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The results of a series of numerical experiments which were intended to simulate the warming and devebping stages of hurricane formation are discussed. In the cxperiments, an initially weak cyclone develops into an intense vortex. However, the deepening proceeds too rapidly and meridional circulations which are too inteiisc develop. The inclusion of ground friction and vertical mixing lcads to solutions which are even less acceptable. Lateral mixing slows the devclopnicnt but only provides a tcinporary dclay in the generation of an unacceptably intense meridional circulation.

SOME ATTEMPTS TO SIMULATE THE DEVELOPMENT OF TROPICAL CYCLONES BY NUMERICAL METHODS