1889 Atlantic hurricane season | |
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Seasonal boundaries | |
First system formed | May 16, 1889 |
Last system dissipated | October 7, 1889 |
Strongest storm | |
Name | Six |
• Maximum winds | 110 mph (175 km/h) (1-minute sustained) |
Seasonal statistics | |
Total storms | 9 |
Hurricanes | 6 |
Major hurricanes (Cat. 3+) | 0 |
Total fatalities | 40 |
Total damage | Unknown |
The 1889 Atlantic hurricane season was a relatively quiet season, with nine tropical storms and six hurricanes and no major 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. [1]
Category 1 hurricane (SSHWS) | |
Duration | May 16 – May 21 |
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Peak intensity | 80 mph (130 km/h) (1-min); |
Based on the Monthly Weather Review reporting a disturbance of "moderate intensity" to the north of the Lesser Antilles beginning on May 16, [2] the Atlantic hurricane database initiates the track for this system on that date about 190 mi (310 km) north of the British Virgin Islands. The cyclone strengthened slightly but remained a tropical storm for the next few days as it headed northwestward, until turning northeastward by May 20. Several hours later, the storm intensified into a hurricane and reached sustained winds of 80 mph (130 km/h), [3] based on the schooner Joseph W. Fish observing sustained winds of 58 mph (93 km/h) and another ship recording an unspecific hurricane-force sustained wind speed on the following day. [4] However, the system weakened to a tropical storm early on May 21 and soon transitioned into an extratropical cyclone about 270 mi (435 km) east of Nags Head, North Carolina. [3]
This cyclone was the first May hurricane on record in the Atlantic basin, and remains one of only four such systems known today. [5] Climate research Michael Chenoweth's 2014 study indicates that this system developed as a tropical depression just north of the Mona Passage on May 16. Other significant changes include that storm intensifying into a hurricane on May 21, as opposed to becoming extratropical that day, a transition that instead occurred on May 22. The extratropical remnants later struck Nova Scotia. [6]
Category 1 hurricane (SSHWS) | |
Duration | June 15 – June 20 |
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Peak intensity | 75 mph (120 km/h) (1-min); |
Maritime observations indicated the presence of a tropical storm over the northwestern Caribbean as early as June 15. [2] Moving north-northwestward, the cyclone struck the Guanahacabibes Peninsula of Cuba several hours later, likely as a minimal hurricane with sustained winds of 75 mph (120 km/h), [3] according to a study of wind damage conducted by meteorologist Ramón Pérez Suárez in 2000. [4] However, the hurricane weakened back to a tropical storm shortly after reaching the Gulf of Mexico on June 16. Gradually curving northeastward on June 17, the system made landfall near Cedar Key, Florida, with winds of 50 mph (85 km/h) around 14:00 UTC. After emerging into the Atlantic from the First Coast on the following day, the system remained closely offshore Georgia, South Carolina, and North Carolina. The cyclone was last noted on June 20 about 115 mi (185 km) southwest of Sable Island, Nova Scotia. [3]
Chenoweth's study suggests that the storm did not strike Cuba and instead moved through the Yucatán Channel before striking Florida farther south, near present-day Sarasota. [6] Heavy rains fell over western Cuba, inundating many streets. Walls and house collapsed, particularly in Batabanó and the Vuelta Abajo region. [7] Several vessels also capsized. [2] : 25 The Daily Inter Ocean noted that no deaths occurred, [7] but Simón Sarasola reported that "lives were lost". Although the highest recorded sustained wind speed in Florida reached only 43 mph (69 km/h) at Cedar Key, [2] : 25 heavy precipitation fell across the state, causing several washouts along the South Florida Railroad. Additionally, a tornado in Lake Mary downed some trees and destroyed a large packinghouse. [8]
Category 1 hurricane (SSHWS) | |
Duration | August 19 – August 28 |
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Peak intensity | 80 mph (130 km/h) (1-min); ≤996 mbar (hPa) |
