Based on ship observations,[10] the cyclone struck the island of New Providence, the seat of the Bahamian capital Nassau, on the morning of July 26, with sustained winds of 135 mph (217 km/h).

Weakening thereafter, the storm moved northwestward, paralleling the east coast of Florida, but came ashore near New Smyrna Beach early on July 28 with winds of 105 mph (169 km/h).

[3][17] The Nova Scotia Hurricane of 1926 Early on July 29, a tropical depression formed more than 1,200 mi (1,930 km) east of the Leeward Islands.

A few days later, it transitioned into an extratropical cyclone and then struck near Port Hawkesbury, Nova Scotia, with winds of 75 mph (121 km/h) and a central pressure at or below 1,000 mb (29.5 inHg).

[10] About this time, five ocean liners near each other encountered the storm; some portholes on the Orca were damaged and 15 passengers were treated for cuts, bruises, and contusions.

[21] Off Nova Scotia, the cyclone produced an unspecified number of casualties,[22] including the sinking of the schooners Sylvia Mosher[23] and Sadie Knickle.

In Nova Scotia, the storm downed trees and electrical poles, damaging some homes and leaving telephone service outages.

[25] The Louisiana hurricane of 1926 On August 20, a low pressure area producing unsettled weather in the western Caribbean Sea,[22] and centered about 400 mi (645 km) west-northwest of Maracaibo, Venezuela, was determined to have become a tropical depression.

On the morning of August 24, the United States Weather Bureau in Washington, D.C., advised that the storm was likely to make landfall between Galveston, Texas, and Burrwood, Louisiana.

[11] As a trough approached,[30] the hurricane suddenly turned northeast late on September 16, and over the next three days, while located about 500 mi (805 km) south-southeast of Halifax in Nova Scotia, it executed a counterclockwise, S-shaped curve.

[10] Early on September 11, a weak tropical depression formed in the western Caribbean Sea about 200 mi (320 km) east-southeast of the Swan Islands, Honduras.

Without strengthening substantially, the depression moved west-northwest for the next day and a half, passing north of the Swan Islands based upon weather reports,[11] and then curved northward.

The weak storm then turned abruptly to the northwest, having been trapped by a building ridge,[30] and early the next day, while centered north of Andros Island, it assumed a gradual curve to the southwest.

Late that day, it degenerated into a tropical depression and dissipated over the Straits of Florida on September 17, as the Great Miami hurricane approached from just 550 mi (885 km) to the east-southeast.

[10][36] Swiftly crossing southernmost Florida, the potent hurricane weakened slightly before entering the Gulf of Mexico near Punta Rassa in the afternoon, and its path gradually curved northwest on September 19.

Late on September 20, its path slowed drastically and curved west, making landfall near Perdido Beach, Alabama, with winds of 115 mph (185 km/h) and a measured pressure of 954.9 mb (28.20 inHg) in the calm eye.

[35] Many people in Miami, transients who knew little of hurricanes, perished after examining damage during the passage of the eye, unaware that the back end of the storm was approaching.

[49] Twelve hours after the Great Miami hurricane struck Alabama, the eighth tropical storm of the season formed in the east-central Atlantic about 2,000 mi (3,220 km) southwest of Horta in the Azores on September 21.

Late that day, the cyclone swerved precipitously to the north, making landfall on the island of São Miguel near Ponta Delgada at peak intensity.

[9] Curving northwest and then south of due west, the cyclone weakened after striking São Miguel and reverted to a minimal hurricane late on September 27.

It gradually completed a counter-clockwise loop through the western Azores, curving due south as a tropical storm, though its cool surface temperatures and enlarged size suggest it might have been a subtropical cyclone then.

[10] Early on October 3, a tropical depression developed in the South-Central Caribbean about 100 mi (160 km)/h) east of Serrana Bank and the Miskito Cays.

Curving west-northwest without further intensification, the weak cyclone made landfall near Barra Patuca in Gracias a Dios Department, Honduras, shortly before 12:00 UTC on October 4.

Shortly thereafter, the storm gradually turned just north of due west, and early on October 5, after degenerating into a tropical depression, it made a second landfall over Belize just south of Alabama Wharf in Toledo District.

[9] The Great Havana-Bermuda Hurricane of 1926 On October 14 a tropical depression developed in the southern Caribbean Sea about 350 mi (565 km) north-northwest of Colón, Panama.

Shortly before striking the Isla de la Juventud south of Nueva Gerona, it attained maximum sustained winds of 145 mph (233 km/h) on October 20.

On October 21, with the eye of the storm still 700 mi (1,130 km) from Bermuda, weather forecasts from the United States called for the hurricane to strike the island on the following morning with gale force.

The Arabis-class sloop HMS Valerian, based at the HMD Bermuda, was returning from providing hurricane relief in the Bahamas and was overtaken by the storm shortly before she could make harbor.

Passing less than 50 mi (80.47 km) west of the Swan Islands, Honduras, early on November 14, the cyclone gradually turned north by the afternoon.

Curving parabolically to the northeast on November 15, it weakened to a tropical depression early the next day before hitting the Isla de la Juventud in Cuba.