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1940 Louisiana hurricane

The 1940 Louisiana hurricane caused record flooding across much of the Southern United States in August 1940. The second tropical cyclone and hurricane of the annual hurricane season, it formed from a frontal low off the west coast of Florida on August 3. Initially a weak disturbance, it moved generally westward, slowly gaining in intensity. Early on August 4, the depression attained tropical storm intensity. Ships in the vicinity of the storm reported a much stronger tropical cyclone than initially suggested. After reaching hurricane strength on August 5 south of the Mississippi River Delta, the storm strengthened further into a Category 2 hurricane with maximum sustained winds of 100 mph and a minimum barometric pressure of 972 mbar (hPa; 28.71 inHg) at 0600 UTC on August 7. The hurricane moved ashore near Sabine Pass, Texas later that day at peak strength. Once inland, the storm executed a sharp curve to the north and quickly weakened, degenerating into a tropical storm on August 8 before dissipating over Arkansas on August 10.

1940 Louisiana hurricane
Surface weather analysis of the storm on August 7, at peak intensity
Meteorological history
FormedAugust 3, 1940 (1940-08-03)
DissipatedAugust 10, 1940 (1940-08-11)
Category 2 hurricane
1-minute sustained (SSHWS/NWS)
Highest winds100 mph (155 km/h)
Lowest pressure972 mbar (hPa); 28.70 inHg
Overall effects
Fatalities7
Damage$10.8 million (1940 USD)
Areas affectedSouthern United States (Texas, Louisiana)
IBTrACS

Part of the 1940 Atlantic hurricane season

Reports of a potentially destructive hurricane near the United States Gulf Coast forced thousands of residents in low-lying areas to evacuate prior to the storm moving inland. Offshore, the hurricane generated rough seas and a strong storm surge, peaking at 6.4 ft (1.95 m) on the western edge of Lake Pontchartrain. The anomalously high tides flooded many of Louisiana's outlying islands, inundating resorts. Strong winds caused moderate infrastructural damage, primarily in Texas, though its impact was mainly to communication networks along the US Gulf Coast which were disrupted by the winds. However, much of the property and crop damage wrought by the hurricane was due to the torrential rainfall it produced in low-lying areas, setting off record floods. Rainfall peaked at 37.5 in (953 mm) in Miller Island off Louisiana, making it the wettest tropical cyclone in state history. Nineteen official weather stations in both Texas and Louisiana recorded record-level 24-hour rainfall totals for the month of August as a result of the slow-moving hurricane. Property, livestock, and crops–especially cotton, corn, and pecan crops–were heavily damaged. Entire ecosystems were also altered by the rainfall. Overall, the storm caused $10.75 million in damages and seven fatalities.[nb 1]

Meteorological history Edit

 
Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
Map key
  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
  Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

In early August, an extratropical trough moved off the coast of South Carolina and Georgia, with a stationary front extending from it.[1][2] A weak low-pressure area began to develop at the southern end of the front just offshore of Jacksonville, Florida.[1] Initially, the storm had an open center of circulation and remained a frontal low as it moved southwestward across Florida, and thus was not considered a fully tropical system at the time. Upon entering the Gulf of Mexico, however, observations indicated that the disturbance developed a closed center of circulation.[2] As a result, the storm was analyzed to have developed into a tropical depression off the western coast of Florida at 1200 UTC on August 3.[3] At the time, weather reports revealed a definite cyclonic rotation, though the depression had a shallow minimum barometric pressure of 1012.5 mbar (hPa; 29.90 inHg).[1] Moving west-southwest, the depression steadily intensified and attained tropical storm intensity at 0000 UTC on August 4.[3] Late that evening, the tropical storm executed a slight northward curve.[1] Strengthening continued into the following day, and ships in the storm's vicinity began to report a much stronger storm than was previously suggested. A ship reported the first gale-force winds associated with the storm at 2100 UTC on August 4.[2] The S.S. Connecticut observed force 11 winds, the strongest wind measurement associated with the storm as recorded by vessel.[1] A minimum pressure of 995 mbar (hPa; 29.39 inHg) was analyzed for the system at 0600 UTC on August 5 based on an observation from a nearby ship.[2]

