1876 Atlantic hurricane season | |
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Seasonal boundaries | |
First system formed | Before September 9, 1876 |
Last system dissipated | October 23, 1876 |
Strongest storm | |
Name | Five |
• Maximum winds | 115 mph (185 km/h) (1-minute sustained) |
• Lowest pressure | 958 mbar (hPa; 28.29 inHg) |
Seasonal statistics | |
Total storms | 5 |
Hurricanes | 4 |
Major hurricanes (Cat. 3+) | 2 |
Total fatalities | 52 |
Total damage | $5.03 million (1876 USD) |
The 1876 Atlantic hurricane season featured the first hurricane landfall in North Carolina since 1861. Overall, the season was relatively quiet, with five tropical storms developing. Four of these became a hurricane, of which two intensified into major hurricanes. [nb 1] However, due to the absence of remote-sensing satellite and other technology, only storms that affected populated land areas or encountered ships at sea were recorded; therefore, the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated. [2]
Of the known 1876 cyclones, both the first and fourth systems were first documented in 1995 by José Fernández-Partagás and Henry Diaz. They also proposed large changes to the known tracks of the second and fifth storms. [3] The track and start position of the fifth system was further amended in 2003 by the Atlantic hurricane reanalysis project, which did not add any storms to the official hurricane database (HURDAT). [4] However, climate researcher Michael Chenoweth authored a reanalysis study, published in 2014, which concluded that the 1876 season featured a total of 12 tropical cyclones. This included the removal of the third system due to a lack of information and the addition of eight previously undocumented storms. Chenoweth also proposed some alterations to the track and intensity of each storm, including a significant extension of the track and duration of the first cyclone. However, these changes have yet to be incorporated into HURDAT.
The season's first known cyclone was first observed between Bermuda and Nova Scotia on September 9. It transitioned into an extratropical cyclone two days later. On September 12, the track of the next storm begins as a hurricane just east of the Leeward Islands. The system crossed the Lesser and Greater Antilles, causing particularly severe impacts on Puerto Rico, including at least 19 deaths. After striking North Carolina on September 17, the storm killed people in the state, all due to drowning. The hurricane and its remnants then impacted the Northeastern United States, with $30,000 (1876 USD) in damage on the barrier islands of Cape May County, New Jersey, alone. [nb 2] In early October, the fourth storm struck Nicaragua, rendering about $5 million in damage and leaving approximately 20 deaths. Later that month, the fifth and final known storm caused damage in the Cayman Islands, Cuba, and Florida prior to being last noted just northeast of Bermuda on October 23. Overall, the cyclones of the 1876 season left 52 fatalities and more than $5.03 million in damage.
The Atlantic hurricane database (HURDAT) officially recognizes five tropical cyclones for the 1876 season. Four storms attained hurricane status, with winds of 75 mph (120 km/h) or greater. The second and fourth hurricanes both peaked with maximum sustained winds up to 115 mph (185 km/h). [5] Thus, both of these storms intensified into a major hurricane. [1] In 1995, reanalysis by José Fernández-Partagás and Henry Diaz led to the addition of the first and fourth systems in HURDAT. While the Atlantic hurricane reanalysis project did not add any new cyclones during their reanalysis in 2003, [4] climate researcher Michael Chenoweth concluded that the 1876 season had a total of 12 storms in a reanalysis study published in 2014. This included the removal of the third system and the addition of eight previously undocumented cyclones. However, Chenoweth's proposals have yet to be incorporated into HURDAT. [6]
