1957 Atlantic hurricane season

The 1957 Atlantic hurricane season featured one of the longest-travelling tropical cyclones in the Atlantic basin, Hurricane Carrie. Nevertheless, the season was generally inactive, with eight tropical storms – two of which went unnamed – and three hurricanes, two of which intensified further to attain major hurricane intensity.<ref group="nb">A major hurricane is a storm that ranks as Category 3 or higher on the Saffir–Simpson hurricane scale.<ref name=BASIC>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref></ref> The season officially began on June 15 and ended on November 15, though the year's first tropical cyclone developed prior to the start of the season on June 8. The final storm dissipated on October 27, well before the official end of the season. The strongest hurricane of the year was Carrie, which reached the equivalent of a Category 4 hurricane on the Saffir–Simpson hurricane scale on two separate occasions in the open Atlantic; Carrie later caused the sinking of the German ship Pamir southwest of the Azores, resulting in 80 deaths.

In total, the season resulted in at least 513 fatalities and $152.5 million in damages.<ref group="nb">All damage totals are in 1957 United States dollars unless otherwise noted.</ref> Hurricane Audrey was the season's most destructive and deadly storm, causing 416 deaths and about $150 million in damages. Audrey made landfall just east of Sabine Pass, Texas, in the U.S. state of Louisiana as a strong Category 3 hurricane in late June. Three other tropical storms in the year made landfalls along the Gulf Coast of the United States, bringing heavy rains that resulted in widespread flooding across much of the Southeastern United States. The highest rainfall total measured associated with a tropical cyclone was Template:Convert in Quarantine, Louisiana, during Tropical Storm Esther. However, an unofficial reading of Template:Convert was measured in an unknown location in the Florida Panhandle during Tropical Storm One.<ref name=Rainfall /><ref name=HPC1 /> The year's other tropical systems curved out to sea without causing much impact. After the season, the name Audrey was retired.

Season summary

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The Atlantic hurricane season officially began on June 15, 1957.<ref name="season dates">Template:Cite news</ref> It was a below-average season in which eight tropical cyclones formed, of which three became hurricanes.<ref name=MWR /> Of these hurricanes, two became major hurricanes.Template:Atlantic hurricane best track In an average season, ten tropical cyclones form, of which five become hurricanes.<ref name=MWR /> Five of the season's eight tropical cyclones developed in the Gulf of Mexico, the most since the 1936 season, in which six formed in the gulf.<ref name="WC September" /> The first tropical storm of the season formed on June 8, a week before the official start of the hurricane season. However, the first named storm, Audrey, formed afterwards, on June 25; these two storms were the only to form in June during the season. July featured no Atlantic tropical cyclones. Tropical Storm Bertha was the only system to form during August, developing in the Gulf of Mexico.Template:Atlantic hurricane best track Despite warm sea surface temperatures (SSTs) in the tropical Atlantic, no storms formed during the month, below the climatological average of one.<ref name="WC August" /> The low monthly activity was in part due to an unfavorable wind pattern which prevailed across the Atlantic for much of the month. In September, however, conditions for tropical cyclogenesis were more favorable, with concomitant cyclonic activity. Four storms formed, of which two attained hurricane strength, higher than the mean activity of the last 70 Septembers.<ref name="WC September">Template:Cite journal</ref> By contrast, only one tropical storm formed in October, below the average of two in the month.<ref name="WC October">Template:Cite journal</ref> This tropical storm dissipated on October 27,Template:Atlantic hurricane best track 16 days before the official end of the hurricane season on November 15.<ref name="season dates"/>

Five tropical cyclones made landfall during the hurricane season, including one hurricane. All of these storms made landfall on the Gulf Coast of the United States. Property damage that resulted from cyclone-related impacts totaled to $152 million in the United States, with most caused by Hurricane Audrey, which made landfall near the border between Texas and Louisiana.<ref name=MWR /> 513 deaths were also caused by tropical storms during the season,<ref name=MWR /><ref name="World Briefs" /><ref name="Climatological Data" /> with 416 deaths attributable to Hurricane Audrey.<ref name=Deadliest>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

