Keith vonder Heydt
Woods Hole Oceanographic Institution
Woods Hole, MA 02543
Arthur M. Baggeroer
Massachusetts Institute of Technology
Cambridge, MA 01239
1. Introduction
The focus of work proposed for the CEAREX Acoustics Camp (A-Camp) was
a better understanding of the environmental dependencies of the acoustic
character of the Arctic. In addition to direct acoustic measurements at
A-Camp using a large horizontal hydrophone array, multiple vertical
hydrophone arrays and geophone arrays, regular CTD and meteorology
measurements were made.
Acoustic data were recorded by a multichannel digital acquisition
system, capable of >120 dB dynamic range, developed at WHOI and described
in "High continuous bandwidth multi-channel acquisition system" (von der
Heydt, 1991). The MIT/WHOI digital data set consisted of 40 channels
devoted to hydrophone sensors of the horizontal array and 12 channels from
four 3-axis geophones. Channels were selectively recorded for periods of
days on a 14-channel FM tape recorder. All data included on the CD-ROM
"CEAREX-1" were acquired on the digital system.
In support of coherent processing techniques for the low frequency
data (1 to 250 Hz) recorded from the hydrophone arrays, an independent
system, operating in the 10 kHz region, was used to continuously measure
time delays between six tone burst sources and the array sensors, all at
a common depth. These travel times were later used to estimate relative
locations of sensors. Nominal estimates of these locations are tabulated
as supporting data on the CD-ROM.
2. Rationale
The following interests highlight the motivation for acoustic work
conducted at the CEAREX A-Camp:
2.1. Previous work has shown that 3-axis geophones can provide
superior data compared to hydrophones for understanding acoustic
energy loss mechanisms related to ice scattering and mode conversion.
For this purpose "Plate Wave" signals were generated at many sites
about the camp by detonating small explosive charges deployed through
holes in the ice at depths ranging from 4 to 64 feet. These signals
were recorded on both hydrophones and geophones.
2.2. Earlier Arctic work has shown both high spatial and temporal
coherence. While high temporal coherence is not surprising given the
lack of surface roughness due to the ice cover, the high spatial
coherence was unexpected. An objective of the CEAREX effort was to
continue these investigations using a horizontal hydrophone array with
a 20 km aperture. A 300 cubic inch airgun was used as the signal
source from the Oceanography Camp (O-Camp) at a range of 200 km.
2.3. Two further objectives were a continuation of Arctic ambient
noise work for the purpose of compiling event statistics, and the
acquisition of long time series receptions from the Greenland Sea
tomography array.
The report "CEAREX "A"-Camp: Navigation, Bathymetry, CTD, Meteorology,
and LORFAR Data Report (von der Heydt, et al., 1991) is a digest of
navigation, bathymetry, CTD, meteorology and one type of ambient noise
acoustic data acquired during the CEAREX experiment at the Acoustic ("A")
Camp site over the period 23 March through 20 April 1989. Other pertinent
information is included in this report that would be useful to anyone
interested in the acoustic data either as presented in the "sampler" data
set on the CD-ROM "CEAREX-1" or from our complete data set from the A-Camp
experiment.
Papers and reports resulting from analysis of the data set include
Fricke (1991), Gerstoft and Schmidt (1991), Miller and Schmidt (1991),
Peal (1990), Schmidt and LePage (1991, work in progress), Schmidt and
Kim (1991, in preparation), and Seong (1991.)
3. Data Format Description
Each file begins with an ASCII header of 512 bytes with information
concerning the experiment, the number of sensors, and the number of data
values in the file. A stream of all the data for the first sensor follows
this header. The end of the data for the sensor is indicated by a newline
character. The data for the second sensor follows in the same way, with
the sequence repeated for all sensors. The last record in the file may be
padded to 512 characters with blanks. All data were sampled at 1 KHz.
A listing of sensor locations relative to the nominal origin at sensor 9
is given in the description of file 3.
