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Copy file name to clipboardExpand all lines: flopy/mf6/data/dfn/exg-gwegwe.dfn
+2-2Lines changed: 2 additions & 2 deletions
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@@ -24,7 +24,7 @@ shape (naux)
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reader urword
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optional true
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longname keyword to specify aux variables
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description an array of auxiliary variable names. There is no limit on the number of auxiliary variables that can be provided. Most auxiliary variables will not be used by the GWF-GWF Exchange, but they will be available for use by other parts of the program. If an auxiliary variable with the name ``ANGLDEGX'' is found, then this information will be used as the angle (provided in degrees) between the connection face normal and the x axis, where a value of zero indicates that a normal vector points directly along the positive x axis. The connection face normal is a normal vector on the cell face shared between the cell in model 1 and the cell in model 2 pointing away from the model 1 cell. Additional information on ``ANGLDEGX'' is provided in the description of the DISU Package. If an auxiliary variable with the name ``CDIST'' is found, then this information will be used as the straight-line connection distance, including the vertical component, between the two cell centers. Both ANGLDEGX and CDIST are required if specific discharge is calculated for either of the groundwater models.
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description an array of auxiliary variable names. There is no limit on the number of auxiliary variables that can be provided. Most auxiliary variables will not be used by the GWE-GWE Exchange, but they will be available for use by other parts of the program. If an auxiliary variable with the name ``ANGLDEGX'' is found, then this information will be used as the angle (provided in degrees) between the connection face normal and the x axis, where a value of zero indicates that a normal vector points directly along the positive x axis. The connection face normal is a normal vector on the cell face shared between the cell in model 1 and the cell in model 2 pointing away from the model 1 cell. Additional information on ``ANGLDEGX'' is provided in the description of the DISU Package. If an auxiliary variable with the name ``CDIST'' is found, then this information will be used as the straight-line connection distance, including the vertical component, between the two cell centers. Both ANGLDEGX and CDIST are required if specific discharge is calculated for either of the groundwater models.
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block options
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name boundnames
@@ -162,7 +162,7 @@ tagged false
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reader urword
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optional false
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longname obs6 input filename
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description is the file name of the observations input file for this exchange. See the ``Observation utility'' section for instructions for preparing observation input files. Table \ref{table:gwe-obstypetable} lists observation type(s) supported by the GWE-GWE package.
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description is the file name of the observations input file for this exchange. See the ``Observation utility'' section for instructions for preparing observation input files. Table \ref{table:gwe-obstypetable} lists observation type(s) supported by the GWE-GWE Exchange Package.
longname longitudinal dispersivity in horizontal direction
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description longitudinal dispersivity in horizontal direction. If flow is strictly horizontal, then this is the longitudinal dispersivity that will be used. If flow is not strictly horizontal or strictly vertical, then the longitudinal dispersivity is a function of both ALH and ALV. If mechanical dispersion is represented (by specifying any dispersivity values) then this array is required.
@@ -45,6 +56,7 @@ type double precision
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shape (nodes)
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reader readarray
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layered true
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netcdf true
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optional true
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longname longitudinal dispersivity in vertical direction
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description longitudinal dispersivity in vertical direction. If flow is strictly vertical, then this is the longitudinal dispsersivity value that will be used. If flow is not strictly horizontal or strictly vertical, then the longitudinal dispersivity is a function of both ALH and ALV. If this value is not specified and mechanical dispersion is represented, then this array is set equal to ALH.
@@ -55,6 +67,7 @@ type double precision
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shape (nodes)
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reader readarray
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layered true
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netcdf true
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optional true
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longname transverse dispersivity in horizontal direction
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description transverse dispersivity in horizontal direction. This is the transverse dispersivity value for the second ellipsoid axis. If flow is strictly horizontal and directed in the x direction (along a row for a regular grid), then this value controls spreading in the y direction. If mechanical dispersion is represented (by specifying any dispersivity values) then this array is required.
