Cataclysmic variables undergo periodic nova explosions during which a finite
mass of material is expelled on a short timescale. The system widens and, as a
result, the mass-transfer rate drops. This state of hibernation may account for
the variety of cataclysmic variable types observed in systems of similar mass
and period. In the light of recent changes to the theory of nova ignition and
magnetic braking we investigate whether hibernation remains a viable mechanism
for creating cataclysmic variable diversity. We model the ratio of time spent
as dwarf novae (DNe) to nova-like systems (NLs). Above a critical mass-transfer
rate the system is NL and below it a DN. The dominant loss of angular momentum
is by magnetic braking but the rate is uncertain. It is also uncertain what
fraction of the mass accreted is expelled during the novae. We compare the
models of the ratios against the period of the system for different magnetic
braking rates and different ejected masses with the ratio of the number of
observed NLs to DNe. We deduce that a rate of angular momentum loss a factor of
ten smaller than that traditionally assumed is necessary if hibernation is to
account for the observed ratios