Английская Википедия:1939 California tropical storm

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Шаблон:Short description Шаблон:Good article Шаблон:Infobox weather eventШаблон:Infobox weather event/NWSШаблон:Infobox weather event/EffectsШаблон:Infobox weather event/Footer The 1939 California tropical storm, also known as the 1939 Long Beach tropical storm, and El Cordonazo (referring to the Cordonazo winds or the "Lash of St. Francis" (Шаблон:Lang-es)), was a tropical cyclone that affected Southern California in September 1939. Formerly classified a hurricane,[1] it was the first tropical cyclone to directly affect California since the 1858 San Diego hurricane,[2] and is the only tropical cyclone of tropical-storm strength (or greater) to make landfall in the U.S. state of California.[3] The storm caused heavy flooding, leaving many dead, mostly at sea.[1]

Meteorological synopsis

On September 15, a tropical depression formed off the southern coast of Central America.[4] It moved west-northwestward, passing southwest of the Revillagigedo Islands. It then turned north and then northeastward.[4] For some time, it was a hurricane, and it lost that intensity on or just before September 25.[1] The tropical storm made landfall near San Pedro, California, early on September 25,[1] with winds of severe gale strength. It dissipated later that day.[4] The strongest reported sustained wind was of Force 11 strength, which was reported by a ship, making this system a minimal hurricane. The lowest pressure was reported by the same ship, and was at 28.67 inHg (971 mb).[4]

Due to the rotation of the Earth, tropical cyclones in the Northern Hemisphere tend to move from east to west. This causes tropical cyclones to approach the West Coast of the United States infrequently. Another inhibiting factor for a California landfall is the surrounding water temperatures. Because of the water currents, the waters off the coast of California are rarely above Шаблон:Convert, which is too cold for hurricanes to sustain themselves.[5] This tropical cyclone was rare enough that only three other eastern Pacific tropical cyclones brought tropical storm-force winds to the Continental United States during the twentieth century. The Long Beach Tropical Storm was the only one to make landfall; the other three hit Mexico before moving north, but didn't make landfall in California.[2]

Preparations and impact

Файл:Digital-elevation-map-california.png
Map of California

The storm dropped heavy rain in California, with Шаблон:Convert falling in Los Angeles (Шаблон:Convert in 24 hours) and Шаблон:Convert recorded at Mount Wilson, both September records. Over three hours, one thunderstorm dropped nearly Шаблон:Convert of rain on Indio. Шаблон:Convert fell on Raywood Flat, and Шаблон:Convert on Palm Springs.[1] Шаблон:Convert fell on Pasadena, a September record at the time. At the Citrus Belt near Anaheim, at least Шаблон:Convert of rain fell. The Шаблон:Convert at Mount Wilson is one of California's highest rainfall amounts from a tropical cyclone, although at least one system has a higher point maximum.Шаблон:Tropical Cyclone Point Maxima The rains caused a flood Шаблон:Convert[6] deep in the Coachella Valley with heavy rain immediately preceding the tropical storm dropping Шаблон:Convert the day before the storm hit.[1] The Los Angeles River, which was usually low during September, became a raging torrent.[6]

With heavy rain immediately preceding the tropical storm, flooding killed 45 in Southern California.[7] At sea, 48 were killed.[1] However, the National Hurricane Center only attributes 45 deaths to this system.[8] Six people caught on beaches drowned during the storm. Most other deaths were at sea. Twenty-four died aboard a vessel called the Spray as it attempted to dock at Point Mugu. The two survivors, a man and a woman, swam ashore and then walked five miles (8 km) to Oxnard. Fifteen people from Ventura drowned aboard a fishing boat named Lur. Many other vessels were sunk, capsized, or blown ashore.[6]

Many low-lying areas were flooded. The Hamilton Bowl overflowed, flooding the Signal Hill area. Along the shore from Malibu to Huntington Beach houses were flooded. Throughout the area, thousands of people were stranded in their homes. Streets in Los Angeles proper were covered with water, flooding buildings and stalling cars. Flooding in Inglewood and Los Angeles reached a depth of Шаблон:Convert. Construction on a flood control project in the Los Angeles River's channel by the Army Corps of Engineers was stopped by the flooding. Windows throughout Long Beach were smashed by the wind. At Belmont Shore and the Peninsula,[9] waves undermined ten homes before washing them away. Debris was scattered throughout the coast. Agriculture was disrupted. Crop damage in the Coachella Valley reached 75%.[6]

Rains washed away a Шаблон:Convert section of the Southern Pacific Railroad near Indio, and a stretch of the Santa Fe main line near Needles. Waters backing up from a storm drain under construction in the San Gabriel Valley blocked California State Route 60. The pier at Point Mugu was washed away. In Pasadena, 5000 people were left without electricity and 2000 telephones lost service. Communications throughout the affected area was disrupted or rendered impossible.[6] The total amount of damage was $2 million (1939 USD,[4] $Шаблон:Inflation million in Шаблон:Inflation-year USD).

The tropical storm was credited with at least one beneficial effect: it ended a vicious heat wave that had lasted for over a week and killed at least 90 people.[10]

People were caught unprepared by the storm,[1] which was described as "sudden". Some people were still on the beach at Long Beach when the wind reached Шаблон:Convert, at which time lifeguards closed the beach. Schools were closed there. At sea, the Coast Guard and Navy conducted rescue operations, saving dozens of people.[6] In response to Californians' unpreparedness, the Weather Bureau established a forecast office for southern California, which began operations in February 1940.[1]

See also

Шаблон:Portal

References

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External links

Шаблон:Floods in California