At 1800 UTC on August 5, the storm strengthened to hurricane strength, the first tropical cyclone of the season to do so. At the time, the hurricane was moving very slowly westward, allowing it to strengthen despite its close proximity to land. The hurricane reached Category 2 intensity by 0600 UTC on August 7.[3] The storm made landfall at peak intensity at around 2100 UTC later that day near Sabine Pass, Texas. At the time, the hurricane had maximum sustained winds of 100 mph (160 km/h), with the storm's maximum winds extending out 10 mi (15 km) from its center.[2] A weather station in Sabine Pass recorded a barometric pressure of 972 mbar (hPa; 28.71 inHg), which was analyzed to have been the lowest pressure measured in association with the storm.[2][3] After moving inland, the storm immediately curved northward and began to gradually weaken.[1] At 0600 UTC on August 8, the cyclone weakened to tropical storm strength while situated over East Texas, and later degenerated to a tropical depression by 1200 UTC the following day. The depression persisted into Arkansas,[4] where it transitioned into a trough of low pressure at 1800 UTC on August 10 after its center of circulation lacked the well-defined closed circulation characteristic of tropical cyclones.[2]

Preparations and impact Edit

 
Rainfall totals in the United States

Upon reaching hurricane strength off the United States Gulf Coast, hurricane warnings were issued for coastal regions from Lake Charles, Louisiana to Sabine Pass, Texas on August 7.[5] Storm warnings were placed for areas east of Lake Charles to Grand Isle, Louisiana and areas west of Sabine Pass to Velasco, Texas.[6] Offshore vessels were also warned of the storm in areas between Bay St. Louis, Mississippi and Galveston, Texas.[7] At the time, the hurricane was forecast to make landfall slightly east of Port Arthur, Texas.[5] In Texas, these warnings were delivered to residents via factory whistles. Evacuation procedures also began as a result of the approaching storm. The Spindletop near Beaumont, Texas and other nearby oil fields were evacuated. Coastal cities near Port Arthur, Texas were also evacuated by state highway police.[6][8] Evacuees took shelter in refitted schools nearby.[8] In the New Orleans, Louisiana area, several thousand residents were evacuated in advance of the storm.[9] On Delacroix Island, Louisiana, 1,000 residents evacuated.[10] Rail and airline operations were halted as a precautionary measure, but were later resumed after the storm passed.[8] All storm warnings were ceased by midnight on August 8.[11]

Even before making landfall, the hurricane caused extensive damage in Louisiana, due in part to the hurricane's slow speed and close proximity to the state coast. Winds as high as 60 mph (100 km/h) brushed the coastline, causing extensive damage. Storm surge pushed coastal waters to near-record heights, inundating low-lying areas. Near Morgan City, Louisiana, 19 people went missing after going on a fishing trip;[5] they were later found marooned at Atchafalaya Basin.[9] The schooner J.W. Clise was abandoned during the storm 135 mi (215 km) south of the Mississippi River Delta, though its crew was also later rescued.[12] Storm surge peaked at 6.4 ft (1.95 m) above-average in western portions of Lake Pontchartrain. A bridge crossing Thunder Bayou, which extended west of the lake, was washed out by the waves. Similarly, a station at Calcasieu Pass reported a storm surge 4.8 ft (1.46 m) high.[12] Conservation officials feared the disturbance would disrupt the seafood and muskrat production.[5] After the storm, it was estimated 75,000 muskrats were killed by the storm's effects.[13] Offshore, Grand Isle was inundated by the strong waves.[10] Around Houma, sugar cane crops were damaged.[14] The hurricane was the strongest to impact Cameron since the tenth hurricane of the 1886 Atlantic hurricane season;[12] strong gusts peaked at 70 mph (115 km/h), disrupting communication lines, thus isolating the city from other locations in the state. The high tides inundated town streets under 2 ft (0.6 m).[9] Other areas extending from western Louisiana to Mobile, Alabama reported communication disruptions. In New Orleans, strong winds uprooted signboards and blew debris across the city streets.[10] Several houses in Shell Beach and Delacroix Island were leveled by strong winds.[12]

