152
Joseph Pedlosky
Gill, A. E., 1985. An explicit solution of the linear thermocline equations. Tellus 37A, 276–285.
Holland, W. R., and P. B. Rhines, 1980. An example of eddy-induced circulation. J. Phys. Oceanogr. 10,
1010–1031.
Huang, R. X., 1988. On boundary value problems of the ideal-fluid thermocline . J. Phys. Oeanogr. 18,
619–641.
Huang, R. X., 1989. On the three dimensional structure of the wind-driven circulation in the North Atlantic.
Dyn. Atmos. Oceans 15, 117–159.
Iselin, C. O’D., 1936. A study of the circulation of the western North Atlantic. Papers in Physical Oceanography and Meteorology. Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, Vol. IV, 101 pp.
Iselin, C. O’D., 1939. The influence of vertical and lateral turbulence on the characteristics of the waters
at mid-depths. Trans. Am. Geophys. Union 20, 414–417.
Ledwell, J. A., J. Watson, and C. S. Law, 1993. Evidence for slow mixing across the pycnocline from an
open-ocean tracer release experiment. Nature 364, 701–703.
Luyten J. R., J. Pedlosky, and H. Stommel, 1983. The ventilated thermocline. J. Phys. Oceanogr. 13,
292–309.
Montgomery, R. B., 1938. Circulation in upper layers of southern North Atlantic deduced with use of
isentropic analysis. Papers in Physical Oceanography and Meteorology. Massachusetts Institute of
Technology and Woods Hole Oceanographic Institution, Vol. VI, 55 pp.
Needler, G. T., 1967. A model for the thermohaline circulation in an ocean of finite depth. J. Mar. Res. 25,
329–342.
Pedlosky, J., 1969. Linear theory of the circulation in a stratified ocean. J. Fluid Mech. 35, 185–205.
Pedlosky, J., 1987. An inertial model of the equatorial undercurrent. J. Phys. Oecanogr. 17, 1978–1985.
Pedlosky, J., and P. Robbins, 1991. The role of finite mixed-layer thickness in the structure of the ventilated
thermocline. J. Phys. Oceanogr. 21, 1018–1031.
Pedlosky, J., and W. R. Young, 1983. Ventilation, potential vorticity homogenization and structure of the
ocean circulation. J. Phys. Oceanogr.13, 2020–2037.
Radko, T., and J. Marshall, 2005. The leaky thermocline. J. Phys. Oceanogr. 34, 1648–1662.
Rhines, P. B., and W. R. Young, 1982a. A theory of the wind-driven circulation. I. Mid-ocean gyres.
J. Mar. Res. 40 (Suppl.), 559–596.
Rhines, P. B., and W. R. Young, 1982b. Homogenization of potential vorticity in planetary gyres. J. Fluid
Mech. 122, 347–367.
Robinson, A., and H. Stommel, 1959. The oceanic thermocline and the associated thermohaline circulation.
Tellus XI, 295–308.
Rossby, C. G., 1937. Isentropic analysis. Bull. Am. Meteorol. Soc. 18, 201–209.
Salmon, R., 1990. The thermocline as an “internal boundary layer”. J. Marine Res. 48, 437–469.
Samelson, R. M., and G. K. Vallis, 1997. Large scale circulation with small diapycnal diffusion: The
two-thermocline limit. J. Marine Res. 55, 223–275.
Stommel, H., 1958. The abyssal circulation. Deep-Sea Res. 5, 80–82.
Stommel, H., and G. Veronis, 1957. Steady convective motion in a horizontal layer of fluid heated uniformly
from above and cooled non-uniformly from below. Tellus IX, 401–407.
Sverdrup, H. U., M. W. Johnson, and R. H. Fleming, 1942 The Oceans: Their Physics, Chemistry and
General Biology. Prentice–Hall, Englewood Cliffs, NJ, 1077 pp.
Veronis, G., 1969. On theoretical models of the thermohaline circulation. Deep Sea Res. (Suppl.) 16,
301–323.
Welander, P., 1959. An advective model of the ocean thermocline. Tellus XI, 309–318.
Welander, P., 1971a. Some exact solutions to the equations describing an ideal-fluid thermocline. J. Mar.
Res. 29, 60–68.
Welander, P., 1971b. The thermocline problem. Philos. Trans. R. Soc. London Ser. A 270, 415–421.
