Sublimative outgassing of comets produces torques that alter the rotation
state of their nuclei. Recently, parameterized sublimative torque models have
been developed to study rotation state changes of individual comet nuclei and
populations of cometary bodies. However, these models simplify the interactions
between the escaping gas and cometary surface into only a few parameters that
hide the details of these complex interactions. Here we directly compare the
X-parameter model (Samarasinha & Mueller, 2013) with the SYORP model (Steckloff
& Jacobson, 2016) to tease out insights into the details of the gas-surface
interactions driving sublimative torques. We find that, for both of these
models to accurately model sublimative torques, the number of sublimating
molecules that contribute to the net torque is largely independent of the
detailed shape and activity of the nucleus, but rather depends primarily on the
size of the nucleus and the effective heliocentric distance of the comet. We
suggest that cometary activity must be largely restricted to regions of steep
gravitational surface slopes (above the angle of repose), where mass wasting
can refresh activity by shedding mantles of refractory materials and exposing
fresh volatiles. We propose a new classification scheme for comets based on the
frequency of this mass-wasting process (relative to the timescale of activity
fading): quasi-equilibrium, episodic, quasi-dormant, and extinct.Comment: 16 pages (plus 9 pages of references), including 3 figures. Accepted
for publication in Icaru