A chemical-family bookkeeping variable in a simple stratospheric model. Interconversion of atomic oxygen and ozone preserves this count, while removes two units. The definition must be extended consistently when including additional reservoirs or excited atomic states.
A basic oxygen–ozone mechanism combining oxygen photodissociation, three-body ozone formation, ozone photodissociation and . The last reaction removes two units of odd oxygen; a catalytic cycle can add another loss pathway.
With photolysis switched off, constant molecular oxygen and collider reservoirs give and for atomic oxygen , ozone , and . Dividing the equations and integrating gives
For , ozone grows toward a finite-reservoir endpoint below . Its value at sunrise depends on the dark-interval duration; is an approximate quasi-steady balance while atomic oxygen remains available.
Under fast Chapman cycle partitioning, an odd oxygen family abundance can satisfy . At equilibrium , its turnover lifetime is , while linearizing gives and relaxation time . A chemical lifetime is therefore not automatically an eigenmode relaxation time. The often-used expression also assumes ozone dominates the family abundance.
Suppose a reduced steady balance is , where , and hold and all specified background concentrations fixed. With , and , implicit differentiation gives . The quadratic loss term includes temperature-dependent O/O3 partitioning as well as the direct reaction coefficient. Holding the loss ratio fixed over a finite change is an additional approximation; solving the new quadratic provides a check.

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