The 1992 Pacific typhoon season was 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.[1] These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
In the West Pacific basin, tropical depressions have the "W" suffix added to their number. Storms reaching tropical storm intensity of 34kn (63km/h) sustained winds were assigned a name by the Joint Typhoon Warning Center (JTWC). Storms with sustained winds exceeding 64 knots (119km/h) are called typhoons, while intense typhoons with sustained winds exceeding 130 knots (240km/h) are designated super typhoons by the JTWC (see tropical cyclone scales).
There were a total of 40 tropical cyclones in the Western Pacific in 1992. 39 of these formed within the basin, and 1 storm, Tropical Storm Ekeka, formed in the Central Pacific basin, crossing the Date Line to enter the Western Pacific. Out of the 39, 32 became named tropical storms, 21 reached typhoon intensity, and 5 reached super typhoon strength. Storms are listed in numerical ascending order by their JTWC tropical depression numbers except for Ekeka, and not in alphabetical order of names. Thus, Tropical Storm Zack (22W) is listed before Super Typhoon Yvette (23W).
The season was hyperactive, featuring the highest Accumulated Cyclone Energy (ACE) for a Pacific typhoon season on record at the time, until it was surpassed by the 1997 Pacific typhoon season. The ACE index for the 1992 Pacific typhoon season as calculated by Colorado State University using data from the Joint Typhoon Warning Center was 470.1units.[3] Broadly speaking, ACE is a measure of the power of a tropical or subtropical storm multiplied by the length of time it existed. It is only calculated for full advisories on specific tropical and subtropical systems reaching or exceeding wind speeds of 39 miles per hour (63km/h).
On 2 January, stronger-than-normal low-level westerlies were observed east of New Guinea. As a result of these increased winds and an area of cloudiness, two areas of convection on different sides of the equator formed. The next day, these areas began consolidating.[4] As a result, on 4 January, the Japan Meteorological Agency (JMA) noted that the northern area of convection had developed into a tropical depression.[5] Several hours later, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert (TCFA) on the depression, issuing their first warning on Tropical Depression 01W later that day.[4] Early on 6 January, both the JTWC and JMA had noted that the tropical depression had intensified into a tropical storm,[5][4] causing the former agency to name it Axel.[4]
As a result of favorable upper-level divergence, Axel was able to significantly intensify,[4] with the JMA noting that the cyclone had developed into a severe tropical storm the next day.[5] Despite the JMA stating that Axel did not develop further until 9 January,[5] later that day, the JTWC noted that Axel had intensified into a typhoon.[4] Soon after, they noted that Axel had peaked with 1-minute sustained winds of 65mph (100km/h)[4] while the JMA stated that Axel had peaked with 10-minute sustained winds of 80mph (130km/h).[5] However, on 10 January, Axel tracked into an environment with high wind shear, causing it to weaken.[4] As a result, three days later, both the JMA and JTWC noted that Axel had weakened into a tropical depression.[4][5] Two days later, Axel had transitioned into a weak extratropical low, causing both agencies to stop tracking it.[4][5]
The worst typhoon to affect the Marshall Islands in over 70 years, waves produced by Axel flooded homes and cars while gusts amounting to 100mph (160km/h) destroyed scores of houses, submerging houses and cars in knee-deep water and leaving hundreds homeless.[6] After passing Majuro, Axel passed across Jaluit Atoll, causing over four feet of water to cover most of the main islands. As a result of Axel's winds, a majority of the outhouses were destroyed, resulting in serious health concerns for the islanders. In the eastern Caroline Islands, Kosrae experienced gusts of 75–90mph (120–150km/h) resulting in severe crop losses, damaged fauna, and several structures being destroyed.As Axel passed just north of Pohnpei, the island’s electrical power was knocked out for several hours and many buildings in low-lying areas flooded. In those islands, a storm surge of fifteen feet was recorded, with a daily total of 9.73in (247mm) of rain seen.[4]
On 3 February, a weakening Tropical Storm Ekeka tracked west of the International Date Line, entering the West Pacific basin and being monitored by the JMA.[5] Early the next day, the JTWC began issuing bulletins on Ekeka, which was in an environment with high wind shear.[7] Later that same day, Ekeka weakened into a tropical depression.[5][7] Several days later, on 8 February, the JMA stopped tracking the depression.[5] The JTWC kept tracking Ekeka for a few hours until it passed over Chuuk.[7] Early on February 9, Ekeka finally dissipated about 800 miles (1,300km) east-southeast of Palau, or about 310 miles (500km) off the north coast of Papua New Guinea.[8]
