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
Extratropical cyclone, remnant low, tropical disturbance, or monsoon depressionAn article in the Monthly Weather Review published by the United States Weather Bureau described the Windward Islands hurricane as "the most important meteorological event of September, 1898". [1] : 391 The origins of the hurricane are unclear due to the dearth of marine weather observations over the central Atlantic. [2] : 20 A compilation of historical tropical cyclone tracks published by the National Climatic Data Center in 1993 listed the storm as having begun south of Cabo Verde on September 5. [3] An analysis of the 1898 Atlantic hurricane season by hurricane expert José Fernández Partagás in 1996 made no modifications to the 1993 track due to the lack of available observations, [2] : 20 as did a reanalysis of the storm conducted by the Atlantic Oceanographic and Meteorological Laboratory in 2003. [4] The storm is first listed in the National Hurricane Center's Atlantic hurricane database at 11°12′N26°54′W / 11.2°N 26.9°W on September 5, 1898, as a tropical storm with estimated maximum sustained winds of 40 mph (65 km/h). [c] The database depicts the storm tracking west with its wind speeds increasing incrementally, reaching hurricane-force over the central Atlantic on September 6. [7] At around midday on September 9, the French barque Tourny encountered the storm near 12°2′N54°2′W / 12.033°N 54.033°W . The ship registered a minimum barometric pressure of around 985 mbar (hPa; 29.1 inHg) during the encounter, though a later assessment of the ship's barometer found that the instrument underestimated pressures by about 8 mbar (hPa; 0.25 inHg). [1] : 392–393
Observations from Martinique and Trinidad on the morning of September 10 tentatively indicated the presence of a tropical disturbance southeast of the Windward Islands, and falling pressures in Barbados later that day provided conclusive evidence of an approaching storm. [2] : 16 The hurricane passed near Barbados on the night of September 10. [1] : 392 No period of calm was reported in Bridgetown, suggesting that the storm's eye missed the city. [8] : 25 An analysis of the storm presented to the Royal Meteorological Society (RMS) in December 1898 determined that the centre of the hurricane passed 18 mi (29 km) south of the island. [8] : 28 HMS Alert encountered the storm while evacuating from Barbados on September 10, recording a minimum barometric pressure of 1002.4 mbar (hPa; 29.60 inHg) at 9:00 p.m. while the hurricane's centre was some 25 mi (40 km) to the northeast. [8] : 25 The storm reached the vicinity of St. Lucia and St. Vincent during the day on September 11. [1] : 392 The calm eye of the storm traversed southern St. Vincent, passing directly over Kingstown at around local noon. [8] : 26 A minimum air pressure of 965.43 mbar (hPa; 28.509 inHg) was recorded at the Saint Vincent and the Grenadines Botanic Gardens at 11:40 a.m. [1] : 393 Based on this measurement, the Atlantic hurricane reanalysis project estimated that the hurricane had maximum sustained winds of approximately 110 mph (175 km/h), an intensity equivalent to a Category 2 hurricane on the modern-day Saffir–Simpson scale. [4] Partagás described the storm as nearly a major hurricane based on the pressure observation at St. Vincent. [2] : 21
After moving west past the Lesser Antilles, the hurricane curved northwest towards Aves Island with a forward speed of around 7.5 mi (12.1 km). The areal extent of the storm's winds expanded significantly during its passage of the Windward Islands: the region of strong winds spanned 35 mi (56 km) in diameter on approach to St. Vincent but subsequently extended outward to 170 mi (270 km) from the centre. [8] : 28 The Weather Bureau noted that "after September 11 [the] storm lost strength rapidly, and there is no evidence at hand to show that during its subsequent northwesterly course over the eastern Caribbean Sea and the ocean to the northward it exhibited destructive violence." [1] : 394 The bureau assessed the storm to have taken a track through the Mona Passage before the storm eventually dissipated east of the Bahamas on September 14. [1] : 391 [9] However, the RMS analysis disputed this description of the storm's path, instead depicting a track that took the storm northward between Puerto Rico and the Windward Islands. [8] : 28 Compendiums of storms affecting Puerto Rico and the Dominican Republic do not suggest impacts from the hurricane. [2] : 19 The centre of the storm likely passed near Sombrero Island on