1957 Pacific hurricane season | |
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Seasonal boundaries | |
First system formed | July 15, 1957 |
Last system dissipated | December 6, 1957 |
Strongest storm | |
Name | Hurricane Twelve |
• Maximum winds | 140 mph (220 km/h) (1-minute sustained) |
• Lowest pressure | 959 mbar (hPa; 28.32 inHg) |
Seasonal statistics | |
Total storms | 13 |
Hurricanes | 9 |
Major hurricanes (Cat. 3+) | 1 |
Total fatalities | 19 direct, 2 indirect |
Total damage | $100,000 (1957 USD) |
Related articles | |
The 1957 Pacific hurricane season was a moderately active year in which 13 tropical cyclones formed. The hurricane season ran through the summer and fall months which conventionally delimit the period during which most tropical cyclones form in the northeastern Pacific Ocean. The first tropical cyclone developed on July 15. The final storm dissipated on December 6, becoming one of the few Pacific storms to exist outside of the seasonal dates. Of the season's 13 storms, five of these formed or crossed into the central Pacific.
During the season, five storms impacted land. Hurricane Twelve was the deadliest, leaving eight casualties in Mazatlán and the costliest was Hurricane Nina, causing an estimated $100,000 in losses. In addition to the damage, four people were killed by Nina in Hawaii. Hurricane Six killed seven people and Hurricane Ten killed two in Mexico.
Category 1 hurricane (SSHWS) | |
Duration | July 15 – July 26 |
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Peak intensity | 85 mph (140 km/h) (1-min); 985 mbar (hPa) |
The first hurricane of the season was identified by the National Weather Bureau in San Francisco, California on July 15. The previous day, the S.S. Garvel Park recorded sustained winds of 50 mph (80 km/h) when it was situated roughly 75 mi (120 km) south of Manzanillo, Mexico. [1] Although listed as a Category 1 hurricane for its entire known existence by the hurricane database, the storm was not confirmed to have attained hurricane intensity until July 21. [2] The storm took a steady westward track during the early portion of its existence in response to a strong ridge located north of Hawaii. [1] [3] On July 18, the National Weather Bureau discontinued advisories on the storm as no information on it was being received. [3]
On July 21, a vessel named Cape Horn relayed information regarding the storm to the National Weather Bureau, leading to them re-issuing advisories on the storm, upgrading it to a hurricane. [1] The following day, a reconnaissance mission from Oahu, Hawaii located the storm's 40 mi (65 km) wide eye and recorded sustained winds of 80 mph (130 km/h) and gusts up to 115 mph (185 km/h). [3] Shortly after, the storm likely attained its peak intensity as a high-end Category 1 hurricane, with winds of 85 mph (135 km/h). [2] Early on July 23, warning responsibility of the storm was given to the National Weather Bureau in Honolulu, Hawaii. [1]
Upon transferring responsibility, the hurricane was given the name Kanoa, the Hawaiian name meaning "the free one". [1] [2] As the storm approached Hawaii, it began to weaken as convection filled the eye. The storm's track mirrored that of the shipping lane between the Panama Canal and Hawaii, leading to several ships being affected. [1] Colder air also began to enter the circulation, leading to further weakening. By the time the system reached Hawaii, it was no more than an area of disturbed weather. The remnants of Kanoa persisted until July 26, at which time they dissipated over the Hawaiian Islands. [3] The remnants of the storm brought beneficial rainfall to most of Hawaii, with heavy rains being reported in parts of the Big Island. [1]
Category 2 hurricane (SSHWS) | |
Duration | August 6 – August 16 |
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Peak intensity | 105 mph (165 km/h) (1-min); 987 mbar (hPa) |
Roughly two weeks after Kanoa dissipated, the season's second hurricane was identified over the open waters of the eastern Pacific on August 6. [2] This storm traveled in a similar fashion to Kanoa in response to a high-pressure system over the northern Pacific. [3] By August 9, the system turned northwest and weakened. [2] Cold, dry air began to enter the storm as it accelerated over cooler waters. Several reconnaissance missions were flown into the storm due to rapid changes in the storm's wind field and structure. [3] Late on August 10, the system intensified into a Category 1 hurricane and its forward motion slowed as it turned more westward. [2]
Although at an unusual latitude, the storm maintained this intensity for over a day before weakening to a tropical storm. [2] During the afternoon of August 13, the small system re-intensified into a hurricane. Reconnaissance reported that gale-force winds extended no more than 100 mi (160 km) from the storm's eye. [3] Shortly thereafter, the system further intensified into a Category 2 hurricane, attaining maximum winds of 105 mph (170 km/h). [2] Weather maps at the time depicted the storm as having a minimum pressure of 987 mbar (hPa). [3] By August 14, the storm began to weaken once more, gradually becoming a tropical storm on August 15. After turning northward, the cyclone became extratropical at a high latitude of 39.8°N. [2] [3]
Category 1 hurricane (SSHWS) | |
