1963 Pacific typhoon season | |
---|---|
Seasonal boundaries | |
First system formed | March 25, 1963 |
Last system dissipated | December 28, 1963 |
Strongest storm | |
Name | Judy |
• Maximum winds | 280 km/h (175 mph) (1-minute sustained) |
• Lowest pressure | 920 hPa (mbar) |
Seasonal statistics | |
Total depressions | 36 |
Total storms | 25 |
Typhoons | 19 |
Super typhoons | 8 (unofficial) |
Total fatalities | Unknown |
Total damage | Unknown |
Related articles | |
The 1963 Pacific typhoon season has no official bounds; it ran year-round in 1963, 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 scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1963 Pacific hurricane season. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions in this basin have the "W" suffix added to their number. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names. This was the first season in which PAGASA assigned local names to typhoons. [1]
Timeline of tropical activity in the 1963 Pacific typhoon season
36 tropical depressions formed this year in the Western Pacific, of which 25 became tropical storms. 19 storms reached typhoon intensity, of which 8 reached super typhoon strength. [2]
Tropical depression (SSHWS) | |
Duration | March 25 – March 25 |
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Peak intensity | 55 km/h (35 mph) (1-min); |
A brief tropical depression developed north of Papua New Guinea at 00:00 UTC on March 25, and tracked west-northwest before it dissipated later that day. Although the Joint Typhoon Warning Center does not list any maximum sustained wind values in its tracking data, [3] the Mariners Weather Log notes that Tropical Depression 03W briefly attained winds of 55 km/h (35 mph) at its peak before dissipating. [4]
Tropical depression (JMA) | |
Duration | March 31 – April 6 |
---|---|
Peak intensity | 55 km/h (35 mph) (10-min); 1001 hPa (mbar) |
The China Meteorological Administration (CMA) analyzed the formation of a disturbance near Micronesia on March 30, though no other agencies monitored the system. Tracking westward, the low-pressure area developed further into a tropical depression the following day. The storm turned towards the north on April 1, reaching peak intensity two days later with winds of 55 km/h and a minimum pressure of 1001 mbar (hPa; 29.56 inHg) before slowly weakening. On April 6, the depression degenerated into a remnant area of low pressure; these remnants tracked westward before dissipating early the next day. [5]
Typhoon (JMA) | |
Category 4-equivalent typhoon (SSHWS) | |
Duration | April 26 – May 5 |
---|---|
Peak intensity | 230 km/h (145 mph) (1-min); 920 hPa (mbar) |
The low-pressure area that eventually developed into Typhoon Olive first formed approximately 155 km (96 mi) southeast of Truk on April 21, [6] embedded within the larger context of a trough. [2] In its nascent stages, the disturbance tracked slowly west-northwestward toward Woleai; the Japan Meteorological Agency (JMA) considers the storm to have developed into a tropical depression on April 26, [7] though the JTWC began monitoring Olive as a 75 km/h (45 mph) tropical storm the day after. [8] Olive quickly intensified following tropical cyclogenesis, becoming a typhoon by 12:00 UTC on April 27. [8] Late on April 28, a reconnaissance mission sampled winds of 230 km/h (145 mph) and a minimum barometric pressure of 932 mbar (hPa; 27.52 inHg); [2] from these parameters Olive reached peak intensity at 00:00 UTC on April 29 with a minimum pressure of 920 mbar as computed by the JMA. [7] Olive passed near Guam and Saipan later that day, impacting the latter with winds of 205 km/h (125 mph). [6] As the typhoon receded to more northerly latitudes, it slowly weakened, transitioning into an extratropical cyclone on May 5 before dissipating four days later; [7] maintaining typhoon strength for 8.5 days, Olive remained a typhoon longer than any other storm in 1963. [6]