September 13, where a minimum air pressure of 998 mbar (29.48 inHg) was measured. [8] : 32 According to the RMS analysis, the hurricane continued northward before curving to the northwest upon reaching the 23rd parallel north. On September 17, the storm reached the 30th parallel north and began accelerating to the northeast at an average forward speed of around 24 mph (39 km/h). The storm spanned around 400 mi (640 km) in diameter when it passed near Bermuda and expanded to around 450 mi (720 km) in diameter when it tracked east of Nova Scotia. The RMS analysis located the storm at around 42°N42°W / 42°N 42°W on September 20. [8] : 28 However, the Atlantic hurricane database depicts the storm completing extratropical transition by September 20 and taking a track across Newfoundland before dissipating in the Labrador Sea later that day. [7]
Preparations and impact
Barbados
Well east of Barbados, the French barque Tourney encountered the storm around midday on September 9 at 12°2′N54°2′W / 12.033°N 54.033°W . The ship lost all sail and nearly all of its rice cargo, and over the course of two days it was blown 60 mi (97 km) off course. [1] : 392–393 Rain showers were frequent in Barbados between September 1 and September 10, but such weather conditions were typical for the island. [1] : 392 More inclement weather began to prevail in Barbados ahead of the hurricane on September 6, continuing for several days with showers and thunderstorms. [8] : 24 Despite the frequent rainfall, the air pressure held steady for several days. [d] The existence of an approaching hurricane remained inconclusive until September 10, when observations suggested a tropical cyclone was present southeast of Barbados, and the air pressure began to fall rapidly. [1] : 392 These findings were transmitted to the U.S. Weather Bureau in Washington, D.C. at 12:40 p.m. that day by P. McDonough, a Weather Bureau Observer stationed at Bridgetown. [1] : 392 [11] : 116 In response, the U.S. Weather Bureau communicated hurricane warnings to the bureau's stations in the Lesser Antilles, requesting the stations to disseminate warnings to those in their purview. Additional advisories were transmitted throughout the Caribbean Sea to support observation of the storm. Initial forecasts from the U.S. Weather Bureau projected that the hurricane would track slowly northwest with increasing strength. [1] : 392 Ships moored at the Bridgetown harbour and Carlisle Bay either left or were secured further in advance of the hurricane. [1] : 393 The hurricane warning efforts of the newly established West Indian Weather Service of the U.S. Weather Bureau were later lauded by the press, including the Daily Gleaner , the New York Times , and the Times-Democrat . [1] : 394 However, McDonough wrote that the many locals "pooh-poohed the information given out," believing that the island was "immune" from hurricanes due to the long period of time elapsed since the last destructive storm. [1] : 393
The hurricane impacted Barbados on the night of September 10–11, a night that the Barbados Agricultural Reporter described as one that would "live forever in the memory of the present generation of Barbadians." The storm's forces were experienced for around ten hours, with the strongest winds buffeting the island from around 7:30 p.m. on September 10 to 4 a.m. on September 11. [1] : 392 Gale-force winds were experienced after 6:30 p.m. and hurricane-force winds set in after 9 p.m. [8] : 25 [1] : 392 McDonough recorded a peak one-minute sustained wind of 75 mph (121 km/h) at 10:18 p.m. The shelter housing the associated anemometer and other weather instruments was subsequently destroyed by the wind, damaging the instruments or leaving them unusable. McDonough believed that winds were at their strongest between 11 p.m. and midnight. [1] : 392 Winds in Bridgetown peaked at 62 mph (100 km/h). [2] : 15 McDonough also recorded a minimum air pressure of 997.7 mbar (hPa; 29.462 inHg) at 9:20 p.m. and a total rainfall accumulation of 11.42 in (290 mm) between 6 p.m. September 10 and 10:30 a.m. September 12. The September 17 issue of The Barbados Advocate provided the following summation of the storm's impact: [1] : 392
Fiercer and more destructive hurricanes may have visited the West Indies in years past, but taking into consideration the general condition of her industry and its gloomy prospects, never has a more appalling calamity fallen on this island since first it rose out of these western seas, than the fearful hurricane that ravaged it from shore to shore on [the night of September 10].
