Browning, G. L., W. R. Holland, H.-O. Kreiss and
S. J. Worley, 1990: An accurate hyperbolic system
for approximately hydrostatic and incompressible
oceanographic flows. Dyn. Atmos. Oceans 14,
303–332. [7.2]
Bruce, J. G., D. R. Johnson and J. C. Kindle, 1994:
Evidence for eddy formation in the eastern
Arabian Sea during the northeast monsoon.
J. Geophys. Res. 99, 7651–7664. [3.3]
Bryan, F., 1986: High latitude salinity effects and
inter-hemispheric
thermohaline
circulations.
Nature, 323, 301–304. [5.6]
Bryan, F., 1987: Parameter sensitivity of primitive equation ocean general circulation models.
J. Phys. Oceanogr. 17, 970–985. [2.2, 2.3, 4.3, 5.2]
Bryan, F., 1998: Climate drift in a multicentury integration of the NCAR Climate System Model.
J. Climate 11, 1455–1471. [2.3, 7.4]
Bryan, F. O. and W. R. Holland, 1989: A high resolution simulation of the wind- and thermohalinedriven circulation in the North Atlantic Ocean. In:
Parameterization of Small-Scale Processes, Proc.
Hawaiian Winter Workshop, P. Müller and
D. Henderson (eds), Hawaii Inst. Geophys. Spec.
Publ., pp. 99–115. [2.2, 7.2]
Bryan, K., 1969: A numerical method for the study
of the circulation of the world ocean. J. Comp.
Phys. 4, 347–376. [2.2, 2.3, 5.2]
Bryan, K., 1982: Seasonal variation in meridional
overturning and poleward heat transport in the
Atlantic and Pacific Oceans: A model study.
J. Mar. Res. 40, 39–53. [2.2, 6.1]
Bryan, K., 1984: Accelerating the convergence to
equilibrium of ocean climate models. J. Phys.
Oceanogr. 14, 666–673. [2.3]
Bryan, K. and M. D. Cox, 1968: A nonlinear model
of an ocean driven by wind and differential heating. Parts I and II. J. Atmos. Sci. 25, 945–967,
968–978. [2.2]
Bryan, K. and M. D. Cox, 1972: The circulation of
the World Ocean: A numerical study. Part I,
A homogenous model. J. Phys. Oceanogr. 2, 319–
335. [4.6]
Bryan, K. and L. J. Lewis, 1979: A water mass model
of the world ocean. J. Geophys. Res. 84, 2503–
2517. [2.2, 7.2]
Bryan, K. and M. J. Spelman, 1985: The ocean’s
response to a CO 2 -induced warming. J. Geophys.
Res. 90, 11679–11688. [2.2]
Bryan, K., F. G. Komro, S. Manabe and
M. J. Spelman, 1982: Transient climate response
to increasing atmospheric carbon dioxide. Science
215, 56–58. [2.2]
Bryan, K., J. K. Dukowicz and R. D. Smith, 1999: On
the mixing coefficient in the parameterization
of bolus velocity. J. Phys. Oceanogr. 29, 2442–
2456. [2.2]
Bryden, H.L., 1979: Poleward heat flux and conversion of available potential energy in Drake
Passage. J. Mar. Res. 37, 1–22. [4.6]
Bryden, H. L., 1993: Ocean heat transport across 24°
latitude. In: Interactions Between Global Climate
Subsystems: The Legacy of Hann, G. A. McBean
and M. Hantel (eds), Geophys. Monographs,
Vol. 75, pp. 65–75. [6.1]
Bryden, H. L. and E. C. Brady, 1985: Diagnostic
model of the three-dimensional circulation in the
upper Equatorial Pacific Ocean. J. Phys.
Oceanogr. 15, 1255–1273. [4.3]
Bryden, H. L. and E. C. Brady, 1989: Eddy momentum and heat fluxes and their effects on the circulation of the Equatorial Pacific Ocean. J. Mar.
Res. 47, 55–79. [4.3]
Bryden, H. L. and M. M. Hall, 1980: Heat transport
by currents across 25°N latitude in the Atlantic
Ocean. Science 207, 884–886. [3.1, 6.3]
Bryden, H. L. and R. A. Heath, 1985: Energetic
eddies at the northern edge of the Antarctic
Circumpolar Current in the Southwest Pacific.
Prog. Oceanogr. 14, 65–87. [4.6]
Bryden, H. L. and T. H. Kinder, 1991: Steady twolayer exchange through the Strait of Gibraltar.
Deep-Sea Res. 38(suppl.), S445–S463. [5.7]
Bryden, H. L. and D. J. Webb, 1998: A perspective
on the need to build a dam across the Strait of
Gibraltar. EGS News Letter 69, December 1998,
1–3 (unpublished document). [5.7]
Bryden, H. L., D. Roemmich and J. Church, 1991:
Ocean heat transport across 24°N in the Pacific.
Deep-Sea Res. 38, 297–324. [1.2, 4.5, 6.1, 6.2]
Bryden, H. L., J. Candela and T. H. Kinder, 1994:
Exchange through the Strait of Gibraltar. Prog.
Oceanogr. 33, 201–248. [5.7]
Bryden, H. L., M. J. Griffiths, A. M. Lavin,
R. C. Maillard, G. Parilla and W. M. Smethie,
1996: Decadal changes in water mass characteristics at 24°N in the Subtropical North Atlantic
Ocean. J. Climate 9, 3162– 3086. [7.3, 7.4]
Bryson, A. E., Jr. and Y.-C. Ho, 1975: Applied
Optimal Control. Hemisphere, NY (revised), 481
pp. [7.1]
Bu, X. and M. Warner, 1995: Solubility of chlorofluorocarbon 113 in water and seawater. DeepSea Res. 42, 1151–1161. [5.8]
Bullister, J. L., 1989: Chlorofluorocarbons as time
dependent tracers in the Ocean. Ocean. Mag.
2, 12–17. [5.8]
Bullister, J. L. and D. P. Wisegarver, 1998: The solubility of carbon tetrachloride in water and seawater. Deep-Sea Res. 45, 1285–1302. [5.8]
REFERENCES
610
S. J. Worley, 1990: An accurate hyperbolic system
for approximately hydrostatic and incompressible
oceanographic flows. Dyn. Atmos. Oceans 14,
303–332. [7.2]
Bruce, J. G., D. R. Johnson and J. C. Kindle, 1994:
Evidence for eddy formation in the eastern
Arabian Sea during the northeast monsoon.
J. Geophys. Res. 99, 7651–7664. [3.3]
Bryan, F., 1986: High latitude salinity effects and
inter-hemispheric
thermohaline
circulations.
Nature, 323, 301–304. [5.6]
Bryan, F., 1987: Parameter sensitivity of primitive equation ocean general circulation models.
J. Phys. Oceanogr. 17, 970–985. [2.2, 2.3, 4.3, 5.2]
Bryan, F., 1998: Climate drift in a multicentury integration of the NCAR Climate System Model.
J. Climate 11, 1455–1471. [2.3, 7.4]
Bryan, F. O. and W. R. Holland, 1989: A high resolution simulation of the wind- and thermohalinedriven circulation in the North Atlantic Ocean. In:
Parameterization of Small-Scale Processes, Proc.
Hawaiian Winter Workshop, P. Müller and
D. Henderson (eds), Hawaii Inst. Geophys. Spec.
Publ., pp. 99–115. [2.2, 7.2]
Bryan, K., 1969: A numerical method for the study
of the circulation of the world ocean. J. Comp.
Phys. 4, 347–376. [2.2, 2.3, 5.2]
Bryan, K., 1982: Seasonal variation in meridional
overturning and poleward heat transport in the
Atlantic and Pacific Oceans: A model study.
J. Mar. Res. 40, 39–53. [2.2, 6.1]
Bryan, K., 1984: Accelerating the convergence to
equilibrium of ocean climate models. J. Phys.
Oceanogr. 14, 666–673. [2.3]
Bryan, K. and M. D. Cox, 1968: A nonlinear model
of an ocean driven by wind and differential heating. Parts I and II. J. Atmos. Sci. 25, 945–967,
968–978. [2.2]
Bryan, K. and M. D. Cox, 1972: The circulation of
the World Ocean: A numerical study. Part I,
A homogenous model. J. Phys. Oceanogr. 2, 319–
335. [4.6]
Bryan, K. and L. J. Lewis, 1979: A water mass model
of the world ocean. J. Geophys. Res. 84, 2503–
2517. [2.2, 7.2]
Bryan, K. and M. J. Spelman, 1985: The ocean’s
response to a CO 2 -induced warming. J. Geophys.
Res. 90, 11679–11688. [2.2]
Bryan, K., F. G. Komro, S. Manabe and
M. J. Spelman, 1982: Transient climate response
to increasing atmospheric carbon dioxide. Science
215, 56–58. [2.2]
Bryan, K., J. K. Dukowicz and R. D. Smith, 1999: On
the mixing coefficient in the parameterization
of bolus velocity. J. Phys. Oceanogr. 29, 2442–
2456. [2.2]
Bryden, H.L., 1979: Poleward heat flux and conversion of available potential energy in Drake
Passage. J. Mar. Res. 37, 1–22. [4.6]
Bryden, H. L., 1993: Ocean heat transport across 24°
latitude. In: Interactions Between Global Climate
Subsystems: The Legacy of Hann, G. A. McBean
and M. Hantel (eds), Geophys. Monographs,
Vol. 75, pp. 65–75. [6.1]
Bryden, H. L. and E. C. Brady, 1985: Diagnostic
model of the three-dimensional circulation in the
upper Equatorial Pacific Ocean. J. Phys.
Oceanogr. 15, 1255–1273. [4.3]
Bryden, H. L. and E. C. Brady, 1989: Eddy momentum and heat fluxes and their effects on the circulation of the Equatorial Pacific Ocean. J. Mar.
Res. 47, 55–79. [4.3]
Bryden, H. L. and M. M. Hall, 1980: Heat transport
by currents across 25°N latitude in the Atlantic
Ocean. Science 207, 884–886. [3.1, 6.3]
Bryden, H. L. and R. A. Heath, 1985: Energetic
eddies at the northern edge of the Antarctic
Circumpolar Current in the Southwest Pacific.
Prog. Oceanogr. 14, 65–87. [4.6]
Bryden, H. L. and T. H. Kinder, 1991: Steady twolayer exchange through the Strait of Gibraltar.
Deep-Sea Res. 38(suppl.), S445–S463. [5.7]
Bryden, H. L. and D. J. Webb, 1998: A perspective
on the need to build a dam across the Strait of
Gibraltar. EGS News Letter 69, December 1998,
1–3 (unpublished document). [5.7]
Bryden, H. L., D. Roemmich and J. Church, 1991:
Ocean heat transport across 24°N in the Pacific.
Deep-Sea Res. 38, 297–324. [1.2, 4.5, 6.1, 6.2]
Bryden, H. L., J. Candela and T. H. Kinder, 1994:
Exchange through the Strait of Gibraltar. Prog.
Oceanogr. 33, 201–248. [5.7]
Bryden, H. L., M. J. Griffiths, A. M. Lavin,
R. C. Maillard, G. Parilla and W. M. Smethie,
1996: Decadal changes in water mass characteristics at 24°N in the Subtropical North Atlantic
Ocean. J. Climate 9, 3162– 3086. [7.3, 7.4]
Bryson, A. E., Jr. and Y.-C. Ho, 1975: Applied
Optimal Control. Hemisphere, NY (revised), 481
pp. [7.1]
Bu, X. and M. Warner, 1995: Solubility of chlorofluorocarbon 113 in water and seawater. DeepSea Res. 42, 1151–1161. [5.8]
Bullister, J. L., 1989: Chlorofluorocarbons as time
dependent tracers in the Ocean. Ocean. Mag.
2, 12–17. [5.8]
Bullister, J. L. and D. P. Wisegarver, 1998: The solubility of carbon tetrachloride in water and seawater. Deep-Sea Res. 45, 1285–1302. [5.8]
REFERENCES
610