The storm deepened significantly over the next few days, and by August 22, it peaked as a Category 3 hurricane with sustained winds of 125 mph (205 km/h) and a minimum pressure of 950 mbar (28 inHg).

Crop damage from the hurricane was severe as the storm destroyed about half of the fruit, vegetable, and hay harvest, leaving a loss of $1 million (1927 CAD).

Moving west-southwestward, the storm passed through the Cape Verde Islands on September 3, striking Boa Vista with winds of 45 mph (75 km/h).

Around that time, a radiogram from the British S.S. Socrates indicated that the ship recorded a barometric pressure of 1,007 mbar (29.7 inHg), the lowest observed in association with the storm.

[5] By September 9, the hurricane peaked with maximum sustained winds of 90 mph (150 km/h) and began curving north-northwestward, which was soon followed by a turn to the north-northeast later that day.

[5] Thereafter, the storm started to lose tropical characteristics, with historical weather maps indicating a low pressure area imbedded within a cold front by September 10.

Late on September 11, the storm weakened to a tropical depression and was last noted at 18:00 UTC, while located about 870 mi (1,400 km) east-northeast of Bermuda.

[5] A low pressure area developed into a tropical depression around 12:00 UTC on September 22 while located about 820 mi (1,320 km) southwest of the southwesternmost islands of Cape Verde.

[4] Early on September 29, the hurricane weakened to a tropical storm and became extratropical six hours later, while situated about 935 mi (1,505 km) south-southeast of Cape Race, Newfoundland.

[5] At approximately 12:00 UTC on September 30,[5] a low pressure area developed into a tropical depression while situated about 175 mi (280 km) northeast of Turks and Caicos Islands.

[4] The depression moved parallel to the islands of the Bahamas and slowly strengthened, reaching tropical storm status early on October 2.

[5] Continuing its northwestward motion, the storm strengthened further and peaked early on October 3 with maximum sustained winds of 60 mph (95 km/h) and a minimum barometric pressure of 1,008 mbar (29.8 inHg),[5] the latter of which was a ship observation.

Many were left without power for several hours on morning of October 3, crippling industries that depended on electricity, including delaying publication of The Beaufort Gazette because the linotype machine could not be used.

[4] Elsewhere in the state, particularly in Charleston, there were widespread telephone, telegraph, and power outages due to downed lines and poles, severing communications.

In North Carolina, similar damage occurred to the methods of communications in Raleigh, Selma, Siler City, and other areas closer to the Virginia state line due to wires knocked over by strong winds.

[9] The season's next cyclone developed from over the northwestern Caribbean Sea from a broad low pressure area near the Bay Islands Department of Honduras on October 16.

[5] Early on October 17, the system peaked with winds of 45 mph (75 km/h), based on a ship observation of a minimum barometric pressure of 999 mbar (29.5 inHg).

[4] Curving northeastward, it made landfall near Santa Cruz del Sur, Camagüey Province, late on October 18 at the same intensity.

Historical weather maps indicated that the highest sustained winds were at 30 mph (50 km/h) and the minimum barometric pressure was 1,004 mbar (29.6 inHg).

[11] The final tropical cyclone of the season developed from a low pressure area early on November 19, while situated about 770 mi (1,240 km) east-northeast of Barbuda.

[4] On November 21, the storm weakened and lost tropical characteristics, merging with a cold front about 585 mi (940 km) east-northeast of Bermuda at 12:00 UTC.