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1917 Atlantic hurricane season

The 1917 Atlantic hurricane season featured nine known tropical cyclones, four of which became tropical storms.[1] The first system appeared on July 6 east of the Windward Islands. After crossing the islands and traversing the Caribbean Sea, the storm struck Honduras, Belize, and Mexico, before dissipating on July 14. After more than three weeks without tropical cyclogenesis, another tropical storm developed west of Bermuda. As the storm brushed eastern New England, four ships sank near Nantucket, causing 41 fatalities. The same cyclone brought damaging winds to Nova Scotia before transitioning into an extratropical cyclone on August 10.

1917 Atlantic hurricane season
Season summary map
Seasonal boundaries
First system formedJuly 6, 1917
Last system dissipatedOctober 20, 1917
Strongest storm
Name"Nueva Gerona"
 • Maximum winds150 mph (240 km/h)
(1-minute sustained)
 • Lowest pressure928 mbar (hPa; 27.4 inHg)
Seasonal statistics
Total depressions9
Total storms4
Hurricanes2
Major hurricanes
(Cat. 3+)
2
Total fatalities76 total
Total damage$170,000 (1917 USD)
Related articles
Atlantic hurricane seasons
1915, 1916, 1917, 1918, 1919

A hurricane developed over the central Atlantic Ocean on August 30 and ultimately affected Bermuda with heightened tides as it passed to the east. Elsewhere, the hurricane had little impact, becoming extratropical on September 5. After the third system, a series of four tropical depressions formed, but failed to become severe. The fourth hurricane brought devastation to Jamaica, Cuba, and portions of the Gulf Coast of the United States, especially western parts of the Florida Panhandle. Overall, the storm left six deaths and inflicted at least $170,000 (1917 USD) in damage.

The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 61,[2] slightly above the 1911–1920 average of 58.7.[3] 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 high 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.[2]

Timeline edit

1917 Neuva Gerona hurricaneSaffir–Simpson Hurricane Scale

Systems edit

Tropical Storm One edit

Tropical storm (SSHWS)
   
DurationJuly 6 – July 14
Peak intensity50 mph (85 km/h) (1-min);
<1006 mbar (hPa)

Historical weather maps indicated a trough east of the Windward Islands on July 6.[1] Around 06:00 UTC, a tropical depression formed about 80 mi (130 km) southeast of Barbados. Moving west-northwestward, the depression crossed the Windward Islands and entered the Caribbean Sea early on July 7. Later that day, the system intensified into a tropical storm. After peaking with winds of 50 mph (85 km/h) on July 8, it began to weaken and fell to tropical depression intensity early on July 10. Early the next day, the depression struck Honduras, before briefly emerging into the Caribbean Sea. The system struck Belize around 06:00 UTC on July 12 and entered the Bay of Campeche about 24 hours later. At midday on July 14, the storm struck south of Tampico, Tamaulipas.[4] In the city of Veracruz, 4 in (100 mm) of rain fell in a 24-hour period.[1]

Tropical Storm Two edit

Tropical storm (SSHWS)
   
DurationAugust 6 – August 10
Peak intensity70 mph (110 km/h) (1-min);
<994 mbar (hPa)

An area of low pressure developed into a tropical storm to the west of Bermuda at 00:00 UTC on August 6.[1][4] Initially the storm drifted westward and strengthened minimally. By August 9, it curved northward and began to accelerate. The storm strengthened further and attained its peak intensity with maximum sustained winds of 70 mph (110 km/h) and a minimum barometric pressure of 994 mbar (29.4 inHg) early on August 10;[4] both were observations from the Nantucket Shoals Lightship. Offshore the island of Nantucket in Massachusetts, four ships were lost, with an estimated 41 people perishing.[1] The storm continued northeastward and made landfall in Saint John County, New Brunswick while becoming extratropical at 00:00 UTC on August 11. The remnants dissipated over the Labrador Sea later that day.[4] In Nova Scotia, dozens of boats were beached. Wind speeds up to 64 mph (103 km/h) in Yarmouth damaged trees, power lines, windows, and roofs. Crops were impacted throughout the Annapolis Valley. Fifteen barns were damaged or demolished.[5]

