A pattern of circulation and convergence in the equatorial zone between 95°E and 160°E during the season from December to February is presented as an improvement over that seen frequently is present literature. The pattern presented serves as a practical basis for synoptic analysis and is in agreement with observations made in the region (hiring and before the recent War.

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* This is an extract from a thesis submitted in partial fulfillment of the requirements for an M.S. Degree at New York University.