ALBERT

Description: Global simulations of atmospheric chemistry are commonly conducted with off-line chemical transport models (CTMs) driven by archived meteorological data from general circulation models (GCMs). The off-line approach has the advantages of simplicity and expediency, but it incurs errors due to temporal averaging in the meteorological archive and the inability to reproduce the GCM transport algorithms exactly. The CTM simulation is also often conducted at coarser grid resolution than the parent GCM. Here we investigate this cascade of CTM errors by using (exp 222)Rn(exp 210)Pb(exp 7)Be chemical tracer simulations off-line in the GEOS-Chem CTM at rectilinear 0.250.3125 (25km) and 22.5 (200km) resolutions and online in the parent GEOS-5 GCM at cubed-sphere c360 (25km) and c48 (200km) horizontal resolutions. The c360 GEOS-5 GCM meteorological archive, updated every 3h and remapped to 0.250.3125, is the standard operational product generated by the NASA Global Modeling and Assimilation Office (GMAO) and used as input by GEOS-Chem. We find that the GEOS-Chem (exp 222)Rn simulation at native 0.250.3125 resolution is affected by vertical transport errors of up to 20% relative to the GEOS-5 c360 online simulation, in part due to loss of transient organized vertical motions in the GCM (resolved convection) that are temporally averaged out in the 3h meteorological archive. There is also significant error caused by operational remapping of the meteorological archive from a cubed-sphere to a rectilinear grid. Decreasing the GEOS-Chem resolution from 0.250.3125 to 22.5 induces further weakening of vertical transport as transient vertical motions are averaged out spatially and temporally. The resulting (exp 222)Rn concentrations simulated by the coarse-resolution GEOS-Chem are overestimated by up to 40% in surface air relative to the online c360 simulations and underestimated by up to 40% in the upper troposphere, while the tropospheric lifetimes of (exp 210)Pb and (exp 7)Be against aerosol deposition are affected by 510%. The lost vertical transport in the coarse-resolution GEOS-Chem simulation can be partly restored by recomputing the convective mass fluxes at the appropriate resolution to replace the archived convective mass fluxes and by correcting for bias in the spatial averaging of boundary layer mixing depths.