The season's activity was reflective with an accumulated cyclone energy (ACE) rating of 84, which is categorized as being "near normal."<ref name=ACE>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> However, this was under the 1950–2000 average of 96.1.<ref name=CSU2009>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> ACE is, broadly speaking, a measure of the power of hurricanes multiplied by the length of time it existed, so storms that last a long time, as well as particularly strong hurricanes, have high ACEs. It is only calculated for full advisories on tropical cyclones with winds exceeding 39 mph (63 km/h), which is tropical storm strength.<ref name=Glossary>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Systems

Unnamed June tropical storm

An area of disturbed weather accompanied by low barometric pressure was first identified near the Yucatán Peninsula on June 7. Reports from the following day in the region reported pressures that were indicative of a developing tropical cyclone,<ref name="Climatological Data"> Template:Cite journal</ref> and at 06:00 UTC, the disturbance attained tropical storm strength, the first of the season.Template:Atlantic hurricane best track Though hurricane reconnaissance flights could not locate a well-defined center, ship observations showed that the tropical storm was moving quickly to the northeast.<ref name="Climatological Data" /> Due to its fast forward motion, the storm gained little in organization and made landfall near Port Leon, Florida, on June 9 with winds of 50 mph (85 km/h).Template:Atlantic hurricane best track<ref name=MWR>Template:Cite journal</ref> However, the system gradually strengthened as it crossed the Florida peninsula, reentering the North Atlantic later that day.Template:Atlantic hurricane best track<ref name=MWR /> On June 10, the storm reached peak winds of 65 mph (100 km/h) prior to becoming an extratropical storm. The post-tropical cyclone then strengthened and moved erratically in open seas before entirely dissipating on June 15.Template:Atlantic hurricane best track

Despite the tropical storm's fast passage over land, heavy rainfall was reported,<ref name="Climatological Data" /> officially peaking at Template:Convert in Live Oak, Florida. However, unofficial reports of at least Template:Convert of rain were collected.<ref name=HPC1>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> In Perry, Florida, 100–200 families were evacuated due to the floodwater. Field crops, including tobacco and watermelon, were damaged, with flood damage estimated at $30,000. The storm also spawned ten tornadoes, with nine in northeastern Florida and one on Georgia's Jekyll Island. All of these tornadoes were relatively weak and caused minor damage, totaling to $12,000. At the coast, the tropical storm's strong winds generated waves Template:Convert high, which caused moderate damage.<ref name=MWR /> Though located south of where the storm made landfall, buildings and roads along the Tampa Bay Area waterfront were flooded by the waves.<ref name="Hard Storm">Template:Cite news</ref> The cabin cruiser Kinnebar capsized in the Gulf of Mexico due to the waves,<ref name=7M>Template:Cite news</ref> and five of the seven crew on board drowned; these were the only deaths associated with the system. Coastal damages due to storm surge amounted to $10,000, and overall the storm caused $52,000 in damages across the southeastern United States.<ref name=MWR />

Hurricane Audrey

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An ill-defined tropical wave was first identified in the Caribbean Sea on June 20, and moved westward into the Bay of Campeche. The disturbance slowly strengthened as it developed a low pressure system.<ref name=Audrey>Template:Cite journal</ref> A nearby trough aided the intensification of the system,<ref name="WC June">Template:Cite journal</ref> and it developed into a tropical depression on June 24, while remaining generally stationary in the Bay of Campeche.Template:Atlantic hurricane best track Situated in an area of favorable upper-air divergence and warm waters,<ref name=Audrey /> the depression intensified into Tropical Storm Audrey about six hours later.Template:Atlantic hurricane best track Audrey began to accelerate northward due to troughing in the upper-levels in the atmosphere.<ref name=Audrey /> The storm became a hurricane late on September 25. Audrey intensified quicker while in the northwestern Gulf of Mexico, reaching peak intensity as a Category 3 hurricane with winds of Template:Convert on June 27. Audrey made landfall at this intensity in extreme southwestern Louisiana very shortly thereafter. The hurricane quickly weakened as it moved inland, becoming an extratropical cyclone by June 28. The extratropical remnants soon dissipated over the Northeastern United States.Template:Atlantic hurricane best track

