Stream and Kuroshio Extension. J. Phys.
Oceanogr. 20, 860–879. [3.3]
Tai, C. K. and W. B. White, 1990: Eddy variability in
the Kuroshio Extension as revealed by GEOSAT
altimetry: Energy propagation away from the
jet, Reynolds stress and seasonal cycle. J. Phys.
Oceanogr. 20, 1761–1777. [3.3]
Tai, C. K. and C. Wunsch, 1983: Absolute measurement by satellite altimetry of the dynamic topography of the Pacific Ocean. Nature 301(5899),
408–410. [3.3]
Takahashi, T., T. T. Takahashi and S. C. Sutherland,
1995: An assessment of the role of the North
Atlantic as a CO 2 sink. Phil. Trans. Roy. Soc.
Lond. B, 348, 143–152. [6.3]
Takahashi, T., R. A. Feely, R. Weiss et al., 1997:
Global air–sea flux of CO 2 : An estimate based
on measurements of sea–air pCO 2 difference.
In: NAS Colloquium Volume on Carbon
Dioxide and Climate Change, C. D. Keeling
(ed), Proc. Natl. Acad. Sci. USA 94, 8292–8299.
[6.3]
Talley, L. D., 1984: Meridional heat transport in the
Pacific Ocean. J. Phys. Oceanogr. 14, 231–241.
[6.1]
Talley, L. D., 1985: Ventilation of the subtropical
North Pacific: The shallow salinity minimum.
J. Phys. Oceanogr. 15, 633–649. [4.2, 5.3]
Talley, L. D., 1988: Potential vorticity distribution in
the North Pacific. J. Phys. Oceanogr. 18, 89–106.
[5.4]
Talley, L. D., 1991: An Okhotsk Sea water anomaly:
Implications for sub-thermocline ventilation in the
North Pacific. Deep-Sea Res. 38 (suppl.), S171–
S190. [5.4]
Talley, L. D., 1993: Distribution and formation
of North Pacific Intermediate Water. J. Phys.
Oceanogr. 23, 517–537. [5.4]
Talley, L. D., 1996a: Antarctic Intermediate Water in
the South Atlantic. In: The South Atlantic: Present
and Past Circulation, G. Wefer, W. H. Berger,
G. Siedler and D. J. Webb (eds), Springer-Verlag,.
pp. 219–238. [4.6, 5.4]
Talley, L. D., 1996b: North Atlantic circulation and
variability, reviewed for the CNLS Conference,
Los Alamos, May 1995. Physica D 98, 625–646.
[5.4, 7.3]
Talley, L. D., 1997: North Pacific intermediate water
transports in the mixed water region. J. Phys.
Oceanogr. 27, 1795–1803. [5.4]
Talley, L. D., 1999a: Some aspects of ocean heat
transport by the shallow, intermediate and deep
overturning circulations. In: Mechanisms of
Global Climate Change at Millennial Time Scales,
Clark, Webb and Keigwin (eds), American
Geophysical Union, Washington, DC. Geophys.
Mono. Ser. 112, 1–22. [5.4]
Talley, L. D., 1999b: Mode waters in the subpolar North Atlantic in historical data
and during the WOCE period. International WOCE Newsletter, No. 37, 3–6, WOCE
International Project Office (unpublished document). [5.4, 7.1]
Talley, L. D., 1999c: Simple coupled midlatitude
climate models. J. Phys. Oceanogr. 29, 2016–
2037. [4.6]
Talley, L. D. and M. O. Baringer, 1997: Preliminary
results from WOCE hydrographic sections at 80°E
and 32°S in the central Indian Ocean. Geophys.
Res. Lett. 24, 2789–2792. [4.3]
Talley, L. D. and G. C. Johnson, 1994: Deep, zonal
subequatorial currents. Science 263, 1125–1128.
[4.2, 4.3, 4.5, 5.8]
Talley, L. D. and T. M. Joyce, 1992: The double silica maximum in the North Pacific. J. Geophys.
Res. 97, 5465–5480. [4.2]
Talley, L. D. and M. S. McCartney, 1982: Distribution
and circulation of Labrador Sea water. J. Phys.
Oceanogr. 12, 1189–1205. [5.4, 5.5]
Talley, L. D. and M. E. Raymer, 1982: Eighteen
Degree Water variability. J. Mar. Res. 40(suppl.),
725–775. [5.4, 7.3]
Tandon, A. and C. Garrett, 1996: On a recent
parameterization of mesoscale eddies. J. Phys.
Oceanogr. 26, 406–411. [5.2]
Tandon, A. and C. Garrett, 1997: Water mass formation from thermodynamics: a framework for
examining compatibility with dynamics. International WOCE Newsletter, No. 28, 34–36.
WOCE International Project Office (unpublished
document). [5.1]
Tandon, A. and K. Zahariev, 2000: Quantifying the
role of mixed layer entrainment for water mass
conversion in the North Atlantic. J. Phys.
Oceanogr. (in press). [5.1]
Taneda, T., T. Suga and K. Hanawa, 2000:
Subtropical mode water variation in the northwestern part of the north Pacific subtropical gyre.
J. Geophys. Res. 105, 19591–19598. [5.4]
Tang, G. L., 1991: A two-dimensional thermodynamical model for sea ice advance and retreat
in the Newfoundland marginal ice zone.
J. Geophys. Res. 96, 4723–4737. [1.2]
Tanimoto, Y., N. Iwasaka, K. Hanawa and Y. Toba,
1993: Characteristic variations of sea surface temperature with multiple time scales on the North
Pacific. J. Climate 6, 1153–1160. [5.4]
Tans, P. P., I. Y. Fung and T. Takahashi, 1990:
Observational constraints on the global atmospheric CO 2 budget. Science 247, 1431–1438. [6.3]
REFERENCES
672
Oceanogr. 20, 860–879. [3.3]
Tai, C. K. and W. B. White, 1990: Eddy variability in
the Kuroshio Extension as revealed by GEOSAT
altimetry: Energy propagation away from the
jet, Reynolds stress and seasonal cycle. J. Phys.
