The 1936 Atlantic hurricane season was a fairly active season, with 20 tropical cyclones recorded, 17 of which became tropical storms. Seven storms became hurricanes, of which one became a major hurricane. In addition, the season was unusual in the fact that no storms moved across large portions of the Caribbean Sea.[1] Seven storms, including three hurricanes, struck the United States.
The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 100units,[2] slightly higher than the 1931–1943 average of 91.2.[3] 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 39mph (63km/h), which is the threshold for tropical storm intensity. Thus, tropical depressions are not included here.[2]
On June9, a tropical cyclone with atmospheric pressure below 988mb (29.18inHg) made landfall on the Pacific coast of Guatemala.[4] It moved northeastward across Central America, but dissipated before reaching the western Caribbean Sea on June12. The storm quickly re-organized, and again developed into a tropical storm on June12. It moved north-northeastward, resulting in light winds as it paralleled the eastern coasts of Belize and the Yucatán Peninsula. After reaching the Gulf of Mexico with peak winds of 45mph (75km/h), the storm turned to the northeast, then to the east. On June15, the tropical storm made landfall about 20mi (32km) to the south of Fort Myers, Florida, and after crossing the state it passed over Miami before entering the Atlantic Ocean.[4] It weakened as it accelerated northeastward through the Bahamas, and on June17 the system dissipated to the north of Bermuda.[1]
While crossing Central America, the storm produced heavy rainfall.. In southern Florida, winds from the storm ranged from 30mph (48km/h) to a peak of 39mph (63km/h) in Miami. The storm produced heavy rainfall in southern Florida, ranging from 8 to 15in (200 to 380mm). The rainfall caused flooding of highways and lowlands, drowned several livestock, and some damage. The storm caused three indirect deaths when a Coast Guard airplane crashed in Tampa Bay while in search of small boats.[1]
An area of disturbed weather was first detected near the Yucatán Peninsula on June18. It tracked west-northwestward, and developed into a tropical storm the following day. The storm continued to the west-northwest until June 21, when the storm turned to the west-southwest. Having remained a minimal tropical storm for all of its lifetime, the 40-mph (65-km/h) storm struck northeast Mexico on June 21, and dissipated the next day. The storm caused higher than normal tides along the Texas coastline, and no damage or deaths were reported.[1]
A small tropical storm developed on June26 while located 125mi (200km) east of Brownsville, Texas. It moved northwestward and rapidly strengthened almost immediately after formation (similar to Humberto of 2007), attaining hurricane status with peak winds of 80mph (130km/h) by early on June27. Later on June27, the hurricane made landfall near Port Aransas with a pressure of 987mb (29.15inHg).[5] The storm rapidly weakened over land, and dissipated on June28 near San Antonio, Texas. A small craft warning was issued for the Corpus Christi area on the morning of the storm making landfall, and the National Weather Bureau issued a hurricane warning just 45minutes prior to the hurricane striking land.[1]
Upon making landfall, the storm caused a 3.8-ft (1.2-m) storm tide, and many small boats were capsized or driven ashore. The hurricane produced wind gusts of up to 90mph (140km/h) in Ingleside and up to 80mph (130km/h) in Port Aransas, destroying cooling towers at a local oil refinery and damaging a few houses. Along its path, the storm produced heavy rainfall, though specifics are unknown.[6] Severe crop damage was reported in San Patricio and Nueces Counties. In all, the hurricane caused $550,000 in damage (1936USD), primarily to oil refinery property, though no deaths or injuries were reported.[1]
On July26, a small tropical storm formed near the western tip of Cuba from a tropical disturbance. It moved quickly northwestward, then turned northward, reaching a peak intensity of 45mph (75km/h) that day. On July27, the storm accelerated northeastward and made landfall on southeastern Louisiana with a pressure of 1003mbar (hPa; 29.62inHg). The storm rapidly weakened over land and dissipated later that day. The Weather Bureau office issued a storm warning for the Louisiana coastline, advising those potentially affected to prepare for strong winds and rising tides. However, the storm caused no serious damage, and no casualties are associated with the storm.[1] Wind speeds topped out at 21mph (34km/h) in New Orleans, Louisiana.[7]
A tropical storm was first observed over the southern Bahamas on July27. It tracked to the west-northwest, and made landfall a short distance south of Homestead, Florida, with winds of 65mph (100km/h). After crossing the state, it intensified over the eastern Gulf of Mexico and became a hurricane on July30. The hurricane continued to strengthen, and on July 31 hit the western Florida Panhandle near Camp Walton with peak winds of 105mph (165km/h).[4] It weakened rapidly over land, and dissipated over western Alabama on August 1.[1]
In south Florida, the storm caused a storm tide of 5.5ft (1.7m) when it made landfall, causing flooding of up to 1.5ft (0.46m) in coastal areas. Though winds reached 60mph (95km/h), damage was minimal there. In Valparaiso in the Florida Panhandle, the hurricane produced wind gusts of up to 100mph (155km/h), along with a storm tide of 6ft (1.8m).[1] Damage from the storm was relatively minor, totaling to $200,000 (1936USD).[8] The hurricane indirectly killed four people when a boat capsized in the Gulf of Mexico.
