1881 Atlantic hurricane season
| 1881 Atlantic hurricane season | |
|---|---|
 Season summary map | |
| Seasonal boundaries | |
| First system formed | August 1, 1881 |
| Last system dissipated | September 24, 1881 |
| Strongest storm | |
| Name | Five |
| • Maximum winds | 105 mph (165 km/h) (1-minute sustained) |
| • Lowest pressure | 970 mbar (hPa; 28.64 inHg) |
| Seasonal statistics | |
| Total storms | 7 |
| Hurricanes | 4 |
| Major hurricanes (Cat. 3+) | 0 |
| Total fatalities | 700 |
| Total damage | Unknown |
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 (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.[1] 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.[2]
Season summary
[edit]
| Deadliest United States hurricanes | |||
|---|---|---|---|
| Rank | Hurricane | Season | Fatalities |
| 1 | 4 "Galveston" | 1900 | 8,000–12,000 |
| 2 | 4 "San Ciriaco" | 1899 | 3,400 |
| 3 | 4 Maria | 2017 | 2,982 |
| 4 | 5 "Okeechobee" | 1928 | 2,823 |
| 5 | 4 "Cheniere Caminada" | 1893 | 2,000 |
| 6 | 3 Katrina | 2005 | 1,392 |
| 7 | 3 "Sea Islands" | 1893 | 1,000–2,000 |
| 8 | 3 "Indianola" | 1875 | 771 |
| 9 | 4 "Florida Keys" | 1919 | 745 |
| 10 | 2 "Georgia" | 1881 | 700 |
| Reference: NOAA, GWU[3][4][nb 1] | |||
The Atlantic hurricane database (HURDAT) recognizes seven tropical cyclones for the 1881 season. Of the seven systems, four intensified into a hurricane, but none strengthened into a major hurricane.[5] José Fernández-Partagás and Henry F. Diaz first documented the third and seventh systems in their 1996 re-analysis of the season. In 2003, the Atlantic hurricane reanalysis project only made a significant track revision to the sixth storm. A reanalysis by climate researcher Michael Chenoweth, published in 2014, adds six storms and removes one, the second system. Chenoweth's study utilizes a more extensive collection of newspapers and ship logs, as well as late 19th century weather maps for the first time, in comparison to previous reanalysis projects. However, Chenoweth's proposals have yet to be incorporated into HURDAT.
Based on observations, the track of the first known system begins over the southeastern Gulf of Mexico on August 1. A few days later, the storm struck the Gulf Coast of the United States and caused flooding in the region. Four other cyclones formed in August, all but one of which impacted land. Most notably, the season's fifth cyclone peaked as a Category 2 hurricane on the Saffir–Simpson scale with sustained winds of 105 mph (165 km/h) and a minimum atmospheric pressure of 970 mbar (29 inHg). That storm caused several deaths due to maritime incidents prior to making landfall in Georgia. Overall, it caused more than $1.7 million in damage and approximately 700 fatalities, making it one of the deadliest hurricanes in the United States.
At least two additional storms developed in September. The first of the two, the season's sixth cyclone, reached an intensity similar to the fifth system. An unknown number of people drowned after it sank the Anne J. Palmer. After striking North Carolina, the hurricane caused severe damage over coastal portions of the state, totaling about $100,000. On September 18, the final known cyclone was first noted northwest of Bermuda. Moving generally northeastward, the storm transitioned into an extratropical cyclone on September 22.