The Fortran data format is E8.6; the C language format is 13.6e.
4. Data Files
Files are in the sub-directory \NOISE\ACOUSTIC on this CD-ROM.
4.1. File CRX22.DAT - AMBIENT NOISE
This file contains 700416 data values (700.416 seconds) from each of four
sensors. These data were acquired as an ambient noise experiment during
a particularly windy day in the field. The initial start time of the data
is 4/11/89/1534Z. The wind speed on this day exceeded twenty knots. The
sensors recorded on the file are (in order): NE320, NW7000, G4Y, and G4Z.
The first two are hydrophones with a sensitivity of -160 db re: 1 volt
per micropascal. The first hydrophone was hardwired to the acquisition
equipment at base camp. The second hydrophone, NW7000, communicated with
base camp via a radio link with 10db of gain. A gain normalization was
applied to the data from this sensor to make the hydrophone gains
consistent. The last two sensors, G4Y and G4Z, include the horizontal and
the vertical component, respectively, of geophone G4.
Total file size is 39223813 bytes, consisting of a 512-character
header, 4 groups of 700416 values each (14 characters per value), a
newline (0D hexadecimal) following each group and an additional newline at
the end of the file. For the CD-ROM, the files were converted into
512-character records.
For cross-referencing with original data held by the investigators,
this file contains data copied from WHOI optical disk CRX22.dat. 72
records starting at record 157 are included, for channels 24, 36, 50, and
51. Channel 36 is scaled by 0.31623 to normalize for preamp gain, as
described above.
4.2. File CRX52.DAT - PLATE WAVE EXPERIMENT
This file contains 450001 values (450.001 seconds) from each of six
sensors: NW20, APEX, NE40, G1X, G1Y, and G1Z. The data were acquired
during a `Plate Wave Experiment' in which primer cord and SUS explosives
were set off near the A-Camp. The data were collected at 1631Z 16 April
1989.
Three shot events are recorded in this file: a primer cord shot at
32 feet depth; a second one at 64 feet depth; and finally a SUS shot at
800 feet. The first three sensors in the file are ordinary hardwired
hydrophones with sensitivity of -160 db re 1V/uPa. The latter three
include both horizontal components and the vertical component of geophone
G1.
Total file size is 37800603 bytes. This consists of a 512-character
header, 4 groups of 450001 values each (14 characters per value), a newline
following each group and an additional newline at the end of the file.
For cross-referencing with original data held by the investigators,
this file contains data copied from WHOI optical disk CRX52.dat. Fifty-four
records starting at record 556 are included for channels 5, 9, 11, 40, 41
and 42.
4.3. File CRX58.DAT - REMOTE AIR GUNS / AMBIENT NOISE
This file contains 55001 data values from 50 sensors, collected at
0848Z 17 April 1989. Only 55 seconds of data are included because of the
large number of sensors. During this interval, an air gun was shooting
at a 48 second period from the O-Camp, approximately 300 km to the
northeast. With signal processing, it is possible to detect these signals.
Otherwise, the data can also serve as a sample of ambient noise on a fairly
quiet day in the Arctic.
The first 38 channels are hydrophones with a sensitivity of -160 dB
re: 1 volt per micropascal. The last twelve channels are geophones. The
last eight hydrophones on the file were radio-linked phones with an extra
10 db of gain, for which no normalization is made.
