1871 Atlantic hurricane season | |
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Seasonal boundaries | |
First system formed | June 1, 1871 |
Last system dissipated | October 13, 1871 |
Strongest storm | |
Name | Three |
• Maximum winds | 115 mph (185 km/h) (1-minute sustained) |
• Lowest pressure | 952 mbar (hPa; 28.11 inHg) |
Seasonal statistics | |
Total storms | 8 |
Hurricanes | 6 |
Major hurricanes (Cat. 3+) | 2 |
Total fatalities | 35+ |
Total damage | Unknown |
The 1871 Atlantic hurricane season lasted from mid-summer to late-fall. Records show that 1871 featured two tropical storms, four 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. According to a study in 2004, 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 is possible. [1] A later study in 2008 estimated that eight or more storms may have been missed prior to 1878. [2]
Of the known 1871 cyclones, both Hurricane Five and Hurricane Eight were first documented in 1995 by José Fernández-Partagás and Henry Díaz, who also proposed large changes to the known tracks of Hurricane Three and of Hurricane Four. [3] Further analysis, in 2008, extended the duration of both Hurricane Three and Hurricane Seven, by one day each. [4] A reanalysis authored by Michael Chenoweth, published in 2014, found fifteen named storms, twelve of which became hurricanes; four attained major hurricane status. However, these results have yet to be officially accepted into HURDAT. [5]
Tropical storm (SSHWS) | |
Duration | June 1 – June 5 |
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Peak intensity | 60 mph (95 km/h) (1-min); ≤999 mbar (hPa) |
At 00:00 UTC on June 1, a tropical storm formed about 60 miles (95 km) east-southeast of Key West, Florida. For the next twelve hours, the system moved westward over the Straits of Florida between Cuba and the lower Florida Keys. Entering the southeastern Gulf of Mexico, the cyclone turned to the northwest and strengthened. While located 165 miles (266 km) west-northwest of the Dry Tortugas, it attained peak winds of 60 mph (95 km/h) early on June 2. Afterward, the system gradually turned to the west-northwest and maintained its intensity. As it neared the Texas coast, its course shifted to the northwest. At 07:00 UTC on June 4, the storm made landfall over San Luis Pass, 50 mi (80 km) south-southeast of Houston, at peak intensity. After landfall, the storm curved northward over East Texas, and dissipated over eastern Oklahoma late on June 5. [6] A preliminary reanalysis in 2014 upgraded the cyclone to a Category 1 hurricane at landfall in Texas. [5]
A weather station in Galveston recorded peak winds of 39 mph (63 km/h) and a total of 6 inches (150 mm ) of rain during the passage of the storm, [7] of which 3.95 in (100 mm) fell in a fourteen-minute time span on June 4. [8] Another source indicated 15.57 in (395 mm) of rainfall took place, including a twenty-four-hour record of 8.55 in (217 mm) on June 4. [9] Additionally, a barometer in the area sampled a minimum peripheral pressure of 29.51 inHg (999 mb). Storm surge flooded onto and eroded Galveston Island, causing washouts of railroad beds and structures. [3] One vessel, the steamship Alabama, beached at Galveston, while another, the Virginia Dare, grounded on an offshore sandbar there. Four drownings occurred at Galveston. Gale-force winds also affected Port Aransas; very high tides occurred there and at Indianola, flooding low ground at the latter place. [9] Extremely heavy rains associated with this cyclone also caused flooding in New Orleans, which was reportedly "submerged". [10] The New York Times on June 6 reported that floodwaters covered 6 square miles (16 km2 ), five hundred blocks in all. [3]
Tropical storm (SSHWS) | |
Duration | June 8 – June 10 |
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Peak intensity | 60 mph (95 km/h) (1-min); ≤1007 mbar (hPa) |
At 00:00 UTC on June 8, the second tropical storm of the season developed 155 mi (250 km) north-northwest of Progreso, Yucatán—three days after Tropical Storm One dissipated. Taking a steady course to the northwest, the cyclone closely followed its predecessor, threatening Southeast Texas yet again. Early on June 9, the system peaked at 60 mph (95 km/h) and turned north-northwestward. At 17:00 UTC, the cyclone made landfall near present-day Jamaica Beach, 15 mi (25 km) west-southwest of Galveston, at peak intensity. After landfall, the system headed northward over the western part of Galveston Bay. Late on June 10, the cyclone dissipated over East Texas, just south of the Texas–Oklahoma border. [6]
