Summary
A one dimensional analytical model of katabatic wind over the Antarctica has been developed. This parametric model is derived from the bulk two-layer model of Ball including the surface friction and taking into account the Earth's rotation and the geostrophic wind in the upper layer.
This model is validated using the data set (70 soundings) collected during IAGO experiment at D47 (67°24′S, 138°43′E, altitude 1 564m), 110 km inland from the coast of Adélie Land.
The parameteric model is then introduced into a GCM which is a spectral global version of the operational numerical weather prediction model used by the French weather service. The most significant effect of the parameterization is a 50 m increase of the geopotential height over the South Pole. The surface temperature at the South Pole increases (2°C) reducing the pole-midlatitude thermal gradient. The westerly circulation at 50° S is slowed down (4m/s at 850 hPa), and the surface pressure at the South Pole increases (4hPa). These results, consistent with an increase of katabatic winds, would however be improved by a better coupling between the parameterization and the GCM boundary layer.
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Pettré, P., Renaud, M.F., Renaud, R. et al. Study of the influence of katabatic flows on the Antarctic circulation using GCM simulations. Meteorl. Atmos. Phys. 43, 187–195 (1990). https://doi.org/10.1007/BF01028121
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DOI: https://doi.org/10.1007/BF01028121