Land-based weather stations first reported this storm about 100 mi (160 km) south of the Dominican Republic on August 19. [2] [3] Several hours later, the cyclone made landfall in the country near Baní with winds of 60 mph (95 km/h). [3] Santo Domingo observed a barometric pressure of 996 mbar (29.4 inHg). Due to moving across rugged terrain, the system likely weakened to a tropical depression, but re-intensified into a tropical storm after emerging into the Atlantic near on August 20. The storm then passed through the southeastern Bahamas and Turks and Caicos Islands early the next day while moving northwestward. By August 24, the cyclone curved northeastward while well offshore the East Coast of the United States. [3] Based on the Monthly Weather Review noting that various ships recorded hurricane-force winds, the system intensified into a hurricane on August 26 and peaked with winds of 80 mph (130 km/h). Turning northward, the hurricane began weakening on August 28, falling to tropical storm intensity before being last noted approximately 160 mi (260 km) east-southeast of Atlantic City, New Jersey. [3]
Chenoweth could not confirm the existence of this cyclone, citing "unreliable" reports from the Dominican Republic "and absence of evidence from daily weather map series". [6] In the Greater Antilles, the storm caused falling barometric pressures and increased wind speeds from the Dominican Republic to as far west as Havana, Cuba. [2] : 26 Santo Domingo in the former recorded sustained winds of 60 mph (95 km/h). [9] The cyclone and its remnants produced gales along the coast of the Mid-Atlantic and New England. [10] On August 29, sustained winds reached 40 mph (64 km/h) in Asbury Park, New Jersey. [9]
Category 2 hurricane (SSHWS) | |
Duration | September 1 – September 12 |
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Peak intensity | 105 mph (165 km/h) (1-min); ≤981 mbar (hPa) |
Hurricane San Martín of 1889
A tropical storm was first reported about 300 mi (485 km) east-southeast of Barbados on September 1. Moving northwestward, the cyclone strengthened into a hurricane on the next day, shortly before striking Guadeloupe. The storm intensified into a Category 2 hurricane on the modern-day Saffir–Simpson scale over the Anegada Passage on September 3, [3] based on Saint Thomas observing a barometric pressure of 981 mbar (29.0 inHg). [2] [4] Shortly thereafter, the cyclone crossed over the Virgin Islands and re-emerged into the Atlantic. Beginning on September 5, the storm switched course a few times, before resuming its original northwestward motion by September 7. As the cyclone approached the Northeastern United States, it slowly weakened, falling to tropical storm intensity by September 11. The system then turned southwestward and was last noted late the next day about 80 mi (130 km) east-northeast of Virginia Beach, Virginia. [3] Chenoweth proposed that this storm moved in a similar trajectory to that shown in HURDAT through September 5, when it instead turned north-northwestward. The cyclone also became more intense, holding major hurricane status from then until September 7. Chenoweth's study also indicates that the system persisted until late on September 14, hours after making landfall near present-day Sandbridge, Virginia, as a tropical storm. [6]
Barbados, Montserrat, and Saint Lucia reported heavy rains but little damage. However, torrential precipitation on Martinique flooded Lamentin and Rivière-Salée. Rough seas capsized a schooner and damaged two others. On Guadeloupe, floodwaters inundated Grande-Terre, carried away a few bridges, and damaged numerous roads. Several homes, plantations, and fences suffered damage on Barbuda. Crops and vessels on Saint Kitts but not infrastructure were significantly impacted. The hurricane damaged many homes, plantations, and vessels in the Virgin Islands, particularly on Saint Thomas and Tortola. [11] Winds of 48 mph (77 km/h) were measured on Puerto Rico. [12] In North Carolina, the northern half of the coast experienced rough seas, including cutting a new inlet at Nags Head. Winds downed communication wires to Hatteras. [13] Farther north, abnormally high tides and severe gales were reported from Virginia to New York. In the former, the cyclone flooded low-lying areas and wharves, ruined crops, carried away bridges, and toppled telegraph wires. A steamship was beached near Cape Henry, causing almost $12,000 in damage. [14] In Delaware, rough seas washed away a telegraph station, damaged a marine hospital, and flooded a life-saving station 40 ft (12 m) above high-water at Lewes. Nearby, abnormally high tides forced 200 people to flee Hugheyville. Along the coast of Delaware, the hurricane wrecked or beached 31 vessels, leading to 40 fatalities. Severe damage occurred to crops and fruit trees in the Egg Harbor City area of New Jersey. [2] : 29 A few cities in the Northeastern United States reported sustained tropical storm-force winds. [15] Overall, the hurricane caused nearly $2.36 million in damage. [2] : 29
Category 1 hurricane (SSHWS) | |
Duration | September 2 – September 11 |
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Peak intensity | 80 mph (130 km/h) (1-min); |