The sixth tropical storm of the season was first spotted on August 4 while located 155mi (250km) east-northeast of Barbuda. It tracked northwestward, and reached a peak intensity of 40mph (65km/h) on August 5. It retained that intensity throughout its lifetime (although it is possible it remained a tropical depression but data was conflicting), which was followed by a turn to the northeast on August 8. On August 9, the storm passed 160mi (255km) to the west of Bermuda, and early on August 10 the storm became extratropical over the open Atlantic Ocean. The extratropical storm continued northeastward until dissipating late on August 11 while 280mi (450km) south of the eastern tip of Nova Scotia.[9]
A weak tropical storm formed on August 7 in the eastern Gulf of Mexico west-northwest of the Dry Tortugas. The system moved northwest towards the northwest Gulf of Mexico through August 9 while maintaining its peak of 40mph (65km/h). It is possible it weakened to a tropical depression at times, but there is no data supporting or denying such. The storm then began to curve more to the west-southwest on August 10 while located just south-southwest of Port Eads, Louisiana, while maintaining intensity. The storm continued moving southwest through August 11, weakening to a tropical depression shortly before making landfall near Tampico on August 12. The system weakened quickly after moving inland, and dissipated shortly afterwards.[9]
Advisories were issued early on August 12 from the U.S. Weather Bureau in New Orleans for the system as it neared Mexico shortly before making landfall,[10] but little damage and no deaths were reported in Mexico.[4]
A tropical disturbance was detected in the western to northwest Caribbean Sea near Cancún on August 15.[1][9] The system moved northwest into the southwest Gulf of Mexico as a tropical storm on August 16 while slowly strengthening. The system reached hurricane intensity as a Category 1 on August 17, and reached its peak of 75mph (120km/h) shortly afterwards. The hurricane began to move west-southwest late on August 17 and through August 18, eventually making landfall near Tampico, Tamaulipas, on August 19 as a minimal hurricane or strong tropical storm. The system quickly weakened just after moving inland and dissipated early the next day.[9]
The hurricane brought heavy rains to mainland Mexico, while the highest winds recorded at Tampico were 30mph (48km/h) on August 19 as the center passed nearby just to the north.[1] Storm warnings were issued on August 17 and 18 as the system initially approached the upper Gulf Coast of Louisiana and Texas, but the system's west-southwest turn prevented a direct United States landfall.[1]
A weak tropical storm formed on August 20 near the eastern Bahamas. Moving slowly west-northwest through August 21, the system strengthened to its peak of 60mph (95km/h) later on August 21, and made landfall on August 22 near Daytona Beach at its peak intensity. The system maintained tropical storm intensity inland while slowly weakening and moving westward, and the storm eventually weakened to a depression on August 23 while entering the eastern Florida Panhandle, and the system dissipated shortly afterwards near as it drifted over eastern Mississippi.[9] The storm caused heavy rains across northern and central Florida, and winds of 40mph (65km/h) were recorded near Titusville. Overall damage was minimal.[1]
This Cape Verde hurricane was first detected in the eastern tropical Atlantic on August 25. Moving northwest on August 29, the system continued to strengthen, eventually reaching a peak of 110mph (175km/h) as a Category 2 hurricane in the central North Atlantic on September 1. The hurricane then began to curve northeast late on September 1 while maintaining intensity, eventually weakening to a 90mph (140km/h)Category 1 hurricane on September 5. The system became extratropical on September 6, and the system dissipated while nearing the British Isles.[9] As the system never affected land, no damage or casualties were reported.[1]
A tropical storm was detected on August 28 in the far western Caribbean Sea. The system moved steadily west-northwest, making landfall shortly afterwards on the Yucatán Peninsula as a 45mph (75km/h) tropical storm. The system weakened slightly to a 40-mph (65-km/h) tropical storm as it steadily crossed the Yucatán, entering the Bay of Campeche late on August 28. The system then began to slow down on August 29 while reintensifying, peaking as an 80-mph (130-km/h) Category 1 shortly afterwards. The hurricane then began to move to the west-southwest, making a final landfall near Tuxpan as a 75-mph (120-km/h) minimal hurricane on August 30. The system quickly weakened to a tropical storm shortly after moving inland, and the weakening storm dissipated shortly afterwards.[9]
