The 1842 Atlantic hurricane season featured several maritime catastrophes in the Gulf of Mexico and along the U.S. East Coast, and produced one of the only known tropical cyclones to directly affect the Iberian Peninsula. As the season falls outside the scope of the Atlantic hurricane database, records of most storms in 1842 are scarce, and only approximate tracks are known. The first documented storm of the season battered the coast of North Carolina in mid-July, wrecking dozens of ships and destroying homes along the Outer Banks. A little over a month later, another storm impacted the same region and caused several more shipwrecks that killed at least 12 men. This storm later doused the Mid-Atlantic states with flooding rains. In early September, a powerful storm known as "Antje's Hurricane"—named after a ship that it dismasted—tracked generally westward after first being spotted over the Leeward Islands. After yielding widespread destruction across the Bahamas, the storm traversed the Florida Straits, causing severe damage in both northern Cuba and the lower Florida Keys. Many ships and their crews were lost to the storm as it crossed the Gulf of Mexico; it finally struck northern Mexico on September 8.
Another intense hurricane churned the Gulf of Mexico in early October, this time tracking from southwest to northeast. The storm moved very slowly and sank or impaired numerous ships along its course. Striking northern Florida on October 5 as the equivalent of a major hurricane, the cyclone produced extreme wind gusts to the north of its center and exceptionally high tides to the south. Extensive property damage in Tallahassee accounted for an estimated $500,000 (1842 USD) in losses. On Cedar Key, the storm surge demolished buildings and threatened to submerge the island. The storm turned northward as it entered the western Atlantic, resulting in strong winds and flooding tides in Savannah, Georgia, and Charleston, South Carolina. Later in the month, an extremely rare hurricane formed in the far eastern Atlantic, to the southwest of Madeira. This storm passed near the islands on October 27 before making landfall in southwestern Spain. Accompanied by significant damage, both along the coast and inland, this storm is considered a historical analogue to Hurricane Vince of 2005. Several other storms also had an impact on land throughout the season.
Attempts to catalog Atlantic hurricanes in the first half of the 19th century began as early as 1855, when Andrés Poey compiled information on just over 400 tropical cyclones from 1493 to 1855. [1] Poey's work serves as the basis for much of what is currently known about historical Atlantic tropical cyclones. [2] He identified four distinct tropical systems that developed in 1842 (six events are listed, though two concern the same storm), plus another in November that was later deemed extratropical in nature. [3] In his 1963 book, Early American Hurricanes, 1492–1870, weather researcher David M. Ludlum discussed, in greater detail, six significant tropical cyclones that impacted the United States in 1842. [4] As the season falls outside the scope of the Atlantic hurricane database (1851 onward) and its associated reanalysis project, [5] records are regarded as incomplete.
1) The first documented hurricane of 1842 severely affected coastal North Carolina from Wilmington to Currituck on July 12. Its center likely remained just east of Cape Hatteras as it washed away houses, drowned livestock, and wreaked havoc on shipping interests. [6] Nearly 30 ships ran aground near Ocracoke Inlet, and two unidentified vessels were wrecked on the shoals near Cape Hatteras with all hands lost; seven more men drowned while trying to salvage goods from the shipwrecks. [7] In late October, a message in a bottle was recovered at Bermuda with an account of the storm from the captain and first mate of the imperiled schooner Lexington, presumed lost at sea. [7] In total, around 40 ships were lost. [8] Although sparse records preclude an accurate death toll, the National Hurricane Center lists the cyclone among those that may have caused 25 or more fatalities. [9]
Described by one writer as "one of the worst in the history of coastal Carolina", the storm reportedly demolished all but one structure in the village of Portsmouth. Further inland, at Washington, damaging gale-force winds continued through July 13 and 14, and boats in the Albemarle Sound broke free of their moorings. Part of the Wilmington and Raleigh Railroad was washed out, preventing mail from reaching Charleston, South Carolina. After its close pass to North Carolina, the storm moved toward the northwest and made landfall near Norfolk, Virginia. Torrential rainfall affected the Mid-Atlantic states, with flooding reported along major rivers; the Schuylkill River in Philadelphia, for instance, rose 5 ft (1.5 m) over its banks. [7]
