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ATMOS. MODEL (MM5/COAMPS/WRF) OCEAN MODEL (HYCOM or 3DUOM) WAVE MODEL

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Presentation on theme: "ATMOS. MODEL (MM5/COAMPS/WRF) OCEAN MODEL (HYCOM or 3DUOM) WAVE MODEL"— Presentation transcript:

1 ATMOS. MODEL (MM5/COAMPS/WRF) OCEAN MODEL (HYCOM or 3DUOM) WAVE MODEL (WAVEWATCH III or WAM) Roughness length Wind-induced stress Surface fluxes SST SSH & current velocity Wave-Induced stress Coupled Atmosphere-Wave-Ocean Modeling System for Hurricane Predictions

2 Coupled Modeling System
MM5 (PSU/NCAR) (vortex-following nests with 45, 15, 5, and 1.67 km grid spacing, NCEP analysis and AVHRR or TMI/AMSR-E SST) WAVEWATCH III (NOAA/EMC) (1/12o, 25 frequency bands, 48 directional frequency bands) HYCOM (UMiami/NRL) (1/12o, 22 vertical levels with 4-6 in the ocean mixed layer) 3DUOM (Price’s 3-D Upper Ocean Circulation Models)

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4 (meter)

5 (meter)

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7 Hurricane Frances

8 Tom Sanford’s floats

9 Float 1633: 50 km to Right in Highest Wind
Tom Sanford, APL/University of Washington

10 Landfall Aug 27 Sept 6

11 Landfall

12 Coupled MM5-WAVEWATCH III
Roughness Length (non-directional) t = tt + tw zo zo - wave-age dependent Stress Vector (directional) Mx = - tx My = - ty tx , ty - components of stress from integral of momentum input to the wave spectrum. V t

13 Wind-Wave Coupling Parameterization
Spectra Tail Parameterization: X-component of stress from integral of momentum input to the spectrum: Growth rate of each component from measurement of pressure-slope correlation Spectrum of long waves from WAVEWATCH III; spectrum of short waves from fit to tail given below. a is adjusted to fit the highest modeled wavenumbers. b is the spreading function for the short waves.

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15 Hurricane Frances (2004) FR RR FR RR FL RL FL RL CD CD Ck Ck

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17 Coupled GPS Dropsondes Uncoupled

18 Total Surface Heat Flux
Uncoupled Coupled Atmos-Wave-Ocean

19 Coupled Uncoupled

20 Coupled Atmosphere-Wave-Ocean Modeling
CBLAST-Hurricane Coupled Atmosphere-Wave-Ocean Modeling Conclusions Atmosphere-Ocean coupling improves tropical cyclone intensity forecasts, especially at very high resolution when eyewalls are explicitly resolved. Wind-Wave coupling contributes to storm asymmetry that very significantly from storm-to-storm. We have developed and tested a number of air-sea coupling parameterizations for fully coupled atmosphere-wave-ocean modeling systems for hurricane prediction, which are designed to be general and easy to be implemented in both research and operational coupled models.


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