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The 1912 Atlantic hurricane season was an average hurricane season that featured the first recorded November major hurricane (Category&nbsp;3 or higher on the modern day Saffir–Simpson scale). There were eleven tropical cyclones, seven of which became tropical storms; four of those strengthened into hurricanes, and one reached major hurricane intensity. The season's first cyclone developed on April&nbsp;4, while the final dissipated on November&nbsp;21. The season's most intense and most devastating tropical cyclone was the final storm, known as the Jamaica hurricane. It produced heavy rainfall on Jamaica, leading to at least 100&nbsp;fatalities and about $1.5&nbsp;million (1912&nbsp;USD) in damage. The storm was also blamed for five deaths in Cuba.

Other tropical cyclones that left notable impact include the fourth and sixth hurricanes. The former brought rough seas and storm surge to portions of the Gulf Coast of the United States, leaving locally severe damage, particularly in Mobile, Alabama, and Pensacola, Florida, totaling about $39,000. One fatality occurred after a barge capsized. The sixth hurricane brought rough seas and heavy precipitation to northeastern Mexico and south Texas, with flooding reported inland. The storm left 15&nbsp;deaths and about $28,000 in damage. Overall, the tropical cyclones of this season collectively caused at least 122&nbsp;fatalities and just under $1.6&nbsp;million in damage.

The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 57, near the 1911&ndash;1920 average of 58.7. ACE is a metric used to express the energy used by a tropical cyclone during its lifetime. Therefore, a storm with a longer duration will have high values of ACE. It is only calculated at six-hour increments in which specific tropical and subtropical systems are either at or above sustained wind speeds of 39&nbsp;mph (63&nbsp;km/h), which is the threshold for tropical storm intensity. Thus, tropical depressions are not included here. Some locations in eastern North Carolina reported strong winds, particularly at Fayetteville, where there was a "severe local storm". In Pensacola, abnormally high tides caused severe damage. Wharves and small buildings used for storing fishing equipment washed away. About 20&nbsp;barges were beached, strewing timber across the beach. Service via the Louisville and Nashville Railroad was briefly interrupted due to timber on a railroad bridge. Wind damage was relatively minor. A dance pavilion on Santa Rosa Island was partially deroofed, as was a hotel. Damage in Pensacola reached approximately $25,000 (1912&nbsp;USD). In Alabama, the city of Mobile in particular suffered impact from the storm. Some ships and vessels capsized in the Mobile Bay and Mobile River, including a $2,000 barge, drowning a watchman. Winds destroyed a church, though wind damage was otherwise limited to downed street signs and fences. Overall, the hurricane caused $39,000 in damage. Moving west-northwestward, the storm strengthened steadily, reaching winds of 70&nbsp;mph (110&nbsp;km/h) before making landfall near Cancún, Quintana Roo, early on October&nbsp;13. The system weakened slightly over land and while situated in the Gulf of Mexico just north of the Yucatán Peninsula, but began re-intensifying later that day. By 12:00&nbsp;UTC on October&nbsp;14, the cyclone deepened into a Category&nbsp;1 hurricane and then a Category&nbsp;2 hurricane about 24&nbsp;hours later. The hurricane made landfall on central Padre Island between Corpus Christi and Port Mansfield in Texas late on October&nbsp;16 with winds of 100&nbsp;mph (155&nbsp;km/h), estimated based on a storm surge of . A barometric pressure of was estimated using the pressure-wind relationship. Many buildings were destroyed and several boats sunk after tides rose in less than 4&nbsp;hours. Fifteen people died and damage reached more than $28,000 (1912&nbsp;USD). Strong winds generated by the storm destroyed approximately 25% of banana trees, while telegraph lines were downed in a number of places. Railway lines were also heavily damaged by the winds and rain. Rough seas also lashed the island, with Savanna-la-Mar suffering near complete destruction and 42&nbsp;deaths in that city alone. Across western Jamaica, roughly a hundred homes were destroyed, while 5,000&nbsp;buildings were damaged or demolished. About 100&nbsp;fatalities and $1.5&nbsp;million in damage occurred in Jamaica.

Other systems

In addition to the seven tropical storms, four tropical depressions developed and remained below tropical storm intensity. The first formed from an extratropical cyclone well to the southwest of the Azores on April&nbsp;4. The depression moved southwestward until being by a frontal boundary on April&nbsp;6. By September&nbsp;25, another tropical depression developed from a formerly extratropical cyclone about halfway between Bermuda and the Azores. However, on September&nbsp;27, the depression lost tropical characteristics again. The next tropical depression formed on October&nbsp;17 to the southeast of Bermuda. Moving generally northwestward, the depression transitioned into an extratropical cyclone by October&nbsp;21. The final non-developing depression formed from an extratropical cyclone to the west of the Canary Islands on November&nbsp;7. The depression tracked generally westward before being absorbed by a frontal system on November&nbsp;11.