On 20 June, a poorly organized area of convection south of Guam near the central Caroline Islands began developing. Embedded in the monsoon trough, the disturbance's circulation began consolidating, prompting the JTWC to issue a TCFA on the disturbance.[9] As a result, on 23 June, the JMA noted that the disturbance had developed into a tropical depression.[5][9] Around that time, the JTWC also upgraded the disturbance into a depression, issuing their first warning on Tropical Depression 02W later that day.[9] Intensifying, early on 24 June, both the JTWC and JMA noted Bobbie intensified into a tropical storm, causing the latter agency to name it Bobbie.[9][5] Just a few hours later, Bobbie began undergoing a binary interaction with nearby Tropical Storm Chuck, which at the time, just formed off the Philippines.[9] As Bobbie was intensifying, it crossed into the Philippine Area of Responsibility (PAR), prompting the Philippine Atmospheric, Geophysical, and Astronomical Services Administration (PAGSA) to name it Asiang.[10]
Early the next day, Bobbie intensified into a severe tropical storm.[9] At that time, the JTWC claimed that Bobbie had intensified into a typhoon,[9] while the JMA noted that Bobbie had actually became a typhoon several hours later.[5] On 18:00 UTC on 26 June, Bobbie peaked with 1-minute sustained winds of 140mph (220km/h) as it tracked the western extent of the mid-level subtropical ridge.[9] Several hours later, Bobbie peaked with 10-minute sustained winds of 105mph (165km/h).[5] As Bobbie began recurving east of Taiwan at 12:00 UTC that day, increasing southwesterly winds caused Bobbie to steadily weaken. Passing over Miyako Jima on 28 June and then just southeast of Okinawa on 29 June, Bobbie began undergoing an extratropical transition on at that time.[9] At that time, Bobbie weakened into a severe tropical storm as it left the PAR, causing PAGASA to stop issuing advisories on the storm.[9] As Bobbie transitioned into an extratropical storm, the JTWC issued their final warning on the system the next day, prior to it brushing the southern tip of Honshu.[9] The JMA noted that Bobbie became extratropical early the next day, prior to it dissipating on 3 July.[5]
Bobbie would primarily bring beneficial rainfall to Luzon, as mostly light showers had persevered over the region.[11] However, combined with the effects of nearby Chuck, heavy rainfall would produce mudflows pouring down the Bucao, Balinquero and Maraunot rivers, causing them to rise up 6ft (1.8m).[12] In Manila, 23 homes were destroyed while 2 people went missing.[13] In Japan, Bobbie primarily brought severe rainfall, causing the prefectures of Okinawa, Miyazaki, Kagoshima, Tokyo, Gifu, and Fukui to receive heavy rainfall. Yakushima received 178mm (7.0in) in a day.[14]
On 19:00 UTC on 21 June, a tropical disturbance began developing over the central Philippines.[15] Initially weakening as it traversed the Philippines, once it crossed into the South China Sea two days later, the convection of the disturbance began organizing.[16][15] As a result, on 24 June, the JMA noted that the disturbance had developed into a tropical depression.[5] As it kept consolidating, the JTWC issued a TCFA on the disturbance later that day, issuing their first warning on it the next day as Tropical Depression 03W.[15] Several hours later, the JMA noted that Chuck had intensified into a tropical storm,[5] causing the JTWC to name it Chuck around 12 hours later.[15]
Steadily intensifying, on 27 June, both the JTWC and JMA noted that Chuck had become a typhoon.[5][15] As a result, the JMA stated that Chuck peaked with 10-minute sustained winds of 80mph (130km/h) around that time.[15] Just a few hours later, early on 28 June, the JTWC stated that Chuck peaked with 1-minute sustained winds of 90mph (150km/h).[15] Later that day, Chuck made landfall along the southern tip of Hainan island as a minimal typhoon.[15] Weakening into a tropical storm as it crossed into the Gulf of Tonkin,[15][5] Chuck made its second landfall around 100mi (160km) east-southeast of Hanoi early on 29 June.[16][15] As a result of this, Chuck rapidly weakened, causing the JTWC to stop tracking it on 1 July.[15] The JMA kept tracking Chuck until it dissipated two days later.[5]
