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An Examination of the Diurnal Cycle in the NCEP GFS (and Eta) Model Precipitation Forecasts (during NAME). John Janowiak, Valery Dagostaro*, Vern Kousky, Bob Joyce Climate Prediction Center/NCEP/NWS, Camp Springs, MD Meteorological Development Laboratory/NWS, Silver Spring, MD.
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An Examination of the Diurnal Cycle in the NCEP GFS (and Eta) Model Precipitation Forecasts (during NAME) John Janowiak, Valery Dagostaro*, Vern Kousky, Bob Joyce Climate Prediction Center/NCEP/NWS, Camp Springs, MD Meteorological Development Laboratory/NWS, Silver Spring, MD 30th Climate Diagnostics and Prediction Workshop, Penn State University, October 26, 2005
MODEL FORECASTS Study Period: July 12 – August 15, 2004 (during NAME field campaign) Every 3 hours after 1st 12 hours from 00Z runs (12h, 15h, …, 36h) 1o 1o x lat/lon grid
VALIDATION DATA • A new member of the “MORPH” family: “RMORPH” (Research-quality) • Land: CPC daily gauge analysis (Higgins & Shi) disaggregated by CMORPH • satellite estimates • Ocean: CMORPH only • Interpolated to match space-time resolution of model forecasts
VALIDATION DATA • A new member of the “MORPH” family: “RMORPH” (Research-quality) • Land: CPC daily gauge analysis (Higgins & Shi) dissaggregated by CMORPH • satellite estimates • Ocean: CMORPH only • Interpolated to match space-time resolution of model forecasts
Precipitation Difference from Validation Data mm/day mm/day
Difference in Frequency (%) by Intensity Eta - RMORPH GFS - RMORPH Percentage Difference
HARMONIC ANALYSIS Applied to period mean diurnal cycle
HARMONIC ANALYSIS Applied to period mean diurnal cycle
% of Daily Mean Precipitation @ 35oN
CONCLUSIONS • Peak daily rainfall 3-6 hrs too early in Eta (SE US) • and GFS (eastern U.S.) • Better phase agreement over NAME “Tier-1” • Models propagate rainfall well (central US -> east ) • Light rain rate OVERforecast in the models & • heavy events UNDERforecast