1933 Pacific hurricane season

Last updated
1933 Pacific hurricane season
Seasonal boundaries
First system formedMay 30, 1933
Last system dissipatedOctober 9, 1933
Strongest storm
NameOne
  Lowest pressure997 mbar (hPa; 29.44 inHg)
Seasonal statistics
Total storms7
Hurricanes1
Total fatalitiesUnknown
Total damageUnknown
Related articles
Pacific hurricane seasons
1931, 1932, 1933, 1934, 1935

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.

Contents

Systems

Tropical Cyclone One

On May 30, a tropical cyclone existed in the Gulf of Tehuantepec. Shortly after its discovery, it dissipated off the coast of Guatemala. A ship reported gales and a pressure of 29.44 inHg (99.7 kPa). [1]

Possible Tropical Cyclone Two

Sometime in June, a possible tropical cyclone existed south of the Mexican coast. [2]

Possible Tropical Cyclone Three

A possible tropical cyclone was reported between Salina Cruz and Acapulco July 7. It had moved closer to Acapulco by July 8. This system might have been associated with the remnants of the Atlantic's second tropical cyclone. [3]

Possible Tropical Cyclone Four

Another possible tropical cyclone existed in the same area on July 29. [3]

Tropical Storm Five

A tropical cyclone formed in the Gulf of Tehuantepec on August. It moved along the coast, becoming at least a tropical storm, and dissipated in the Gulf of California on August 19 or 20. A ship reported an uncorrected barometer reading of 29.48 inHg (99.8 kPa). [4]

Possible Tropical Cyclone Six

A possible tropical cyclone existed on September 13. It was located well west of Manzanillo. [5]

Hurricane Seven

A "tropical hurricane" was tracked well northeast of Hawaii between October 7 and 9. [6]

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 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 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.

References

  1. Hurd, Willis (May 1933). "North Pacific Ocean, May 1933" (PDF). Monthly Weather Review . 61 (5): 148. Bibcode:1933MWRv...61..148H. doi:10.1175/1520-0493(1933)61<148b:NPOM>2.0.CO;2 . Retrieved 2011-01-18.
  2. Hurd, Willis (June 1933). "North Pacific Ocean, June 1933" (PDF). Monthly Weather Review . 61 (6): 179. Bibcode:1933MWRv...61..179H. doi:10.1175/1520-0493(1933)61<179b:NPOJ>2.0.CO;2 . Retrieved 2011-01-18.
  3. 1 2 Hurd, Willis (July 1933). "North Pacific Ocean, July 1933" (PDF). Monthly Weather Review . 61 (7): 209. Bibcode:1933MWRv...61..209H. doi:10.1175/1520-0493(1933)61<209b:NPOJ>2.0.CO;2 . Retrieved 2011-01-18.
  4. McDonald, WF (August 1933). "North Pacific Ocean, August, 1933" (PDF). Monthly Weather Review . 61 (8): 241. Bibcode:1933MWRv...61..241M. doi:10.1175/1520-0493(1933)61<241b:NPOA>2.0.CO;2 . Retrieved 2011-01-18.
  5. Hurd, Willis (September 1933). "North Pacific Ocean, September 1933" (PDF). Monthly Weather Review . 61 (9): 283. Bibcode:1933MWRv...61..283H. doi:10.1175/1520-0493(1933)61<283:NPOS>2.0.CO;2 . Retrieved 2011-01-18.
  6. United States Weather Bureau (1947). Pressure Center Tracks From the 1300 GMT Northern Hemisphere Sea Level Pressure Maps. Tracks of Lows 1929-1933.