As Olive neared Guam, then-governor Manuel Guerrero ordered the evacuation of low-lying areas and the opening of shelters at schools, churches, and other locations. [9] Olive caused considerable damage in the Mariana Islands: 95 percent of homes on Saipan sustained extensive damage, with another 5 percent destroyed by the storm. Homes were also damaged on nearby Rota, with the widespread loss of crops; property and agricultural losses were also accrued on Guam and Tinian, where power lines were downed by strong winds and 1,000 people were left homeless. [6] The effects of the typhoon set back Guam's recovery from Typhoon Karen the previous year, damaging homes partially repaired via recovery loans for Karen. [10] Estimated damage from Olive amounted to US$5 million. [6] In the storm's aftermath, deputy high commissioner for the Trust Territory of the Pacific Islands Jose Benitez requested the declaration of Tinian and Saipan as disaster areas. [11] On April 30, then-U.S. President John F. Kennedy acknowledged Benitez's request and declared a disaster area for the impacted islands. Kennedy would later allocate US$1.3 million for storm relief in Saipan, Tinian, and Rota. [12] Food and medical supplies were sent from the Caroline and Marshall Islands to the Mariana Islands. [13]
Typhoon (JMA) | |
Category 1-equivalent typhoon (SSHWS) | |
Duration | May 27 – June 5 |
---|---|
Peak intensity | 130 km/h (80 mph) (1-min); 978 hPa (mbar) |
Polly originated from an area of low pressure first detected 145 km (90 mi) north-northwest of Woleai on May 25. [6] The JMA determined that the disturbance developed into a tropical depression on May 27, [14] though the JTWC initiated warnings on the system on May 31. [6] The cyclone gradually strengthened after formation, reaching tropical storm strength on June 1 and typhoon intensity the day after. [14] On June 3, Polly reached peak intensity with sustained winds of 130 km/h (80 mph) and a minimum pressure of 978 mbar (hPa; 28.88 inHg), [15] after which it began to slowly taper off in strength and accelerate northeastward. On June 5, Polly passed 190 km (120 mi) southeast of Tokyo as a low-end typhoon before recurving towards the east-northeast. [6] [16] The extratropical remnants of Polly reached the Bering Sea and the coast of Alaska on June 10 before dissipating. [16] Polly was the first storm ever to be named by PAGASA.
Remaining offshore Japan, Polly's impacts were caused primarily by heavy rainfall. Flooding inundated caused 807 landslides and inundated over 36,000 homes. Another 11 houses and 270 bridges were washed away by the floods. Polly caused an estimated US$138 million in damage to crops, with the total damage figure in excess of US$143 million. [6] Eighteen people were killed and another seventeen were injured; [6] 20,702 others were homeless after Polly's passage. [17]
Tropical storm (JMA) | |
Tropical storm (SSHWS) | |
Duration | June 6 – June 14 |
---|---|
Peak intensity | 95 km/h (60 mph) (1-min); 992 hPa (mbar) |
Tropical Storm Rose began as a tropical depression in the South China Sea on June 6, and tracked southeastward towards Luzon in its early stages. [18] On June 8, the JTWC began issuing warnings on Rose as a tropical storm while the cyclone was just off Luzon's northwestern coast. [6] [19] Slow strengthening continued thereafter, with Rose's peaking as a 95 km/h (60 mph) tropical storm as it was tracking across the Ryukyu Islands, [19] though the storm's strongest winds were contained within a narrow rainband near the center. [6] Moving rapidly northeastward, Rose passed over western Honshu as a lower-end tropical storm on June 13, [19] briefly emerging into the Sea of Japan before recurving eastward and transitioning into an extratropical cyclone over northern Honshu on June 14. [18] The remnants of Rose merged with another weak extratropical low off the Japanese coast, and this combined system continued eastward before dissipating over the Bering Sea on June 18. [6]
Typhoon (JMA) | |
Category 5-equivalent super typhoon (SSHWS) | |
Duration | June 12 – June 20 |
---|---|
Peak intensity | 260 km/h (160 mph) (1-min); 935 hPa (mbar) |
Typhoon (JMA) | |
Category 1-equivalent typhoon (SSHWS) | |
Duration | June 15 – July 2 |
---|---|
Peak intensity | 130 km/h (80 mph) (1-min); 984 hPa (mbar) |
Tropical storm (JMA) | |
Tropical storm (SSHWS) | |
Duration | July 1 – July 9 |
---|---|
Peak intensity | 95 km/h (60 mph) (1-min); 990 hPa (mbar) |
Tropical depression (PAGASA) | |
Duration | July 11 – July 13 |
---|---|
Peak intensity | 55 km/h (35 mph) (10-min); |
A system that lasted from July 11–13.