In Vietnam, at least 21 people died and while 80 were reported missing.[15] Intense winds uprooted over 500 trees, downed electrical cables and damaged about 140 houses in Hanoi. As a result of the storm, in the capital alone, three people were killed while another three were injured. Massive waves engulfed several coastal fishing villages in Cát Hải district, with seven people being missing there.[17] Elsewhere, in Hainan, one person died.[16] In the Philippines, combined with the effects of nearby Bobbie, heavy rainfall would produce mudflows in the Philippines. These poured down the Bucao, Balinquero and Maraunot rivers, causing them to rise up 6ft (1.8m).[12]
On 25 June, the Joint Typhoon Warning Center (JTWC) began tracking a tropical disturbance over the open Pacific. On 6:00 UTC the next day, they issued a TCFA on the consolidating system, later issuing their first advisory on it just a few hours later as Tropical Depression 04W.[18] Initially, the depression was slow to consolidate due to wind shear produced by a nearby Typhoon Bobby alongside a tropical upper tropospheric trough (TUTT). This hindered much development of the depression's convection, causing it to not intensify into a tropical storm until 1 July. As a result of it becoming a tropical storm, the JTWC named it Deanna. Slowly developing, the next day, Deanna peaked with 1-minute sustained winds of 45mph (75km/h).[18] Accelerating towards the northeast, Deanna weakened into a depression around 700km (380NM) east-northeast of Okinawa.[19] As Deanna tracked northwards, it dissipated on 3 July.[18] Despite that, the remnants of Dianna tracked towards Japan, prior to becoming extratropical the next day.[19]
In the Philippines, Deanna, known there as Biring, would prompt PAGASA to issue PSWS #1 for Batanes and Cagayan.[20] Additionally, the remnants of Deanna produced moderate to heavy rainfall in the Ryukyu Islands and Southern Japan.[21]
One person was killed and eight others were reported missing when the storm moved through the Philippines. Extensive damage took place in China with losses amounting to $235million.
Typhoon Irving caused over $4 million in damages and 3 fatalities. The storm formed south of Japan and moved north. Then, it recurved west and moved towards South Korea and dissipated.
Kent formed on August 5 in the Federated States of Micronesia. Then, it tracked northwest and was intensified into a tropical storm. Then, it was upgraded into a category 1 typhoon. A few days later, the JTWC upgraded Kent into a category 2 typhoon. Then, Kent intensified into a category 3 then to a category 4 typhoon. Kent reached its peak intensity as a super typhoon. Afterwards, Kent moved very slowly. Then, the JTWC downgraded Kent into a category 4 typhoon then to a category 3 typhoon. Kent still moved slowly. Afterwards, the JTWC downgraded Kent into a category 2 typhoon. However, it still moved slowly until it was downgraded into a category 1 typhoon. Afterwards, the JTWC downgraded Kent into a tropical storm. Kent moved northeastwards then affected Japan. After it affected Japan, it weakened into a tropical depression then dissipated on the Sea of Japan.
When Kent was traveling towards Japan, its large waves swept five people on the sea. Overall, Kent caused five deaths.
Typhoon Omar originated into a tropical disturbance on August 20. On those days, the basin saw the dissipation of 2 tropical cyclones and another two more cyclones that begin their extratropical transition. The system intensified, prompting JMA and JTWC to name the Tropical depression 15W. 15W tracked westward, and it intensified to a tropical storm then was named Omar by the JMA. Omar begin to track westward, causing the outflow of Tropical Storm Polly to shear the system and slowing intensification. Then JTWC noticed that the wind shear can weaken Omar. The two storms furthered apart, allowing a ridge to develop between them. This caused Omar to drift slowly on the north, and because of the decreasing wind shear, Omar resumed strengthening. The storm later resumed its west-northwest track. On August 27, JTWC designed the storm as a typhoon, developing an eye. On August 28, Omar rapidly intensified and it made landfall on Guam with maximum sustained winds with 195km/h (121mph). On August 29, the storm reached its peak intensity with 10 min. sustained winds of 185km/h (115mph) and the lowest pressure of 920 mbar. This intensity remained for 24 hours before it weakened. However, JTWC estimated 1 min. winds at 240km/h (150mph). Two days later, Omar entered the PAR and PAGASA assigned the local name Lusing. On September 3, Omar weakened into a tropical storm by JMA, but JTWC maintained the storm at the typhoon strength. The storm still tracked westward, then made landfall on east coast of Taiwan. Then it made its final landfall near Fujian in Eastern China on September 5. Then it degenerated to a tropical depression before turning west-southwest. Then it moved on southern China as a weak system, dissipating on September 9 on northern Vietnam.