Hurricane Audrey caused widespread impacts across a wide swath of the United States and Canada.<ref name=Audrey /> The storm's worst effects were felt in Louisiana, where the storm caused $120 million in damages. The highest storm surge measured with the hurricane was Template:Convert, reported west of Cameron, Louisiana. The strong surge inundated much of the coast, killing much of the local wildlife and causing widespread property damage.<ref name=LAHurricane>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Heavy rainfall also caused flooding, peaking at Template:Convert west of Basile, Louisiana. Rainfall was concentrated particularly in the Atchafalaya Basin.<ref name="HPC Audrey">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> In Texas, effects of the storm were much less severe, but the storm still caused $8 million in damages, primarily as a result of strong winds.<ref name=TXHurricane>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Further inland, the weakening hurricane spawned tornadoes and caused additional flooding in conjunction with a frontal boundary.<ref name="HPC Audrey" /> The effects of Audrey were felt as far north as Canada, where 15 people died due to the strong winds and heavy rain.<ref name="EC Audrey">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> In total, the storm caused $152 million in damages and at least 416 deaths.<ref name=MWR />

Tropical Storm Bertha

A weak extratropical low entered the Gulf of Mexico on August 6 and drifted slowly westward.<ref name=MWR /> The system slowly organized, developing into a tropical depression on August 8 about Template:Convert southeast of the Mississippi River Delta. Moving westward, the depression intensified into Tropical Storm Bertha later on August 8. Bertha then turned northwestward and quickly organized;Template:Atlantic hurricane best track the system attained its peak intensity with Template:Convert and an estimated minimum pressure of 998 mbar (hPa; 29.47 inHg) on August 9.<ref name="WC August">Template:Cite journal</ref> Early on August 10, Bertha came ashore near Cameron, Louisiana. at the same intensity.Template:Atlantic hurricane best track After landfall, the storm moved northward due to a strong high-pressure system and weakened over land,<ref name="WC August" /> before degenerating into a remnant low at 0600 UTC on August 11 over Oklahoma.Template:Atlantic hurricane best track The storm's remnants later moved across the U.S. Interior Highlands before dissipating.<ref name="Climatological Data" />

In the Gulf of Mexico, 1,350 workers on offshore oil drilling platforms were evacuated in preparation for the storm.<ref name="Climatological Data" /> The oil drilling tender Murmanill No. 1 sunk due to the strong waves,<ref name="Oil">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> though the two people on board at the time were evacuated by helicopter. At the coast, the maximum storm surge height measured was Template:Convert at the Schooner Bayou Control Structure.<ref name="Climatological Data" /> Bertha dropped heavy rainfall primarily as a remnant low across much of The Ozarks. Rainfall peaked at Template:Convert near Damascus, Arkansas, which set a 24-hour rainfall record for the city and made August 1957 the wettest month on record.<ref name="Bertha Record">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref name="HPC Bertha">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Across Arkansas, the heavy rains triggered flash floods after numerous rivers exceeded flood stage. The flash floods caused property damage in cities adjacent to rivers. Though damage estimates were difficult to accurately obtain, four Arkansas counties reported combined losses of $925,000,<ref name="Climatological Data" /> and two deaths were reported.<ref name=MWR />

Hurricane Carrie

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An easterly tropical wave spawned a tropical depression near the Cabo Verde Islands on September 2.<ref name=MWR /> The depression moved generally west-northwestward and became Tropical Storm Carrie on September 3, before becoming a hurricane on September 5. Carrie intensified further, before reaching peak intensity on early September 8 as a Category 4 hurricane with maximum sustained winds of Template:Convert in the open Atlantic Ocean. The hurricane curved northward and fluctuated in intensity, bottoming out at Category 1 intensity early on September 10. After turning northward on September 11, the storm began re-strengthening, reaching a secondary peak as a Category 3 hurricane on September 13. However, the storm soon began slowly weakening, falling to Category 2 intensity shortly before curving west-northwestward on September 14. Although Carrie threatened Bermuda, the storm passed northeast of the island and then turned in a general eastward direction by September 17. Carrie accelerated northeastward by September 22 and passed through the Azores over of close to Terceira Island as a Category 1 hurricane. The storm transitioned into an extratropical cyclone on September 23,Template:Atlantic hurricane best track prior to affecting areas of the British Isles.<ref name=MWR /> The extratropical system dissipated near the southwestern tip of England on September 25.Template:Atlantic hurricane best track