2) Based on an August 2 diary entry describing heavy rainfall and gusty northeasterly winds at Fort George Island, a tropical storm is believed to have made landfall just south of there. [10] In southeastern Georgia, the storm negatively affected the cotton crop that was already suffering from persistent drought conditions. [11]
3) Another damaging tropical cyclone, "hardly less severe" and reportedly of a much longer duration than the July hurricane, [9] [12] struck the Outer Banks of North Carolina on August 24. The storm wrecked numerous vessels, [13] among them being the Kilgore at Currituck, the Pioneer and the Granary at Ocracoke, and the Congress at Cape Hatteras. At least 12 men died in these shipwrecks. [14] [12] As the storm continued northward, severe weather conditions affected the Mid-Atlantic and Northeastern states on August 25. Extensive flooding in Washington, D.C. turned Pennsylvania Avenue into "a broad river" and inundated homes and cellars, with losses in the city estimated at $50,000 (1842 USD). Streets, wharves, shipyards, and lumberyards in Baltimore were submerged, while further north, hurricane-force winds and a flooding storm surge affected New York City. [15]
4) "Antje's Hurricane" took its name from the ship HMS Antje, which was dismasted by the cyclone in the western Atlantic on August 30. [16] [17] This cyclone was first noted in the Leeward Islands in late August, [18] and went on to ruin over 100,000 bushels of salt across the Turks and Caicos Islands. [19] Overspreading the Bahamas on September 2 and 3, the storm caused "very great" damage and loss of life throughout the island chain. In particular, reports indicated that most of the homes were destroyed on Watlings Island in the eastern Bahamas. [20] The storm passed through the Florida Straits on September 4. Barometric pressure fell to 28.93 inHg (980 mbar ) at Havana, where strong winds persisted for 36 hours. The storm sank several boats and damaged many others in Havana Harbor, while on land, the winds blew down trees and small buildings. [21]
The lower Florida Keys were battered; "half of Sand Key was blown away", including the lightkeeper's house, [16] and extensive damage to buildings and vegetation was reported on Key West. [22] However, the offshore wind apparently allowed Key West to escape with relatively light shipping losses. The storm subsequently followed a path due westward across the Gulf of Mexico. [17] Along the hurricane's course, many vessels—such as the brig Chili, en route to Havana—were lost with their crews. [23] [24] By September 8, the cyclone had made landfall along the coast of Tamaulipas in Mexico, and the eye passed directly over Ciudad Victoria as evidenced by a brief, five-minute lull. Heavy rain swept across southern Texas as the cyclone dissipated over mountainous terrain. [16]
5) On the night of September 17–18, a new tropical storm in the northwestern Gulf of Mexico affected Galveston, Texas. Northerly winds drove water from Galveston Bay over the island to a depth of up to 4 ft (1.2 m). [25] The storm surge destroyed several structures and washed ashore small boats, while strong winds heavily damaged two churches. [16] Many families were forced to evacuate their homes in the middle of the night by wading through floodwaters to reach higher ground. [26] Estimates of total monetary damage ranged from $10,000 to as high as $50,000. [16] [26] Though no people lost their lives, 40 cattle were killed in a building collapse. [25]
6) Several days later, the Florida Panhandle experienced the effects of a tropical storm, marked by gale-force winds at Pensacola on September 22 and 23. No appreciable damage was reported. Ludlum considered that this may have been a continuation of the Galveston storm, but judged it to be a separate system. [16]
7) The most destructive storm of the season can be traced back to near Saint Thomas at the end of September. [4] By the beginning of October, it had tracked into the extreme southern Bay of Campeche. For several days, the strengthening storm battered ships as it turned northeastward through the Gulf of Mexico, with numerous vessels lost and many more damaged. [27] [28] The steamship Merchant began taking on water on October 3, and the next day she broke up after running aground several hundred yards offshore. All but 8 of the 72 passengers were rescued on October 5. [29] [30] The brig Cuba and about 14 passengers were lost off Key West. [31] During this period, many birds died over open waters after becoming trapped in the circulation of the slow-moving hurricane. [27] The system delivered a glancing blow to Galveston, where the storm surge flooded streets and a few buildings were blown down. [25]
