1928 Pacific hurricane season

Last updated
1928 Pacific hurricane season
Seasonal boundaries
First system formedMay 24, 1928
Last system dissipatedOctober 17, 1928
Strongest storm
NameFour
  Lowest pressure965 mbar (hPa; 28.5 inHg)
Seasonal statistics
Total storms9
Hurricanes4
Total fatalities14
Total damageUnknown
Related articles
Pacific hurricane seasons
1926, 1927, 1928, 1929, 1930

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.

Contents

Systems

Tropical Cyclone One

A weak tropical cyclone existed south of the Gulf of California was spotted on May 24. It moved westward, and was last seen on May 27. The lowest pressure reported was 29.77 inHg (100.8 kPa). [1]

Tropical Cyclone Two

A tropical cyclone in the Gulf of Tehuantepec produced gales on June 5. The lowest reported pressure was 29.67 inHg (100.5 kPa). [2]

Hurricane Three

A hurricane existed south of Cape Corrientes on July 28 and 29. The lowest reported pressure was a reading of 29.64 inHg (100.4 kPa). [3]

Hurricane Four

A tropical cyclone was noticed just south of the Mexican coast on August 6. This system might have formed south of Costa Rica three days earlier. Wherever it formed, this tropical cyclone intensified into a hurricane, and paralleled the coast. It passed south of the Gulf of California on August 10. The hurricane passed northwestward of Cabo San Lucas on September, and dissipated on August 11 while over the southern part of the Baja California Peninsula. The lowest pressure reported in association with this hurricane was 28.50 inHg (96.5 kPa). [4]

This hurricane brought gale or hurricane-force winds to several areas of the Mexican coast. An American steamer, the William A. McKenney, had its cargo and structure damaged by the hurricane. Repairs were attempted during the storm, and 14 members of its crew were washed overboard and drowned. [4]

Tropical Cyclone Five

On September 1, a tropical cyclone formed well south of the southern tip of the Baja California Peninsula. It moved west-northwest and was last seen on September 3. A ship reported a pressure reading of 29.44 inHg (99.7 kPa). [5]

Hurricane Six

About 200 miles west-southwest of Acapulco, a tropical cyclone formed on September 17. It slowly moved northwestward. It had intensified into a hurricane by September 18. On September 21, the hurricane weakened and recurved to the east-northeast. It made landfall north of Mazatlán and became a remnant over Mexico. Its remnants had crossed Mexico by September 22 and entered the Gulf of Mexico south of Brownsville, Texas. [5] They never developed into anything, [6] and had dissipated by the end of the month. The lowest pressure reported by a ship was 28.82 inHg (97.6 kPa). [5]

Tropical Cyclone Seven

From September 20 to 22, a tropical cyclone existed south of the Gulf of Tehuantepec. [5]

Hurricane Eight

On October 7, at a location well south of the entrance to the Gulf of California, a hurricane existed. It was moving northwest. A ship measured a central pressure of 29.60 inHg (100.2 kPa). [7]

Tropical Cyclone Nine

On October 16 and 17, a ship encountered a tropical cyclone well south of the southern Tip of the Baja California Peninsula. The ship reported a pressure of 29.48 inHg (99.8 kPa). [7]

See also

Related Research Articles

<span class="mw-page-title-main">Tehuantepecer</span> Violent mountain-gap wind traveling through Chivela Pass

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.

<span class="mw-page-title-main">1939 Pacific hurricane season</span> Hurricane season in the Pacific Ocean

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.

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 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.

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 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 1942–48 Pacific hurricane seasons all began during late spring in the northeast Pacific Ocean and the central Pacific. They ended in late fall.

References

  1. Hurd, Willis (May 1928). "North Pacific Ocean" (PDF). Monthly Weather Review . 56 (2): 73. Bibcode:1928MWRv...56...73H. doi:10.1175/1520-0493(1928)56<73:NPO>2.0.CO;2 . Retrieved 2011-01-18.
  2. Hurd, Willis (June 1928). "North Pacific Ocean" (PDF). Monthly Weather Review . 56 (2): 73. Bibcode:1928MWRv...56...73H. doi:10.1175/1520-0493(1928)56<73:NPO>2.0.CO;2 . Retrieved 2011-01-18.
  3. Hurd, Willis (July 1928). "North Pacific Ocean" (PDF). Monthly Weather Review . 56 (2): 73. Bibcode:1928MWRv...56...73H. doi:10.1175/1520-0493(1928)56<73:NPO>2.0.CO;2 . Retrieved 2011-01-18.
  4. 1 2 Hurd, Willis (August 1928). "North Pacific Ocean" (PDF). Monthly Weather Review . 56 (2): 73. Bibcode:1928MWRv...56...73H. doi:10.1175/1520-0493(1928)56<73:NPO>2.0.CO;2 . Retrieved 2011-01-18.
  5. 1 2 3 4 Hurd, Willis (September 1928). "North Pacific Ocean" (PDF). Monthly Weather Review . 56 (2): 73. Bibcode:1928MWRv...56...73H. doi:10.1175/1520-0493(1928)56<73:NPO>2.0.CO;2 . Retrieved 2011-01-18.
  6. "Atlantic hurricane best track (HURDAT version 2)" (Database). United States National Hurricane Center. September 19, 2022. Retrieved February 15, 2023.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  7. 1 2 Hurd, Willis (October 1928). "North Pacific Ocean" (PDF). Monthly Weather Review . 56 (2): 73. Bibcode:1928MWRv...56...73H. doi:10.1175/1520-0493(1928)56<73:NPO>2.0.CO;2 . Retrieved 2011-01-18.