We discuss the characteristics of analytical solutions for the mean age of
air in a simple, one-dimensional conceptual model of stratospheric transpor
t. This "leaky pipe" model is a version of the "tropical pipe" model which
has been modified to include detrainment of surf zone air into the tropics.
We examine the dependence of the mean age on advection, diffusive mixing,
and quasi-horizontal mixing between the surf zones and the tropics. In the
absence of vertical diffusion across tracer mixing ratio isopleths the age
difference between the tropics and midlatitudes does not depend on mixing a
cross the edge of the tropics, but only on advection. The age difference gi
ven by this nondiffusive limit is an upper bound on the tropical-midlatitud
e age difference. This work provides some insight into the results of recen
t modeling studies that have used the mean age as a diagnostic of stratosph
eric transport.