User:CapeVerdeWave/1878 Kissimmee hurricane

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Hurricane Four
Meteorological history
FormedSeptember 1, 1878
ExtratropicalSeptember 13
DissipatedSeptember 13, 1878
Category 2 hurricane
1-minute sustained (SSHWS/NWS)
Highest winds105 mph (165 km/h)
Lowest pressure≤970 mbar (hPa); ≤28.64 inHg
Tornado outbreak
Tornadoes≥8
Maximum ratingF2+ tornado
DurationSeptember 12, 1878
Overall effects
Fatalities≥ 13 (+2 tornado-related)
Damage
($Format price error: cannot parse value "Error when using {{Inflation}}: |value= (parameter 2) and |start_year= (parameter 3) must be specified." in 2024 USD)
Areas affected
Part of the 1878 Atlantic hurricane season

The 1878 Kissimmee hurricane was a slow-moving Atlantic hurricane that was the most severe to impact the island of Trinidad since 1838. It caused significant damage to portions of Hispaniola and Florida, primarily via storm surge and rainfall-induced flooding, and was regarded as the most outstanding Atlantic tropical cyclone in the month of September, 1878. The fifth tropical storm and fourth hurricane of the 1878 Atlantic hurricane season, it developed over the western tropical Atlantic north of South America; well developed at the time, it likely originated farther east but went undetected. Quickly strengthening into a hurricane, it passed over the Windward Islands, extensively damaging... For several days the storm delivered copious rainfall to Florida, as it moved erratically over or near much of that state.

Meteorological history[edit]

Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
Map key
Saffir–Simpson scale
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
triangle Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

A tropical storm of moderate intensity was first noted on September 1 about 200 miles (320 km) north-northeast of Paramaribo, Dutch Surinam.[1] The storm may have formed much farther east, south of the Cape Verde islands, between 6° and 10°N,[2] but insufficient data exist to confirm this, so independent reanalyses failed to detect genesis earlier.[3][4] Bearing 60-mph (95-km/h) winds, the storm headed west-northwest, quickly gaining hurricane status within a day. At 06:00 UTC on September 2, the eye of the storm passed between Tobago and Trinidad, accompanied by maximum sustained winds of 80–90 mph (130–150 km/h).[1][5] As it did so, it gradually veered northwestward, a heading it maintained over the eastern Caribbean for two days. Maintaining force, the storm made two consecutive landfalls on Hispaniola early on September 4: over present-day Jaragua National Park, Dominican Republic, then near Belle-Anse, Haiti, at a slightly lower intensity. A study by Michael Chenoweth in 2014, however, concluded that the storm never hit the Dominican Republic and grazed the southwestern edge of the Tiburon Peninsula instead. (As of 2024, HURDAT has not adopted the results of the study.)[3]

The hurricane lost some potency over western Haiti, reemerging over water near Gressier. Bypassing Port-au-Prince Bay, it briefly degenerated into a tropical storm over Gonâve Island. It quickly recovered, however, over the Windward Passage, and reached a secondary peak of 80 mph (130 km/h) before striking eastern Cuba on September 5. Interaction with land failed to weaken the storm appreciably; for a few days the system, now heading west-northwestward, slowed and meandered along the northern coast of Cuba, maintaining winds of 60 mph (95 km/h). Early on September 7 the storm, traversing the Sabana-Camagüey Archipelago, turned sharply northward, toward the Straits of Florida. At 21:00 UTC that day it struck the Florida Keys with winds of 70 mph (110 km/h), and five hours later hit South Florida.[1] Spending a day over land, the storm abruptly shifted course, heading west-northwestward once more, and entered the eastern Gulf of Mexico between Tampa Bay and Charlotte Harbor early on September 9. Rapidly intensifying over water, the storm attained winds of 105 mph (165 km/h)—the highest in its lifespan—and suddenly reversed course, moving inland near present-day Pine Island, north of Bayport, at 11:00 UTC on September 10.[6] Its track on September 9–10 was corroborated by data from three weather stations; however, older analysis and Chenoweth's study kept it no farther west than Punta Gorda.[3][4][7] Atmospheric pressure at landfall was estimated to be 970 mb (29 inHg), based on a later report of 29.09 inHg (985 mb) taken in the eye at St. Augustine.[8][4]