Hurricane Three edit

Category 3 hurricane (SSHWS)
   
DurationAugust 30 – September 5
Peak intensity120 mph (195 km/h) (1-min);
<980 mbar (hPa)

Weather maps indicated that an area of low pressure existed between the Lesser Antilles and Cape Verde on August 30. At 12:00 UTC that day, a tropical storm developed while located about 900 mi (1,400 km) northeast of Cayenne, French Guiana.[1][4] Moving west-northwestward, the tropical storm reached Category 1 hurricane intensity early on August 31. By late on September 1, the storm had intensified into a Category 2 hurricane. Further strengthening occurred brought the hurricane to a Category 3 intensity late on September 3, while briefly heading northward. Early the next day, the cyclone attained its peak force with winds of 120 mph (195 km/h); the lowest barometric pressure reading in association with the storm was 980 mbar (29 inHg).[4]

While passing east of Bermuda late on September 4, the storm's "unprecedented high tides" lashed the island. Portions of Market Square on St. David's Island were submerged. Additionally, a large section of Higgs' Island was completely washed away.[1] The storm accelerated to the northeast and weakened to a Category 2 hurricane around 12:00 UTC on September 5. Losing tropical characteristics, the hurricane transitioned into an extratropical cyclone at 00:00 UTC the following day, while located about 290 mi (470 km) southeast of Cape Race, Newfoundland. Its remnants tracked northeastward until dissipating near Iceland on September 7.[4]

Hurricane Four edit

Category 4 hurricane (SSHWS)
   
DurationSeptember 20 – September 30
Peak intensity150 mph (240 km/h) (1-min);
928 mbar (hPa)

The Nueva Gerona Hurricane of 1917

A tropical storm formed about 160 mi (260 km) east-northeast of Barbados on September 20. Later that day, the storm crossed the Lesser Antilles between the islands of Saint Lucia and Martinique. Upon entering the Caribbean Sea on September 21, the system intensified quicker, becoming a Category 1 hurricane several hours later. While passing south of the Tiburon Peninsula on the following day, the storm strengthened into a Category 2 hurricane. Later on September 23, the hurricane struck the northern coast of Jamaica, before re-emerging into the Caribbean Sea. Around 06:00 UTC on September 24, it intensified into a Category 3 hurricane. Approximately 24 hours later, the hurricane deepened into a Category 4 hurricane.[4]

Ramón Perez of the Instituto de Meteorología de la República de Cuba estimated that this hurricane attained a minimum barometric pressure of 928 mbar (27.4 inHg) on September 25. Using the pressure-wind relationship, HURDAT increased the maximum sustained wind speed to 150 mph (240 km/h).[1] Within the next six hours, the hurricane made landfall in the eastern Pinar del Río Province of Cuba. The system entered the Gulf of Mexico later on September 25. While moving northwestward, the storm fell to Category 3 hurricane intensity early on September 27. It briefly tracked generally northward and approached southeastern Louisiana before re-curving northeastward late the next day. At 02:00 UTC on September 29, the hurricane made landfall near Camp Walton, Florida with winds of 115 mph (185 km/h). Shortly thereafter, the system rapidly weakened to a Category 1 hurricane and fell to a tropical storm several hours later. Early on September 30, it became extratropical over Georgia. About six hours later, the remnants of the hurricane dissipated.[4]

