The influence of eddy viscosity parameterization and turbulence energy closure scheme upon the coupling in tidal and wind induced currents

Citation
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
Citations number
33
Categorie Soggetti
Aquatic Sciences
Journal title
ESTUARINE COASTAL AND SHELF SCIENCE
ISSN journal
02727714 → ACNP
Volume
53
Issue
4
Year of publication
2001
Pages
415 - 436
Database
ISI
SICI code
0272-7714(200110)53:4<415:TIOEVP>2.0.ZU;2-C
Abstract
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.