Duration | August 9 – August 15 |
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Peak intensity | 85 mph (140 km/h) (1-min); 972 mbar (hPa) |
As Hurricane Two intensified over open waters, the season's third storm was identified on August 9. Initially tracking westward, the hurricane turned sharply north, maintaining an intensity of 85 mph (135 km/h) during its known existence. Briefly slowing on August 11, the system quickly picked up forward speed as it turned northwestward, paralleling the coastline of the Baja California Peninsula. On August 14, the hurricane turned north once more; however, it lost its identity the following day off the coast of Baja California. [2]
Category 1 hurricane (SSHWS) | |
Duration | September 1 – September 9 (Exited basin) |
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Peak intensity | 85 mph (140 km/h) (1-min); 980 mbar (hPa) |
Hurricane Della was first identified on September 1 southeast of Hawaii as a tropical depression. The depression quickly intensified into a tropical storm as it traveled northwest; [2] however, operational advisories were not issued until September 3. By that time, a ship reported they had encountered a storm and recorded winds of 100 mph (160 km/h). Radar images also depicted an eye had developed within the storm. [1] After becoming a hurricane, Della began a gradual turn towards the southwest. [2] During the day on September 4, the storm passed roughly 10 mi (15 km) south of the French Frigate Shoals, bringing strong winds gusting up to 110 mph (175 km/h). During the storm's passage, a pressure of 980 mbar (hPa) was recorded, the lowest in relation to the storm. [1] By September 9, Della began to turn westward as it approached the International Date Line with winds of 85 mph (135 km/h). [2]
During the day, the storm crossed 180°, entering the western Pacific basin and being re-designated as a typhoon. [1] The storm tracked steadily northwestward, attaining a peak intensity of 125 mph (200 km/h), a high-end Category 3 storm, before turning back towards the east. The storm gradually weakened, transitioning into an extratropical cyclone on September 17 and again crossing the International Date Line. The system dissipated shortly thereafter over open waters. [1] [2] Throughout its existence, Hurricane/Typhoon Della traveled roughly 5,000 mi (8,000 km), the longest known track of any Pacific hurricane at the time. [1]
Tropical storm (SSHWS) | |
Duration | September 9 – September 11 |
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Peak intensity | 50 mph (85 km/h) (1-min); |
The fifth tropical cyclone of the season was first identified as a tropical storm several hundred miles southeast of Hawaii on September 9. The storm quickly attained winds of 50 mph (80 km/h) before weakening. By September 11, the system weakened to a tropical depression. [2] Later that day, the system entered an area with no ships available for reporting. However, no ships reported a storm in the region for several days, signifying the depression's dissipation. [1]
Category 1 hurricane (SSHWS) | |
Duration | September 17 – September 18 |
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Peak intensity | 85 mph (140 km/h) (1-min); 984 mbar (hPa) |
On September 17, a new hurricane was identified just off the southern coast of Mexico with winds of 85 mph (135 km/h). Moving northwestward, the storm eventually made landfall near Acapulco, Mexico at this intensity. Shortly after moving over land, the storm lost its identity. [2]
High winds and heavy rains from the storm caused moderate damage to structures and vessels throughout Acapulco, Mexico. [4] Several roads were washed out or flooded by the storm. [5] Seven people were killed throughout the region by the storm, including one U.S. citizen who was electrocuted by a downed power line. [6]
Tropical storm (SSHWS) | |
Duration | September 20 – September 23 |
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Peak intensity | 50 mph (85 km/h) (1-min); 991 mbar (hPa) |
Several days after Hurricane Six lost its identity over Mexico, a new tropical storm formed near the southern edge of the Gulf of California on September 20. Some forecasters stated that the system may have been the remnants of the preceding storm which regenerated. However, the Hurricane Database did not confirm this. The system tracked nearly due north, attaining maximum winds of 50 mph (80 km/h), nearing the coastline of Mexico several times. However, the storm did not make landfall during its existence. On September 22, it turned westward before dissipating just off the coast of Baja California Sur. [2]
Tropical storm (SSHWS) | |
Duration | September 25 – September 28 |
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Peak intensity | 50 mph (85 km/h) (1-min); |
The fifth tropical cyclone to form or enter the central Pacific was first identified on September 25 several hundred miles south of the Hawaiian Islands. Traveling nearly due west, the storm attained an intensity of 50 mph (80 km/h) before weakening. By September 27, the storm weakened to a tropical depression and later dissipated on September 28 over open waters. [2]
Tropical storm (SSHWS) | |
Duration | September 26 – September 27 |
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Peak intensity | 50 mph (85 km/h) (1-min); 999 mbar (hPa) |