The first storm of the season, initially observed by three ships on September 9, was a hurricane that existed for two days offshore Atlantic Canada. Three other cyclones developed in September. The season's second storm, also known as the San Felipe hurricane, was first observed near the Windward Islands on September 12 and struck Puerto Rico as a Category 3 hurricane before crossing Hispaniola and Cuba. It then turned north-northeastward and made landfall in North Carolina, [5] becoming the first to strike the coast of that state since 1861. [7] [nb 3] The cyclone continued through the interior of the United States until dissipating near Cape Cod on September 19. [5] Officially, this storm caused 52 deaths and more than $30,000 in damage, as the latter only includes Cape May County, New Jersey. [3] [8] [9] The season's fourth cyclone and third to form in the month of September struck Nicaragua in early October, leaving about $5 million in damage and about 20 deaths. [10] Later, the fifth and final known storm impacted the Cayman Islands, Cuba, and Florida before being last detected to the northeast of Bermuda on October 23. [3] Overall, the cyclones of the 1876 season are known to have collectively caused at least 52 deaths and more than $5.03 million in damage. [3] [8] [9] [10]
The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 57, the second lowest total of the 1870s decade. 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 higher 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 mph (63 km/h), which is the threshold for tropical storm intensity. Thus, tropical depressions are not included here. [1]
Category 1 hurricane (SSHWS) | |
Duration | September 9 – September 11 |
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Peak intensity | 90 mph (150 km/h) (1-min); 970 mbar (hPa) |
On September 9, the ships Annie and Lilly, Alfred, and Astor each encountered this storm south of Atlantic Canada. [11] Because the Alfred observed a barometric pressure of 970 mbar (29 inHg), HURDAT begins the track of this cyclone as a hurricane with winds of 90 mph (150 km/h) about halfway between Bermuda and Nova Scotia. [4] [5] The hurricane did not strengthen and began to gradually weaken as it moved to the south of Newfoundland. It weakened to a tropical storm early on September 11 and transitioned into an extratropical cyclone several hours later. [5]
Climate researcher Michael Chenoweth theorized that this storm began as a tropical depression near the Cabo Verde Islands on September 2. Chenoweth's study, published in 2014, notes that the cyclone intensified into a tropical storm by the following day and moved generally northwestward until September 7. Additionally, Chenoweth concluded that it did not attain hurricane status. [6]
Category 3 hurricane (SSHWS) | |
Duration | September 12 – September 19 |
---|---|
Peak intensity | 115 mph (185 km/h) (1-min); 980 mbar (hPa) |
Hurricane San Felipe of 1876
While the bark Mary M. Williams reportedly encountered this storm before September 12, the official track for this system begins on that day due to the system's close proximity to the Lesser Antilles, which allowed more observations to confirm its existence. [3] Considered a hurricane at the beginning of its track, the storm moved generally westward and passed either or over Anguilla, Saint Barthélemy, and Saint Martin late on September 12. By early the next day, the cyclone briefly intensified into a Category 3 hurricane, peaking with winds of 115 mph (185 km/h), several hours before striking Puerto Rico between Yabucoa and Humacao. The system moved west-northwestward across the Mona Passage and struck the Dominican Republic, weakening to a tropical storm on September 14 as it traversed Hispaniola. Thereafter, the storm briefly re-attained hurricane status while crossing the Windward Passage early on the next day and soon made landfall in Cuba near San Antonio del Sur. Weakening to a tropical storm, the cyclone continued west-northwestward until turning northward over the central part of the island, barely avoiding Florida on September 16. The storm became a hurricane again early on September 17, several hours before striking near Wilmington, North Carolina. The storm moved parabolically across the interior of the United States, dissipating on September 19 near Cape Cod, Massachusetts. [5]
A newspaper on Saint Thomas noted that many homes lost their roofs and fences, but that impact from this storm was less than during other storms. Saint Croix, however, reportedly experienced its worst hurricane in 50 years, while Saint Kitts also suffered considerably. [12] In Puerto Rico, the storm was remembered as the "San Felipe Hurricane" because it struck on September 13, the feast day of Saint Philip. Exactly 52 years later, Puerto Rico was struck by Hurricane San Felipe Segundo, a much more destructive and powerful cyclone. The lowest pressure during the 1876 storm was 989 mb (29.20 inHg) at San Juan, [13] where the storm left few homes undamaged. Overflowing rivers and the storm itself carried away many bridges and caused significant losses to coffee, rice, and sugarcane estates. [14] A total of 19 deaths were reported, but historians suspected the Spanish government withheld the actual damage and death toll data for Puerto Rico. [13] At least 13 drownings occurred in North Carolina, two in Onslow County and eleven others after the Rebecca Clyde sank at Portsmouth. [3] [8] Many other ships capsized along the coast of North Carolina. Flooding, damage to buildings, and uprooted trees were reported in Wilmington. [15] The cyclone impacted several other states, particularly New Jersey, with The New York Times declaring it the "one of the most severe ever known along the coast of New Jersey." Damage on the barrier islands of Cape May County reached $30,000. [9]
