The 1987 Atlantic hurricane season was a below-average hurricane season that was limited by an ongoing El Niño. The season officially began on June 1, 1987, and lasted until November 30, 1987, although activity began on May 24 when a tropical depression developed east of the central Bahamas. The June through November dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first cyclone to attain tropical storm status was an unnamed tropical storm which formed on August 9, nearly a month later than usual. The final storm of the year, Tropical Depression Fourteen, merged with a weak extratropical low on November 4. The season marked the first year tropical storm watches and warnings were issued; previously, gale watches and warnings were used for tropical storms, and this season was one of only a few seasons with no deaths in the United States; the last time this happened was in the 1981 season.

During this season, 14 tropical depressions formed of which seven attained tropical storm status. One tropical storm was operationally classified as a tropical depression but was reclassified in post-analysis. Three tropical cyclones reached hurricane status of which only one became a major hurricane, which is a Category 3 or greater on the Saffir–Simpson scale. Hurricane Emily was the costliest storm of the season, causing $80.3 million in damage (1987 USD) as it ravaged the Dominican Republic and Bermuda. Tropical Depression Fourteen was the deadliest storm of the season, causing six deaths as it passed across Jamaica. Of the seven cyclones that attained tropical storm status, three did not affect land.

Seasonal forecasts and activity +Predictions of tropical activity in the 1987 seasonSourceDateNamedstormsHurricanesMajorhurricanesRefCSUJune 285N/ARecord high activity30157†Record low activity10†0†Actual activity 7 3 1 Forecasts of hurricane activity are issued before each hurricane season by hurricane expert Dr. William M. Gray and his associates at Colorado State University. An average season, as defined by NOAA, has 6 to 14 named storms, with 4 to 8 of those reaching hurricane strength, and with 3 hurricanes becoming major hurricanes. The June 2, 1987, report suggested that eight tropical storms would form during the 1987 season, five of them becoming hurricanes.

The forecast anticipated more tropical activity than what ultimately occurred. During the season, 14 tropical depressions formed from May 25 to November 5. Seven of the depressions strengthened into tropical storms, six of them named. Tropical Depression Two was upgraded into a tropical storm in post-season analysis, and as a result has no name. Tropical storms Arlene, Emily and Floyd all reached hurricane status during their durations, of which only Emily reached major hurricane status.

The United States was affected by four tropical cyclones in 1987, of which three struck Florida. The unnamed tropical storm struck Texas and affected much of the Gulf Coast of the United States.

The season's activity was reflected with a cumulative accumulated cyclone energy (ACE) rating of 34, which is classified as "below normal". ACE is, broadly speaking, a measure of the power of the hurricane multiplied by the length of time it existed, so storms that last a long time, as well as particularly strong hurricanes, have high ACEs. ACE is only calculated for full advisories on tropical systems at or exceeding or tropical storm strength. Subtropical cyclones are excluded from the total.

Systems

Tropical Depression One

A low-pressure area developed into a tropical depression just east of the Turks and Caicos Islands on May 24. Operationally, the system was declared the first tropical depression of the season on May 25, following confirmation from a reconnaissance aircraft flight. Moving at about , the depression was located from the east central Bahamas. It moved towards Florida and stalled off the coast, with a prediction to cause thundershowers across the state on May 28. The Bahamian government released a storm warning for its northern islands as the system grew stronger. The depression brought some heavy showers and thunderstorms to South Florida, before dissipating just south of Key West on June 1.

Tropical Storm Two

The second tropical depression of the season formed in the northwestern Gulf of Mexico from a tropical wave on August 9. It quickly strengthened into a tropical storm, though the strengthening was not known until post-season analysis. Based on lack of significant organization or reports at the time, the storm remained unnamed. It traveled northwestward and neared the coast. The tropical storm made landfall near High Island, Texas, with winds of 45 mph (75 km/h) on August 10, and quickly weakened to a tropical depression as it moved northeastward. It turned to the southeast and re-emerged into the Gulf of Mexico on August 15, before striking near St. Marks, Florida, on the next day. The weakening system turned back to the northeast, continued weakening, and dissipated over Georgia on August 17.

The slow-moving system produced heavy rainfall along the Gulf Coast, particularly in southern Mississippi and Alabama, with just over of precipitation recorded in the former. In Mississippi, the Biloxi and Tchoutacabouffa rivers crested at major flood stage, forcing 357 people to evacuate. Floodwaters reached in height along several roads and entered many homes in Jackson County. Additionally, many businesses suffered water damage in Columbia, where about 25 families also evacuated due to flooding. Overall, damage from the system amounted to $7.4 million.

