RADON-222 AS A COMPARATIVE TRACER OF TRANSPORT AND MIXING IN 2 GENERAL-CIRCULATION MODELS OF THE ATMOSPHERE

Radon 222 (Rn-222) is used as a tracer to probe and intercompare trans port, turbulent mixing, and convective mixing in the Laboratoire de Me teorologie Dynamique (LMD) and Goddard Institute for Space Studies (GI SS) atmospheric general circulation models (GCMs), Formulations for tr acer transport and mixing and their control on the global distribution and time variability of Rn-222, as well as parameterizations for the continental surface source flux, are directly implemented into the two GCMs and run ''inline.'' Tracer formulations are largely inspired by climate variables (heat, moisture, momentum) formulations in the base GCMs. The comparison of model-calculated Rn-222 with observations of t ime (diurnal, seasonal, sporadic), variability, and spatial (horizonta l, vertical) distribution shows partial agreement only. Uncertainties of the sources of Rn-222, in particular of the dependence of Rn-222 em anation on soil freezing, are substantial, and the significance and re liability of some of the available observations are low. Model interco mparison is not subject to observation limitations, and it clearly ind icates that the boundary layer is more homogeneously mixed in the LMD model, whereas deep convection is more efficient at carrying surface-p roduced quantities to high tropospheric levels in the GISS model. Reso lution also makes a large difference. The LMD model has a finer horizo ntal grid over most of the globe and is almost systematically better t han the GISS model at reproducing sharp fluctuations of Rn-222 and sea sonal cycles. Our results support that Rn-222 could provide an unequiv ocal absolute measure of the GCM's performances if a more comprehensiv e observational validation was available.