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Finite differences on a fix grid mesh (Arakawa C) At bottom: Chezy condition ... Open boundary: inverted barometer effect radiation condition ... – PowerPoint PPT presentation

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Title: Storm%20surge%20forecast%20at%20M


1
Storm surge forecast at Météo-France
Pierre Daniel
2
Storm surge model
  • Two versions of one model
  • Overseas territories (for tropical cyclones storm
    surges)
  • Metropolitan coasts

3
Model installation
4
Model equations
  • Shallow water equations
  • Finite differences on a fix grid mesh (Arakawa C)
  • At bottom Chezy condition
  • Wind stress Smith and Sandwell formulation
  • Coast normal componant of current is set to zero
  • Open boundary inverted barometer effect
    radiation condition
  • Inputs wind, atmospheric pressure, bathymetry

5
Atmospheric forcing
  • Modified Holland model pressure profile and
    gradient wind
  • Information needed position, intensity, size
  • Provided by cyclone advisories
  • Example
  • FORECAST VALID 21000Z 20.7S 165.8E.
  • MAX SUSTAINED WINDS OF 80 KT.
  • RADIUS OF 50 KT WINDS 65NE 40SE 25SW 40NW
  • RADIUS OF 34 KT WINDS 85NE 60SE 40SW 60NW

6
Bathymetry
  • Hand extracted from nautical charts
  • 30 islands, grid mesh from 150 m to 2 km.
  • Examples

7
Model calibration
  • On selected cyclones from 1975 to 1990
  • Very few tide gauges 6 for 30 islands

Largest surge 250 cm in Guadeloupe (Hugo, 1989)
8
Model forecasts
  • Largest surges Luis, 1995
  • estimated 2 m in St Martin (2 m forecast)
  • measured 40 cm in Guadeloupe (35 cm forecast)

9
What is the best way to use the model ?
  • Real-time forecast accuracy
  • When a hurricane is crossing an island, a small
    error in the trajectory forecast gives a large
    error in the space distribution of the surge.
  • Pre-computed storm surge data base
  • More than 1000 model runs for each island.
  • A data base available for graphical display on a
    computer.

10
Storm surge data base
11
Coastline of France
  • Same equations and numerical scheme
  • Wind stress Wu formulation
  • Tide 16 waves 13 tide gauges
  • Calibration on selected situations (1987-1992)
  • In operation since October, 1999.
  • Under development Improvement of the wind
    interpolation (spatial and temporal).
  • Sensitivity to atmospheric forcing ECMWF,
    ARPEGE, ALADIN.

12
Surges with ECMWF analyses (6 hours)
13
Surges at La Rochelle (ECMWF analyses 6 hours)
14
Temporal frequency impact of atmospheric forcing
at Le Verdon (ALADIN - December 27th, 1999)
15
Next steps
  • Mediterranean sea
  • North sea
  • Wave surges in the lagoons
  • Real time access to tide gauge data
  • Data assimilation
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