Difference between revisions of "Mohid Best Practices"
From MohidWiki
Paulochambel (talk | contribs) (Created page with "== Downscalling from 3D solutions (e.g. MyOcean, RTOFS) == === Download === MyOcean NOOA : GFS, RTOFS === Conversion === grib-netcdf-hdf5 === Interpolation ==== z-level t...") |
Paulochambel (talk | contribs) (→Downscalling from 3D solutions (e.g. MyOcean, RTOFS)) |
||
| Line 1: | Line 1: | ||
| − | == Downscalling from 3D solutions | + | == Downscalling from 3D solutions == |
=== Download === | === Download === | ||
| Line 11: | Line 11: | ||
grib-netcdf-hdf5 | grib-netcdf-hdf5 | ||
| − | === Interpolation | + | === Interpolation === |
z-level to MOHID geo | z-level to MOHID geo | ||
| Line 34: | Line 34: | ||
| − | === Spin up ==== | + | ==== Spin up ==== |
slow connection of terms: wind, tide, atmospheric pressure, baroclinc force | slow connection of terms: wind, tide, atmospheric pressure, baroclinc force | ||
Revision as of 14:34, 9 May 2013
Contents
Downscalling from 3D solutions
Download
MyOcean
NOOA : GFS, RTOFS
Conversion
grib-netcdf-hdf5
Interpolation
z-level to MOHID geo
bilinear vs triangulation
linear horizontally and vertically
Boundary conditions
Open boundary
high frequency vs low frequency = mohid 2D + 3D external solution
radiation + flow relaxation scheme
Surface
impose wind stress, solar radiation
Compute sensible heat, latent heat based in the water/air temperature, wind, relative humidity
Spin up
slow connection of terms: wind, tide, atmospheric pressure, baroclinc force
initial condition : salinity and temperature from external solutions, null sea level gradient and null velocities
initial strong relaxation of temperature and salinity in all domain
