Received 25 September 2001; revised 27 March 2002; accepted 31 March 2002; published 30 October 2002.

Keywords: carbon-14-monoxide, model evaluation, hydroxyl-radical, stratosphere-troposphere-exchange, 3-dimensional global model, radiocarbon.

Index Terms: 0368 Atmospheric Composition and Structure: Troposphere—constituent transport and chemistry; 1610 Global Change: Atmosphere (0315, 0325); 3362 Meteorology and Atmospheric Dynamics: Stratosphere/troposphere interactions; 0325 Atmospheric Composition and Structure: Evolution of the atmosphere.

Citation: Jöckel, P., C. A. M. Brenninkmeijer, M. G. Lawrence, A. B. M. Jeuken, and P. F. J. van Velthoven, Evaluation of stratosphere–troposphere exchange and the hydroxyl radical distribution in three-dimensional global atmospheric models using observations of cosmogenic 14CO, J. Geophys. Res., 107(D20), 4446, doi:10.1029/2001JD001324, 2002.

Copyright 2002 by the American Geophysical Union.


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