Severe tropical storm (JMA scale) | |
---|---|
Tropical storm (SSHWS) | |
![]() Severe Tropical Storm Faxai at peak intensity on October 27 | |
Formed | October 25, 2007 |
Dissipated | October 29, 2007 |
(Extratropical after October 27, 2007) | |
Highest winds | 10-minute sustained: 100 km/h (65 mph) 1-minute sustained: 75 km/h (45 mph) |
Lowest pressure | 975 hPa (mbar); 28.79 inHg |
Fatalities | 1 direct, 9 injuries |
Damage | $1.5 million (2007 USD) |
Areas affected | Japan |
Part of the 2007 Pacific typhoon season |
Severe Tropical Storm Faxai, known in the Philippines as Tropical Storm Juaning, was a short-lived tropical storm that had minor effects on land. The twentieth named storm of the 2007 Pacific typhoon season, Faxai originated from a tropical depression over the open waters of the western Pacific Ocean in late October. The storm quickly strengthened, becoming a severe tropical storm on October 26 as it rapidly traveled toward the northeast. The storm became extratropical the following day as it brushed Japan. The remnants dissipated on October 28.
Although Faxai never made landfall, outer bands associated with the storm produced torrential rains, amounting to 458 mm (18.0 in) on Miyakejima. A Japan Airlines flight to Narita Airport encountered severe turbulence during the afternoon of October 27. One person sustained serious injuries, and five others received minor injuries; the plane was damaged during the event. One person was killed near Tokyo as the storm passed by, and three others were injured. Damages from the storm amounted to ¥150 million (US$1.5 million).
Tropical Storm Faxai began as an area of convection that persisted about 805 kilometers (500 mi) west of Guam on October 24. Satellite imagery indicated broad cyclonic turning in the lower levels of the atmosphere, and a trough was near the surface. Convection consolidated around the center of the low-level circulation, and the upper-level environment—low wind shear and good divergence—favored development. [1] The following day, the Japan Meteorological Agency (JMA) classified the system as a tropical depression. [2] Shortly after, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert as convection deepened around a partially exposed low. The storm traveled northwest under the influences of a subtropical ridge to the north. [3] At 0000 UTC on October 26, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) designated the system as a tropical depression and gave it the local name Juaning. [4] Around the same time, the JMA upgraded the depression to a tropical storm and gave it the name Faxai. [2]
The JTWC issued advisories on Faxai, designating it as 20W; however, they classified it as a tropical depression. [5] Several hours later, the storm began to undergo an extratropical transition, with convection persisting mainly in the northwestern portion of the storm and cold, dry air entering into the southwestern portion. [6] At 1200 UTC, PAGASA issued their final advisory on Tropical Storm Juaning as it moved out of their area of responsibility. [4] The JTWC reported that Tropical Depression 20W (Faxai) had become extratropical around this time as it merged with a baroclinic zone. A cold front developed along the southern portion of Faxai, a feature of extratropical cyclones. [7] Around that time, the JMA upgraded Faxai to a severe tropical storm with (10-minute sustained) winds of 95 km/h (59 mph). [2]
The JTWC subsequently upgraded the depression to a tropical storm based on the development of a very impactful central dense overcast. A shortwave trough over the Korean peninsula provided a favorable upper-level environment for Faxai to intensify. [8] Early the next day, Faxai began accelerating rapidly towards the northeast in the mid-latitude westerlies. An anticyclone over Japan created a strong pressure gradient between it and the tropical storm, causing the wind field of Faxai to expand significantly to the northeast. As the JTWC issued their final advisory, [9] they assessed the storm to have reached its peak intensity, with (one-minute sustained) winds of 75 km/h (47 mph). [10] The JMA also assessed Faxai to have reached its peak intensity at that time, with (10-minute sustained) winds of 100 km/h (62 mph) and a minimum pressure of 975 hPa (mbar); however, the National Oceanic and Atmospheric Administration (NOAA) reported that Faxai had attained hurricane-force winds by this time, peaking at 130 km/h (81 mph). [11] The storm continued towards the northeast at a rapid pace and became extratropical off the eastern coast of Honshu around 1200 UTC on October 27. The extratropical remnants persisted for more than a day before dissipating over open waters late on October 28. [2] NOAA, on the other hand, continued to monitor the remnants of Faxai, with the system reaching the Aleutian Islands on October 29. The following day, the storm rapidly intensified, with the central pressure dropping to 957 hPa (mbar) by 1800 UTC. On October 31, the system tracked into Alaska and weakened. [11]
