Basin: | EPac |
Year: | 1932 |
First Storm Formed: | June 21, 1932 |
Last Storm Dissipated: | October 1, 1932 |
Strongest Storm Name: | One |
Strongest Storm Winds: | 115 |
Total Storms: | 5 |
Total Hurricanes: | 4 |
Fatalities: | 15 |
Damages: | 5 |
Five Seasons: | 1930, 1931, 1932, 1933, 1934 |
Atlantic Season: | 1932 Atlantic hurricane season |
West Pacific Season: | 1932 Pacific typhoon season |
North Indian Season: | 1930s North Indian Ocean cyclone seasons |
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 29.48inHg. 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 29.08inHg.[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 28.64inHg. 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 7inches in the mountains of Southern California. Over a seven-hour period, 4.38inches 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]