Typhoon Omar was a destructive storm to Guam, causing over a foot of rain there, amounting to $702 million in damage (2008 USD) and a death. In Taiwan, the storm caused 2 deaths and heavy rainfall, which warranted the name's retirement. The name Omar was replaced with Oscar which was first used in the 1995 season.
Developing to Omar's west, Polly began its life on August 23 and reached tropical storm strength on the 26th. As a developing monsoon depression, it had a large outflow. Polly retained that throughout its lifetime, inhibiting intensification past 60mph (97km/h) winds. On the 30th, the storm hit southeastern Taiwan, and on the 31st it hit China.
Torrential rains produced by Tropical Storm Polly triggered devastating floods that killed 202 people and injured hundreds more. More than 5million people were left homeless across Fujian and Zhejiang Provinces in China. Total losses from the storm were roughly $450million.
Typhoon Sibyl took an unusual track east of Japan, first heading northward, then back south, and finally north again while strengthening. Then, it curved west and dissipated as it recurved eastward.
Tropical Storm Ted, having developed on September 14, stalled off northern Luzon on the 20th. It turned northward, and hit southern Taiwan on the 22nd as a minimal typhoon. Ted weakened to a tropical storm over the island, and hit eastern China on the 23rd. It turned to the northeast, hit South Korea, and became extratropical on the 24th.
At least 61 people were killed by Typhoon Ted and 51 others were reported missing. Losses from the storm reached $360million in China.
On September23, a tropical depression developed just east of the International Dateline; however, it was warned upon by the Joint Typhoon Warning Center rather than the Central Pacific Hurricane Center as it was expected to become a significant tropical cyclone outside of the CPHC's area of responsibility. Just prior to crossing into the Western Pacific basin, it reached tropical storm intensity, at which time it was given the name Ward from the list of Pacific typhoon names. Winds at this time were estimated at 40mph (64km/h);[22] the Japan Meteorological Agency reported the system to have also attained a pressure of 1,002mbar (1,002hPa; 29.6inHg).[23] Over the following days, Ward gradually intensified, peaking as a Category2 storm with winds of 110mph (180km/h). The storm eventually weakened as it moved through higher latitudes, becoming extratropical on October7 over open waters.[22]
A depression that formed near the Mariana Islands organized and was upgraded into a tropical storm on October 7, and was given the name Yvette. It rapidly intensified into a super typhoon which started to recurve out at sea, preventing major impacts at the Philippines. Yvette started to weaken as it headed towards colder waters and eventually dissipated on October 17.
At least 49 people were killed by Typhoon Angela, mostly in Vietnam, while 14 others were reported missing. In the history of Vietnam's list of storm numbers in the East Sea, this storm is a rare storm. When it was re-issued twice, the number were 6 and 8. The thing is, when storm number 6 made landfall in Central Vietnam, it weakened into a tropical depression and its remnants strengthened in the Gulf of Thailand into storm number 8. This is also a rare time when two storms are active at the same time because of storm Colleen below entering the East Sea area.
On October 30, a tropical disturbance began to form west of the International Date Line. The JTWC then issued a Tropical Cyclone Formation Alert late the next day as the system moved westward and started warnings on Tropical Depression 29W on November 1. However, intensification was severely inhibited by outflow from nearby Typhoon Dan, and the depression failed to develop. It passed within 30 nautical miles (56 kilometres) of Wake Island, causing a minor pressure dip and gusts to 32kn (60km/h). No damage was reported, due to the relative weakness of 29W as compared to Dan, which ravaged the island 3days earlier. The depression dissipated on November 2 over open ocean.[24]
On November 8 a tropical depression formed from the monsoon trough east of the Philippines. It crossed the islands, and strengthened to a tropical storm in the South China Sea on the 12th. Forrest continued westward until hitting and crossing the Malay Peninsula on the 15th. It reached a peak of 145mph (233km/h) winds in the Bay of Bengal before hitting Myanmar on the 21st.
