Difference between revisions of "Mohid Ocean Downscalling"
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MSMalhadas (talk | contribs) (→Bathymetry transition) |
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MyOcean | MyOcean | ||
− | NOOA : GFS, RTOFS | + | To download my ocean solution go to http://www.myocean.eu/. and click in ACCES THE CATALOGUE. In block 1 choose "Global Ocean", in 2 the parameters and in 3 choose forecast products. After fill all the blocks click search and in the next web page choose DATA ACCES and then GO. Prescribe the user name and password and then choose the dates and area of interest. |
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+ | NOOA : GFS, RTOFS | ||
== Conversion == | == Conversion == |
Revision as of 15:43, 10 May 2013
Contents
Download
MyOcean
To download my ocean solution go to http://www.myocean.eu/. and click in ACCES THE CATALOGUE. In block 1 choose "Global Ocean", in 2 the parameters and in 3 choose forecast products. After fill all the blocks click search and in the next web page choose DATA ACCES and then GO. Prescribe the user name and password and then choose the dates and area of interest.
NOOA : GFS, RTOFS
Conversion
grib-netcdf-hdf5
Bathymetry transition
Running tool SmoothBathymNesting.exe
Example of the input file SmoothBathymNesting.dat
! File bathymetry of the external 3D solution FATHER_BATIM : !Bathymetry File of MOHID solution SON_BATIM : !New Bathymetry File NEW_SON_BATIM : <begin_coef> NAME : generic property !Name of generic property INITIALIZATION_METHOD : sponge !Type of initialization used DEFAULTVALUE : 1 !0-external 3D solution, 1-MOHID solution SPONGE_OUT : 0 SPONGE_CELLS : 10 !sponge cells number SPONGE_EVOLUTION : 2 !1-exponential, 2-linear <end_coef>
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