Typhoon (JMA) | |
Category 4-equivalent typhoon (SSHWS) | |
Duration | July 9 – July 20 |
---|---|
Peak intensity | 250 km/h (155 mph) (1-min); 930 hPa (mbar) |
Tropical depression (CMA) | |
Duration | July 11 – July 13 |
---|---|
Peak intensity | 55 km/h (35 mph) (10-min); 1002 hPa (mbar) |
Typhoon (JMA) | |
Category 2-equivalent typhoon (SSHWS) | |
Duration | July 15 – July 24 |
---|---|
Peak intensity | 155 km/h (100 mph) (1-min); 992 hPa (mbar) |
Typhoon (JMA) | |
Category 4-equivalent typhoon (SSHWS) | |
Duration | July 25 – August 11 |
---|---|
Peak intensity | 240 km/h (150 mph) (1-min); 930 hPa (mbar) |
On July 27 Tropical Depression 20W formed in the West Pacific. It drifted northward, reaching tropical storm on the 30th before turning to the southwest. Bess turned to the north on August 2, and reached typhoon status early on the 3rd. Bess rapidly intensified to a peak of 150 mph on the 4th, but weakened as it continued northward. On the 9th it struck Japan, and on the 11th Bess became extratropical. At the time, Bess had the longest longevity of a Western Pacific tropical cyclone. Typhoon Bess caused severe damage on the island of Kyūshū. 23 people were killed and 6 were missing. [20]
Tropical depression (JMA) | |
Tropical storm (SSHWS) | |
Duration | July 29 – August 2 |
---|---|
Peak intensity | 65 km/h (40 mph) (1-min); 997 hPa (mbar) |
Typhoon (JMA) | |
Category 4-equivalent typhoon (SSHWS) | |
Duration | August 8 – August 18 |
---|---|
Peak intensity | 230 km/h (145 mph) (1-min); 930 hPa (mbar) |
Tropical depression (CMA) | |
Duration | August 21 – August 23 |
---|---|
Peak intensity | 55 km/h (35 mph) (10-min); 1001 hPa (mbar) |
Typhoon (JMA) | |
Category 3-equivalent typhoon (SSHWS) | |
Duration | August 23 – August 27 |
---|---|
Peak intensity | 185 km/h (115 mph) (1-min); 965 hPa (mbar) |
Typhoon (JMA) | |
Category 3-equivalent typhoon (SSHWS) | |
Duration | August 23 – August 29 |
---|---|
Peak intensity | 185 km/h (115 mph) (1-min); 975 hPa (mbar) |
Tropical depression (SSHWS) | |
Duration | August 27 – August 28 |
---|---|
Peak intensity | 55 km/h (35 mph) (1-min); |
Typhoon (JMA) | |
Category 3-equivalent typhoon (SSHWS) | |
Duration | August 28 – September 11 |
---|---|
Peak intensity | 205 km/h (125 mph) (1-min); 960 hPa (mbar) |
Typhoon Faye struck Hong Kong killing 3 people. [21]
Tropical depression (CMA) | |
Duration | August 28 – August 31 |
---|---|
Peak intensity | 55 km/h (35 mph) (10-min); 997 hPa (mbar) |
Tropical depression (SSHWS) | |
Duration | August 26 – August 26 |
---|---|
Peak intensity | 45 km/h (30 mph) (1-min); |
Tropical depression (CMA) | |
Duration | September 1 – September 2 |
---|---|
Peak intensity | 45 km/h (30 mph) (10-min); 1002 hPa (mbar) |
Typhoon (JMA) | |
Category 4-equivalent typhoon (SSHWS) | |
Duration | September 3 – September 15 |
---|---|
Peak intensity | 250 km/h (155 mph) (1-min); 920 hPa (mbar) |
Typhoon Gloria, known in the Philippines as Typhoon Oniang was a typhoon of the 1963 Pacific typhoon season. [22] Gloria impacted Taiwan and China.