The following is a list of "X-Y" sensor position estimates in meters
realtive to a Y-axis baseline between the apex sensor, Ch9, and Ch7. The
position listing is in the order of the channels in the data file (note
that Ch16 has been deleted.) Channels 2, 4, 6, 8, 10 and 12 were "source"
sensors used for the acousting tracking system, from which these positions
were derived. GX and GY denote the horizontal components of a geophone,
GZ denotes the vertical component.
ch0: 5755.07 2583.25 S8
ch 1: 14.0834 17.537 NE20
ch 2: 1338.32 -1742.18 S9
ch 3: 51.0266 62.375 NE80
ch 4: -5563.56 -3346.58 S10
ch 5: -34.8596 30.741 NW40
ch 6: -2443.09 4484.51 S11
ch 7: 23.3318 -9.845 SE20
ch 8: -2.7237 288.45
ch 9: 0 0 APEX
ch 10: -2.7237 -401.526 S13
ch 11: 28.6041 30.965 NE40
ch 12: -21.6686 12.825 NW20
ch 13: -10.28 -13.397 SW20
ch 14: -27.8904 -34.931 SW40
ch 15: 37.2584 -29.693 SE40
ch 16: 64.7682 -50.206 SE80 (deleted from file)
ch 17: 129.213 -99.734 SE160
ch 18: -59.3577 55.013 NW80
ch 19: -49.2728 -62.052 SW80
ch 20: 103.035 121.974 NE160
ch 21: -96.0213 -122.533 SW160
ch 22: -117.35 99.552 NW160
ch 23: -272.318 222.216 NW320
ch 24: 170.479 197.15 NE320
ch 25: -187.487 -289.897 SW320
ch 26: 263.392 -211.6 SE320
ch 27: 547.593 -432.586 SE640
ch 28: -372.394 -568.349 SW640
ch 29: -499.854 415.074 NW640
ch 30: 402.652 489.644 NE640
ch 31: -1570.55 1156.8 NW2400
ch 32: -3054.26 2043.8 NW4800
ch 33: 1075.34 -766.27 SE1200
ch 34: 2118.93 -1530.41 SE2400
ch 35: 3880.64 -1319.69 SE4800
ch 36: -6252.05 3747.81 NW7000
ch 37: 8007.07 -141.98 SE9000
ch 38: -9458.89 6173.48 NW11000
Geophones:
ch 40: -31.38 45.66 G1X
ch 41: G1Y
ch 42: G1Z
ch 43: -27 -12 G2X
ch 44: G2Y
ch 45: G2Z
ch 46: 28.76 -5.07 G3X
ch 47: G3Y
ch 48: G3Z
ch 49: 22.95 49.21 G4X
ch 50: G4Y
ch 51: G4Z
Total file size is 38501263 bytes. This consists of a 512-character
header, 50 groups of 55001 values each (14 characters per value), a
newline following each group and an additional newline at the end of the
file.
For cross-referencing with original data held by the investigators,
this file contains data copied from WHOI optical disk CRX58.dat. Six
records starting at record 26 are included. Channel 16 was deleted due to
excessive noise.
5. References
Fricke, R. (1991) Finite Difference Solution For Acoustic Scattering From
Ice Keels and Rough Ice. MIT-WHOI Joint Program, Ph.D. thesis, May 1991.
In preparation for Journal of the Acoustical Society of America.
Gerstoft, P., and Schmidt, H. (1991) Boundary element approach to ocean
seismo-acoustic facet reverberation, Journal of the Acoustical Society of
America, 89(4), pp. 1629-1642.
Miller, B., and Schmidt, H. (1991) Observation and inversion of
seismo-acoustic waves in a complex Arctic ice environment, Journal of
the Acoustical Society of America, 89(4), pp. 1668-1685.
Peal, K.R. (1990) Arctic remote autonomous measurement platform - post
CEAREX engineering report. Woods Hole Oceanographic Institution. Technical
Report no. 90-46.
Schmidt, H. and LePage, K. (1991) Three-dimensional diffuse scattering by
a rough ice cover. Journal of the Acoustical Society of America, work in
progress.
Schmidt, H., and Kim, J. (1991) Numerical modeling of acoustic emission from
propagating cracks. Journal of the Acoustical Society of America, in
preparation.
Seong, W. (1991) Hybrid Galerkin Boundary Element Wavenumber Integration
Method for Acoustic Propagation in Laterally Inhomogenous Media.
