The diffusive regime of double-diffusive convection is discussed, with a particular focus on unresolved issues that are holding up the development of large-scale parameterizations. Some of these issues, such as interfacial transports and layer-interface interactions, may be studied in isolation. Laboratory work should help with these. However, we must also face more difficult matters that relate to oceanic phenomena that are not represented easily in the laboratory. These lie beneath some fundamental questions about how double-diffusive structures are formed in the ocean, and how they evolve in the competitive ocean environment
The article of record as published may be found at https://darchive.mblwhoilibrary.org/handle/1912/2...
Much progress has recently been made in understanding and quantifying vertical mixing induced by dou...
The linear stability of a double-diffusively stratified, inflectional shear flow is investigated. Do...
The diffusive regime of double-diffusive convection is discussed, with a particular focus on unresol...
The diffusive regime of double-diffusive convection is reviewed, with a particular focus on issues t...
The physics of double diffusion and the role that it plays in the ocean provided the central theme f...
A series of large-scale numerical simulations is presented, which incorporate parameterizations of v...
Three-dimensional direct numerical simulations are performed that give us an in-depth account of the...
Double diffusive (DD) convection is a phenomenon frequently observed in the oceans and in many ind...
Double-diffusive convection (DDC), which is the buoyancy-driven flow with fluid density depending on...
A sequence of two- and three-dimensional simulations are conducted for the double-diffusive convecti...
When fluid stratification is induced by the vertical gradients of two scalars with different diffusi...
Double-diffusive convection (DDC), which is the buoyancy-driven flow with fluid density depending on...
Double-diffusive convection in a horizontally infinite layer of a unit height in a large Rayleigh nu...
Double-diffusive convection, often referred to as semi-convection in astrophysics, occurs in thermal...
The article of record as published may be found at https://darchive.mblwhoilibrary.org/handle/1912/2...
Much progress has recently been made in understanding and quantifying vertical mixing induced by dou...
The linear stability of a double-diffusively stratified, inflectional shear flow is investigated. Do...
The diffusive regime of double-diffusive convection is discussed, with a particular focus on unresol...
The diffusive regime of double-diffusive convection is reviewed, with a particular focus on issues t...
The physics of double diffusion and the role that it plays in the ocean provided the central theme f...
A series of large-scale numerical simulations is presented, which incorporate parameterizations of v...
Three-dimensional direct numerical simulations are performed that give us an in-depth account of the...
Double diffusive (DD) convection is a phenomenon frequently observed in the oceans and in many ind...
Double-diffusive convection (DDC), which is the buoyancy-driven flow with fluid density depending on...
A sequence of two- and three-dimensional simulations are conducted for the double-diffusive convecti...
When fluid stratification is induced by the vertical gradients of two scalars with different diffusi...
Double-diffusive convection (DDC), which is the buoyancy-driven flow with fluid density depending on...
Double-diffusive convection in a horizontally infinite layer of a unit height in a large Rayleigh nu...
Double-diffusive convection, often referred to as semi-convection in astrophysics, occurs in thermal...
The article of record as published may be found at https://darchive.mblwhoilibrary.org/handle/1912/2...
Much progress has recently been made in understanding and quantifying vertical mixing induced by dou...
The linear stability of a double-diffusively stratified, inflectional shear flow is investigated. Do...