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
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.