The shortest lived storm of the season, Tropical Storm Nine, formed south of Mexico on September 26. The system attained peak winds of 50 mph (80 km/h) during its existence. Later that day, the center of the storm relocated several dozen miles to the west. Shortly thereafter, the storm dissipated on September 27 over open waters. [2]
Category 1 hurricane (SSHWS) | |
Duration | October 1 – October 6 |
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Peak intensity | 85 mph (140 km/h) (1-min); 996 mbar (hPa) |
The tenth known storm of the season was identified on October 1 several hundred miles southwest of the tip of the Baja California Peninsula. Maximum winds observed during the storm's existence reached 85 mph (135 km/h); however, no air pressure was recorded. Initially tracking westward, the system turned northwest and later northeast by October 3. After a brief acceleration on October 4, the hurricane slowed as it neared the coastline of Baja California. Early on October 5, the storm crossed the Peninsula as a Category 1 hurricane before entering the Gulf of California. The hurricane made another landfall near Navojoa, Mexico later that day. Rapid weakening took place as the storm moved over the high terrain over northern Mexico. Early on October 6, the system transitioned into an extratropical cyclone over New Mexico before dissipating several hours later. [2]
At least two people were killed after their home collapsed on them a result of the storm in Mexico. [7] Severe cotton crop damage was reported in the Mexican states of Sonora and Baja California Sur and bridges were washed away by flood waters. [8]
Category 1 hurricane (SSHWS) | |
Duration | October 17 – October 20 |
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Peak intensity | 85 mph (140 km/h) (1-min); 986 mbar (hPa) |
The season's eleven known storm identified several hundred miles south of Mexico on October 17. Quickly tracking northwestward, the storm attained an intensity of 85 mph (135 km/h) during its existence. Early on October 19, the hurricane turned due north, brushing the coastline of Mexico before dissipating just offshore the following day. [2]
Category 4 hurricane (SSHWS) | |
Duration | October 20 – October 22 |
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Peak intensity | 140 mph (220 km/h) (1-min); 959 mbar (hPa) |
The strongest storm of the season, Hurricane Twelve, was first identified as a tropical depression several hundred miles southwest of Sonora, Mexico on October 20. Tracking northeastward, the system gradually intensified into a tropical storm. Late on October 21, the storm underwent a brief period of explosive intensification, strengthening from a 50 mph (80 km/h) tropical storm to a 140 mph (225 km/h) Category 4 hurricane in roughly six hours. The hurricane maintained this intensity for a further six hours before making landfall near Mazatlán. Rapid weakening took place as the hurricane moved inland, with the system dissipating during the afternoon of October 22. [2]
Throughout the affected region, eight people were killed by the storm. Extensive property damage was reported in the region, including the complete collapse of the local baseball stadium. Power lines and telegraph wires were downed throughout the region and high winds reportedly tossed vehicles into buildings. [9] Many shrimp trawlers sank in the storm, leaving substantial losses in Mexico's shrimping industry. [10]
Category 1 hurricane (SSHWS) | |
Duration | November 29 – December 6 |
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Peak intensity | 85 mph (140 km/h) (1-min); ≤1002 mbar (hPa) |
The last storm of the 1957 season, Hurricane Nina, was an unusually late-forming system. It was first identified on November 29 as a tropical storm to the southwest of Hawaii. [2] Steadily tracking north-northeast, the storm intensified into a Category 1 hurricane, by which time it was given the name Nina. As it approached Hawaii, the National Weather Bureau issued warnings for the storm, advising residents to take precaution and possibly evacuate. [1] However, the storm turned westward before moving over the Hawaiian Islands with winds of 85 mph (135 km/h). Gradual weakening took place as the storm continued to move over open waters. Nina eventually dissipated after turning south on December 6. [2]
Waves up to 35 ft (11 m) [1] damaged up to 50 homes across Hawaii [11] and roughly 12 of them being destroyed on Kauai alone. [12] One person was killed on land after being electrocuted by a downed power line. [13] Offshore, a sampan called the Setsu Maru sent a distress call reporting that the boat was sinking 10 miles east of Niihau. [14] All three people aboard the boat were reported dead as a result. [15] In all, damage from the hurricane was estimated at $100,000. [1]
During 1957, tropical storms that formed in the Eastern Pacific region, east of 140°W, were not given names by the local warning center. Those that formed in the Central Pacific, between the International Dateline and 140°W, were named by the National Weather Bureau in Honolulu, Hawaii, as follows: Kanoa, a Hawaiian name; Della and Nina, from the Western Pacific typhoon naming list. [16] No names were retired from either region following the season.
