Modelling the surface orography at an appropriate resolution is crucial to an effective forecast. However, at some level, there always will be smoothing that misses important detail. Model orography is derived from a data set with a resolution of about 1km, which contains:
This detailed data is upscaled (aggregated) to the coarser model resolution.
The standard deviation, slope, orientation and anisotropy of the surface in each grid box can be important for assessment of sub-grid scale local wind effects, solar heating etc. These are not yet included directly in the atmospheric models. However, in mountainous areas the upscaled orography is supplemented by fields describing some characteristics of the sub-grid orography (sub-grid scale slope, orientation and anisotropy of the orography - GRIB fields are available for use by forecasters locally). This allows better parameterisation of the effects of gravity waves and better representation of flow-dependent blocking of the airflow (e.g. cold air drainage trapped in valleys can effectively raise the local orography).
Compare HRES or medium range ENS model orography (resolution 9km), and extended-range ENS model orography (resolution 36km).
In the diagrams, note:
Orography has a direct bearing upon the drag on the lower layers of the model atmosphere. Also, in some atmospheric situations, it influences the development of standing waves through the atmosphere and possibly inducing upper air drag if they break. Orographic enhancement of precipitation depends upon the detail of the model orography.
Fig2.1.3.2-1: Schematic of the preparation of the data sets to characterize the sub-grid scale orography.
Fig2.1.3.2-2: Schematic of the spectral representation of orography. Model orography matches true orography over large parts of the earth but is less exact in rugged mountainous regions.
Generally model orography matches true orography over large parts of the earth. However, the spectral representation of orography in the IFS can:
See also selection of grid points for meteograms and model representation of orography.