The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 59, ahead of only 1885 and tied with 1882 for the lowest total of the 1880s. ACE is a metric used to express the energy used by a tropical cyclone during its lifetime. Therefore, a storm with a longer duration will have higher values of ACE. It is only calculated at six-hour increments in which specific tropical and subtropical systems are either at or above sustained wind speeds of 39 mph (63 km/h), which is the threshold for tropical storm intensity. Thus, tropical depressions are not included here.[6]
Systems
[edit]Tropical Storm One
[edit]| Tropical storm (SSHWS) | |
 | |
| Duration | August 1 – August 4 |
|---|---|
| Peak intensity | 60 mph (95 km/h) (1-min); |
Observations suggest the presence of a tropical storm over the southern Gulf of Mexico on August 1.[7] The storm moved generally north-northwestward across the Gulf of Mexico before striking Dauphin Island, Alabama, and then near the Alabama-Mississippi state line on August 3 with winds of 60 mph (95 km/h).[5] An assessment of the storm by the Atlantic hurricane reanalysis project estimated that it weakened to a tropical depression early the following day, shortly before dissipating over east-central Mississippi.[8]
Heavy rains fell along the Gulf Coast of the United States, including up to 15.8 in (400 mm) from August 2 to August 5 in Pensacola, Florida.[7] Floodwaters reached 3 ft (0.91 m) above ground in the nearby community of Millview, forcing residents to evacuate. The storm also beached a few fishing smacks and the schooner Ella, which was loaded with a cargo of lumber.[9] Climate researcher Michael Chenoweth argued that this storm actually developed as a tropical depression offshore North Carolina on July 26. The cyclone intensified into a hurricane as it moved generally southwestward, but generated into a tropical wave before crossing southern Florida on July 30. The remnants developed into a cyclone on August 2 over the central Gulf of Mexico and turned northward, striking Mississippi on the next day.[10]
Tropical Storm Two
[edit]| Tropical storm (SSHWS) | |
 | |
| Duration | August 11 – August 14 |
|---|---|
| Peak intensity | 45 mph (75 km/h) (1-min); |
Little information exists on this storm beyond the 1960 reanalysis by Gordon E. Dunn and Banner I. Miller.[7] The track begins near the center of the Gulf of Mexico on August 11. Moving westward and then northwestward by the following day, the cyclone made landfall near Corpus Christi, Texas, at 21:00 UTC on August 13 with winds of 45 mph (75 km/h).[5] Early the next day, the storm weakened to a tropical depression and dissipated over Mason County several hours later.[5] Signals were blown down at the harbor, and one boat was lost.[11] Chenoweth could not confirm the existence of this system as a tropical cyclone, noting "No storm in Texas press accounts" and that Dunn and Miller's 1960 reanalysis misdated a hurricane in 1880.[10]
Hurricane Three
[edit]| Category 1 hurricane (SSHWS) | |
 | |
| Duration | August 11 – August 18 |
|---|---|
| Peak intensity | 90 mph (150 km/h) (1-min); |
With The Times noting that the brigantine Fonthill "encountered a tremendous hurricane with a heavy cross sea" over the far eastern Atlantic on August 11,[12] the official track begins on that day approximately 375 mi (605 km) west of the Cabo Verde Islands with winds already at 90 mph (150 km/h). After initially moving westward, the hurricane turned northwestward by August 13. The cyclone is estimated to have weakened to a tropical storm on August 17, by which time it turned northward. No evidence of this storm exists past August 18, when the official track ceases about 780 mi (1,255 km) south-southeast Cape Race, Newfoundland.[5] The study by Chenoweth develops this system as a tropical depression on August 11. Moving in a more pronounced northwestward direction, the cyclone steadily intensified into a hurricane by the next day. By August 18, the storm turned northeastward, three days before becoming extratropical.[10]
Hurricane Four
[edit]| Category 1 hurricane (SSHWS) | |
 | |
| Duration | August 16 – August 21 |
|---|---|
| Peak intensity | 80 mph (130 km/h) (1-min); |
Land-based observations from the Gulf Coast of the United States attest to the existence of this storm beginning on August 16,[12] while HURDAT initiates the cyclone's track close to Cozumel. Moving northeastward on August 16 and then east-northeastward on the next day, the system avoided striking Cuba and Florida as it traversed the Straits of Florida. However, the cyclone resumed a northeastward motion on August 17 and passed through the Bahamas between then and early on the following day, making landfall on the Abaco Islands.[5] Based on reports from the ships Anna and Cohasset, the storm intensified into a hurricane on August 19 and peaked with winds of 80 mph (130 km/h).[5][8] It weakened to a tropical storm on August 21 and became extratropical the same day approximately 280 mi (450 km) east-southeast of Sable Island, Nova Scotia.[5]
In Cuba, the storm dropped heavy rainfall in Havana.[13] The Gulf Coast of the United States reported elevated winds from Florida to Louisiana, but sustained winds remained under tropical storm-force, while Key West and Punta Rassa in the former also recorded heavy precipitation.[12] Chenoweth proposed that this storm developed as a tropical depression offshore Cape Coral, Florida, on August 16. After moving south-southeastward toward the Florida Keys, the cyclone turned northeastward and made landfall near present-day Everglades City as a minimal hurricane. Early on August 18, the hurricane exited the state near West Palm Beach and remained north of the Bahamas.[10]
