Tropical Storm Faxai (2007)
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Severe Tropical Storm Faxai, known in the Philippines as Tropical Storm Juaning, was a short-lived tropical storm that had minor effects on land in late October 2007. The twentieth named storm of the
2007 Pacific typhoon season 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 weste ...
, Faxai originated from a tropical depression over the open waters of the
western Pacific Ocean The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean, or, depending on the definition, to Antarctica in the south, and is bounded by the contine ...
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 on Miyakejima. A
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flight to
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encountered severe
turbulence In fluid dynamics, turbulence or turbulent flow is fluid motion characterized by chaotic changes in pressure and flow velocity. It is in contrast to laminar flow, which occurs when a fluid flows in parallel layers with no disruption between ...
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
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as the storm passed by, and three others were injured. Damages from the storm amounted to ¥150 million (US$1.5 million).


Meteorological history

Tropical Storm Faxai began as an area of
convection Convection is single or Multiphase flow, multiphase fluid flow that occurs Spontaneous process, spontaneously through the combined effects of material property heterogeneity and body forces on a fluid, most commonly density and gravity (see buoy ...
that persisted about west of
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on October 24. Satellite imagery indicated broad cyclonic turning in the lower levels of the atmosphere, and a
trough Trough may refer to: In science * Trough (geology), a long depression less steep than a trench * Trough (meteorology), an elongated region of low atmospheric pressure * Trough (physics), the lowest point on a wave * Trough level (medicine), the l ...
was near the surface. Convection consolidated around the center of the low-level circulation, and the upper-level environment—low
wind shear Wind shear (; also written windshear), sometimes referred to as wind gradient, is a difference in wind speed and/or direction over a relatively short distance in the atmosphere. Atmospheric wind shear is normally described as either vertical ...
and good divergence—favored development. The following day, the
Japan Meteorological Agency The Japan Meteorological Agency (JMA; ''気象庁, Kishō-chō'') is a division of the Ministry of Land, Infrastructure, Transport and Tourism dedicated to the Scientific, scientific observation and research of natural phenomena. Headquartered ...
(JMA) classified the system as a tropical depression. Shortly after, the
Joint Typhoon Warning Center The Joint Typhoon Warning Center (JTWC) is a joint United States Navy – United States Air Force command in Pearl Harbor, Hawaii. The JTWC is responsible for the issuing of tropical cyclone warnings in the North-West Pacific Ocean, South P ...
(JTWC) issued a
Tropical Cyclone Formation Alert A Tropical Cyclone Formation Alert (TCFA) is a bulletin released by the U.S. Navy-operated Joint Typhoon Warning Center in Honolulu, Hawaii or the Fleet Weather Center in Norfolk, Virginia, warning of the possibility of a tropical cyclone formi ...
as convection deepened around a partially exposed low. The storm traveled northwest under the influences of a
subtropical The subtropical zones or subtropics are geographical zone, geographical and Köppen climate classification, climate zones immediately to the Northern Hemisphere, north and Southern Hemisphere, south of the tropics. Geographically part of the Ge ...
ridge A ridge is a long, narrow, elevated geomorphologic landform, structural feature, or a combination of both separated from the surrounding terrain by steep sides. The sides of a ridge slope away from a narrow top, the crest or ridgecrest, wi ...
to the north. At 0000 UTC on October 26, the
Philippine Atmospheric, Geophysical and Astronomical Services Administration The Philippine Atmospheric, Geophysical and Astronomical Services Administration (, abbreviated as PAGASA , which means "hope" as in the Tagalog word ''pag-asa'') is the National Meteorological and Hydrological Services (NMHS) agency of the P ...
(PAGASA) designated the system as a tropical depression and gave it the local name ''Juaning''. Around the same time, the JMA upgraded the depression to a tropical storm and gave it the name ''Faxai''. The JTWC issued advisories on Faxai, designating it as 20W; however, they classified it as a tropical depression. 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. At 1200 UTC, PAGASA issued their final advisory on Tropical Storm Juaning as it moved out of their area of responsibility. The JTWC reported that Tropical Depression 20W (Faxai) had become extratropical around this time as it merged with a baroclinic zone. A
cold front A cold front is the leading edge of a cooler mass of air at ground level that replaces a warmer mass of air and lies within a pronounced surface Trough (meteorology), trough of Low-pressure area, low pressure. It often forms behind an extratropica ...
developed along the southern portion of Faxai, a feature of extratropical cyclones. Around that time, the JMA upgraded Faxai to a severe tropical storm with (10-minute sustained) winds of . The JTWC subsequently upgraded the depression to a tropical storm based on the development of a very impactful
central dense overcast The central dense overcast, or CDO, of a tropical cyclone or strong subtropical cyclone is the large central area of thunderstorms surrounding its circulation center, caused by the formation of its eyewall. It can be round, angular, oval, or ir ...
. A shortwave
trough Trough may refer to: In science * Trough (geology), a long depression less steep than a trench * Trough (meteorology), an elongated region of low atmospheric pressure * Trough (physics), the lowest point on a wave * Trough level (medicine), the l ...
over the
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provided a favorable upper-level environment for Faxai to intensify. Early the next day, Faxai began accelerating rapidly towards the northeast in the mid-latitude
westerlies The westerlies, anti-trades, or prevailing westerlies, are prevailing winds from the west toward the east in the middle latitudes between 30 and 60 degrees latitude. They originate from the high-pressure areas in the horse latitudes (about ...
. An
anticyclone A high-pressure area, high, or anticyclone, is an area near the surface of a planet where the atmospheric pressure is greater than the pressure in the surrounding regions. Highs are middle-scale meteorological features that result from interpl ...
over Japan created a strong
pressure gradient In hydrodynamics and hydrostatics, the pressure gradient (typically of air but more generally of any fluid) is a physical quantity that describes in which direction and at what rate the pressure increases the most rapidly around a particular locat ...
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, they assessed the storm to have reached its peak intensity, with (one-minute sustained) winds of . The JMA also assessed Faxai to have reached its peak intensity at that time, with (10-minute sustained) winds of and a minimum pressure of 975 
hPa The pascal (symbol: Pa) is the unit of pressure in the International System of Units (SI). It is also used to quantify internal pressure, stress, Young's modulus, and ultimate tensile strength. The unit, named after Blaise Pascal, is an S ...
(
mbar The bar is a metric unit of pressure defined as 100,000  Pa (100 kPa), though not part of the International System of Units (SI). A pressure of 1 bar is slightly less than the current average atmospheric pressure on Earth at sea ...
); however, the
National Oceanic and Atmospheric Administration The National Oceanic and Atmospheric Administration (NOAA ) is an American scientific and regulatory agency charged with Weather forecasting, forecasting weather, monitoring oceanic and atmospheric conditions, Hydrography, charting the seas, ...
(NOAA) reported that Faxai had attained hurricane-force winds by this time, peaking at . The storm continued towards the northeast at a rapid pace and became extratropical off the eastern coast of
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around 1200 UTC on October 27. The extratropical remnants persisted for more than a day before dissipating over open waters late on October 28. NOAA, on the other hand, continued to monitor the remnants of Faxai, with the system reaching the
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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. The
Japan Meteorological Agency The Japan Meteorological Agency (JMA; ''気象庁, Kishō-chō'') is a division of the Ministry of Land, Infrastructure, Transport and Tourism dedicated to the Scientific, scientific observation and research of natural phenomena. Headquartered ...
uses 10-minute sustained winds, while the
Joint Typhoon Warning Center The Joint Typhoon Warning Center (JTWC) is a joint United States Navy – United States Air Force command in Pearl Harbor, Hawaii. The JTWC is responsible for the issuing of tropical cyclone warnings in the North-West Pacific Ocean, South P ...
uses one-minute sustained winds. The conversion factor between the two is 1.14. JMA's peak intensity for Faxai was 100 km/h (65 mph) 10-minute sustained, or 120 km/h (75 mph) one-minute sustained. The JTWC's peak intensity for Faxai was one-minute sustained, or 10-minute sustained.


