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Home
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Sea
Technology Article: Drinking from the Fire-Hose |
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By: Tom Reed, president of Oceanic
Imaging Consultants, Inc.,
INTRODUCTION
The acquisition of seafloor mapping data has matured remarkably
in the past decade. This article reviews some of these advances,
with particular attention to how some new technologies have
effectively dealt with "data-overload" made possible
by sensors with greater resolution and bandwidth.
Seafloor mapping - while admittedly potentially a complex,
detail-intensive task involving numerous electronic sensors,
telemetry systems and logging/display devices - can be, and
often is best thought of, as making pictures of the bottom
of the sea. Pictures, as we all know, contain a lot of information.
A typical 35mm color slide, at 9000 scan lines per inch and
approximately a 4x3 aspect ratio, contains over 2.5 Giga-bits
of information. Clearly, mapping the seafloor can be highly
data-intensive, resulting in data overload on both operators
and logging devices. "The Matrix" notwithstanding,
people do not deal gracefully with scrolling alpha-numeric
byte-streams. Scrolling pictorial representations (waterfalls,
graphic recorders, etc.) are the usual solution, but often
with compression in both physical resolution, and data dynamic
range. With recording mimicking display, loss of resolution,
or reduction in survey coverage and pace, was considered inevitable.
These mandatory losses are now a thing of the past. Sustainable,
24-7-365 reliable logging and real-time processing of seabed
mapping data at rates in excess of 10 mega-bytes per second
is available in commercial, off the shelf PC-based packages
today.
HISTORICAL PERSPECTIVE
At a first glance, seabed mapping systems can be categorized
into two families: acoustic systems, such as echo-sounders,
sidescans, multi-beams and swath-interferrometric devices,
and non-acoustic devices, such as traditional cameras and
videos, electronic still cameras (ESC's) and laser linescan
systems (LLS's). We recognize that profiling systems such
as single and multi-channel seismics, magnetometers and gravimeters
are equally important mapping tools, but for the moment restrict
our analysis to systems providing imaging in the traditional
planimetric format.
A typical two-channel analog sidescan system actually provides
a large amount of information. Fortunately, roll-paper records
are quite efficient at gathering this, albeit somewhat difficult
to carry around in significant quantities. When taken to the
digital domain, a quantitative notion of the data available
to us becomes apparent. Assume a reasonable digitization rate
of 24 KHz, yielding a constant slant-range resolution of 3
centimeters. Assume 16-bits sample resolution to encompass
the likely range of raw backscatter variations in amplitude.
This implies a data rate from a simple two-channel sidescan
of approximately 100 Kbytes per second, or 360 megabytes per
hour. This will fill a Zip-disk in 15 minutes, and a 1 GB
Optical platter in under 3 hours. To people planning a 30
day cruise, this begins to look expensive. In steps downsampling.
Perception is everything, they say. A high-quality roll-paper
recorder can display 4096 samples across a scan, and you don't
need to hire a programmer to show your boss the data. For
the typical sidescan mentioned above, this would allow you
to show full resolution data for any swath of 50 meters range
or less. At any range greater than that, you would have to
throw away some of the data. At 100 meter range, you would
have to throw away half the data, for example. Furthermore,
the human eye can only distinguish between 16 and 32 shades
of grey. This translates to retaining at best one third of
the original dynamic range. If you take this same data to
an XGA computer monitor, you are limited to only 1024 samples
across a line, and a depth resolution of 8-bits. Let's assume
you may have 2 screens, so now, in theory, you would need
to log only 1024 samples per side, 8-bits per sample to make
maximum use of your digital display system. If you operate
at 100 meters range or greater, and only log what you display,
you have irretrievably discarded over 75% of your data. No
amount of post-acquisition signal processing magic can bring
this lost data back. Furthermore, any operator-induced changes
to gains, contrast stretches, etc. are likely to be permanent.
Logging raw data at full resolution and full dynamic range
obviates these problems. It just requires media space, and
through-put bandwidth.
NEW DEVELOPMENTS
In 1997, the United States Naval Oceanographic Office (NAVOCEANO)
embarked upon a fleet modernization program for its T-AGS
51, T-AGS 60 and T-AGS 45 class oceanographic survey vessels
and accompanying Hydrographic Survey Launches (HSL's). Mission
requirements included high-resolution sea floor mapping and
object location/identification in littoral areas of the world,
typically under adverse environmental conditions. Specific
requirements included simultaneous acquisition, display and
logging of dual-frequency sidescan sonar data, single and
multibeam bathymetry, and beam amplitude and backscatter.