Chenoweth extended the track of this system back two days, with a tropical storm east of the Lesser Antilles, and proposed that the cyclone did not weaken to a tropical storm despite its passage over Puerto Rico, Hispaniola, and Cuba. [6]
Tropical storm (SSHWS) | |
Duration | September 16 – September 18 |
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Peak intensity | 60 mph (95 km/h) (1-min); |
The track of the season's third cyclone begins about 270 mi (435 km) east-northeast of the Lesser Antilles. It headed north, peaking with winds of 60 mph (95 km/h) and passing well to the east of Bermuda. The system apparently dissipated on September 18. [5] Chenoweth could not confirm the existence of this storm, noting "Insufficient supporting evidence from other neighboring data sources". [6]
Category 2 hurricane (SSHWS) | |
Duration | September 29 – October 5 |
---|---|
Peak intensity | 105 mph (165 km/h) (1-min); |
The RMS Nile first observed a tropical storm east of Martinique on September 29. [3] By early on October 1, the storm strengthened into a hurricane as it passed near the Netherlands Antilles. It later peaked as a Category 2 hurricane before making landfall just south of Bluefields, Nicaragua, late on October 3. The system weakened to a tropical storm early on the next day, but remained a tropical cyclone due to crossing relatively flat terrain. Several hours later, the storm reached the Pacific Ocean, but dissipated on October 5. [5]
The cyclone severely damaged parts of Central America, inundating the Nicaraguan capital of Managua with floodwaters. People climbed rooftops to evade the floodwaters. On the east coast of the country, 300 homes were destroyed at Bluefields. [3] The hurricane also demolished some 500 homes in Managua. Overall, the cyclone left approximately $2 million in damage to property and $3 million to coffee crops. About 20 deaths occurred. [10] The ship Costa Rica, in the eastern Pacific and bound for Acapulco on October 4, lost her hurricane-deck as well as the head of her main mast, main topmast, and gaff. She also lost one of her quarter boats and experienced a wind shift at 2030 UTC. [16]
The 2014 study by Chenoweth proposed a much slower-moving system, which began near Tobago on September 24. Initially moving west-northwestward, the storm begins a west-southwestward trajectory two days later. Additionally, the cyclone attains a much stronger intensity, peaking with winds of 150 mph (240 km/h), equivalent to Category 4 status. [6]
Category 3 hurricane (SSHWS) | |
Duration | October 12 – October 23 |
---|---|
Peak intensity | 115 mph (185 km/h) (1-min); 958 mbar (hPa) |
The Cuba-South Florida Hurricane of 1876
A tropical storm was discovered north of Panama on October 12. The storm moved very slowly and generally northward. It became a hurricane early on October 17 and passed just east of Grand Cayman. [17] It attained a peak intensity of 115 mph (185 km/h) just before making landfall on Bejucal in western Cuba, where the barometer dropped as low as 958 mbar (28.3 inHg) on October 19. [18] The calm center of the storm passed over the capital Havana and then turned northeastward as it entered the Straits of Florida. [3] Just before 00:00 UTC on October 20, the eye of the cyclone struck Key West, Florida. [3] About six hours later, early on October 20, the hurricane made landfall on the mainland near Chokoloskee with winds of 105 mph (165 km/h) and emerged into the Atlantic near Sebastian around 12:00 UTC. [3] In passing over Eau Gallie near Melbourne, the calm eye lasted about four hours between 08:30–12:30 UTC. [19] The cyclone later passed north of Bermuda before dissipating on October 23. [5]