Hurricane Five
[edit]| Category 2 hurricane (SSHWS) | |
 | |
| Duration | August 21 – August 29 |
|---|---|
| Peak intensity | 105 mph (165 km/h) (1-min); 970 mbar (hPa) |
The Georgia Hurricane of 1881
The Atlantic hurricane best track begins the path for this storm just east of the Lesser Antilles on August 21, one day before the cyclone passed north of the islands. Moving northwestward, the system intensified, reaching hurricane status early on August 24. The hurricane passed northeast of the Abaco Islands in the Bahamas two days later and strengthened into a Category 2 hurricane on the present-day Saffir–Simpson scale, peaking with maximum sustained winds of 105 mph (165 km/h). After moving north-northwestward late on August 26 and early the next day, the storm then turned west-northwestward. Around 02:00 UTC on August 28, the hurricane made landfall in Georgia between St. Simons Island and Savannah, likely at the same intensity.[5] Upon the cyclone moving ashore, the Atlantic hurricane reanalysis project estimated that it had a barometric pressure of 970 mbar (29 inHg).[8] Thereafter, the storm briefly moved westward and quickly weakened to a tropical storm within 10 hours of moving inland. By early on August 29, the system turned northwestward and weakened to a tropical depression later that day, before dissipating near the Arkansas-Mississippi state line.[5]
Chenoweth proposed a more consistent northwestward movement of this storm, leading to a landfall around Hilton Head Island, South Carolina, instead of in Georgia. He also argued that the cyclone persisted longer inland, dissipating over Missouri on August 30.[10]
Between August 26 and August 27, the ship Sandusky encountered the storm, with the loss of all but two people,[14] while most of the crew of the Hannah M. Lallis also drowned.[15] Landfall coincided with high tide and proved very destructive as several barrier islands were completely submerged by storm surge.[16] In Savannah, Georgia, few structures escaped damage, with the Monthly Weather Review noting that "nearly every house received a copious supply of salt water." in the Bohanville section of the city. A number of streets were blocked, especially by large trees and the remnants of tin roofs. Property damage in the city reached about $1.5 million. Approximately 100 ships capsized in the vicinity of Savannah.[17] A barometric recorded a pressure of 984.76 mbar (29.08 inHg), while a wind speed of 80 mph (130 km/h) was observed before the anemometer was destroyed. At least 335 people died in Savannah alone.[16] Tybee Island was also among the localities severely impacted. There, the storm demolished rows of cottages and even some of the sturdiest homes. Additionally, South Carolina experienced extensive coastal flooding. In Charleston, several feet of water submerged areas east of East Bay Street and inundated many properties in the southwest sections of city. Substantial damage to businesses, fences, roofs, telegraph wires, and trees were also reported. Damage in the city ranged from $200,000 to $300,000.[17] Overall, the storm caused an estimated 700 fatalities, making the hurricane among the deadliest to strike the United States.[18]
Hurricane Six
[edit]| Category 2 hurricane (SSHWS) | |
 | |
| Duration | September 7 – September 11 |
|---|---|
| Peak intensity | 105 mph (165 km/h) (1-min); ≤975 mbar (hPa) |
The Anne J. Palmer first encountered this storm on September 7 before capsizing in rough seas that day.[19] Thus, the track for this cyclone begins at that time to the northeast of the Turks and Caicos Islands as a Category 1 hurricane. Moving northeastward, the storm intensified slightly, becoming a Category 2 hurricane with maximum sustained winds of 105 mph (165 km/h) early on September 9, several hours prior to making landfall in present-day Oak Island, North Carolina.[5] The Atlantic hurricane reanalysis project estimated that upon landfall, the storm had a barometric pressure of 975 mbar (28.8 inHg).[8] Rapidly weakening to a tropical storm by early on September 10, the cyclone then turned northeastward, passing close to Wilmington–Wrightsville Beach area and later near Norfolk, Virginia, before re-emerging into the Atlantic that day. The cyclone was last noted only 50 mi (80 km) offshore Massachusetts on September 11.[5] One of the few changes proposed by Chenoweth's 2014 study was the extension of the storm's duration and track back to September 3, as a tropical depression east of the Windward Islands.[10]
An unknown number of deaths occurred when the Anne J. Palmer capsized, with only one person surviving.[19] In North Carolina, the storm uprooted trees and demolished buildings at both Smithville (present-day Southport) and Wilmington. An anemometer at Wilmington indicate sustained windspeeds of 90 mph (150 km/h) before it was destroyed.[20] At least 600 bushels of peanuts suffered damage after a warehouse lost its roof. Wilmington also entirely lost communications outside the city after winds toppled many telephone and telegraph wires.[21] Damage in North Carolina totaled approximately $100,000.[20] The hurricane weakened to a tropical storm over land, bringing heavy, yet beneficial, precipitation to other states, including the first rainfall in Washington, D.C. in 33 days.[22]