This is a table of all of the storms that formed in the 1957 Pacific hurricane season. It includes their name, duration, peak classification and intensities, areas affected, damage, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all of the damage figures are in 1957 USD.
Name | Dates active | Peak classification | Peak 1-minute sustained winds | Land areas affected | Damage (USD) | Deaths | Refs | |
---|---|---|---|---|---|---|---|---|
Kanoa | July 15–26 | Category 1 hurricane | 85 mph (135 km/h) | None | None | None | ||
Two | August 6–16 | Category 2 hurricane | 105 mph (170 km/h) | None | None | None | ||
Three | August 9–16 | Category 1 hurricane | 85 mph (135 km/h) | None | None | None | ||
Della | September 1–9 | Category 1 hurricane | 85 mph (135 km/h) | Hawaii | None | None | ||
Five | September 9–11 | Tropical storm | 50 mph (80 km/h) | None | None | None | ||
Six | September 17–18 | Category 1 hurricane | 85 mph (135 km/h) | Mexico | Unknown | 7 | ||
Seven | September 20–23 | Tropical storm | 50 mph (80 km/h) | None | None | None | ||
Eight | September 25–28 | Tropical storm | 50 mph (80 km/h) | None | None | None | ||
Nine | September 26–27 | Tropical storm | 50 mph (80 km/h) | None | None | None | ||
Ten | October 1–6 | Category 1 hurricane | 85 mph (135 km/h) | Mexico | 2 | |||
Eleven | October 17–20 | Category 1 hurricane | 85 mph (135 km/h) | None | None | None | ||
Twelve | October 20–22 | Category 4 hurricane | 140 mph (225 km/h) | Mexico | Unknown | 8 | ||
Nina | November 29 – December 6 | Category 1 hurricane | 85 mph (135 km/h) | Mexico | $100,000 | 4 | ||
Season Aggregates | ||||||||
13 storms | July 15 – December 6 | 140 mph (225 km/h) | $100,000 | 21 |
The 2005 Pacific hurricane season was a near-average Pacific hurricane season which produced fifteen named storms, seven hurricanes and two major hurricanes. It was also the second consecutive season in which no tropical cyclone of at least tropical storm intensity made landfall. The season officially began on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. However, the formation of tropical cyclones is possible at any time of the year.
The 2000 Pacific hurricane season was an above-average Pacific hurricane season, although most of the storms were weak and short-lived. There were few notable storms this year. Tropical storms Miriam, Norman, and Rosa all made landfall in Mexico with minimal impact. Hurricane Daniel briefly threatened the U.S. state of Hawaii while weakening. Hurricane Carlotta was the strongest storm of the year and the second-strongest June hurricane in recorded history. Carlotta killed 18 people when it sank a freighter. Overall, the season was significantly more active than the previous season, with 19 tropical storms. In addition, six hurricanes developed. Furthermore, there were total of two major hurricanes.
The 1998 Pacific hurricane season was a fairly average Pacific hurricane season. Despite this, it had nine hurricanes and six major hurricanes, which was well above average. The season officially started on May 15 in the eastern Pacific and on June 1 in the central Pacific, and ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in that region. The first tropical cyclone developed on June 11, about ten days later than the normal start of the season. The final storm of the year, Hurricane Madeline, dissipated on October 20. Storm activity in the Central Pacific Hurricane Center's warning zone was low, with just one tropical depression observed in the region. Two tropical cyclones from the eastern Pacific also entered the central Pacific; the former did so as a hurricane.
