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NPVU - National Precipitation Verification Unit
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How the NPVU interpolates the Forecast and Observation Grids
NOTE: The gray text will be valid when the NDFD QPF verification implementation process is complete.
NPVU Receives: Converts to 32km HRAP by: Converts to 4km HRAP grid by:
4km QPE from RFC Spatial Average No Conversion Needed
10km QPF from RFC Area Preservation Technique Area Preservation Technique
1x1 degree AVN Area Preservation Technique Linear Interpolation
32km Eta Change coverage area Linear Interpolation
90km NGM Area Preservation Technique Linear Interpolation
32km HPC No Conversion Needed Linear Interpolation
5km QPF from NDFD Spatial Average Area Preservation Technique

Method Definitions:

Area Preservation Technique
The Area Preservation Technique is an interpolation method that was developed by NCEP/EMC to interpolate QPF from native NWP model grids to output grids, while preserving the aerial amounts of QPF. This technique is similar to calculating an integral in calculus. Where the one grid is divided into sub-grids and then used to ensure that the output grid is coarser or finer than the original grid. It is most beneficial when the ratio between original to output or output to original is less than 4 to 1. If the output is much finer than the original then linear interpolation is better or if the output is much coarser than the original than spatial averaging is better. These two methods work just as well but without as much computation.


Change coverage area
The Eta is received on the 32km grid but it is for a much larger geographical area. This area is then "cut" down to the grid size needed to cover just the CONUS RFC areas.


Linear Interpolation
Come back later to learn more


No Conversion Needed
This is the exact grid the NPVU verifies on, so no change is needed


Spatial Average
The spatial averaging technique is a simple average of all of the original grid points with in the area of the output grid.



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Page last modified: Tuesday, 09-Nov-2004 19:11:43 UTC