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Double Diffusion and the Distribution of the Density Ratio in the Mediterranean Waterfront Southeast of the Azores
Mediterranean Water Temperture salinity
2009/1/6
Temperture and salinity (T–S) finestructure on vertical scales of 10 db and larger is examined in a 500 by 500 km grid located southeast of the Azores in the North Atlantic. The convergence of several...
Determining the Strength of the Deep Western Boundary Current Using the Chlorofluoromethane Ratio
chloro fluoro methanes Deep Western Boundary Current
2009/1/4
The dilution of a passive tracer during deep water formation and the subsequent advection/mixing in a deep boundary current is modeled with application to chlorofluoromethanes (CFMs) in the North Atla...
A Relationship between the Bowen Ratio and Sea–Air Temperature Difference under Unstable Conditions at Sea
Bowen Ratio Sea–Air Temperature Unstable Conditions
2008/10/23
At the air–sea interface, estimates of evaporation or latent heat flux and the Monin–Obukhov stability parameter require the measurements of dewpoint (Tdew) or wet-bulb temperature, which are not rout...
On the Estimation of Overwater Bowen Ratio from Sea–Air Temperature Difference
Overwater Bowen Ratio Sea–Air Temperature Difference
2008/7/11
On the basis of thermodynamic considerations, a relationship between overwater Bowen ratio, B, and sea–air temperature difference, (Tsea − Tair), under unstable conditions has been formulated by...
Double-Diffusive Interleaving in the Presence of Turbulence: The Effect of a Nonconstant Flux Ratio
Double-Diffusive Interleaving Turbulence Nonconstant Flux Ratio
2008/7/3
The influence of turbulent mixing on double-diffusively driven thermohaline interleaving is investigated. The problem is formulated using a turbulence-modified flux ratio to link the fluxes of T and S...