At least two people were killed by Tropical Storm Forrest and 31 others were reported missing after a ship capsized.
Typhoon Gay was the strongest and longest-lasting storm of the season, forming on November13 near the International Date Line. As it moved to the west, Gay steadily intensified and moved through the Marshall Islands as an intensifying typhoon. After passing through the country, it intensified its peak intensity over open waters. The JTWC estimated peak winds of 295km/h (183mph) and a minimum barometric pressure of 872mb (25.8inHg). However, the Japan Meteorological Agency (JMA), which is the official warning center in the western Pacific, estimated winds of 205km/h (127mph), with a pressure of 900mbar (27inHg). Typhoon Gay weakened rapidly after peaking due to interaction with another typhoon, and it struck Guam with winds of 160km/h (99mph) on November23. The typhoon briefly re-intensified, although it weakened as it turned toward Japan and became extratropical on November29.[25][26]
The typhoon first affected the Marshall Islands, where 5,000people were left homeless and heavy crop damage was reported. The nation's capital of Majuro lost power during the storm and experienced power and water outages. No Marshall Islands citizens were killed,[25] although the typhoon killed a sailor who was traveling around the world.[27] When Gay struck Guam, it became the sixth typhoon of the year to affect the island. Most of the weaker structures were destroyed during Typhoon Omar earlier in the year. Due to its substantial weakening, Gay had a disrupted inner-core that dropped minimal rainfall, which caused extensive defoliation of plants due to salt water scorching. Further north, the typhoon destroyed a house on Saipan from high waves.[25]
During the season 31 named tropical cyclones developed in the Western Pacific and were named by the Joint Typhoon Warning Center, when it was determined that they had become tropical storms. These names were contributed to a revised list which started on mid-1989.
Axel
Bobbie
Chuck
Deanna
Eli
Faye
Gary
Helen
Irving
Janis
Kent
Lois
Mark
Nina
Omar
Polly
Ryan
Sibyl
Ted
Val
Ward
Yvette
Zack
Angela
Brian
Colleen
Dan
Elsie
Forrest
Gay
Hunt
Philippines
Asiang
Biring
Konsing
Ditang
Edeng
Gloring
Huaning
Isang
Lusing
Maring
Ningning
Osang
Paring
Reming
Seniang
Toyang(unused)
Ulpiang(unused)
Welpring(unused)
Yerling(unused)
Auxiliary list
Apiang(unused)
Basiang(unused)
Kayang(unused)
Dorang(unused)
Enang(unused)
Grasing(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 6 of which are published each year before the season starts. Names not retired from this list will be used again in the 1996 season. This is the same list used for the 1988 season, except for Ulpiang and Yerling, which replaced Unsang and Yoning. 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.). Names that were not assigned/going to use are marked in gray.
Retirement
Due to extensive damage caused by Omar in Guam, the name was later retired and was replaced by Oscar and was first used in the 1995 season.
Season effects
This table summarizes all the systems that developed within or moved into the North Pacific Ocean, to the west of the International Date Line during 1992. The tables also provide an overview of a systems intensity, duration, land areas affected and any deaths or damages associated with the system.
The 2007 Pacific typhoon season was a near average season which featured 24 named storms, fourteen typhoons, and five 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 2007, though most tropical cyclones typically develop between May and November. The season's first named storm, Kong-rey, developed on March 30, while the season's last named storm, Mitag, dissipated on November 27. The season's first typhoon, Yutu, reached typhoon status on May 18, and became the first super typhoon of the year on the next day.
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 22.
The 2002 Pacific typhoon season was a slightly above average Pacific typhoon season, producing twenty-six named storms, fifteen becoming typhoons, and eight super typhoons. It had an ACE over 400 units, making it one of the most active seasons worldwide. 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 2002, though most tropical cyclones typically develop between May and October. The season's first named storm, Tapah, developed on January 11, while the season's last named storm, Pongsona, dissipated on December 11. The season's first typhoon, Mitag, reached typhoon status on March 1, and became the first super typhoon of the year four days later.
The 2001 Pacific typhoon season was an average season with twenty-six named storms, sixteen typhoons and three super typhoons, with a near normal Accumulated Cyclone Energy (ACE) of 307.3 units. It ran year-round in 2001, with most tropical cyclones in the northwestern Pacific Ocean tending between May and November.