Joseph Pedlosky
Gill, A. E., 1985. An explicit solution of the linear thermocline equations. Tellus 37A, 276–285.
Holland, W. R., and P. B. Rhines, 1980. An example of eddy-induced circulation. J. Phys. Oceanogr. 10,
1010–1031.
Huang, R. X., 1988. On boundary value problems of the ideal-fluid thermocline . J. Phys. Oeanogr. 18,
619–641.
Huang, R. X., 1989. On the three dimensional structure of the wind-driven circulation in the North Atlantic.
Dyn. Atmos. Oceans 15, 117–159.
Iselin, C. O’D., 1936. A study of the circulation of the western North Atlantic. Papers in Physical Oceanography and Meteorology. Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, Vol. IV, 101 pp.
Iselin, C. O’D., 1939. The influence of vertical and lateral turbulence on the characteristics of the waters
at mid-depths. Trans. Am. Geophys. Union 20, 414–417.
Ledwell, J. A., J. Watson, and C. S. Law, 1993. Evidence for slow mixing across the pycnocline from an
open-ocean tracer release experiment. Nature 364, 701–703.
Luyten J. R., J. Pedlosky, and H. Stommel, 1983. The ventilated thermocline. J. Phys. Oceanogr. 13,
292–309.
Montgomery, R. B., 1938. Circulation in upper layers of southern North Atlantic deduced with use of
isentropic analysis. Papers in Physical Oceanography and Meteorology. Massachusetts Institute of
Technology and Woods Hole Oceanographic Institution, Vol. VI, 55 pp.
Needler, G. T., 1967. A model for the thermohaline circulation in an ocean of finite depth. J. Mar. Res. 25,
329–342.
Pedlosky, J., 1969. Linear theory of the circulation in a stratified ocean. J. Fluid Mech. 35, 185–205.
Pedlosky, J., 1987. An inertial model of the equatorial undercurrent. J. Phys. Oecanogr. 17, 1978–1985.
Pedlosky, J., and P. Robbins, 1991. The role of finite mixed-layer thickness in the structure of the ventilated
thermocline. J. Phys. Oceanogr. 21, 1018–1031.
Pedlosky, J., and W. R. Young, 1983. Ventilation, potential vorticity homogenization and structure of the
ocean circulation. J. Phys. Oceanogr.13, 2020–2037.
Radko, T., and J. Marshall, 2005. The leaky thermocline. J. Phys. Oceanogr. 34, 1648–1662.
Rhines, P. B., and W. R. Young, 1982a. A theory of the wind-driven circulation. I. Mid-ocean gyres.
J. Mar. Res. 40 (Suppl.), 559–596.
Rhines, P. B., and W. R. Young, 1982b. Homogenization of potential vorticity in planetary gyres. J. Fluid
Mech. 122, 347–367.
Robinson, A., and H. Stommel, 1959. The oceanic thermocline and the associated thermohaline circulation.
Tellus XI, 295–308.
Rossby, C. G., 1937. Isentropic analysis. Bull. Am. Meteorol. Soc. 18, 201–209.
Salmon, R., 1990. The thermocline as an “internal boundary layer”. J. Marine Res. 48, 437–469.
Samelson, R. M., and G. K. Vallis, 1997. Large scale circulation with small diapycnal diffusion: The
two-thermocline limit. J. Marine Res. 55, 223–275.
Stommel, H., 1958. The abyssal circulation. Deep-Sea Res. 5, 80–82.
Stommel, H., and G. Veronis, 1957. Steady convective motion in a horizontal layer of fluid heated uniformly
from above and cooled non-uniformly from below. Tellus IX, 401–407.
Sverdrup, H. U., M. W. Johnson, and R. H. Fleming, 1942 The Oceans: Their Physics, Chemistry and
General Biology. Prentice–Hall, Englewood Cliffs, NJ, 1077 pp.
Veronis, G., 1969. On theoretical models of the thermohaline circulation. Deep Sea Res. (Suppl.) 16,
301–323.
Welander, P., 1959. An advective model of the ocean thermocline. Tellus XI, 309–318.
Welander, P., 1971a. Some exact solutions to the equations describing an ideal-fluid thermocline. J. Mar.
Res. 29, 60–68.
Welander, P., 1971b. The thermocline problem. Philos. Trans. R. Soc. London Ser. A 270, 415–421.