Some islands in the Lesser Antilles experienced strong winds and heavy rainfall, including Dominica, Guadeloupe, and Saint Lucia.[1] In Jamaica, the hurricane caused significant damages to banana and coconut plantations. Communications from Holland Bay were disrupted when the station was demolished.[6] The greatest damages were reported from the northern half of the island. In Nueva Gerona, strong winds destroyed well-constructed buildings, devastating the town. Orchards and crops were destroyed on the Pinar del Río Province.[7] In Louisiana and Mississippi, impact was generally limited to damaged crops and timber stands.[1] One death from drowning was reported in Louisiana.[7] Farther east in Mobile, Alabama, portions of roofs, trees, and other debris littered streets.[8] Communications were severed in Pensacola, Florida. Several small watercraft washed ashore, and numerous wharves, docks, and boat storages suffered impact. Total damages were estimated near $170,000 in Pensacola area. Five deaths were reported in Florida, all of them in the city of Crestview.[7]

Tropical depressions edit

In addition to the four systems reaching tropical storm intensity, there were five other tropical depressions. The first probably developed from a tropical wave offshore western Africa on September 12, according to historical weather maps and the Comprehensive Ocean-Atmosphere Data Set (COADS), both of which indicated a closed circulation. This depression was last observed on September 14. Another depression also developed on September 12, well to the east of the Lesser Antilles. While approaching the islands, the storm may have briefly strengthened into a tropical storm on September 15, as suggested by a ship report of winds blowing 40 mph (65 km/h). The cyclone likely dissipated on September 15.[1]

The next tropical depression briefly existed off the east coast of Florida on September 14. It soon became extratropical, though its remnants lasted several days, traveling along the East Coast of the United States. At Nantucket, a wind gust up to 69 mph (111 km/h) was observed. The extratropical remnants probably dissipated near Newfoundland on September 20. Meanwhile, a trough in the Gulf of Mexico had developed into a tropical depression on September 14. The following day, the system made landfall in Louisiana and disintegrated into a disorganized area of thunderstorms over Mississippi and Arkansas on September 16. The last tropical depression and final cyclone of the season developed on October 19 from a trough over the central Atlantic Ocean. Two days later, the depression was absorbed by a cold front.[1]

See also edit

References edit

  1. ^ a b c d e f g h i j k l Christopher W. Landsea; et al. (December 2012). Documentation of Atlantic Tropical Cyclones Changes in HURDAT. Atlantic Oceanographic and Meteorological Laboratory (Report). Miami, Florida: National Oceanic and Atmospheric Administration. Retrieved July 11, 2014.
  2. ^ a b Atlantic basin Comparison of Original and Revised HURDAT. Hurricane Research Division; Atlantic Oceanographic and Meteorological Laboratory (Report). Miami, Florida: National Oceanic and Atmospheric Administration. September 2021. Retrieved October 1, 2021.
  3. ^ Landsea, Christopher W.; et al. (May 15, 2008). "A Reanalysis of the 1911–20 Atlantic Hurricane Database" (PDF). Journal of Climate. 21 (10). Miami, Florida: National Oceanic and Atmospheric Administration: 2146. Bibcode:2008JCli...21.2138L. doi:10.1175/2007JCLI1119.1. S2CID 1785238. Retrieved September 6, 2021.
  4. ^ a b c d e f g h i "Atlantic hurricane best track (HURDAT version 2)" (Database). United States National Hurricane Center. April 5, 2023. Retrieved April 9, 2024.   This article incorporates text from this source, which is in the public domain.
  5. ^ 1917-1 (Report). Moncton, New Brunswick: Environment Canada. November 20, 2009. from the original on July 3, 2013. Retrieved July 12, 2014.
  6. ^ "Storm News Received From the Various Districts". The Daily Gleaner. 1917.
  7. ^ a b c Henry C. Frankenfield (October 1, 1917). Section III. – Forecasts (PDF). Weather Bureau (Report). Washington, D.C.: National Oceanic and Atmospheric Administration. Retrieved July 12, 2014.
  8. ^ "Reports Indicate Slight Life Loss". The Daily News. 1917.

