original: Convection increased on August 11, and by August 12 the interaction between a tropical wave and an upper-level low in the area resulted in a large area of disorganized thunderstorms extending from the western Caribbean Sea into the central Bahamas.
simplifications: Convection increased on August 11, and by August 12 the interaction between a tropical wave and an upper-level low in the area created a large area of disorganized thunderstorms. Transfer of heat increased on August 11. By August 12 the connection between a tropical wave and an upper-level low in the area created in an area of thunderstorms in the western Caribbean Sea to the central Bahamas. Convection increased on August 11. The interaction between a tropical wave and an upper-level low resulted in disorganized thunderstorms on the 12th. It extended from the western Caribbean Sea into the central Bahamas. Convection increased on August 11. By August 12, the interaction between a tropical wave and an upper-level low in the area created a large area of disorganized thunderstorms. This extended from the western Caribbean Sea into the central Bahamas. Convection increased on August 11. By August 12 the interaction between a tropical wave and an upper-level low in the area made a large area of disorganized thunderstorms. They went from the western Caribbean Sea into the central Bahamas. Convection increased on August 11, on August 12 he interaction between a tropical wave and upper-level low in the area resulted in a large area of disorganized thunderstorms from the western Caribbean Sea into the central Bahamas. By August 12, a tropical wave and an upper-level low in the area were causing a large area of thunderstorms. Convection currents increased on August 11. By August 12, a tropical wave and an upper-level low interacted and created a large area of disorganized thunderstorms from the western Caribbean Sea into the central Bahamas. Convection risen on August 11, and by August 12, the interaction between the tropical wave and the upper-level low in the area resulted in a large area of disorganized thunderstorms extending from the western Caribbean Sea to the central Bahamas. Convection increased by August 11, and by August 12 the interaction between a tropical wave and an upper-level low in the area caused a large area of disorganized thunderstorms from the western Caribbean Sea into the middle of the Bahamas.