This component of the Deep Basin experiment produced 30 current meter records from 6 moorings. From here you can
If you download any of the records you should read the note on file format.
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The Deep Basin Experiment took place in and around the Brazil
Basin, a region west of the Mid-Atlantic Ridge stretching from
the Ceara Rise near the equator in the north, to the Santos
Plateau - Rio Grande Rise system near 30 deg S. A principal
objective was to understand the mean circulation below the
thermocline; the Brazil Basin was selected because it is a region
of expected low eddy KE, a useful attribute in a program aimed at
the mean flow.
Five current meter arrays were deployed at passages that connect
the Brazil Basin to neighboring regions. Each array was in the
water for approximately two years. We are concerned here with a
line of 13 moorings that was installed jointly by IFM-Kiel and
the Woods Hole Oceanographic Institute, along the southwestern
boundary of the basin. Six of the moorings were deployed by WHOI
and were assigned the WOCE designation ACM3. The remaining 7
moorings (one of which was not recovered) were deployed by IFM-Kiel
and comprise ACM12. The ACM12 moorings were installed during
January 1991 and were recovered during December 1992.
The joint array extended in a line running from the edge of the
continental shelf, southeastward across the Santos Plateau and the
Vema Channel, to the Rio Grande Rise
(see map). The goal was to measure inflow and outflow along the
southern boundary of the Brazil Basin. For a detailed description
of the purpose and rationale of this segment of the Deep Basin
experiment, as well as data plots and statistics, see the joint
technical report WHOI-94-07, IFM-Kiel 243. In addition, there is
a relevant note in WOCE Newsletter #17, dated November 1994.
See also
Hogg, N.G., W.B. Owens, G. Siedler and W. Zenk (1996): Circulation
in the deep Brazil Basin. In The South Atlantic (ed. G. Wefer,
et al). Berlin: Springer. 644pp, pp249-260.
Zenk, W. and N.G.Hogg (1996): Warming trend in Antarctic Bottom Water
flowing into the Brazil Basin. Deep-Sea Res. I, 43(9), 1461-1473.
Boebel, O., C. Schmid and W. Zenk (1997): Flow and recirculation of
Antarctic Intermediate Water across the Rio Grande Rise. J. Geophys.
Res., 102(C9), 967-986.
Hogg, N.G., and W. Zenk (1997): Long period changes in the bottom
water flowing through Vema Channel. J. Geophys. Res., 102(C7),
15639-15646.
Mueller, T.J., Y. Ikeda, N. Zangenberg and L.V.Nonato (1998): Direct
measurements of western boundary currents off Brazil between 20S and
28S. J. Geophys. Res., 103(C3), 5429-5437.
Hogg, N.G., and W.B. Owens (1999): Direct measurement of the deep
circulation within the Brazil Basin. Deep-Sea Res. II, 46, 335-353.
Hogg, N.G., G. Siedler and W. Zenk (1999): Circulation and variability
at the southern boundary of the Brazil Basin. J. Phys. Oceanogr., 29,
145-157.
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These files have been compressed with the ZIP compression utility.
After downloading them, you will need to expand them. On a PC,
WinZip or Pkunzip will do the job. Other utilities are available
for the Unix and Macintosh environments. After expansion, you will
have ascii files in OSU's stranger format.
The stranger format begins with several lines of header information
that are meant to be machine-readable. They contain a Fortran format
specification that will be useful in reading the file, a pointer to the
first line of data, and a description of the data. Each line of the
current record itself contains the time of the sample, the values
recorded, and a line count.
Please be aware that end-of-line in these files is a carriage-return
plus line-feed (the PC convention). This means that in a Unix
environment (where a single line-feed serves as end-of-line) you may
want to remove the carriage-returns.
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mooring instr depth instr type dates metadata download
BW/333
230 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BW/333
475 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BW/333
680 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BW/333
885 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BM/334
230 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BM/334
470 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BM/334
870 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BM/334
1370 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BM/334
2140 meters
Aanderaa RCM8
03 Jan 91 - 26 Nov 92
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BE/335
275 meters
Aanderaa RCM8
04 Jan 91 - 25 Nov 92
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BE/335
515 meters
Aanderaa RCM8
04 Jan 91 - 25 Nov 92
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BE/335
915 meters
Aanderaa RCM8
04 Jan 91 - 25 Nov 92
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BE/335
1415 meters
Aanderaa RCM8
04 Jan 91 - 25 Nov 92
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BE/335
2510 meters
Aanderaa RCM8
04 Jan 91 - 25 Nov 92
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BE/335
3215 meters
Aanderaa RCM8
04 Jan 91 - 25 Nov 92
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VW/336
470 meters
Aanderaa RCM8
18 Mar 91 - 05 Dec 92
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VW/336
870 meters
Aanderaa RCM8
10 Jan 91 - 05 Dec 92
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VW/336
2970 meters
Aanderaa RCM8
10 Jan 91 - 06 Dec 92
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VW/336
3620 meters
Aanderaa RCM8
10 Jan 91 - 05 Dec 92
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VE/338
720 meters
Aanderaa RCM8
12 Jan 91 - 05 Dec 92
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VE/338
1100 meters
Aanderaa RCM8
12 Jan 91 - 05 Dec 92
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VE/338
2900 meters
Aanderaa RCM8
12 Jan 91 - 05 Dec 92
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VE/338
3850 meters
Aanderaa RCM8
12 Jan 91 - 05 Dec 92
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VE/338
4150 meters
Aanderaa RCM8
12 Jan 91 - 05 Dec 92
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VE/338
4425 meters
Aanderaa RCM8
12 Jan 91 - 05 Dec 92
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VE/338
4625 meters
Aanderaa RCM8
12 Jan 91 - 05 Dec 92
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DBK/343
525 meters
Aanderaa RCM5
04 Mar 91 - 19 Aug 91
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DBK/343
925 meters
Aanderaa RCM5
13 Jan 91 - 20 Dec 91
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DBK/343
3025 meters
Aanderaa RCM5
13 Jan 91 - 06 Dec 92
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DBK/343
3602 meters
Aanderaa RCM5
13 Jan 91 - 06 Dec 92
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Brief description of ACM12
Zenk, W., K.G. Speer and N.G. Hogg (1993): Bathymetry at the Vema
Sill. Deep-Sea Res. 40(9), 1925-1933.
Format of the current records