The hurricane killed 83 people and injured 150 on Barbados according to the U.S. Weather Bureau, [1] : 391 though a report published in the Quarterly Journal of the Royal Meteorological Society documented 115 fatalities on the island. [8] : 29 McDonough reported that 5,062 houses were completely destroyed and another 2,359 sustained at least partial damage, displacing some 40,000–45,000 people. [1] : 393 The RMS report enumerated 11,400 destroyed homes and 50,000 displaced people. [8] : 29 Property damage resulting from the hurricane amounted to US$2.5 million according to the U.S. Weather Bureau. [1] : 391 Impacts from the hurricane were experienced throughout Barbados, though the most severe effects occurred along the eastern and southern areas of the island. Despite being secured by additional anchors, several ships harboured at Carlisle Bay were severed from their anchorage and blown out to sea by the hurricane and marooned on reefs near Bridgeport and 100 mi (160 km) to the west along reefs near St. Vincent. [1] : 393 Five ships were driven out to sea with their anchors dragged along the seafloor, losing all sail and drifting broadside for a distance of roughly 105 mi (169 km) over the course of 15 hours before beaching near Georgetown, St. Vincent. [8] : 26 The crews of the vessels Grace Lynwood, Lapland, and Loando were rescued after being blown onto the St. Vincent reefs. The vessels Florence, Florence B. Parr, Kate Florence, and Lovdahl were all blown out to sea with no subsequent correspondence. The Campania, Elmo, Ocean Traveller, and many lighters were beached on reefs near Bridgeport and deemed total losses. Smaller ships were destroyed by the heavy surf. [1] : 393
A section of the Bridgetown wharf was severed by the rough seas, and waves crashed over the wharf onto the city streets. The streets were rendered impassable by the storm, snarling vehicle traffic and streetcar service; the Bridgetown streetcar service was restored in limited capacity on September 12. The suburbs of Bridgetown sustained considerable damage, with trees snapped or uprooted and frame houses razed. Strong winds blew down thousands of telephone poles, incapacitating the island's entire telephone system. [1] : 393 St. Michael and Belleville also suffered extensively, with The Times reporting them as "totally demolished". [2] : 17 The sugar cane crop also experienced significant losses. [1] : 393
St. Vincent and St. Lucia
St. Vincent and St. Lucia sustained severe effects comparable to those experienced on Barbados. [1] : 391 Rough seas began to encroach upon the St. Vincent coast 20 hours before the hurricane arrived. [8] : 29 By 3 p.m. on September 10, falling air pressures on St. Vincent began to indicate that a hurricane was imminent, prompting warnings of the approaching storm. Strong winds battered St. Vincent on September 11, uprooting trees and disrupting telecommunications. [1] : 393 The hurricane's winds were at their strongest between 1 and 2 p.m., and the storm's effects largely subsided by 3 p.m. H. Powell, the curator of the Saint Vincent and the Grenadines Botanic Gardens, estimated that wind speeds reached 90–100 mph (140–160 km/h). A minimum barometric pressure of 965.43 mbar (hPa; 28.509 inHg) was recorded during a period of calm on the island. Between 9 a.m. on September 11 and 9 a.m. on September 12, 9.17 in (233 mm) of rainfall was recorded at the Botanic Gardens; [1] : 393 an estimated 14 in (360 mm) of rain fell at St. Vincent during the entirety of the storm. [8] : 27
Powell described a previous hurricane in 1886 as being "mere 'child's play'" compared to the 1898 storm in St. Vincent, and reported that some residents described the hurricane as "in every way more destructive" than a significant hurricane in 1831. [1] : 393–394 The death toll in St. Vincent tallied around in the hundreds; [8] : 29 the RMS analysis reported roughly 200 fatalities while the New York Times reported around 300 fatalities. [8] : 29 [2] : 15 Around 6,000 homes were destroyed or irreparably damaged, displacing approximately 20,000 people. Strong winds destroyed almost every church and chapel on the island and