At the time, the storm's trek across Florida was regarded as atypical, as its effects lasted for up to four days. As a result, "extreme rainfalls" were reported.[9] The center tracked northeastward across North Florida, entering the western Atlantic Ocean on September 11. Having weakened to a strong tropical storm, the cyclone soon became a hurricane again while curving sharply north-northeastward, and attained winds of 90 mph (150 km/h).[1] At 12:00 UTC the next day, it made its final landfall near Edisto Island, South Carolina, at the same intensity.[6] Accelerating inland, the storm steadily lost strength, becoming extratropical over eastern West Virginia on the morning of September 13. The remnants of the storm reached southernmost Ontario late that day, at which point they lost identity.[1]

Preparations, impact, and aftermath[edit]

As the storm passed near Trinidad, the island registered a minimum pressure of 29.05 inHg (984 mb), accompanied by veering winds. An hour-long lull was reported as the eye passed close to the island. Effects on land were severe: all watercraft in the harbor were mangled, infrastructure and housing destroyed, and entire plantations "swept away". Up to 7 in (180 mm) of rainfall swamped the island, and eyewitnesses reported tremors during the storm. The impacts of the hurricane on the island were the worst in 40 years. In Hispaniola the storm struck with great fanfare, doing severe damage. Structures were wrecked at Port-au-Prince, and high seas badly damaged infrastructure at Jacmel, along with the cocoa and coffee crops. Fierce winds swept Les Cayes, called Aux Cayes then, destroying 434 homes. An unknown number of dead and wounded were reported there. Almost all houses at Cavaillon and Aquin were blown down, resulting in great loss of life. High seas virtually leveled Jérémie and Saint-Louis-du-Sud, along with Grand'Anse.[2]

Hurricane-force winds of "remarkable velocity" were reported during landfall in Cuba. At Santiago de Cuba, an observer registered a barometric minimum of 29.49 inHg (999 mb). Between Colón and Cárdenas the storm inundated 60 plantations.[10] Across parts of western Cuba flooding was the most destructive on record.[2]

Crops and several homes were blown down on Bimini.[11] Key West was flooded to a depth of 1 ft (0.30 m).

In Central Florida, the cyclone, dubbed "the great hurricane", flooded the area near Fort Basinger, including the Kissimmee River valley, in present-day Okeechobee County. The river itself overflowed its banks several miles, rendering all travel impossible but by boat.[12] A denizen of Fort Myers recalled that men from Fort Basinger traveled "in a straight line" 30 mi (48 km) by boat between both points over a minimum depth of 5 ft (1.5 m). They were unable to distinguish Fisheating Creek from surrounding floodwater. Even the highest grazing lands, covered by saw palmetto and populated by cattle, were underwater, though some cattle survived standing partially submerged. 19 of 20 houses on the bank abutting Fort Myers were flooded, the exception being sited on 6-foot-tall (1.8 m) stilts. Water reached the floor of the highest house, and the others were inundated up to the peaks of their roofs. Farther inland, "above" Fort Myers, similar effects on homes 6 to 8 ft (1.8 to 2.4 m) above the Caloosahatchee River were reported. 60-mile-per-hour (97 km/h) winds buffeted Sarasota intermittently for five days.[13]

Upon reaching the western Atlantic, the storm caused several ships to be wrecked along the northeast coast of Florida, between Cape Canaveral and Amelia Island. At Butler Island, Georgia, the storm ruined the local rice crop and caused the highest tides locally since a major hurricane almost exactly 24 years earlier.[14]

In Ontario, where it had been raining since September 10, flooding claimed at least four lives.[15] In the United States the hurricane caused at least nine deaths, and some sources suggested "hundreds" of deaths in the Caribbean.[16][9]

Tornado outbreak[nb 1][edit]

Confirmed tornadoes by Fujita rating
FU F0 F1 F2 F3 F4 F5 Total
3 ? 1 4 ? ? ? ≥8

Prior to 1990, there is a likely undercount of tornadoes, particularly E/F0–1, with reports of weaker tornadoes becoming more common as population increased. A sharp increase in the annual average E/F0–1 count by approximately 200 tornadoes was noted upon the implementation of NEXRAD Doppler weather radar in 1990–1991.[18][nb 2] 1974 marked the first year where significant tornado (E/F2+) counts became homogenous with contemporary values, attributed to the consistent implementation of Fujita scale assessments.[22][nb 3]