The storm buffeted Florida for an extended period from October 4 through 6, [27] and moved ashore just north of Cedar Key as the equivalent of a major hurricane on the modern-day Saffir–Simpson scale. The minimum central pressure at the time of landfall has been estimated at 955 mb (28.2 inHg). [10] [32] "Extreme" winds in the northern side of the hurricane proved devastating along the Florida Panhandle. In Apalachicola, a lighthouse and keeper's house were destroyed, and a multitude of homes were unroofed. Several people in the area drowned in storm surge flooding. In Tallahassee, the storm wrought $500,000 in losses in the form of widespread structural damage. Thousands of trees were blown down throughout the region, [27] and a significant portion of the cotton crop was lost. Two slaves on a plantation near Tallahassee were injured, one of them severely. [33] To the south of the storm center, Cedar Key faced exceptionally high tides that swept entire homes away and threatened to submerge the island. [27] [34] Several ships were wrecked along the coast of Florida. [34]
The hurricane continued northeastward across northern Florida before emerging into the Atlantic between Mayport and St. Augustine. [10] [27] At the latter city, the storm was regarded as the most severe in 15 years; fences, trees, and crops were destroyed, [35] and a few ships were driven aground, though the sea wall largely protected St. Augustine. [34] Winds at Savannah, Georgia increased to hurricane strength on the night of October 5–6 and were accompanied by torrential rains. [27] The storm surge there flooded wharves and other low-lying areas. [36] The slow-moving storm buffeted the southern Georgia Sea Islands with a prolonged period of strong winds and heavy rain, blowing down trees and destroying some houses. Rice plantations along the Altamaha River experienced significant losses. [37] "Unprecedented" tides also flooded streets farther up the coast in Charleston, South Carolina, [38] such that some residents had to be rescued from their homes by boat. Though damage there was generally minor, five slaves drowned when their fishing boat capsized in rough seas. [39] As the hurricane moved away from the coast, several ships were lost off North Carolina. On October 8 and 9, Bermuda experienced strong winds as the storm passed nearby. [27]
8) In late October, a highly unusual tropical cyclone formed in the far eastern Atlantic, first detected to the southwest of Madeira on October 24. [4] On October 26, a ship near Madeira recorded a barometric pressure of 965 mb (28.5 inHg), suggesting a hurricane of Category 2 intensity. [40] The hurricane passed just north of Madeira on October 27, producing heavy damage in Funchal. After brushing the northwestern coast of Morocco on the night of October 28–29, [41] the hurricane moved ashore over southwestern Spain and likely became extratropical shortly thereafter. As a result of the extratropical transition, damaging winds extended far from the storm center and affected much of inland Spain. [42] Dozens of ships, including three belonging to the Spanish Navy, were lost or severely damaged in the storm. Two bridges were washed away in Cádiz and homes were destroyed in Seville. [41] [43] Hurricane-force winds reached as far inland as Madrid, and thousands of trees were uprooted in the province of Badajoz. [44] This storm serves as an important historical analogue for Hurricane Vince, which followed a similar course in October 2005. [45]
9) Around the same time, a separate tropical cyclone formed in the western Atlantic. It moved from off the coast of Florida to near Bermuda between October 24 and November 1, [4] brushing the coast from St. Augustine to Charleston with gale-force winds. No significant damage occurred, [27] though coastal flooding and heavy rainfall that caused a break in an earthen dam were reported along the coast of Georgia. [39]
The decade of the 1820s featured the 1820s Atlantic hurricane seasons. While data is not available for every storm that occurred, some parts of the coastline were populated enough to give data of hurricane occurrences. Each season was an ongoing event in the annual cycle of tropical cyclone formation in the Atlantic basin. Most tropical cyclone formation occurs between June 1 and November 30.
The decade of the 1830s featured the 1830s Atlantic hurricane seasons. While data is not available for every storm that occurred, some parts of the coastline were populated enough to give data of hurricane occurrences. Each season was an ongoing event in the annual cycle of tropical cyclone formation in the Atlantic basin. Most tropical cyclone formation occurs between June 1 and November 30.
