Abstract
We investigate the ergodicity of 2D large scale quasigeostrophic
flows under random wind forcing. We show that the quasigeostrophic
flows are ergodic under suitable conditions on the random forcing
and on the fluid domain, and under no restrictions on viscosity,
Ekman constant or Coriolis parameter. When these conditions are
satisfied, then for any observable of the quasigeostrophic flows,
its time average approximates the statistical ensemble average, as
long as the time interval is sufficiently long.