Topography and the dynamical response to easterly flow in Southern Hemisphere subtropical West Coast regions

Author:

Reason C. J. C.

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Reference25 articles.

1. Anh, N. N., Gill, A. E., 1981: Generation of coastal lows by synoptic-scale waves.Quart. J. Roy. Meteor. Soc. 107, 521?530.

2. Bannon, P. R. 1981: Synoptic-scale forcing of coastal lows. Forced double Kelvin waves in the atmosphere.Quart. J. Roy. Meteor. Soc.,107, 313?327.

3. Church, J. A., Cresswell, G. R., Godfrey, J. S., 1989: The Leeuwin Current. In: Neshyba, S. J., Mooers, C. N. K., Smith, R. L., Barber, R. T., (eds.)Poleward Flows along Eastern Ocean Boundaries. New York: Springer, pp. 230?252.

4. Cosijn, C., 1996: Stable discontinuities in the atmosphere ever southern Africa.South African J. Sci., (in press).

5. Fandry, C. B., Leslie, L. M. 1984: A two-layer quasigeostrophic model of summer trough formation in the Australian subtropical easterlies.J. Atmos. Sci.,41, 807?818.

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