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The 1943 Atlantic hurricane season marked the first deliberate reconnaissance aircraft flights into tropical cyclones. The season officially lasted from June&nbsp;16 to October&nbsp;31, which was, at the time, considered the most likely period for tropical cyclone formation in the Atlantic Ocean. A total of ten storms from 1943 are listed in the Atlantic hurricane database, and an eleventh system that affected Florida and Georgia has been identified as a probable tropical depression. The first system of the year, dubbed the "Surprise Hurricane", caused severe damage throughout Texas and Louisiana in June, partially because information about its approach was censored in the fray of World War II; the storm caused 19 deaths and $17&nbsp;million in damage. A major hurricane in mid-August produced hurricane-force winds in Bermuda, and several other tropical cyclones throughout the year resulted in strong winds there. In September, a hurricane impacted the western Gulf Coast of the United States, then a tropical storm struck the Mid-Atlantic. The two storms resulted in $419,000 and $20,000 in damage, respectively; one death was attributed to the latter system. In mid-October, a strong hurricane resulted in flooding and damage to crops throughout the Caribbean; after becoming post-tropical, it contributed to moderate impacts across Nova Scotia.

The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 94&nbsp;units, above the 1931&ndash;1943 average of 91.2. 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. was found to have organized into a tropical storm by 18:00&nbsp;UTC on July&nbsp;25 while situated about 110&nbsp;mi (175&nbsp;km) southeast of the Mississippi Delta. The nascent cyclone rapidly intensified thereafter, attaining hurricane intensity by 18:00&nbsp;UTC on July&nbsp;26 and reaching its peak as a Category&nbsp;2 hurricane with winds of 105&nbsp;mph (165&nbsp;km/h) early the following morning. The compact hurricane moved ashore the coastline of Texas near Galveston Bay at 18:00&nbsp;UTC on July&nbsp;27, around which time it was intercepted by the first reconnaissance aircraft to intentionally fly into a tropical cyclone. Rainfall across Texas and Louisiana varied, but Devers, Texas, recorded a maximum storm total of 23&nbsp;in (584&nbsp;mm). Widespread freshwater flooding occurred in the Beaumont and Port Arthur areas. At Ellington Field Joint Reserve Base, scores of air cadets and soldiers held onto the wings of airplanes to prevent them from going airborne; almost two dozen were injured in the aftermath. Offshore, the hopper dredge Galveston and tugboat Titan were capsized, leading to a total of 15 deaths. Overall, damage from the hurricane reached $17 million, 19 deaths were documented, and hundreds of people were injured. As a result of the casualties, the decision to censor information during an approaching storm was never again repeated.

Hurricane Three

The third tropical cyclone of the 1943 season was noted about 265&nbsp;mi (425&nbsp;km) east of Barbados around 06:00&nbsp;UTC on August&nbsp;19. Like its predecessor, the storm steered clear of the Caribbean on its west-northwest course, producing only minor squally weather across the Leeward Islands as it intensified. It became a hurricane around 00:00&nbsp;UTC on August&nbsp;20, intensified into the season's first major hurricane by 18:00&nbsp;UTC on August&nbsp;22, and further organized to attain its peak intensity as a Category&nbsp;4 hurricane with winds of 140&nbsp;mph (220&nbsp;km/h) around 06:00&nbsp;UTC on August&nbsp;24. It curved northeast after passing within 165&nbsp;mi (265&nbsp;km) of Bermuda, where winds peaked at 81&nbsp;mph (130&nbsp;km/h),

Hurricane Six

A circulation aloft was first documented across the western Gulf of Mexico on September&nbsp;12. It became evident in surface maps three days later, marking the formation of a tropical storm by 18:00&nbsp;UTC about 270&nbsp;mi (435&nbsp;km) southeast of Matamoros, Tamaulipas. The nascent cyclone tracked northwest and attained hurricane intensity on September&nbsp;16 before reaching its peak as a Category&nbsp;2 hurricane with winds of 100&nbsp;mph (160&nbsp;km/h) the following morning. Thereafter, an area of high pressure over the northern High Plains forced the system to complete a counter-clockwise loop. As a post-tropical cyclone, the system produced winds near 70&nbsp;mph (110&nbsp;km/h) across Nova Scotia, cut electricity to Liverpool and Annapolis Valley (where the apple crop sustained $300,000 in losses), and disrupted telephone service in Halifax. Heavy surf washed out a 200&nbsp;ft (60&nbsp;m) section of railway in Shelburne while some railway lines in Lockeport suffered damage. A barge was severed from a large ship in Halifax and went aground on Georges Island.

Tropical Storm Ten

The final tropical cyclone of the season formed about 160&nbsp;mi (260&nbsp;km) northeast of the Honduras–Nicaragua border around 12:00&nbsp;UTC on October&nbsp;20. The fledgling cyclone intensified into a tropical storm twelve hours later and then attained winds of 45&nbsp;mph (75&nbsp;km/h) a while thereafter, marking its peak intensity. The system moved west for several days and passed through the Belize Barrier Reef before executing a sharp eastward turn early on October&nbsp;24, causing only delayed shipping and aviation schedules, as well as peak winds of 35&nbsp;mph (56&nbsp;km/h) in the Swan Islands.