The new low caused the tropical storm to degenerate into a trough about 275 mi (445 km) southeast of Wilmington, North Carolina, and Danny's remnants were absorbed into a developing frontal zone shortly thereafter.
The new low caused the tropical storm. This was to degenerate into a trough about 275 mi (445 km) southeast of Wilmington, North Carolina. Danny's remnants were absorbed into a developing frontal zone shortly thereafter.