Although advisories were issued for Mexico on August 29 and early on August 30 from the U.S. Weather Bureau in New Orleans, little overall damage was reported in mainland Mexico.[1]
On September 7, a ship reported southwest winds at a location about 405mi (650km) northeast of Antigua, indicating the presence of a tropical cyclone. The storm tracked to the west-northwest without strengthening, and the following day no circulation was reported. It is estimated the storm weakened to a tropical depression and dissipated on September 8 while located about 235mi (380km) north-northeast of Saint Martin, although it may have remained a tropical depression throughout its short lifespan.[9] The storm never affected land.[1]
A tropical storm was first observed by a ship on September 8 while located about 750mi (1,205km) east of Barbados. The storm moved northwestward, and slowly intensified to attain hurricane status on September 10 about 425mi (685km) northeast of Barbados. The hurricane continued to slowly strengthen as it decelerated its forward motion, and on September 15 it reached its peak intensity of 120mph (195km/h) while located 375mi (605km) south-southwest of Bermuda. By the morning of September 15, the hurricane had winds exceeding 25mph (40km/h) in a diameter of about 1,000mi (1,610km), among the largest tropical cyclones on record. It slowly weakened as it approached the East Coast of the United States. Late on September 18, the hurricane passed within 45mi (70km) of the Outer Banks before it accelerated and turned to the northeast. It remained close to the Mid-Atlantic and New England coastline, and passed near Nantucket before turning to the east-northeast. The hurricane remained south of Atlantic Canada by a short distance, and became extratropical on September 19 while located about 50mi (80km) east of Nantucket. The extratropical storm decelerated as it turned northeastward, and the system dissipated on September 25.[1][9]
Early on September 17, Weather Bureau offices began issuing storm warnings from Beaufort, North Carolina, to the Virginia capes.[1] In North Carolina, the hurricane produced winds of up to 90mph (140km/h) in Manteo. Described as one of the worst hurricanes in record in Hatteras, the storm resulted in $25,000 in damage (1936USD) to roads and bridges and $30,000 in damage (1936USD) to buildings and piers. Very high tides were reported along the Outer Banks, with Nags Head losing about 35ft (11m) of beach. The hurricane destroyed the highway bridge along the Currituck Sound, and resulted in heavy crop damage in northeastern North Carolina.[11] The hurricane was also considered among the worst hurricanes on record in the Norfolk, Virginia, area. Winds of up to 84mph (135km/h) at Cape Henry destroyed windows, roofs, and some entire buildings, resulting in around $500,000 in damage (1936USD). The hurricane produced a storm tide of 9.3ft (2.8m) in Sewell's Point, Virginia, the second highest on record at that location. Two locations along the James River experienced record crest levels of over 20ft (6.1m). Rough seas washed several boats ashore, and shipping was cancelled in and out of Norfolk. The hurricane resulted in cancelled train service and increased traffic.[12][13] The hurricane was indirectly responsible for two casualties. The first fatality occurred when debris from the hurricane struck a person in the head and later died. Another person drowned in the Elizabeth River in an effort to recover a rowboat blown adrift.[1] Though hurricane warnings were posted for the northeast United States and hurricane-force winds occurred there, damage, if any, is unknown.[14] Extensive property damage was reported in Nova Scotia. Up to 7in (180mm) of precipitation washed out a number of bridges, roads, and railroad tracks, causing two train derailments. Dozens of cars stalled, while slick roads resulted in several vehicular accidents. Crops also suffered significant damage, with thousands of dollars in losses to grain alone in Annapolis Valley. One person drowned in Antigonish while swimming in a lake that swelled to about twice its normal size. In Newfoundland, rough seas capsized a few boats, causing two deaths, while two fishing stages were also destroyed. Overall, the extratropical remnants of this hurricane caused five fatalities in Atlantic Canada.[15]
A tropical storm moved northward into Acapulco in the middle of September. Its large area of disturbed weather organized in the Bay of Campeche and developed into a tropical storm on September 10 a short distance off the coast of Tabasco.[16] The storm initially moved westward, then turned to the north. It remained a minimal tropical storm for its entire lifetime, and after turning to the north west it made landfall near Brownsville, Texas, on September 13 with winds of 50mph (85km/h). The system weakened over Texas, and dissipated over northern Coahuila on September 14. Winds were generally minor from the storm, and tides were not much above normal. The storm resulted in heavy rainfall totaling 30.00in (762mm) at Broome, Texas, between September 15 and 17.[17] Anticipating further intensification, one bulletin from the local weather bureau recommended citizens on offshore islands to evacuate inland.[1]
