We explore the stability characteristics of a single, barotropic, wind
-driven gyre as a function of the strength of the wind forcing and the
size and shape of the basin. We find steady solutions for the barotro
pic flow in a basin driven by a steady wind stress over a range of val
ues of the Reynolds number and the strength of the wind stress. For th
ose solutions that are close to the stability boundary, we examine the
form of the most unstable normal mode. We find that for sufficiently
weak forcing, the form of the first instability seen is an instability
of the western boundary current. However, for larger values of the fo
rcing, the first instability to set in, as the Reynolds number is redu
ced, is centered on a standing meander that forms on the continuation
of the boundary current after it has left the boundary. Both types of
instability are oscillatory. There are several different modes of stan
ding meander instability each associated with Rossby wave-like disturb
ances in the eastern half of the basin. Each of these modes is most un
stable when its frequency is close to a resonance with a basin mode wi
th similar spatial scales.