Due to the storm's slow movement just offshore the Louisiana coast, the hurricane became the wettest tropical cyclone in state history, with numerous locations reporting record rainfall across the state. Of the state's ten highest official rainfall measurements associated with tropical cyclones, the two highest were measurements taken during the hurricane.[12] Precipitation peaked at 37.5 in (953 mm) on Miller Island. For any given 20,000 mi2 (50,000 km/h2) area of Louisiana, the maximum rainfall averaged 12.1 in (307.3 mm).[15] Thirteen official weather stations in the state reported monthly 24-hour rainfall total records. The highest of these was in Crowley, where 19.76 in (501.9 mm) of precipitation fell on August 9; the station would record 33.71 in (856.2 mm) of rain over the course of the storm. The torrential rainfall submerged the city under 2 ft (0.6 m) of floodwater.[12] In Cameron, the storm dropped 21 in (533 mm) of rain was reported.[16] In St. Landry Parish, bayous flowed over their banks, causing refugees to evacuate to Opelousas. In the Acadiana region of southern Louisiana, the resulting floods were considered worse than the floods that resulted from the Sauvé's Crevasse in 1849. There, whooping crane populations were severely impacted by the rainfall, and only one was known to be alive by 1947. The floods inundated roughly 2,000,000 acres (800,000 hectares) of land in Louisiana. Much of the lowland areas remained underwater until October 1940. As a result, cotton and corn crops experienced significant losses, as well as pecans. Livestock also saw large losses. Impassable areas caused by rising floodwaters prevented firefighters from extinguishing a fire which burned down much of the Shell Oil Company's offices and supply warehouses in the town of Iowa. Across the state, the hurricane caused $9 million in damages, though only six fatalities resulted, relatively less than most storms of similar scale. The low death count was attributed to large evacuation procedures which underwent prior to the storm, as well as guidance provided from the newly opened Weather Bureau east of Lake Charles.[12]

In East Texas, where the hurricane made landfall late on August 7, strong winds were felt across the region. Sustained winds of 80 mph (130 km/h) were widespread, with occasional gusts peaking in excess of 90 mph (145 km/h). In Port Arthur, a barometer recorded a minimum pressure of 978 mbar (hPa; 28.87 inHg), establishing a new record for the lowest pressure measured by the particular weather station.[6] The same station recorded 5.87 in (149.1 mm) of rainfall.[17] Elsewhere in Port Arthur, strong winds caused significant damage to local oil refineries, with slight to moderate damage to other homes and businesses.[2] Six people were injured in the city.[11] Property damage in Jefferson County, containing Port Arthur and nearby suburbs, was estimated at $1 million.[2] The city's communication and power service was cut during the storm.[18] A weather station near Sabine Pass recorded a similarly low pressure of 973 mbar (hPa; 28.74 inHg). In Sabine Pass, strong winds unroofed houses, uprooted trees, and destroyed billboards. At the nearby Ged Oil Field, four wooden oil derricks were blown down.[17] In Beaumont, three people were injured due to flying window and structural debris.[19] Further inland, the hurricane produced considerable rainfall, though relatively less than in Louisiana. Six weather stations in the state set new 24–hour precipitation records for August. A measurement of 6.99 in (177.4 mm) on August 8 in Kirbyville was the highest of these records.[17] However, maximum rainfall in the state was estimated to be in excess of 10 in (255 mm).[15] The rice crop was particularly damaged by the rainfall. In Jefferson County, crop damage was estimated between $450,000–$500,000.[2] In Texas, the hurricane caused $1.75 million in damages and resulted in one fatality.[17]

See also Edit

Notes Edit

  1. ^ All damage totals are in 1940 United States dollars unless otherwise noted.

