Representation of submesoscale baroclinic instabilities in ROMS and
MPAS-O
- Kyle Hinson,
- Robert D. Hetland,
- Darren Engwirda,
- Katherine Smith
Abstract
The representation of submesoscale processes in ocean models is critical
for accurately representing the exchange of mass and tracers between the
surface mixed layer and subsurface waters. Comparisons of these
processes using multiple models is an important step for the validation
of different numerical schemes and identifying possible future
opportunities for model coupling. This study investigated the
representation of submesoscale processes using two ocean models, the
structured regional ocean model ROMS and the unstructured global ocean
model MPAS-O in an idealized domain. Results from the two models are
highly similar for multiple statistical metrics of submesoscale dynamics
including frontal processes, and also show that the impact of ocean
model choice is smaller than the choice of spatial grid resolution.
Overall, these results show promise for the successful coupling of the
two ocean models, and highlight additional differences in the
representation of along- and cross-frontal divergence estimates for
further exploration.