We study solutions to the 2D quasi-geostrophic (QGS) equation
partial derivative theta/partial derivative t + u . del theta + kappa(-Delt
a)(alpha)theta = f
and prove global existence and uniqueness of smooth solutions if alpha is a
n element of (1/2; 1]; weak solutions also exist globally but are proven to
be unique only in the class of strong solutions. Detailed aspects of large
time approximation by the linear QGS equation are obtained.