A tropical storm was first observed about 140mi (225km) north of Anguilla on September 19. The storm moved northwestward and quickly attained hurricane status on September 20. After turning to the northeast, the hurricane reached a peak intensity of 105mph (165km/h) on September21 while located about 500mi (805km) southwest of Bermuda. It turned to the north and slowly weakened. A cold front turned the hurricane to the northeast, and the system became extratropical on September 25 a short time before making landfall on southern Nova Scotia. Hours after striking the providence, the extratropical remnant was absorbed by the approaching cold front while located over the Gulf of St. Lawrence.[9]
Rough seas offshore Nova Scotia capsized the ship Village Queen near Cape St. Marys, nearly drowning six fishermen. At least 13boats also sank in Newfoundland. The storm also produced rainfall as far west as Ontario, with crops and subway systems flooded in Ottawa.[18]
A tropical depression formed in the western Atlantic Ocean on September 25. It moved west-northwestward, making landfall on eastern Florida before entering the Gulf of Mexico on September 28. The depression turned to the northwest, and struck land near Apalachicola as a minimal system. It dissipated over land on October 1. The minimum central pressure in the depression was 1,006mbar (29.7inHg). The depression produced winds of up to 35mph (55km/h) in Tarpon Springs. Effects were minimal.[1]
An area of disturbed weather persisted across the northwestern Caribbean Sea in early October. It tracked northwestward over the Yucatán Peninsula, and subsequent to the development of a low-level circulation the system organized into a tropical storm on October 9 while located about 60mi (95km) northwest of the capital of Campeche. After moving northward, the storm turned sharply southward, and made landfall in northern Tabasco as a minimal tropical storm on October 10. The system quickly weakened over land, and dissipated over Chiapas on October 11.[9] The system dropped heavy rainfall across southeastern Mexico, though damage, if any, is unknown.[1]
Toward the end of November, a cold front was moving eastward across the central Atlantic Ocean. A broad low formed on November28, but it was not evident by two days later. Another low formed on December2 to the west-southwest of the Canary Islands, which was an occluded low. It moved to the west-northwest and became more tropical, finally transitioning into a tropical storm by December4. The transition to a tropical cyclone was determined on ships reporting gale-force winds near the center, although it is possible the system was a subtropical cyclone instead. On December6, the storm turned to the west-southwest and reached its peak winds of 65mph (100km/h). An approaching cold front caused the storm to become extratropical early on December7. After reaching a position to the northeast of the Lesser Antilles, the extratropical storm turned to the northwest on December10, later turning to the northeast on December14. A larger extratropical low absorbed the storm on December16.[19]
The 1961 Atlantic hurricane season was a very active Atlantic hurricane season, with an accumulated cyclone energy (ACE) total of 189, the highest since 1950 and until being surpassed by 1995. The season, however, was an average one in terms of named storms. The season featured eight hurricanes and a well above average number of five major hurricanes. It was previously thought that the season had a record-tying seven major hurricanes, before the Atlantic hurricane reanalysis project downgraded two storms in 2019. Two Category 5 hurricanes were seen in 1961, making it one of only eight Atlantic hurricane seasons to feature multiple Category 5 hurricanes in one season. The season started on June 15, and ended on November 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first system, an operationally unclassified tropical depression, formed offshore east Central Florida on June 10, but dissipated a few days later. Next, Hurricane Anna developed in the eastern Caribbean Sea near the Windward Islands on July 20. It brought minor damage to the islands in, as well as wind and flood impacts to Central America after striking Belize as a hurricane. Anna caused one death and about $300,000 (1961 USD) in damage. Activity went dormant for nearly a month and a half, until Hurricane Betsy developed on September 2. Betsy peaked as a Category 4 hurricane, but remained at sea and caused no impact.
