Vanmarcke, E., 1983: Random Fields: Analysis and
Synthesis. MIT Press, Cambridge, MA, 382 pp.
[2.1]
Verduin, J. and D. Quadfasel, 2000: Long-term
temperature and salinity trends in the central
Greenland Sea. In: European Sub-Polar
Ocean Programme, Scientific Report, E. Jansen
(ed.). [7.3]
Veronis, G., 1975: The role of models in tracer studies. In: Numerical Models of Ocean Circulation,
R. O. Reid (ed.), National Academy of Science,
Washington, DC, pp. 133–146. [5.2]
Veronis, G., 1981: Dynamics of large-scale ocean circulation. In: Evolution of Physical Oceanography,
B. A. Warren and C. Wunsch (eds), MIT Press,
Cambridge, MA, pp. 140–183. [4.2]
Verschell, M., J. Kindle and J. O’Brien, 1995: Effects
of Indo-Pacific throughflow on the upper tropical
Pacific and Indian Oceans. J. Geophys. Res. 100,
18409–18420. [4.7]
Verschell, M. A., M. A. Bourassa, D. E. Weissman
and J. J. O’Brien, 1999: Ocean model validation of
the NASA scatterometer winds. J. Geophys. Res.
104, 11359–11373. [3.4]
Vialard, J. and P. Delecluse, 1998a: An OGCM study
for the TOGA decade. Part I: Role of salinity in
the physics of the Western Pacific Fresh Pool.
J. Phys. Oceanogr. 28, 1071–1106. [4.3]
Vialard, J. and P. Delecluse, 1998b: An OGCM
study for the TOGA decade. Part I: Barrier-layer
formation and variability. J. Phys. Oceanogr. 28,
1071–1106. [4.3]
Vinje, T., N. Nordlund and A. Kvambekk, 1998:
Monitoring ice thickness in Fram Strait. J.
Geophys. Res. 103, 10437–10450. [1.2, 7.3]
Visbeck, M. and M. Rhein, 2000: Is bottom boundary layer mixing slowly ventilating Greenland Sea
Deep Water? J. Phys. Oceanogr. 30, 215–224.
[7.3]
Visbeck, M. and F. Schott, 1992: Analysis of seasonal current variations in the western Equatorial
Indian Ocean: Direct measurements and GFDL
model comparison. J. Phys. Oceanogr. 22, 1112–
1128. [4.3]
Visbeck, M., J. Marshall, T. Haine and M. Spall,
1997: Specification of eddy transfer coefficients
in coarse-resolution ocean circulation models.
J. Phys. Oceanogr. 27, 381–402. [2.2, 2.3, 4.6]
Visser, P. N . A . M., K. F. Wakker and B. A . C.
Ambrosius, 1993: Dynamic Sea Surface Topography from GEOSAT Altimetry. Mar. Geod. 16(3),
215–239. [3.3]
Viudez, A., 2000: Volume and mass transport across
isosurfaces of a balanced fluid property. J. Phys.
Oceanogr. 30, 1478–1485. [5.1]
Vivier, F., K. A. Kelly and L. Thompson, 1999:
Contributions of wind forcing, waves, and surface
heating to sea-surface height observations in the
Pacific Ocean. J. Geophys. Res. 104, 20767–
20788. [3.3]
Völker, C., 1999: Momentum balance in zonal flows
and resonance of baroclinic Rossby waves.
J. Phys. Oceanogr. 29, 1666–1681. [4.6]
von Reden, K. F., R. J. Schneider, G. J. Cohen and
G. A. Jones, 1994: Performance characteristics of
the 3MV Tandetron AMS system at the National
Ocean Sciences AMS Facility. Nuclear Instr. and
Methods B92, 7–11. [5.8]
Voss, R., R. Sausen and U. Cubasch, 1998:
Periodically synchronously coupled integrations
with the atmosphere–ocean general circulation
model ECHAM3/LSG. Climate Dyn. 14,
249–266. [2.3]
Vossepoel, F. C., R. W. Reynolds and L. Miller,
1999: Use of sea level observations to estimate
salinity variability in the tropical Pacific. J. Atmos.
