资 源 简 介
idealised two layer model with boussinesq approximation, vertically integrated with free surface to simulate idealised problems of circulation of a two layer stratified fluid (oceanic large scale or estuarine system)
horizontal advection is currently calculated with simple upstream based advection schemes. horizontal diffusion is included as well as coriolis force and internal and external (baroclinic and barotropic) pressure gradients.
the mixing/entrainment (mixing of ligher surface water into the dense bottom water) is parameterised via an empiric formula calculating the amount of entrainment as a function of velocity, layer thickness, rotational forces and density difference between upper and lower layer (Arneborg et al. 2007).
Hannes Rennau
文 件 列 表
src
do_density_advection.F90
cfl_check.F90
ncdf_write.F90
layer_thickness.F90
do_entrainment.F90
ncdf_read.F90
TwoLM.F90
ncdf_header.F90
do_momentum_advection.F90
check.F90
TwoLM.F90.backup
do_elevations.F90
.TwoLM.F90.swp
ncdf_init.F90
do_advection.F90
bott_fric.F90
salinity_init.F90
variables.F90
run
my.cdl
Makefile
bathymetry.nc
