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A Note on the Boundary Layer Wind Structure Above Sloping Terrain
Publisher: American Meteorological Society
Abstract: The role of topography in the mean structure of low-level winds is investigated. Because the gravitational force vector has a component locally parallel to the sloping terrain, the low-level temperature anomaly, created ...
Mesoscale Turbulence Spectra over The Indian Ocean
Publisher: American Meteorological Society
Abstract: Doppler wind data obtained over the Indian Ocean during the 1964 Indian Ocean Expedition are analyzed in terms of power spectrum estimates. Peculiarities in the computed distribution of the mean horizontal kinetic energy ...
A Numerical Study of Currents, Heat Advection, and Sea-Level Fluctuations in the Yellow Sea in Winter 1986
Publisher: American Meteorological Society
Abstract: A vertically integrated model that incorporates horizontal temperature variations is used to study the circulation of the Yellow Sea in a wintertime period for which velocity and temperature measurements are available at ...
Inverse Determination of Surface Heat Flux over the Yellow Sea in Winter 1986 from Sea Surface Temperature Data
Publisher: American Meteorological Society
Abstract: An assimilation of routine sea surface temperature observations is conducted to estimate the sea surface heat flux in the Yellow Sea during the winter of 1986. Ten-day mean SST compilations, published by the Japan ...
Steady Coastal Upwelling in a Continuously Stratified Ocean
Publisher: American Meteorological Society
Abstract: Steady coastal upwelling driven by wind-stress and surface apparent temperature anomalies in a continuously stratified ocean of infinite depth is examined within the framework of a set of linearized hydrodynamic and ...
The Importance of Density Stratification to Bottom Boundary Layers over Continental Margins
Publisher: American Meteorological Society
Abstract: Because continental margins are inclined, the boundary layer over them is tied to bottom density as well as to the barotropic pressure gradient. Through the no-flux condition at the sea floor, the bottom boundary layer, ...
On the Possibilities of Coastal, Mid-Shelf, and Shelf Break Upwelling
Publisher: American Meteorological Society
Abstract: The steady-state circulation on a continental shelf under the combined influence of a wind stress, a surfacedensity distribution, and a longshore current over the shelf break is investigated in a linear, ?-plane modelthat ...
A Hindcast of Barotropic Response over the Oregon-Washington Continental Shelf during the Summer of 1972
Publisher: American Meteorological Society
Abstract: Hindeasts of bottom currents on the southern Washington continental shelf are made on the basis of a long-wave approximation to the vorticity equation for a barotropic flow. Resistance of the shelf bottom to the flow is ...
On the Theory of Coastal-Trapped Waves in an Upwelling Frontal Zone
Publisher: American Meteorological Society
Abstract: Free, stable, coastal-trapped waves propagating in a continental shelf regime typical of coastal upwelling areas are studied using a two-layer analytical model. Two cases of interfacial geometry and mean current simulate ...
Coastally Trapped Long Waves in the Yellow Sea
Publisher: American Meteorological Society
Abstract: The coastally trapped long-wave theory is adapted to a double shelf bottom topography in the development of a barotropic long-wave model for calculating wintertime wind-driven currents and sea level fluctuations in the ...