Due to its distance away from any major land masses, Carrie caused relatively minor damage along its path. On September 16, the hurricane passed well north of Bermuda, causing minimal damage despite its intensity at the time,<ref name=New>Template:Cite news</ref> though hurricane reconnaissance flights in the area were postponed due to damage sustained by one of the aircraft.<ref name=Peril>Template:Cite news</ref> As it was transitioning into an extratropical cyclone southwest of the Azores, the German ship Pamir encountered the storm and capsized on September 21, resulting in the deaths of 80 crew members on board.<ref name=MWR /> On September 23, Carrie completed its extratropical transition. As an extratropical storm, Carrie brought strong storm surge and heavy rain to the British Isles, which claimed three lives.<ref name="World Briefs">Template:Cite news</ref> The hurricane's long duration and path in open water also helped it attain a number of Atlantic hurricane records.<ref name="Climatological Data 2">Template:Cite journal</ref>

Tropical Storm Debbie

On September 5, a weak easterly wave moved into the Gulf of Mexico from the Caribbean Sea due to the influence of an upper-level trough.<ref name=MWR /> The wave organized and spawned a weak area of circulation which developed into a tropical storm by 0600 UTC on September 7.<ref name="Climatological Data" />Template:Atlantic hurricane best track Moving steadily towards the northeast at roughly Template:Convert, Debbie only marginally strengthened due to the presence of cooler air entrainment. Late on September 8, Debbie made landfall near Fort Walton Beach, Florida as a minimal tropical storm with winds of Template:Convert.<ref name=MWR />Template:Atlantic hurricane best track A minimum barometric pressure of 1005 mbar (hPa; 29.68 inHg) was recorded in Pensacola, Florida.<ref name="Climatological Data" /> The tropical storm weakened as it moved over land, degenerating to a tropical depression on September 9.Template:Atlantic hurricane best track The system became increasingly diffuse, and later merged with strong weather systems by 0600 UTC later that day.<ref name="Climatological Data" />Template:Atlantic hurricane best track

Offshore, the tropical storm generated high tides Template:Convert above average in Apalachee Bay, located about Template:Convert east of where Debbie made landfall. The strong surf caused some localized flooding. In St. Marks, Florida, a station recorded maximum sustained winds of Template:Convert, the highest measured in association with the storm. However, a station in Tampa, Florida recorded a peak wind gust of Template:Convert in a squall.<ref name=MWR /> Heavy rainfall caused widespread flooding, though rainfall was mostly beneficial to crops. Rainfall peaked at Template:Convert in Wewahitchka, Florida,<ref name="Climatological Data" /> while precipitation was reported as far north as Pennsylvania.<ref name="HPC Debbie">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The tropical storm only caused minor damage,<ref name=SlightDebbie>Template:Cite news</ref> but was indirectly responsible for four deaths.<ref name=MWR />

Tropical Storm Esther

On September 12, a mid-level circulation area formed over Nicaragua and slowly drifted northeastward into the Gulf of Mexico.<ref name="Climatological Data" /> As it entered the Gulf, the system developed thunderstorm activity and an area of low pressure, and as a result the Weather Bureau began initiating advisories on a newly formed tropical depression on September 16.<ref name=MWR />Template:Atlantic hurricane best track The depression quickly intensified and attained tropical storm strength. Esther continued to strengthened, reaching a minimum pressure of 1000 mbar (hPa; 29.53 inHg) early on September 18,Template:Atlantic hurricane best track as reported by a hurricane reconnaissance flight.<ref name=MWR /> Shortly thereafter, the large tropical storm peaked with sustained winds of Template:Convert as it made landfall to the southwest of Dulac, Louisiana.<ref name=MWR />Template:Atlantic hurricane best track Esther weakened over land and later dissipated over the Mississippi Valley by 1200 UTC on September 19.<ref name=MWR />Template:Atlantic hurricane best track

