International audienceThe 2004 Gibbs thermodynamic potential function of naturally abundant water ice is based on much more experimental data than its predecessors, is therefore significantly more accurate and reliable, and for the first time describes the entire temperature and pressure range of existence of this ice phase. It is expressed in the ITS-90 temperature scale and is consistent with the current scientific pure water standard, IAPWS-95, and the 2003 Gibbs potential of seawater. The combination of these formulations provides sublimation pressures, freezing points, and sea ice properties covering the parameter ranges of oceanographic interest. This paper provides source code examples in Visual Basic, Fortran and C++ for the computa...
An energy loan sea ice model was developed to manage the energetics of water phase changes in a cons...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
December 1995.Includes bibliographical references.We describe a simple two-layer thermodynamic ocean...
International audienceThe 2004 Gibbs thermodynamic potential function of naturally abundant water ic...
International audienceThe 2003 Gibbs thermodynamic potential function represents a very accurate, co...
A new Gibbs thermodynamic potential function of ice Ih is proposed to extend and improve already exi...
Very accurate thermodynamic potential functions are available for fluid water, ice, seawater and hum...
The performance of the sea ice component of two ocean general circulation models (OGCMs) is investig...
We explore the properties of the hydrosphere on Europa involving both a modeling technique and exper...
A fully prognostic 1-D thermodynamic model, functional for studies of sea-ice biogeochemistry is d...
International audiencePure ice, brine and solid minerals are the main contributors to sea ice mass. ...
The Finite Element Sea-ice Ocean Model (FESOM) is being utilized with a high resolution mesh focuse...
In this paper, a new predictive model for the ice layer and water film growth, which occurs due to s...
Accurate values of the freezing point of seawater are necessary for considering thermal processes at...
An energy loan sea ice model was developed to manage the energetics of water phase changes in a cons...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
December 1995.Includes bibliographical references.We describe a simple two-layer thermodynamic ocean...
International audienceThe 2004 Gibbs thermodynamic potential function of naturally abundant water ic...
International audienceThe 2003 Gibbs thermodynamic potential function represents a very accurate, co...
A new Gibbs thermodynamic potential function of ice Ih is proposed to extend and improve already exi...
Very accurate thermodynamic potential functions are available for fluid water, ice, seawater and hum...
The performance of the sea ice component of two ocean general circulation models (OGCMs) is investig...
We explore the properties of the hydrosphere on Europa involving both a modeling technique and exper...
A fully prognostic 1-D thermodynamic model, functional for studies of sea-ice biogeochemistry is d...
International audiencePure ice, brine and solid minerals are the main contributors to sea ice mass. ...
The Finite Element Sea-ice Ocean Model (FESOM) is being utilized with a high resolution mesh focuse...
In this paper, a new predictive model for the ice layer and water film growth, which occurs due to s...
Accurate values of the freezing point of seawater are necessary for considering thermal processes at...
An energy loan sea ice model was developed to manage the energetics of water phase changes in a cons...
Description: Outputs from the MIT General Circulation Model (MITgcm) run in an idealized coupled oce...
December 1995.Includes bibliographical references.We describe a simple two-layer thermodynamic ocean...