A low-pressure area developed near just north of eastern Cuba along the axis of a quasi-stationary cold front. The low became a subtropical depression on October 4. Shortly before striking Andros Island on October 6, the system strengthened into a subtropical storm. The storm made its closest approach to Florida early on October 7. Peaking with sustained winds of 50 mph (85 km/h), the system veered northward and then northeastward, but nonetheless caused heavy rainfall and coastal flooding on land in Florida. While paralleling offshore North Carolina and South Carolina, the storm began to slowly weaken. By late on October 8, the subtropical cyclone merged with a cold front while well east of Cape Hatteras. The extratropical remnants persisted for several more hours, before dissipating on October 9.