Massachusetts Institute of Technology, Department of Oceanographic
Engineering, Ph.D. thesis.
von der Heydt, K.(1991) High Continuous Bandwidth Multichannel Acquisition
System. Woods Hole Oceanographic Institution. Technical Report no. 91-14.
von der Heydt, K., Galbraith, N.R., Baggeroer, A.B., Meunch, R., Guest, P.S.,
Davidson, K.L. (1991) CEAREX "A" - Camp: Navigation, Bathymetry, CTD,
Meteorology, and LOFAR Data Report. Woods Hole Oceanographic Institution.
Technical Memorandum no. WHOI-1-91, 152 pp. + appendix. Includes 14 color
plates.
6. Contact Information
Dr. Arthur B. Baggeroer (MIT PI, acoustics)
Massachusetts Institute of Technology
Building 5-204
77 Massachusetts Avenue
Cambridge, MA 01239
Phone: 617-253-4336
Telemail: A.BAGGEROER/Omnet
Internet: abb@arctic.mit.edu
Keith von der Heydt, (WHOI PI, data acquisition systems)
Woods Hole Oceanographic Institution
Woods Hole, MA 02543
Phone: 508-457-2000
Telemail: K.VONDERHEYDT/Omnet
Internet: kvdh@polar.whoi.edu
Dr. Ira Dyer (acoustics)
Massachusetts Institute of Technology
Building 5-212
77 Massachusetts Avenue
Cambridge, MA 01239
Phone: 617-253-6824
Telemail: I.DYER/Omnet
Dr. Henrik Schmidt (acoustics)
Massachusetts Institute of Technology
Building 5-204
77 Massachusetts Avenue
Cambridge, MA 01239
Phone: 617-253-5727
Telemail: H.SCHMIDT.MIT/Omnet
Dr. Robin Muench (oceanography)
Science Applications International Corporation
13400B Northrup Way
Suite 36
Bellevue, WA 98005
Phone: 206-747-7152
Telemail: R.MUENCH/Omnet
Dr. Ken Davidson (meteorology)
Naval Postgraduate School
Department of Meteorology, Code MR/Gs
Monterey, CA 93943-5000 USA
Phone: 408-646-2451
Telemail: K.DAVIDSON/Omnet
Edward K. Scheer (acoustics processing)
Woods Hole Oceanograhic Institution
Woods Hole, MA 02543
Phone: 508-457-2000
Internet: eks@polar.whoi.edu
T.C. Yang (acoustics, vertical arrays)
Naval Research Laboratory
4555 Overlook Avenue SW
Washington DC 20375-5000
Telemail: T.YANG/Omnet
Peter Weibe (biology)
Woods Hole Oceanographic Institution
Woods Hole, MA 02543
Phone: 508-457-2000
Charles Greene (biology)
Cornell University
Ecology and Systematics
Ithaca, NY
Telemail: C.GREEN/Omnet
7. Acknowledgments
We would like to acknowledge the following people, some as participants
at the CEAREX A-Camp, and some for work in preparation for and analysis
following the field effort. In some cases these people have made independent
submissions of data to the CD-ROM "CEAREX-1".
Jay Ardai, LDGO; Tom Bordley, NRL (during CEAREX); John Borge,
Luftransport; Tom Curtin, ONR; Edgar Depowski, Luftransport;
Greg Duckworth, BBN; Ira Dyer, MIT; Rob Fricke, MIT; Nan
Galbraith, WHOI; Allan Gill, AE; Chuck Green, Cornell; Peter Guest,
NPS; Rob Handy, WHOI; Pat Kelly, NRL (during CEAREX); Neil McPhee,
WHOI; Robin Muench, SAIC; Bob Obrochta, ONR; Ken Peal, WHOI; Ken
Prada, WHOI; Henrik Schmidt, MIT; Don Spiel, NPS; Dean Stuart,
PSC; Matt Valley, JCSAC; Pete Weibe, WHOI.