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Strong wind events at Dumont d'Urville (DdU), an East Antarctic coastal station, and Dome C, an interior station,&#13; were studied to determine if the wind along the Adelie Land coast increases with the approach of the depression&#13; from the west of the site or after its passage to the east of it. The events for the year 1993 were studied using&#13; synoptic observations, mean sea level pressure charts and composite infrared satellite images. It was found that the&#13; winds are enhanced with the approach of a depression from the west towards the DdU coast. The wind increases in&#13; response to the decreasing pressure at the coastal site and increasing downslope pressure difference (dp). The wind&#13; starts decreasing once the system moves to the east of DdU and the pressure at DdU starts building up, as reported&#13; in some earlier studies. The response of wind to the approaching depression is not the same for all the events but&#13; depends on the downslope pressure difference and the movement of the depression that is often conditioned by&#13; the presence of a blocking high to the northeast. The wind comes down if the system starts penetrating inland&#13; due to the presence of the high pressure ridge to the northeast and decreasing dp. It is observed that the winds at&#13; Dome C increase to as high as 17 m s-1 with the inland penetration of the depression

Analysis of strong wind events around Adelie Land, East Antarctica