Atmospheric gas concentrations were measured at I s intervals in the upper
troposphere during a flight through and near the anvil of a storm. The obse
rved very high correlations between the concentrations of CO and CH4 are in
terpreted as arising from the mixing of two distinct air masses with differ
ing concentrations of each species, and is due to the nearly identical diff
usivities of CO and CH4 in air. We find that the correlations depend on the
period over which each concentration measurement was made. Correlations in
measurements made over short periods decay with time, while correlations o
ver larger scales remain high. We interpret this using a simple mixing mode
l.