The 1950 Atlantic hurricane season was the first year in the Atlantic hurricane database (HURDAT) that storms were given names in the Atlantic basin. Names were taken from the Joint Army/Navy Phonetic Alphabet, with the first named storm being designated "Able", the second "Baker", and so on. It was a very active season with sixteen tropical storms, with eleven of them developing into hurricanes. Six of these hurricanes were intense enough to be classified as major hurricanes—a denomination reserved for storms that attained sustained winds equivalent to a Category 3 or greater on the present-day Saffir–Simpson scale. One storm, the twelfth of the season, was unnamed and was originally excluded from the yearly summary, and three additional storms were discovered in re-analysis. The large quantity of strong storms during the year yielded, prior to modern reanalysis, what was the highest seasonal accumulated cyclone energy (ACE) of the 20th century in the Atlantic basin; 1950 held the seasonal ACE record until broken by the 1995 Atlantic hurricane season. However, later examination by researchers determined that several storms in the 1950 season were weaker than thought, leading to a lower ACE than assessed originally. This season also set the record for the most tropical storms, eight, in the month of October.
The 1951 Atlantic hurricane season was the first hurricane season in which tropical cyclones were officially named by the United States Weather Bureau. The season officially started on June 15, when the United States Weather Bureau began its daily monitoring for tropical cyclone activity; the season officially ended on November 15. It was the first year since 1937 in which no hurricanes made landfall on the United States; as Hurricane How was the only tropical storm to hit the nation, the season had the least tropical cyclone damage in the United States since the 1939 season. As in the 1950 season, names from the Joint Army/Navy Phonetic Alphabet were used to name storms this season.
The 1949 Atlantic hurricane season was the last season that tropical cyclones were not publicly labeled by the United States Weather Bureau. It officially began on June 15, and lasted until November 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first storm, a tropical depression, developed in the northern Gulf of Mexico on August 14. The final system, Tropical Storm Sixteen, dissipated in the southwestern Caribbean Sea on November 5. It was a fairly active season, featuring 16 tropical storms and seven hurricanes. Two of these strengthened into major hurricanes, which are Category 3 or higher on the Saffir–Simpson hurricane wind scale.
The 1942 Atlantic hurricane season was one of seven seasons to feature multiple hurricane landfalls in Texas. The season officially lasted from June 16, 1942, to October 31, 1942. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. A total of 11 tropical storms from 1943 are listed in the Atlantic hurricane database, with two additional tropical depressions. The first system of the year, a tropical depression, developed over the central Gulf of Mexico on June 3, while the last system, the Belize hurricane, dissipated over the Yucatán Peninsula on November 11. After the depression dissipated on June 3, the season remained dormant until the next system developed two months later. In mid-August, a hurricane struck Texas, causing about $790,000 (1942 USD) in damage.
The 1933 Atlantic hurricane season is the most active Atlantic hurricane season on record in terms of accumulated Cyclone Energy (ACE), with a total of 259. It also set a record for nameable tropical storms in a single season, 20, which stood until 2005, when there were 28 storms. The season ran for six months of 1933, with tropical cyclone development occurring as early as May and as late as November. A system was active for all but 13 days from June 28 to October 7.
