 On November 2 , a trough of low @-@ pressure was analyzed near the Lesser Antilles . The system moved westward into the Caribbean Sea without much organization . On November 7 , the low @-@ pressure area moved south of Cuba and became sufficiently organized to be considered a tropical depression with a pressure of at least <unk> mbar ( hPa ; 29 @.@ 83 inHg ) . The depression moved over Cuba and into the Atlantic , where it dissipated the following day . On November 9 , a second system was detected northeast of Bermuda with a pressure of 1005 mbar ( hPa ; 29 @.@ 68 inHg ) , though it remained unclear whether the two systems were related . 
