Summary
The Adélie Land coastal section of East Antarctica is known for strong katabatic winds. Although the primary forcing of these persistent drainage flows has been attributed to the radiative cooling of the sloping ice topography, effects of ambient horizontal pressure gradients can play a central role in shaping the Antarctic surface wind regime as well. Oberrvations of the katabatic wind at the near-coastal Adélie Land station D-10 have been sorted into strong and weak wind classes. Concurrent radiosonde ascents at nearby Dumont D'Urville have been used to depict the timeaveraged large scale conditions accompanying the katabatic wind classes. Results suggest that strong katabatic wind cases are associated with low pressure over the coastal margin and easterly upper level motions. Numerical simulations have been conducted to examine the effect of prescribed large scale forcing on the evolution of the katabatic wind. The model runs indicate that the ambient environment plays a key role in the development and intensity of the katabatic wind regime.
Similar content being viewed by others
References
Anthes, R. A., Warner, T. T., 1978: The development of hydrodynamical models suitable for air pollution and other mesometeorological studies.Mon. Wea. Rev.,106, 1045–1078.
Ball, F. K., 1960: Winds on the ice slopes of Antarctica.Antarctic Meteorology, Proceedings of the Symposium in Melbourne, 1959. New York: Pergamon, pp. 9–16.
Bromwich, D. H., 1989: An extraordinary katabatic wind regime at Terra Nova Bay, Antarctica.Mon. Wea. Rev.,117, 688–695.
Drewry, D. J., 1983: The surface of the Antarctic ice sheet. In: Drewry, D. J. (ed.)Antarctica: Glaciological and Geophysical Folio, sheet 2. Cambridge: Scott Polar Research Institute.
Egger, J., 1985: Slope winds and the axisymmetric circulation over Antarctica.J. Atmos. Sci.,42, 1859–1867.
Egger, J., 1992: Topographic wave modification and the angular momentum balance of the Antarctic troposphere.J. Atmos. Sci.,49, 327–334.
James, I. N., 1989: The Antarctic drainage flow: Implications for hemispheric flow on the Southern Hemisphere.Antarct. Sci.,1, 279–290.
Kidson, E., 1946: Discussion of observations at Adélie Land, Queen Mary Land, and Macquarie Island. Austr. Ant. Exp. 1911–1914. Scient. Rep. Ser. B, vol. 6.
Kodama, Y., Wendler, G., Ishikawa, N., 1989: On the diurnal variation of the boundary layer in summer in Adélie Land, Eastern Antarctica.J. Appl. Meteor.,28, 16–24.
Loewe, F., 1974: Considerations concerning the winds of Adélie Land.Z. Gletscherkd. Glazialgeol.,10, 189–197.
Parish, T. R., 1982: Surface airflow over East Antarctica.Mon. Wea. Rev.,110, 84–90.
Parish, T. R., 1992: On the role of Antarctic katabatic winds in forcing large-scale tropospheric motions.J. Atmos. Sci.,49, 1374–1385.
Parish, T. R., Waight, K. T., 1987: The forcing of Antarctic katabatic winds.Mon. Wea. Rev.,115, 2214–2226.
Périard, C., Pettré, P., 1991: Climatology of Dumont D'Urville, Adélie Land, Antarctica. Centre National de Recherches Météorologiques, Toulouse, 19 pp.
Schwerdtfeger, W., 1984:Weather and Climate of the Antarctic. New York: Elsevier Science Publishers, 261 pp.
Schwerdtfeger, W., 1967: Annual and semi-annual changes of atmospheric mass over Antarctica.J. Geophys. Res.,72, 3543–3547.
Tauber, G. M., 1960: Characteristics of Antarctic katabatic winds.Antarctic Meteorology, Proceedings of the Symposium in Melbourne, 1959. New York: Pergamon, pp. 52–64.
Wendler, G., Ishikawa, N., Kodama, Y., 1988. On the heat balance of the icy slope of Adélie Land, Eastern Antarctica.J. Appl. Meteor.,27, 52–65.
Author information
Authors and Affiliations
Additional information
With 7 Figures
Rights and permissions
About this article
Cite this article
Parish, T.R., Pettré, P. & Wendler, G. The influence of large-scale forcing on the katabatic wind regime at Adélie Land, Antarctica. Meteorl. Atmos. Phys. 51, 165–176 (1993). https://doi.org/10.1007/BF01030492
Received:
Revised:
Issue Date:
DOI: https://doi.org/10.1007/BF01030492