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  • systematic errors reflect the limitations of the NWP model’s ability to simulate the physical and dynamic properties of the system.
  • non-systematic errors reflect synoptic phase and intensity errors (as indicated by the left hand green arrow in Fig3.2-1).
  • systematic and non-systematic errors occur when the NWP output is verified against point observations.  The NWP output may not be representative of the location, height, aspect of the observation or capture sub-grid scale variability.

 

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Fig3.2-1:  Comparison between NWP model output and observations ought ideally to follow a two-step procedure:

  • first step: compare grid point average to observation area average.  The systematic errors are then due to model shortcomings; the non-systematic errors stem from synoptic phase and intensity errors.
  • second step: compare the systematic errors between observation average and point observation.  The systematic errors come from station representativeness (i.e. the location, height and aspect of the observation).  The non-systematic errors come from sub-grid scale variability.


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Fig3.2-2:  In reality, the comparison between NWP and observations must for simplicity bypass the area average stage.  This results in the systematic and non-systematic errors arising from distinctly different sources.  The effects related to the two green arrows in Fig3.2-1 are here combined into one.

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