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HydroEstimator HE

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NAM or GFS PW, 1000-700 hPa mean RH, u, v, convective EL computed from T, q profile ... areas of positive Z (local Tb minima); effective screening of cirrus by using Z ... – PowerPoint PPT presentation

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Title: HydroEstimator HE


1
Hydro-Estimator (HE)
  • Bob Kuligowski, Clay Davenport, Rod Scofield,
    Gilberto Vicente
  • NOAA/NESDIS/ORA

2
Theory / Schematic
  • Algorithm Inputs (IR, MW, NWP)
  • 10.7-µm IR window Tbs from GOES-9, -10, -12,
    Meteosat-5 and -7
  • NAM or GFS PW, 1000-700 hPa mean RH, u, v,
    convective EL computed from T, q profile
  • Satellite inputs are from GVAR feeds model
    inputs come from NCEP
  • Algorithm Process (how the inputs are converted
    to rainfall estimates)
  • Adjust Tb (Tadj) by reducing values where
    convective EL temperaturegt213 K
  • Z-(Tadj-µT)/sT rain only where Zgt0
  • Rain ratef(Tadj, Z, PW)
  • Reduce rain rate in low-RH environments

3
Theory / Schematic
  • Strengths and Weaknesses of Underlying
    Assumptions
  • Standard IR assumption that Tb is a proxy for
    cloud depth / updraft strength and hence for rain
    rate works best for convective precipitation
  • Assumes rainfall only in areas of positive Z
    (local Tb minima) effective screening of cirrus
    by using Z
  • Adjusts for environments with low convective EL
    by adjusting Tb downward based on convective EL
    temperature, but still underestimates warm-cloud
    rainfall
  • Underestimates rainfall early in convective life
    cycle where updrafts are strong and clouds are
    rapidly cooling, but still relatively warm
  • Planned Modifications / Improvements
  • Currently undergoing recalibration using 6 weeks
    of CONUS data from summer 2003 with bias-adjusted
    radar as target data should be completed by end
    of summer
  • Inclusion of Lagrangian ?Tb to improve
    performance in early stages of convection work
    planned for this fall

4
Algorithm Output Information
  • Spatial Resolution 4 km Western Hemisphere, 6 km
    elsewhere
  • Spatial Coverage global (60S 60N)
  • Update Frequency same as IR update frequency
  • 15 min over CONUS
  • Generally 30 min elsewhere, but up to 3 h in
    parts of Southern Hemisphere
  • Data Latency 10 min after data received at ORA
  • Source of Real-Time Data
  • (graphic) http//www.orbit.nesdis.noaa.gov/smcd/em
    b/ff/auto.html
  • (digital) ftp//www.orbit.nesdis.noaa.gov/pub/smcd
    /emb/f_f/hydroest/world/world/

5
Algorithm Output Information
  • Source of Archive Data
  • limited online archive at real-time ftp site
  • offline global archive back to 25 May 2005
  • offline CONUS archive back to April 2003
  • Capability of Producing Retrospective Data (data
    and resources required / available)
  • CONUS tape archive of component files back to
    1997
  • Northern Hemisphere can get GOES IR data from
    CLASS (back to December 2003) and use archive Eta
    adjustment files
  • Elsewhere need 10.7-µm data and AVN/GFS fields
    (PW, RH, T, u, v)
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