Meteorologist Charles J. Mitchell noted in 1924 that this system was first observed about halfway between the Cabo Verde Islands and the Lesser Antilles on September 2. The storm travelled to the northwest and increased in strength, reaching wind speeds of 60 mph (95 km/h) by September 4. The storm continued at that intensity on the same track for a further two days. The cyclones became a Category 1 hurricane as it gradually began curving northeastward on September 7, [3] based on the Monthly Weather Review noting that ships reported a disturbance of "great violence". [2] [4] By September 8, the storm turned eastward and then to the northeast on September 10. Weakening to a tropical storm on September 11, the cyclone passed through the Azores and was last noted several hours later. [3] The study by Chenoweth extended the storm's duration back to September 1. Later, Chenoweth also shifted the track to the west of the Azores and added an extratropical transition on September 10. [6]
Category 2 hurricane (SSHWS) | |
Duration | September 12 – September 25 |
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Peak intensity | 110 mph (175 km/h) (1-min); 982 mbar (hPa) |
Guadeloupe observed stormy conditions on September 12. [2] : 33 Consequently, the track for this system begins just east of the Leeward Islands that day. After passing between Guadeloupe and Dominica later on September 12, the cyclone moved west-northwestward to westward across the Caribbean. By September 17, the storm intensified into a hurricane over the northwestward Caribbean, [3] based on conditions reported by the steamer Mascotte. [2] : 33 The system strengthened further, likely to a strong Category 2 hurricane prior to making landfall in Mexico near Felipe Carrillo Puerto, Quintana Roo, several hours later. Late on September 18, the storm emerged into the Gulf of Mexico near Campeche after weakening to a tropical storm. However, the cyclone quickly re-gained hurricane status and curved northward on September 19. [3] The hurricane turned northeastward by September 22 and then made landfall near Buras, Louisiana, as a Category 1 hurricane with a barometric pressure of 982 mbar (29.0 inHg). [3] [4] Later on September 23, the system struck near Gulf Shores, Alabama, likely as a strong tropical storm. After crossing the Southeastern United States, the storm emerged into the Atlantic from the Delmarva Peninsula early on September 25 and crossed far eastern Massachusetts before becoming extratropical over the Gulf of Maine. [3]
The 2014 study by Chenoweth proposed that this storm did not pass through the Lesser Antilles and instead formed on September 14 near La Blanquilla Island. More intensification occurred than shown in HURDAT, with the cyclone holding major hurricane status for about 18 hours. The storm also underwent extratropical transition earlier, on September 24 over North Carolina. [6]
Only minor impacts occurred in the Lesser Antilles. Heavy rains overflowed a few rivers on Martinique, causing flooding at Les Anses-d'Arlet. [16] : 3 However, this precipitation may have been as a result of a low-pressure area unrelated to the cyclone. [16] : 4 In Mexico, the states of Campeche and Tabasco reported a few days of heavy rains, overflowing rivers, causing mudslides, and destroying some homes. Additionally, strong winds toppled trees and damaged crops, especially bananas and corn. [17] Many of these trees fell onto dwellings, demolishing more than 100 and destroying some 250 others in Carmen. [2] : 34 In Louisiana, the hurricane produced beneficial rainfall in the Buras area. [18] Although the storm remained far south of Florida as it headed towards the Yucatán Peninsula, a few locations observed tropical storm-force wind gusts, including up to 60 mph (95 km/h) at Key West. [2] : 34 Many communities across the northern portion of the state reported some damaged homes and downed trees, [2] : 35 with damage totaling approximately $40,000 in the Jacksonville area alone. [19] A tornado at Pablo Beach damaged or destroyed a few buildings near the Murray Hall hotel, damaged the hotel itself, and tossed a freight train car, buggy, horse, and boy, killing him after he struck the ground. [20] Several locations across Georgia observed at least 1 in (25 mm) of rain, including 1.93 in (49 mm) in Smithville. [21] Although the storm crossed the interior portions of North Carolina, wind gusts reached as high as 70 mph (110 km/h) along the coast, likely at Frying Pan Shoals. [13] Some wind damage was reported over the western part of the state, mainly downed telegraph wires in Asheville and a hotel partially deroofed in Swannanoa. [22]
Tropical storm (SSHWS) | |
Duration | September 12 – September 19 |
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Peak intensity | 60 mph (95 km/h) (1-min); |