As it affected Galveston, the storm destroyed a church and many houses. Storm surge occurred on the island for the second time in a week, as floodwaters engulfed the eastern section of Galveston Island. Several ships wrecked as well, and some sailing ships were deemed lost at sea. A cotton steamship, the Mollie Hambleton, sank while at anchor. One person died at Refugio, when winds unroofed a church. Storm surge-related flooding was minimal at Indianola. [9] Strong gales affected coastal Louisiana, and neared hurricane intensity at Lake Charles, downing fruit trees. Torrential rain damaged corn and cotton crops, and numerous cattle drowned. A tornado struck Chatawa, Mississippi, destroying a schoolhouse and trees. [10]
A reanalysis in 2014 tentatively determined that this storm and the preceding system were a single hurricane. [5]
Category 3 hurricane (SSHWS) | |
Duration | August 14 – August 23 |
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Peak intensity | 115 mph (185 km/h) (1-min); 952 mbar (hPa) |
Early on August 14, the ship Tybee reported hurricane-force winds to the east of The Bahamas, signaling the presence of a well-formed system. At 00:00 UTC on August 14, the third tropical cyclone of the season was noted, 210 mi (340 km) northeast of San Salvador Island, with 90-mph (150-km/h) winds. Tracking generally westward, the hurricane gradually strengthened. At 12:00 UTC on August 15, the cyclone attained peak winds of 115 mph (185 km/h)—equivalent to Category 3 status on the modern Saffir–Simpson scale, which it maintained until landfall in Florida. Several hours later, the hurricane crossed the northern Abaco Islands and continued westward toward the Gulf Stream. Early on August 16, a barque, the Bridgeport, measured a pressure of 28.10 inHg (952 mb) in the storm's eye. [3] As it neared eastern Florida, the storm curved slightly west-northwestward, before making landfall north of Hobe Sound at 02:00 UTC on August 17. [6] Over the next few days, the cyclone parabolically turned to the northeast, re-entering the Atlantic near Darien, Georgia, on August 18. While executing a clockwise loop off the Southeastern United States, the system maintained winds just below hurricane intensity. On August 22, the system ended its loop and headed westward, toward the Georgia coast. Final landfall occurred near Brunswick at 00:00 UTC on August 23. At the time, the cyclone still contained winds of 70 mph (110 km/h). The system decayed as it moved inland, and dissipation took place 18 hours later. [6]
Despite crossing the Bahamas at peak strength, damage in the archipelago, if any, is unknown. The hurricane was of great extent as it struck Florida, with hurricane-force winds occurring at New Smyrna—115 mi (185 km) from the eye. The local U.S. Army Signal Corps observer judged the storm to be the worst since October 23, 1865. In New Smyrna, the storm snapped or otherwise damaged oak and citrus trees. At Enterprise, several homes were unroofed as well. Winds destroyed another home at Ocala. [11] Cotton, oranges, and sugar cane crops in Hillsborough County experienced their largest losses since the 1848 hurricane. [12] Numerous ships were tossed ashore, [13] leaving the beaches "strewn with wrecks". [11] Gale-force winds in Jacksonville uprooted many trees, topped a few brick walls, damaged tin roofs, and downed telegraph wires, cutting off communications. Abnormally high tides inundated parts of the city, although water remained "about a foot [0.3 m] below the market floor." Damage in Jacksonville reached several thousands of dollars. [14] Impacts to Georgia, if any, are unknown. Winds reached 60 mph (97 km/h) in Savannah, which registered a pressure of 29.55 inHg (1,001 mb). [11] In South Carolina, Charleston reportedly experienced its heaviest rain storm since 1854, with 8.53 in (217 mm) of precipitation falling in a 36-hour period, more than 2 in (51 mm) above the total amount of rainfall observed between May 1 and August 1. However, little flooding occurred except on a few streets. One man drowned after attempting to step from a wharf to his sloop during the height of the storm. [15] A telegram from North Carolina described the rainfall as being generally beneficial to crops in the vicinity of Wilmington and reported that the brig Alice Lee was beached at Frying Pan Shoals. [16]
