搜索结果: 1-12 共查到“海洋物理学 Wind-Induced”相关记录12条 . 查询时间(0.125 秒)
Water motion in the barotropic mode, directly forced by suddenly imposed wind stress, is investigated in basins with arbitrary topography, but paying special attention to long basins, in which the dep...
Wind–Induced Baroclinic Motions at the Edge of the Continental Shelf
Wind–Induced Baroclinic Motions Continental Shelf
2009/4/2
In a two-layer model of stratified fluid flow, motions in the internal mode are governed by the distribution of an equivalent depth he. For a typical continental shelf, the distribution of he with dis...
Realistic Model of the Wind-Induced Ekman Boundary Layer
Realistic Model Wind-Induced Ekman Boundary Layer
2009/3/7
A physically realistic and general model for the vertical eddy viscosity in a homogeneous fluid is proposed. For an infinitely deep ocean the vertical eddy viscosity increases linearly with depth from...
An Experimental Study of Gravity-Inertial Waves and Wind-Induced Kelvin-Type Upwellings in a Rotating System
Gravity-Inertial Waves Rotating System Wind-Induced Kelvin-Type Upwellings
2009/2/10
Large-amplitude gravity-inertial waves have been observed in stratified seas. These waves, of a shorter period than the Coriolis period, are linked to a gust of wind. Numerous theories have been propo...
Wind-Induced Sea-Surface Slopes on the West Florida Shelf
Wind-Induced Sea-Surface Slopes West Florida Shelf
2009/2/6
Tidal and meteorological records at stations in the eastern Gulf of Mexico have been studied. The sea-level response is a maximum for winds along the coast and varies symmetrically with angle. The coh...
Wave-Turbulence interactions in the Upper Ocean. Part I：The Energy Balance of the Interacting Fields of Surface Wind Waves and Wind-Induced Three-Dimensional Turbulence
Wave-Turbulence interactions Upper Ocean Surface Wind Waves
2009/2/6
We analyze in detail the budget of total and fluctuating energy in the surface layer of the ocean. We suggest a rational scheme for separating the budget of turbulence from that of random wind-generat...
A Numerical Study of the Effects of Coastline Geometry on Wind-Induced Upwelling in the Gulf of Lions
Coastline Geometry Wind-Induced Upwelling Gulf of Lions
2009/2/5
An attempt is made to explain the fixed locations of coastal upwelling centers in the Gulf of Lions as a function of the coastline geometry alone. The semi-implicit numerical model, based on two-layer...
Effects of Near-Bottom Return Flows on Wind-Induced Currents
Near-Bottom Return Flows Wind-Induced Currents
2009/1/9
Wind, currents, and surface waves have been measured in a circulating wind-wave tank. Conditions corresponding to both coast and ocean, with and without bottom return flows respectively, have been sim...
Wind-Induced Destratification in Chesapeake Bay
Wind-Induced Destratification Chesapeake Bay
2009/1/9
Multiyear continuous observations of velocity and salinity in the Chesapeake Bay indicate that wind-induced destratification occurs frequently from early fall through midspring over large areas of the...
The Prediction of Nearshore Wind-induced Surface Currents from Wind Velocities Measured at Nearby Land Stations
Nearshore Wind-induced Surface Currents Wind Velocities Nearby Land Stations
2008/12/19
This paper aims to find a fast and efficient way to predict the wind-induced components of surface currents in a nearshore coastal area of several hundred square kilometers from wind velocities measur...
The Wind-Induced Wave Growth Rate and the Spectrum of the Gravity-Capillary Waves
Wind-Induced Gravity-Capillary Waves Growth Rate
2008/12/12
A kinematic wave breaking criterion is applied in the calculation of the short-wave dissipation. It is found that this short-wave dissipation, due to wave-drift interactions, has the effect of suppres...
Wind-Induced Currents and Bottom-Trapped Waves in the Santa Barbara Channel
Wind-Induced Currents Bottom-Trapped Waves Santa Barbara Channel
2008/11/6
The Santa Barbara Channel (SBC) is a coastal basin about 100 km long bounded by the Southern California mainland on the north and by a chain of islands on the south. The SBC is at most 50 km wide and ...