The 2006 Pacific typhoon season was a below-average season that produced a total of 23 named storms, 15 typhoons, and six super typhoons. The season ran throughout 2006, though most tropical cyclones typically develop between May and October. The season's first named storm, Chanchu, developed on May 9, while the season's last named storm, Trami, dissipated on December 20.
The 2007 Pacific typhoon season was a below 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 2003 Pacific typhoon season was a slightly below average yearlong period of tropical cyclogenesis exhibiting the development of 45 tropical depressions, of which 21 became named storms; of those, 14 became typhoons. Though every month with the exception of February and March featured tropical activity, most storms developed from May through October. During the season, tropical cyclones affected the Philippines, Japan, China, the Korean Peninsula, Indochina, and various islands in the western Pacific.
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 one of the highest ACE of any season worldwide, with over 400 units. 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 the fourth and final consecutive year with below-average activity, making it the lowest four-year period of activity since 1976–1979, due to the presence of a strong La Niña that had persisted from 1998 to 2001. The season produced twenty-five named storms, sixteen typhoons and three super typhoons. It ran year-round in 2001, with most tropical cyclones in the northwestern Pacific Ocean tending between May and November.
The 1999 Pacific typhoon season was the last Pacific typhoon season to use English names as storm names. It was a very inactive season, featuring the lowest number of typhoons on record, five. It had no official bounds; it ran year-round in 1999, 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.
The 1988 Pacific typhoon season had no official bounds; it ran year-round in 1988, 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. Tropical Storms 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 has no official bounds; it ran year-round in 1987, 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. Tropical storms 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.
Super Typhoon Kent, known in the Philippines as Typhoon Gening, was a powerful Category 4-equivalent typhoon that formed in late August during the 1995 Pacific typhoon season.
Severe Tropical Storm Kammuri, known in the Philippines as Tropical Storm Julian, was a storm which made landfall on south China in August 2008, having a maximum wind speed of 50 kn (93 km/h). The name Kammuri was submitted to the World Meteorological Organisation's Typhoon Committee by Japan and is Japanese for the Corona Borealis constellation of stars.
Typhoon Pabuk, known in the Philippines as Tropical Storm Chedeng, was a minimal typhoon that formed on August 5, 2007. The system made landfall on Taiwan on August 7, and on August 9 Pabuk passed to the south of Hong Kong.
The 2017 Pacific typhoon season was a below-average season in terms of accumulated cyclone energy and the number of typhoons and super typhoons, and the first since the 1977 season to not produce a Category 5-equivalent typhoon on the Saffir–Simpson scale. The season produced a total of 27 named storms, 11 typhoons, and only two super typhoons, making it an average season in terms of storm numbers. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season runs throughout 2017, though most tropical cyclones typically develop between May and October. The season's first named storm, Muifa, developed on April 25, while the season's last named storm, Tembin, dissipated on December 26. This season also featured the latest occurrence of the first typhoon of the year since 1998, with Noru reaching this intensity on July 23.
Tropical Storm Toraji was a short-lived and minimal tropical cyclone that brought inundating rainfall to areas of Southeast Asia in July 2007. The name Toraji was contributed to the western Pacific typhoon naming list by North Korea and stands for a broad bell flower. The third named storm of the annual typhoon season, Toraji developed from an area of disturbed weather within the South China Sea on July 4. As a result of its northwesterly track, the tropical depression moved over Hainan shortly after tropical cyclogenesis. Upon its emergence into the Gulf of Tonkin on July 5, Toraji quickly intensified into a tropical storm with winds of 65 km/h (40 mph); this would be the tropical cyclone's peak intensity for its entire duration. However, the JMA indicated that tropical storm intensity had been reached a day earlier. On the evening of July 5, Toraji made its final landfall on Dongxing, Guangxi before rapidly deteriorating inland and degenerating into a remnant low-pressure area by the following day.
Typhoon Sally, known in the Philippines as Typhoon Maring was an intense tropical cyclone that caused widespread damage across southeastern Asia, particularly in China, in September 1996. Forming well east of the Philippines on September 5, Sally quickly intensified as it tracked westward within favorable conditions. The system reached tropical storm intensity several hours after tropical cyclogenesis was completed, and strengthened further into typhoon intensity the following day. On September 7, Sally reached super typhoon status shortly before attaining its peak intensity with maximum sustained winds of 260 km/h (160 mph) and a barometric pressure of 940 mbar. Quickly moving across the South China Sea, Sally substantially weakened but remained a strong typhoon before making its first landfall on the Leizhou Peninsula on September 9. The tropical cyclone's trek brought it briefly over the Gulf of Tonkin before making a final landfall near the border of China and Vietnam. The typhoon rapidly deteriorated inland and dissipated later that day.
Tropical Storm Morakot, known in the Philippines as Tropical Storm Juaning, brought significant rainfall to Taiwan before alleviating drought conditions in mainland China in August 2003. The tenth named storm in the western Pacific that year, Morakot spawned from an area of disturbed weather in the Philippine Sea on July 31. Tracking northwest, favorable conditions allowed for the intensification of the system to tropical storm strength on August 2. Morakot reached peak intensity later that day with winds of 85 km/h (50 mph) and a minimum barometric pressure of 992 mbar. This intensity was held for several hours until less conducive atmospheric conditions slightly weakened the system; this was followed by Morakot making landfall on southern Taiwan on August 3. Subsequently, the storm weakened and moved into the Taiwan Strait before making its final landfall near Quanzhou, China the next day. The storm quickly weakened over the Chinese mainland, and dissipated entirely several hours after landfall.
