4-d coastal ocean dynamics detected by surface current radar and auvs l. k. shay meteorology and...

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4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An Ocean Engineering Florida Atlantic University SCIENTIFIC GOAL: To provide a first-order description of complex oceanic flows and their relationship to surface processes in the littoral ocean subjected to tidal currents, western boundary currents, topographical changes and surface winds. RESEARCH SUPPORTED BY ONR.

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Page 1: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT

RADAR AND AUVsL. K. Shay

Meteorology and Physical Oceanography University of Miami

P. Edgar AnOcean Engineering

Florida Atlantic University

SCIENTIFIC GOAL:

To provide a first-order description of complex oceanic flows and their relationship to surface processes in the littoral ocean subjected to tidal currents, western boundary currents, topographical changes and surface winds.

RESEARCH SUPPORTED BY ONR.

Page 2: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

LITTORAL ZONE

Complex Coastal Processes. 2-D/ 3-D Flow Fields. Boundary Current & Topography. Waves & Boundary Layer Winds. Impact: Civilian and US Navy Needs. Radar/AUV/Mooring/Ship-based

Approach. Applicable to Any Theater.

Page 3: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Ocean Explorer AUV

Page 4: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

VHF RADAR

Phased Array 32 Elements. Electronic Beam Forming. 700 Cells (250 m resolution). 60 km Square Domain. 20 Minute Sample Cycle. Theoretical Limit 11 km. Spectra and Currents.

Page 5: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

ENGINEERINGOBJECTIVES:

Design/Implement Multiple ADCPs as Part of AUV Payload.

Evaluate Side-Looking Beam Orientations.

Map Currents Relate To Surface Dynamics.

Train Next Generation Graduate Students (i.e. Tactical Oceanography)

Page 6: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

SCIENCE OBJECTIVES:

Coherent Structures (Vortices, Fronts) Isolate BC and Tidal Flows/Forcing of

Iws At Shelf Break. Expand IWs Into Baroclinic Modes. Determine Wavenumber Spectra. Assess Boundary Layer Processes

During Storm and Quiescent Periods.

Page 7: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Experimental Domain

Page 8: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

EXPERIMENTALDESIGN

VHF Mode of OSCR (7x9 km: 250 m Cell Spacing).

Ship-Based CTD/ADCP (2x2 km) 4-AUV Sampling Patterns (0.5-1km). Cyclesonde. NOVA/USF Moorings. NAVY ADCPs.

Page 9: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Experimental Domain

Page 10: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Sub-Mesoscale Vortex

Page 11: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Vortex Propagation

Page 12: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Surface Current Regimes

Strong Florida Current Lobe Structure

Page 13: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

AUV MISSIONS

Mixed Layer: (Current and Turbulence)

Tidal Current: Bottom Boundary: Turbulence: Planned Adverse

Weather:

6 and 12-hr repeated grids : 500 m x 500 m.

15-26 hr: 1km x 1km 7 hr: 1 km x .500 km 4-6 hr: 1 km Xsects 12 hr : 500 m x 500

m (March-April 00)

Page 14: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

AUV Section

Page 15: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

AUV Maps

Page 16: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Ship ADCP Transect

Page 17: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Ship ADCP/AUV and OSCR Comparison

Page 18: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

Mooring Comparison

Page 19: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

FUTURE RESEARCH

Long-Term Monitoring of Florida Current Using HiFAR (100 km range).

Develop Long-Range AUVs (24-48 hr). Surface/Subsurface Moorings (Cross-

Shelf) Ship-Based Observations (Cross-Shelf) Drifter-Based Deployments Modeling/Assimilation

Page 20: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

GOAL:

To assess long-term variability of the Florida Current and its influence on Coastal Circulation and Atmospheric Weather Patterns/Events.

Important to Civilian Needs (Ship Traffic; Pollutant Dispersion; Renourishment.)

Important to Navy (Ship/Radar Signatures; Acoustics;Internal Waves)

Page 21: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

SFTF APPLICATIONS

US Navy Coastal Surveys. METOC (JTFX) Operations. Ship-based Operations In Differing

Venues/Theaters. Coupling With Models (i.e. LES). Provides Environmental Data To

Assess Impact on Fleet Operations.

Page 22: 4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs L. K. Shay Meteorology and Physical Oceanography University of Miami P. Edgar An

SUMMARY

Synergistic Approach: Synoptic Variability.

Fine-Scale to Submesoscale Processes. 2-D/3-D Variability not Mean. Real Time: JTFX (Ships,Aircraft,AUV). Improve Predictive Capability At Navy

Centers. Train Next-Generation Students.