The Japan Meteorological Agency uses 10-minute sustained winds, while the Joint Typhoon Warning Center uses one-minute sustained winds. [12] The conversion factor between the two is 1.14. [13] JMA's peak intensity for Faxai was 100 km/h (65 mph) 10-minute sustained, or 120 km/h (75 mph) one-minute sustained. [2] [13] The JTWC's peak intensity for Faxai was 75 km/h (47 mph) one-minute sustained, or 65 km/h (40 mph) 10-minute sustained. [13] [14]
As Faxai approached Japan, All Nippon Airways canceled all of its day[ discuss ] flights between Tokyo and the Izu Islands. Tokai Kisen, which operates ferries between Tokyo, the Izu Islands and Shizuoka Prefecture, canceled some services due to the storm. Areas around Tokyo were warned of the expected heavy rains, waves up to 6 m (20 ft), and high winds. [15] Residents were advised to stay indoors during the storm, especially after sunset, and to avoid possible flying debris. [16]
Although Faxai did not make landfall, the outer bands produced heavy rains, which caused minor damage along the eastern coast of Japan. [17] The highest total rainfall was recorded on Miyakejima at 458 mm (18.0 in) and in the Ōshima Subprefecture of Tokyo, 192 mm (7.6 in) was recorded. [18] The rainfall in Miyakejima nearly surpassed the record daily rainfall for October 27. [19] Rainfall rates peaked at 95 mm/h (3.7 in/h) on Miyaketsubota, [18] which triggered seven mudslides throughout the country. [17] One woman was killed near Tokyo, [20] and three people were injured. One home, two hectares of farmland, 2 km (1.2 mi) of roads, and one ship were damaged by the storm. At the height of the storm, 9,605 residences were without power throughout Japan. Damages from cyclone totaled ¥150 million (US$1.5 million). [17]
At 5:31 pm Japan Standard Time (0831 UTC) on October 27, a Japan Airlines Boeing 767-300 heading to Narita International Airport, encountered severe turbulence from Faxai about 74 km (46 mi) southeast of Narita. The turbulence caused seven injuries on the flight, as well as some damage to the plane. [21]
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 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.
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. The first tropical cyclone of the season formed on January 13. The timeline also includes information which was not operationally released, meaning that information from post-storm reviews by the various warning agencies, such as information on a storm that was not operationally warned on, has been included.
Typhoon Rammasun, known in the Philippines as Typhoon Butchoy, was recognized as the second typhoon of the 2008 Pacific typhoon season by the Japan Meteorological Agency (JMA) and the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA). Rammasun was also recognised as the third tropical storm, the second typhoon and the first super typhoon of the 2008 Pacific typhoon season by the Joint Typhoon Warning Center (JTWC).
The 2009 Pacific typhoon season was a below average season that spawned only 22 named storms, 13 typhoons, and five super typhoons. It was also recognized as the deadliest season in the Philippines for decades. The first half of the season was very quiet whereas the second half of the season was extremely active. The season's first named storm, Kujira, developed on May 3 while the season's last named storm, Nida, dissipated on December 3.
The 2008–09 South Pacific cyclone season was a below-average season with only six tropical cyclones occurring within the South Pacific between 160°E and 120°W. The season officially ran from November 1, 2008 to April 30, 2009 with the first disturbance of the season forming on December 1 and the last disturbance moving out of the region on April 11.
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.
The 2010 Pacific typhoon season was the least active Pacific typhoon season on record, featuring only 14 named storms; seven of them strengthened into typhoons while one reached super typhoon intensity. The Pacific typhoon season during 2010 was in fact less active than the 2010 Atlantic hurricane season, with only two other occurrences of that happening, 2005 and 2020. In the same year, the Pacific hurricane season broke the same record being the least active season on record. During the season, no storms made landfall in mainland Japan, only the second such occurrence since 1988. Also, all of the 14 named storms developed west of 150°E.
