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.
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 1810s witnessed a series of tumultuous and devastating Atlantic hurricane seasons. These powerful tropical cyclones left a profound impact on the coastal regions and communities of the Americas. In this article, we will delve into the history of the 1810s Atlantic hurricane seasons, exploring their significance, notable storms, and the lessons learned from these natural disasters.
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 1780 Atlantic hurricane season ran through the summer and fall in 1780. The 1780 season was extraordinarily destructive, and was the deadliest Atlantic hurricane season in recorded history, with over 28,000 deaths. Four different hurricanes, one in June and three in October, caused at least 1,000 deaths each; this event has never been repeated, and only in the 1893 and 2005 seasons were there two such hurricanes. The season also had the deadliest Atlantic hurricane of all time, the Great Hurricane of 1780. Only one of the known storms was not a hurricane.
The 1870 Atlantic hurricane season lasted from mid-summer to late-fall and comprised one tropical storm and ten hurricanes, two of which became 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.
The 1848 Tampa Bay hurricane was the strongest known hurricane to impact the Tampa Bay area of the U.S. state of Florida. Along with the 1921 Tampa Bay hurricane, it is one of only two major hurricanes to make landfall along Central Florida's west coast since Florida became a United States territory in 1821.
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. Of the six storms, three only have a single point in their track known.
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 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.
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 1806 Great Coastal hurricane was a severe and damaging storm along the East Coast of the United States which produced upwards of 36 in (91 cm) of rainfall in parts of Massachusetts. First observed east of the Lesser Antilles on 17 August, the hurricane arrived at the Bahamas by 19 August. The disturbance continued to drift northward and made landfall at the mouth of the Cape Fear River in North Carolina on 22 August. The storm soon moved out to sea as a Category 2-equivalent hurricane on the Saffir–Simpson hurricane wind scale, persisting off of New England before dissipating south of Nova Scotia on 25 August as a markedly weaker storm. Several French and British warships were damaged out at sea.
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 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.
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.