Tropical Storm Seven
[edit]| Tropical storm (SSHWS) | |
 | |
| Duration | September 18 – September 22 |
|---|---|
| Peak intensity | 70 mph (110 km/h) (1-min); |
The bark J.E. Fisher first encountered this storm on September 18,[23] leading the Atlantic hurricane database to begin the track about 270 mi (435 km) northwest of Bermuda. After initially trekking to the northwest, the storm curved to northeastward and moved in that direction for the remainder of its duration.[5] According to ship records,[8] the system likely remained just below hurricane intensity, with winds reaching 70 mph (110 km/h) on September 19. It weakened over the north Atlantic, becoming extratropical on September 22 about 575 mi (925 km) east of Newfoundland and fully dissipating by September 24.[5] Chenoweth did not proposed significant changes to this storm's track or duration, but started it as a hurricane, which peaked with winds of 90 mph (150 km/h). On September 21, the cyclone weakened to a tropical storm.[10]
Other storms
[edit]Chenoweth proposed six storms not currently listed in HURDAT. The first such system formed well east of the Lesser Antilles on August 23. After moving generally northwestward for several days, the cyclone trekked mostly northeastward, with the exception of a northward jog, until dissipating on September 6 over the central Atlantic. A second unofficial system developed on August 27 north of Barbados and headed north-northwestward across Leeward Islands before dissipating on August 29 near Saint Martin. Chenoweth's third new storm developed near Eleuthera in the Bahamas on October 15. The cyclone meandered slowly near or over the island for nearly 30 hours, but then turned southwestward and dissipated on October 17 near the north end of Exuma. None of these aforementioned storm strengthened beyond tropical storm status.[10]
A fourth unofficial system developed well east of the Lesser Antilles on October 16. The cyclone initially moved west-northwestward, before turning northwestward two days later, followed by a northeastward curve on October 21 until its extratropical transition west-northwest of the Azores on October 23. This storm maintained major hurricane status from October 18 to early on October 21, peaking as a Category 3 hurricane with winds of 120 mph (195 km/h). Another storm formed northeast of the Lesser Antilles on November 9. Moving erratically for about a week, during which time it held hurricane intensity on November 10, the cyclone turned northeastward on November 16. The storm transitioned into an extratropical system two day later to the southwest of the Azores. Chenoweth's final proposed system formed well east of the Lesser Antilles on December 7 and moved slowly westward before dissipating the next day.[10]
Season effects
[edit]This is a table of all of the known storms that have formed in the 1881 Atlantic hurricane season. It includes their duration, landfall, 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 1881 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 1–4 | Tropical storm | 60 (95) | Unknown | Gulf Coast of the United States (Alabama) | Unknown | None | |||
| Two | August 11–14 | Tropical storm | 45 (75) | Unknown | Texas | Unknown | None | |||
| Three | August 11–18 | Category 1 hurricane | 90 (150) | Unknown | None | None | None | |||
| Four | August 16–21 | Category 1 hurricane | 80 (130) | Unknown | Cuba, Florida, Bahamas | Unknown | None | |||
| Five | October 22–24 | Category 2 hurricane | 105 (165) | 970 | Bahamas, Southeastern United States (Georgia) | >$1.7 million | >700 | [17][18] | ||
| Six | October 22–24 | Category 2 hurricane | 105 (165) | ≤975 | East Coast of the United States (North Carolina) | >$100,000 | Unknown | [20] | ||
| Seven | October 22–24 | Tropical storm | 70 (110) | Unknown | None | None | None | |||
| Season aggregates | ||||||||||
| 7 systems | August 1 – September 22 | 105 (165) | 970 | >$1.8 million | >700 | |||||
See also
[edit]
Notes
[edit]- ^ The storm category color indicates the intensity of the hurricane when landfalling in the U.S.
References
[edit]- Specific
- ^ Landsea, C. W. (2004). "The Atlantic hurricane database re-analysis project: Documentation for the 1851–1910 alterations and additions to the HURDAT database". In Murname, R. J.; Liu, K.-B. (eds.). Hurricanes and Typhoons: Past, Present and Future. New York: Columbia University Press. pp. 177–221. ISBN 0-231-12388-4.
- ^ Fernández-Partagás, José (1996). A Reconstruction of Historical Tropical Cyclone Frequency in the Atlantic from Documentary and other Historical Sources: 1881–1883 Part III: 1881–1890. Storms of 1881–1883 (PDF) (Report). Climate Diagnostics Center, National Oceanic and Atmospheric Administration. p. 3. Retrieved December 18, 2024.
- ^ Blake, Eric S; Landsea, Christopher W; Gibney, Ethan J (August 10, 2011). The deadliest, costliest and most intense United States tropical cyclones from 1851 to 2010 (and other frequently requested hurricane facts) (PDF) (NOAA Technical Memorandum NWS NHC-6). National Oceanic and Atmospheric Administration. p. 47. Archived (PDF) from the original on May 17, 2024. Retrieved August 10, 2011.