Category 3 hurricane (SSHWS) | |
Duration | August 17 – August 30 |
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Peak intensity | 115 mph (185 km/h) (1-min); 962 mbar (hPa) |
On August 17, the fourth tropical storm of the season developed 550 mi (885 km) west-southwest of the Cape Verde islands. The system progressed on a west-northwest track and steadily intensified, becoming a major hurricane at 00:00 UTC on August 21. Bearing peak winds of 115 mph (185 km/h), the hurricane passed over Antigua, Sint Eustatius, Saint Kitts, and Saint Thomas. Continuing northwestward, it passed 30 mi (50 km) northeast of Fajardo, Puerto Rico. [17] The hurricane then weakened to a Category 2 hurricane, maintaining this strength while making further landfalls in the Bahamas. At 05:00 UTC on August 25, the storm struck near present-day Vero Beach, Florida, with winds of 105 mph (165 km/h). [18] After crossing Central Florida, it entered the Gulf of Mexico and made a final landfall on Taylor County, Florida, as a tropical storm. The storm then moved north and east over land, weakening into a tropical depression, before strengthening back into a tropical storm after re-emerging into the Atlantic off South Carolina. At 12:00 UTC on August 30, the cyclone reattained winds of 70 mph (110 km/h). The storm was last sighted 90 mi (145 km) east of Cape Cod. [6] Chenoweth's study reassessed the hurricane as a Category 4 over the Leeward Islands, with a pressure of 947 mb (28.0 inHg), and shifted the landfall in Florida farther south, close to the present-day Broward–Palm Beach county line. [5]
At least 30 deaths occurred on Antigua and the storm was considered the worst to impact the island since 1835. [19] : 4 Le Moniteur de la Martinique reported two fatalities and considerable damage on Saint Kitts. As the storm passed near Saba, resident Catholic priest Father Koch observed a barometric pressure of 998 mbar (29.5 inHg) and the destruction of many thatch houses. [19] : 5 Some newspapers noted that "not a house was left standing on the whole island" and that the storm killed or injured about 150 people, [20] although the death toll is officially listed as 27. [21] Additionally, numerous shipwrecks occurred, including three ships lost in Puerto Rico, where the storm was dubbed the Santa Juana hurricane. [17] In Florida, storm surge and abnormally high tides damaged a number of boats in the St. Johns River. Winds in the Jacksonville area mainly toppled fences and trees, [12] although a warehouse and church were destroyed. Downed telegraph wires severed communications between Lake City and St. Augustine. [22] The storm demolished several dwellings in Orlando and many others at nearby Fort Reid, along with a gristmill at Fort Mellon. The surrounding countryside was reportedly littered with "one solid fallen mass" of timber "for miles and miles". Several other localities reported crop damage, including Alachua County, Marianna, and Marion County; a report from Gainesville deemed the storm the worst locally in many years, noting that the "most comely shade trees" in town were downed, along with much timber elsewhere. Some homes were blown off their foundations near Ocala, and fencing was "almost universally destroyed". [12]
Category 2 hurricane (SSHWS) | |
Duration | August 30 – September 2 |
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Peak intensity | 105 mph (165 km/h) (1-min); |
The only storm of the year not to make landfall, this system was first observed as a Category 2 hurricane with winds of 105 mph (165 km/h) north of Puerto Rico on August 30. Hurricane Five maintained this intensity until it was last observed south of Nova Scotia. [6] Chenoweth's renanalysis shows genesis three days earlier, with the storm attaining hurricane status a day sooner. The storm also is depicted as a major hurricane at its peak, with winds of 120 mph (195 km/h), based on a measured barometric pressure of 941 mb (27.8 inHg). Chenoweth also indicates that the system made landfall on Nova Scotia as a minimal hurricane on September 3. [5]
Category 1 hurricane (SSHWS) | |
Duration | September 5 – September 8 |
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Peak intensity | 80 mph (130 km/h) (1-min); |
A hurricane formed near the geographic center of the Gulf of Mexico on September 5. At 14:00 UTC the next day, it made landfall near Cedar Key, Florida, as a minimal hurricane. [6] It brought heavy rainfall to Florida and Georgia before entering the Atlantic off the east coast of Georgia. [23] Still continuing to the northeast, it was last sighted south of Cape Hatteras. [6]
