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Providing Environmental Awareness for the Urban Ocean Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

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Page 1: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

Providing Environmental Awareness for the Urban

Ocean

Alan F. Blumberg and

Nickitas Georgas

Davidson Laboratory August 22 -23, 2013

Page 2: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

New York Harbor Observing and Prediction System

Integrated system of observing sensors and forecast modelsTO OBSERVE TO PREDICTTO COMMUNICATE Weather Currents Water Level Salinity Temperature Waves

Page 3: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

3D Circulation Model (ECOM/POM-derived):Boussinesq, Hydrostatic, Primitive Equation, Sigma Coordinate

ModelMode Splitting: 10 external/internal steps, Δte=1sec. Smagorinksy lateral diffusion: HORCON=0.01, Prandtl

Number=1000!Mellor-Yamada 2.5-Kl vertical closure: UMOL=10-6 m2/s.Bottom stress: CDmin=3x10-3, z0=10-

3m, everywhere!*Modified by dynamic wave boundary layer (Grant-Madsen)!

Surface Wind Stress: Large and Pond 1982.Barometric Pressure Gradient forcing: Switched off.2D Surface Heat Fluxes: Ahsan and Blumberg, QUAL-2E-type.

*Modified for 10m winds, generalized for UTC or local time coordinate.

Robust, explicit, wetting and drying.

Dynamically Coupled, Surface Wind Wave Model (GLERL-derived):Empirical Wave Momentum Model, JONSWAP spectrum.Wind-wave growth equation: γ=2.8%, CDs=0.7x10-3,

,z0w=σ/5.Incl. Bottom dissipation: fw=0.04Incl. Depth-induced breaking: γB=0.8261 (Longuet-Higgins and

Fenton, 1974).*Dynamic depth from circulation model.

Incl. Offshore wave boundary condition. Adopted new dispersion eqn. for shallows.

Included and validated Thin Dams (obstruction grids).Standardized, CF-protocol-compliant, NetCDF Outputs.

sECOM Hydrodynamic Model. NYHOPS App.

Page 4: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

Bathymetry:Over 1M soundings!

Resolution: 4km -> 25m

DE

NJ

CT RINY

NYC

NYHOPS Forecast Model _ it is all about realism! 3D General Circulation Model dynamically coupled with Surface Wind-Wave modelInput forcing:(O): Observed(F): Forecasted(H): Historic Tides (O+F) NOS Offshore Surge and Steric (O+F) NOS Offshore Waves (O+F) Surface Winds (O+F) NAM 12km Heating and Cooling (O+F) 239 Rivers and Streams (O+F) NERFC 280 Major Dischargers (H) River Ice (O+F)

Output: hindcasts+forecasts 4x/day Results every 10min, since 2006.Total water level.3D Currents, Salinity, Temperature.Significant wave height and wave period. Colored DOM and light absorption.

+

1967

+Real timeObservatio

ns

External dataand models

Distributed Inflows and Effluents

Page 5: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

A fully automated system of systems

New York Harbor Observing and Prediction System

0.5 hrs + 1.5 hrs + 2.0 hrs

Page 6: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

ValidationEvery model has errors. Validation tells us that they are sufficiently small.

Adopted NOAA/NOS Model Evaluation Software (DB-MEE).2 years of recent in situ data: 2007-2009; 6+ years of real-time experienceOver 100 local stations (Georgas and Blumberg ‘10, DiLiberto et al ’11, etc.)T/S vertical transect profiles from gliders (Georgas and Blumberg ‘08)Satellite SST comparisons (Bhushan ‘09, Bhushan, Blumberg, Georgas ‘10)HF-radar (Gopalakrishnan ‘11) and surface drifters (Blumberg et al, forthcoming).

Page 7: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

Marine Search and Rescue (SAR) Missions…………

NY/NJ Harbor Commercial Pilots & Schedulers (Harbor Pilots Associations, Marine Transportation)……………

Recreational Boaters (Regattas, Kayaks,…)………………..

Coastal Flooding Responders (PD, FEMA, NWS)……

Scientists/Engineers……

NYHOPS supports:

New York Harbor Observing and Prediction System

Page 8: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

Sandysurge Post-Sandy

Nor’easter

1

Totals for Sandy’s forecast period: 30,334 unique hits.

The NYHOPS/SSWS forecast water elevation (posted Saturday at 6am): - Along coast of NJ/NY and all

of the Hudson River were within 5%,

- the Battery, NY was low by 20%,

- Long Island Sound was low by 10%

Page 9: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

ConclusionsNYHOPS established as an urban ocean forecast system –

large following – extensive validationMARACOOS assets a blessing – hf radar, drifters, gliders

and “met forcing”Need more robust assimilation – bring in mobile sensors,

including truncated fisheries dataNeed better offshore boundary forcingStudy wave and wave-driven set-up modelingFaster code… offsite mirroring… online data storeThank you NWS & NCEP & NOS– great operational

productsLinks needed to National Hurricane Center collection of

hurricane models;Include infrastructure ensembles/probabilistic forecasts;

Page 10: Alan F. Blumberg and Nickitas Georgas Davidson Laboratory August 22 -23, 2013

Thank You! [email protected]