Abstract. This paper contains a description of recent changes to
the formulation and numerical implementation of the Quasi-Geostrophic
Coupled Model (Q-GCM), which constitute a major update of the previous
version of the model (Hogg et al., 2014). The Q-GCM model has been designed
to provide an efficient numerical tool to study the dynamics of multi-scale
midlatitude air–sea interactions and their climatic impacts. The present
additions/alterations were motivated by an inquiry into the dynamics of
mesoscale ocean–atmosphere coupling and, in particular, by an apparent lack
of the Q-GCM atmosphere's sensitivity to mesoscale sea-surface temperature (SST)
anomalies, even at high (mesoscale) atmospheric resolutions, contrary to
ample theoretical and observational evidence otherwise. Major modifications
aimed at alleviating this problem include an improved radiative-convective
scheme resulting in a more realistic model mean state and associated model
parameters; a new formulation of entrainment in the atmosphere, which
prompts more efficient communication between the atmospheric mixed layer and
free troposphere; and an addition of a temperature-dependent wind
component in the atmospheric mixed layer and the resulting mesoscale
feedbacks. The most drastic change is, however, the inclusion of moist
dynamics in the model, which may be key to midlatitude ocean–atmosphere
coupling. Accordingly, this version of the model is to be referred to as the
MQ-GCM model. Overall, the MQ-GCM model is shown to exhibit a rich spectrum
of behaviors reminiscent of many of the observed properties of the Earth's
climate system. It remains to be seen whether the added processes are able
to affect in fundamental ways the simulated dynamics of the midlatitude
ocean–atmosphere system's coupled decadal variability.