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Eddy-Potential vorticity Fluxes in the Gulf Stream Recirculation
Eddy-Potential vorticity Fluxes Gulf Stream Recirculation
2009/1/10
The local effect of the mesoscale eddy field on the mean potential vorticity distribution of the Gulf Stream recirculation region is determined from the quasi-geostrophic eddy potential vorticity flux...
Meridional Ekman Heat Fluxes for the World Ocean and Individual Ocean Basins
Heat Fluxes Individual Ocean Basins World Ocean
2009/1/8
Monthly climatological estimates of wind stress and sea surface temperature are used to compute meridional Ekman heat fluxes in the world ocean. Qualitatively the annual cycles of the Atlantic and Pac...
Ekman Volume Fluxes for the World Ocean and Individual Ocean Basins
Ekman Volume Fluxes World Ocean Individual Ocean Basins
2009/1/5
Monthly climatological estimates of wind stress have been used to compute Ekman volume fluxes in the world ocean. Specifically, meridional and zonal Ekman volume fluxes have been computed and from the...
Evaporation Minus Precipitation and Density Fluxes for the North Atlantic
North Atlantic precipitation evaporation
2009/1/4
Estimates of evaporation (E) over the North Atlantic Ocean by Bunker have been combined with estimates of precipitation (P) by Dorman and Bourke to produce new annual and seasonal maps of E–P and surf...
The Use of Mean Atmospheric Parameters in the Calculation of Modeled Mean Surface Heat Fluxes over the World’s Oceans
Mean Atmospheric Parameters World’s Oceans Surface Heat Fluxes
2008/12/30
There are a number of atlases that display the distribution of ocean-atmosphere sensible and latent heat fluxes over various regions. Many are based on the “classical” method, in which time mean quant...
The scalar flux due to small amplitude waves that exhibit a preferred sense of rotation or polarization is shown to consist of a component. FS, that is skewed, being everywhere orthogonal to the mean ...
Effect of Breaking Waves on the Transport of Heat and Vapor Fluxes from the Ocean
atmospheric surface layer high sea Transport
2008/12/19
One method of studying the complexities of the atmospheric surface layer over the ocean during high sea states is to consider the waves as moving drag objects for the wind. The study treats transport ...
When averaging the equations of motion, thermodynamics, and scalar conservation over turbulent fluctuations, we perform the process in several stages. First, an average is taken over the microscopic s...
Statistics of the Air-Sea Fluxes of Momentum and Mechanical Energy in a Coupled Wave-Atmosphere Model
circulation model Mechanical Energy Air-Sea Fluxes Coupled Wave-Atmosphere Model
2008/12/16
An atmospheric general circulation model (GCM) and a wind wave model are coupled through the wind stress. The wind stress which forces the wave model, depends in the coupled model on the stage of deve...
Interdecadal Variability of the Thermohaline Circulation and High-Latitude Surface Fluxes
Interdecadal Variability Thermohaline Circulation High-Latitude Surface Fluxes
2008/12/12
An idealized North Atlantic Ocean model is forced by climatological wind stress, restoring temperature, and a diagnosed salinity flux. Both centennial and interdecadal oscillations are sustained in th...
Eddy Amplitudes and Fluxes in a Homogeneous Model of Fully Developed Baroclinic Instability
Eddy Amplitudes Baroclinic Instability Homogeneous Model
2008/12/12
A horizontally homogeneous two-layer quasigeostrophic model with imposed environmental vertical shear is used to study eddy energies and fluxes in the regime in which an inverse barotropic energy casc...
Oceanic Fluxes on the WOCE A11 Section
subantarctic zone Circumpolar Current cruise track lay Oceanic Fluxes
2008/12/12
The most southerly WOCE one-time section in the South Atlantic, designated A11, was occupied in January 1993. The cruise track lay across the cool subantarctic zone of the Circumpolar Current in the w...
Density Compensated Thermohaline Gradients and Diapycnal Fluxes in the Mixed Layer
Mixed Layer salinity gradients Density-compensated temperature
2008/12/12
Density-compensated temperature and salinity gradients are often observed in mixed layer fronts. A possible explanation Of this Observation is that there is a systematic relation between the “strength...
Surface Heat Fluxes in the Western Equatorial Pacific Ocean Estimated by Bulk Parameterization and by an Inverse Mixed Layer Model
Tropical Ocean Global Atmosphere Coupled Ocean–Atmosphere Response Experiment
2008/12/3
Sea surface heat fluxes in the western equatorial Pacific Ocean estimated by bulk parameterization are compared with fluxes computed with a one-dimensional, level 2.5 turbulence closure inverse mixed ...
Circulation and Fluxes in the North Atlantic between Greenland and Ireland
East Greenland Current Circulation Fluxes Ireland
2008/11/24
Quasi-meridional flux estimates for volume, heat, and freshwater, with computed errors, in the region of the subpolar gyre of the North Atlantic between Cape Farewell and Ireland between 53° and 60°N ...