The 1920 Atlantic hurricane season featured tropical storms and hurricanes only in the month of September. The first system, a hurricane, developed on September 7 while the last, a tropical depression, transitioned into an extratropical cyclone on October 27. Of note, four of the six cyclones co-existed with another tropical cyclone during the season.
The 1918 Atlantic hurricane season was inactive, with a total of six tropical storms developing, four of which intensified into hurricanes. Two of the season's hurricanes made Landfall in the United States, and one became a major hurricane, which is Category 3 or higher on the modern-day Saffir–Simpson scale. Additionally, there were four suspected tropical depressions, including one that began the season on June 19 and one that ended the season when it dissipated on October 19. The early 20th century lacked modern forecasting and documentation, and thus, the hurricane database from these years may be incomplete. Four previously unknown tropical cyclones were identified using records, including historical weather maps and ship reports, while information on the known storms was amended.
The 1913 Atlantic hurricane season was the third consecutive year with a tropical cyclone developing before June. The first system, a tropical depression, developed on May 5 while the last transitioned into an extratropical cyclone on October 30. Of note, the seventh and eighth cyclones existed simultaneously from August 30 to September 4.
The 1906 Atlantic hurricane season was an average season in terms of number of named storms, hurricanes, and major hurricanes. However, it's considered extremely active in terms of accumulated cyclone energy. It featured twelve tropical cyclones, eleven of which became storms, six became hurricanes and three became major hurricanes. The first storm of the season, a tropical storm in the northern Caribbean, formed on June 8; although it struck the United States, no major impacts were recorded. July saw a period of inactivity, with no known storms. However, in August, the streak of inactivity ended with two storms, including a powerful hurricane. September brought three storms, including a deadly hurricane, with catastrophic impacts in Pensacola and Mobile. October included three storms, with a powerful hurricane that killed over 200 people. The final storm of the season impacted Cuba in early November and dissipated on November 9. The season was quite deadly, with at least with 381 total recorded deaths.
The 1905 Atlantic hurricane season featured five known tropical cyclones, two of which made landfall in the United States. The first system was initially observed near the Windward Islands on September 6. The last system to dissipate, the fourth storm, transitioned into an extratropical cyclone on October 11, while located well southeast of Newfoundland. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Between October 5 and October 10, the fourth and fifth system existed simultaneously.
The 1903 Atlantic hurricane season featured seven hurricanes, the most in an Atlantic hurricane season since 1893. The first tropical cyclone was initially observed in the western Atlantic Ocean near Puerto Rico on July 21. The tenth and final system transitioned into an extratropical cyclone well northwest of the Azores on November 25. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Six of the ten tropical cyclones existed simultaneously.
The 1901 Atlantic hurricane season was the most active season without a major hurricane – tropical cyclones that reach at least Category 3 on the Saffir–Simpson hurricane wind scale – until 2013. The first system was initially observed in the northeastern Caribbean on June 11. The fourteenth and final system transitioned into an extratropical cyclone near Bermuda on November 5. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Eight of the fourteen tropical cyclones existed simultaneously.
The 1900 Atlantic hurricane season featured the Galveston hurricane, the deadliest natural disaster in the history of the United States. A total of 10 tropical cyclones formed, seven of which intensified into a tropical storm. Three of those made landfall in the United States. The first system was initially observed over the central Atlantic Ocean on January 17, while the final storm transitioned into an extratropical cyclone on October 28. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Every storm of the season except the seventh system existed simultaneously with another tropical cyclone.
The 1899 Atlantic hurricane season featured the longest-lasting tropical cyclone in the Atlantic basin on record. There were nine tropical storms, of which five became hurricanes. Two of those strengthened into major hurricanes, which are Category 3 or higher on the modern day Saffir–Simpson scale. The first system was initially observed in the northeastern Gulf of Mexico on June 26. The tenth and final system dissipated near Bermuda on November 10. These dates fall within the period with the most tropical cyclone activity in the Atlantic. In post-season analysis, two tropical cyclones that existed in October were added to HURDAT – the official Atlantic hurricane database. At one point during the season, September 3 through the following day, a set of three tropical cyclones existed simultaneously.