External links edit

  • Monthly Weather Review

1917, atlantic, hurricane, season, featured, nine, known, tropical, cyclones, four, which, became, tropical, storms, first, system, appeared, july, east, windward, islands, after, crossing, islands, traversing, caribbean, storm, struck, honduras, belize, mexic. The 1917 Atlantic hurricane season featured nine known tropical cyclones four of which became tropical storms 1 The first system appeared on July 6 east of the Windward Islands After crossing the islands and traversing the Caribbean Sea the storm struck Honduras Belize and Mexico before dissipating on July 14 After more than three weeks without tropical cyclogenesis another tropical storm developed west of Bermuda As the storm brushed eastern New England four ships sank near Nantucket causing 41 fatalities The same cyclone brought damaging winds to Nova Scotia before transitioning into an extratropical cyclone on August 10 1917 Atlantic hurricane seasonSeason summary mapSeasonal boundariesFirst system formedJuly 6 1917Last system dissipatedOctober 20 1917Strongest stormName Nueva Gerona Maximum winds150 mph 240 km h 1 minute sustained Lowest pressure928 mbar hPa 27 4 inHg Seasonal statisticsTotal depressions9Total storms4Hurricanes2Major hurricanes Cat 3 2Total fatalities76 totalTotal damage 170 000 1917 USD Related articles1910 19 Pacific hurricane seasons 1902 19 Pacific typhoon seasons 1910s North Indian Ocean cyclone seasonsAtlantic hurricane seasons1915 1916 1917 1918 1919A hurricane developed over the central Atlantic Ocean on August 30 and ultimately affected Bermuda with heightened tides as it passed to the east Elsewhere the hurricane had little impact becoming extratropical on September 5 After the third system a series of four tropical depressions formed but failed to become severe The fourth hurricane brought devastation to Jamaica Cuba and portions of the Gulf Coast of the United States especially western parts of the Florida Panhandle Overall the storm left six deaths and inflicted at least 170 000 1917 USD in damage The season s activity was reflected with an accumulated cyclone energy ACE rating of 61 2 slightly above the 1911 1920 average of 58 7 3 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 high 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 2 Contents 1 Timeline 2 Systems 2 1 Tropical Storm One 2 2 Tropical Storm Two 2 3 Hurricane Three 2 4 Hurricane Four 2 5 Tropical depressions 3 See also 4 References 5 External linksTimeline editSystems editTropical Storm One edit Tropical storm SSHWS nbsp nbsp DurationJuly 6 July 14Peak intensity50 mph 85 km h 1 min lt 1006 mbar hPa Historical weather maps indicated a trough east of the Windward Islands on July 6 1 Around 06 00 UTC a tropical depression formed about 80 mi 130 km southeast of Barbados Moving west northwestward the depression crossed the Windward Islands and entered the Caribbean Sea early on July 7 Later that day the system intensified into a tropical storm After peaking with winds of 50 mph 85 km h on July 8 it began to weaken and fell to tropical depression intensity early on July 10 Early the next day the depression struck Honduras before briefly emerging into the Caribbean Sea The system struck Belize around 06 00 UTC on July 12 and entered the Bay of Campeche about 24 hours later At midday on July 14 the storm struck south of Tampico Tamaulipas 4 In the city of Veracruz 4 in 100 mm of rain fell in a 24 hour period 1 Tropical Storm Two edit Tropical storm SSHWS nbsp nbsp DurationAugust 6 August 10Peak intensity70 mph 110 km h 1 min lt 994 mbar hPa An area of low pressure developed into a tropical storm to the west of Bermuda at 00 00 UTC on August 6 1 4 Initially the storm drifted westward and strengthened minimally By August 9 it curved northward and began to accelerate The storm strengthened further and attained its peak intensity with maximum sustained winds of 70 mph 110 km h and a minimum barometric pressure of 994 mbar 29 4 inHg early on August 10 4 both were observations from the Nantucket Shoals Lightship Offshore the island of Nantucket in Massachusetts four ships were lost with an estimated 41 people perishing 1 The storm continued