uprooted numerous trees. [8] : 29 Nearly all of the large trees at the Botanic Gardens were downed. Trees and homes that withstood the northerly winds accompanying the initial approach of the hurricane were destroyed by the opposing winds that followed. [1] : 393 Heavy rain from the hurricane produced floods that cascaded down mountainsides, razing entire villages and estates. [8] : 29 Shipping in Kingstown was wrecked by the rough seas. [8] : 29 The villages of Richmond and Wallibou were a "complete wreck", with no houses remaining. In Chateaubelair, many houses were demolished, while a few were still standing after the storm, albeit with severe damage. Forty-five deaths occurred in the village. Similar impact was reported in Cumberland, with one death. Only one house was not destroyed at Barrouallie. Thirty fatalities were reported, eleven of which occurred after a church which people sought refuge in was wrecked. In Layou, only the police barracks remained standing.[ citation needed ]
Much of the damage in St. Lucia was inflicted by a ten-hours-long rainfall that led to floods and landslides. [2] : 17 Valleys in St. Lucia temporarily became lakes after accumulating floodwaters. A landslide triggered by heavy rain in St. Lucia engulfed homes within a 3 mi (4.8 km) stretch of a valley. Castries Harbour suffered heavy damage due to the heavy seas. [8] : 29
Elsewhere
William B. Stockman, a U.S. Weather Bureau forecaster serving under the agency's West Indian Weather Service at Kingston, Jamaica, directed the raising of hurricane signals at Saint-Pierre, Martinique, St. Kitts, and St. Thomas after receiving weather observations on September 10 indicative of a hurricane. Spanish ships delayed their departures from San Juan, Puerto Rico, upon receiving notice of the storm. [1] : 394
Within the Lesser Antilles outside of Barbados, St. Lucia, and St. Vincent, impacts were comparatively minor and limited to roiled seas and heavy rain. [1] : 394 Impacts in the Grenadines were minor outside of Bequia, located just south of St. Vincent. [2] : 18 Thunderstorms and rainfall spread to other parts of the Windward Islands, with rainfall totals reaching 2.25 in (57 mm) at Grenada and 5.5 in (140 mm) at Dominica. [8] : 27 A landslide in Trois-Rivières, Guadeloupe, engulfed two homes, causing nine deaths. The sloop Marie Stella capsized off Goyave, resulting in another nine deaths near Guadeloupe. [2] : 17
The storm passed near St. Kitts without causing much damage. [1] : 394 [2] : 15 Winds at Basseterre peaked at 58 mph (93 km/h) on September 12. [2] : 15 Rainfall accumulations between the morning of September 12 and the morning of September 13 reached 5.5 in (140 mm) on St. Kitts; roughly the same amount was recorded in Antigua. Around 20 in (510 mm) of rain was recorded at Nevis throughout the storm and 17.25 in (438 mm) of rain was recorded in Montserrat over a 48-hour period. [8] : 28
The ship Fluminense arrived in Barbados with damage from a storm encounter on September 18 after departing from New York. Partagás surmised that the vessel likely encountered the hurricane somewhere between Cape Hatteras and Bermuda. On September 19, the ship Osorno possibly encountered the storm en route from Bordeaux to New York, experiencing 24 hours of gale-force winds. One crewmember was washed overboard and drowned. [2] : 18
See also
Notes
- ↑ All times and dates are based on Coordinated Universal Time (UTC) unless otherwise noted.
- ↑ All monetary values are in 1898 United States dollar unless otherwise noted.
- ↑ HURricane DATa (HURDAT) is a database of historical tropical cyclones maintained by the National Hurricane Center. The database is routinely revised to incorporate new data. [5] [6]
- ↑ An approaching hurricane is associated with a decrease in air pressure ahead of the storm. [10] : 2, 5
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References
- 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 Garriott, E. B. (September 1898). Abbe, Cleveland (ed.). "Forecasts and Warnings". Monthly Weather Review. 26 (9): 391–394. Bibcode:1898MWRv...26..391G. doi: 10.1175/1520-0493(1898)26[391b:FAW]2.0.CO;2 .