References Edit

  1. ^ a b c d e f Gallene, Jean H. (August 1940). "Tropical Disturbances of August 1940". Monthly Weather Review. American Meteorological Society. 68 (8): 217–218. Bibcode:1940MWRv...68..217G. doi:10.1175/1520-0493(1940)068<0217:TDOA>2.0.CO;2.
  2. ^ a b c d e f g h i j Landsea, Chris; Atlantic Oceanic Meteorological Laboratory; et al. (December 2012). "Documentation of Atlantic Tropical Cyclones Changes in HURDAT". United States National Oceanic and Atmospheric Administration. Retrieved April 11, 2013.
  3. ^ a b c d "Atlantic hurricane best track (HURDAT version 2)" (Database). United States National Hurricane Center. April 5, 2023. Retrieved September 20, 2023.   This article incorporates text from this source, which is in the public domain.
  4. ^ "Chart III. Tracks of Centers of Cyclones, August 1940. (Inset) Change in Mean Pressure from Preceding Month" (PDF). Monthly Weather Review. American Meteorological Society. 68 (8): c3. August 1940. Bibcode:1940MWRv...68X...3.. doi:10.1175/1520-0493(1940)068<0096:CITOCO>2.0.CO;2. Retrieved April 20, 2013.
  5. ^ a b c d "Gulf Coast Warned of Hurricane". The Telegraph-Herald. New Orleans, Louisiana. Associated Press. August 7, 1940. p. 1. Retrieved April 22, 2013.
  6. ^ a b c "Gale Blows 90 Miles Per Hour". San Jose News. Port Arthur, Texas. United Press. August 7, 1940. p. 1. Retrieved April 22, 2013.
  7. ^ "Tropical Storm Moves Inland". Spokane Daily Chronicle. New Orleans, Louisiana. Associated Press. April 6, 1940. p. 1. Retrieved April 22, 2013.
  8. ^ a b c "Port Arthur Citizens Flee Coming Storm". The Tuscaloosa News. Port Arthur, Texas. Associated Press. August 7, 1940. p. 1. Retrieved April 23, 2013.
  9. ^ a b c "Gulf Storm Nearing Coastline of Texas". The Evening Independent. New Orleans, Louisiana. Associated Press. August 7, 1940. pp. 1–2. Retrieved April 23, 2013.
  10. ^ a b c "Refugees Scud Before Storms". The Spokesman-Review. New Orleans, Louisiana. Associated Press. August 6, 1940. p. 12. Retrieved April 23, 2013.
  11. ^ a b "Storm Ends Over Texas". Reading Eagle. Port Arthur, Texas. Associated Press. August 8, 1940. p. 4. Retrieved April 23, 2013.
  12. ^ a b c d e f g Roth, David M; Hydrometeorological Prediction Center. Louisiana Hurricane History (PDF). United States National Oceanic and Atmospheric Administration's National Weather Service. Retrieved April 23, 2013.
  13. ^ "Hurricanes in Louisiana History". thecajuns.com. March 25, 2013. Retrieved April 23, 2013.
  14. ^ "Hurricane in South". The Leader-Post. Port Arthur, Texas. August 8, 1940. p. 2. Retrieved April 23, 2013.
  15. ^ a b Schoner, R.W.; Molansky, S. "Rainfall Associated With Hurricanes (And Other Tropical Disturbances)" (PDF). United States Weather Bureau's National Hurricane Research Project. pp. 7–8. Retrieved April 22, 2013.
  16. ^ Williams, Jim. "Cameron,Louisiana's history with tropical systems". Hurricane City. Retrieved April 23, 2013.
  17. ^ a b c d Roth, David M; Hydrometeorological Prediction Center. Texas Hurricane History (PDF). United States National Oceanic and Atmospheric Administration's National Weather Service. Retrieved April 22, 2013.
  18. ^ "Texas Ripped By Hurricane". Lodi News-Sentinel. Port Arthur, Texas. Associated Press. August 7, 1940. p. 1. Retrieved April 23, 2013.
  19. ^ "3 Killed, Heavy Property Loss In Hurricane On The Gulf Coast". Lewiston Morning Tribune. Port Arthur, Texas. Associated Press. August 7, 1940. pp. 1, 8. Retrieved April 22, 2013.

