Due to the lack of systems that developed, only one tropical cyclone, the second hurricane, managed to make landfall during the season.

[2] The extratropical storm was tracked due east towards the Azores for a few days while gradually weakening before abruptly turning to the north and dissipating.

[4] The Dominican Republic Hurricane of 1930 A tropical depression developed well east of the Lesser Antilles on August 29.

Moving westward over the Caribbean Sea, the storm failed to re-strengthen before making landfall in western Cuba with winds of 40 mph (65 km/h) around midday on September 6.

The following day, the storm deteriorated further to a tropical depression, and late on September 17, the cyclone dissipated southwest of the Azores.

[2] While crossing the Lesser Antilles, the hurricane brought powerful winds and heavy rainfall to the islands.

[6] In the Dominican Republic, three districts of Santo Domingo were destroyed,[8] with half of the city leveled by the hurricane.

After passing the Outer Banks of North Carolina as re-intensifying hurricane, power outages occurred across the region.

[11] The final storm of the season developed in the Bay of Campeche on October 18 at the tail end of a frontal boundary.

Although cool-air advection was occurring off the United States coast, warm air around the system allowed the tropical storm to intensify.

Moving to the northeast, the system reached peak intensity as a high-end tropical storm with winds of 70 mph (110 km/h).