Results of an interactively coupled atmospheric chemistry - general circulation model: Comparison with observations

Citation
R. Hein et al., Results of an interactively coupled atmospheric chemistry - general circulation model: Comparison with observations, ANN GEOPHYS, 19(4), 2001, pp. 435-457
Citations number
86
Categorie Soggetti
Earth Sciences
Journal title
ANNALES GEOPHYSICAE
ISSN journal
09927689 → ACNP
Volume
19
Issue
4
Year of publication
2001
Pages
435 - 457
Database
ISI
SICI code
0992-7689(200104)19:4<435:ROAICA>2.0.ZU;2-3
Abstract
The coupled climate-chemistry model ECHAM4.L39(DLR)/CHEM is presented which enables a simultaneous treatment of meteorology and atmospheric chemistry and their feedbacks. This is the first model which interactively combines a general circulation model with a chemical model, employing most of the imp ortant reactions and species necessary to describe the stratospheric and up per tropospheric ozone chemistry, and which is computationally fast enough to allow long-term integrations with currently available computer resources . This is possible as the model time-step used for the chemistry can be cho sen as large as the integration time-step for the dynamics. Vertically the atmosphere is discretized by 39 levels from the surface up to the top layer which is centered at 10 hPa, with a relatively high vertical resolution of approximately 700 m near the extra-tropical tropopause. We present the res ults of a control simulation representing recent conditions (1990) and comp are it to available observations. The focus is on investigations of stratos pheric dynamics and chemistry relevant to describe the stratospheric ozone layer. ECHAM4.L39(DLR)/CHEM reproduces main features of stratospheric dynamics in the arctic vortex region, including stratospheric warming events. This cons titutes a major improvement compared to earlier model versions. However, ap parent shortcomings in antarctic circulation and temperatures persist. The seasonal and interannual variability of the ozone layer is simulated in acc ordance with observations. Activation and deactivation of chlorine in the p olar stratospheric vortices and their inter-hemispheric differences are rep roduced. Considering methane oxidation as part of the dynamic-chemistry fee dback results in an improved representation of the spatial distribution of stratospheric water vapour concentrations. The current model constitutes a powerful tool to investigate, for instance, the combined direct and indirect effects of anthropogenic trace gas emissi ons.