Typhoon Gloria developed on September 5, over the open waters of the West Pacific. The storm rapidly intensified to a peak of 155 mph on September 9. It weakened as it continued west-northwestward, and made landfall on extreme northeastern Taiwan on September 11, as a 100 mph typhoon. [22] The typhoon caused severe flooding in Northern Taiwan and killed hundreds of people. [23] Gloria continued westward, and hit eastern China that night as an 85 mph typhoon. The storm looped over land to the northeast, and dissipated on September 13, to the east of China. Gloria killed 239 people, and left 89 missing. [23]
Tropical storm (JMA) | |
Tropical storm (SSHWS) | |
Duration | September 7 – September 13 |
---|---|
Peak intensity | 85 km/h (50 mph) (1-min); 998 hPa (mbar) |
Tropical storm (JMA) | |
Tropical storm (SSHWS) | |
Duration | September 16 – September 19 |
---|---|
Peak intensity | 75 km/h (45 mph) (1-min); 1002 hPa (mbar) |
Tropical depression (JMA) | |
Tropical depression (SSHWS) | |
Duration | September 20 – September 24 |
---|---|
Peak intensity | 45 km/h (30 mph) (10-min); 1004 hPa (mbar) |
This tropical depression hit Vietnam in late September and crossed into the Northern Indian Ocean, reforming as Deep Depression Nine. [24]
Typhoon (JMA) | |
Category 5-equivalent super typhoon (SSHWS) | |
Duration | September 27 – October 4 |
---|---|
Peak intensity | 280 km/h (175 mph) (1-min); 920 hPa (mbar) |
Tropical depression (CMA) | |
Duration | October 2 – October 3 |
---|---|
Peak intensity | 45 km/h (30 mph) (10-min); 1005 hPa (mbar) |
Typhoon (JMA) | |
Category 4-equivalent typhoon (SSHWS) | |
Duration | October 3 – October 11 |
---|---|
Peak intensity | 250 km/h (155 mph) (1-min); 930 hPa (mbar) |
Typhoon (JMA) | |
Category 4-equivalent typhoon (SSHWS) | |
Duration | October 6 – October 19 |
---|---|
Peak intensity | 240 km/h (150 mph) (1-min); 943 hPa (mbar) |
Typhoon (JMA) | |
Category 3-equivalent typhoon (SSHWS) | |
Duration | October 13 – October 18 |
---|---|
Peak intensity | 185 km/h (115 mph) (1-min); 965 hPa (mbar) |
Tropical depression (JMA) | |
Tropical storm (SSHWS) | |
Duration | October 18 – October 20 |
---|---|
Peak intensity | 75 km/h (45 mph) (1-min); 1000 hPa (mbar) |
Typhoon (JMA) | |
Category 1-equivalent typhoon (SSHWS) | |
Duration | October 22 – October 30 |
---|---|
Peak intensity | 150 km/h (90 mph) (1-min); 985 hPa (mbar) |
Tropical storm (JMA) | |
Category 1-equivalent typhoon (SSHWS) | |
Duration | December 8 – December 15 |
---|---|
Peak intensity | 140 km/h (85 mph) (1-min); 994 hPa (mbar) |
Typhoon (JMA) | |
Tropical storm (SSHWS) | |
Duration | December 15 – December 19 |
---|---|
Peak intensity | 75 km/h (45 mph) (1-min); 998 hPa (mbar) |
Typhoon (JMA) | |
Category 4-equivalent typhoon (SSHWS) | |
Duration | December 18 – December 28 |
---|---|
Peak intensity | 250 km/h (155 mph) (1-min); 935 hPa (mbar) |
|
|
|
|
Auring | Bebeng | Karing | Diding | Etang |
Gening | Herming | Ising | Luding | Mameng |
Neneng | Oniang | Pepang | Rosing | Sisang |
Trining | Uring (unused) | Welming (unused) | Yayang (unused) | |
Auxiliary list | ||||
---|---|---|---|---|
Ading (unused) | ||||
Barang (unused) | Krising (unused) | Dadang (unused) | Erling (unused) | Goying (unused) |