The 1988 Pacific typhoon season was a very active season in terms of named storms, though it only featured 11 typhoons and 1 super typhoon. It had no official bounds; it ran year-round in 1988, but most tropical cyclones formed between May and November. Tropical storms that formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. 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 1987 Pacific typhoon season was a below average season, though it featured a relatively high amount of typhoons. It had no official bounds; it ran year-round in 1987, but most tropical cyclones formed between May and November. Tropical storms that formed in the entire basin were assigned a name by the Joint Typhoon Warning Center. 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 1980 Pacific typhoon season was a slightly-below average season when compared to the long-term average, though it featured several intense storms. It ran year-round in 1980, but most tropical cyclones formed between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. A total of 28 tropical depressions formed this year in the Western Pacific, of which 24 became tropical storms and were assigned a name by the Joint Typhoon Warning Center. Beginning in March, tropical cyclones formed in each subsequent month through December. Of the 24 named storms, 15 storms reached typhoon intensity, of which 2 reached super typhoon strength.
The 2008 Pacific typhoon season was a below average season which featured 22 named storms, eleven typhoons, and two super typhoons. The season had no official bounds; it ran year-round in 2008, but 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.
Typhoon Isa was the first of a record eleven super typhoons to occur during the 1997 Pacific typhoon season. The second tropical cyclone of the season, Isa developed from a disturbance in the monsoon trough near the Caroline Islands on April 12. It moved erratically at first, though after attaining tropical storm status it curved westward due to the subtropical ridge to its north. Isa very gradually intensified, and on April 20 the typhoon reached peak 1-min winds of 270 km/h (170 mph), as reported by the Joint Typhoon Warning Center; Japan Meteorological Agency reported maximum 10-min winds of 155 km/h (95 mph). After turning northward, it accelerated to the northeast, and merged with a larger extratropical cyclone on April 24.
This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation during the 2008 Pacific typhoon season. The 2008 Pacific typhoon season officially started on January 1, 2008 and ended on January 1, 2009.
Typhoon Dolphin, known in the Philippines as Typhoon Ulysses, was the final named storm and typhoon of the 2008 Pacific typhoon season. The only impact that was reported from Dolphin was to the M/Bca Mae Jan, which was a cargo passenger ship which sank on December 14, due to rough seas caused by Dolphin. There were 46 people reported dead while seven were reported as missing.
Typhoon Yagi was an intense typhoon, the strongest of the 2006 Pacific typhoon season, which reached the equivalence of Category 5 on the Saffir–Simpson scale. Forming out of a tropical depression on September 16, Yagi quickly strengthened as it executed a slow clockwise loop over the open waters of the western Pacific Ocean. On September 19, Yagi strengthened into a typhoon as a subtropical ridge steered the storm towards the west. Two days later, the storm reached its peak intensity with winds of 195 km/h (121 mph) 10-minute winds with a minimum pressure of 910 hPa (mbar). The typhoon gradually weakened as it recurved towards the northeast and was downgraded to a severe tropical storm on September 24 and became extratropical the next day. The storm was last noted near the Aleutian Islands on September 27. The typhoon caused severe damage on the island of Chichijima but no injuries were reported as a result of the storm.
Typhoon Melor, known in the Philippines as Super Typhoon Quedan, was a powerful typhoon that hit Japan in early October 2009, causing significant damage. As part of the 2009 Pacific typhoon season, Melor formed as a tropical depression on September 29 and rapidly intensified into a Category 4-equivalent typhoon just three days later. Subsequently, on October 4, Melor became the second Category 5-equivalent super typhoon to form in the season. During the next days, the typhoon would interact with Typhoon Parma southeast of Taiwan, causing Parma to be almost stationary over northern Luzon and drop near-records of rainfall there. Afterwards, Melor gradually weakened in its approach to Japan, making landfall on October 7. As the storm exited Japan during the next day, it transitioned into an extratropical cyclone. The remnants of Melor were absorbed by a newly-formed extratropical cyclone near Alaska, which strengthened significantly and impacted the West Coast of the United States on October 13.
The 2011 Pacific typhoon season was a below average season that produced a total of 21 named storms, 8 typhoons, and four super typhoons. This season was much more active than the previous season, although both seasons were below the Pacific typhoon average of 26. The season ran throughout 2011, though most tropical cyclone tend to develop between May and October. The season's first named storm, Aere, developed on May 7 while the season's last named storm, Washi dissipated on December 19.