Oceanogr. 20, 1761–1777. [3.3]
Tai, C. K. and C. Wunsch, 1983: Absolute measurement by satellite altimetry of the dynamic topography of the Pacific Ocean. Nature 301(5899),
408–410. [3.3]
Takahashi, T., T. T. Takahashi and S. C. Sutherland,
1995: An assessment of the role of the North
Atlantic as a CO 2 sink. Phil. Trans. Roy. Soc.
Lond. B, 348, 143–152. [6.3]
Takahashi, T., R. A. Feely, R. Weiss et al., 1997:
Global air–sea flux of CO 2 : An estimate based
on measurements of sea–air pCO 2 difference.
In: NAS Colloquium Volume on Carbon
Dioxide and Climate Change, C. D. Keeling
(ed), Proc. Natl. Acad. Sci. USA 94, 8292–8299.
[6.3]
Talley, L. D., 1984: Meridional heat transport in the
Pacific Ocean. J. Phys. Oceanogr. 14, 231–241.
[6.1]
Talley, L. D., 1985: Ventilation of the subtropical
North Pacific: The shallow salinity minimum.
J. Phys. Oceanogr. 15, 633–649. [4.2, 5.3]
Talley, L. D., 1988: Potential vorticity distribution in
the North Pacific. J. Phys. Oceanogr. 18, 89–106.
[5.4]
Talley, L. D., 1991: An Okhotsk Sea water anomaly:
Implications for sub-thermocline ventilation in the
North Pacific. Deep-Sea Res. 38 (suppl.), S171–
S190. [5.4]
Talley, L. D., 1993: Distribution and formation
of North Pacific Intermediate Water. J. Phys.
Oceanogr. 23, 517–537. [5.4]
Talley, L. D., 1996a: Antarctic Intermediate Water in
the South Atlantic. In: The South Atlantic: Present
and Past Circulation, G. Wefer, W. H. Berger,
G. Siedler and D. J. Webb (eds), Springer-Verlag,.
pp. 219–238. [4.6, 5.4]
Talley, L. D., 1996b: North Atlantic circulation and
variability, reviewed for the CNLS Conference,
Los Alamos, May 1995. Physica D 98, 625–646.
[5.4, 7.3]
Talley, L. D., 1997: North Pacific intermediate water
transports in the mixed water region. J. Phys.
Oceanogr. 27, 1795–1803. [5.4]
Talley, L. D., 1999a: Some aspects of ocean heat
transport by the shallow, intermediate and deep
overturning circulations. In: Mechanisms of
Global Climate Change at Millennial Time Scales,
Clark, Webb and Keigwin (eds), American
Geophysical Union, Washington, DC. Geophys.
Mono. Ser. 112, 1–22. [5.4]
Talley, L. D., 1999b: Mode waters in the subpolar North Atlantic in historical data
and during the WOCE period. International WOCE Newsletter, No. 37, 3–6, WOCE
International Project Office (unpublished document). [5.4, 7.1]
Talley, L. D., 1999c: Simple coupled midlatitude
climate models. J. Phys. Oceanogr. 29, 2016–
2037. [4.6]
Talley, L. D. and M. O. Baringer, 1997: Preliminary
results from WOCE hydrographic sections at 80°E
and 32°S in the central Indian Ocean. Geophys.
Res. Lett. 24, 2789–2792. [4.3]
Talley, L. D. and G. C. Johnson, 1994: Deep, zonal
subequatorial currents. Science 263, 1125–1128.
[4.2, 4.3, 4.5, 5.8]
Talley, L. D. and T. M. Joyce, 1992: The double silica maximum in the North Pacific. J. Geophys.
Res. 97, 5465–5480. [4.2]
Talley, L. D. and M. S. McCartney, 1982: Distribution
and circulation of Labrador Sea water. J. Phys.
Oceanogr. 12, 1189–1205. [5.4, 5.5]
Talley, L. D. and M. E. Raymer, 1982: Eighteen
Degree Water variability. J. Mar. Res. 40(suppl.),
725–775. [5.4, 7.3]
Tandon, A. and C. Garrett, 1996: On a recent
parameterization of mesoscale eddies. J. Phys.
Oceanogr. 26, 406–411. [5.2]
Tandon, A. and C. Garrett, 1997: Water mass formation from thermodynamics: a framework for
examining compatibility with dynamics. International WOCE Newsletter, No. 28, 34–36.
WOCE International Project Office (unpublished
document). [5.1]
Tandon, A. and K. Zahariev, 2000: Quantifying the
role of mixed layer entrainment for water mass
conversion in the North Atlantic. J. Phys.
Oceanogr. (in press). [5.1]
Taneda, T., T. Suga and K. Hanawa, 2000:
Subtropical mode water variation in the northwestern part of the north Pacific subtropical gyre.
J. Geophys. Res. 105, 19591–19598. [5.4]
Tang, G. L., 1991: A two-dimensional thermodynamical model for sea ice advance and retreat
in the Newfoundland marginal ice zone.
J. Geophys. Res. 96, 4723–4737. [1.2]
Tanimoto, Y., N. Iwasaka, K. Hanawa and Y. Toba,
1993: Characteristic variations of sea surface temperature with multiple time scales on the North
Pacific. J. Climate 6, 1153–1160. [5.4]
Tans, P. P., I. Y. Fung and T. Takahashi, 1990:
Observational constraints on the global atmospheric CO 2 budget. Science 247, 1431–1438. [6.3]
REFERENCES
672