1885 Atlantic hurricane season | |
---|---|
Seasonal boundaries | |
First system formed | August 7, 1885 |
Last system dissipated | October 13, 1885 |
Strongest storm | |
Name | Two |
• Maximum winds | 105 mph (165 km/h) (1-minute sustained) |
• Lowest pressure | 953 mbar (hPa; 28.14 inHg) |
Seasonal statistics | |
Total storms | 8 |
Hurricanes | 6 |
Major hurricanes (Cat. 3+) | 0 |
Total fatalities | 25 |
Total damage | $1.806 million (1885 USD) |
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. [1]
The Atlantic hurricane database (HURDAT) [2] recognizes eight tropical cyclones for 1885 in the Atlantic basin; two were tropical storms and six were hurricanes. The most significant storm of the season was Hurricane Two, which hit Georgia as a Category 2 hurricane, causing 25 deaths. The first cyclone was a tropical storm that existed in the Atlantic between August 7 and August 13 without making landfall. From north of Puerto Rico, Hurricane Two struck the Bahamas but then remained offshore until making a landfall in South Carolina. The hurricane caused considerable damage throughout the Carolinas, Georgia and Maryland. Also in August, Tropical Storm Three formed in the Gulf of Mexico, before crossing Florida and dissipating off South Carolina. Hurricane Four also grew from a tropical storm that formed in the Gulf of Mexico. It brought high winds and flooding to towns along the Gulf coast. This storm also crossed over Florida into the Atlantic and eventually made another landfall at New Brunswick as an extratropical storm. Hurricane Five existed in the tropical Atlantic between September 18 and September 21, without making landfall. Hurricane Six formed as a tropical storm in the Gulf of Mexico and reached hurricane strength off North Carolina a week later on October 2. The cyclone had impacted both Mississippi and Florida as it had travelled north. Hurricane Seven existed in the mid-Atlantic between September 26 and September 29. The last known cyclone of 1885 was Tropical Storm Eight which formed north of Cuba and impacted Florida. It travelled through the south-east United States and brought gales and flooding to the North Carolina coast.
.
Category 1 hurricane (SSHWS) | |
Duration | August 7 – August 13 |
---|---|
Peak intensity | 90 mph (150 km/h) (1-min); ≤981 mbar (hPa) |
A tropical storm was seen on August 7 to the southeast of Bermuda. It moved north-northeastward, and became a hurricane on August 8. It turned to the northeast, and passed offshore of Newfoundland on the 10th as a 90 mph (145 km/h) hurricane. The hurricane weakened over the north Atlantic Ocean, and became extratropical on the 14th. [2]
Category 2 hurricane (SSHWS) | |
Duration | August 21 – August 27 |
---|---|
Peak intensity | 105 mph (165 km/h) (1-min); ≤953 mbar (hPa) |
Although observations prior to August 23 could not be located, [3] HURDAT begins the track of this storm approximately 185 mi (300 km) north of Puerto Rico on August 21, [4] based on a 1993 reanalysis led by C. J. Neumann. [3] The tropical storm moved generally westward and crossed the southern Bahamas, until curving north-northwestward while passing just west of Andros between August 22 and August 23. After intensifying into a hurricane early on August 24, the cyclone passed very close to Florida, including just over 10 mi (15 km) east of Jupiter Island at 06:00 UTC. The storm then curved northeastward early the next day, hours prior to making landfall on Kiawah Island, South Carolina. Based on a pressure observation of 974 mbar (28.8 inHg ), the cyclone was likely a Category 2 hurricane with winds of 105 mph (165 km/h). The hurricane passed across North Carolina just west of Wilmington and Hatteras, near where it re-emerged into the Atlantic early on August 26. Although the storm weakened to a Category 1 hurricane, it re-intensified into a 105 mph (165 km/h) Category 2 hurricane, [4] based on the bark Harold recording a barometric pressure of 958 mbar (28.3 inHg). [5] Late on August 27, the system transitioned into an extratropical cyclone about 290 mi (470 km) east of Newfoundland, and continued northeastward until dissipating late the next day. [4]
In Florida, abnormally high tides and "high winds pummeled the coast" according to Jay Barnes, [6] with a sustained wind speed of 60 mph (95 km/h) and hurricane-force wind gusts in Jacksonville. [7] Nearby, winds destroyed a hotel, while many buildings and boats suffered significant damage in Fernandina Beach. [8] The storm disrupted attempts to settle present-day Cocoa Beach, with waves flooding many homesteads. Nearby, severe erosion occurred in the vicinity of the Cape Canaveral Lighthouse, prompting an effort to move the lighthouse about 1 mi (1.6 km) farther inland. [6] Sustained winds in Georgia reached 56 mph (90 km/h) on Tybee Island. [7] About $1.69 million in damage occurred in Charleston, South Carolina. In North Carolina, an anemometer at Smithville (modern-day Southport) measured a 5-minute sustained wind speed of 98 mph (158 km/h) before being destroyed. The storm caused considerable damage at Wilmington, Smithville, and Morehead City. The value of this damage was estimated at $100,000. [9] Heavy rains and flooding were also seen across Maryland. At Ellicott City, lightning set fire to a residence, causing about $16,000 in damage. [10] In total, the hurricane caused 25 deaths, [11] with 21 of those occurring in South Carolina. [12]
Tropical storm (SSHWS) | |
Duration | August 29 – August 31 |
---|---|
Peak intensity | 60 mph (95 km/h) (1-min); |
A tropical storm formed in the western Gulf of Mexico on August 29. It moved quickly to the northeast, and made landfall on extreme southeastern Louisiana on the 30th as a 60 mph (97 km/h) tropical storm. After crossing Florida, the storm was last seen off the coast of South Carolina on August 31. [2]
Category 1 hurricane (SSHWS) | |
Duration | September 17 – September 23 |
---|---|
Peak intensity | 90 mph (150 km/h) (1-min); 973 mbar (hPa) |
