1874 Atlantic hurricane season | |
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Seasonal boundaries | |
First system formed | July 2, 1874 |
Last system dissipated | November 4, 1874 |
Strongest storm | |
Name | Seven |
• Maximum winds | 100 mph (155 km/h) (1-minute sustained) |
Seasonal statistics | |
Total depressions | 7 |
Total storms | 7 |
Hurricanes | 4 |
Total fatalities | 1 |
Total damage | Unknown |
The 1874 Atlantic hurricane season was a relatively inactive one, in which seven tropical cyclones developed. Four storms intensified into hurricanes, but none attained major hurricane (Category 3+) 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. [1]
The first storm of the season developed on July 2, and the final storm was last sighted on November 4, while situated just to the north of the Bahamas. Most of the systems directly impacted land. A tropical storm that developed in the Bay of Campeche during the month of September destroyed the Brazos Santiago lighthouse. [2] in the state of Texas. The sixth storm of the season, and also the third hurricane, made landfall in Florida as a Category 1 hurricane before making a second landfall in South Carolina at the same intensity. The seventh, final, and strongest system of the season developed in the Caribbean on the last day of October, and made landfall in Jamaica as a Category 2 hurricane before weakening to a tropical storm by the time it made a second landfall in Eastern Cuba. The storm was last sighted to the north of the Bahamas on November 4, as a Category 1 hurricane.
The Atlantic hurricane database (HURDAT) officially recognizes seven tropical cyclones from the 1874 season. Four storms attained hurricane status, with winds of 75 miles per hour (121 km/h) or greater. The seventh hurricane of the season was the most intense, with maximum sustained winds up to 100 mph (160 km/h). The first storm of the season was a tropical storm that formed in the Gulf of Mexico during the month of July. The system made landfall near Galveston, Texas on July 5, although it is unknown whether any damages or fatalities were caused as a result of the storm. The second and third systems of the season were both hurricanes, with winds up to 80 and 90 mph (130 and 140 km/h) respectively. The first system made landfall in Newfoundland as a tropical storm. In early September, another tropical system developed in the Bay of Campeche and made landfall in Northeast Mexico with winds up to 60 mph (97 km/h). The fifth storm of the season formed northeast of the Bahamas on September 8, and moved northward before turning to the north-northeast. It was last sighted to the south of Newfoundland on September 11. The next system developed in the western Caribbean on the last day of October, before crossing over the Yucatan Peninsula and making landfall in Florida as a Category 1 hurricane. The storm briefly weakened to a tropical storm over the state before restrengthening into a hurricane off the coast of Georgia. It made a second landfall in South Carolina on September 28, and became extratropical on September 30, while moving across the northeast. This was the first hurricane to ever be shown on a weather map. The seventh, and final, hurricane of the season was also the most intense of the year. It developed several hundred miles north of Panama on the last day of October, before striking Jamaica as a Category 2 hurricane. It weakened to a tropical storm before making landfall in Eastern Cuba, but later strengthened into a hurricane again while north of the Bahamas, where it was last sighted on November 4.
Tropical storm (SSHWS) | |
Duration | July 2 – July 5 |
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Peak intensity | 60 mph (95 km/h) (1-min); |
Based on the Monthly Weather Review , [3] : 35 a tropical storm was first noted over the east-central Gulf of Mexico on July 2 about 200 mi (320 km) west-southwest of present-day Naples, Florida. Moving westward, the tropical storm steadily strengthened to reach a peak intensity of 60 mph (95 km/h) on July 3. The system later made landfall near Port O'Connor, Texas, on July 5, likely around the same intensity, and then rapidly dissipated shortly after moving inland that same day. [4]
In the vicinity of Indianola, Texas, the storm blew down fledgling settlements and sank ships, seriously hindering coastal trade. [5] Climate researcher Michael Chenoweth proposed the removal of this storm in a 2014 study, noting there was "No evidence in land-based reports or from ships". [6]
Category 1 hurricane (SSHWS) | |
Duration | August 3 – August 7 |
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Peak intensity | 80 mph (130 km/h) (1-min); |
Although the no observations of this system exist prior to August 5, a 1993 reanalysis by C. J. Neumann and others began the track of cyclone two days earlier, about 700 mi (1,125 km) northeast of the Lesser Antilles. [3] : 35 Slowly gaining strength, the system reached hurricane status and peaked with maximum sustained winds of 80 mph (130 km/h) while located just northeast of the island of Bermuda on August 5, [4] based on a ship recording sustained winds of 81 mph (130 km/h). [7] Late on August 6, the storm turned northeastward as it approached Atlantic Canada. The system then weakened back to a tropical storm on August 7, and made landfall on Newfoundland the same day, with sustained winds up to 70 mph (110 km/h). It dissipated shortly afterwards. [4]
