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Lawrence A. Hughes
,
Ferdinand Baer
,
Gene E. Birchfield
, and
Robert E. Kaylor

It is believed that the severity of the storm hitting Canada on October 15, 1954 was due to the addition of an independent development to the dying hurricane Hazel. The problem of forecasting this event is discussed in the light of forecasts made at the time. The presence of a secondary development is verified.

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