h-resolution
simulations where the elastic waves are not sufficiently damped out in a
small timestep without a significant amount of subcycling.  This procedure
works by reducing the effective ice strength that's used by the dynamics
and is not a supported option.

<P>
<TT>advection</TT> determines the horizontal transport scheme used. The default
scheme is the incremental remapping method ((<A
 HREF="node40.html#lipshunke04">Lipscomb and Hunke(2004)</A>)).  This method
is less diffusive and is computationa