Changes between Version 85 and Version 86 of doc/app/errmsg

Timestamp:

Nov 15, 2011 2:03:21 PM (13 years ago)

Author:

fricke

Comment:

--

doc/app/errmsg

@@ -360 +360 @@
 ||[=#PA0337 PA0337]   ||NetCDF file for "..." data for mask "..." from previous run found but this file cannot be extended because the current output time is less or equal than the last output time on this file. New file is created instead.  ||  ||
 ||[=#PA0338 PA0338]   ||NetCDF file for "..." data for mask "..." from previous run found. This file will be extended.  ||  ||
-||[=#PA0339 PA0339]   ||coupling mode "...: nx+1 in ocean is not divisible without remainder with nx+1 in atmosphere || Jens ||
-||[=#PA0340 PA0340]   ||'coupling mode "...": ny+1 in ocean is not divisible without remainder with ny+1 in atmosphere || Jens ||
+{{{#!tr
+   {{{#!td 
+[=#PA0339 PA0339]
+   }}}
+   {{{#!td 
+coupling mode "...: nx+1 in ocean is not divisible without remainder with nx+1 in atmosphere
+   }}}
+   {{{#!td
+For the coupling between atmosphere and ocean, a smaller grid length in the x-direction can be chosen for the ocean, so that the ocean has more grid points in the x-direction then the atmosphere. In this case, the information must be interpolated for the data exchange between atmosphere and ocean. Therefor it must be ensured that each interpolation interval has the same number of gridpoints. This is ensured if the following equation is fulfilled: 
+{{{#!Latex 
+(nx_o + 1) - INT \left( \frac{nx_o + 1}{nx_a + 1} \right) * (nx_a + 1) = 0 \; ,
+}}}
+with
+{{{#!Latex
+ nx_o,  nx_a
+}}}
+as the number of grid points in the x-direction for the ocean and atmosphere model, respectively. \\ To avoid this error ensure that the equation above is fulfilled.
+   }}}
+}}}
+{{{#!tr
+   {{{#!td 
+[=#PA0340 PA0340]
+   }}}
+   {{{#!td 
+coupling mode "...: ny+1 in ocean is not divisible without remainder with ny+1 in atmosphere
+   }}}
+   {{{#!td
+For the coupling between atmosphere and ocean, a smaller grid length in the y-direction can be chosen for the ocean, so that the ocean has more grid points in the y-direction then the atmosphere. In this case, the information must be interpolated for the data exchange between atmosphere and ocean. Therefor it must be ensured that each interpolation interval has the same number of gridpoints. This is ensured if the following equation is fulfilled: 
+{{{#!Latex 
+(ny_o + 1) - INT \left( \frac{ny_o + 1}{ny_a + 1} \right) * (ny_a + 1) = 0 \; ,
+}}}
+with
+{{{#!Latex
+ ny_o,  ny_a
+}}}
+as the number of grid points in the y-direction for the ocean and atmosphere model, respectively. \\ To avoid this error ensure that the equation above is fulfilled.
+   }}}
+}}}
 ||[=#PA0341 PA0341]   ||Topography is still not allowed with momentum_advec = 'ws-scheme' or scalar_advec = 'ws-scheme'. || Matthias ||
 ||[=#PA0342 PA0342]   ||Non-cyclic lateral boundaries do not allow loop_optimization = 'vector' and ws-scheme'. || Matthias ||