Per the specification, the maximum anticipated data rate would
be up to 1 Gigabyte per hour, which the sonar data acquisition
workstation would be required to log to both tape and hard-drive.
Anecdotally, this prompted the requirement for at best a 9
GB hard drive, as it was mentioned that "...no government
worker was ever required to work more than an 8 hour day...".
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Figure 1. NAVOCEANO Hydrographic survey launch (34'
LOA). |
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Oceanic Imaging Consultants (OIC) was selected
to provide GeoDAS as the Sonar Data Acquisition and Processing
workstation for the T-AGS ships and HSL's, interfacing to the
Datasonics SIS1502 Dual-frequency sidescan, as well as the Simrad
EM3000 for multibeam bathymetry and backscatter.
The rack-mount GeoDAS workstation, as shown below, was delivered
with dual 1280x1024 monitors, dual 18-GB hard-drives, and dual
20 GB Exabyte Mammoth tape drives. A quad-port Ethernet card
allows simultaneous receipt of both the broadcast Simrad multibeam
bathymetry and TSS-PosMV navigation and motion sensor data,
as well as re-broadcast of processed OIC records of merged sidescan
and bathymetry to client workstations, either on the launch,
or at a remote location, via Ethernet Radio Link. The latter
technique allows observers back on the host T-AGS ship or land
to view raw or processed data from the HSLs as the data are
being acquired, offering both immediacy of analysis, and easy
remote trouble-shooting of any data quality issues which might
arise. |
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Figure 2. GeoDAS equipment rack aboard NAVOCEANO ship,
with dual 1280x1024 monitors, rack-mount keyboard, CPU, Sonar
MUX and printer, plus integrated winch controls, USBL tracking
unit & deck cameras. |
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The sidescan on the HSL's is a Datasonics SIS1501/2
dual-frequency system. The 1501 model indicates CW technology,
while the 1502 indicates that the sonar can operate in both
CW and Chirp mode. GeoDAS interfaces to and controls the SIS1501/2
through the through the Datasonics multiplexor and proprietary.dll, which allows full control of sonar range, wet-gains, pulse
type, length and power, as also provide both sensor telemetry
and a continuous 192 Kbytes per second data feed. GeoDAS logs
all this data raw, without any filtering or downsampling, and
then applies user-specified processing to allow realtime data
display in a variety of views (profile, waterfall, mosaic).
The multibeam on the HSL's is the Simrad EM3000s, a 300 KHz
sounder which provides 127 beams over a swath of upto 200 meters
or four times water-depth, in waters from 0.5 to 150 meters
deep. The system outputs both raw and corrected bathymetrye
datagrams over a 10 Mb/sec UDP link. It can also broadcast both
beam amplitude (average backscatter per beam) and the raw time-series
backscatter data at full resolution (3 cm). GeoDAS catches all
these datagrams and logs them in parallel with the SIS1501 sidescan
data, and offers the user options for both processing and display
selection. By default, the console will present a waterfall
showing platform and sidescan attitude, course, etc., along
with synchronized color-contoured bathymetry, and either low
or high-frequency sidescan. The user may modify views and processing
on the fly without interrupting data logging, to optimize onboard
analysis such as target detection and survey status. |
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Figure 3. GeoDAS user interface, showing color-contour
bathymetry in parallel with sidescan (100 or 500 KHz).
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The combined data streams from the sidescan and
multibeam comes to just under 1 GB per hour, which GeoDAS logs
continually to dual Exabyte 8900 tape drives, and optionally
prints to a rack-mounted roll-paper recorder. The operators
may also elect to create realtime mosaics of both the sidescan
and bathymetry data, in a variety of projections, at user-definable
scale and orientation. The geo-coded mosaics can be export to
an on-board GIS package, and merged with existing data for quick-look
mission products. |
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Figure 4. "Quick-look" mission product created
from HSL bathymetry and sidescan, mosaicked at 1 centimeter
resolution and merged with available air-photo data for the
surrounding region. |
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DOUBLE OR NOTHING...
In the fall of 2000, OIC began work on an interface to the
Raytheon LS-4096 Laser Linescan system. The LS-4096 provides
continuous 14-bit imagery from a scanning laser mounted on
an underwater vehicle. Resolution is configurable from 512
to 4096 samples per scan line, at scan rates up to 4000 RPM.