This article encompasses the 1840–1849 Atlantic hurricane seasons. While data is not available for every storm that occurred, some parts of the coastline were populated enough to give data of hurricane occurrences. Each season was an ongoing event in the annual cycle of tropical cyclone formation in the Atlantic basin. Most tropical cyclone formation occurs between June 1 and November 30.
The decade of the 1810s featured the 1810s Atlantic hurricane seasons. While data is not available for every storm that occurred, some parts of the coastline were populated enough to give data of hurricane occurrences. Each season was an ongoing event in the annual cycle of tropical cyclone formation in the Atlantic basin. Most tropical cyclone formation occurs between June 1 and November 30.
The decade of the 1800s featured the 1800s Atlantic hurricane seasons. While data is not available for every storm that occurred, some parts of the coastline were populated enough to give data of hurricane occurrences. Each season was an ongoing event in the annual cycle of tropical cyclone formation in the Atlantic basin. Most tropical cyclone formation occurs between June 1 and November 30.
The 1821 Norfolk and Long Island Hurricane was one of four known tropical cyclones that have made landfall in New York City. Another, even more intense hurricane in pre-Columbian times left evidence that was detected in South Jersey by paleotempestological research. The third was the 1893 New York hurricane, and the fourth was Hurricane Irene in 2011.
The 1846 Havana hurricane was the most intense tropical cyclone in recorded history for 78 years and the first known Category 5-strength hurricane to strike Cuba. The first indications of the formation of a disturbance were first noted on 5 October in the Caribbean Sea, but little else was known until the storm approached Cuba on 10 October. There, it brought extreme winds and the lowest known atmospheric pressure of the time – 938 millibars (27.7 inHg) – a record which remained unbroken until the development of a later cyclone in 1924. It soon curved toward Florida, where it maintained its intensity, continuing to rapidly hasten northward along the East Coast of the United States to New England. It entered an extratropical transition while situated over New York on 13 October, producing intense Category 2-force winds and unusually little precipitation. Eventually, the gale dissipated over the Canadian Maritimes the following day as a markedly weaker storm.
The 1852 Atlantic hurricane season was one of only three Atlantic hurricane seasons in which every known tropical cyclone attained hurricane status. 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. 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.
The 1860 Atlantic hurricane season featured three severe hurricanes that struck Louisiana and the Gulf Coast of the United States within a period of seven weeks. The season effectively began on August 8 with the formation of a tropical cyclone in the eastern Gulf of Mexico, and produced seven known tropical storms and hurricanes until the dissipation of the last known system on October 24. Six of the seven storms were strong enough to be considered hurricanes on the modern-day Saffir–Simpson Hurricane Scale, of which four attained Category 2 status and one attained Category 3 major hurricane strength. The first hurricane was the strongest in both winds and pressure, with peak winds of 125 miles per hour (201 km/h) and a barometric pressure of 950 millibars (28 inHg). Until contemporary reanalysis discovered four previously unknown tropical cyclones that did not affect land, only three hurricanes were known to have existed; all three made landfall in Louisiana, causing severe damage.
The 1861 Atlantic hurricane season occurred during the first year of the American Civil War and had some minor impacts on associated events. Eight tropical cyclones are believed to have formed during the 1861 season; the first storm developed on July 6 and the final system dissipated on November 3. Six of the eight hurricanes attained Category 1 hurricane status or higher on the Saffir-Simpson Hurricane Scale, of which three produced hurricane-force winds in the United States. No conclusive damage totals are available for any storms. Twenty-two people died in a shipwreck off the New England coast, and an undetermined number of crew members went down with their ship in the July hurricane. Based on maximum sustained winds, the first and third hurricanes are tied for the strongest of the year, although the typical method for determining that record—central barometric air pressure—is not a reliable indicator due to a general lack of data and observations.
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 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. Operationally, another tropical storm was believed to have existed offshore Atlantic Canada in late August and early September, but HURDAT – the official Atlantic hurricane database – now excludes this system. The first system, Hurricane One, was initially observed on August 6. The final storm, Hurricane Five, was last observed 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, so storm summaries for those systems are unavailable.
