While it has been known for several decades that the variability of the ocean circulation in the gyre
interiors is much stronger than the mean flow, the sources of these strong eddies are still not well
understood. Baroclinic instability of the large scale circulation is a likely source, but it has been shown
that zonal flows with weak shear typical of the gyre interiors can not generate very strong variability. I
have recently addressed the question of whether the meridional component of the wind-driven gyres
might generate strong mesoscale eddies more effectively than can zonal flows. Scale analaysis and and
nonlinear numerical modelling studies show that the potential energy stored in the meridional component
of the large-scale wind-driven gyres may be effectively converted to eddy kinetic energy even for very
weakly sheared mean flows. For parameters typical of the interior of the mid-latitude subtropical gyres
the eddy kinetic energy at equilibration is two orders of magnitude greater than the mean kinetic energy.
This work has been generously supported through grants from the
National Science Foundation and the Office of Naval Research.
Recent manuscripts on these subjects :
Wang, J., M. A. Spall, G. R. Flierl, P. Malanotte-Rizzoli, 2012: A new
mechanism for the generation of quasi-zonal jets in the ocean. Geophys. Res. Lett.,
Hristova, H, J. Pedlosky, and M. A. Spall, 2008:
Radiating instability of a meridional boundary current.
J. Phys. Oceanogr., 38, 2294-2307.
Spall, M. A., 2000. Generation of strong mesoscale eddies by weak ocean gyres. Journal of Marine
Research, 58(1), 97-116.
Spall, M. A., 1994. A mechanism for low frequency variability and salt flux in the Mediterranean
salt tongue. Journal of Geophysical Research, 99(C5), 10121,10129.