Typhoon Maria was a minimal typhoon which brushed the southeastern coast of Japan during early August 2006. The seventh named storm of the 2006 Pacific typhoon season, Maria formed out of a tropical depression over the open waters of the western Pacific Ocean. On August 5, the Japan Meteorological Agency (JMA) classified the depression as a tropical storm while the Joint Typhoon Warning Center (JTWC) kept it as a depression. The storm quickly strengthened into a typhoon the next day, reaching its peak intensity with winds of 130 km/h early on August 6. The storm gradually weakened as it began to recurve, causing it to parallel the southeastern coast of Japan. On August 9, Maria weakened into a tropical depression and later into an extratropical cyclone before dissipating on August 15. Maria had only minor effects in Japan, mainly heavy rains which were estimated to have peaked over 400 mm (15.7 in) on the Izu Peninsula. One person was killed after being struck by lightning and six others were injured.
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 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.
Cyclone Arthur was the eighth tropical depression and fourth tropical cyclone of the 2006–07 South Pacific cyclone season. Forming as tropical depression on January 25, Arthur rapidly intensified into a strong Category 2 cyclone on the Australian intensity scale according to the Regional Specialized Meteorological Centre in Nadi, Fiji. The Joint Typhoon Warning Center assessed the storm to have peaked as a minimal category 1 cyclone. Shortly after peaking in intensity, the cyclone began to weaken due to unfavorable conditions. Quickly moving towards the east-southeast, the Arthur began to undergo an extratropical transition. After turning towards the southeast, the center of circulation was almost fully exposed due to strong wind shear. However, Arthur briefly re-strengthened late on January 26 before becoming extratropical the next day. Tropical Cyclone Arthur affected several small islands during its existence. French Polynesia observed the most noteworthy effects from the storm, where several landslides damaged a few homes.
This timeline documents all of the events of the 2009 Pacific typhoon season which was the period that tropical cyclones formed in the Western Pacific Ocean during 2009, with 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.
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.
The 2014 Pacific typhoon season was a slightly below average season, featuring 23 tropical storms, 11 typhoons, 8 super typhoons, and 7 Category 5 typhoons. The season's peak months August and September saw minimal activity caused by an unusually strong and a persistent suppressing phase of the Madden–Julian oscillation (MJO). The season ran throughout 2014, though most tropical cyclones typically develop between May and October. The season began with the development of Tropical Storm Lingling on January 18, and ended after Tropical Storm Jangmi which dissipated on January 1 of the next year.
The 2019 Pacific typhoon season was the costliest Pacific typhoon season on record, just ahead of the previous year. The season was fairly above-average, producing 29 named storms, 17 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 2019, though most tropical cyclones typically develop between May and October. The season's first named storm, Pabuk, reached tropical storm status on January 1, becoming the earliest-forming tropical storm of the western Pacific Ocean on record, breaking the previous record that was held by Typhoon Alice in 1979. The season's first typhoon, Wutip, reached typhoon status on February 20. Wutip further intensified into a super typhoon on February 23, becoming the strongest February typhoon on record, and the strongest tropical cyclone recorded in February in the Northern Hemisphere. The season's last named storm, Phanfone, dissipated on December 29 after it made landfall in the Philippines. The accumulated cyclone energy (ACE) index of this season amounted to 269 units.
This timeline documents all of the events of the 2010 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.
The 2004–05 Australian region cyclone season was a near-average season with eleven tropical cyclones occurring within the Australian region south of the equator and from 90°E to 160°E. The season officially ran from 1 November 2004 to 30 April 2005 with pre-season Tropical Cyclone Phoebe forming on 1 September and an unnamed tropical cyclone dissipating on 15 April. This is the period of the year when most tropical cyclones form within the Australian region.
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.
This timeline documents all of the events of the 2015 Pacific typhoon season. Most of the tropical cyclones formed 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. This area, called the Western Pacific basin, is the responsibility of the Japanese Meteorological Agency (JMA). They host and operate the Regional Specialized Meteorological Center (RSMC), located in Tokyo. The Japanese Meteorological Agency (JMA) is also responsible for assigning names to all tropical storms that are formed within the basin. However, any storm that enters or forms in the Philippine Area of Responsibility (PAR) will be named by the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) using a local name. Also of note - the Western Pacific basin is monitored by the United States' Joint Typhoon Warning Center (JTWC), which gives all Tropical depressions a number with a "W" suffix.
![]() | Wikimedia Commons has media related to Severe Tropical Storm Faxai (2007) . |