| 1932 Pacific hurricane season | |
|---|---|
| Seasonal boundaries | |
| First system formed | June 21, 1932 |
| Last system dissipated | October 1, 1932 |
| Strongest storm | |
| Name | One |
| • Maximum winds | 130 mph (215 km/h) |
| Seasonal statistics | |
| Total storms | 5 |
| Hurricanes | 4 |
| Total fatalities | 15 |
| Total damage | $5 million (1932 USD) |
| Related articles | |
The 1932 Pacific hurricane season ran through the summer and fall of 1932. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
A tropical cyclone formed in the Gulf of Tehuantepec on June 18. It moved along the coast, became a hurricane, and was last seen June 21. The lowest pressure was an uncorrected 29.48 inHg (99.8 kPa). This hurricane was reported to have winds of 130 mph. [1]
On August 21, tropical cyclone was heading northwestward south of the Revillagigedo Islands. A ship at the fringes of the cyclone measured a pressure of 29.08 inHg (98.5 kPa). [2]
Between August 25 and 27, a "tropical hurricane" formed offshore southern Mexico, and moved north-northwest into southwest Mexico east of Manzanillo before dissipating. [3]
Somewhere southwest of the Gulf of Tehuantepec, a tropical cyclone formed on September 24. It paralleled the coast, and intensified into a hurricane on September 25. It then recurved, and made landfall near Mazatlán late during the night of September 26 and 27, while still a hurricane. It dissipated inland over the mountains of Mexico. The lowest pressure reported by a ship was 28.64 inHg (97.0 kPa). The hurricane caused about $5,000,000 (1932 USD) in damage. [2]
On September 26, a hurricane was spotted south of Acapulco. It headed along the coast, and entered the Gulf of California sometime on or after September 28, [4] wherein it moved north-northwest and dissipated, with its remnants continuing into the Southwestern United States. [5]
Powerful winds in Mazatlán were attributed to this system. [4] Over a four-day period ending October 1, those remnants caused heavy rain of up to 7 inches (180 mm) in the mountains of Southern California. Over a seven-hour period, 4.38 inches (111 mm) fell at Tehachapi. [5] That total by itself is enough to make this tropical cyclone one of California's wettest tropical storm. [6] Those rains also caused flash flooding on Tehachapi and Agua Caliente Creeks, which killed fifteen people. [7]
Tehuantepecer, or Tehuano wind, is a violent mountain-gap wind that travels through the Chivela Pass in southern Mexico, across the Isthmus of Tehuantepec. It is most common between October and February, with a summer minimum in July. It originates from eastern Mexico and the Bay of Campeche as a post-frontal northerly wind, accelerated southward by cold air damming, that crosses the isthmus and blows through the gap between the Mexican and Guatemalan mountains. The term dates back to at least 1929. This wind can reach gale, storm, even hurricane force. The leading edge of its outflow may form rope cloud over the Gulf of Tehuantepec. These winds can be observed on satellite pictures such as scatterometer wind measurements, they influence waves which then propagate as swell and are sometimes observed 1,600 km (1,000 mi) away. These strong winds bring cooler sub-surface waters to the surface of the tropical eastern Pacific Ocean and may last from a few hours to 6 days.
The 1939 Pacific hurricane season ran through the summer and fall of 1939. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land. However, 1939 saw a large number of storms threaten California.
A Pacific hurricane is a mature tropical cyclone that develops within the northeastern and central Pacific Ocean to the east of 180°W, north of the equator. For tropical cyclone warning purposes, the northern Pacific is divided into three regions: the eastern, central, and western, while the southern Pacific is divided into 2 sections, the Australian region and the southern Pacific basin between 160°E and 120°W. Identical phenomena in the western north Pacific are called typhoons. This separation between the two basins has a practical convenience, however, as tropical cyclones rarely form in the central north Pacific due to high vertical wind shear, and few cross the dateline.
The 1940 Pacific hurricane season ran through the summer and fall of 1940. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land. During this season, there is a former typhoon that crossed into central north Pacific.
The 1941 Pacific hurricane season ran through the summer and fall of 1941. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land. 1941 season was the last season before Monthly Weather Review stopped publishing temporarily due to World War II.
The 1938 Pacific hurricane season ran through the summer and fall of 1938. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land. However, 1938 saw an unusually active season, with numerous tropical cyclones forming in January and a hurricane struck Northern California in February, killing five people. On August 18, Cyclone Mokapu caused record August rainfall, and a record low pressure when it struck Hawaiian Islands. It brought down power lines and damages into a plantation.
The 1937 Pacific hurricane season ran through the summer and fall of 1937. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land. 1937 season was mostly inactive season, as there is no known tropical cyclones in September during this season. In May, a tropical cyclone struck Acapulco, cutting that city off from the outside communication for four days, causing buildings in the city to be damaged, and caused a woman's death.
The 1936 Pacific hurricane season ran through the summer and fall of 1936. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land. There are numerous damaging tropical cyclones during the season, and half of tropical cyclones during the season became hurricanes.
The 1935 Pacific hurricane season ran through the summer and fall of 1935. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land. This season saw three tropical cyclones and ended early in August.
The 1934 Pacific hurricane season ran through the summer and fall of 1934. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
The 1933 Pacific hurricane season ran through the summer and fall of 1933. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
The 1931 Pacific hurricane season ran through the summer and fall of 1931. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
The 1930 Pacific hurricane season ran through the summer and fall of 1930. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
The 1929 Pacific hurricane season ran through the summer and fall of 1929. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
The 1927 Pacific hurricane season ran through the summer and fall of 1927. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
The 1928 Pacific hurricane season ran through the summer and fall of 1928. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
The 1926 Pacific hurricane season ran through the summer and fall of 1926. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land.
The 1925 Pacific hurricane season ran through the summer and fall of 1925. Before the satellite age started in the 1960s, data on east Pacific hurricanes was extremely unreliable. Most east Pacific storms were of no threat to land. 1925 season was the first Pacific hurricane season that was covered in detail by Monthly Weather Review, and this season included the most intense November Pacific hurricane on record until beaten by Hurricane Kenneth in 2011.
The 1975 Pacific Northwest hurricane was an unusual Pacific tropical cyclone that attained hurricane status farther north than any other Pacific hurricane. It was officially unnamed, with the cargo ship Transcolorado providing vital meteorological data in assessing the storm. The twelfth tropical cyclone of the 1975 Pacific hurricane season, it developed from a cold-core upper-level low merging with the remnants of a tropical cyclone on August 31, well to the northeast of Hawaii. Convection increased as the circulation became better defined, and by early on September 2, it became a tropical storm. Turning to the northeast through an area of warm water temperatures, the storm quickly strengthened, and, after developing an eye, it attained hurricane status late on September 3, while located about 1,200 miles (1,950 km) south of Alaska. After maintaining peak winds for about 18 hours, the storm rapidly weakened, as it interacted with an approaching Cold front. Early on September 5, it lost its identity near the coast of Alaska.
The 1942–48 Pacific hurricane seasons all began during late spring in the northeast Pacific Ocean and the central Pacific. They ended in late fall.
