Cnk. Mooers et J. Wang, ON THE IMPLEMENTATION OF A 3-DIMENSIONAL CIRCULATION MODEL FOR PRINCE-WILLIAM-SOUND, ALASKA, Continental shelf research, 18(2-4), 1998, pp. 253-277
The POM (Princeton Ocean Model), a three-dimensional, primitive equati
on ocean circulation model, is applied to Prince William Sound, Alaska
. A 3-D concentration equation for passive tracers is added to POM to
explore transport pathways and rates, plus retention zones and residen
ce times. The 3-D structures of the current, density, and passive trac
er concentration are examined for realistic bottom topography, idealiz
ed Alaskan coastal water inflow/outflow and idealized wind-forcing. Ba
sed on observational evidence and ecological concerns, the 'lake/river
hypothesis' (i.e, the effect of weak versus strong throughflow on the
ecology of the Sound) is explored to determine its influence on the c
irculation and transport patterns of passive tracers. Strong inflow th
rough Hinchinbrook Entrance (river-like case) is crucial to the vigoro
us cyclonic circulation in the Sound and strong coupling to offshore i
nfluences, while with a weak inflow (lake-like case), the circulation
in the Sound is much weaker and weakly coupled to offshore influences.
The strength of the inflow and the wind direction are particularly im
portant for determining the nature of the secondary branches of the th
roughflow in the northwestern Sound and the position, strength, and nu
mber of cyclonic and anticyclonic gyres, Mesoscale eddies are induced
in the deep basins that have not yet been studied observationally. The
advection of buoyant (relatively fresh) coastal water into the Sound
significantly influences the circulation pattern and upper-layer densi
ty stratification. Idealized winter and summer wind-forcing generate d
istinctive surface circulation patterns that are important to the tran
sport pathways, residence times, and retention zones of passive tracer
s; for example, northward and westward winds increase the northernmost
penetration of passive tracers entering the Sound from offshore and t
he residence time substantially. (C) 1998 Elsevier Science Ltd, All ri
ghts reserved