A flow-dependent critical-point method for investigating topographically co
ntrolled flow in natural channels is applied to the bottom current through
the Irbe Strait connecting the Baltic proper and the Gulf of Riga. This app
roach is based on the functional formalism due to Gill [Gill, A.E., 1977. T
he hydraulics of rotating-channel flow. J. Fluid Mech., 80, 641-671.], and
here is used for the stratified flow structure observed during the IRBEX-95
field campaign. A critical section of the realizable flow regime was found
to be located slightly downstream of the most pronounced horizontal constr
iction of the channel. The predicted baroclinic volume flux 7200 m(3) s(-1)
overestimates the observed mean bottom-water transport by around 30%, a di
screpancy which most likely can be explained by the lack of sea level condi
tions and friction in the model. (C) 2000 Elsevier Science B.V, All rights
reserved.