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Static fields are archived only as of the analysis type. Even For users' convenience, even they are invariant fields for users' convenience , they should be archived for all analysis output times stated above. In case of ensemble products they should be archived with all ensemble members (again as of the analysis type only). The surface roughness could be either static or changing field parameter depending on model and should be handled accordingly as a static or a prognostic model field. |
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- COSMO: 8 soil levels/layers (sot on levels the rest on layers)
level borders at 0, 1, 3, 9, 27, 81, 243, 729, 2187 cm - HARMONIE: 3 soil levels/layers (sot on levels, vsw on layers)
level depths are grid dependant MESCAN-SURFEX:TBD
- MO: 4 soil layers (both sot and vsw on layers)
level borders at 0, 0.1, 0.35, 1 and 3 m
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The soil depth is considered as a static field. It could be either a constant or a grid dependant parameter depending on model soil scheme. As the other static fields for users' convenience it should be archived for all analysis output times. In case of ensemble products it should be archived with all ensemble members (again as of the analysis type only). |
Soil | Abbreviation | Unit |
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Liquid non-frozen volumetric soil water | liqvsm | m3 m-3 |
vsw | m3 m-3 | |
sot | K | |
Soil depth | sod | m |
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