Tropospheric chemical mechanisms can generate oscillations in which th
e concentrations of all reactive chemical species oscillate on timesca
les ranging from days to years, depending on certain parameter ranges
of specified sources for NOx; and a reduced species (e.g., carbon mono
xide, isoprene, or methane). A simple carbon monoxide oxidation mechan
ism is presented that exhibits oscillatory solutions qualitatively sim
ilar to those found in more complex mechanisms. This allows the deriva
tion of a two-variable oscillatory model for ozone and carbon monoxide
. Using this model, an analytic estimation of the oscillation period i
s given, the chemical sources required for oscillatory solutions are e
valuated, and the mechanism for the oscillation is elucidated. Some of
these: results can be extended to more complex oscillatory mechanisms
.