1940, louisiana, hurricane, caused, record, flooding, across, much, southern, united, states, august, 1940, second, tropical, cyclone, hurricane, annual, hurricane, season, formed, from, frontal, west, coast, florida, august, initially, weak, disturbance, move. The 1940 Louisiana hurricane caused record flooding across much of the Southern United States in August 1940 The second tropical cyclone and hurricane of the annual hurricane season it formed from a frontal low off the west coast of Florida on August 3 Initially a weak disturbance it moved generally westward slowly gaining in intensity Early on August 4 the depression attained tropical storm intensity Ships in the vicinity of the storm reported a much stronger tropical cyclone than initially suggested After reaching hurricane strength on August 5 south of the Mississippi River Delta the storm strengthened further into a Category 2 hurricane with maximum sustained winds of 100 mph and a minimum barometric pressure of 972 mbar hPa 28 71 inHg at 0600 UTC on August 7 The hurricane moved ashore near Sabine Pass Texas later that day at peak strength Once inland the storm executed a sharp curve to the north and quickly weakened degenerating into a tropical storm on August 8 before dissipating over Arkansas on August 10 1940 Louisiana hurricane Surface weather analysis of the storm on August 7 at peak intensityMeteorological historyFormedAugust 3 1940 1940 08 03 DissipatedAugust 10 1940 1940 08 11 Category 2 hurricane1 minute sustained SSHWS NWS Highest winds100 mph 155 km h Lowest pressure972 mbar hPa 28 70 inHgOverall effectsFatalities7Damage 10 8 million 1940 USD Areas affectedSouthern United States Texas Louisiana IBTrACSPart of the 1940 Atlantic hurricane seasonReports of a potentially destructive hurricane near the United States Gulf Coast forced thousands of residents in low lying areas to evacuate prior to the storm moving inland Offshore the hurricane generated rough seas and a strong storm surge peaking at 6 4 ft 1 95 m on the western edge of Lake Pontchartrain The anomalously high tides flooded many of Louisiana s outlying islands inundating resorts Strong winds caused moderate infrastructural damage primarily in Texas though its impact was mainly to communication networks along the US Gulf Coast which were disrupted by the winds However much of the property and crop damage wrought by the hurricane was due to the torrential rainfall it produced in low lying areas setting off record floods Rainfall peaked at 37 5 in 953 mm in Miller Island off Louisiana making it the wettest tropical cyclone in state history Nineteen official weather stations in both Texas and Louisiana recorded record level 24 hour rainfall totals for the month of August as a result of the slow moving hurricane Property livestock and crops especially cotton corn and pecan crops were heavily damaged Entire ecosystems were also altered by the rainfall Overall the storm caused 10 75 million in damages and seven fatalities nb 1 Contents 1 Meteorological history 2 Preparations and impact 3 See also 4 Notes 5 ReferencesMeteorological history Edit nbsp Map plotting the storm s track and intensity according to the Saffir Simpson scaleMap keySaffir 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 nbsp Tropical cyclone nbsp Subtropical cyclone nbsp Extratropical cyclone remnant low tropical disturbance or monsoon depressionIn early August an extratropical trough moved off the coast of South Carolina and Georgia with a stationary front extending from it 1 2 A weak low pressure area began to develop at the southern end of the front just offshore of Jacksonville Florida 1 Initially the storm had an open center of circulation and remained a frontal low as it moved southwestward across Florida and thus was not considered a fully tropical system at the time Upon entering the Gulf of Mexico however observations indicated that the disturbance developed a closed center of circulation 2 As a result the storm was analyzed to have developed into a tropical depression off the western coast of Florida at 1200 UTC on August 3 3 At the time weather reports revealed a