At maximum resolution, the LS-4096 delivers 2.2 Mbytes per
second, at approximately 267 scan lines per second. This data
rate doubled that which had been required of GeoDAS in the
past, and exceeds conventional sonar imaging requirements
by at least a factor of 100, if not more. The original top-side
processor allowed saving of user-selected "snapshots",
but any continuous data logging could only be accommodated
on video tape, which could not take advantage of the full
imaging resolution potential of this system. Any geo-coding
of data required manual "cut-and-paste"operations
post acquisition.
GeoDAS-LLS provides a complete control, processing and display
interface to the laser linescan system, treating the data
stream as a single-channel sidescan (albeit, a VERY FAST sidescan).
This includes full resolution raw data logging, as well as
realtime and post-acquisition processing, targeting and geo-coding.
The laser data can even be merged with co-registered sidescan
data, to provide an ultra-high resolution "gap-filler"
directly beneath the track of the sonar. Co-registration of
sidescan and laser imagery provides significant improvements
for search and recovery, bottom characterization and mine-hunting
operations, with the laser data offering the potential of
on-the-fly target identification, augmenting the sonar's extended
abilities for target detection. |
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Figure 5. GeoDAS-LLS, showing data from the Raytheon
LS-4096. |
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NOT JUST ANOTHER PRETTY PICTURE...
This spring, OIC completed it's modifications to GeoDAS to support
Electronic Still Camera imaging. The completed interface retains
the "look-and-feel" of the orginal GeoDAS user interface,
while allowing continuous acquistion, processing and display
of single or dual camera imagery, at data rates up to 10 MB
per second. The interface supports multiple modes of display,
including scrolling, binocular and single image view, to accommodate
images up to 1280 by 1280 pixels on a side, at 16-bits dynamic
range. A dual camera configuration at one Hertz frame rate in
continuous operation mode will fill a 60 GB 8-mm tape in just
over 2 hours. Dual tape-drives allow automatic roll-over, for
uninterrupted logging (provided you brought A LOT of tapes...).
Retaining the basic GeoDAS format while accommodating data records
easily 1000 times more than your average sidescan record proved
challenging, but the result provides the same processing, targeting,
logging and QA/QC interface as available for scan-line based
systems, minimizing operator re-training, and maximizing product
reliability. |
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Figure 6. GeoDAS-ESC, in the dual-camera configuration.
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DATA INTEGRATION
While the above examples demonstrate available solutions for
the mechanics of multi-sensor, high-rate data acquisition,
there remains the issue of operator overload, and interpretation.
Simply put, someone has to look at all this. If we can now
simultaneously acquire swath acoustic data, providing a half-kilometer
swath of acoustic imagery and bathymetry, and optical data,
providing sub-centimeter scale imagery over a patch which
might barely cover the nadir footprint of the sonar, how are
we to co-register and compare the two modalities?
ROVer's Eye, a real-time terrain visualization package developed
by OIC under DARPA funding, provides one option. ROVer integrates
a hi-speed 3-D rendering package with GeoDAS's realtime-processing
and target analysis package, to provide an interactive immersive
experience, wherein underwater vehicle operators can work
not only with existing models, but see new data from on-board
sensors evolve into the current model in realtime. ROVer accommodates
simultaneous inputs from sidescan, bathymetry and navigation
systems, while accessing a database of existing data, targets
and as-built structure models. Operators see new data evolve
in a model before them, just as headlights reveal the road
ahead to night-time drivers. "Road-signs" in ROVer
reveal not gratuitous advertising (nor Burma Shave ditties)
but full resolution images of proximal targets, which "pop-up"
as the vehicle passes by. The combination of synoptic swath
data with detail-rich target imagery in a fully geo-coded
environment provides a whole new level of data interpretation
experience. |
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Figure 7. ROVer's Eye view of the bottom of Honolulu Harbor,
with TargetView mode on, providing automatic notification of
proximity of previously marked targets. |
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SUMMARY
Seafloor imaging is a data-intensive process. Down-sampling
strategies compromise both image resolution and quantitative
information potential. GeoDAS, an off-the-shelf solution for
acoustic and non-acoustic seabed data acquisition and processing,
can provide a uniform interface to sonar, laser and camera-based
imaging systems, handling raw data rates up to 10 MB per second
with no down-sampling losses, while retaining realtime interactivity.
Examples are provided from working installations. |
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Dr. Thomas B. Reed IV is founder and president of Oceanic
Imaging Consultants, Inc. of Honolulu, HI. He received his undergraduate
education from Harvard University in 1982, where he majored
in Economic Geology, and completed his graduate work in Marine
Geology and Geophysics at Hawaii Institute of Geophysics, in
1987. |
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