The 1924 report from Mitchell noted that this storm was first observed near the Cabo Verde Islands on September 12. [2] : 37 Initially moving northwestward, the storm curved north-northwestward two days later, but then resumed a northwestward course by September 16. The cyclone is estimated to have peaked with winds of 60 mph (95 km/h). By September 18, the system turned north-northeastward and was last noted on the following day about 290 mi (465 km) southeast of Cape Race, Newfoundland. [3] Chenoweth's study indicates that the cyclone developed as a tropical depression on September 14. An extratropical transition on September 19 has also been proposed. [6]
Tropical storm (SSHWS) | |
Duration | September 29 – October 6 |
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Peak intensity | 70 mph (110 km/h) (1-min); |
As meteorologist Ivan Ray Tannehill in 1938 documented this storm as far back as September 29, [2] : 37 the official Atlantic hurricane database initiates the track on that date about 425 mi (685 km) northeast of Paramaribo, Suriname. Moving northeastward, the storm struck Dominica late on October 1 with winds estimated at 50 mph (85 km/h). The storm passed through the British Virgin Islands on the following day. After re-emerging into the Atlantic, the system curved north-northwestward on October 3 and then northeastward on October 4. As the cyclone neared Bermuda on October 5, it nearly became a hurricane, peaking with winds of 70 mph (110 km/h). On October 6, the storm was last noted approximately 270 mi (435 km) southeast of Sable Island, Nova Scotia. [3]
The 2014 study by Chenoweth indicates that this cyclone on October 1 and did not cross the Lesser Antilles, instead moving remaining northeast of the islands. Chenoweth also proposed that further intensification occurred than shown in HURDAT, with the storm maintaining hurricane status from October 3 to October 5. [6] Antigua experienced severe squalls and rough seas. The captain of a ship anchored at Parham reported winds reaching force 11 on the Beaufort scale, indicating near-hurricane conditions. [23]
Tropical storm (SSHWS) | |
Duration | October 5 – October 7 |
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Peak intensity | 60 mph (95 km/h) (1-min); ≤1002 mbar (hPa) |
Although reports suggest the presence of a tropical depression over the northwestern Caribbean starting on October 4, the official track begins on the following day, when the existence of a closed circulation could be confirmed. [4] Moving quickly northeastward, the depression struck the Zapata Swamp of Cuba and entered the Straits of Florida less than six hours later. Intensifying into a tropical storm late on October 5, the cyclone made landfall near Marathon, Florida, around 23:00 UTC. A second landfall occurred in Florida around 01:00 UTC the next day near Flamingo, about five hours before the storm emerged into the Atlantic near Stuart. [3] Because ships recorded barometric pressure as low as 1,002 mbar (29.6 inHg) on October 7, [2] : 38 the storm is estimated to have peaked with winds of 60 mph (95 km/h). The system transitioned into an extratropical cyclone later that day, just prior to striking near Northwest Cove, Nova Scotia. After crossing Nova Scotia, the extratropical remnants turned northward over the Gulf of Saint Lawrence, crossing far eastern Canada before dissipating over the Labrador Sea on October 11. [3] Chenoweth also proposed the removal of this storm from HURDAT, finding "No evidence in land-based reports or from ships". [6]
Chenoweth proposed four other storms not currently listed in HURDAT: [6]
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 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 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 1894 Atlantic hurricane season included four major hurricanes, one of the highest totals in the second half of the 19th century and behind only the previous year. Additionally, the season featured a total of seven tropical storms, five of which strengthened into a 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 featured the only known instance of more than one tropical cyclone causing at least 1,000 deaths in the United States. It was a fairly active season, with 12 tropical storms forming, 10 of which became hurricanes. Of those, five became major hurricanes. The season is considered hyper-active in terms of accumulated cyclone energy, achieving a total of 231 units, which remains the third-highest ever recorded in the Atlantic basin. Additionally, 1893 became one of two seasons on record to see four Atlantic hurricanes active simultaneously, along with 1998. 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 June 12 in the Bay of Campeche, while the twelfth and final storm transitioned into an extratropical cyclone on November 9 over the northwestern Atlantic.
