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Tellus A: Dynamic Meteorology and Oceanography Volume 36, 1984 - Issue 2
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Original Articles

The delicate interplay between wind-stress and buoyancy input in ocean circulation: the Goldsbrough variationsFootnote*

Henry StommelWoods Hole Oceanographic Institution, Woods Hole, Massachusetts02543. USA.
Pages 111-119 | Published online: 15 Dec 2016

References

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  • Blandford, R. 1965. inertial flow in the Gulf Stream. Tellus 17, 69–76.
  • Chantey, J. G. and Eliassen, A. 1949. A numerical method for predicting the perturbation of the middle latitude westerlies. Tellus 1 (2), 38–54.
  • Ekman, V. W. 1905. On the influence of the earth's rotation on ocean-currents. Arkiv f Matem., Astr. o. Fystk (Stockholm), Bd. 2, No. 11, 53 pp.
  • Ekman, V. W. 1923. Ober Horizontalzirkulation bei winderzeugten Meeresstromungen. Arktv f. Matem., Asir. o. Fystk (Stockholm), Bd. 17, No. 26, 74 pp.
  • Goldsbrough, G. R. 1933. Ocean currents produced by evaporation and precipitation. Proc. Roy. Soc. London A 141 512–517.
  • Goldsbrough, G. R. 1934. On ocean currents produced by winds. Proc. Roy. Soc. London A 148, 47–58.
  • Luyten, J., Pedlosky, J. and Stommel, H. 1983. The ventilated thennocline. J. Phys. Oceanogr. 13, 292–309.
  • Luyten, J. and Stommel, H. 1983. upstream effects of the Gulf Stream on the structure of the mid-ocean thenno-cline. Prog. Oceanogr. in press.
  • Rhines, P. B. and Young, W. R. 1982. A theory of the wind-driven circulation. I. Mid-ocean gyres. J. Mar. Res. Supplement to 40, 559–596.
  • Robinson, A. and Stommel, H. 1959. The oceanic thermocline and the associated thennohaline circu-lation. Tellus II, 295–308.
  • Rossby, V. G. and Collaborators, 1939. Relation between variations in the intensity of the zonal circulation of the atmosphere and the displacements of the semi-permanent centers of action. J. Mar. Res. 2, 38–55.
  • Stommel, H. 1948. The westward intensification of wind-driven ocean currents. Trans. Amer.Geophys. Union 29 (2), 202–206.
  • Stommel, H. and Schott, F. 1977. The beta-spiral and the determination of absolute velocity field from hydrographic station data. Deep-Sea Res. 24, 325–329.
  • Sverdrup, H. U. 1947. Wind-driven currents in a baroclinic ocean; with application to the equatorial currents of the eastern Pacific. Proc. Natl. Acad. Sci., Wash. 33, 318–326.
  • Welander, P. 1959. An advective model of the ocean thennocline. Tellus 11, 309–318.
  • Weller, R. A. 1981. Observations of the velocity response to wind forcing in the upper ocean. J. Geophys. Res. 86 (C3), 1969–1977.

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