The 1997 Pacific hurricane season was a very active hurricane season. With hundreds of deaths and hundreds of millions of dollars in damage, this was one of the deadliest and costliest Pacific hurricane seasons on record. This was due to the exceptionally strong 1997–98 El Niño event. The season officially started on May 15, in the eastern Pacific, and on June 1, in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when almost all tropical cyclones form in the northeastern Pacific Ocean.
The 1995 Pacific hurricane season was the least active Pacific hurricane season since 1979, and marked the beginning of a multi-decade period of low activity in the basin. Of the eleven tropical cyclones that formed during the season, four affected land, with the most notable storm of the season being Hurricane Ismael, which killed at least 116 people in Mexico. The strongest hurricane in the season was Hurricane Juliette, which reached peak winds of 150 mph (240 km/h), but did not significantly affect land. Hurricane Adolph was an early-season Category 4 hurricane. Hurricane Henriette brushed the Baja California Peninsula in early September.
The 1993 Pacific hurricane season included more than double the average number of major hurricanes – Category 3 or stronger cyclones on the Saffir–Simpson scale. This activity was the result of an El Niño event, which is the main factor contributing to above-average activity across the Pacific basin. The season featured 15 named storms, 11 hurricanes, and 9 major hurricanes. While the number of named storms was near the long-term average, the number of hurricanes was above the average of 8, and the number of major hurricanes far exceeded the long-term average of 4. Seasonal activity began on May 17 and ended on November 8, within the confines of a traditional hurricane season which begins on May 15 in the East Pacific and June 1 in the Central Pacific. The season ends on November 30 in both basins. These dates conventionally delimit the period during each year when most tropical cyclones form.
The 1986 Pacific hurricane season featured several tropical cyclones that contributed to significant flooding to the Central United States. The hurricane season officially started May 15, 1986, in the eastern Pacific, and June 1, 1986 in the central Pacific, and lasted until November 30, 1986 in both regions. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. A total of 17 named storms and 9 hurricanes developed during the season; this is slightly above the averages of 15 named storms and 8 hurricanes, respectively. In addition, 26 tropical depressions formed in the eastern Pacific during 1986, which, at the time, was the second most ever recorded; only the 1982 Pacific hurricane season saw a higher total.
The 1985 Pacific hurricane season is the third-most active Pacific hurricane season on record. It officially started on May 15, 1985, in the eastern Pacific, and on June 1, 1985, in the central Pacific, and lasted until November 30, 1985. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. At the time, the 1985 season was the most active on record in the eastern north Pacific, with 28 tropical cyclones forming. Of those, 24 were named, 13 reached hurricane intensity, and 8 became major hurricanes by attaining Category 3 status or higher on the Saffir–Simpson scale. At that time, the 24 named storms was a record; however, this record was broken seven years later in 1992, and was therefore recognized as the second busiest season within the basin, until it was surpassed exactly thirty years later by the 2015 season.
The 1984 Pacific hurricane season featured numerous tropical cyclones, several of which were impactful to land. It was a busy hurricane season with 21 named storms, 13 hurricanes, and 7 major hurricanes, the latter of which are Category 3 or stronger cyclones on the Saffir–Simpson scale. This activity was unusual given the presence of a La Niña, which typically suppresses Central and East Pacific tropical cyclone activity, and only average sea surface temperatures. Seasonal activity began on May 17 and ended on November 8. This lies within the confines of a traditional hurricane season which begins on May 15 in the East Pacific and June 1 in the Central Pacific, and ends on November 30 in both basins. These dates conventionally delimit the period during each year when most tropical cyclones form.
The 1983 Pacific hurricane season was the longest season ever recorded at that time. It was a very active Pacific hurricane season. The season started on May 15, 1983 in the eastern Pacific, and on June 1, 1983 in the central Pacific, and lasted until November 30, 1983. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. During the 1983 season, there were 20 named storms, which was slightly less than the previous season. Furthermore, twelve of those storms became hurricanes. And eight of the storms reached major hurricane status, or Category 3 or higher on the Saffir–Simpson hurricane wind scale (SSHWS). The decaying 1982–83 El Niño event likely contributed to this level of activity. That same El Niño influenced a very quiet Atlantic hurricane season.
The 1982 Pacific hurricane season was, at the time, the most active Pacific hurricane season on record, with 23 named storms. Of those, 12 became hurricanes, with 5 intensifying into major hurricanes. The season officially started on May 15 in the eastern Pacific basin and June 1 in the central Pacific basin. The season in both basins ended on November 30. These dates conventionally delimit the period during which most tropical cyclones form in these regions of the Pacific Ocean. The first tropical cyclone of the season, Tropical Storm Aletta, formed on May 20, and the final one of the season, Hurricane Iwa, dissipated on November 25. A strengthening El Niño that year fueled the season's above normal activity.
