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Composite-based Verification
Jason Nachamkin Naval Research Laboratory Monterey, CA References Nachamkin, J. E., 2004: Mesoscale verification using meteorological composites. Mon. Wea. Rev., 132, Nachamkin, J. E., S. Chen, and J. S.Schmidt 2005: Evaluation of heavy precipitation forecasts using composite-based methods: A distributions-oriented approach. Mon. Wea. Rev.,133,
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Meteorological Fields
Observations (gridded, point obs, swaths) SSMI winds RFC/ST4, BMRC rainfall Satellite rainfall estimates Storm reports? Forecast data Wind speed/direction Rainfall (resolved, parameterized, snow)
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The Composite Method SSMI Winds Composite Forecast m s-1 27 km COAMPS®* wind speed (2001) Identify events of interest in the forecasts and observations Collect coordinated samples Compare forecast distribution to observed distribution *COAMPS® is a registered trademark of the Naval Research Laboratory
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Quantifying the Results
Given FC Event All Events ≥ 25 mm 24-hr FCST-OBS Bias (mm) mm Given OB Event 27 km COAMPS® rainfall (summer 2003) mm 810 x 810 km
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Mistral Statistics Given an event is predicted
All northwest winds ≥ 12.5 m s-1 Given an event is predicted Given an event is observed 27 km COAMPS® winds (2001) 810 x 810 km Dist of all known FCST events Dist of all known OBS events
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Strengths Simplicity Flexibility Sampling and averages
Minimal data manipulation Straightforward uncertainty calculations No dependence on field structure Flexibility Many data types accepted Multiple variables validated Database capable Probabilistic statistics applicable
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Weaknesses Simplicity Dependent on event parameters
Only general systematic biases No rotation/shape parameters Difficult to apply to single cases Dependent on event parameters Not good for very large, complex shapes (synoptic cloud fields) No funding
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Case Study All Events ≥ 0.5 inches
WRF2CAPS 13 May WRF4NCAR 13 May WRF4NCAR 1 June in×100 WRF4NCAR 1 June mm 400 x 400 km COAMPS® 27 km 400 x 400 km WRF2CAPS 13 May best overall WRF4NCAR 1 June missed forecasts High-res forecasts show improved ability to resolve more observed events at smaller scales
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