The 1897 Atlantic hurricane season was an inactive season, featuring only six known tropical cyclones, four of which made landfall. There were three hurricanes, none of which strengthened into major hurricanes, which are Category 3 or higher on the modern-day Saffir–Simpson hurricane wind scale. The first system was initially observed south of Cape Verde on August 31, an unusually late date. The storm was the strongest of the season, peaking as a Category 2 hurricane with winds of 100 mph (155 km/h). While located well north of the Azores, rough seas by the storm sunk a ship, killing all 45 crewmen. A second storm was first spotted in the Straits of Florida on September 10. It strengthened into a hurricane and tracked northwestward across the Gulf of Mexico, striking Louisiana shortly before dissipating on September 13. This storm caused 29 deaths and $150,000 (1897 USD) in damage.
The 1890 Atlantic hurricane season was among the least active Atlantic hurricane seasons on record. The first tropical cyclone of the season was initially observed on May 27 and the last storm, Hurricane Four, dissipated over Central America on November 1. These dates fall within the period with the most tropical cyclone activity in the Atlantic. The first storm moved slowly north-northwestward, bringing heavy rains and extensive flooding to Cuba, which caused at least three fatalities and at least $1 million (1890 USD) in damage. It dissipated in the Gulf of Mexico on May 29. Tropical cyclogenesis went dormant for nearly two and a half months, until another system was observed near the Windward Islands on August 18. It traversed the Caribbean Sea and Gulf of Mexico, grazing the Yucatan Peninsula and making landfall in Louisiana before dissipating on August 28. Impact from the storm was minimal.
The 1975 Pacific hurricane season officially started May 15, 1975, in the eastern Pacific, and June 1, 1975, in the central Pacific, and lasted until November 30, 1975. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeast Pacific Ocean.
The 1957 Pacific typhoon season has no official bounds; it ran year-round in 1957, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1924 Atlantic hurricane season featured the first officially recorded Category 5 hurricane, a tropical cyclone with maximum sustained winds exceeding 155 mph (249 km/h) on the modern-day Saffir–Simpson scale. The first system, Tropical Storm One, was first detected in the northwestern Caribbean Sea on June 18. The final system, an unnumbered tropical depression, dissipated on November 24. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Of the 13 tropical cyclones of the season, six existed simultaneously. The season was average with 11 tropical storms, five of which strengthened into hurricanes. Further, two of those five intensified into major hurricanes, which are Category 3 or higher on the Saffir–Simpson scale.
1 2 3 4 National Hurricane Center; Hurricane Research Division; Atlantic Oceanographic and Meteorological Laboratory (December 2012). "Atlantic hurricane best track (HURDAT) Meta Data, 1936". United States National Oceanic and Atmospheric Administration's Office of Oceanic & Atmospheric Research. Archived from the original on May 12, 2014. Retrieved 2012-12-21.
↑ National Hurricane Center; Hurricane Research Division; Atlantic Oceanographic and Meteorological Laboratory (April 2012). "Chronological List of All Continental United States Hurricanes: 1851–2011". United States National Oceanic and Atmospheric Administration's Office of Oceanic & Atmospheric Research. Archived from the original on February 10, 2014. Retrieved 2012-05-14.
↑ David Roth (2000). "Texas Hurricane History". National Oceanic and Atmospheric Administration. Archived from the original on June 13, 2007. Retrieved September 10, 2006.
↑ "Storm to Diminish in Intensity". Alexandria Daily Town Talk. Vol.54, no.114. Alexandria, Louisiana. Associated Press. July 27, 1936. p.1. Retrieved January 27, 2020.
↑ "Hurricane Warning Issued To Mexico". The Monitor. McAllen, Texas. Associated Press. August 13, 1936. p.1. Retrieved October 5, 2021– via Newspapers.com.
↑ Wakefield and Blacksburg, Virginia National Weather Service (2006). "Virginia Hurricane History". Archived from the original on September 4, 2005. Retrieved November 27, 2006.
↑ David Roth & Hugh Cobb (2001). "Virginia Hurricane History 1900–1949". National Oceanic and Atmospheric Administration. Archived from the original on November 16, 2006. Retrieved November 27, 2006.
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