Interacting chemical systems can be analyzed using the structures and lifet
imes of characteristic modes of variation about a quasi-steady state. For t
he atmospheric CH4-CC-OH system, characteristic modes of concentration vari
ation involve predominantly a single species, but their lifetimes differ fr
om the dominant species turnover times. Here a species turnover time is the
species amount divided by its removal rate, whereas the characteristic mod
e lifetime is the amplitude of a perturbation pattern divided by its rate o
f change and includes feedback effects. Characteristic mode analysis is use
d here to consider variations in both concentrations and isotopic ratios fo
r such systems. New 'isotopic modes' are identified which are only weakly a
ffected by feedbacks and have lifetimes very close to species turnover time
s. This raises the possibility that analysis of variations in both concentr
ation and isotopic ratios may provide a unique tool for resolving turnover
times and chemical feedbacks in atmospheric chemistry.