The radiative decay of idealized stratospheric filaments embedded in a refe
rence midlatitude troposphere is investigated. The filaments are characteri
zed by typical lower stratospheric values of potential vorticity (PV), ozon
e, and humidity. The evolution of the filaments is obtained numerically in
the framework of a plane symmetric balanced model. Diabatic heating due to
radiation is accounted for by using a realistic parameterization scheme. Th
e control parameter for the numerical experiments is the aspect ratio of th
e initial PV anomaly, which determines the partitioning into a thermal and
a dynamical anomaly. For shallow filaments, both the temperature and the hu
midity anomaly are radiatively relevant. Initially, the decay of the filame
nt is independent on whether or not the moisture anomaly is accounted for.
At later times the effect of the moisture anomaly slows down the evolution
significantly. For intermediate and tall filaments the humidity anomaly dom
inates the evolution from the beginning, leading to an enhancement rather t
han a decay of the PV anomaly. In addition, for tall filaments the advectio
n by the induced Sawyer-Eliassen circulation has a significant impact on th
e evolution of the anomaly. In all experiments, ozone plays a minor role. T
he characteristic timescale of the evolution scales somewhat less than line
arly with the filament thickness and shows only weak sensitivity to the asp
ect ratio.