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 featured the most devastating tropical cyclone to impact the French overseas territory of Martinique since the early 19th century. Overall, ten tropical storms formed, seven of which became hurricanes. Of those, one 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. Therefore, 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 July 3 in the Bay of Campeche, while the tenth and final storm was last noted offshore Atlantic Canada on November 6.
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 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 1881 Atlantic hurricane season featured a tropical cyclone that remains one of the deadliest in the history of the United States. Seven tropical storms are known to have developed, four of which strengthened into hurricanes, though none of those intensified 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 1879 Atlantic hurricane season ran from the summer to near the end of autumn in 1879. In 1879 there were two tropical storms, four hurricanes, and two 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 1879 cyclones, Hurricane One were first documented in 1995 by Jose Fernandez-Partagas and Henry Diaz. They also proposed large changes to the known tracks of Hurricanes Two, Three, Seven and Eight. Later one storm was deemed not to be a tropical cyclone at all and was dropped from the database.
The 1878 Atlantic hurricane season lasted from the summer through much of the fall. Records show that 1878 featured a relatively active hurricane season. A total of twelve storms were observed during the year. There were twelve tropical storms, eight hurricanes and two 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 1878 cyclones, both Hurricane Three and Hurricane Four were first documented in 1995 by Jose Fernandez-Partagas and Henry Diaz, who also proposed large changes to the known tracks of Hurricanes Two, Seven and Eight. Further analysis from 2000 onwards extended the duration of Hurricane Three by one day and identified major track changes for Hurricane Five.
The 1877 Atlantic hurricane season featured one of the most devastating tropical cyclones to impact the Dutch Caribbean constituent country of Curaçao. Eight tropical storms are known to have developed, three of which strengthened into hurricanes, while one of those intensified 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 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. 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.
The 1875 Atlantic hurricane season featured three landfalling tropical cyclones. 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 has been estimated. There were five recorded hurricanes and one major hurricane – Category 3 or higher on the modern-day Saffir–Simpson scale.
The 1874 Atlantic hurricane season featured the first hurricane to be recorded on a weather map by the United States Signal Service. It was a relatively inactive season, 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.
The 1872 Atlantic hurricane season included a storm whose track became one of the first to be published by the United States Army Signal Service, a predecessor of the National Weather Service. The season was quiet, with only five documented tropical cyclones, of which four attained hurricane status. None of them intensified 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 has been estimated.
The 1863 Atlantic hurricane season featured five landfalling tropical cyclones. 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 has been estimated. There were seven recorded hurricanes and no major hurricanes, which are Category 3 or higher on the modern day Saffir–Simpson scale. Of the known 1863 cyclones, seven were first documented in 1995 by José Fernández-Partagás and Henry Diaz, while the ninth tropical storm was first documented in 2003. These changes were largely adopted by the National Oceanic and Atmospheric Administration's Atlantic hurricane reanalysis in their updates to the Atlantic hurricane database (HURDAT), with some adjustments.