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       1994 PRELIMINARY 
        REPORTS  |  
      
 a. Synoptic HistoryChris originated from as a tropical wave that moved across 
        the African coast and into the eastern tropical Atlantic on 11 August. 
        Moving westward, the wave acquired significant convection and signs of 
        rotation on the 15th and became a depression on the 16th, midway between 
        Africa and the Lesser Antilles. The depression strengthened to a tropical storm by the 15th 
        and to a hurricane on the 18th, while moving toward the northwest at 12 
        to 17 mph. This strengthening occurred even though there was evidence 
        of vertical shearing from an upper-level low located to the northwest. 
        Chris remained a hurricane for almost two days before the strong vertcal 
        wind shear significantly disrupted the circular symmetry of the cloud 
        pattern and caused weakening. b. Meteorological StatisticsThe maximum flight level winds mreasured by reconnaissance 
        aircraft was 70 mph at 700 millibars midday on the 20th. This was the 
        first aircraft into Chris and, based on satellite intensity estimates, 
        weakening had already begun. The central sea-level pressure by then was 
        up to 1009 millibars. Dvorak estimates give a minimum pressure of 979 
        millibars and a maximum 1-minute surface wind speed of 81 mph on the 19th. 
         c. Casualty and Damage StatisticsThere were no casualties or damage from Chris. However, Bermuda received 2.83 inches of rainfall from the passage of Chris. 
     Maximum 
          Intensity For Hurricane Chris 
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