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Difference between revisions of "Mohid Ocean Downscalling"

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(Bathymetry transition)
(Download)
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MyOcean
 
MyOcean
  
NOOA : GFS, RTOFS  
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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 16:43, 10 May 2013

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