1855 Atlantic hurricane season | |
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Seasonal boundaries | |
First system formed | August 5, 1855 |
Last system dissipated | September 17, 1855 |
Strongest storm | |
Name | Five |
• Maximum winds | 125 mph (205 km/h) (1-minute sustained) |
• Lowest pressure | 945 mbar (hPa; 27.91 inHg) |
Seasonal statistics | |
Total storms | 5 |
Hurricanes | 4 |
Major hurricanes (Cat. 3+) | 1 |
Total fatalities | 1 |
Total damage | Unknown |
The 1855 Atlantic hurricane season featured tropical cyclone landfalls in the Gulf Coast of the United States, the Greater Antilles, and Mexico, but none along the East Coast of the United States. It was inactive, with only five known tropical cyclones. Another tropical storm was believed to have existed offshore Atlantic Canada in late August and early September, [1] but HURDAT – the official Atlantic hurricane database – now excludes this system. [2] The first known system was initially observed on August 5, while the final known storm was last noted on September 17. These dates fall within the period with the most tropical cyclone activity in the Atlantic. At one point during the season, two tropical cyclones existed simultaneously. Two of the cyclones only have a single known point in their tracks due to a sparsity of data.
Of the season's five tropical cyclones, four reached hurricane status. Furthermore, one of those four strengthened into a major hurricane, which are Category 3 or higher on the modern-day Saffir–Simpson scale. The strongest cyclone of the season, the fifth system, peaked at Category 3 strength with 125 mph (205 km/h) winds. It reportedly produced some of the worst impacts in Louisiana and Mississippi since 1819 and killed at least one person in the latter. The first storm of the season brought locally severe impact to Tampico, Tamaulipas, in Mexico in early August. Additionally, the fourth storm caused severe damage in the Lesser Antilles.
Category 2 hurricane (SSHWS) | |
Duration | August 6 – August 6 |
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Peak intensity | 105 mph (165 km/h) (1-min); |
Based on newspaper reports, [3] the first hurricane of the season was within the vicinity of Tampico, Tamaulipas, on August 6. Maximum sustained winds were at 105 mph (165 km/h), indicating a Category 2 hurricane. [2] No further information is available on the meteorological history of this storm. However, it is possible that the storm developed in the Caribbean in late July, due to data obtained from the barque Bercaldine. [1] Torrential rainfall in the Tampico area caused disastrous flooding, with heavy damage to goods and property. Eleven vessels were docked at Tampico, some of which lost their cargo. At the mouth of the Pánuco River, a pilot station and a fort were swept away. The event was considered the worst inundation of Tampico over the last 30 years. [3]
Category 2 hurricane (SSHWS) | |
Duration | August 10 – August 11 |
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Peak intensity | 105 mph (165 km/h) (1-min); |
The ship James Foster Jr. encountered a hurricane on August 10, while located about 575 mi (925 km) east-southeast of Cape Race, Newfoundland. Sustained winds of 105 mph (165 km/h) were observed, equivalent to a Category 2 hurricane. Data from the James Foster Jr. and Rebecca indicate that the storm moved rapidly northeastward. This system was last noted about 560 mi (900 km) west of Ireland on August 11. [1] [2] Climate researcher Michael Chenoweth proposed the removal of this storm from HURDAT, noting "Insufficient supporting evidence from other neighboring data sources". [4]
Category 1 hurricane (SSHWS) | |
Duration | August 11 – August 11 |
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Peak intensity | 80 mph (130 km/h) (1-min); |
HMS Walverine reported a hurricane at 12.5°N, 83.0°W, which is located about 15 mi (25 km) north of Nicaragua's Corn Islands. [1] A sustained wind speed of 80 mph (130 km/h) was observed. [2] Shortly thereafter, HMS Walverine was wrecked and no further information is known about this storm. [1] Chenoweth also argued for the exclusion of this cyclone from HURDAT, noting that logbooks do not seem to indicate the presence of the storm and Walverine actually sank due to crashing into rocks for reasons unrelated to weather. [4]
Tropical storm (SSHWS) | |
Duration | August 24 – August 27 |
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Peak intensity | 70 mph (110 km/h) (1-min); 997 mbar (hPa) |
Based on reports of a strong gale, a tropical storm was first tracked about 250 mi (400 km) east-southeast of Barbados early on August 24. [1] It initially headed westward, before re-curving west-northwestward early on the following day. Shortly thereafter, the storm passed through the Windward Islands between Grenada and Saint Vincent and the Grenadines. The storm peaked with winds of 70 mph (110 km/h) while moving northwestward across the Caribbean Sea. It weakened slightly before making landfall near San Pedro de Macorís, Dominican Republic, with winds of 60 mph (95 km/h) early on August 27. The storm slowly weakened over Hispaniola and was last noted near Bombardopolis, Haiti, later that day. [2]
Considerable damage occurred in the Lesser Antilles. On Saint Vincent, rains destroyed roads and a number of houses. Many sugar cane fields were also ruined. Several vessels were lost there and on other islands, including Barbados, Dominica, and Martinique. On Saint Croix in the present-day United States Virgin Islands, at least one vessel was destroyed by the heavy gales. There were also strong gales reported in Puerto Rico and the Dominican Republic. [1]
Category 3 hurricane (SSHWS) | |
Duration | September 15 – September 17 |