The 1857 Atlantic hurricane season was the earliest season documented by HURDAT – the official Atlantic hurricane database – to feature no major hurricanes. A total of four tropical cyclones were observed during the season, three of which strengthened into 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 has been estimated. Additionally, documentation by Jose Fernandez-Partagas and Henry Diaz included a fifth tropical cyclone near Port Isabel, Texas; this storm has since been removed from HURDAT as it was likely the same system as the fourth tropical cyclone.
The 1815 North Carolina hurricane caused the most severe flooding in New Bern, North Carolina since 1795. First detected east of the Lesser Antilles on 26 August, the disturbance drifted toward the northwestern Leeward Islands, arriving by 29 August. The hurricane soon approached Charleston, South Carolina, on 1 September, and subsequently made landfall near Cape Lookout in North Carolina on 3 September. The gale reached New England by 5 September, departing the region on 6 September. The hurricane caused significant impact even before coming ashore: many vessels were damaged, grounded, capsized, or destroyed offshore throughout the course of the storm. Extensive damage to corn, cotton, and rice crops was also noted. Flood waters brought rivers as much as 8 ft (2.4 m) above normal, inundating streets and structures. Overall, the hurricane inflicted at least 15 deaths throughout its existence, and more than $60,000 (1815 USD) in property damage.
The 1850 Atlantic hurricane season was the last season excluded from the scope of the official Atlantic hurricane database. Although meteorological records are sparse and generally incomplete, they indicate that three significant tropical cyclones affected land, each causing some degree of damage. The first system struck North Carolina on July 18, causing significant damage before battering the Mid-Atlantic states with high tides, strong winds, and heavy rainfall. Torrential rainfall caused river flooding from Baltimore to Philadelphia, particularly along the Schuylkill River, which took the lives of 20 people in various incidents. Strong winds damaged property and public facilities in and around New York City, and damaging floods extended into central and northern New England. Crops and railroad infrastructure suffered throughout the entire region.
The 1933 Florida–Mexico hurricane was the first of two Atlantic hurricanes to strike the Treasure Coast region of Florida in the very active 1933 Atlantic hurricane season. It was one of two storms that year to inflict hurricane-force winds over South Texas, causing significant damage there; the other occurred in early September. The fifth tropical cyclone of the year, it formed east of the Lesser Antilles on July 24, rapidly strengthening as it moved west-northwest. As it passed over the islands, it attained hurricane status on July 26, producing heavy rains and killing at least six people. Over the next three days, it moved north of the Caribbean, paralleling the Turks and Caicos Islands and the Bahamas. The storm produced extensive damage and at least one drowning as it crossed the Bahamas. On July 29, the cyclone came under the influence of changing steering currents in the atmosphere, which forced the storm into Florida near Hobe Sound a day later. A minimal hurricane at landfall, it caused negligible wind damage as it crossed Florida, but generated heavy rains along its path, causing locally severe flooding. The storm turned west, weakened to below hurricane status, and later exited the state north of Charlotte Harbor on July 31.
Racer's hurricane was a destructive tropical cyclone that had severe effects in northeastern Mexico, the Republic of Texas, and the Gulf Coast of the United States in early October 1837. It was named after the Royal Navy ship HMS Racer, which encountered the cyclone in the northwestern Caribbean. Termed "one of the most famous and destructive hurricanes of the century" by meteorology historian David Ludlum, the storm first affected Jamaica with flooding rainfall and strong winds on September 26 and 27, before entering the Gulf of Mexico by October 1. As the hurricane struck northern Tamaulipas and southern Texas, it slowed to a crawl and turned sharply northeastward. The storm battered the Gulf Coast from Texas to the Florida Panhandle between October 3 and 7. After crossing the Southeastern United States, it emerged into the Atlantic shipping lanes off the Carolinas by October 9.
The 1896 East Coast hurricane was a slow-moving tropical cyclone that battered the East Coast of the United States from Florida to New England in mid-October 1896. The fifth tropical cyclone of the 1896 Atlantic hurricane season, it formed on October 7 in the southern Gulf of Mexico, and caused minor damage in Florida while crossing the state two days later. From October 10 through 13, the hurricane drifted northeastward along the coast, reaching its peak intensity as the equivalence of a Category 2 hurricane on the modern-day Saffir–Simpson scale. The hurricane subjected many areas along the East Coast to days of high seas and damaging northeasterly winds, which halted shipping operations.