Typhoon Gay, known in the Philippines as Typhoon Seniang, was the strongest and longest-lasting storm of the 1992 Pacific typhoon season and most intense globally in 1992. It formed on November 14 near the International Date Line from a monsoon trough, which also spawned two other systems. Typhoon Gay later moved through the Marshall Islands as an intensifying typhoon, and after passing through the country it reached its peak intensity over open waters. The Joint Typhoon Warning Center (JTWC) estimated peak winds of 295 km/h (183 mph) and a minimum barometric pressure of 872 mb (25.8 inHg). However, the Japan Meteorological Agency (JMA), which is the official warning center in the western Pacific, estimated winds of 205 km/h (127 mph), with a pressure of 900 mbar (27 inHg). Gay weakened rapidly after peaking because of interaction with another typhoon, and it struck Guam with winds of 160 km/h (99 mph) on November 23. The typhoon briefly re-intensified before weakening and becoming extratropical south of Japan on November 30.
Typhoon Yuri was the most intense tropical cyclone in 1991 in terms of minimum central pressure. The nineteenth typhoon and final super typhoon of the 1991 Pacific typhoon season, Yuri was a tropical disturbance that strengthened into a tropical depression on November 22 in the Philippine Sea. Moving rather slowly at first, the system continued to intensify, and was given the name Yuri. It had become a severe tropical storm about 1,480 kilometers east of Truk Island and took on a west-northwestward track at 22 km/h. Typhoon intensity was attained that night when Yuri was 1,050 km. Yuri turned more to the west on 26 November and reached peak intensity the following morning packing winds of over 220 km/h near its centre. Moving northwestwards at 30 km/h, Yuri passed 140 km to the south-southwest of Guam on the evening of November 27. After recurving November 29, Yuri accelerated northeastwards on November 30 and weakened to a severe tropical storm that night. By the morning of December 1, it had degenerated into a tropical storm about a few hundred kilometers east-northeast of Iwo Jima. Extratropical transition was completed soon afterward, and the storm's remnants persisted until December 3.
Most of the tropical cyclones of the 2013 Pacific typhoon season formed between May and November of that year. The scope of this article is the Pacific Ocean north of the equator, between 100°E and the International Date Line. Tropical storms which form in the Western Pacific basin are assigned a name by the Japan Meteorological Agency (JMA). Tropical depressions forming in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center (JTWC). The Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility, but these names are not in common use outside the Philippines.
This timeline documents all of the events of the 2014 Pacific typhoon season. Most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.
Severe Tropical Storm Axel was a moderate tropical storm which affected the Marshall, Caroline, and Mariana islands in January 1992. The first tropical depression and storm of the 1992 Pacific typhoon season, Axel developed from a significant equatorial westerly wind burst east of New Guinea, alongside two other cyclones, Betsy and Mark, in the Southern Hemisphere, intensifying at an abnormally low latitude. By January 9, Axel had peaked as a high-end tropical storm, passing near Kosrae and Pingelap in the eastern Caroline Islands. Soon after, Axel began steadily weakening due to increased wind shear. As a result, just prior of passing south of Guam, Axel weakened into a tropical depression. Recurving northwards soon after, on January 15, Axel transitioned into an extratropical low, dissipating just a few hours later.
Typhoon Bobbie, known in the Philippines as Typhoon Asiang, was an intense typhoon which affected the Philippines and Japan during June 1992. The third tropical depression, storm, and first typhoon of the 1992 Pacific typhoon season, Bobbie developed from a weak area of convection in the monsoon trough. Intensifying as it underwent a binary interaction with nearby Chuck, on 25 June, Bobbie became a typhoon. Further developing as it tracked northwards, two days later, Bobbie peaked as a very strong typhoon. Soon after, Bobbie began weakening as it recurved northeastward, transitioning into an extratropical cyclone on 1 July. It was at this time when Bobbie made its closest approach to Japan, just southeast of Kyushu. The extratropical remnants of the former typhoon persevered until they dissipated on 3 July.
1 2 "1992 Tropical Cyclone Summary for the Western North Pacific Ocean (west of 180 degrees)". BULLETIN(PDF) (3ed.). Hong Kong Meteorological Society. 1993. p.42. Retrieved 28 August 2024.
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