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Quantitative Precipitation Forecasting in Tropical Cyclones
Shuyi S. Chen Manuel Lonfat, Joseph Tenerelli, Frank Marks Robert Rogers, Fiona Horsfall Rosenstiel School of Marine and Atmospheric Science University of Miami NOAA/AOML/HRD NOAA/NWS/TPC
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Factors that Influence TC Rainfall
Intensity Shear Landmass/Topography TC/Synoptic System Interaction Translation speed Moisture advection Microphysics/Aerosol Surface Flux
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HRD/AOML P3 LF REFLECTIVITY
2030 UTC 14 SEP 1999 2300 UTC 13 SEP 1999
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Uncoupled
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Sensitivity to Model Grid Resolution
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15 km 1.67 km
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Influence of Vertical Shear and Synoptic Weather Systems
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Hurricane Floyd (1999)
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Hurricane Bonnie (1998)
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Quantitative Precipitation Estimates from TRMM TMI/PR
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Hurricane Floyd (1999)
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TRMM/TMI Azimuthal Averages (1998-2000)
R (mm/hr)
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TMI PDF of R 90% or 50%
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Measures of R PDF R-CLIPER uses mean from PDF - not best measure of PDF (log-normal) - shows intensity influence Other measures are the median of the PDF (area and flux). Area shows intensity influence, but flux does not, except in the inner core.
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TC QPF Questions What characteristic of PDF of R are we trying to predict, i.e., mean R, Rmax, etc.? What is best measure of PDF of R to use to answer the question, i.e., mean, median, 90% of PDF? How do we develop a evaluation/validation system for high-resolution QPF product? How will it be used operationally, perhaps a combination of deterministic and probabilistic measure that takes into account of track errors?
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