On Grand Cayman, where west winds occurred during the closest approach of the cyclone, severe damage and the destruction of 170 houses was reported. [20] The storm disrupted communications via telegram across the island of Cuba, [21] although the most significant damage occurred in Havana and Matanzas provinces. [3] The city of Havana reported significant damage to several buildings. [21] In South Florida, the hurricane produced tides of 8 to 10 ft (2.4 to 3.0 m) on Biscayne Bay, but local ships rode out the storm in a natural anchorage called Hurricane Harbor, on the west side of Key Biscayne. [22] The bark Three Sisters was wrecked on Virginia Key, her cargo of lumber being salvaged by local residents. [22] The storm flooded the islands on Biscayne Bay and destroyed many structures. [23] On the Lake Worth Lagoon, the cyclone snapped or blew down large mastic and banyan trees, each more than 3 ft (0.9 m) in diameter and believed to have been hundreds of years old. All vegetation was stripped of foliage and branches were downed, while settlers' furniture was blown away. After the storm, the Atlantic Ocean appeared yellowish-brown due to silt, and numerous fish and sea mammals, including porpoises, were found beached. [24] The settlement that later became Palm Beach was destroyed. [25] Two decades later in 1896, the storm was still noted by settlers as among the worst ever in South Florida. [23] Bermuda recorded gale-force winds and a pressure of 29.30 inHg (992 mb). [3]
Chenoweth began the track for this system farther south and two days earlier, October 10. The storm intensified into a hurricane on October 12, several days before HURDAT indicates. Additionally, the study proposed that the cyclone weakened to a tropical storm slightly earlier on October 23 and transitioned into an extratropical cyclone that day. [6]
A reanalysis study proposed eight additional tropical cyclones during the 1876 season, including five before the first system currently listed in HURDAT. Chenoweth's first unofficial storm begins over the eastern Caribbean Sea on July 17. Moving west-northwestward, the system remained just south of the Greater Antilles as it intensified into a hurricane. Two landfalls at hurricane intensity occurred in Mexico – first on the Yucatán Peninsula and then in the state of Veracruz – before the storm dissipated near Mexico City on July 23. About a week later, on July 30, a tropical depression formed approximately halfway between Bermuda and South Carolina. Trekking to the northwest, the cyclone approached North Carolina on August 1 but then turned northeastward. Chenoweth theorized that the storm briefly attained hurricane status on the following day before weakening to a tropical depression and dissipating roughly halfway between Bermuda and Nova Scotia. The next unofficial system began about halfway between Bermuda and Puerto Rico on August 13. Moving generally north-northwestward, the depression dissipated just west of Bermuda three days later. Chenoweth concluded that the cyclone briefly attained hurricane status on August 14. A third unofficial system formed on August 17 near Barbados. The storm moved generally northwestward and passed near Martinique on the following day. It later crossed Hispaniola and Cuba before becoming extratropical over the Straits of Florida on August 25. That same day, another storm formed about halfway between Bermuda and Puerto Rico. Moving mostly north-northeastward throughout its duration, the storm held hurricane status from August 26 to August 29 and was last noted east of Newfoundland on August 30. [6]
Chenoweth proposed that another storm developed roughly halfway between the Capo Verde Islands and the Leeward Islands on September 12. The cyclone initially moved north-northwestward to northwestward before turning to the northeast three days later. On September 18, the system became extratropical just north of the Azores. Chenoweth initiated the track of another storm just east of the Windward Islands on September 29. Moving north-northwestward, the cyclone passed just west of Barbados that day and briefly attained hurricane status. The storm then turned westward and struck Martinique early on September 30 before curving southwest over the Caribbean. On October 1, the system weakened to a tropical depression and dissipated near La Orchila Island. The track of the final unofficial begins as a hurricane over the central Atlantic on November 7. After initially trekking to the northwest, the storm turned northeastward by the next day. The hurricane weakened to a tropical storm early on November 10 and was last noted southwest of the Azores on November 12. [6]
This is a table of all of the known storms that formed in the 1876 Atlantic hurricane season. It includes their known duration (within the basin), areas affected, damages, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all of the damage figures are in 1876 USD.
