acoustic seaglider results from summer 2006 bruce m. howe applied physics laboratory university of...
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Acoustic Seaglider Results from Summer 2006
Bruce M. HoweApplied Physics Laboratory University of Washington
ONR CODE 32 NW REGIONAL PROGRESS REVIEWApplied Physics Laboratory, University of Washington
27 February – 1 March 2007Seattle, WA
Goals and Outline
• Develop and demonstrate the acoustic Seaglider in the persistent surveillance context:– As a communications gateway between subsurface
platforms and land– To act as a general purpose acoustic receiver/tactical
sensor for all signals and “noise”, with near-real time reporting of processed results
– To provide oceanographic data
• Review results from 3 field experiments• Discuss next steps
Acoustic Seaglider
• ½ knot at ½ W• Up to 1000 m dives• > 6 months, 3000 km,
600 dives• Temperature, salinity
and others• Now with hydrophone
and acoustic modemFumin Zhang
Philippine Sea
Kauai
Monterey Bay
Acoustic Seaglider Operations – Summer 2006
Philippine Sea – SG022, 7/29/06-7/30/06, 1 day, 15 dives, low ARS band,CTDMonterey Bay – SG022, 8/15/06-8/21/06, 6 days, 61 dives, low ARS band,CTD SG023, 8/18/06-8/23/06, 5 days, 83 dives, low ARS band, CTD SG106, 8/12/06-8/18/06, 6 days, 131 dives, high + low ARS bands,CTD,modemKauai - SG023, 8/31/06-10/8/06, 39 days, 143 dives, low ARS band, CTD
Monterey Bay 06:Positions where SG106 read modem FSK packets
• Black circles: SG106 at surface after dive - no acomms received
• Blue circles: dives where acomms commands logged
• 106 sent FSK command to turn off the ARL-UT array
• Most FSK came from ARL-UT or Gateway
• Black +: dives after recording acomms logs ceased
• 4-5 km ranges are evident
First FSK packet at 2006.08.15:0857 (UTC) from unit ARL-UT to Gateway, Dive 22.
1 km
ARL-UT bottom node
Gateway
Kelp Array
Lat
itud
e
MB06: RXD receptions vs range and depth
Histograms of depths for RXD receptions
C
ount
s0
1
0
20
3
0
40
0 50 100 depth(m)
0 20 40 60 80 100 120 140 depth (m)
C
ount
s0
2
0
40
6
0
SG106 descending SG106 ascending
Depth
0 m
100 m
5 km0 km Range
10 20
10 20
Time (s)30
30
25
20
15
10
5
Fre
q (k
Hz)
Modem performance: 1st 30 sec of dive 41
30
PSD @ 8-10 sec
0 5 10 15 20 25 30 35 kHz
Simple ACOMMS detector: ratio of energy in23-27 kHz band to energy in 15-19 kHz band
glider pump noise
ACOMMS band – 23-27kHzReference band – 15-19kHz
{
telling kelp to talk to GB
from kelp to GBtelling UT-VS to talk to GB
Missed packet
Missed packet
21:24:14 UTC
Frequency
Time (s) 150
~10 nm from shipDive 13, file 2
0
Distant source
Ship source, harmonics and reverb
SignalsExample of Lubell source recorded at SG023(dive 20 segment 2)
LWAD
MB06
NPAL / ATOC Kauai source
• 260 W• M-sequence coded
signals• 75 Hz, 35 Hz bandwidth• 28 ms peak• 27.28 s period• 2 hour transmissions,
1 per dayDIVE 56 -example
30
79
Red segments = ARS recordings
10
.8 m
s
}1
4.7
ms
}1
3.0
ms
}
}
1/75 Hz = 13.3 msExample time series
Example PSD
zoom PSD
Kauai example
Motion and Coherent gain
Doppler + stack:• from 35 to 44 dB• 9 dB of gain • vs theoretical gain 14 dB• Variation during 12 minutes
Time – 12 minutes
Relative travel time – 0.4 s Relative travel time – 0.16 s
Relative travel time – 0.4 s
Time – 12 minutes
Doppler
Arrival times(72.7195)
(72.282)
(72.8654)(72.9153)
(73.4143)
Single block 27.28 s
Peaks shift due to changing s/r range•Measured travel time changes
•~3.7 ms per block•Match glider kinematics
•0.204 m/s, 136 m horizontal, 33 m vertical, 12 minutes
kHz
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
1.8
2.0
2.2
2.4
s0 2 4 6 8 10 12 14
humpbackHz
0
5
10
15
20
25
30
35
40
45
50
55
60
65
70
75
80
85
90
95
100
105
110
115
s0 5 10 15 20 25 30 35 40 45
3rd harmonic ~48 Hz
1st harmonic ~16 Hz
Blue whale ‘B’ call
Hz
0
5
10
15
20
25
30
35
40
45
50
55
60
65
70
75
80
85
90
95
100
105
110
115
s0 5 10 15 20 25 30 35 40 45
Blue whale ‘D’ call