definite cyclonic rotation though the depression had a shallow minimum barometric pressure of 1012 5 mbar hPa 29 90 inHg 1 Moving west southwest the depression steadily intensified and attained tropical storm intensity at 0000 UTC on August 4 3 Late that evening the tropical storm executed a slight northward curve 1 Strengthening continued into the following day and ships in the storm s vicinity began to report a much stronger storm than was previously suggested A ship reported the first gale force winds associated with the storm at 2100 UTC on August 4 2 The S S Connecticut observed force 11 winds the strongest wind measurement associated with the storm as recorded by vessel 1 A minimum pressure of 995 mbar hPa 29 39 inHg was analyzed for the system at 0600 UTC on August 5 based on an observation from a nearby ship 2 At 1800 UTC on August 5 the storm strengthened to hurricane strength the first tropical cyclone of the season to do so At the time the hurricane was moving very slowly westward allowing it to strengthen despite its close proximity to land The hurricane reached Category 2 intensity by 0600 UTC on August 7 3 The storm made landfall at peak intensity at around 2100 UTC later that day near Sabine Pass Texas At the time the hurricane had maximum sustained winds of 100 mph 160 km h with the storm s maximum winds extending out 10 mi 15 km from its center 2 A weather station in Sabine Pass recorded a barometric pressure of 972 mbar hPa 28 71 inHg which was analyzed to have been the lowest pressure measured in association with the storm 2 3 After moving inland the storm immediately curved northward and began to gradually weaken 1 At 0600 UTC on August 8 the cyclone weakened to tropical storm strength while situated over East Texas and later degenerated to a tropical depression by 1200 UTC the following day The depression persisted into Arkansas 4 where it transitioned into a trough of low pressure at 1800 UTC on August 10 after its center of circulation lacked the well defined closed circulation characteristic of tropical cyclones 2 Preparations and impact Edit nbsp Rainfall totals in the United StatesUpon reaching hurricane strength off the United States Gulf Coast hurricane warnings were issued for coastal regions from Lake Charles Louisiana to Sabine Pass Texas on August 7 5 Storm warnings were placed for areas east of Lake Charles to Grand Isle Louisiana and areas west of Sabine Pass to Velasco Texas 6 Offshore vessels were also warned of the storm in areas between Bay St Louis Mississippi and Galveston Texas 7 At the time the hurricane was forecast to make landfall slightly east of Port Arthur Texas 5 In Texas these warnings were delivered to residents via factory whistles Evacuation procedures also began as a result of the approaching storm The Spindletop near Beaumont Texas and other nearby oil fields were evacuated Coastal cities near Port Arthur Texas were also evacuated by state highway police 6 8 Evacuees took shelter in refitted schools nearby 8 In the New Orleans Louisiana area several thousand residents were evacuated in advance of the storm 9 On Delacroix Island Louisiana 1 000 residents evacuated 10 Rail and airline operations were halted as a precautionary measure but were later resumed after the storm passed 8 All storm warnings were ceased by midnight on August 8 11 Even before making landfall the hurricane caused extensive damage in Louisiana due in part to the hurricane s slow speed and close proximity to the state coast Winds as high as 60 mph 100 km h brushed the coastline causing extensive damage Storm surge pushed coastal waters to near record heights inundating low lying areas Near Morgan City Louisiana 19 people went missing after going on a fishing trip 5 they were later found marooned at Atchafalaya Basin 9 The schooner J W Clise was abandoned during the storm 135 mi 215 km south of the Mississippi River Delta though its crew was also later rescued 12 Storm surge peaked at 6 4 ft 1 95 m above average in western portions of Lake Pontchartrain A bridge crossing Thunder Bayou which extended west of the lake was washed out by the waves Similarly