upper ocean response to 2002 hurricanes isidore and lili ...assimilation of ssh and sst prior to...

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Upper Ocean Response to 2002 Hurricanes Isidore and Lili in Tandem Wei Zhao Shuyi S. Chen and Joseph Tenerelli Rosenstiel School of Marine and Atmospheric Science University of Miami

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Page 1: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

Upper Ocean Response to 2002 Hurricanes Isidore and Lili in Tandem

Wei ZhaoShuyi S. Chen and Joseph Tenerelli

Rosenstiel School of Marine and Atmospheric ScienceUniversity of Miami

Page 2: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

ATMOS. MODEL(MM5/COAMPS/WRF)

OCEAN MODEL(HYCOM or 3DUOM)

WAVE MODEL

(WAVEWATCH III or WAM)

Wave-Induced stress

Surface Wind

Surface fluxes and stress

SST

SSH

& cu

rrent

velo

city

Wav

e-In

duce

d stre

ss

Coupled Atmosphere-Wave-Ocean Modeling System for Hurricane Predictions

Page 3: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

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)

(1/6o, 25 frequency bands, 48 directional bands)•HYCOM (UMiami/NRL)

(1/12o, 22 vertical levels with 4-6 in the ocean mixed layer)•3DUOM (WHOI’s 3-D Upper Ocean Circulation Models)

(15 km, 30 vertical levels with 4-6 in the ocean mixed layer)

Page 4: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

Before Bonnie

After Bonnie... .

...

..

Page 5: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers
Page 6: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers
Page 7: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

Hurricanes Isidore and Lili (2002) in tandem

Page 8: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

Objectives

To examine the upper ocean circulation in response to a dual hurricane passage in the Gulf of Mexico.

To test HYCOM performance under high-resolution, complex atmospheric forcing.

Page 9: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

HYCOM Configuration• one-way nested Western Atlantic-Gulf of Mexico-

Caribbean Sea regional domain with data assimilation of SSH and SST prior to hurricane simulations

• 0.08 degree grid spacing• 22 Vertical layer, 4-6 layers in mixed layer with the

1st layer at 3 meter • MM5 atmospheric forcing, 17 August – 17 October

2002 (1.67-km grid resolution during Hurricanes Isidore and Lili, 45-km in pre- and post-hurricane periods)

Page 10: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

AUG17 SEP18SEP08 OCT04SEP27 SEP30 OCT17

MODAS SST data

assimilationHurricane

IsidoreHurricane

Lili

Page 11: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

Hurricane Isidore Hurricane Lili

Page 12: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

SSHA (satellite)

SST/SSC (HYCOM)

Pre-Isidore

Page 13: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers
Page 14: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

SatelliteSST pre- and post-Isidore

HYCOM

Page 15: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

HYCOM

Satellite

SST Cooling post-Isidore

Page 16: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

SatelliteSST pre- and post-Lili

HYCOM

Page 17: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

HYCOM

Satellite

SST Cooling post-Lili

Page 18: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

A B

Page 19: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

B: Loop CurrentA: Gulf Common Water

Isidore Lili Isidore Lili

Page 20: Upper Ocean Response to 2002 Hurricanes Isidore and Lili ...assimilation of SSH and SST prior to hurricane simulations • 0.08 degree grid spacing • 22 Vertical layer, 4-6 layers

satelliteSSH & SST data assimilation

O.M. Smedstad

SSH data assimilation only21 days SST data assimilation