The 1956 Atlantic hurricane season officially began on June 1, 1956, and lasted until November 30, 1956. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The season was slightly below average, with only four hurricanes and eight total storms forming.
Most of the tropical cyclones of 1956 remained at sea. However, Hurricane Betsy passed directly over Puerto Rico as a Category 1 hurricane on the Saffir-Simpson hurricane scale, causing millions in damages and killing 27.
The southern portion of a polar trough, combined with a tropical wave, led to the formation of a Tropical Depression in the Bay of Campeche on June 12. It moved north-northeastward, and became a tropical storm later that day. It reached a peak intensity of 50 mph winds before hitting south-central Louisiana on the 13th, bringing heavy rain and flooding. Tropical Storm One dissipated on the 15th over Arkansas, after causing $50,000 in damage (1965 dollars) and four deaths from drowning.
The easterly wave which became Hurricane Anna formed on July 25 in the Bay of Campeche. It became a tropical storm the next day, and a hurricane late on the 26th. Anna moved inland south of Tampico, Mexico on the 26th, and dissipated the next day over Mexico after causing $50,000 in damage (1956 dollars).
As the Azores-Bermuda high moved northeastward and cold air aloft entered the Tropics, strong divergence led to the formation of Tropical Storm Betsy on August 9 in the tropical Atlantic. It moved westward, and rapidly intensified to a 120 mph major hurricane on the 10th. Betsy moved through the Lesser Antilles on the 11th, causing major damage to Guadeloupe, and weakened as it moved northwestward. The hurricane hit Puerto Rico on the 12th, and after causing heavy flooding while crossing, re-strengthened to a 110 mph hurricane. Betsy crossed the Bahamas, turned northeastward, and became extratropical on the 18th over the North Atlantic. Betsy was responsible for $35.88 million (1956 dollars) in damage and 27 fatalities.
A tropical wave over the Bahamas developed into a tropical depression on September 5. Upper level winds were fairly strong, but it managed to reach a peak of 50 mph winds before weakening from cool, dry air. Carla continued northeastward, and dissipated on the 11th.
Dora developed in the Bay of Campeche on September 10. It moved westward, gradually strengthening to a peak of 70 mph winds before hitting near Tuxpan, Mexico as a tropical depression. Despite being a weak system, Dora managed to cause 27 deaths, mostly from mudslies and flooding, yet little property damage.
Tropical Storm Ethel developed from the southern end of a quasi-stationary cold front on September 11 over the Bahamas. It intensified as it moved northeastward, reaching a peak of 70 mph winds due to the instability of the atmosphere, but cool air caused Ethel to lose her identity on the 14th.
The origin of Flossy is uncertain; one possibility is it developed from an Eastern Pacific disturbance, while the other is a disturbance moving through the Caribbean. Regardless, a tropical depression formed in the extreme western Caribbean Sea on September 21. It moved northwestward across the Yucatán Peninsula, and became a tropical storm on the 22nd. Flossy gradually strengthened over the Gulf of Mexico, becoming a hurricane on the 23rd.
Flossy totally submerged Grand Isle, Louisiana on 24 September. A flood wall was topped in New Orleans, flooding some 2.5 square miles of the Ninth Ward of New Orleans. The hurricane turned northeast in respone to the Westerlies, and hit near Fort Walton Beach, Florida on the 25th. Flossy became extratropical on the 25th over Georgia and continued northeastward, dropping heavy rain throughout its path and breaking a drought in the northeast. Flossy caused nearly $25 million in damage (1956 dollars) and 15 casualties.
The Intertropical Convergence Zone developed a tropical depression on October 30 just southwest of Haiti. It moved northward without intensifying, possibly due to the cold-core nature of the system in the Mid-levels, but as a ridge of high pressure built to the north, the depression was forced southeastward. On November 2, it was able to strengthen into a tropical storm, and a warm core developed. Greta rapidly intensified on the 4th and 5th, reaching a peak of 140 mph winds over the open Atlantic. It is theorized that the transfer of energy from upper levels to the surface attributed to the intensification. Nonetheless, Greta gradually weakened over the cooler waters of the Central Atlantic, and became extratropical on the 7th. Greta caused $3.6 million in damage (1956 dollars), almost half of which occurred in Florida from large waves and storm surge, and one death from drowning in Puerto Rico.
No names were retired after the 1956 season.
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"1956 Atlantic hurricane season".
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