a station at Calcasieu Pass reported a storm surge 4 8 ft 1 46 m high 12 Conservation officials feared the disturbance would disrupt the seafood and muskrat production 5 After the storm it was estimated 75 000 muskrats were killed by the storm s effects 13 Offshore Grand Isle was inundated by the strong waves 10 Around Houma sugar cane crops were damaged 14 The hurricane was the strongest to impact Cameron since the tenth hurricane of the 1886 Atlantic hurricane season 12 strong gusts peaked at 70 mph 115 km h disrupting communication lines thus isolating the city from other locations in the state The high tides inundated town streets under 2 ft 0 6 m 9 Other areas extending from western Louisiana to Mobile Alabama reported communication disruptions In New Orleans strong winds uprooted signboards and blew debris across the city streets 10 Several houses in Shell Beach and Delacroix Island were leveled by strong winds 12 Due to the storm s slow movement just offshore the Louisiana coast the hurricane became the wettest tropical cyclone in state history with numerous locations reporting record rainfall across the state Of the state s ten highest official rainfall measurements associated with tropical cyclones the two highest were measurements taken during the hurricane 12 Precipitation peaked at 37 5 in 953 mm on Miller Island For any given 20 000 mi2 50 000 km h2 area of Louisiana the maximum rainfall averaged 12 1 in 307 3 mm 15 Thirteen official weather stations in the state reported monthly 24 hour rainfall total records The highest of these was in Crowley where 19 76 in 501 9 mm of precipitation fell on August 9 the station would record 33 71 in 856 2 mm of rain over the course of the storm The torrential rainfall submerged the city under 2 ft 0 6 m of floodwater 12 In Cameron the storm dropped 21 in 533 mm of rain was reported 16 In St Landry Parish bayous flowed over their banks causing refugees to evacuate to Opelousas In the Acadiana region of southern Louisiana the resulting floods were considered worse than the floods that resulted from the Sauve s Crevasse in 1849 There whooping crane populations were severely impacted by the rainfall and only one was known to be alive by 1947 The floods inundated roughly 2 000 000 acres 800 000 hectares of land in Louisiana Much of the lowland areas remained underwater until October 1940 As a result cotton and corn crops experienced significant losses as well as pecans Livestock also saw large losses Impassable areas caused by rising floodwaters prevented firefighters from extinguishing a fire which burned down much of the Shell Oil Company s offices and supply warehouses in the town of Iowa Across the state the hurricane caused 9 million in damages though only six fatalities resulted relatively less than most storms of similar scale The low death count was attributed to large evacuation procedures which underwent prior to the storm as well as guidance provided from the newly opened Weather Bureau east of Lake Charles 12 In East Texas where the hurricane made landfall late on August 7 strong winds were felt across the region Sustained winds of 80 mph 130 km h were widespread with occasional gusts peaking in excess of 90 mph 145 km h In Port Arthur a barometer recorded a minimum pressure of 978 mbar hPa 28 87 inHg establishing a new record for the lowest pressure measured by the particular weather station 6 The same station recorded 5 87 in 149 1 mm of rainfall 17 Elsewhere in Port Arthur strong winds caused significant damage to local oil refineries with slight to moderate damage to other homes and businesses 2 Six people were injured in the city 11 Property damage in Jefferson County containing Port Arthur and nearby suburbs was estimated at 1 million 2 The city s communication and power service was cut during the storm 18 A weather station near Sabine Pass recorded a similarly low pressure of 973 mbar hPa 28 74 inHg In Sabine Pass strong winds unroofed houses uprooted trees and destroyed billboards At the nearby Ged Oil Field four wooden oil derricks were blown down 17 In Beaumont three people were injured due to flying window