- 1 2 3 4 5 6 7 8 9 10 11 12 13 14 Partagás, José Fernandez; Diaz, Henry F. (1999). "Year 1910". A Reconstruction of Historical Tropical Cyclone Frequency in the Atlantic from Documentary and Other Historical Sources Part IV: 1891–1900 (PDF). Boulder, Colorado: NOAA Climate Diagnostics Center. pp. 13–21. Retrieved 11 August 2023– via Atlantic Oceanographic and Meteorological Laboratory.
- ↑ Neumann, Charles J.; Jarvinen, B. R.; McAdie, C. J.; Elms, J. D. (November 1993). Tropical Cyclones of North Atlantic Ocean, 1871-1992 (Report). Historical Climatology Series. Asheville, North Carolina: National Oceanic and Atmospheric Administration. p. 141 – via HathiTrust.
- 1 2 Landsea, Chris; Anderson, Craig; Bredemeyer, William; Carrasco, Cristina; Charles, Noel; Chenoweth, Michael; Clark, Gil; Delgado, Sandy; Dunion, Jason; Ellis, Ryan; Fernandez-Partagas, Jose; Feuer, Steve; Gamanche, John; Glenn, David; Hagen, Andrew; Hufstetler, Lyle; Mock, Cary; Neumann, Charlie; Perez Suarez, Ramon; Prieto, Ricardo; Sanchez-Sesma, Jorge; Santiago, Adrian; Sims, Jamese; Thomas, Donna; Lenworth, Woolcock; Zimmer, Mark (2003). "Documentation of Atlantic Tropical Cyclones Changes in HURDAT". Atlantic Oceanographic and Meteorological Laboratory (Metadata). Miami, Florida: National Oceanic and Atmospheric Administration. [Information regarding modifications to the track of the 1898 Windward Islands hurricane]. Retrieved 19 August 2023.
- ↑ Landsea, Chris; Franklin, James; Blake, Eric; Tanabe, Ray (April 2013). "The revised Northeast and North Central Pacific hurricane database (HURDAT2)" (PDF). Atlantic Oceanographic and Meteorological Laboratory. Retrieved 23 August 2023.
- ↑ Rappaport, Edward N.; Franklin, James L.; Avila, Lixion A.; Baig, Stephen R.; Beven, John L.; Blake, Eric S.; Burr, Christopher A.; Jiing, Jiann-Gwo; Juckins, Christopher A.; Knabb, Richard D.; Landsea, Christopher W.; Mainelli, Michelle; Mayfield, Max; McAdie, Colin J.; Pasch, Richard J.; Sisko, Christopher; Stewart, Stacy R.; Tribble, Ahsha N. (April 2009). "Advances and Challenges at the National Hurricane Center". Weather and Forecasting. 24 (2): 395–419. Bibcode:2009WtFor..24..395R. doi: 10.1175/2008WAF2222128.1 .
- 1 2 "1898 Hurricane NOT_NAMED (1898249N11333)". International Best Track Archive for Climate Stewardship (IBTrACS) (Database). Asheville, North Carolina: University of North Carolina at Asheville . Retrieved 23 August 2023.
- 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 Carpenter, A. (1899). "The West Indian Hurricane, September 1898". Quarterly Journal of the Royal Meteorological Society. 25 (109). Royal Meteorological Society: 23–32. Bibcode:1899QJRMS..25...23C. doi:10.1002/qj.49702510904. S2CID 122299216.
- ↑ "Chart XV. Weather Charts. September 11, 1898". Monthly Weather Review. 24 (9). United States Weather Bureau: 54. September 1898. Retrieved 16 September 2023– via Internet Archive.
- ↑ Tannehill, Ivan Ray (February 1939). The Hurricane (PDF) (Report). Washington, D.C.: United States Government Printing Office. Retrieved 19 August 2023– via National Agricultural Library Digital Collections.
- ↑ Ward, R. DeC. (20 January 1899). "The Windward Islands Hurricane of September, 1898". Science. 9 (212): 116–117. doi:10.1126/science.9.212.116.c. S2CID 239783629.
External links
 Weather map depicting the hurricane moving through the Windward Islands on the morning of September 11 |
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