International audienceIn a previous study, the authors studied a low order pressure gradient force (PGF) scheme referred to as the Primitive-Modified scheme, that appears to be equivalent to the Pressure-Jacobian PGF ( Lin, 1997). The scheme was successfully tested on the seamount experiment using a simplified equation of state (EOS). Yet, a complete equation of state, including compressibility effect, can raise a serious problem of accuracy. A new implementation is thus proposed in the present paper. The scheme is rewritten using a (numerically equivalent) geopotential formulation. The PGF truncation errors are removed by computing the EOS compressibility terms with potential temperature and salinity interpolated on a suitable geopotential...
This work will focus on how the internal pressure gradient errors affect the numerical instability i...
A semi-implicit, control-volume, nonhydrostatic model is presented. Advection is fifth order with re...
A new density variable, empirically corrected for pressure, is constructed. This is done by first fi...
International audienceIn a previous study, the authors studied a low order pressure gradient force (...
It is shown that the differencing scheme cited here, though conventional, is not hydrostatically inc...
Potential density referenced to sea level pressure $(\sigma\sb0$) has shown its usefulness as vertic...
[1] How to reduce the horizontal pressure gradient error is a key issue in terrain-following coastal...
International audienceThis paper revisits the classic seamount test used in numerous previous studie...
Terrain-following (sigma-coordinate) models are widely used. They are often advantageous when dealin...
© 2017 Elsevier Ltd Discretisation of the horizontal pressure gradient force in layered ocean models...
Discretisation of the horizontal pressure gradient force in layered ocean models is a challenging ta...
How to reduce the horizontal pressure gradient error is a key issue of using s-coordinate ocean mode...
A new set of approximations to the standard TEOS-10 equation of state are presented. These follow a ...
Eight equations of state (EOS) have been evaluated for the simulation of compressible liquid water p...
There is a growing realization that the nonlinear nature of the equation of state has a deep impact ...
This work will focus on how the internal pressure gradient errors affect the numerical instability i...
A semi-implicit, control-volume, nonhydrostatic model is presented. Advection is fifth order with re...
A new density variable, empirically corrected for pressure, is constructed. This is done by first fi...
International audienceIn a previous study, the authors studied a low order pressure gradient force (...
It is shown that the differencing scheme cited here, though conventional, is not hydrostatically inc...
Potential density referenced to sea level pressure $(\sigma\sb0$) has shown its usefulness as vertic...
[1] How to reduce the horizontal pressure gradient error is a key issue in terrain-following coastal...
International audienceThis paper revisits the classic seamount test used in numerous previous studie...
Terrain-following (sigma-coordinate) models are widely used. They are often advantageous when dealin...
© 2017 Elsevier Ltd Discretisation of the horizontal pressure gradient force in layered ocean models...
Discretisation of the horizontal pressure gradient force in layered ocean models is a challenging ta...
How to reduce the horizontal pressure gradient error is a key issue of using s-coordinate ocean mode...
A new set of approximations to the standard TEOS-10 equation of state are presented. These follow a ...
Eight equations of state (EOS) have been evaluated for the simulation of compressible liquid water p...
There is a growing realization that the nonlinear nature of the equation of state has a deep impact ...
This work will focus on how the internal pressure gradient errors affect the numerical instability i...
A semi-implicit, control-volume, nonhydrostatic model is presented. Advection is fifth order with re...
A new density variable, empirically corrected for pressure, is constructed. This is done by first fi...