Saffir–Simpson scale | ||||||
TD | TS | C1 | C2 | C3 | C4 | C5 |
Storm name | Dates active | Storm category at peak intensity | Max 1-min wind mph (km/h) | Min. press. (mbar) | Areas affected | Damage (USD) | Deaths | Ref(s) | ||
---|---|---|---|---|---|---|---|---|---|---|
One | September 9–11 | Category 1 hurricane | 90 (150) | 970 | None | None | None | |||
Two | September 12–19 | Category 3 hurricane | 115 (185) | 980 | Lesser Antilles (Puerto Rico), Greater Antilles (Dominican Republic, Cuba), Florida, the Bahamas, North Carolina, Virginia, Northeastern United States | >$30,000 | 32 | [3] [8] [9] | ||
Three | September 16–18 | Tropical storm | 60 (95) | Unknown | None | None | None | |||
Four | September 29 – October 5 | Category 2 hurricane | 105 (165) | Unknown | Lesser Antilles, Nicaragua | $5 million | 20 | [10] | ||
Five | October 12–23 | Category 3 hurricane | 115 (185) | 958 | Greater Antilles (Cuba), Florida, Bermuda | Unknown | Unknown | |||
Season aggregates | ||||||||||
5 systems | September 9 – October 23 | 115 (185) | 958 | >$5.03 million | 52 |
The 1921 Atlantic hurricane season was an active hurricane season, with 12 tropical cyclones forming. Among them, seven became tropical storms, of which five strengthened into hurricanes. Furthermore, two of these strengthened into a major hurricane, Category 3 or higher on the modern-day Saffir–Simpson hurricane wind scale, the most since the 1917 season. The first system, a tropical depression, developed on June 1, while the last, a tropical storm, dissipated on November 25. Of note, three tropical cyclones co-existed with another during the season.
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 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 1898 Atlantic hurricane season marked the beginning of the Weather Bureau operating a network of observation posts across the Caribbean Sea to track tropical cyclones, established primarily due to the onset of the Spanish–American War. A total of eleven tropical storms formed, five of which intensified into a hurricane, according to HURDAT, the National Hurricane Center's official database. Further, one cyclone strengthened into a major hurricane. However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated. The first system was initially observed on August 2 near West End in the Bahamas, while the eleventh and final storm dissipated on November 4 over the Mexican state of Veracruz.
The 1895 Atlantic hurricane season was a fairly inactive one, featuring only six known tropical cyclones, although each of them made landfall. Of those six systems, only two intensified a hurricane, while none of those strengthened into a major hurricane. However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.
The 1893 Atlantic hurricane season ran through the summer and the first half of fall in 1893. The 1893 season was fairly active, with 12 tropical storms forming, 10 of which became hurricanes. Of those, five became major hurricanes. This season proved to be a very deadly season, with two different hurricanes each causing over 2,000 deaths in the United States; at the time, the season was the deadliest in U.S. history. The season was one of two seasons on record to see four Atlantic hurricanes active simultaneously, along with the 1998 Atlantic hurricane season. Additionally, August 15, 1893 was the only time since the advent of modern record keeping that three storms have formed on the same day until 2020 saw Wilfred, Alpha, and Beta forming on the same day; and for the first time, there were two high-intensity hurricanes simultaneously in one month of August, and this was not repeated until the year 2023.
The 1892 Atlantic hurricane season included the last tropical cyclone on record to pass through the Cabo Verde Islands at hurricane intensity until 2015. A total of nine tropical storms developed, five of which strengthened into a hurricane, though none of them became a major hurricane. However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated. Three tropical storms made landfall on the United States.
The 1891 Atlantic hurricane season began during the summer and ran through the late fall of 1891. The season had ten tropical cyclones. Seven of these became hurricanes; one becoming a major Category 3 hurricane.
The 1889 Atlantic hurricane season ran through the summer and the first half of fall in 1889. In the 1889 Atlantic season there were nine tropical storms and six hurricanes. However, due to scarce technology and the fact that only storms that affected populated land or ships were recorded, the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.
