1852 Atlantic hurricane season | |
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Seasonal boundaries | |
First system formed | August 19, 1852 |
Last system dissipated | October 11, 1852 |
Strongest storm | |
Name | One |
• Maximum winds | 115 mph (185 km/h) (1-minute sustained) |
• Lowest pressure | 961 mbar (hPa; 28.38 inHg) |
Seasonal statistics | |
Total storms | 5 |
Hurricanes | 5 |
Major hurricanes (Cat. 3+) | 1 |
Total fatalities | 100+ direct |
Total damage | $1 million (1852 USD) |
The 1852 Atlantic hurricane season was one of only three Atlantic hurricane seasons in which every known tropical cyclone attained hurricane status. [1] Five tropical cyclones were reported during the season, which lasted from late August through the middle of October; these dates fall within the range of most Atlantic tropical cyclone activity, and none of the cyclones coexisted with another. Though there were officially five tropical cyclones in the season, hurricane scholar Michael Chenoweth assessed two of the cyclones as being the same storm. [2] There may have been other unconfirmed tropical cyclones during the season, as meteorologist Christopher Landsea estimated that up to six storms were missed each year from the official database; this estimate was due to small tropical cyclone size, sparse ship reports, and relatively unpopulated coastlines. [3]
Every tropical cyclone in the season was of hurricane status, or with winds at or exceeding 74 mph (119 km/h). In only two other seasons did every cyclone attain hurricane status; those years were 1858 and 1884. [1] All five cyclones affected land; the strongest was the first storm, which caused severe damage and loss of life when it made landfall near the border between Mississippi and Alabama. The second storm of the season struck Puerto Rico, where it caused over 100 deaths, primarily from flooding. In the middle of September, the third storm moved across Florida with strong wind gusts and light rainfall, and a week later the fourth storm passed over or north of the Lesser and Greater Antilles. The last storm hit the Florida Panhandle, though damage was less than expected.
Category 3 hurricane (SSHWS) | |
Duration | August 19 – August 30 |
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Peak intensity | 115 mph (185 km/h) (1-min); 961 mbar (hPa) |
The Great Mobile Hurricane of 1852 was the first tropical cyclone of the year. It was first observed on August 19 about 140 mi (225 km) north of Puerto Rico. It moved on a west-northwest motion before passing through the Bahamas as it attained hurricane status on August 20. After paralleling the northern coast of Cuba, the storm passed between the Dry Tortugas and Key West, Florida on August 22, and two days later it is estimated the hurricane attained peak winds of 115 mph (185 km/h). The storm slowed on August 25 before turning northward, and early on August 26 it made landfall near Pascagoula, Mississippi at peak strength, and the hurricane rapidly weakened to tropical storm status as it accelerated east-northeastward. On August 28 it emerged into the Atlantic Ocean from South Carolina, and after turning to the northeast, it was last observed on August 30 about 130 mi (210 km) southeast of Cape Cod. [4]
In the Florida Keys, rough waves forced several ships ashore, leaving some damaged. [5] Strong waves created four new channels in the Chandeleur Islands, and the storm's passage also destroyed the island lighthouse; the three keepers were found three days later. Two schooners were also washed ashore along Cat Island. [6] The hurricane produced an estimated storm tide of 12 ft (3.7 m) in Mobile, Alabama, [4] where strong winds damaged much of the city, leaving the majority of the houses destroyed. Trees were downed up to 30 mi (50 km) inland, [7] and coastal areas were flooded. Damage along the coastline was estimated at $1 million (1852 USD), and at least five people died. [8] While crossing the southeastern United States, the storm brought light rainfall but moderately strong winds; in Charleston, South Carolina, the storm destroyed several bridges and crop fields. [4] [9]
Category 1 hurricane (SSHWS) | |
Duration | September 5 – September 6 |
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Peak intensity | 80 mph (130 km/h) (1-min); |
Hurricane San Lorenzo of 1852
Early on September 5, a hurricane was first observed about 65 mi (105 km) southeast of Christiansted in the Danish Virgin Islands. [1] One meteorologist assessed the hurricane as being located near Antigua on September 3. [2] Tracking steadily west-northwestward, it quickly moved ashore near Ponce, Puerto Rico with winds estimated at 80 mph (130 km/h). After crossing southwestern Puerto Rico, the hurricane emerged into the Mona Passage as a tropical storm. Late on September 5 it made landfall on eastern Dominican Republic; it quickly weakened over Hispaniola, dissipating on September 6 over the northwestern portion of the island. [1] An assessment by scholar Michael Chenoweth in 2006 indicated this storm was the same as the next hurricane, with it continuing northwestward and ultimately reaching the Gulf of Mexico. [2] Due to not being considered the same cyclone in the official hurricane database, [1] this hurricane and the following hurricane are listed separately. [4] There, the passage of the storm caused severe flooding, which destroyed large quantities of crops and damaged several roads. Storm damage was heaviest between Guayanilla and Mayagüez. [10] More than 100 people were killed in Puerto Rico, [11] many of whom died due to flooding. [10]
Category 1 hurricane (SSHWS) | |
Duration | September 9 – September 13 |