The Philippine Atmospheric, Geophysical and Astronomical Services Administration uses its own naming scheme for tropical cyclones in their area of responsibility. PAGASA assigns names to tropical depressions that form within their area of responsibility and any tropical cyclone that might move into their area of responsibility. Should the list of names for a given year prove to be insufficient, names are taken from an auxiliary list, the first 10 of which are published each year before the season starts. Names not retired from this list will be used again in the 1967 season. PAGASA uses its own naming scheme that starts in the Filipino alphabet, with names of Filipino female names ending with "ng" (A, B, K, D, etc.). This was the first season in which PAGASA assigned local names to typhoons. Names that were not assigned/going to use are marked in gray.
The 2004 Pacific typhoon season was an extremely active season that featured the second-highest ACE ever recorded in a single season, second only to 1997, which featured 29 named storms, nineteen typhoons, and six super typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2004, though most tropical cyclones typically develop between May and October. The season's first named storm and also the first typhoon, Sudal, developed on April 4, later was reached typhoon status two days later, and became the first super typhoon of the year three days later. The season's last named storm, Noru, dissipated on December 21.
The 1998 Pacific typhoon season was the least active Pacific typhoon season on record, until it was surpassed 12 years later. It would produce 16 tropical storms, 8 strengthening into typhoons. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1998 Pacific hurricane season. Tropical Storms formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions in this basin have the "W" suffix added to their number. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
The 1992 Pacific typhoon season is the fourth consecutive above-average season, producing 31 tropical storms, 16 typhoons and five super typhoons. It had no official bounds; it ran year-round in 1992. Despite this, most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1979 Pacific typhoon season featured the largest and most intense tropical cyclone recorded globally, Typhoon Tip. The season also used both male and female names as tropical cyclone names for the first time. Additionally, the season was slightly below-average in terms of tropical cyclone activity, with only 24 storms, 12 typhoons, and 4 super typhoons developing. The season had no official bounds; it ran year-round in 1979, 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 1978 Pacific typhoon season was a very active season that produced 31 tropical storms, 16 typhoons and one intense typhoon. It ran year-round in 1978, 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 1959 Pacific typhoon season was regarded as one of the most devastating years for Pacific typhoons on record, with China, Japan and South Korea sustaining catastrophic losses. It was an event in the annual cycle of tropical cyclone formation. The season had no official bounds, but tropical cyclones in the Western Pacific Ocean normally develop between May and October.
