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Difference between revisions of "Geostrophic Initialization"

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(Example File)
 
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''''Warning: this page is under construction - do not use it directely''''
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= Description =
 
= Description =
 +
 +
In this initialization methodology all forces are switched (except tidal force) at the first iteration. The velocity and sea surface height initial fields have non zero values consistent with the salinity and temperature initial fields, trough the geostrophic equilibrium. If the initialization is made in a level 2 embedded in a 2D  tidal model (level 1), tidal force must be switched progressively along a selected period (in level 1).
  
 
= Example File =
 
= Example File =
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  GEOST_INITIALIZATION      : 1  ! Select geostrophic initialization
 
  GEOST_INITIALIZATION      : 1  ! Select geostrophic initialization
  SUBMODEL_FATHER_HOT_START : 0  ! MUST BE ZERO for geostrophic initialization
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  SUBMODEL_FATHER_HOT_START : 0  ! must be zero for embedded models to prevent the imposition of father values
 
   
 
   
 +
! imposed water level initial solution
 
  <begin_waterlevel>
 
  <begin_waterlevel>
  NAME                      : water level
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  NAME                      : water level  
 
  DEFAULTVALUE              : 0
 
  DEFAULTVALUE              : 0
 
  INITIALIZATION_METHOD    : HDF
 
  INITIALIZATION_METHOD    : HDF
 
  FILENAME                  : ..\..\GeneralData\Mercator\Mercator_ANA_Level2_Jun.hdf5
 
  FILENAME                  : ..\..\GeneralData\Mercator\Mercator_ANA_Level2_Jun.hdf5
 
  TYPE_ZUV                  : z
 
  TYPE_ZUV                  : z
  ADDING_FACTOR   : 0.0  ! This factor adds to the mean level of the Initial Solution
+
  ADDING_FACTOR             : 0.0  ! This factor adds to the mean level of the Initial Solution
 
  <end_waterlevel>
 
  <end_waterlevel>
 
   
 
   
  TIDE                      : 1    ! If tide is to be initializated, it MUST be 1
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  TIDE                      : 0
  TIDEPOTENTIAL            : 1
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  TIDEPOTENTIAL            : 1   ! If model run embedded in a 2D tide model
 
  CONTINUOUS                : 0    ! The model cannot be a continous run
 
  CONTINUOUS                : 0    ! The model cannot be a continous run
 
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RESIDUAL                : 1
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DATA_ASSIMILATION         : 1
ENERGY                  : 1
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BRFORCE                   : 1
CONTINUOUS              : 0
+
BRGEOMETRY               : 1
 
+
BRWATERLEVEL             : 0
DATA_ASSIMILATION       : 1
+
BRFORCE                 : 1
+
RADIATION                 : 2
BRGEOMETRY               : 1
+
LOCAL_SOLUTION           : 3   ! 5 or 7 if model runs embedded
BRWATERLEVEL             : 0
+
SUBMODEL                 : 0   ! 1 if model runs embedded
 
+
MISSING_NULL             : 1
 
+
 
+
WIND                     : 1
RADIATION               : 2
+
ATM_PRESSURE             : 1
LOCAL_SOLUTION           : 3
+
ATM_PRESSURE_TYPE         : 2    ! can be 1 or 2
 
+
ATM_RAMP                 : 0
SUBMODEL                 : 0
+
ATM_PERIOD               : 86400  
MISSING_NULL             : 1
+
IMPOSE_INVERTED_BAROMETER : 1
 
+
WIND                     : 1
+
BIHARMONIC               : 1
!WIND_SMOOTH_PERIOD      : 86400
+
BIHARMONIC_COEF           : 1e10
!WIND_SMOOTH_PERIOD      : 2678400.
 
 
 
 
 
ATM_PRESSURE             : 1
 
ATM_PRESSURE_TYPE       : 2
 
ATM_RAMP                 : 0
 
!ATM_PERIOD               : 86400
 
!ATM_PERIOD              : 2678400.
 
 
 
 
 
IMPOSE_INVERTED_BAROMETER : 1
 
 
 
!5 períodos inérciais na nossa costa
 
INERTIAL_PERIODS        : 6
 
INITIAL_ELEVATION        : 0
 
SURFACEWATERFLUX        : 0
 
WATER_DISCHARGES        : 0
 
MOMENTUM_DISCHARGE      : 0
 
 
 
FLATHER_COLD_PERIOD      : 0.
 
 
 
BIHARMONIC               : 1
 
BIHARMONIC_COEF         : 1e10
 

Latest revision as of 11:05, 31 January 2012

'Warning: this page is under construction - do not use it directely'

Description

In this initialization methodology all forces are switched (except tidal force) at the first iteration. The velocity and sea surface height initial fields have non zero values consistent with the salinity and temperature initial fields, trough the geostrophic equilibrium. If the initialization is made in a level 2 embedded in a 2D tidal model (level 1), tidal force must be switched progressively along a selected period (in level 1).

Example File

Hydrodynamic_1.dat

OUTPUT_TIME               : 0  3600
SURFACE_OUTPUT_TIME       : 0  3600

GEOST_INITIALIZATION      : 1   ! Select geostrophic initialization
SUBMODEL_FATHER_HOT_START : 0   ! must be zero for embedded models to prevent the imposition of father values 

! imposed water level initial solution
<begin_waterlevel>
NAME                      : water level 
DEFAULTVALUE              : 0
INITIALIZATION_METHOD     : HDF
FILENAME                  : ..\..\GeneralData\Mercator\Mercator_ANA_Level2_Jun.hdf5
TYPE_ZUV                  : z
ADDING_FACTOR             : 0.0  ! This factor adds to the mean level of the Initial Solution
<end_waterlevel>

TIDE                      : 0
TIDEPOTENTIAL             : 1    ! If model run embedded in a 2D tide model
CONTINUOUS                : 0    ! The model cannot be a continous run

DATA_ASSIMILATION         : 1
BRFORCE                   : 1
BRGEOMETRY                : 1
BRWATERLEVEL              : 0

RADIATION                 : 2
LOCAL_SOLUTION            : 3    ! 5 or 7 if model runs embedded
SUBMODEL                  : 0    ! 1 if model runs embedded
MISSING_NULL              : 1

WIND                      : 1
ATM_PRESSURE              : 1
ATM_PRESSURE_TYPE         : 2    ! can be 1 or 2
ATM_RAMP                  : 0
ATM_PERIOD                : 86400 
IMPOSE_INVERTED_BAROMETER : 1

BIHARMONIC                : 1
BIHARMONIC_COEF           : 1e10