Difference between revisions of "Module Geometry"
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TYPE : char - !Type of vertical coordinate of the domain | TYPE : char - !Type of vertical coordinate of the domain | ||
!Multiple options: FIXSPACING, SIGMA, | !Multiple options: FIXSPACING, SIGMA, | ||
− | !LAGRANGIAN, CARTESIAN, HARMONIC, FIXSEDIMENT | + | !LAGRANGIAN, CARTESIAN, HARMONIC, FIXSEDIMENT, CARTESIANTOP. |
LAYERS : int - !Number of layers | LAYERS : int - !Number of layers | ||
EQUIDISTANT : real [0] !Equidistant layers spacing in meters | EQUIDISTANT : real [0] !Equidistant layers spacing in meters | ||
Line 75: | Line 75: | ||
EMPTY_TOP_LAYERS : int [0] !Number of empty layers counting from top | EMPTY_TOP_LAYERS : int [0] !Number of empty layers counting from top | ||
DOMAINDEPTH : real | DOMAINDEPTH : real | ||
+ | <enddomain> |
Revision as of 13:18, 13 November 2009
Contents
Overview
Module Geometry handles the vertical discretization in MOHID. It was designed to divide the water column (in MOHID Water) or the soil compartment (in MOHID Land) in different vertical coordinates: Sigma, Cartesian, Lagrangian, Fixed Spacing, Harmonic, etc. A subdivision of the vertical domain into different sub-domains using different vertical coordinate systems is also possible.
General options
- Minimum depth
Vertical coordinate system
Sigma
Cartesian
The Cartesian coordinate can be used with or without shaved cells.
Fixspacing
The Fixed Spacing coordinate allows the user to study flows close to the bottom.
Lagrangian
The Lagrangian coordinate moves the upper and lower faces with the vertical flow velocity.
Harmonic
The Harmonic coordinate works like the Cartesian coordinate, just that the horizontal faces close to the surface expand and collapse depending on the variation of the surface elevation. This coordinate was implemented in the geometry module to simulate reservoirs.
Fixsediment
SigmaTop
Cartesiantop
Cartesiantop is equal to cartesian but builds layers from top to bottom. This type of coodinates are used for Mohid Land. The top is the topography and the bottom is the non-porousmedia (rock).
Distances
Public routines
- ModuleHorizontalGrid
- GetHorizontalGrid(HorizontalGridID, XX_IE, YY_IE, XX_Z, YY_Z,XX_U, YY_U, XX_V, YY_V, XX_Cross, YY_Cross, DXX, DYY, DZX, DZY, DUX, DUY, DVX, DVY, XX, YY, XX2D_Z, YY2D_Z, STAT)
- ModuleGeometry
- GetGeometryDistances(GeometryID, SZZ, DZZ, DWZ, DUZ, DVZ, DZI, DZE,ZCellCenter, ActualTime, STAT)
Areas
Volumes
Bathymetry consistency diagnostic
Once the vertical discretization is imposed and the bathymetry is chosen, the bottom layer can yield stability problems when using shaved cells. You can have very thin bottom cell next to a very wide bottom cell. To diagnose the existence of such problematic cells, a geometry diagnostic tool was developed.
Input data file
Keywords
IMPERMEABILITY : 0/1 - !Consider impermeable cell faces IMPER_COEF_U : real [1] ! IMPER_COEFX_U : real [0] ! IMPER_COEF_V : real [1] ! IMPER_COEFX_V : real [0] ! <begindomain> ID : int - !Domain ID TYPE : char - !Type of vertical coordinate of the domain !Multiple options: FIXSPACING, SIGMA, !LAGRANGIAN, CARTESIAN, HARMONIC, FIXSEDIMENT, CARTESIANTOP. LAYERS : int - !Number of layers EQUIDISTANT : real [0] !Equidistant layers spacing in meters LAYERTHICKNESS : real vector - !If not equidistant specifies layers thickness !starting from bottom layer (e.g. 50. 20. 10. 5.) TOLERANCEDEPTH : real [0.05] !Just for SIGMA,ISOPYCNIC, LAGRANGIAN coordinates TOTALTHICKNESS : real - !Total domain thickness !(Just for FIXSPACING, FIXSEDIMENT, SOIL_TOPLAYER) EMPTY_TOP_LAYERS : int [0] !Number of empty layers counting from top DOMAINDEPTH : real <enddomain>