A tropical wave moving west through the northern Caribbean developed into Tropical Storm Kyle on September 25. Because of a stationary front off the Atlantic coast, Kyle was turned northward. Due to strong west to east sheer, Kyle's convection stayed away from the right side of the system. After being hindered by Hispaniola, the system was free of land, and therefore rapidly strengthened into Hurricane Kyle on the 27. Kyle then briefly reached its peak intensity of 80 mph and a pressure of 994 millibars. Soon, Kyle accelerated northward before making landfall in Nova Scotia as an extratropical storm on the 29.
Hurricane Kyle. Note the lopsidedness of the convection.
Track of Kyle.
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