False diapycnal mixing often occurs due to horizontal diffusion in the simu
lation of heat, salinity, or water quality in estuaries by using a sigma co
-ordinated ocean model. The Princeton ocean model (POM) is used as a basic
cr co-ordinated model and is applied to Tokyo Bay. Only river discharges ar
e introduced into the model as external forces. Two remedies recommended in
the POM, Stelling's horizontal diffusion approximation, Huang's new diffus
ion formula, Song and Haidvogel's s co-ordinates, and Smolarkiewicz advecti
on scheme have all been examined for suppressing the false diapycnal mixing
. The conclusions are that the simultaneous use of POM's remedy and Stellin
g's approximation and the simultaneous use of POM's remedy and s co-ordinat
es are the most effective. Copyright (C) 2001 John Wiley & Sons, Ltd.