 Hurricane Omar was a strong hurricane that took an unusual southwest to northeast track through the eastern Caribbean Sea during October , 2008 . Forming out of a tropical disturbance on October 13 , Omar initially moved slowly in the eastern Caribbean Sea . By October 15 , Omar began to quickly intensify as deep convection developed around the center of circulation . Later that day , an eye developed and the storm began to accelerate to the northeast . Early on October 16 , Omar reached its peak intensity with winds of 130 mph ( 215 km / h ) and a barometric pressure of 958 mbar ( hPa ; 28 @.@ 29 inHg ) . Shortly after , the hurricane rapidly weakened to Category 1 intensity . After slightly re @-@ strengthening the next day , Omar weakened to a tropical storm before degenerating into a non @-@ convective low pressure area . The remnants of Omar persisted until October 21 at which time it dissipated to the west of the Azores . 
 Hurricane Omar was a strong hurricane <a href='null_relcl' title='1'><mark>that</mark></a>took an unusual southwest to northeast track through the eastern Caribbean Sea during October , 2008 . Forming out of a tropical disturbance on October 13 , Omar initially moved slowly in the eastern Caribbean Sea . By October 15 , Omar began to quickly intensify as deep convection developed around the center of circulation . Later that day , an eye<a href='been_done' title='2'><mark></mark></a> developed and the storm began to accelerate to the northeast . Early on October 16 , Omar reached its peak intensity with winds of 130 mph ( 215 km / h ) and a barometric pressure of 958 mbar ( hPa ; 28 @.@ 29 inHg ) . Shortly after , the hurricane rapidly weakened to Category 1 intensity . After slightly re @-@ strengthening the next day , Omar weakened to a tropical storm before degenerating into a non @-@ convective low pressure area . The remnants of Omar persisted until October 21 at which time it dissipated to the west of the Azores . 
Hurricane Omar was a strong hurricane took an unusual southwest to northeast track thru the eastern Caribbean Sea during October , 2008 . Forming out of a tropical disturbance on October 13 , Omar initially moved slowly in da eastern Caribbean Sea . By October 15 , Omar began to quickly intensify as deep convection developed around tdacenter of circulation . Later dat day , an eye done developed and the storm began to accelerate to the northeast . Early on October 16 , Omar reached its peak intensity with winds of 130 mph ( 215 km / h ) and a barometric pressure of 958 mbar ( hPa ; 28 @.@ 29 inHg ) . Shortly after , the hurricane rapidly weakened to Category 1 intensity . After slightly re @-@ strengthening thdaext day , Omar weakened to a tropical storm b4 degenerating into a non @-@ convective low pressure area . Thedamnants of Omar persisted until October 21 at which time it dissipated to the dat of the Azores .