Oceanic Technol. 16, 1401–1415. [7.4]
Wacongne, S., 1990: On the difference in strength
between Atlantic and Pacific undercurrents.
J. Phys. Oceanogr. 20, 792–799. [4.3]
Wacongne, S. and R. Pacanowski, 1996: Seasonal
heat transport in a primitive equation model of
the Indian Ocean. J. Phys. Oceanogr. 26,
2666–2699. [4.3, 6.1]
Wadley, M. R. and G. R. Bigg, 1996: Abyssal channel
flow in ocean general circulation models with
application to the Vema Channel. J. Phys.
Oceanogr. 26, 38–48. [2.3]
Wagner, C. A. and R. E. Cheney, 1992: Global sea
level change from satellite altimetry. J. Geophys.
Res. 97, 15607–15616. [3.3]
Wagner, D., E. Ruprecht and C. Simmer, 1990: A
combination of microwave observations from
satellite and an EOF analysis to retrieve vertical
humidity profiles over the ocean. J. Appl. Meteor.
29, 1142–1157. [3.4]
Wahr, J., M. Molenaar and F. Bryan, 1998: Time
variability of the Earth’s gravity field: hydrological
and oceanic effects and their possible detection
using GRACE. J. Geophys. Res. 103, 30205–
30229. [3.3]
Wajsowicz, R. C., 1996: Flow of a western boundary current through multiple straits: An electrical
circuit analogy for the Indonesian throughflow
and archipelago. J. Geophys. Res. 101, 12295–
12300. [4.7]
Wajsowicz, R. C., 1999: Variations in gyre closure at
the water mass crossroads of the western equatorial Pacific Ocean. J. Phys. Oceanogr. 29, 3001–
3024. [4.7]
REFERENCES
676
Synthesis. MIT Press, Cambridge, MA, 382 pp.
[2.1]
Verduin, J. and D. Quadfasel, 2000: Long-term
temperature and salinity trends in the central
Greenland Sea. In: European Sub-Polar
Ocean Programme, Scientific Report, E. Jansen
(ed.). [7.3]
Veronis, G., 1975: The role of models in tracer studies. In: Numerical Models of Ocean Circulation,
R. O. Reid (ed.), National Academy of Science,
Washington, DC, pp. 133–146. [5.2]
Veronis, G., 1981: Dynamics of large-scale ocean circulation. In: Evolution of Physical Oceanography,
B. A. Warren and C. Wunsch (eds), MIT Press,
Cambridge, MA, pp. 140–183. [4.2]
Verschell, M., J. Kindle and J. O’Brien, 1995: Effects
of Indo-Pacific throughflow on the upper tropical
Pacific and Indian Oceans. J. Geophys. Res. 100,
18409–18420. [4.7]
Verschell, M. A., M. A. Bourassa, D. E. Weissman
and J. J. O’Brien, 1999: Ocean model validation of
the NASA scatterometer winds. J. Geophys. Res.
104, 11359–11373. [3.4]
Vialard, J. and P. Delecluse, 1998a: An OGCM study
for the TOGA decade. Part I: Role of salinity in
the physics of the Western Pacific Fresh Pool.
J. Phys. Oceanogr. 28, 1071–1106. [4.3]
Vialard, J. and P. Delecluse, 1998b: An OGCM
study for the TOGA decade. Part I: Barrier-layer
formation and variability. J. Phys. Oceanogr. 28,
1071–1106. [4.3]
Vinje, T., N. Nordlund and A. Kvambekk, 1998:
Monitoring ice thickness in Fram Strait. J.
