MATHEMATICAL-MODEL OF LOWER QUASI-HOMOGEN EOUS OCEANIC LAYER EFFECTS OF TEMPERATURE AND SALINITY STRATIFICATION AND TIDAL OSCILLATIONS

Authors
BARENBLATT GI GALERKINA NL LEBEDEV IA
Citation
Gi. Barenblatt et al., MATHEMATICAL-MODEL OF LOWER QUASI-HOMOGEN EOUS OCEANIC LAYER EFFECTS OF TEMPERATURE AND SALINITY STRATIFICATION AND TIDAL OSCILLATIONS, Izvestia Akademii nauk. Rossijskaa akademia nauk. Fizika atmosfery iokeana, 29(4), 1993, pp. 537-542
Citations number
7
Categorie Soggetti
Metereology & Atmospheric Sciences",Oceanografhy
Journal title
Izvestia Akademii nauk. Rossijskaa akademia nauk. Fizika atmosfery iokeana → ACNP
ISSN journal
10236317
Volume
29
Issue
4
Year of publication
1993
Pages
537 - 542
Database
ISI
SICI code
1023-6317(1993)29:4<537:MOLQEO>2.0.ZU;2-R
Abstract
Contributions of temperature and salinity stratification and tidal osc illation in development of high-energy oceanic boundary layer are cons idered. These factors increase local velocity maximum near bottom. Rel ative effects from temperature and salinity stratification and stratif ication caused by suspended particles are studied using simple model o f constant shear stress layer. Influence of the bottom slope is estima ted numerically.