Chenoweth theorized that this system developed as a subtropical storm offshore the Mid-Atlantic and moved mostly northeastward. The storm transitioned into a tropical storm but failed to attain hurricane status prior to becoming extratropical late on August 6, almost 24 hours before reaching Newfoundland. [6]
Category 1 hurricane (SSHWS) | |
Duration | August 29 – September 7 |
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Peak intensity | 90 mph (150 km/h) (1-min); ≤980 mbar (hPa) |
The bark Colchaqua encountered this storm nearly 900 mi (1,450 km) west of the Capo Verde Islands on August 29, recording sustained winds of 46 mph (74 km/h). [7] Moving towards the west-northwest, the storm steadily gained strength, and reached hurricane strength early on September 2. The storm peaked its peak intensity of September 6 with sustained winds of 90 mph (150 km/h) and a minimum atmospheric pressure of 980 mbar (29 inHg), [4] the former recorded by the ship Swallow and the latter by the ship State of Virginia. [7] Moving just to the west of Bermuda, the cyclone began to turn more northerly, and transitioned into an extratropical cyclone later on September 7. By the following day, the system made landfall in Newfoundland as an extratropical system. [4]
On Bermuda, the hurricane generated huge swells and strong winds, causing sea spray that defoliated plants across the territory. [8] Approximately 1 in (25 mm) of rain fell in Halifax, Nova Scotia, during a 3.5 hour-period as a result of the storm. [3] : 37 The 2014 reanalysis study by Chenoweth concludes that this storm formed on September 2 and intensified more than HURDAT suggests, peaking as a strong Category 2 hurricane. [6]
Tropical storm (SSHWS) | |
Duration | September 2 – September 7 |
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Peak intensity | 60 mph (95 km/h) (1-min); |
On September 2, a tropical storm developed in the Bay of Campeche. Moving generally towards the west-northwest, the storm reached a peak intensity of 60 mph (95 km/h) on September 4, while approaching northeastern Mexico. Shortly thereafter, the cyclone made landfall in northern Tamaulipas and weakened into a tropical depression on September 5, several hours after crossing into Texas. Moving northward through the state, the storm dissipated on September 7, while located to the southwest of the Dallas–Fort Worth area. [4] Chenoweth argued that this system developed as a tropical depression near the central Gulf of Mexico on September 1 and became much more intense, reaching Category 3 intensity on September 5. The system struck south Texas later that day. [6]
In Mexico, the storm demolished some homes and all huts along the coast in Bagdad. Telegraph wires in the town were also almost completely destroyed. Farther inland, towns in Nuevo León reported flooding, with several bridges swept away in the vicinity of Cerralvo. [9] The system generated rough seas along the coast of Texas, especially in Corpus Christi. Waves destroyed bathhouses and wharves and beached several schooners, some of which collided with homes and trees. Abnormally high tides also destroyed salt lakes on Padre Island, ending a salt boom. The storm was responsible for destroying the Brazos Santiago lighthouse and causing one fatality. [2]
Tropical storm (SSHWS) | |
Duration | September 8 – September 11 |
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Peak intensity | 60 mph (95 km/h) (1-min); |
Based on a combination of the tracks created by Ivan Ray Tannehill in 1938 and a reanalysis led by C. J. Neumann in 1993, [3] : 39 HURDAT begins the path of a tropical storm about 275 mi (445 km) north of Turks and Caicos Islands on September 8. Moving towards the west-northwest, the system is estimated to maintained sustained winds of 60 mph (95 km/h) as it passed between North Carolina and Bermuda. Turning towards the northeast, it was last observed to the south of Newfoundland on September 11. [4] Chenoweth also argued for the removal of this cyclone from HURDAT, noting there was "No evidence in land-based reports or from ships". [6] A ship known as Titan recorded sustained winds of September 12. [7] However, it could not be determined if the Titan actually encountered the storm, given that the location was not logged. [3] : 40
Category 1 hurricane (SSHWS) | |
Duration | September 25 – September 30 |
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Peak intensity | 90 mph (150 km/h) (1-min); 981 mbar (hPa) |
On September 25, a tropical storm was first noted in the western Caribbean, north of Honduras. Upon striking the Yucatán Peninsula shortly afterwards, the storm briefly weakened into a tropical depression. However, when the system emerged into the Gulf of Mexico, it attained tropical storm status once again. Steadily gaining strength, the cyclone reached hurricane status on September 28, after reports from the ship Emma D. Finney indicated such. [10] Moving north-northeastward, the storm made landfall near Cedar Key, Florida several hours later, with an estimated minimum central pressure of 981 mbar (29.0 inHg). The system briefly fell to tropical storm status over the state, but strengthened into a hurricane again after exiting near Jacksonville and crossing the Gulf Stream. It hit South Carolina as a hurricane that same day, with the center passing just east of Charleston and west of Wilmington. [11] : 13 The storm lost hurricane status again over eastern North Carolina. Thereafter, the system crossed the northeastern United States, becoming extratropical on September 30 over Maine. On October 1, it dissipated over eastern Canada. [4]