Typhoon Krovanh, known in the Philippines as Typhoon Niña, was a moderate tropical cyclone that caused a swath of damage stretching from the Philippines to Vietnam in August 2003. The fifteenth named storm and sixth typhoon in the western Pacific that year, Krovanh originated from a tropical disturbance within the monsoon trough on August 13. Despite rather favorable conditions, the initial tropical depression did not intensify significantly and degenerated into a remnant low on August 18. However, these remnants were able to reorganize and the system was reclassified as a tropical cyclone a day later. Intensification was rather rapid upon the storm's reformation – the depression reached tropical storm status on August 20 and then typhoon intensity two days later. Shortly after, Krovanh made landfall on Luzon at peak intensity with winds of 120 km/h (75 mph). The typhoon emerged into the South China Sea as a much weaker tropical storm, though it was able to restrengthen over warm waters. Once again at typhoon intensity, Krovanh clipped Haiyan before moving over the Leizhou Peninsula on its way to a final landfall near Cẩm Phả, Vietnam on August 25. Quick weakening due to land interaction occurred as Krovanh moved across northern Vietnam, where the storm met its demise the following day.
Typhoon Kim, known in the Philippines as Typhoon Osang, was the second typhoon in a week to directly affect the Philippines during July 1980. Like Typhoon Joe, Kim formed from the near equatorial monsoon trough in the northwestern Pacific Ocean on July 19. The disturbance tracked quickly westward-northwest underneath a subtropical ridge, reaching tropical storm strength on the July 21 and typhoon strength on July 23. After developing an eye, Kim began to rapidly intensify, and during the afternoon of July 24, peaked in intensity as a super typhoon. Several hours later, Kim made landfall over the Philippines, but the storm had weakened considerably by this time. Throughout the Philippines, 40 people were killed, 2 via drownings, and 19,000 others were directly affected. A total of 12,000 homes were destroyed and 5,000 villages were flooded. Less than a week earlier, the same areas were affected by Joe; however, Kim was considered the more damaging of the two typhoons. Land interaction took its toll on Kim, and upon entering the South China Sea, the storm was down below typhoon intensity. Kim continued northwestward but its disrupted circulation prevented re-intensification, and it remained a tropical storm until hitting southern China July 27 to the northeast of Hong Kong, where only slight damage was reported. Later that day, Kim dissipated.
Severe Tropical Storm Utor, known in the Philippines as Typhoon Feria, was a large and deadly system that caused heavy rains and landslides throughout the Philippines, Taiwan, and China. The eighth tropical depression and fourth named storm of the 2001 Pacific typhoon season, Utor formed on July 1 and intensified into a tropical storm shortly after. Utor was upgraded to a typhoon by the JTWC on July 3, and a day later, Utor was estimated to have peaked with 10-min winds of 110 km/h (70 mph), with the JTWC estimating 1-min winds of 150 km/h (95 mph). After passing just north of Luzon, Utor began to weaken, before making landfall on the district of Dapeng as a minimal typhoon. Utor caused 203 deaths, of which 168 were in the Philippines, 23 were in the province of Guangdong, 10 were in the province of Guangxi, and 2 were in Taiwan. Total damages from the storm amounted to $2.78 billion.
Severe Tropical Storm Durian was a deadly system that caused severe impacts in China and Vietnam. The seventh tropical depression and third named storm of the 2001 Pacific typhoon season, the storm was first noted on June 29 and quickly intensified into a tropical storm and given the name Durian by the Japan Meteorological Agency (JMA). Durian continued northwestward before intensifying into a severe tropical storm as it approached the Chinese coast. On July 1 just before landfall, Durian peaked in intensity, with the JMA estimating 10-min winds of 110 km/h (68 mph) and the Joint Typhoon Warning Center (JTWC) estimating 1-min winds of 140 km/h (87 mph). Durian made landfall on Zhanjiang at peak intensity, before quickly weakening over land and dissipating on July 3 over the mountains of Vietnam.
Typhoon Lola, known in the Philippines as Typhoon Monang, was a deadly typhoon that impacted the Philippines and Indochina. The 47th tropical depression, 26th named storm, and 14th typhoon of the 1993 Pacific typhoon season, the origins of Lola can be traced back to an active near-equatorial trough. The JTWC began monitoring an area of convection on November 27, and on December 1, it developed into a tropical depression. The JMA upgraded the depression to a tropical storm the next day, with the JTWC giving it the name Lola on December 3. 12 hours later, the JMA upgraded Lola to a severe tropical storm. On December 4 at 6:00 UTC, the JTWC upgraded Lola to a typhoon. Shortly after, Lola reached its initial peak intensity, with the JMA assessing that it had peaked with a minimum central pressure of 955 hPa; Lola made landfall near the municipality of Vinzons on December 5 at 12:00 UTC. After making landfall, Lola weakened to a tropical storm as it emerged over the South China Sea on December 6, before re-strengthening into a typhoon. After strengthening into a typhoon, Lola began to quickly intensify, reaching its peak intensity with 1-min winds of 195 km/h (120 mph) on December 8 at 12:00 UTC. Lola weakened slightly before making its final landfall near the city of Camh Ranh as a Category 2-equivalent storm. Lola quickly weakened over land, dissipating on December 9.
