P1.8
The development of forecast confidence measures using NCEP ensembles
Robert Hart, Florida State University, Tallahassee, FL; and A. V. Durante and A. I. Watson
Ensemble model data can provide a wealth of knowledge to forecasters
especially in terms of forecast confidence. A model run where members
diverge corresponds to a low confidence forecast while a model run where
members converge corresponds to a forecast of high confidence. The current
NWS graphically based forecasts accessible to the public do not show this
measure of uncertainty and thus communicate an often exaggerated sense of
precision and confidence.
Starting August 2004 and extending into 2007, analysis of about 3 years of
individual global GFS ensemble data is occurring as part of a
COMETcooperative project with the NWS Office in Tallahassee. A climatology
for each GFS ensemble member is being developed as a function of variable,
location, time of year, and forecast length. Once the normalized
climatology distributions are calculated, forecast confidence/uncertainty
measures can be developed from comparing the normalized spread of the
real-time GFS ensemble members to the average spread of the GFS ensemble
climatology. This normalized spread will also be compared to the typical
spread for that time of year and location to arrive at a relative measure
of forecast uncertainty. If the current model ensemble uncertainty is
greater (less) than the uncertainty of the model ensemble climatology,
then there is a lower (higher) than normal confidence.
Confidence graphics have been developed and analyzed
(http://moe.met.fsu.edu/confidence) to examine how confidence values
behave within certain synoptic situations. Preliminary results have shown
that when the forecast confidence is above normal, the average NWS
forecast error is approximately 40 to 50% of the error when the forecast
confidence is below normal. A confidence climatology and several case
studies will be examined in this paper to illustrate how the forecast
confidence graphics can be used to not only speed up the forecast process
for the forecaster, but also to improve the accuracy of resulting
forecasts by knowing when using climatology for a forecast is most
appropriate.
Poster Session 1, Posters: Probability and Statistics in the Atmospheric Sciences
Wednesday, 23 January 2008, 2:30 PM-4:00 PM, Exhibit Hall B
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