 After affecting Florida, the depression continued to the northeast, and although it had a warm core, it was not able to develop significantly due to lack of temperature instability, as well as another low developing southwest of the circulation. The depression was briefly forecast to strike North Carolina, but instead an eastward moving ridge kept it offshore. In Hatteras, North Carolina, the depression dropped 3 in (76 mm) of rainfall. The influx of cold air transitioned the depression to an extratropical cyclone on May 28. An approaching cold front absorbed the depression and produced heavy rainfall in eastern Canada.