Geophys. Res. 103, 10437–10450. [1.2, 7.3]
Visbeck, M. and M. Rhein, 2000: Is bottom boundary layer mixing slowly ventilating Greenland Sea
Deep Water? J. Phys. Oceanogr. 30, 215–224.
[7.3]
Visbeck, M. and F. Schott, 1992: Analysis of seasonal current variations in the western Equatorial
Indian Ocean: Direct measurements and GFDL
model comparison. J. Phys. Oceanogr. 22, 1112–
1128. [4.3]
Visbeck, M., J. Marshall, T. Haine and M. Spall,
1997: Specification of eddy transfer coefficients
in coarse-resolution ocean circulation models.
J. Phys. Oceanogr. 27, 381–402. [2.2, 2.3, 4.6]
Visser, P. N . A . M., K. F. Wakker and B. A . C.
Ambrosius, 1993: Dynamic Sea Surface Topography from GEOSAT Altimetry. Mar. Geod. 16(3),
215–239. [3.3]
Viudez, A., 2000: Volume and mass transport across
isosurfaces of a balanced fluid property. J. Phys.
Oceanogr. 30, 1478–1485. [5.1]
Vivier, F., K. A. Kelly and L. Thompson, 1999:
Contributions of wind forcing, waves, and surface
heating to sea-surface height observations in the
Pacific Ocean. J. Geophys. Res. 104, 20767–
20788. [3.3]
Völker, C., 1999: Momentum balance in zonal flows
and resonance of baroclinic Rossby waves.
J. Phys. Oceanogr. 29, 1666–1681. [4.6]
von Reden, K. F., R. J. Schneider, G. J. Cohen and
G. A. Jones, 1994: Performance characteristics of
the 3MV Tandetron AMS system at the National
Ocean Sciences AMS Facility. Nuclear Instr. and
Methods B92, 7–11. [5.8]
Voss, R., R. Sausen and U. Cubasch, 1998:
Periodically synchronously coupled integrations
with the atmosphere–ocean general circulation
model ECHAM3/LSG. Climate Dyn. 14,
249–266. [2.3]
Vossepoel, F. C., R. W. Reynolds and L. Miller,
1999: Use of sea level observations to estimate
salinity variability in the tropical Pacific. J. Atmos.
Oceanic Technol. 16, 1401–1415. [7.4]
Wacongne, S., 1990: On the difference in strength
between Atlantic and Pacific undercurrents.
J. Phys. Oceanogr. 20, 792–799. [4.3]
Wacongne, S. and R. Pacanowski, 1996: Seasonal
heat transport in a primitive equation model of
the Indian Ocean. J. Phys. Oceanogr. 26,
2666–2699. [4.3, 6.1]
Wadley, M. R. and G. R. Bigg, 1996: Abyssal channel
flow in ocean general circulation models with
application to the Vema Channel. J. Phys.
Oceanogr. 26, 38–48. [2.3]
Wagner, C. A. and R. E. Cheney, 1992: Global sea
level change from satellite altimetry. J. Geophys.
Res. 97, 15607–15616. [3.3]
Wagner, D., E. Ruprecht and C. Simmer, 1990: A
combination of microwave observations from
satellite and an EOF analysis to retrieve vertical
humidity profiles over the ocean. J. Appl. Meteor.
29, 1142–1157. [3.4]
Wahr, J., M. Molenaar and F. Bryan, 1998: Time
variability of the Earth’s gravity field: hydrological
and oceanic effects and their possible detection
using GRACE. J. Geophys. Res. 103, 30205–
30229. [3.3]
Wajsowicz, R. C., 1996: Flow of a western boundary current through multiple straits: An electrical
circuit analogy for the Indonesian throughflow
and archipelago. J. Geophys. Res. 101, 12295–
12300. [4.7]
Wajsowicz, R. C., 1999: Variations in gyre closure at
the water mass crossroads of the western equatorial Pacific Ocean. J. Phys. Oceanogr. 29, 3001–
3024. [4.7]
REFERENCES
676