...
| Info |
|---|
Note that as a consequence, MIR does not apply land-sea mask processing when using the nearest neighbour method, which was the case in EMOSLIB. Actually, the EMOSLIB interpolation "nearest neighbour" and "nearest lsm" produce the same results. |
Grid to grid interpolations
EMOSLIB cannot handle interpolations from a regular latitude-longitude grid to a reduced gaussian, but MIR does not have that limitation. Interpolations from any global regular or reduced gaussian or latitude-longitude grids to regular or reduced gaussian or regular latitude longitude grids are now supported in MIR.
Spectral to grid point transformations
...
RESOL=AV uses wrong intermediate Gaussian grid
When using RESOL=AV and transforming from spectral to grid, the corresponding intermediate Gaussian grid to be used should be the cubic reduced Gaussian grid by default (i.e., O = T+1), as described above. However, at this point MIR uses a full (regular) gaussian grid with linear truncation (i.e., F = (T+1)/2).
| Info |
|---|
This issue has been resolved in a version of the MARS client using MIR (version 0.8.5) released on 14 November 2017. |
Winds on rotated grids
There are known issues with wind fields when working with rotated grids. In particular, wind speeds are correct but the direction is wrong due to a problem in computing the angles.
| Info |
|---|
This issue has been resolved in a version of the MARS client using MIR (version 0.8.5) released on 14 November 2017. |
...