northeastward and made landfall in Saint John County New Brunswick while becoming extratropical at 00 00 UTC on August 11 The remnants dissipated over the Labrador Sea later that day 4 In Nova Scotia dozens of boats were beached Wind speeds up to 64 mph 103 km h in Yarmouth damaged trees power lines windows and roofs Crops were impacted throughout the Annapolis Valley Fifteen barns were damaged or demolished 5 Hurricane Three edit Category 3 hurricane SSHWS nbsp nbsp DurationAugust 30 September 5Peak intensity120 mph 195 km h 1 min lt 980 mbar hPa Weather maps indicated that an area of low pressure existed between the Lesser Antilles and Cape Verde on August 30 At 12 00 UTC that day a tropical storm developed while located about 900 mi 1 400 km northeast of Cayenne French Guiana 1 4 Moving west northwestward the tropical storm reached Category 1 hurricane intensity early on August 31 By late on September 1 the storm had intensified into a Category 2 hurricane Further strengthening occurred brought the hurricane to a Category 3 intensity late on September 3 while briefly heading northward Early the next day the cyclone attained its peak force with winds of 120 mph 195 km h the lowest barometric pressure reading in association with the storm was 980 mbar 29 inHg 4 While passing east of Bermuda late on September 4 the storm s unprecedented high tides lashed the island Portions of Market Square on St David s Island were submerged Additionally a large section of Higgs Island was completely washed away 1 The storm accelerated to the northeast and weakened to a Category 2 hurricane around 12 00 UTC on September 5 Losing tropical characteristics the hurricane transitioned into an extratropical cyclone at 00 00 UTC the following day while located about 290 mi 470 km southeast of Cape Race Newfoundland Its remnants tracked northeastward until dissipating near Iceland on September 7 4 Hurricane Four edit Category 4 hurricane SSHWS nbsp nbsp DurationSeptember 20 September 30Peak intensity150 mph 240 km h 1 min 928 mbar hPa The Nueva Gerona Hurricane of 1917 Main article 1917 Nueva Gerona hurricane A tropical storm formed about 160 mi 260 km east northeast of Barbados on September 20 Later that day the storm crossed the Lesser Antilles between the islands of Saint Lucia and Martinique Upon entering the Caribbean Sea on September 21 the system intensified quicker becoming a Category 1 hurricane several hours later While passing south of the Tiburon Peninsula on the following day the storm strengthened into a Category 2 hurricane Later on September 23 the hurricane struck the northern coast of Jamaica before re emerging into the Caribbean Sea Around 06 00 UTC on September 24 it intensified into a Category 3 hurricane Approximately 24 hours later the hurricane deepened into a Category 4 hurricane 4 Ramon Perez of the Instituto de Meteorologia de la Republica de Cuba estimated that this hurricane attained a minimum barometric pressure of 928 mbar 27 4 inHg on September 25 Using the pressure wind relationship HURDAT increased the maximum sustained wind speed to 150 mph 240 km h 1 Within the next six hours the hurricane made landfall in the eastern Pinar del Rio Province of Cuba The system entered the Gulf of Mexico later on September 25 While moving northwestward the storm fell to Category 3 hurricane intensity early on September 27 It briefly tracked generally northward and approached southeastern Louisiana before re curving northeastward late the next day At 02 00 UTC on September 29 the hurricane made landfall near Camp Walton Florida with winds of 115 mph 185 km h Shortly thereafter the system rapidly weakened to a Category 1 hurricane and fell to a tropical storm several hours later Early on September 30 it became extratropical over Georgia About six hours later the remnants of the hurricane dissipated 4 Some islands in the Lesser Antilles experienced strong winds and heavy rainfall including Dominica Guadeloupe and Saint Lucia 1 In Jamaica the hurricane caused significant damages to banana and coconut plantations Communications from Holland Bay were disrupted when the station was demolished 6 The greatest damages were reported from the northern half