- ^ "Ascertainment of the Estimated Excess Mortality from Hurricane María in Puerto Rico" (PDF). Milken Institute of Public Health. August 27, 2018. Archived (PDF) from the original on August 29, 2018. Retrieved August 28, 2018.
- ^ a b c d e f g h i j k l m n "Atlantic hurricane best track (HURDAT version 2)" (Database). United States National Hurricane Center. April 5, 2023. Retrieved December 20, 2024.
This article incorporates text from this source, which is in the public domain.
- Landsea, Chris (April 2022). "The revised Atlantic hurricane database (HURDAT2) - Chris Landsea – April 2022" (PDF). Hurricane Research Division – NOAA/AOML. Miami: Hurricane Research Division – via Atlantic Oceanographic and Meteorological Laboratory.
- ^ North Atlantic Hurricane Basin (1851-2022) Comparison of Original and Revised HURDAT. Hurricane Research Division; Atlantic Oceanographic and Meteorological Laboratory (Report). Miami, Florida: National Oceanic and Atmospheric Administration. April 2023. Retrieved October 15, 2024.
- ^ a b c Fernández-Partagás (1996), p. 8.
- ^ a b c d e Christopher W. Landsea; et al. (May 2015). "Documentation of Atlantic Tropical Cyclones Changes in HURDAT". National Hurricane Center, Hurricane Research Division. Retrieved April 3, 2024.
- ^ "Storm at Pensacola". The Daily Picayune. New Orleans, Louisiana. August 6, 1881. p. 1. Retrieved April 22, 2024 – via Newspapers.com.
- ^ a b c d e f g h i Chenoweth, Michael (December 2014). "A New Compilation of North Atlantic Tropical Cyclones, 1851–98". Journal of Climate. 27 (12). American Meteorological Society: 8682. Bibcode:2014JCli...27.8674C. doi:10.1175/JCLI-D-13-00771.1. Retrieved April 29, 2024.
- ^ David Roth (2010-02-04). "Texas Hurricane History" (PDF). National Weather Service. Retrieved 2011-06-22.
- ^ a b c Fernández-Partagás (1996), p. 9.
- ^ "A Great Storm in Cuba". New-York Tribune. August 18, 1881. p. 4. Retrieved December 16, 2024 – via Newspapers.com.
- ^ Fernández-Partagás (1996), p. 12.
- ^ Fernández-Partagás (1996), p. 13.
- ^ a b Al Sandrik; Christopher W. Landsea (2003). "Chronological Listing of Tropical Cyclones affecting North Florida and Coastal Georgia 1565-1899". Hurricane Research Division. Archived from the original on December 6, 2006. Retrieved April 3, 2024.
- ^ a b c "Barometric Pressure" (PDF). Monthly Weather Review. 9 (8). August 1881. Bibcode:1881MWRv....9RR..1.. doi:10.1175/1520-0493(1881)98[1b:BP]2.0.CO;2. Archived from the original (PDF) on March 3, 2017. Retrieved April 3, 2024.
- ^ a b Edward N. Rappaport; José Fernández-Partagás (1996). "The Deadliest Atlantic Tropical Cyclones, 1492–1996: Cyclones with 25+ deaths". National Hurricane Center. Retrieved April 3, 2024.
- ^ a b Fernández-Partagás (1996), p. 16.
- ^ a b c Hudgins, James E. (April 2000). Tropical cyclones affecting North Carolina since 1586: An historical perspective. National Weather Service (Report). Blacksburg, Virginia: National Oceanic and Atmospheric Administration. p. 15-16. Retrieved April 21, 2023.
- ^ "Yesterday's Hurricanes". The Morning Star. Wilmington, North Carolina. September 10, 1881. p. 1. Retrieved April 21, 2024 – via Newspapers.com.
- ^ Roth, David; Cobb, Hugh (July 16, 2001). "Late Nineteenth Century Virginia Hurricanes". Virginia Hurricane History (Report). National Oceanic and Atmospheric Administration. Archived from the original on January 8, 2008. Retrieved April 21, 2024.
- ^ Fernández-Partagás (1996), p. 17.
- General
- Fernández-Partagás, José; Diaz, Henry F. (1996). A Reconstruction of Historical Tropical Cyclone Frequency in the Atlantic from Documentary and other Historical Sources: 1881–1883 Part III: 1881–1890 (PDF) (Report). Climate Diagnostics Center, National Oceanic and Atmospheric Administration. Retrieved December 18, 2024.