Category 1 hurricane (SSHWS) | |
Duration | September 30 – October 7 |
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Peak intensity | 80 mph (130 km/h) (1-min); |
A tropical storm was first sighted in the Bay of Campeche on September 30. It continued moving in a northeast direction, paralleling the Texas coast and strengthening to a Category 1 hurricane while doing so. Early on October 4, the hurricane passed south of the Mississippi River Delta. At 16:00 UTC on October 5, it finally made landfall on Taylor County, Florida, as a strong tropical storm with winds of 70 mph (110 km/h). After re-entering the Atlantic Ocean, the storm was last sighted east of Cape Hatteras. [6] At least three people were killed at Galveston and several ships were wrecked or foundered, some with the loss of all hands. [9]
Category 1 hurricane (SSHWS) | |
Duration | October 10 – October 13 |
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Peak intensity | 80 mph (130 km/h) (1-min); |
A hurricane was first observed northeast of the British Virgin Islands on the morning of October 10. At this point it was already a Category 1 hurricane with winds of 80 mph (130 km/h). Its intensity remained steady at that level as it traveled first west, then veered north before travelling parallel to the US coast. The hurricane dissipated shortly after making landfall at Nova Scotia on October 13. [6]
In Nova Scotia, strong winds produced by the storm reportedly downed all telegraph wires between Bedford and Halifax. [24] The railroad tracks linking the two cities also suffered damage, totaling approximately $16,000. Shipping and wharves at the latter and in Sydney experienced significant impacts, while 30 vessels ran aground at the Dartmouth harbor. Abnormally high tides flooded the basements of oceanfront homes in Halifax. Three people drowned near Devils Island while attempting to set fish nets. Damage throughout Atlantic Canada reached roughly $200,000. [25]
Chenoweth's study indicates formation occurred five days earlier, over the tropical Atlantic. The storm is also estimated to have peaked with winds of 140 mph (220 km/h) on October 10, equivalent to a Category 4 hurricane, based on a pressure of 930 mb (27 inHg). The system then neared the Canadian Maritimes with winds approaching 100 mph (155 km/h) and made landfall as a low-end hurricane. [5]
Chenoweth proposed eight other storms not currently listed in HURDAT: [5]
This is a table of the storms in 1871 and their landfall(s) in bold, if any. The minimum pressures, in most cases, are based on limited observations and may not have occurred at their peak intensity.
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 | June 1–5 | Tropical storm | 60 (95) | 999 | Texas , Louisiana | Unknown | 4 | [9] | ||
Two | June 8–10 | Tropical storm | 60 (95) | 1007 | Texas , Louisiana | Unknown | 1 | [9] | ||
Three | August 14–23 | Category 3 hurricane | 115 (185) | 952 | The Bahamas, Florida, Georgia | Unknown | Unknown | |||
Four | August 17–30 | Category 3 hurricane | 115 (185) | 962 | Leeward Islands, The Bahamas, Florida | Unknown | 27 | [21] | ||
Five | August 30–September 5 | Category 2 hurricane | 105 (165) | Unknown | Nova Scotia | Unknown | Unknown | |||
Six | September 5–September 8 | Category 1 hurricane | 80 (130) | Unknown | Florida | Unknown | Unknown | |||
Seven | September 30–October 7 | Category 1 hurricane | 80 (130) | Unknown | Texas, Florida | Unknown | >3 | [9] | ||
Eight | October 10–13 | Category 1 hurricane | 80 (130) | Unknown | Nova Scotia | Unknown | Unknown | |||
Season aggregates | ||||||||||
8 systems | June 1–October 13 | 115 (185) | 952 | Unknown | >35 |
The 1909 Atlantic hurricane season was an average Atlantic hurricane season. The season produced thirteen tropical cyclones, twelve of which became tropical storms; six became hurricanes, and four of those strengthened into major hurricanes. The season's first storm developed on June 15 while the last storm transitioned into an extratropical cyclone on November 14. The most notable storm during the season formed in late August, while east of the Lesser Antilles. The hurricane devastated the Lesser Antilles, the Greater Antilles, and Mexico, leaving around 4,000 fatalities and more than $50 million (1909 USD) in damage.
