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Tellus Volume 25, 1973 - Issue 5
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Shorter Contribution

The effect on ocean circulation of a change in the sign of ?

K. H. BrinkDepartment of Geology and Geophysics, Yale University, New Haven, Conn. USA
,
G. VeronisDepartment of Geology and Geophysics, Yale University, New Haven, Conn. USA
&
C. C. YangDepartment of Geology and Geophysics, Yale University, New Haven, Conn. USA
Pages 518-521 | Received 26 Mar 1973, Published online: 15 Dec 2016

References

  • Fandry, C. B. and Leslie, L. M. 1972. A note on the effect of latitudinally varying bottom topography on the wind-driven ocean circulation. Tellus 24, 164–167.
  • Johnson, J. A., Fandry, C. B. and Leslie, L. M. 1971. On the variations of ocean circulation produced by bottom topography. Part 1. Tellus 23, 113–122.
  • Kamenkovich, V. M. and Mitrofanov, V. A. 1971. On a case of bottom reflief influence on currents in the ocean. (In Russian.) Dokla,dy, Akademia NA UK, 8SSR 199, 78-81.
  • Kuo, H. H. and Veronis, G.. 1971. The source-sink flow in a rotating system and its oceanic analogy. J. Fluid Mech. 45, 441-464.
  • Stommel, H.. 1948. The western intensification of wind-driven ocean currents. Trans. Am. Geoph. Union 29, 202-206.
  • Stommel, H., Arons, A. B. and Faller, A. J. 1958. Some examples of stationary planetary flows. Tellus 10, 179–187.
  • Welander, P. 1968. Wind-driven circulation in one-and two-layer oceans of variable depth. Tellus 20, 1–15.

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