Humpback (very close)
Blue whale
Sea lions?birds
Humpback @ 15 and 65 secBlue @ 35 secSea Lions? @ 50 sec
Animal sounds recorded on Seaglider ARS Monterey Bay, MB06
Ambient noise levels compared to Wenz
ASG – Summer 2006 Summary
• Demonstrated gateway capability – connecting subsurface platforms to shore via acoustic modem/satellite Iridium
• Demonstrated acoustic receiver – man-made signals, whales, noise… with near-real time processed results
• Potential – general ocean acoustics tool, tactical sensors, navigation/time node, data truck, marine mammal observing, tomography receiver, basin-scale thermometry, climate change, …
Next steps• Fall 07 – PLUSNet07 off La Jolla
– Spring/summer – mini PLUSNet in Puget Sound + scouting mission off La Jolla
• PLUS - Continuing development and field work– Communications: Modem integration and HFGW – Nexgen glider (payload, buoyancy, processing, …), – Tactical sensors – add directivity and gain
• Mission management– Optimization: High currents, power, multiple gliders– Navigation and timing– Overall situational awareness
• Integrating acoustics + nav into data assimilation – mobile acoustic tomography receiver
Related Projects• ONR Philippine Sea 2009 –
Ocean acoustics deep water, QPE DRI (many)
• NASA: A Smart Sensor Web for Ocean Observation (APL, EE, JPL)
• NSF STC Coastal Margin Observation and Prediction (OHSU, OSU, UW)
• NSF ORION …
Many helped!Geoff ShillingJason GobatCraig LeeRuss LightPete SabinRex AndrewKeith van ThielKeith MagnessTroy SwansonTim McGinnisMike BoydKate StaffordSue MooreRobert MiyamotoMarc StewartJim LubyNeil BogueAndrew WhiteJim MercerLinda BuckJoe WigtonFritz Stahr and the Seaglider
Fabrication Center
Lee Freitag and Matt GrundTom Hoover, Jim Bellingham, et alJoe Curcio and the MIT kayaksClay Spikes, Dave Porter, et alYi ChaoPierre Lermusiaux
ONR sponsorship
Skip Denny and the ANTS crew
Thank you
Questions?
Backup/Extras
Glider – Kayak interactions in Monterey Bay
Kayaks pinging to glider
Graphs by Alexander Bahr
MIT Computer Science & Artificial Intelligence Laboratory
Monterey Bay MB06SG023 was allowed to drift on the surface for 2 extended periods during MB06The resulting drifts were compared to surface current predictions from the HOPS model
Leg 83
Current shear eventexperienced by glider but not captured by model
forecast nowcast
Leg 25
Temperature, salinity, conductivity data usually available within 5 min of dive completion – example SG023 dive 46
Dive 46 temperature and salinity as plotted on IOP website
recovered
Drift 2
Drift 1
78
80
SG023 surface drifts
• Dives 55 and 83 followed by surface drift tests• Data compared to current prediction models
Drift 2 shows a current shear event
MB06 Acoustic Seaglider Accomplishments
• Deploy and operate sensors in field– 428+ hours of dive time– 300+ dives (acomms, T, S, Depth, acoustics, surface currents, depth-avg
currents)• Demonstrated Seaglider communications gateway capability
– In-air – Iridium satellite – Sub-sea – acoustic modem at various depths and ranges– Passing NAFCON orders to remote kayak to prosecute target
detected/reported by other kayaks (node of LBL navigation)– Turned bottom vector sensor array node on/off
• Ambient sound– Active source emissions - Lubell source (for TL, propagation)– Marine mammals (blues, humpbacks, sea lions, …)– Ambient noise budget (ships, seismics, wind, rain, …)
• Environmental data– Temperature and salinity into Harvard and JPL models– Depth averaged and surface currents– Bottom resting mode– Adaptive sampling
Coherent processing of M-sequence coded signals
Arrival times(72.7195)
(72.282)
(72.8654)(72.9153)
(73.4143)
Peaks in each block shift due to changing s/r range
•Measured travel time changes•~3.7 ms per 27.28 s block
•Match glider kinematics•0.0204 m/s, 136 m horizontally, 33 m vertically, in 12 minutes
Relative travel time – 27.28 s
Relative travel time – 0.3 s
Relative travel time – 0.4 s