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 1894 Atlantic hurricane season ran through the summer and the first half of fall in 1894. The 1894 season was a fairly inactive one, with seven storms forming, five of which became hurricanes.
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 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 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 1884 Atlantic hurricane season was one of only three Atlantic hurricane seasons, along with 1852 and 1858, in which every known tropical cyclone attained hurricane status. Overall, four tropical cyclones developed, three of which made landfall. The first system was initially observed over the northwestern Atlantic Ocean on September 1. It struck Newfoundland the following day, but impact there is unknown. On September 3, the next hurricane developed, though it did not affect land in its duration. The third hurricane struck Georgia, accompanied by damaging waves in north Florida.
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. It is also worthy of note that the volume of recorded activity was documented largely without the benefit of modern technology. Tropical cyclones during this era did not approach populated areas or shipping lanes, especially if they were relatively weak and of short duration, may have remained undetected. Because technologies such as satellite monitoring were not available until the 1960s, historical data on tropical cyclones from this period may not be comprehensive. 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 1887 cyclones, Tropical Storm One and Tropical Storm Three were first documented in 1996 by Jose Fernandez-Partagas and Henry Diaz. They also proposed large alterations to the known tracks of several of the other 1887 storms. Later re-analysis led to the known duration of Hurricane Six, and also that of Hurricane Fifteen, being increased.
The 1888 Atlantic hurricane season ran through the summer and the first half of fall in 1888. In the 1888 Atlantic season 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 are known, 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 1886 Atlantic hurricane season was a very active and record breaking Atlantic hurricane season that ran through the early summer and the first half of fall in 1886. Out of the ten known hurricanes, six of them struck the United States; an event that would not occur again until 1985 and 2020. The season also had the most active June on record, and reached the modern seasonal average of hurricanes by mid-August. This record has only occurred once more in 1893, and has yet to come close since. Four of the hurricanes also reached major hurricanes status. However, with the absence of modern satellites and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were documented. The actual total is likely higher with a average under-count bias estimate of zero to six tropical cyclones per year between 1851 to 1885. Several studies have also suggested that the 1883 eruption of Krakatoa may have played a significant role in the unusual and enhanced activity. Hurricane Seven and Tropical Storm Eleven were recently documented in 1996 by Jose Fernandez-Partagas and Henry Diaz, in which they also proposed alterations to other known tracks of several other 1886 storms.
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 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 1853 Atlantic hurricane season featured eight known tropical cyclones, none of which made landfall. Operationally, a ninth tropical storm was believed to have existed over the Dominican Republic on November 26, but HURDAT – the official Atlantic hurricane database – now excludes this system. The first system, Tropical Storm One, was initially observed on August 5. The final storm, Hurricane Eight, was last observed on October 22. These dates fall within the period with the most tropical cyclone activity in the Atlantic. At two points during the season, pairs of tropical cyclones existed simultaneously. Four of the cyclones only have a single known point in their tracks due to a sparsity of data, so storm summaries for those systems are unavailable.
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 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 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.
The 1859 Atlantic hurricane season featured seven hurricanes, the most recorded during an Atlantic hurricane season until 1870. 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. Of the eight known 1859 cyclones, five were first documented in 1995 by Jose Fernandez-Partagás and Henry Diaz, which was 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. HURDAT is the official source for hurricane data such as track and intensity, although due to sparse records, listings on some storms are incomplete.