Hurricane Arlene

A low pressure system on the tail end of a stationary cold front organized into a subtropical depression on August 8 near the South Carolina coast, and drifted southward. Convection became more organized, and the storm was classified Tropical Depression Three on August 10 over the Bahamas. It executed an anticyclonic loop to the northeast, and was estimated to have attained tropical storm status on August 11, based on reports from hurricane hunters. Small cells in the ridge of high pressure caused Arlene to take an unusual track to the east, with two southward jogs in its path. A trough of low pressure near Bermuda initially inhibited strengthening. However, after high pressures to its east forced the storm northward, more favorable conditions allowed Arlene to intensify into a hurricane on August 22. Operationally, it was upgraded two days earlier, based on the appearance of an eye feature on satellite imagery. After becoming a hurricane, Arlene accelerated to the northeast into the cold waters of the north Atlantic Ocean, and on August 23 it became extratropical about halfway between Newfoundland and Ireland. The extratropical remnants turned to the southeast and later to the east, making landfall on the Iberian Peninsula before dissipating on August 28 over Spain.

As Arlene approached, islanders of Bermuda were warned to board up windows, with winds of expected. Ultimately, the island experienced winds of with gusts up to . A blind sailor on a trip across the Atlantic was unable to make it to a harbor in Bermuda due to the hurricane, and rode out the storm in the open sea. The storm produced moderate rainfall to coastal areas of Spain, contributing to a monthly rainfall record at Rota. The 14.5 day total between the start of its best track and when it attained hurricane status is the largest on record for a North Atlantic hurricane.

Tropical Depression Four

The fourth tropical depression of the season formed about east of Barbados early on August 13. Initially, forecasters anticipated the system to intensify into a tropical storm; however, a reconnaissance mission into the depression on August 15 revealed that it was poorly organized and was declassified a tropical cyclone. Tropical Depression Four peaked with sustained winds of and dissipated on August 15 about northeast of Anegada in the British Virgin Islands.

Tropical Storm Bret

A well-organized tropical disturbance formed off the African coast on August 17 and became a tropical depression the following day, as classified by satellite imagery. Later the same day, the ship S.S. Columbus Canterrury reported winds and a pressure of , and the depression became Tropical Storm Bret.

The cyclone moved a westward course of and reached its peak intensity of winds and in pressure on August 20. A ridge of high pressure in the eastern Atlantic Ocean, north of Bret, began to weaken and drift to the east on August 20. Bret was moving at to the east on August 21. It was thought that Bret would strengthen at this point. Bret slowed from August 21 until August 23, moving at only .

The cyclone soon moved on a northwestward course and encountered wind shear. Bret weakened into a depression on August 23, due to the wind shear over the system. The next morning, the depression became a tropical wave with no low-level circulation left. The wave was soon absorbed by a trough of low pressure during the next few days.

Tropical Depression Six

A tropical depression formed well west-southwest of the Cape Verde Islands on August 30. Forecasters predicted would become the third tropical storm of the season. At 0600 UTC August 31, the depression was seemingly unchanged, with winds of averaging about . The depression was then located west of Sao Taigo in Cape Verde, stirring up seas.

The next day, Tropical Depression Six moved westward to a position more than away from the Cape Verde Islands and the Lesser Antilles, too far away from land for the National Hurricane Center to send a reconnaissance flight into the depression. Tropical Depression Six was at the time not a threat to land and few ships were in the area. The depression degenerated into a tropical wave by September 2, though it was operationally considered a tropical cyclone until the following day.

Tropical Storm Cindy

On September 1 a tropical wave exited the African coast, and moved westward across the Atlantic Ocean. A trough of low pressure moved southeastward through the tropics, and brought the wave more towards the north. Generally favorable conditions for development allowed the wave to organize into a tropical depression on September 5, and two days later it attained tropical storm status. Cindy continued northward, and peaked at winds on September 8 before turning to the northeast. Strong upper-level shear weakened the storm, and after two days of struggling as a tropical storm, Cindy became extratropical on September 10 to the northwest of the Azores. Cindy did not affect any landmasses.

Tropical Depression Eight

A tropical depression formed in the Caribbean on September 6. It tracked westward through the body of water, and reached peak winds of on September 7. Despite its appearance, Tropical Depression Eight failed to develop further and early on September 8, the depression made landfall near Puerto Cabezas, Nicaragua, shortly before dissipating.

Tropical Depression Nine