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Peak intensity | 80 mph (130 km/h) (1-min); 985 mbar (hPa) |
A hurricane was located in the central Gulf of Mexico on September 9, [1] potentially the same hurricane as the previous storm. [2] It tracked generally eastward toward the coast of Florida, with its hurricane intensity estimation based on two ship reports. At about 00:00 UTC on September 12, it moved ashore near Clearwater, Florida, as a minimal hurricane, with an estimated minimum barometric central pressure of 985 mbar (29.1 inHg ). Accelerating east-northeastward while crossing the state, the cyclone emerged into the Atlantic Ocean as a weakened tropical storm before regaining hurricane status on September 13. Later that day, it was last observed about 250 mi (400 km) east-southeast of Cape Hatteras. [1]
A post in Fort Meade, Florida, reported at least 0.55 in (14 mm) of rainfall during the storm's passage. The hurricane was considered "violent", and gusts were estimated to have reached hurricane force. [4] Rough seas and strong easterly winds beached a vessel near St. Augustine. [12] [13]
Category 1 hurricane (SSHWS) | |
Duration | September 22 – September 30 |
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Peak intensity | 90 mph (150 km/h) (1-min); |
On September 22, a tropical storm was located about 200 mi (320 km) east of Guadeloupe. With a steady west-northwest path, the storm moved across the northern Lesser Antilles on September 23, during which it intensified into a hurricane. It passed a short distance north of Puerto Rico and the Dominican Republic as it reached its peak intensity of 90 mph (150 km). Late on September 26 the hurricane turned northwestward, bringing it through the Turks and Caicos Islands and eastern Bahamas. Recurving north-northeastward, the cyclone moved into open waters, and was last classified as a tropical cyclone on September 30 about 390 mi (630 km) east of Cape Hatteras. [1] However, one hurricane researcher assessed the hurricane as lasting until October 3, with the cyclone turning eastward and dissipating near the Azores. [2]
Category 2 hurricane (SSHWS) | |
Duration | October 6 – October 11 |
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Peak intensity | 105 mph (165 km/h) (1-min); 965 mbar (hPa) |
A moderately strong hurricane with winds of 105 mph (165 km/h) was first spotted on October 6 east of Jamaica. Passing a short distance south of the island, the hurricane tracked northwestward and brushed the Yucatán Peninsula before turning north-northeastward into the Gulf of Mexico. [1] Late on October 9, it made landfall a short distance east of Apalachicola, Florida, at peak winds with an estimated pressure of 965 mbar (28.5 inHg). [14] Rapidly weakening to tropical storm status, the cyclone continued northeastward and emerged into the Atlantic Ocean from North Carolina on October 11. Later that day, it was last observed about 250 mi (400 km) southeast of Cape Cod. [1]
Heavy damage was reported in Jamaica. Upon making landfall in Florida, the hurricane produced a 7 ft (2.1 m) storm tide, and in Georgia, hurricane-force winds extended into the southwestern portion of the state, [4] while tropical storm force winds occurred along the coastline. In the state, moderate winds damaged trees and roofs, though the destruction was less than anticipated. [12]
This is a table of all of the storms that formed in the 1852 Atlantic hurricane season. It includes their duration (within the basin), names, 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 1852 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 19–30 | Category 3 hurricane | 115 (185) | 961 | Turks and Caicos Islands, Bahamas, Florida, Gulf Coast of the United States (Mississippi), Southeastern United States | $1 million | Unknown | [8] | ||
Two | September 5–6 | Category 1 hurricane | 80 (130) | Unknown | Puerto Rico, Hispaniola (the Dominican Republic) | Unknown | >100 | [11] | ||
Three | September 9–13 | Category 1 hurricane | 80 (130) | 985 | Florida | Unknown | None | |||
Four | September 22–30 | Category 1 hurricane | 90 (150) | Unknown | Lesser Antilles, Bahamas | Unknown | None | |||
Five | October 6–11 | Category 2 hurricane | 105 (165) | 965 | Jamaica, Southeastern United States (Florida) | Unknown | None | |||
Season aggregates | ||||||||||
5 systems | August 19 – October 11 | 115 (185) | 961 | >$1 million | >100 |
The 1950 Atlantic hurricane season was the first year in the Atlantic hurricane database (HURDAT) that storms were given names in the Atlantic basin. Names were taken from the Joint Army/Navy Phonetic Alphabet, with the first named storm being designated "Able", the second "Baker", and so on. It was a very active season with sixteen tropical storms, with eleven of them developing into hurricanes. Six of these hurricanes were intense enough to be classified as major hurricanes—a denomination reserved for storms that attained sustained winds equivalent to a Category 3 or greater on the present-day Saffir–Simpson scale. One storm, the twelfth of the season, was unnamed and was originally excluded from the yearly summary, and three additional storms were discovered in re-analysis. The large quantity of strong storms during the year yielded, prior to modern reanalysis, what was the highest seasonal accumulated cyclone energy (ACE) of the 20th century in the Atlantic basin; 1950 held the seasonal ACE record until broken by the 1995 Atlantic hurricane season. However, later examination by researchers determined that several storms in the 1950 season were weaker than thought, leading to a lower ACE than assessed originally. This season also set the record for the most tropical storms, eight, in the month of October.