of the island In Nueva Gerona strong winds destroyed well constructed buildings devastating the town Orchards and crops were destroyed on the Pinar del Rio Province 7 In Louisiana and Mississippi impact was generally limited to damaged crops and timber stands 1 One death from drowning was reported in Louisiana 7 Farther east in Mobile Alabama portions of roofs trees and other debris littered streets 8 Communications were severed in Pensacola Florida Several small watercraft washed ashore and numerous wharves docks and boat storages suffered impact Total damages were estimated near 170 000 in Pensacola area Five deaths were reported in Florida all of them in the city of Crestview 7 Tropical depressions edit In addition to the four systems reaching tropical storm intensity there were five other tropical depressions The first probably developed from a tropical wave offshore western Africa on September 12 according to historical weather maps and the Comprehensive Ocean Atmosphere Data Set COADS both of which indicated a closed circulation This depression was last observed on September 14 Another depression also developed on September 12 well to the east of the Lesser Antilles While approaching the islands the storm may have briefly strengthened into a tropical storm on September 15 as suggested by a ship report of winds blowing 40 mph 65 km h The cyclone likely dissipated on September 15 1 The next tropical depression briefly existed off the east coast of Florida on September 14 It soon became extratropical though its remnants lasted several days traveling along the East Coast of the United States At Nantucket a wind gust up to 69 mph 111 km h was observed The extratropical remnants probably dissipated near Newfoundland on September 20 Meanwhile a trough in the Gulf of Mexico had developed into a tropical depression on September 14 The following day the system made landfall in Louisiana and disintegrated into a disorganized area of thunderstorms over Mississippi and Arkansas on September 16 The last tropical depression and final cyclone of the season developed on October 19 from a trough over the central Atlantic Ocean Two days later the depression was absorbed by a cold front 1 See also edit nbsp Tropical cyclones portal1900 1940 South Pacific cyclone seasons 1900 1950 South West Indian Ocean cyclone seasons 1910s Australian region cyclone seasonsReferences edit a b c d e f g h i j k l Christopher W Landsea et al December 2012 Documentation of Atlantic Tropical Cyclones Changes in HURDAT Atlantic Oceanographic and Meteorological Laboratory Report Miami Florida National Oceanic and Atmospheric Administration Retrieved July 11 2014 a b Atlantic basin Comparison of Original and Revised HURDAT Hurricane Research Division Atlantic Oceanographic and Meteorological Laboratory Report Miami Florida National Oceanic and Atmospheric Administration September 2021 Retrieved October 1 2021 Landsea Christopher W et al May 15 2008 A Reanalysis of the 1911 20 Atlantic Hurricane Database PDF Journal of Climate 21 10 Miami Florida National Oceanic and Atmospheric Administration 2146 Bibcode 2008JCli 21 2138L doi 10 1175 2007JCLI1119 1 S2CID 1785238 Retrieved September 6 2021 a b c d e f g h i Atlantic hurricane best track HURDAT version 2 Database United States National Hurricane Center April 5 2023 Retrieved April 9 2024 nbsp This article incorporates text from this source which is in the public domain 1917 1 Report Moncton New Brunswick Environment Canada November 20 2009 Archived from the original on July 3 2013 Retrieved July 12 2014 Storm News Received From the Various Districts The Daily Gleaner 1917 a b c Henry C Frankenfield October 1 1917 Section III Forecasts PDF Weather Bureau Report Washington D C National Oceanic and Atmospheric Administration Retrieved July 12 2014 Reports Indicate Slight Life Loss The Daily News 1917 External links edit nbsp Wikimedia Commons has media related to 1917 Atlantic hurricane season Monthly Weather Review Retrieved from https en wikipedia org w index php title 1917 Atlantic hurricane season amp oldid 1194665839 Hurricane Three, wikipedia, wiki, book, books, library,

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