On September 17, a tropical storm developed in the western Gulf of Mexico near Veracruz, Mexico. It paralleled the Gulf of Mexico coastline to the northeast flooding coastal towns. Winds along the Texas coast at Indianola were reported at 45 miles per hour (72 km/h). After hitting southeastern Louisiana on September 21, the storm crossed Florida. Over the Western Atlantic, it strengthened to become a hurricane on the 22nd before becoming extratropical near its New Brunswick landfall on the 23rd. The storm brought flooding to Indianola and coastal flooding in the Galveston area. Four people died when a coal barge, the Orient, was cast adrift in the Gulf. [13]
Category 1 hurricane (SSHWS) | |
Duration | September 18 – September 21 |
---|---|
Peak intensity | 80 mph (130 km/h) (1-min); ≤999 mbar (hPa) |
From September 18 to the 21st, a hurricane existed in the tropical Atlantic Ocean to the northeast of the Lesser Antilles, peaking at 80 mph (129 km/h) before never being seen again. [2]
Category 1 hurricane (SSHWS) | |
Duration | September 24 – October 2 |
---|---|
Peak intensity | 80 mph (130 km/h) (1-min); |
A tropical storm formed in the central Gulf of Mexico on September 24. It drifted northward, and hit southeastern Mississippi before turning eastward. It moved across the Florida panhandle and peninsula, and became a hurricane to the southeast of North Carolina on October 2. Its track after this point is unknown. [2] Climate researcher Michael Chenoweth's 2014 study argued that the Gulf of Mexico portion of the track of this storm should deleted from HURDAT and the remaining path to be reclassified as extratropical. [14]
Category 1 hurricane (SSHWS) | |
Duration | September 26 – September 29 |
---|---|
Peak intensity | 90 mph (150 km/h) (1-min); 982 mbar (hPa) |
A tropical storm in the central Atlantic Ocean moved northward in late September, steadily strengthening and eventually reached 90 mph (145 km/h) winds. The storm was last recorded to the south of Nova Scotia and east of New England on September 29th. [2] The storm peaked with winds of 90 mph (145 km/h) and a central pressure of 982 mbar (hPa)
Tropical storm (SSHWS) | |
Duration | October 10 – October 13 |
---|---|
Peak intensity | 70 mph (110 km/h) (1-min); 988 mbar (hPa) |
A tropical storm formed north of Cuba on October 10. It moved northward, and hit Florida as a strong tropical storm. It moved northeastward through the southeast United States, passing west of Jacksonville and later Savannah. It reached southwestern Virginia around midnight on October 12 and became extratropical on the 13th. Gales of 44-56 mph occurred along the North Carolina coast. High tides coincided with the storms passage and led to the waterfront at Smithville (Southport) being flooded. [9]
Chenoweth proposed three other storms not currently listed in HURDAT: [14]
The 1907 Atlantic hurricane season was a very inactive hurricane season. Only five tropical storms formed, and none of them reaching hurricane strength. This season is one of only two that did not produce any hurricanes. Of the season's storms, three made landfall, all of them on the Gulf Coast of the United States. The first storm of the season formed on June 24, while the final dissipated on November 12. Damage from the storms was minimal, and no deaths were reported. Due to the lack of modern technology, including satellite imagery, information is often sparse, and four additional systems could have formed during the season. A documentation for four possible storms during the season exists, although it has not been proven that these systems were fully tropical.
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 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 1897 Atlantic hurricane season was an inactive season, featuring only six known tropical cyclones, four of which made landfall. There were three hurricanes, none of which 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 south of Cape Verde on August 31, an unusually late date. The storm was the strongest of the season, peaking as a Category 2 hurricane with winds of 100 mph (155 km/h). While located well north of the Azores, rough seas by the storm sunk a ship, killing all 45 crewmen. A second storm was first spotted in the Straits of Florida on September 10. It strengthened into a hurricane and tracked northwestward across the Gulf of Mexico, striking Louisiana shortly before dissipating on September 13. This storm caused 29 deaths and $150,000 (1897 USD) in damage.
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 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 1864 Atlantic hurricane season was the third consecutive Atlantic hurricane season with no hurricane landfall in the United States – the longest period on record. Of the five known 1864 cyclones, four were first documented in 1995 by Jose Fernandez-Partagas and Henry Diaz. 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 first system was initially observed offshore the Southeastern United States on July 16. It peaked as a Category 1 hurricane on the modern day Saffir–Simpson hurricane wind scale. Moving rapidly northeastward, the storm was last noted well east of Newfoundland on July 18.
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 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 recognised in 1997. 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, 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 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 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 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 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.
The 1859 Atlantic hurricane season featured seven hurricanes, the most recorded during an Atlantic hurricane season until 1870. 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. Of the eight known 1859 cyclones, five were first documented in 1995 by Jose Fernandez-Partagás and Henry Diaz, which was 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. HURDAT is the official source for hurricane data such as track and intensity, although due to sparse records, listings on some storms are incomplete.