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and Geochemical Tracer Transport, Vol. 284
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Olbers, D. J. and C. Wübber, 1991: The role of wind
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Olbers, D. J., M. Wenzel and J. Willebrand, 1985:
The inference of North Atlantic circulation patterns from climatological hydrographic data. Rev.
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Alfred Wegener Institute for Polar and Marine
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Ollitrault, M., 1999: MARVOR floats reveal intermediate circulation in the western equatorial and
tropical South Atlantic (30°S to 5°N). International WOCE Newsletter, No. 34, 7–10,
WOCE International Project Office (unpublished
document). [3.2]
Olson, D. B., R. A. Fine and A. L. Gordon, 1992:
Convective modifications of water masses in the
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[5.4]
Ono, T., S. Watanabe, K. Okuda and M. Fukasawa,
1998: Distribution of total carbonate and
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30°N. J. Geophys. Res. 103, 30873–30883.
[6.3]
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Circumpolar Current at Drake Passage. J. Mar.
Res. 40(suppl.), 481–507. [4.6]
Nowlin, Jr., W. D. and J. M. Klinck, 1986: The
physics of the Antarctic Circumpolar Current. Rev.
Geophys. Space Phys. 24, 469–491. [4.6, 4.7]
Nowlin, Jr., W. D., S. J. Worley and T. Whitworth, III,
1985: Methods for making point estimates of eddy
heat flux as applied to the Antarctic circumpolar
current. J. Geophys. Res. 90, 3305– 3324. [4.6]
Nowlin, W. D. Jr., M. Briscoe, N. Smith et al., 2000:
Evolution of a sustained ocean observing system.
Bull. Amer. Meteor. Soc. (submitted) [7.4]
Nurser, A. J. G. and J. C. Marshall, 1991: On the
relationship between subduction rates and diabatic forcing of the mixed layer. J. Phys.
Oceanogr. 21, 1793–1802. [7.3]
Nurser, A. J. G., R. Marsh and R. G. Williams, 1999:
Diagnosing water mass formation from air–sea
fluxes and surface mixing. J. Phys. Oceanogr. 29,
1468–1487. [5.1, 5.2]
O’Connor, B. M., R. A. Fine, K. A. Maillet and D. B.
Olson, 2000: Formation rates of Subtropical
Underwater in the Pacific Ocean. Deep-Sea Res.
(submitted). [5.8]
O’Dwyer, J. and R. G. Williams, 1997: The climatological distribution of potential vorticity over the
abyssal Ocean. J. Phys. Oceanogr. 27, 2488–
2506. [7.1]
Oakey, N. S. and J. A. Elliott, 1980: The variability
of temperature gradient microstructure observed
in the Denmark Strait. J. Geophys. Res. 85, 1933–
1944. [5.2]
Obata, A., R. Furue, S. Aoki and N. Suginohara,
1996: Modeling layered structure in deep Pacific
circulation. J. Geophys. Res. 101, 3663–3674. [4.2]
Oberhuber, J. M., 1988: An atlas based on the
COADS data set: the budgets of heat, buoyancy
and turbulent kinetic energy at the surface of the
global
ocean.
Max-Planck
Institut
für
Meteorologie, Hamburg, Report No. 15, 19 pp.
[5.1, 6.2]
Oberhuber, J. M., 1993: Simulation of the Atlantic
circulation with a coupled sea ice-mixed layerisopycnal general circulation model, Parts I and
II. J. Phys. Oceanogr. 23, 808–829, 830–845.
[2.2, 2.3]
Ochoa, J. and N. A. Bray, 1991: Water mass
exchange in the Gulf of Cadiz. Deep-Sea Res. 38
(suppl.) S465–S503. [5.7]
Ohlmann, J. C., P. P. Niiler, C. A. Fox and
R. R. Leben, 2001: Eddy energy and shelf interactions in the Gulf of Mexico. J. Geophys. Res. (in
press). [4.1]
Olbers, D. J., 1998: Comment on ‘On the obscurantist physics of “form drag” in theorizing about the
Circumpolar Current’. J. Phys. Oceanogr. 28,
1647–1654. [4.6]
Olbers, D. J. and C. Völker, 1996: Steady states and
variability in oceanic zonal flows. In: Decadal
Climate Variability Dynamics and Predictability,
D. Anderson and J. Willebrand (eds), SpringerVerlag, Berlin, pp. 407–443. [4.6]
Olbers, D. J. and M. Wenzel, 1989: Determining
diffusivities from hydrographic data by inverse
methods with applications to the circumpolar current. In: Modelling the Ocean General Circulation
and Geochemical Tracer Transport, Vol. 284
of NATO ASI Series C, J. Willebrand and D. L . T.
Anderson (eds), Kluwer Acad. Publ., Dordrecht,
pp. 95–122. [4.6, 5.2]
Olbers, D. J. and C. Wübber, 1991: The role of wind
and buoyancy forcing of the Antarctic Circumpolar Current. In: Strategies for Future Climate
Research, M. Latif (ed.), Max-Planck Institut für
Meteorologie, pp. 161–191. [4.6]
Olbers, D. J., M. Wenzel and J. Willebrand, 1985:
The inference of North Atlantic circulation patterns from climatological hydrographic data. Rev.
Geophys. 23, 313–356. [5.2, 7.1]
Olbers, D. J., V. Gouretski, G. Seiss and J. Schröter,
1992: Hydrographic Atlas of the Southern Ocean.
Alfred Wegener Institute for Polar and Marine
Research, Bremerhaven, 17 pp.;82 plates. [4.2,
4.6]
Ollitrault, M., 1999: MARVOR floats reveal intermediate circulation in the western equatorial and
tropical South Atlantic (30°S to 5°N). International WOCE Newsletter, No. 34, 7–10,
WOCE International Project Office (unpublished
document). [3.2]
Ollitrault, M., G. Loaëc and C. Dumortier, 1994:
MARVOR: a multicycle RAFOS float. Sea Tech.
35, 39–44. [3.2]
Ollitrault, M., 1999: MARVOR floats reveal intermediate circulation in the western equatorial and
tropical South Atlantic (30°S to 5°N). International WOCE Newsletter, No. 34, 7–10,
WOCE International Project Office (unpublished
document). [3.2]
Olson, D. B., R. A. Fine and A. L. Gordon, 1992:
Convective modifications of water masses in the
Agulhas. Deep-Sea Res. 39(suppl.), S163–S181.
[5.4]
Ono, T., S. Watanabe, K. Okuda and M. Fukasawa,
1998: Distribution of total carbonate and
related properties in the North Pacific along
30°N. J. Geophys. Res. 103, 30873–30883.
[6.3]
REFERENCES
653