Like Tropical Storm Debbie, which had made landfall just a week prior in the same area, Esther's wind impacts were minimal.<ref name=MWR /> The strongest gust measured associated with the storm was Template:Convert, as recorded at Pensacola International Airport. Other locations reported similar gusts and strong winds in squalls. Heavy rains persisted in the region well after Esther moved inland, resulting in high rainfall amounts. Rainfall peaked at Template:Convert in Quarantine, Louisiana, near the mouth of the Mississippi River. The heavy rains breached several levees, resulting in severe flooding, particularly in Buras, Louisiana. Although rainfall was beneficial in many places due to an existing drought, cotton, pecan, and peanut crops were damaged by the floods. While crop damage amounted to $1 million,<ref name="Climatological Data" /> property damage amounted to $1.5 million.<ref name=MWR /> Esther also caused three indirect deaths, all of which were in Louisiana.<ref name="Climatological Data" />

Hurricane Frieda

On September 20, a low pressure area developed within the same frontal boundary that had curved Hurricane Carrie towards the Azores.<ref name=MWR /> Rapidly developing, the system was classified as a tropical depression at 1200 UTC later that day, southwest of Bermuda.Template:Atlantic hurricane best track Initially, the depression was ill-defined and was slowly moving to the southwest.<ref name="Climatological Data" />Template:Atlantic hurricane best track The following day, the attached cold front dissipated, allowing for the system to intensify. The system was subsequently upgraded a tropical storm by September 22,Template:Atlantic hurricane best track following a reconnaissance flight into the system which reported a minimum pressure of 1001 mbar (hPa; 29.56 inHg). At the time, however, Frieda was a small system with minimal shower activity.<ref name=MWR /> Gradually strengthening, Frieda reached an initial peak intensity with winds of Template:Convert later that day.Template:Atlantic hurricane best track Following the split of an upper-level ridge to the north, Frieda recurved towards the northeast the next day. As it sped to the northeast, a westerly shortwave progressed eastward, enhancing environmental conditions. As a result, the tropical storm began to quickly strengthen. By 1200 UTC on September 25, Frieda attained hurricane strength, and reached peak intensity with winds of Template:Convert and a minimum pressure of 992 mbar (hPa; 29.30 inHg), as reported by the Canadian merchant ship Irvingbrook. However, a cold front associated with the shortwave encountered the hurricane, which caused it to transition into an extratropical cyclone on September 26. Frieda's extratropical remnants later passed over Newfoundland.<ref name=MWR /> Though Frieda remained far from any land masses, a peak rainfall amount of Template:Convert was measured in Bermuda.<ref name="Rainfall">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Unnamed October tropical storm

On October 22, an area of thunderstorm activity developed north of the Lesser Antilles, and barometric pressures fell throughout the region. The following day, a cut-off low developed and strengthened along the edge of a trough extending from Bermuda.<ref name=MWR /> This justified the classification of the system as a tropical depression on October 23,Template:Atlantic hurricane best track Template:Convert northeast of Puerto Rico.<ref name="Climatological Data" /> Moving towards the west, the depression attained tropical storm strength shortly after formation.Template:Atlantic hurricane best track A ship reported a minimum pressure of 999 mbar (hPa; 29.50 inHg) in the storm's vicinity.<ref name=MWR /> The large system gradually strengthened the following day, reaching its peak intensity by 1800 UTC on October 24.Template:Atlantic hurricane best track A ship reported a minimum pressure of 993 mbar (hPa; 29.33 inHg) early the next day, the lowest pressure measured in association with the tropical storm. At the same time, the tropical storm also recurved towards the northeast. Heading towards more northerly latitudes, a gradual weakening trend began, due to the presence of an extratropical system. The tropical storm was itself absorbed by the same system on October 27. This storm may not have been named operationally due to a lack of discernible tropical characteristics.<ref name=MWR />

Storm names

The following list of names was used for named storms (tropical storms and hurricanes) that formed in the North Atlantic in 1957.<ref name=Nomenclature>Template:Cite news</ref> This was a completely new set of names, thus every name used this season was used for the first (and only, in the case of Audrey) time. <ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Audrey Bertha Carrie Debbie Esther Frieda

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Retirement

Due to the extensive damage and high fatalities, the name Audrey was retired by the U.S. Weather Bureau after the 1957 season. The name will never be used to name another Atlantic hurricane.<ref name=Retiring>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

See also

• 1957 Pacific hurricane season
• 1957 Pacific typhoon season
• Australian region cyclone seasons: 1956–57 1957–58
• South Pacific cyclone seasons: 1956–57 1957–58
• South-West Indian Ocean cyclone seasons: 1956–57 1957–58