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Evaluation and Improvement of Spray-Modified Air-Sea Enthalpy and Momentum Flux Parameterizations for Operational Hurricane Prediction. Jian-Wen Bao Christopher W. Fairall Sara A. Michelson Laura Bianco NOAA/ESRL/physical Sciences Division
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Evaluation and Improvement of Spray-Modified Air-Sea Enthalpy and Momentum Flux Parameterizations for Operational Hurricane Prediction Jian-Wen Bao Christopher W. Fairall Sara A. Michelson Laura Bianco NOAA/ESRL/physical Sciences Division (in collaboration with Naomi Surgi and Young Kwon of NCEP/EMC) Presented at: The 62nd Interdepartmental Hurricane Conference Charleston, SC: March 5, 2008
OUTLINE • Parameterization of sea-spray mediated sensible and latent heat fluxes • Parameterization of sea-spray modification of momentum flux • Implementation andtesting of the ESRL sea-spray scheme in the HWRF model • Summary and Preliminary Conclusions
Parameterization of Sea Spray: Wind Speed DrivenFairall/Andreas/Kepert Early 1990’s Raw Direct sensible Raw Direct Latent Raw Droplet Sensible Raw Droplet Latent Net fluxes emerging from top of droplet layer Alpha accounts for SUBGRID feedback (droplet – T/q profile interactions)
Feedback The thermal feedback is defined by distortions of the temperature and humidity profiles in the droplet –filled surface layer: δT and δq, which are determined by the source strength and residence time.
Parameterization of the Sea-Spray Modification of Momentum Flux (e.g., Barenblatt 1996 and Lykossov 2001) where S is the spray concentration profile. Where the mean fall speed of droplets spray generation height empirical parameter
Implementation in the HWRF model The subroutine of the NOAA/ESRL sea-spray parameterization is called by (and appended to the end of) module_bl_gfs.F A function routine (function qsat_spray) is added to module_gfs_funcphys.F Testing experiments have been conducted on Haze with Katrina (2005), Rita (2005), Emily (2005), Dennis (2005) and Helene (2006).
max. wind speed min. sea-level pressure track Test with Katrina (2005)initial time: 0000 UTC 27 August 2005
Test with Katrina (2005) control thermal thermal + momentum Valid at 0060 UTC 29 Aug 2005
Test with Katrina (2005) thermal control thermal + momentum Valid at 0060 UTC 29 Aug 2005
Summary and Conclusions • The impact of the sea-spray parameterization on the track forecast is negligible, despite the noticeable impact on the intensity. • Both the intensity and structure are influenced by the parameterized thermal and kinematic effects of sea spray. • The response of the storm intensity does not appear to be proportional to the change in the droplet source strength and feedback strength. • The errors in the HWRF model forecast can only be partially • attributed to the errors in the surface fluxes. • The performance of the sea-spray parameterization scheme in the HWRF model needs to be further evaluated and calibrated.