List of confirmed tornadoes in the tornado outbreak of September 12, 1878[nb 4]
F# Location County / Parish State Time (UTC) Path length Width[nb 5] Damage
F2 Between Clover Hill and Summit Chesterfield South Carolina Un­known 8 mi (13 km) 100 yd (91 m) Un­known
Many homes were wrecked, with eight injuries. "Everything" in the path was ruined.[32][33]
F1 Short Pump Hanover Virginia Un­known 15 mi (24 km) 125 yd (114 m) Un­known
This tornado damaged trees, carrying off all debris.[32][33]
F2 ENE of Goldsboro Wayne North Carolina 11:45–? 5 mi (8.0 km) 100 yd (91 m) Un­known
2 deaths – A few farms and much timber were leveled. About 1,200 chickens were shorn of feathers. A man was killed instantly, and a member of his family was fatally injured, dying days afterward. One of the dead was carried far, debris was strewn countywide, and cattle and dogs were killed. There were three—possibly four—injured.[32][34]
FU SE of Petersburg Dinwiddie Virginia 18:00–? Un­known Un­known Un­known
Details are unknown.[32]
F2 E of Ford's Depot Dinwiddie Virginia 18:20–? Un­known 70 yd (64 m) Un­known
Small homes and a barn were felled, along with trees.[32][33]
FU W of Burkeville Nottoway Virginia Un­known Un­known Un­known Un­known
Trees were sheared off.[32][33]
F2 Bosher's Dam Henrico Virginia Un­known Un­known Un­known Un­known
1 death – Outbuildings and small homes were wrecked. Seven injuries occurred.[32][33]
FU Near Dover Mines Goochland Virginia 21:00–? 28 mi (45 km) 150 yd (140 m) Un­known
Details are unknown.[32]

See also[edit]

Notes[edit]

  1. ^ An outbreak is generally defined as a group of at least six tornadoes (the number sometimes varies slightly according to local climatology) with no more than a six-hour gap between individual tornadoes. An outbreak sequence, prior to (after) the start of modern records in 1950, is defined as a period of no more than two (one) consecutive days without at least one significant (F2 or stronger) tornado.[17]
  2. ^ Historically, the number of tornadoes globally and in the United States was and is likely underrepresented: research by Grazulis on annual tornado activity suggests that, as of 2001, only 53% of yearly U.S. tornadoes were officially recorded. Documentation of tornadoes outside the United States was historically less exhaustive, owing to the lack of monitors in many nations and, in some cases, to internal political controls on public information.[19] Most countries only recorded tornadoes that produced severe damage or loss of life.[20] Significant low biases in U.S. tornado counts likely occurred through the early 1990s, when advanced NEXRAD was first installed and the National Weather Service began comprehensively verifying tornado occurrences.[21]
  3. ^ The Fujita scale was devised under the aegis of scientist T. Theodore Fujita in the early 1970s. Prior to the advent of the scale in 1971, tornadoes in the United States were officially unrated.[23][24] Tornado ratings were retroactively applied to events prior to the formal adoption of the F-scale by the National Weather Service.[25] While the Fujita scale has been superseded by the Enhanced Fujita scale in the U.S. since February 1, 2007,[26] Canada used the old scale until April 1, 2013;[27] nations elsewhere, like the United Kingdom, apply other classifications such as the TORRO scale.[28]
  4. ^ All dates are based on the local time zone where the tornado touched down; however, all times are in Coordinated Universal Time and dates are split at midnight CST/CDT for consistency.
  5. ^ The listed width values are primarily the average/mean width of the tornadoes, with those having known maximum widths denoted by ♯. From 1952 to 1994, reports largely list mean width whereas contemporary years list maximum width.[29] Values provided by Grazulis are the average width, with estimates being rounded down (i.e. 0.5 mi (0.80 km) is rounded down from 880 yards to 800 yards.[30][31]

References[edit]

