Broadband acoustic scattering from nonlinear internal waves Andone - - PowerPoint PPT Presentation
Broadband acoustic scattering from nonlinear internal waves Andone - - PowerPoint PPT Presentation
Broadband acoustic scattering from nonlinear internal waves Andone C. Lavery Woods Hole Oceanographic Institution Presented by Timothy K. Stanton Woods Hole Oceanographic Institution Acknowledgements: Dezhang Chu (Northwest Fisheries
Why use acoustic scattering techniques for investigating physical processes?
Moum et. al., J. Phys. Oceanography 33, 2093-2112, 2003. Depth [m] Distance along ship track [m]
20 40
- 200 –100 0 100 200
120 kHz
Fish or large zooplankton Small zooplankton/ Microstructure?
Sources of scattering and scattering models
FREQUENCY (Hz) Volume Scattering Strength (dB)
Fish (Gas-bearing) Squid (Fluid-like?) Turbulent Microstructure Medusae (Fluid-like) Euphausiids (Fluid-like) Copepods (Fluid-like) Pteropods (Elastic-shelled) Siphonophores (Gas-bearing)
Bandwidth of acoustic system
SW06/NLIWI Experiment
Latitude
Longitude Longitude
Long Island N e w J e r s e y
SARS Satellite Image July 23, 2006 Experiment duration: July 31- August 27, 2006
50 100
Complex IW field
Broadband acoustic backscattering system
Vertical Down-Looking Horizontal Side-Looking
4 Broadband Transducers: 160 – 270 kHz, 10o (3dB-BW) 220 – 330 kHz , 8o (3dB-BW) 340 – 470 kHz ,12o (3dB-BW) 450 – 600 kHz , 9o (3dB-BW)
Microstructure measurements (Jim Moum)
Zooplankton net tows
Conclusions:
1. Abundance and biomass dominated by small copepods (fluid-like) 2. Scattering dominated by small pteropods (elastic-shelled) and amphipods (fluid-like)
Depth (m) Local Time
1 2 3 4 5 6 7 8 9
MOC 4: 24 August 2006 MOCNESS: Multiple Opening/Closing Net and Environmental Sampling System MOCNESS track superimposed on 120 kHz echogram
Depth (m) Depth (m) Depth (m) Depth (m) Time (GMT) Mika 1: 08-14-2006
Region 2: Zooplankton dominated. Inferred pteropod: diameter = 0.78 mm. Frequency (kHz) Volume Scattering Strength (dB)
1 2 2 2 2 1 1 1
160-270 kHz 220-330 kHz 340-470 kHz 450-600 kHz
Dominated by turbulence Dominated by zooplankton
Region 1: Microstructure dominated. Inferred dissipation: ε = 8x10-6 W/kg. Kelvin-Helmholtz shear instability (region 1) Zooplankton (region 2)
Broadband spectra: example 1
Broadband spectra: example 2
8.05 8.1 8.15 8.2 8.25 8.3
Time (GMT) Broadband: 160-270 kHz Broadband: 450-590 kHz Depth (m) Depth (m) Region 2: MIXED:
- Microstructure dominated at low frequencies.
Inferred dissipation: ε = 2.5×10-6 W/kg.
- Zooplankton dominated at high frequencies.
Region 3: Zooplankton dominated at all frequencies. Inferred: 960 pteropods/m3 of diameter 0.53 mm.
region 1 region 3 region 2
Dominated by turbulence Dominated by zooplankton
Summary/Conclusions
- First use of broadband acoustics to image microstructure.
- Improved image resolution.
- Improved discrimination from zooplankton.
- Scattered spectra often consistent with scattering from biology alone,
particularly at depths below the thermocline.
- Scattered spectra consistent with scattering from turbulent oceanic