The 1979 Pacific hurricane season was an inactive North Pacific hurricane season, featuring 10 named storms, 6 hurricanes, and 4 major hurricanes. All tropical cyclone activity this season was confined to the Eastern Pacific, east of 140°W. For the first time since 1977, no tropical cyclones formed in, or entered into the Central Pacific, between 140°W and the International Date Line.
The 1974 Pacific hurricane season featured one of the most active periods of tropical cyclones on record with five storms existing simultaneously. The season officially started May 15 in the eastern Pacific, and June 1 in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeast Pacific Ocean.
The 1976 Pacific hurricane season was a very deadly and costly season. Hurricanes Kathleen, Liza, and Madeline were the most notable storms this year. Hurricane Kathleen caused death and destruction in California and Arizona due to flooding. Hurricane Liza was the deadliest storm of the season when it killed over 600 people in Mexico. Hurricane Madeline is notable for being one of the most intense Pacific hurricanes at landfall.
The 1975 Pacific hurricane season officially started May 15, 1975, in the eastern Pacific, and June 1, 1975, in the central Pacific, and lasted until November 30, 1975. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeast Pacific Ocean.
The 1978 Pacific hurricane season was the first Pacific hurricane season to use both masculine and feminine names for tropical cyclones. It also began the modern practice of utilizing naming lists every six years. Despite lacking an El Niño, a common driver of enhanced activity in the East and Central Pacific basins, the 1978 season was active. It featured 19 named storms, 14 hurricanes, and 7 major hurricanes, the latter of which are Category 3 or stronger cyclones on the Saffir–Simpson scale. Within the confines of the Central Pacific basin, located between the International Date Line and 140°W, 13 tropical cyclones or their remnants were observed by forecasters at the Central Pacific Hurricane Center, a record number of occurrences at the time. Seasonal activity began on May 30 and ended on October 21, within the limits of a traditional hurricane season which begins on May 15 in the East Pacific and June 1 in the Central Pacific. The season ends on November 30 in both basins. These dates conventionally delimit the period during each year when most tropical cyclones form.
The 1957 Pacific typhoon season has no official bounds; it ran year-round in 1957, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 2007 Pacific hurricane season was a well below-average Pacific hurricane season, featuring only one major hurricane. The season officially started on May 15 in the eastern Pacific and on June 1 in the central Pacific, and ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in the region. The first tropical cyclone of the season, Alvin, developed on May 27, while the final system of the year, Kiko, dissipated on October 23. Due to unusually strong wind shear, activity fell short of the long-term average, with a total of 11 named storms, 4 hurricanes, and 1 major hurricane. At the time, 2007 featured the second-lowest value of the Accumulated cyclone energy (ACE) index since reliable records began in 1971. Two tropical cyclones – Cosme and Flossie – crossed into the central Pacific basin during the year, activity below the average of 4 to 5 systems.
The 2008 Pacific hurricane season was a near-average Pacific hurricane season which featured seventeen named storms, though most were rather weak and short-lived. Only seven storms became hurricanes, of which two intensified into major hurricanes. This season was also the first since 1996 to have no cyclones cross into the central Pacific. The season officially began on May 15 in the eastern Pacific and on June 1 in the central Pacific. It ended in both regions on November 30. These dates, adopted by convention, historically describe the period in each year when most tropical cyclone formation occurs in these regions of the Pacific. This season, the first system, Tropical Storm Alma, formed on May 29, and the last, Tropical Storm Polo, dissipated on November 5.
The 2015 Pacific hurricane season is the second-most active Pacific hurricane season on record, with 26 named storms, only behind the 1992 season. A record-tying 16 of those storms became hurricanes, and a record 11 storms further intensified into major hurricanes throughout the season. The Central Pacific, the portion of the Northeast Pacific Ocean between the International Date Line and the 140th meridian west, had its most active year on record, with 16 tropical cyclones forming in or entering the basin. Moreover, the season was the third-most active season in terms of accumulated cyclone energy, amassing a total of 290 units. The season officially started on May 15 in the Eastern Pacific and on June 1 in the Central Pacific; they both ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Northeast Pacific basin. However, the formation of tropical cyclones is possible at any time of the year. This was shown when a tropical depression formed on December 31. The above-average activity during the season was attributed in part to the very strong 2014–2016 El Niño event.