The 1880 Atlantic hurricane season ran through the summer and fall of 1880. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1880 Atlantic season there were two tropical storms, seven hurricanes, and two major hurricanes (Category 3+). However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated. Of the known 1880 cyclones, Hurricane Six was first documented in 1995 by José Fernández-Partagás and Henry Díaz. They also proposed large changes to the known tracks of several other storms for this year and 're-instated' Hurricane Ten to the database. A preliminary reanalysis by Michael Chenoweth, published in 2014, found thirteen storms, nine hurricanes, and four major hurricanes.
The 1887 Atlantic hurricane season was the most active Atlantic hurricane season on record at the time in terms of the number of known tropical storms that had formed, with 19. This total has since been equaled or surpassed multiple times. The 1887 season featured five off-season storms, with tropical activity occurring as early as May, and as late as December. Eleven of the season's storms attained hurricane status, while two of those became major hurricanes. It is also worthy of note that the volume of recorded activity was documented largely without the benefit of modern technology. Consequently, tropical cyclones during this era that did not approach populated areas or shipping lanes, especially if they were relatively weak and of short duration, may have remained undetected. Thus, historical data on tropical cyclones from this period may not be comprehensive, with an undercount bias of zero to four per year between 1886 and 1910 estimated. The first system was initially observed on May 15 near Bermuda, while the final storm dissipated on December 12 over Costa Rica.
The 1870 Atlantic hurricane season marked the beginning of Father Benito Viñes investigating tropical cyclones, inspired by two hurricanes that devastated Cuba that year; Viñes consequently became a pioneer in studying and forecasting such storms. The season featured 11 known tropical cyclones, 10 of which became a hurricane, while 2 of those intensified into major hurricanes. However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.
The 1885 Atlantic hurricane season ran through the summer and the first half of fall in 1885. This is the period of each year when most tropical cyclones form in the Atlantic basin. In 1885 there were two tropical storms and six hurricanes in the Atlantic basin. However, in the absence of modern satellite monitoring and remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.
The 1883 Atlantic hurricane season ran through the summer and the first half of fall in 1883. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1883 Atlantic season there was one tropical storm, one Category 1 hurricane, and two major hurricanes. However, in the absence of modern satellite monitoring and remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.
The 1851 Atlantic hurricane season was the first Atlantic hurricane season to be included in the official Atlantic tropical cyclone record. Six known tropical cyclones occurred during the season, the earliest of which formed on June 25 and the latest of which dissipated on October 19. These dates fall within the range of most Atlantic tropical cyclone activity. None of the cyclones existed simultaneously with another. Three of the six storms only have a single point in their track known.
The 1881 Atlantic hurricane season ran through the summer and early fall of 1881. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1881 Atlantic season there were three tropical storms and four hurricanes, none of which became major hurricanes. However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated. Of the known 1881 cyclones, Hurricane Three and Tropical Storm Seven were both first documented in 1996 by Jose Fernandez-Partagas and Henry Diaz. They also proposed changes to the known tracks of Hurricane Four and Hurricane Five.
The 1854 Atlantic hurricane season featured five known tropical cyclones, three of which made landfall in the United States. At one time, another was believed to have existed near Galveston, Texas in September, but HURDAT – the official Atlantic hurricane database – now excludes this system. The first system, Hurricane One, was initially observed on June 25. The final storm, Hurricane Five, was last observed on October 22. These dates fall within the period with the most tropical cyclone activity in the Atlantic. No tropical cyclones during this season existed simultaneously. One tropical cyclone has a single known point in its track due to a sparsity of data.
The 1877 Atlantic hurricane season lasted from mid-summer to late-fall. Records show that in 1877 there were eight cyclones, of which five were tropical storms and three were hurricanes, one of which became a major hurricane. However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.
The 1874 Atlantic hurricane season was a relatively inactive one, in which seven tropical cyclones developed. Four storms intensified into hurricanes, but none attained major hurricane status. However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.
The 1873 Atlantic hurricane season was quiet, featuring only five known tropical cyclones, but all of them made landfall, causing significant impacts in some areas of the basin. Of these five systems, three intensified into a hurricane, while two of those attained major hurricane status. However, in the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.