Preparations and impact

As Faxai approached Japan,
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canceled all of its day flights between Tokyo and the
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. Tokai Kisen, which operates ferries between Tokyo, the Izu Islands and
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, canceled some services due to the storm. Areas around Tokyo were warned of the expected heavy rains, waves up to , and high winds. Residents were advised to stay indoors during the storm, especially after sunset, and to avoid possible flying debris. Although Faxai did not make landfall, the outer bands produced heavy rains, which caused minor damage along the eastern coast of Japan. The highest total rainfall was recorded on Miyakejima at and in the Ōshima Subprefecture of Tokyo, was recorded. The rainfall in Miyakejima nearly surpassed the record daily rainfall for October 27. Rainfall rates peaked at on Miyaketsubota, which triggered seven mudslides throughout the country. One woman was killed near Tokyo, and three people were injured. One home, two hectares of farmland, 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). At 5:31 pm
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(0831 UTC) on October 27, a
Japan Airlines Japan Airlines (JAL) is the flag carrier airline of Japan. JAL is headquartered in Shinagawa, Tokyo. Its main hubs are Tokyo's Narita International Airport, Narita and Haneda Airport, Haneda airports, as well as secondary hubs in Osaka's Kansai ...
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heading to
Narita International Airport , also known as Tokyo-Narita International Airport or simply Narita Airport, formerly and originally known as , is the secondary international airport serving the Greater Tokyo Area, the only other one being Haneda Airport (HND). It is about e ...
, encountered severe
turbulence In fluid dynamics, turbulence or turbulent flow is fluid motion characterized by chaotic changes in pressure and flow velocity. It is in contrast to laminar flow, which occurs when a fluid flows in parallel layers with no disruption between ...
from Faxai about southeast of Narita. The turbulence caused seven injuries on the flight, as well as some damage to the plane.


See also

* Other tropical cyclones named Faxai * Other tropical cyclones named Juaning * Timeline of the 2007 Pacific typhoon season


References


External links


JMA General Information
of Severe Tropical Storm Faxai (0720) from Digital Typhoon
JMA Best Track Data
of Severe Tropical Storm Faxai (0720)
JMA Best Track Data (Graphics)
of Severe Tropical Storm Faxai (0720)


JTWC Best Track Data
of Tropical Storm 20W (Faxai)
20W.FAXAI
from the U.S. Naval Research Laboratory {{DEFAULTSORT:Faxai (2007) 2007 Pacific typhoon season Typhoons in Japan J Western Pacific severe tropical storms Tropical Storm Faxai J Faxai