An Automated Mesoscale Forecast Verification System
Scott Sandgathe
Principal Meteorologist, APL/UW
Traditional
verification schemes tend to penalize mesoscale numerical weather prediction
(NWP) systems, which realistically portray high amplitude, short duration
mesoscale phenomena. Small phase, timing or location errors for high amplitude
features result in apparent poor performance when traditional verification
schemes based on synoptic observations or grid point analyses are employed. Yet
these same NWP systems provide much more realistic and often more operationally
useful depictions of weather events than smoother global NWP or ensemble-mean
systems. Unfortunately, taking into consideration small phase or timing errors
generally requires labor-intensive case studies which are unable to address the
large number of cases required for reliable mesoscale NWP or mesoscale ensemble
verification. NWP centers and forecasters need automated, rapid and more
realistic evaluation of mesoscale NWP and ensemble performance.
The University of
Washington, as part of a DoD-funded interdisciplinary university research
project, is developing an automated mesoscale forecast verification system.
This system follows the ideas of Hoffman, et. al. (1995) and incorporates rapid
search techniques developed by the motion picture industry. The system will be
used to assess the performance of the UW MM5 ensemble forecast system and
provide guidance to Navy and NOAA forecasters in the NW region. Besides
addressing issues of rapid evaluation, the research will also address methods
of evaluating and displaying the relative “goodness” of phase, amplitude, and
distortion errors for customer use.
Recent efforts by Du
and Mullen (2000) and Ebert and McBride (2000) have adapted the Hoffman
technique for verification of precipitation forecasts. In addition to
precipitation verification which is significantly complicated by terrain in the
NW region, the UW group hopes to address overall mesoscale NWP performance on
continuous state variables.