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Peak intensity | 125 mph (205 km/h) (1-min); 945 mbar (hPa) |
The Middle Gulf Shore Hurricane of 1855
The ship Orphan encountered a hurricane with winds of 80 mph (130 km/h) in the central Gulf of Mexico on September 15. [5] It strengthened quickly while moving northward, becoming a Category 2 hurricane later that day. By 00:00 UTC on September 16, the storm peaked as a Category 3 hurricane with maximum sustained winds of 125 mph (205 km/h), making it the strongest tropical cyclone of the season. Shortly thereafter, the hurricane made landfall near Buras-Triumph, Louisiana, at the same intensity. [2] Based on the pressure-wind relationship, the storm had a minimum barometric pressure of approximately 945 mbar (27.9 inHg) upon striking the coast. [6] It weakened after moving inland, decreasing to Category 1 intensity later on September 16. Early on the following day, the system weakened to a tropical storm, several hours before dissipating over central Alabama. [2]
This was regarded as the worst hurricane in the region since 1819. In Louisiana, winds and storm surge impacted the eastern portions of the state. The wharf and bathhouse in Proctorville were swept away. About 4 ft (1.2 m) of water was reported at Proctor's Landing. A combination of strong winds and storm surge destroyed a number of houses along the shores of Lake Borgne. Along the coast of Mississippi, most structures were swept to sea. [7] The foundation of the Biloxi Lighthouse was endangered due to erosion from this storm. [8] Additionally, locals described the Cat Island Lighthouse as being left in "severe peril". Several ships were damaged or capsized in the Mississippi River, including Atchafalaya, J.S. Chenoweth, Ship Shoal, and Venice. [7] [9] One death occurred in Mississippi City after winds unroofed some lodging at the Teagarden Hotel, [10] while two women may have drowned along the coast of the state. [11]
In addition to the five tropical systems, another storm was operationally believed to have existed in late August and early September. The ship Atlantic encountered a very heavy gale while located west of Sable Island, Nova Scotia, on August 31. The storm moved rapidly east-northeastward offshore Atlantic Canada. It was last noted on September 2 and was thought to have transitioned into an extratropical cyclone. [1] However, HURDAT no longer includes this system in its database. [2]
This is a table of all of the known storms that formed in the 1855 Atlantic hurricane season. It includes their 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 1855 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 | August 6 | Category 2 hurricane | 105 (165) | Unknown | Mexico (Tamaulipas) | Unknown | Unknown | |||
Two | August 10–11 | Category 2 hurricane | 105 (165) | Unknown | None | None | None | |||
Three | August 11 | Category 1 hurricane | 80 (130) | Unknown | Nicaragua | Unknown | Unknown | |||
Four | August 24–27 | Tropical storm | 70 (110) | 997 | Lesser Antilles, Hispaniola (Dominican Republic) | Unknown | Unknown | |||
Five | September 15–17 | Category 3 hurricane | 125 (205) | 945 | Gulf Coast of the United States (Louisiana) | Unknown | 1 | [10] | ||
Season aggregates | ||||||||||
5 systems | August 6 – September 17 | 125 (205) | 945 | Unknown | 1 |
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 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 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 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 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.
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 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, while three of the storms only have a single point in their track known.
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 1882 Atlantic hurricane season ran through the summer and early fall of 1882. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1882 Atlantic season there were two tropical storms, two Category 1 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 1882 cyclones, Hurricane One and Hurricane Five were both first documented in 1996 by Jose Fernandez-Partagas and Henry Diaz, while Tropical Storm Three was first recognized in 1997 and added to HURDAT in 2003. Partagas and Diaz also proposed large changes to the known track of Hurricane Two while further re-analysis, in 2000, led to the peak strengths of both Hurricane Two and Hurricane Six being increased. In 2011 the third storm of the year was downgraded from a hurricane to a tropical storm.
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. However, 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 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 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. 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. A later study in 2008 estimated that eight or more storms may have been missed prior to 1878.
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.
The 1856 Atlantic hurricane season featured six tropical cyclones, five of which made landfall. The first system, Hurricane One, was first observed in the Gulf of Mexico on August 9. The final storm, Hurricane Six, was last observed on September 22. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Only two tropical cyclones during the season existed simultaneously. One of the cyclones has only a single known point in its track due to a sparsity of data. Operationally, another tropical cyclone was believed to have existed in the Wilmington, North Carolina area in September, but HURDAT – the official Atlantic hurricane database – excludes this system. Another tropical cyclone that existed over the Northeastern United States in mid-August was later added to HURDAT.