Am. Davies et J. Xing, The influence of eddy viscosity parameterization and turbulence energy closure scheme upon the coupling in tidal and wind induced currents, EST COAST S, 53(4), 2001, pp. 415-436
A three-dimensional model of the Irish Sea, and the shelf and shelf-edge re
gion off the west coast of Scotland is used to examine the interaction of w
ind induced surface currents and M-2 tidal currents which can lead to an in
creased near surface M-4 tidal current in the region. Calculations are perf
ormed using uniform southerly and westerly wind stresses, with vertical edd
y viscosity computed using either a simple flow dependent form of viscosity
, or one related to the flow and surface wind stress or derived using a two
-equation turbulence model. Resulting M-4 tidal distributions computed with
the various viscosity formulations are compared with each other. The spati
al distribution the M-4 tidal current in the case of the flow dependent vis
cosity, shows a significant enhancement of the surface M-4 tide due to non-
linear coupling between the surface shear and the tidally dependent viscosi
ty. In deep water this is the dominant mechanism giving rise to an enhancem
ent in near surface M-4 current. In shallow water, however, where other non
-linear processes are important in generating the M-4 tide, namely changes
in water depth and friction, these are significant as well as the non-linea
r surface shear effect, in changing the M-4 tidal distribution. However, wh
en an eddy viscosity formulation depending upon flow and surface wind stres
s is used, the non-linear coupling mechanism producing an enhanced M-4 tida
l surface current is reduced, and no increase in M-4 surface current occurs
.
Calculations with the two equation turbulence model, do not produce an incr
ease in the near surface M-4 tide, as the near surface viscosity in this mo
del is determined principally by the wind stress rather than the tidal curr
ent. Some conclusions concerned with developing a simple eddy viscosity mod
el having similar characteristics to the turbulence energy model, and exper
imental data sets for validation are considered at the end of the paper. (C
) 2001 Academic Press.