The 1976 Pacific typhoon season has no official bounds; it ran year-round in 1976, 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 1970 Pacific typhoon season has no official bounds; it ran year-round in 1970, 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 1975 Pacific typhoon season was one of the deadliest tropical cyclone seasons on record, with nearly 229,000 fatalities occurring during the season. It had no official bounds; it ran year-round in 1975, 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 1974 Pacific typhoon season was the first season on record to not feature a Category 5 equivalent super typhoon; a feat later repeated by the 1977 and 2017 seasons. Even so, the season was overly active, with 32 tropical storms and 16 typhoons being developed this year. It has no official bounds; it ran year-round in 1974, 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 1971 Pacific typhoon season was an extremely active season that featured the second highest typhoon count on record. It has no official bounds; it ran year-round in 1971, 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 1968 Pacific typhoon season has no official bounds; it ran year-round in 1968, 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 1967 Pacific typhoon season was one of the most active Pacific typhoon seasons on record, witnessing the formation of 35 tropical storms during the season. It began on January 1, 1967, though most storms usually form between June and December within the basin. The first storm of the season, Ruby, formed on January 28 west of the Philippines. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1967 Pacific hurricane season. Tropical depressions that are monitored by the United States' Joint Typhoon Warning Center (JTWC) were given a numerical designation with a "W" suffix, and any storms reaching 1-minute sustained winds of over 40 mph were given a name. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
The 1966 Pacific typhoon season was an active season, with many tropical cyclones having severe impacts in China, Japan, and the Philippines. Overall, there were 49 tropical depressions declared officially or unofficially, of which 30 officially became named storms; of those, 20 reached typhoon status, while 3 further became super typhoons by having winds of at least 240 km/h (150 mph). Throughout the year, storms were responsible for at least 997 fatalities and $377.6 million in damage; however, a complete record of their effects is unavailable.
The 1964 Pacific typhoon season was the most active tropical cyclone season recorded globally, with a total of 39 tropical storms forming. It had no official bounds; it ran year-round in 1964, 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 1961 Pacific typhoon season had no official bounds; it ran year-round in 1961, 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 1945 Pacific typhoon season was the first official season to be included in the West Pacific typhoon database. It was also the first season to name storms. It has no official bounds; it ran year-round in 1945, 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.
Typhoon Joan was the longest-lasting super typhoon at the time, maintaining 1-minute maximum sustained winds of at least 240 km/h (150 mph) for 4.5 days. Joan, concurrently with Typhoon Ivan to its west, also became the strongest typhoons at the same time in the northwest Pacific Ocean. The 25th named storm during the hyperactive 1997 Pacific typhoon season, Joan developed from the same trough as Typhoon Ivan on October 11. It moved northwestward and later to the west, undergoing explosive deepening to its peak intensity on October 15. One typhoon warning agency estimated that Joan was among the strongest storms on record in the basin, and that Ivan and Joan marked the first occurrence of simultaneous super typhoons. While near peak intensity, Joan passed between Anatahan and Saipan in the Northern Marianas Islands. Later, the typhoon weakened and turned to the north and east, becoming extratropical on October 24.
Typhoon Carmen was a powerful tropical cyclone that was the ninth of eleven super typhoons to occur during the 1965 Pacific typhoon season. Originating as a tropical depression on October 1, the system tracked northwestward, before it had intensify into a tropical storm two days later. Carmen was later upgraded to a typhoon on October 3, before forming an eye while moving northward. Carmen underwent rapid intensification into a super typhoon in the vicinity of Agrihan on October 6, as its center passed above the island of Pagan, where powerful winds of 150 knots from the storm were recorded. The storm held onto this intensity until it began weakening from cold air on October 9. Carmen quickly shifted northeastward, before transitioning into an extratropical cyclone on the same day. Carmen later dissipated over southeastern Alaska on October 15.
The 1940 Pacific typhoon season marked an interruption in meteorological records in both the Philippines and Hong Kong due to the start of World War II. There were 43 reported tropical cyclones, including 27 that attained typhoon status. The first storm was observed in February, and the first typhoon formed two months later, killing three people along Mindanao. Several storms formed in June and July, including reports of a typhoon in the newspapers that killed 52 in South Korea, and another typhoon reported in newspapers that killed one person on Samar after dropping heavy rainfall. The strongest typhoon of the season originated in July and attained a minimum pressure of 927 mbar (27.4 inHg), as reported by a ship northeast of the Philippines.