@@ -65,6 +78,7 @@ type double precision
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shape (nodes)
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reader readarray
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layered true
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netcdf true
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optional true
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longname transverse dispersivity in horizontal direction
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description transverse dispersivity in horizontal direction. This is the transverse dispersivity value for the third ellipsoid axis. If flow is strictly horizontal and directed in the x direction (along a row for a regular grid), then this value controls spreading in the z direction. If this value is not specified and mechanical dispersion is represented, then this array is set equal to ATH1.
@@ -75,6 +89,7 @@ type double precision
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shape (nodes)
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reader readarray
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layered true
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netcdf true
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optional true
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longname transverse dispersivity when flow is in vertical direction
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description transverse dispersivity when flow is in vertical direction. If flow is strictly vertical and directed in the z direction, then this value controls spreading in the x and y directions. If this value is not specified and mechanical dispersion is represented, then this array is set equal to ATH2.
@@ -85,6 +100,7 @@ type double precision
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shape (nodes)
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reader readarray
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layered true
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netcdf true
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optional true
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longname thermal conductivity of the simulated fluid
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description thermal conductivity of the simulated fluid. Note that the CND Package does not account for the tortuosity of the flow paths when solving for the conductive spread of heat. If tortuosity plays an important role in the thermal conductivity calculation, its effect should be reflected in the value specified for KTW.
@@ -95,7 +111,8 @@ type double precision
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shape (nodes)
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reader readarray
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layered true
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netcdf true
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optional true
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longname thermal conductivity of the aquifer material
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description thermal conductivity of the aquifer material
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description thermal conductivity of the solid aquifer material
description is the column spacing in the row direction.
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default_value 1.0
@@ -94,6 +148,7 @@ name delc
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type double precision
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shape (nrow)
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reader readarray
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netcdf true
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longname spacing along a column
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description is the row spacing in the column direction.
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default_value 1.0
@@ -103,6 +158,7 @@ name top
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type double precision
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shape (ncol, nrow)
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reader readarray
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netcdf true
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longname cell top elevation
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description is the top elevation for each cell in the top model layer.
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default_value 1.0
@@ -113,6 +169,7 @@ type double precision
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shape (ncol, nrow, nlay)
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reader readarray
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layered true
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netcdf true
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longname cell bottom elevation
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description is the bottom elevation for each cell.
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default_value 0.
@@ -123,6 +180,7 @@ type integer
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shape (ncol, nrow, nlay)
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reader readarray
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layered true
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netcdf true
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optional true
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longname idomain existence array
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description is an optional array that characterizes the existence status of a cell. If the IDOMAIN array is not specified, then all model cells exist within the solution. If the IDOMAIN value for a cell is 0, the cell does not exist in the simulation. Input and output values will be read and written for the cell, but internal to the program, the cell is excluded from the solution. If the IDOMAIN value for a cell is 1, the cell exists in the simulation. If the IDOMAIN value for a cell is -1, the cell does not exist in the simulation. Furthermore, the first existing cell above will be connected to the first existing cell below. This type of cell is referred to as a ``vertical pass through'' cell.
description is the top elevation for each cell in the top model layer.
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@@ -91,6 +145,7 @@ type double precision
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shape (ncpl, nlay)
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reader readarray
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layered true
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netcdf true
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longname model bottom elevation
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description is the bottom elevation for each cell.
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@@ -100,6 +155,7 @@ type integer
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shape (ncpl, nlay)
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reader readarray
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layered true
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netcdf true
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optional true
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longname idomain existence array
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description is an optional array that characterizes the existence status of a cell. If the IDOMAIN array is not specified, then all model cells exist within the solution. If the IDOMAIN value for a cell is 0, the cell does not exist in the simulation. Input and output values will be read and written for the cell, but internal to the program, the cell is excluded from the solution. If the IDOMAIN value for a cell is 1, the cell exists in the simulation. If the IDOMAIN value for a cell is -1, the cell does not exist in the simulation. Furthermore, the first existing cell above will be connected to the first existing cell below. This type of cell is referred to as a ``vertical pass through'' cell.
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