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Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated Model-Based Localization of Marine Mammals

Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

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Page 1: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Christopher O. Tiemann

Michael B. PorterScience Applications International Corporation

John A. HildebrandScripps Institution of Oceanography

Automated Model-Based Localizationof Marine Mammals

Page 2: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Advantages of Model-Based Localization Technique

• Acoustic propagation model provides accuracy

• Robust against environmental and acoustic variability

• Graphical display with inherent confidence metrics

• Applicable to sparse arrays

• Fast for real-time processing without user interaction

• Hyperbolic fixing – Assumption of direct acoustic path and constant soundspeed

• Matched-field processing – Sensitive to environment

Traditional Passive Acoustic Localization Methods

Page 3: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Algorithm has been tested with real acoustic data from two locations

PMRFDeep waterHumpback whale calls .2-4 kHz 2 sec durationSperm whale clicksHydrophone array

San ClementeShallow waterBlue whale calls 10-20 Hz 20 sec duration

Seismometer array

Robust against differences in environment and species

Page 4: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Pacific Missile Range FacilityHydrophone Positions

San ClementeSeismometer Positions

Array Geometries

Page 5: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Time-Lag

dB

dB

Spectrograms from PMRF Channels 2 and 4

3/22/01 20:16:30

Page 6: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

San Clemente Seismometer Spectrograms

4 receivers11 days of data128 Hz sample rate

Blue whale type ‘A’ and ‘B’ calls observed

Sensors measured 3-axis velocityplus pressure

Seismometer #1 08/28/01 11:36

Page 7: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

3) Compare predicted vs measured time-lags for likelihood scores

Algorithm Overview

1) Predict direct and reflected acoustic path travel times and time-lags

2) Pair-wise cross- correlation measures time-lag

4) Summed scores form ambiguity surface indicating mammal position and confidence

Page 8: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

1) Pixilate spectrograms to binary intensity (black & white)

SpectrogramCorrelation

Ch. 2, 3/22/01 20:16:30

Ch. 4, 3/22/01 20:16:30

2) Correlate via logical AND and count of overlapping pixels

Time-lag between Ch. 2 & 4, 3/22/01 20:16:00

3) Maximum correlation score determines time-lag

Page 9: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Time-lag between PMRF Ch. 2 & 4, 3/22/01 20:16:00Time-lag between PMRF Ch. 2 & 4, 3/22/01 20:16:00

Spectral correlations provide more consistent time-lag estimates than do waveform correlations

Page 10: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Phase-Only Correlation• Measures time-lag between receiver pairs• Product of two whitened spectra• Frequency-band specific• Advantages over waveform or spectrogram correlation• Over time, see change in bearing to persistent sources

Pair-wise Time-lag between Seismometers #1 and #4 08/28/01 – 08/30/01

Page 11: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

1) Discard low-score time-lags

2) Compare predicted vs measured time-lags for all candidate source positions

3) Sum likelihood contributions from all hydrophone pairs

Ambiguity Surface Construction

PMRF 3/22/01 20:16

Page 12: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Whale TrackingAmbiguity surface peaks from consecutive localizations follow movement of source

San Clemente

Page 13: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

• Sources can be localized far outside array• Tracks give clues to animal behavior

08/28/01 02:52-04:52 08/28/01 09:33-13:50 08/29/01 02:55-04:50

Tracking Examples

Page 14: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Tracking ExamplesWhale movement can be followed with time-lapse movies.

Click on a figure to play.

San Clemente 08/28/01 02:52 – 04:43 San Clemente 08/28/01 09:33 – 13:50

Page 15: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Depth Estimation

Repeat modeling and surface construction for several depths

Surface peak defocuses at incorrect depths

UTM East (km)UTM East (km)

UT

M N

orth

(km

)

Sperm whale localization at PMRF 03/10/02 11:53

200 m depth 800 m depth

Page 16: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Multiple SourcesSinging whales

• Time-lag from single correlation peak limits one localization per receiver pair• Different receiver pairs can localize different sources on same ambiguity surface

Clicking whales• Pair-wise click association tool measures time-lag• Can track multiple whales simultaneously

Time (sec)

Am

plitu

de

PMRF receiver 501 waveform, 03/10/02 11:52, with clicks identified

Page 17: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

Verification• Goal to verify accuracy of localization algorithm

• Low probability of concurrent visual and acoustic localization of same individual

• Matched acoustics to visual sighting of sperm whale pod at PMRF

• Have data from controlled-source localization experiment at AUTEC

Sperm Whale Localizations at PMRF 03/10/02

11:53-11:56

11:54-11:56

11:55

11:58

Page 18: Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated

ConclusionsModel-based algorithm benefits:

• Portable to other distributed array shapes, environments, and sources of interest• Robust against environmental variability• Suitable for automated real-time processing• Modular design

Future work:• Test on other ranges, species and vs. controlled source• Add species identification tool• Long-term, real-time range monitoring and alert generation