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چکیده
This paper is Part III in a series examining aspects of a monsoon depression that formed within the monsoon trough near the coast of northwestern Australia in February 1994. The depression was a prominent feature in that area for about a week. Aspects of the structure and evolution of the depression are described in Part I by Hell and Smith (1998). In Part II, Dengler and Smith (1998) describe idealised model calculations pertaining to the event using a three-layer baroclinic model. In this paper we examine aspects of the depression’s motion. Aust. Met. Mag. 49 (2000) 1-21
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