and structural debris 19 Further inland the hurricane produced considerable rainfall though relatively less than in Louisiana Six weather stations in the state set new 24 hour precipitation records for August A measurement of 6 99 in 177 4 mm on August 8 in Kirbyville was the highest of these records 17 However maximum rainfall in the state was estimated to be in excess of 10 in 255 mm 15 The rice crop was particularly damaged by the rainfall In Jefferson County crop damage was estimated between 450 000 500 000 2 In Texas the hurricane caused 1 75 million in damages and resulted in one fatality 17 See also Edit nbsp Tropical cyclones portalList of Texas hurricanes 1900 49 1933 Texas tropical storm Hurricane Six 1943 Hurricane Barry 2019 Notes Edit All damage totals are in 1940 United States dollars unless otherwise noted References Edit a b c d e f Gallene Jean H August 1940 Tropical Disturbances of August 1940 Monthly Weather Review American Meteorological Society 68 8 217 218 Bibcode 1940MWRv 68 217G doi 10 1175 1520 0493 1940 068 lt 0217 TDOA gt 2 0 CO 2 a b c d e f g h i j Landsea Chris Atlantic Oceanic Meteorological Laboratory et al December 2012 Documentation of Atlantic Tropical Cyclones Changes in HURDAT United States National Oceanic and Atmospheric Administration Retrieved April 11 2013 a b c d Atlantic hurricane best track HURDAT version 2 Database United States National Hurricane Center April 5 2023 Retrieved September 20 2023 nbsp This article incorporates text from this source which is in the public domain Chart III Tracks of Centers of Cyclones August 1940 Inset Change in Mean Pressure from Preceding Month PDF Monthly Weather Review American Meteorological Society 68 8 c3 August 1940 Bibcode 1940MWRv 68X 3 doi 10 1175 1520 0493 1940 068 lt 0096 CITOCO gt 2 0 CO 2 Retrieved April 20 2013 a b c d Gulf Coast Warned of Hurricane The Telegraph Herald New Orleans Louisiana Associated Press August 7 1940 p 1 Retrieved April 22 2013 a b c Gale Blows 90 Miles Per Hour San Jose News Port Arthur Texas United Press August 7 1940 p 1 Retrieved April 22 2013 Tropical Storm Moves Inland Spokane Daily Chronicle New Orleans Louisiana Associated Press April 6 1940 p 1 Retrieved April 22 2013 a b c Port Arthur Citizens Flee Coming Storm The Tuscaloosa News Port Arthur Texas Associated Press August 7 1940 p 1 Retrieved April 23 2013 a b c Gulf Storm Nearing Coastline of Texas The Evening Independent New Orleans Louisiana Associated Press August 7 1940 pp 1 2 Retrieved April 23 2013 a b c Refugees Scud Before Storms The Spokesman Review New Orleans Louisiana Associated Press August 6 1940 p 12 Retrieved April 23 2013 a b Storm Ends Over Texas Reading Eagle Port Arthur Texas Associated Press August 8 1940 p 4 Retrieved April 23 2013 a b c d e f g Roth David M Hydrometeorological Prediction Center Louisiana Hurricane History PDF United States National Oceanic and Atmospheric Administration s National Weather Service Retrieved April 23 2013 Hurricanes in Louisiana History thecajuns com March 25 2013 Retrieved April 23 2013 Hurricane in South The Leader Post Port Arthur Texas August 8 1940 p 2 Retrieved April 23 2013 a b Schoner R W Molansky S Rainfall Associated With Hurricanes And Other Tropical Disturbances PDF United States Weather Bureau s National Hurricane Research Project pp 7 8 Retrieved April 22 2013 Williams Jim Cameron Louisiana s history with tropical systems Hurricane City Retrieved April 23 2013 a b c d Roth David M Hydrometeorological Prediction Center Texas Hurricane History PDF United States National Oceanic and Atmospheric Administration s National Weather Service Retrieved April 22 2013 Texas Ripped By Hurricane Lodi News Sentinel Port Arthur Texas Associated Press August 7 1940 p 1 Retrieved April 23 2013 3 Killed Heavy Property Loss In Hurricane On The Gulf Coast Lewiston Morning Tribune Port Arthur Texas Associated Press August 7 1940 pp 1 8 Retrieved April 22 2013 Retrieved from https en wikipedia org w index php title 1940 Louisiana hurricane amp oldid 1170503912, wikipedia, wiki, book, books, library,

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