The atmospheric model uses a Reduced Gaussian Octahedral grid.  This is triangular in nature and NWP model values are interpolated both onto and from the grid by MIR (Meteorological Interpolation and Regridding) using a triangular interpolation technique which:


Fig33.A: The Reduced Gaussian grid is triangular in nature.  The interpolation uses the three corner points (black points) closest to the selected location (red point) and takes a weighted average based upon the proximity of the point to the to vertices to arrive at the interpolated value.  

In deriving a value for point P the weighting factor apportioned to each point A,B,C is equal to the area of the diametrically opposite triangle. Therefore the weighting for:


A special case then arises when Point P lies on the line directly between two points. (see Fig33.B).

Fig33.B: Sometimes a point lies directly between two grid points. The interpolation then takes a weighted average based upon the ratio of distances from the two end points (black points) each side of selected location (red point) to arrive at the interpolated value.

The weighting factor apportioned to each point is by linear interpolation.  Therefore the weighting for: