Analyzer for Total Carbon Dioxide with
Coulometric Detection. DOE Research Summary.
No. 19, Carbon Dioxide Information Analysis
Center, Oak Ridge National Laboratory, Oak
Ridge, TN, 4 pp. [6.3]
Johnson, K. M., A. E. King and J. M. Sieburth, 1985:
Coulometric TCO 2 analysis for marine studies: An
Introduction. Mar. Chem., 16, 61–82. [6.3]
Johnson, K. M., J. M. Sieburth, J. M. Williams and
L. Brandstrom, 1987: Coulometric total carbon
dioxide analysis for marine studies: automation
and calibration. Mar. Chem. 21, 117–133. [6.3]
Johnson, K. M., K. D. Wills, D. B. Butler, W. K.
Johnson and C. S. Wong, 1993: Coulometric total
carbon dioxide analysis for marine studies:
maximizing the performance of an automated gasextraction system and coulometric detector. Mar.
Chem. 44, 167–188. [6.3]
Johnson, K. M., A. Dickson, G. Eischeid et. al.,
1998b: Coulometric total carbon dioxide analysis
for marine studies: assessment of the quality of
total inorganic carbon measurements made during
the US Indian Ocean CO 2 Survey 1994–1996.
Mar. Chem. 63, 21–37. [6.3]
Johnson, R. E., 1973: Antarctic Intermediate Water
in the South Pacific Ocean. In: Oceanography of
the South Pacific Ocean 1972, R. Frazer (compiler) New Zealand National Commission for
UNESCO, pp. 55–69. [4.4]
Johnson, T. J., R. H. Stewart, C. K. Shum and
B. D. Tapley, 1992: Distribution of Reynolds
stress carried by mesoscale variability in the
Antarctic Circumpolar Current. Geophys. Res.
Lett. 19, 1201–1204. [3.3]
Jones, A., D. L. Roberts and M. -J. Woodage, 1999a:
The Indirect Effects of Anthropogenic Sulphate
Aerosol Simulated Using a Climate Model with
an Interactive Sulphur Cycle. Hadley Centre
Technical Note No. 14, Meteorological Office,
Bracknell, UK. [2.3]
Jones, C., P. Peterson and C. Gautier, 1999b: A new
method for deriving ocean surface specific humidity
and air temperature: An artificial neural network
approach. J. Appl. Meteor. 38, 1229–1246. [3.4]
Jones, E. P., L. G. Anderson and J. H. Swift, 1998:
Distribution of Atlantic and Pacific waters in the
upper Arctic Ocean: Implications for circulation.
Geophys. Res. Lett. 25, 769–772. [4.7]
Jones, G. A., A. R. Gagnon, R. J. Schneider,
K. F. von Reden and A. P. McNichol, 1994: Highprecision AMS radiocarbon measurements of
central Arctic Ocean seawaters. Nuclear Instr. and
Methods, B92, 426–430. [5.8]
Jones, H. and J. Marshall, 1993: Convection with
rotation in a neutral ocean: a study of open-ocean
convection. J. Phys. Oceanogr. 23, 1009–1039.
[5.5]
Jones, H. and J. Marshall, 1997: Restratification
after deep convection. J. Phys. Oceanogr. 27,
2276–2287. [5.5]
Jones, P. D., T. Jonsson and D. Wheeler, 1997:
Extension of the North Atlantic Oscillation using
early instrumental pressure observations from
Gibraltar and south-west Iceland. Int. J. Climatol
17, 1433–1450. [7.3]
Jones, W. L., F. J. Wentz and L. C. Schroeder, 1978:
Algorithm for inferring wind stress from SEASATA. Spacecraft and Rockets, 15, 368–374. [3.4]
Jónsson, S., 1991: Seasonal and interannual variability of wind stress curl over the Nordic Seas.
J. Geophys. Res. 96, 2649–2659. [7.3]
Josey, S. A., E. C. Kent, D. Oakley and P. K. Taylor,
1996: A new global air–sea heat and momentum
flux climatology. International WOCE Newsletter,
No. 24, 3–5, WOCE International Project Office
(unpublished document). [6.2]
Josey, S. A., R. Pascal and P. Taylor, 1997: Air–sea
interaction studies in the Mediterranean Sea. In:
Abstracts Volume of the International Conference,
Progress in Oceanography of the Mediterranean
Sea, Rome, 17–19 November, 1997, 253 pp.
[5.7]
Josey, S. A., E. C. Kent and P. K. Taylor, 1998:
The Southampton Oceanography Centre (SOC)
Ocean–Atmosphere Heat, Momentum and
Freshwater Flux Atlas. Southampton Oceanography Centre, Report 6, 30 pp ;Figs. [5.1]
Josey, S. A., E. C. Kent and P. K. Taylor, 1999: New
insights into the ocean heat budget closure
problem from analysis of the SOC air–sea flux
climatology. J. Climate 12, 2856–2880. [1.2, 5.1,
6.1, 7.1]
Josey, S. A., E. C. Kent and P. K. Taylor, 2000: On
the wind stress forcing of the ocean in the SOC
and Hellerman and Rosenstein climatologies.
J. Phys. Oceanogr. (submitted). [1.2]
Jourdan, D. and C. Gautier, 1994: Comparison
between global latent heat flux computed from
multi-sensor (SSM/I and AVHRR) and from in-situ
data. J. Atmos. Oceanic Technol. 12, 46–72. [3.4]
Jourdan, D., P. Peterson and C. Gautier, 1997:
Oceanic freshwater budget and transport as
derived from satellite radiometric data. J. Phys.
Oceanogr. 27, 457–467. [6.2]
Joyce, T. M., 1977: A note on the lateral mixing of
water masses. J. Phys. Oceanogr. 7, 626–629.
[5.2]
Joyce, T. M., 1988: Wind-driven cross-equatorial
flow in the Pacific Ocean. J. Phys. Oceanogr. 18,
19–24. [4.3]
REFERENCES
634
Coulometric Detection. DOE Research Summary.
No. 19, Carbon Dioxide Information Analysis
Center, Oak Ridge National Laboratory, Oak
Ridge, TN, 4 pp. [6.3]
Johnson, K. M., A. E. King and J. M. Sieburth, 1985:
Coulometric TCO 2 analysis for marine studies: An
Introduction. Mar. Chem., 16, 61–82. [6.3]
Johnson, K. M., J. M. Sieburth, J. M. Williams and
L. Brandstrom, 1987: Coulometric total carbon
dioxide analysis for marine studies: automation
and calibration. Mar. Chem. 21, 117–133. [6.3]
Johnson, K. M., K. D. Wills, D. B. Butler, W. K.
Johnson and C. S. Wong, 1993: Coulometric total
carbon dioxide analysis for marine studies:
maximizing the performance of an automated gasextraction system and coulometric detector. Mar.
Chem. 44, 167–188. [6.3]
Johnson, K. M., A. Dickson, G. Eischeid et. al.,
1998b: Coulometric total carbon dioxide analysis
for marine studies: assessment of the quality of
total inorganic carbon measurements made during
the US Indian Ocean CO 2 Survey 1994–1996.
Mar. Chem. 63, 21–37. [6.3]
Johnson, R. E., 1973: Antarctic Intermediate Water
in the South Pacific Ocean. In: Oceanography of
the South Pacific Ocean 1972, R. Frazer (compiler) New Zealand National Commission for
UNESCO, pp. 55–69. [4.4]
Johnson, T. J., R. H. Stewart, C. K. Shum and
B. D. Tapley, 1992: Distribution of Reynolds
stress carried by mesoscale variability in the
Antarctic Circumpolar Current. Geophys. Res.