Few reports of damage in Florida exist. [12] : 68 Jacksonville observed sustained winds of 48 mph (77 km/h). Stronger winds impacted coastal Georgia, with a sustained wind speed of 68 mph (109 km/h) at the Tybee Island Lighthouse. Tides generated by the storm inundated portions of the island with up to 3 ft (0.91 m) of water. [13] Heavy rainfall in the Savannah area raised the height of the river to its highest height in 20 years and flooded many rice plantations, causing about $100,000 in damage. [14] Coastal flooding also occurred in South Carolina, including in Charleston, where parts of The Battery were swept away. [15] In North Carolina, Virginia, and several other states to the north, there were reports of trees being brought down, and shipping disrupted. At Smithville (present-day Southport) several houses, warehouses, telegraph lines and railroad bridges were destroyed. Additionally, about 33% of rice crops along the Cape Fear River were damaged. [11] : 13 This was also the first hurricane ever to be recorded on a weather map by the U.S. Weather Bureau. [16] The reanalysis study authored by Chenoweth proposed few changes to this system compared to HURDAT, other than some small eastward and westward along different sections of the track and a slightly earlier extratropical transition. [6]
Category 2 hurricane (SSHWS) | |
Duration | October 31 – November 4 |
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Peak intensity | 105 mph (165 km/h) (1-min); |
The track for this storm begins about 290 mi (465 km) northwest of Barranquilla, Colombia, on October 31, [4] one day before Jamaica first observed sustained hurricane-force winds. [7] Moving towards the east-northeast, the storm attained hurricane status on November 1, while situated just south of Jamaica. Upon making landfall in the island nation near Rocky Pointon November 2, the storm strengthened into a Category 2 hurricane with 105 mph (165 km/h) winds. After crossing Jamaica, the system weakened into a Category 1 hurricane and then further into a tropical storm prior to making landfall in eastern Cuba late on November 2. The system emerged in the Bahamas on the next day, and strengthened into a hurricane once again early on November 4. Several hours later, the hurricane was last sighted to the northeast of the Bahamas. [4]
On Jamaica, Kingston reported sustained winds of 81 mph (130 km/h). [7] According to a telegraph from the city, the hurricane wrecked or destroyed 17 vessels. [3] Heavy rains led to landslides and floods that swept away some bridges and animals, while winds damaged crops, toppled many trees, [17] and severely damaged or destroyed a number of homes. [18] At least five deaths occurred and damage in the Kingston area alone reached $75,000. [19] Chenoweth's study begins the track of this storm to the southeast of Jamaica. The storm instead moves northwestward across the island and then curved north-northeastward thereafter, striking Cuba north of Manzanillo. Thereafter, the cyclone treks slightly farther west over the Bahamas. [6]
Chenoweth proposed two other storms not currently listed in HURDAT: [6]
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 1903 Atlantic hurricane season featured seven hurricanes, the most in an Atlantic hurricane season since 1893. The first tropical cyclone was initially observed in the western Atlantic Ocean near Puerto Rico on July 21. The tenth and final system transitioned into an extratropical cyclone well northwest of the Azores on November 25. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Six of the ten 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 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 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 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 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. 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 1870 Atlantic hurricane season marked the beginning of Father Benito Viñes investigating tropical cyclones, inspired by two hurricanes that devastated Cuba that year; Viñes consequently became a pioneer in studying and forecasting such storms. The season featured 11 known tropical cyclones, 10 of which became a hurricane, while 2 of those intensified into 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 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 1883 Atlantic hurricane season ran through the summer and the first half of fall in 1883. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1883 Atlantic season there was one tropical storm, one Category 1 hurricane, and two major hurricanes. 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 1881 Atlantic hurricane season ran through the summer and early fall of 1881. This is the period of each year when most tropical cyclones form in the Atlantic basin. In the 1881 Atlantic season there were three tropical storms and four hurricanes, none 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. Of the known 1881 cyclones, Hurricane Three and Tropical Storm Seven were both first documented in 1996 by Jose Fernandez-Partagas and Henry Diaz. They also proposed changes to the known tracks of Hurricane Four and Hurricane Five.
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 lasted from mid-summer to late-fall. Records show that in 1877 there were eight cyclones, of which five were tropical storms and three were hurricanes, one of which 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.
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 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.
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