The predictions of general-circulation models (GCMs) are sensitive to the a
ssumed cloud overlap within a vertical column of model grid boxes, but unti
l now no reliable observations of the degree of cloud overlap have been ava
ilable. In this note we derive the overlap characteristics of clouds from 7
1 days of high vertical resolution 94 GHz cloud radar data in the UK. It is
found that, contrary to the assumption made in most models, vertically con
tinuous clouds tend not to be maximally overlapped. Rather, the overlap of
clouds at two levels tends to fall rapidly as their vertical separation is
increased, and for levels more than 4 bm apart, overlap is essentially rand
om. A simple inverse-exponential expression for the degree of overlap as a
function of level separation is proposed that could, once results become av
ailable from a variety of other locations and seasons, be implemented in cu
rrent GCMs with relatively little difficulty.