Validation of an off‐line three‐dimensional chemical transport model using observed radon profiles: 2. Model results

We parameterize radon emissions in the TOMCAT global off-line three-dimensional chemical transport model (CTM) and compare modeled radon profiles with spatially and temporally matched observations obtained near Moffett Field, California, in June 1994. The CTM was forced using European Centre for Medium-Range Weather Forecasts analyses for April-August 1994. To identify the origin of modeled radon, we divided the radon sources into three regions. We performed CTM sensitivity experiments at horizontal resolutions of 2.8° × 2.8° (latitude × longitude) and 7.5° × 7.5°, and with and without moist convection and/or vertical diffusion. At the higher resolution the full CTM (i.e., including convection and vertical diffusion) generally agrees well with the observations in the free troposphere. The observations exhibit free-tropospheric radon peaks at altitudes where zonal wind speeds in the Pacific jet stream are greatest (generally at ≥7 km). In this region the modeled radon originates from Asia, and the observed variability in the radon concentration is reproduced. Thus, the model reproduces the position and strength of the jet. We identify observed radon peaks that may originate from convective lifting, as they do in the model results. If these observed peaks do originate from convection, then the full CTM captures the correct temporal variability in convection over Asia and the Pacific for the observation period. Quantitative comparison shows that the model-data agreement is degraded if we decrease the model resolution to 7.5° × 7.5°, or remove the parameterizations of convection and/or vertical diffusion. This suggests a resolution of near 2.8° × 2.8° is needed in global models for realistic simulations of short-lived species. We have identified certain shortcomings with TOMCAT: the model underestimates the amount of convective cloud, the convective cloud top height, and the amount of vertical diffusion. We identify improvements to ameliorate these problems.

[1]  D. Legates,et al.  Mean seasonal and spatial variability in gauge‐corrected, global precipitation , 1990 .

[2]  W. Broecker,et al.  Radium-226 and Radon-222: Concentration in Atlantic and Pacific Oceans , 1967, Science.

[3]  C. Genthon,et al.  Radon 222 as a comparative tracer of transport and mixing in two general circulation models of the atmosphere , 1995 .

[4]  J. Louis A parametric model of vertical eddy fluxes in the atmosphere , 1979 .

[5]  M. Prather Numerical advection by conservation of second-order moments. [for trace element spatial distribution and chemical interaction in atmosphere] , 1986 .

[6]  M. Wilkening,et al.  Factors affecting exhalation of radon from a gravelly sandy loam , 1984 .

[7]  Richard B. Rood,et al.  Three-dimensional radon 222 calculations using assimilated meteorological data and a convective mixing algorithm , 1996 .

[8]  P. Crutzen,et al.  Parameterization of vertical tracer transport due to deep cumulus convection in a global transport model and its evaluation with 222Radon measurements , 1990 .

[9]  J. Deardorff,et al.  Theoretical expression for the countergradient vertical heat flux , 1972 .

[10]  Karl K. Turekian,et al.  Geochemistry of atmospheric radon and radon products , 1977 .

[11]  Radon‐222 as a test of convective transport in a general circulation model , 1990 .

[12]  R. Cicerone,et al.  RADON 222 AND TROPOSPHERIC VERTICAL TRANSPORT. , 1984 .

[13]  E. Danielsen,et al.  The China Clipper - Fast advective transport of radon-rich air from the Asian boundary layer to the upper troposphere near California , 1990 .

[14]  Albert A. M. Holtslag,et al.  Local Versus Nonlocal Boundary-Layer Diffusion in a Global Climate Model , 1993 .

[15]  A. Matthews,et al.  Intraseasonal oscillations in 15 atmospheric general circulation models: results from an AMIP diagnostic subproject , 1996 .

[16]  G. Lambert,et al.  Long-range transport of continental radon in subantarctic and antarctic areas , 1986 .

[17]  S. Schery,et al.  Measurements of the effect of cyclic atmospheric pressure variation on the flux of 222RN from the soil , 1982 .

[18]  D. Jacob,et al.  Transport of continental air to the subantarctic Indian Ocean , 1990 .

[19]  G. Lambert,et al.  The China Clipper—Fast advective transport of radon-rich air from the Asian boundary layer to the upper troposphere near California , 1988 .

[20]  Richard B. Rood,et al.  An assimilated dataset for Earth science applications , 1993 .

[21]  N. Mahowald Development of a 3-dimensional chemical transport model based on observed winds and use in inverse modeling of the sources of CCl₃F , 1996 .

[22]  R. Chatfield,et al.  Transport of radon in a three-dimensional, subhemispheric model , 1989 .

[23]  M. Tiedtke A Comprehensive Mass Flux Scheme for Cumulus Parameterization in Large-Scale Models , 1989 .

[24]  M. Kritz,et al.  Validation of an off‐line three‐dimensional chemical transport model using observed radon profiles: 1. Observations , 1998 .

[25]  Martyn P. Chipperfield,et al.  Evaluation and intercomparison of global atmospheric transport models using 222Rn and other short-lived tracers , 1997 .

[26]  N. Mahowald,et al.  Transport of 222radon to the remote troposphere using the Model of Atmospheric Transport and Chemistry and assimilated winds from ECMWF and the National Center for Environmental Prediction/NCAR , 1997 .