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Original Articles

On the variation of ocean circulation produced by bottom topography

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Pages 113-121 | Received 30 Jun 1970, Published online: 15 Dec 2016

References

  • Barrett, J. R. 1965. Subsurface currents off Cape Hatteras. Deep Sea Res. 12, 173–184.
  • Clarke, R. A. & Fofonoff, N. P. 1969. Oceanic flow over varying bottom topography. J. Mar. Res. 27,226–240.
  • Holland, W. R. 1967. On the wind-driven circula-tion in an ocean with bottom topography. Tellus 19, 582–600.
  • Hsueh, Y. 1969. Bottom topography and variable wind stress. J. Geophys. Res. 72, 4101–4107.
  • Johnson, J. A. 1968. A three dimensional model of the wind driven ocean circulation. J. Fluid Mech. 34, 721–734.
  • Lighthill, M. J. 1966. Dynamics of rotating fluids: a survey. J. Fluid Mech. 26, 411–431.
  • Pedlosky, J. 1965. A note on the western intensi-fication of the oceanic circulation. J. Mar. Res. 23, 207–209.
  • Pedlosky, J. 1968. An overlooked aspect of the wind-driven oceanic circulation. J. Fluid Mech. 32, 809–821.
  • Stommel, H. 1958. The Gulf Stream. University of California Press.
  • Veronis, G. 1966. Rossby waves with bottom topography. J. Mar. Rea. 24, 338–349.
  • Warren, B. A. 1963. Topographic influences on the path of the Gulf Stream. Tellus 15, 167–183.
  • Welander, P. 1968. Wind-driven circulation in one and two layer oceans of variable depth. Tellus 20, 1–16.