Lett. 19, 1201–1204. [3.3]
Jones, A., D. L. Roberts and M. -J. Woodage, 1999a:
The Indirect Effects of Anthropogenic Sulphate
Aerosol Simulated Using a Climate Model with
an Interactive Sulphur Cycle. Hadley Centre
Technical Note No. 14, Meteorological Office,
Bracknell, UK. [2.3]
Jones, C., P. Peterson and C. Gautier, 1999b: A new
method for deriving ocean surface specific humidity
and air temperature: An artificial neural network
approach. J. Appl. Meteor. 38, 1229–1246. [3.4]
Jones, E. P., L. G. Anderson and J. H. Swift, 1998:
Distribution of Atlantic and Pacific waters in the
upper Arctic Ocean: Implications for circulation.
Geophys. Res. Lett. 25, 769–772. [4.7]
Jones, G. A., A. R. Gagnon, R. J. Schneider,
K. F. von Reden and A. P. McNichol, 1994: Highprecision AMS radiocarbon measurements of
central Arctic Ocean seawaters. Nuclear Instr. and
Methods, B92, 426–430. [5.8]
Jones, H. and J. Marshall, 1993: Convection with
rotation in a neutral ocean: a study of open-ocean
convection. J. Phys. Oceanogr. 23, 1009–1039.
[5.5]
Jones, H. and J. Marshall, 1997: Restratification
after deep convection. J. Phys. Oceanogr. 27,
2276–2287. [5.5]
Jones, P. D., T. Jonsson and D. Wheeler, 1997:
Extension of the North Atlantic Oscillation using
early instrumental pressure observations from
Gibraltar and south-west Iceland. Int. J. Climatol
17, 1433–1450. [7.3]
Jones, W. L., F. J. Wentz and L. C. Schroeder, 1978:
Algorithm for inferring wind stress from SEASATA. Spacecraft and Rockets, 15, 368–374. [3.4]
Jónsson, S., 1991: Seasonal and interannual variability of wind stress curl over the Nordic Seas.
J. Geophys. Res. 96, 2649–2659. [7.3]
Josey, S. A., E. C. Kent, D. Oakley and P. K. Taylor,
1996: A new global air–sea heat and momentum
flux climatology. International WOCE Newsletter,
No. 24, 3–5, WOCE International Project Office
(unpublished document). [6.2]
Josey, S. A., R. Pascal and P. Taylor, 1997: Air–sea
interaction studies in the Mediterranean Sea. In:
Abstracts Volume of the International Conference,
Progress in Oceanography of the Mediterranean
Sea, Rome, 17–19 November, 1997, 253 pp.
[5.7]
Josey, S. A., E. C. Kent and P. K. Taylor, 1998:
The Southampton Oceanography Centre (SOC)
Ocean–Atmosphere Heat, Momentum and
Freshwater Flux Atlas. Southampton Oceanography Centre, Report 6, 30 pp ;Figs. [5.1]
Josey, S. A., E. C. Kent and P. K. Taylor, 1999: New
insights into the ocean heat budget closure
problem from analysis of the SOC air–sea flux
climatology. J. Climate 12, 2856–2880. [1.2, 5.1,
6.1, 7.1]
Josey, S. A., E. C. Kent and P. K. Taylor, 2000: On
the wind stress forcing of the ocean in the SOC
and Hellerman and Rosenstein climatologies.
J. Phys. Oceanogr. (submitted). [1.2]
Jourdan, D. and C. Gautier, 1994: Comparison
between global latent heat flux computed from
multi-sensor (SSM/I and AVHRR) and from in-situ
data. J. Atmos. Oceanic Technol. 12, 46–72. [3.4]
Jourdan, D., P. Peterson and C. Gautier, 1997:
Oceanic freshwater budget and transport as
derived from satellite radiometric data. J. Phys.
Oceanogr. 27, 457–467. [6.2]
Joyce, T. M., 1977: A note on the lateral mixing of
water masses. J. Phys. Oceanogr. 7, 626–629.
[5.2]
Joyce, T. M., 1988: Wind-driven cross-equatorial
flow in the Pacific Ocean. J. Phys. Oceanogr. 18,
19–24. [4.3]
REFERENCES
634