You can use espc_mean25 to form a daily (running) mean of SSH. Note that this can probably also be applied to hourly GOFS SSH.
Or you can use hourly steric SSH, which removes the external tide signal.
However, I]m not sure if either approach will produce compatible datasets. An ocean model only cares about the gradient of SSH, so SSH can be offset by a spatially constant field with no effect. So the two SSH data sets might be offset by a constant, or perhaps by a non-constant offset with weak gradients.
Alan.