  1. ^ a b c d e "Atlantic hurricane best track (HURDAT version 2)" (Database). United States National Hurricane Center. April 5, 2023. Retrieved May 14, 2024. Public Domain This article incorporates text from this source, which is in the public domain.
  2. ^ a b c USASC 1878a, p. 3.
  3. ^ a b c Chenoweth 2014.
  4. ^ a b c Landsea, Chris; Anderson, Craig; Bredemeyer, William; et al. Documentation of Atlantic Tropical Cyclones Changes in HURDAT: 1878/05 - 2000 ORIGINAL. Re-Analysis Project (Report). Miami, Florida: Atlantic Oceanographic and Meteorological Laboratory, Hurricane Research Division. Retrieved May 14, 2024.
  5. ^ Partagás & Díaz 1995, pp. 27, 30.
  6. ^ a b Landsea, Chris; Anderson, Craig; Bredemeyer, William; et al. (January 2022). Continental United States Hurricanes (Detailed Description). Re-Analysis Project (Report). Miami, Florida: Atlantic Oceanographic and Meteorological Laboratory, Hurricane Research Division. Retrieved May 14, 2024.
  7. ^ Ho 1989.
  8. ^ Ho 1989, p. 133.
  9. ^ a b Barnes 1998, p. 70.
  10. ^ Partagás & Díaz 1995, p. 28.
  11. ^ "[No title]". Nassau Times. Nassau, Bahamas. September 21, 1878. p. 2. Retrieved 3 May 2024.
  12. ^ Kyle S. Van Landingham (2021) [1976]. Written at Okeechobee, Florida. William LaMartin (ed.). Pioneer Families of the Kissimmee River Valley (Report). Tampa: LaMartin.com. OL 4916266M. Retrieved 10 September 2021.
  13. ^ Webb, John G. (October 12, 1878). William LaMartin (ed.). "1878 Flood in Florida". Letter to the Editor. Sunland Tribune. Tampa: LaMartin.com. Retrieved 10 September 2021.
  14. ^ Al Sandrik & Chris 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 2007-01-02.
  15. ^ "The Great Rainstorm". The Globe. September 14, 1878. p. 8.
  16. ^ Rappaport, Edward N.; Fernández-Partagás, José (22 April 1997) [28 May 1995]. "Appendix 2: Cyclones that may have 25+ deaths". The Deadliest Atlantic Tropical Cyclones, 1492–1996 (Technical report). National Weather Service, National Hurricane Center. NWS NHC 47. Retrieved 10 September 2021.
  17. ^ Schneider, Russell S.; Brooks, Harold E.; Schaefer, Joseph T. (2004). Tornado Outbreak Day Sequences: Historic Events and Climatology (1875–2003) (PDF). 22nd Conf. Severe Local Storms. Hyannis, Massachusetts: American Meteorological Society. Retrieved September 17, 2019.
  18. ^ Agee and Childs 2014, p. 1496.
  19. ^ Grazulis 2001a, pp. 251–4.
  20. ^ Edwards, Roger (March 5, 2015). "The Online Tornado FAQ (by Roger Edwards, SPC)". Storm Prediction Center: Frequently Asked Questions about Tornadoes. Storm Prediction Center. Retrieved February 25, 2016.
  21. ^ Cook & Schaefer 2008, p. 3135.
  22. ^ Agee and Childs 2014, pp. 1497, 1503.
  23. ^ Grazulis 1993, p. 141.
  24. ^ Grazulis 2001a, p. 131.
  25. ^ Edwards et al. 2013, p. 641–642.
  26. ^ Edwards, Roger (March 5, 2015). "Enhanced F Scale for Tornado Damage". The Online Tornado FAQ (by Roger Edwards, SPC). Storm Prediction Center. Archived from the original on July 9, 2011. Retrieved February 25, 2016.
  27. ^ "Enhanced Fujita Scale (EF-Scale)". Environment and Climate Change Canada. Environment and Climate Change Canada. June 6, 2013. Archived from the original on March 3, 2016. Retrieved February 25, 2016.
  28. ^ "The International Tornado Intensity Scale". Tornado and Storm Research Organisation. Tornado and Storm Research Organisation. 2016. Archived from the original on March 5, 2016. Retrieved February 25, 2016.
  29. ^ Agee and Childs 2014, p. 1494.
  30. ^ Brooks 2004, p. 310.
  31. ^ Grazulis 1990, p. ix.
  32. ^ a b c d e f g h Grazulis 1993, p. 596.
  33. ^ a b c d e USASC 1878b, p. 11.
  34. ^ USASC 1878b, pp. 10–1.

Sources[edit]

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