MIAMI — The National Hurricane Center reported at 800 PM EDT Saturday, May 30, 2026, that tropical cyclone formation is not expected in the North Atlantic, Caribbean Sea, and Gulf of America during the next 7 days. This assessment covers a broad region that includes all major basins where tropical systems commonly develop during the Atlantic hurricane season.
An Atlantic Gale Warning remains in effect for waters between northeast Florida and Bermuda due to a cold front moving through the area on May 30–31, 2026. Gale-force winds are expected south and southeast of Bermuda between 29N and from 55W to 65W on Sunday afternoon, May 31, according to the latest data.
Although tropical cyclone development is not anticipated, tropical waves are present across several parts of the Atlantic and Caribbean. As of May 30, these waves are located along 19W south of 16N, 62W south of 17N, and 75W–76W south of 16N. None of these systems currently show signs of organization that would lead to tropical cyclone formation in the near term.
Scattered showers and thunderstorms are active over the eastern half of the Gulf of America as of May 30, driven by an upper-level trough. Meanwhile, fresh to strong easterly trade winds and seas of 6–8 feet are present in the south-central Caribbean Sea, as confirmed by scatterometer and altimeter data.
The National Hurricane Center will resume routine issuance of the Tropical Weather Outlook on June 1, 2026. During the off-season, Special Tropical Weather Outlooks will be issued as conditions warrant, ensuring that any unexpected developments receive timely monitoring and public notification.
The Atlantic hurricane season officially begins on June 1 and runs through November 30. Historical data from the National Oceanic and Atmospheric Administration indicates that the majority of tropical cyclone activity in the Atlantic basin occurs between August and October. Despite the current lack of development, the presence of multiple tropical waves is typical for late May as ocean temperatures begin to rise and atmospheric conditions gradually become more conducive to storm formation.