Salt fingering is an oceanographic small-scale phenomenon that occurs in statically stable regions where relatively warm salty water lies above cold, fresh water. Currently, analyses and interpretation of most microstructure measurements and salt fingers in particular, are based upon the fundamental assumption that the microstructure is isotropic. While is it generally accepted that the isotropic assumption may lead to underestimates of the dissipation rates of thermal and velocity fluctuations by factors of two to four, no significant attempt has been made to take the anisotropy of microstructure into account yet. Thus, the anisotropy remains one of the key elements of uncertainty in the microstructure analysis and a major obstacle in ...
Abstract: Improving observational capabilities in the ocean are revealing a substantial body of evi...
Observations of diapycnal mixing rates are examined and related to diapycnal advection for both doub...
The article of record as published may be found at https://darchive.mblwhoilibrary.org/handle/1912/2...
Many hypotheses have been advanced to explain the formation of mixed layers in the ocean; the salt f...
Salt and heat are two ocean properties of vital importance. Their mean distribution, their advective...
This is a transient two-dimensional numerical study of double-diffusive salt fingers in a two-layer ...
Double-diffusive instabilities are often invoked to explain enhanced transport in stably stratified ...
Fingering double diffusive convection with real seawater properties is studied by two-dimensional di...
Graduation date: 2010Instability and turbulence in sheared, salt-fingering favorable stratification ...
When fluid stratification is induced by the vertical gradients of two scalars with different diffusi...
The phenomena of double-diffusive processes occur when two fluids with molecular diffusivities, ope...
Results are presented of calculations with a second-order turbulence model which has been modified t...
Double-diffusive finger convection occurs in many natural processes. The theories for double-diffusi...
Direct numerical simulations of two-dimensional fingering convection are presented. They show the gr...
Simulations of double-diffusion with a two-dimensional, vertical plane spectral transform model reve...
Abstract: Improving observational capabilities in the ocean are revealing a substantial body of evi...
Observations of diapycnal mixing rates are examined and related to diapycnal advection for both doub...
The article of record as published may be found at https://darchive.mblwhoilibrary.org/handle/1912/2...
Many hypotheses have been advanced to explain the formation of mixed layers in the ocean; the salt f...
Salt and heat are two ocean properties of vital importance. Their mean distribution, their advective...
This is a transient two-dimensional numerical study of double-diffusive salt fingers in a two-layer ...
Double-diffusive instabilities are often invoked to explain enhanced transport in stably stratified ...
Fingering double diffusive convection with real seawater properties is studied by two-dimensional di...
Graduation date: 2010Instability and turbulence in sheared, salt-fingering favorable stratification ...
When fluid stratification is induced by the vertical gradients of two scalars with different diffusi...
The phenomena of double-diffusive processes occur when two fluids with molecular diffusivities, ope...
Results are presented of calculations with a second-order turbulence model which has been modified t...
Double-diffusive finger convection occurs in many natural processes. The theories for double-diffusi...
Direct numerical simulations of two-dimensional fingering convection are presented. They show the gr...
Simulations of double-diffusion with a two-dimensional, vertical plane spectral transform model reve...
Abstract: Improving observational capabilities in the ocean are revealing a substantial body of evi...
Observations of diapycnal mixing rates are examined and related to diapycnal advection for both doub...
The article of record as published may be found at https://darchive.mblwhoilibrary.org/handle/1912/2...