The 1949 Atlantic hurricane season was the last season that tropical cyclones were not publicly labeled by the United States Weather Bureau. It officially began on June 15, and lasted until November 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first storm, a tropical depression, developed in the northern Gulf of Mexico on August 14. The final system, Tropical Storm Sixteen, dissipated in the southwestern Caribbean Sea on November 5. It was a fairly active season, featuring 16 tropical storms and seven hurricanes. Two of these strengthened into major hurricanes, which are Category 3 or higher on the Saffir–Simpson hurricane wind scale.
The 1930 Atlantic hurricane season was the second least active Atlantic hurricane season on record in terms of tropical storms formed, only behind 1914, with only three systems reaching tropical storm intensity. Of those three, two reached hurricane status, both of which also became major hurricanes, Category 3 or higher storms on the Saffir–Simpson hurricane wind scale. The first system developed in the central Atlantic Ocean on August 21. Later that month, a second storm, the Dominican Republic hurricane, formed on August 29. It peaked as a Category 4 hurricane with winds of 155 mph (250 km/h). The third and final storm dissipated on October 21.
The 1929 Atlantic hurricane season was among the least active Atlantic hurricane seasons on record, with only five tropical cyclones forming. Three of them intensified into a hurricane, with one strengthening further into a major hurricane. The first tropical cyclone of the season developed in the Gulf of Mexico on June 27. Becoming a hurricane on June 28, the storm struck Texas, bringing strong winds to a large area. Three fatalities were reported, while damage was conservatively estimated at $675,000 (1929 USD).
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 1920 Atlantic hurricane season featured tropical storms and hurricanes only in the month of September. The first system, a hurricane, developed on September 7 while the last, a tropical depression, transitioned into an extratropical cyclone on October 27. Of note, four of the six cyclones co-existed with another tropical cyclone during the season.
The 1919 Atlantic hurricane season was among the least active hurricane seasons in the Atlantic on record, featuring only five tropical storms. Of those five tropical cyclones, two of them intensified into a hurricane, with one strengthening into a major hurricane Two tropical depressions developed in the month of June, both of which caused negligible damage. A tropical storm in July brought minor damage to Pensacola, Florida, but devastated a fleet of ships. Another two tropical depressions formed in August, the first of which brought rainfall to the Lesser Antilles.
The 1918 Atlantic hurricane season was inactive, with a total of six tropical storms developing, four of which intensified into hurricanes. Two of the season's hurricanes made Landfall in the United States, and one became a major hurricane, which is Category 3 or higher on the modern-day Saffir–Simpson scale. Additionally, there were four suspected tropical depressions, including one that began the season on June 19 and one that ended the season when it dissipated on October 19. The early 20th century lacked modern forecasting and documentation, and thus, the hurricane database from these years may be incomplete. Four previously unknown tropical cyclones were identified using records, including historical weather maps and ship reports, while information on the known storms was amended.
The 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 hurricane wind 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 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 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 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 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 1926 Nassau hurricane also known as the San Liborio hurricane or The Great Bahamas Hurricane of 1926, in Puerto Rico, was a destructive Category 4 hurricane that affected the Bahamas at peak intensity. Although it weakened considerably before its Florida landfall, it was one of the most severe storms to affect the Bahamian capital Nassau and the island of New Providence in several years until the 1928 Okeechobee hurricane, which occurred just two years later. The storm also delivered flooding rains and loss of crops to the southeastern United States and Florida. Being a slightly mid-range Category 4, this hurricane peaked at about 967 mbars, making it the least intense Category 4 Atlantic hurricane on record, especially for wind speeds of 140 mph.
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 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 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, with only two tropical storms and three hurricanes, two of which were major hurricanes, being recorded. 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 cyclones, large alterations were made to the tracks of Hurricane Two and Hurricane Five in 1995 by Jose Fernandez-Partagas and Henry Diaz, who also proposed smaller changes to the known track of Hurricane Three. All of the tropical cyclones, other than Hurricane Two, made landfall in Florida.
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.