Tag Archives: 14W

Typhoon Faxai Strengthens to Equivalent of Major Hurricane South of Tokyo

Typhoon Faxai strengthened into the equivalent of a major hurricane south of Tokyo, Japan on Saturday.  At 11:00 p.m. EDT on Saturday the center of Typhoon Faxai was located at latitude 31.8°N and longitude 139.7°E which put it about 300 miles (485 km) south of Tokyo, Japan.  Faxai was loving toward the northwest at 18 m.p.h. (30 km/h).  The maximum sustained wind speed was 130 m.p.h. (215 km/h) and there were wind gusts to 160 m.p.h. (260 km/h).  The minimum surface pressure was 944 mb.

Typhoon Faxai intensified rapidly into the equivalent of a major hurricane on Saturday.  There was a small circular eye at the center of circulation.  The eye was surround by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Typhoon Faxai.  Storms near the core were generating upper level divergence which was pumping mass away from the typhoon.

The circulation around Typhoon Faxai became more symmetrical on Saturday.  Winds to typhoon force extended out about 40 miles (65 km) from the center of circulation.  Winds to tropical storm force extended out about 140 miles (220 km) from the center.  The Hurricane Intensity Index (HII) for Typhoon Faxai was 25.1.  The Hurricane Size Index (HSI) was 15.0 and the Hurricane Wind Intensity Size Index (HWISI) was 40.1.  Typhoon Faxai was capable of causing regional major damage.

Typhoon Faxai will move through an environment favorable for powerful typhoons during the next 12 hours.  Faxai will move over water where the Sea Surface Temperature is near 28°C.  It will move under the middle of an upper level ridge where the winds are weak and there will be little vertical wind shear.  Typhoon Faxai is likely to maintain its intensity during the next 12 hours and it could strengthen a little more.  Typhoon Faxai will reach the coast of Honshu in about 12 hours and Faxai will weaken when it moves over land.  Faxai will move under the westerly winds in the middle latitudes in a day or so and the vertical wind shear will increase when that happens.

Typhoon Faxai will move around the western end of a subtropical high pressure system over the Western North Pacific Ocean.  The high will steer Faxai toward the north during the next 12 to 18 hours.  The high pressure system and the westerly winds in the middle latitude will turn Typhoon Faxai toward the northeast in 18-24 hours.  On its anticipated track Typhoon Faxai will approach the coast of Honshu near Tokyo in about 12 hours.  Faxai will be capable of causing major damage when it reaches Honshu.

Typhoon Lingling Speeds Toward Korea

Typhoon Lingling sped toward the Korean peninsula on Friday.  At 5:00 p.m. EDT on Friday the center of Typhoon Lingling was located at latitude 34.8°N and longitude 125.0°E which put it about 100 miles (160 km) west of Mokpo, South Korea.  Lingling was moving toward the north at 30 m.p.h. (48 km/h).  The maximum sustained wind speed was 105 m.p.h. (165 km/h) and thee were wind gusts to 125 m.p.h. (200 km/h).  The minimum surface pressure was 955 mb.

Typhoon Lingling was weakening gradually while it was speeding toward the north.  Lingling was moving over water where the Sea Surface Temperature was near 26°C.  An upper level trough over eastern Asia was producing strong southerly winds which blowing toward the top of the typhoon.  Those winds were causing moderate vertical wind shear.  The circulation around Typhoon Lingling was also pulling in drier air from Asia around the southern side of the circulation.  Even though it was weakening, Lingling remained a dangerous typhoon.  Winds to typhoon force extended out about 45 miles (75 km) from the center of circulation.  The stronger winds were primarily in the eastern half of the circulation.  Winds to tropical storm force extended out about 220 miles (350 km) from the center.

The upper trough over eastern Asia was steering Typhoon Lingling rapidly toward the north.  On its anticipated track Typhoon Lingling could reach the west coast of North Korea in less than 12 hours.  Lingling will be capable of causing serious damage.  It will also drop locally heavy rain over the Korean peninsula which could cause flash floods in some locations.

Elsewhere over the Western North Pacific Ocean, former Tropical Storm Faxai strengthened into a typhoon east of iwo To.  At 5:00 p.m. EDT on Friday the center of Typhoon Faxai was located at latitude 26.1°N and longitude 145.6°E which put it about 325 miles (520 km) east of Iwo To.  Faxai was moving toward the west-northwest at 21 m.p.h. (34 km/h).  The maximum sustained wind speed was 75 m.p.h. (120 km/h) and there were wind gusts to 90 m.p.h. (145 km/h).  The minimum surface pressure was 979 mb.  Typhoon Faxai is forecast to move toward the northwest and strengthen.  Faxai could intensify into the equivalent of a major hurricane.  Typhoon Faxi could approach the area around Tokyo, Japan in less than 72 hours.

Typhoon Jongdari Nears Iwo To

Typhoon Jongdari neared Iwo To on Thursday.  At 11:00 a.m. EDT on Thursday the center of Typhoon Jongdari was located at latitude 24.2°N and longitude 140.5°E which put it about 105 miles (170 km) southwest of Iwo To.  Jongdari was moving toward the northeast at 13 m.p.h. (21 km/h).  The maximum sustained wind speed was 75 m.p.h. (120 km/h) and there were wind gusts to 90 m.p.h. (145 km/h).  The minimum surface pressure was 975 mb.

Former Tropical Storm Jongdari strengthened as it neared Iwo To on Thursday.  An eye developed at the center of circulation and the Japan Meteorological Agency classified Jongdari as a typhoon.  The eye was surrounded by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms.  Several bands of showers and thunderstorms were revolving around the core of Jongdari.  Thunderstorms in the core of Jongdari were generating strong upper level divergence which was pumping mass away from the typhoon.  Winds to typhoon force extended out about 20 miles (30 km) from the center of circulation.  Winds to tropical storm force extended out about 130 miles (210 km) from the center.

Typhoon Jongdari will move through an environment favorable for intensification during the next day or two.  Jongdari will move over water where the Sea Surface Temperature is near 28°C.  An upper level low southeast of Honshu will cause easterly winds which will blow over the northern part of the circulation.  Those winds will cause some vertical wind shear, but the shear will be less over the core of the typhoon.  Typhoon Jongdari will strengthen during the next 24 to 48 hours and it could become the equivalent of a major hurricane.

Typhoon Jongdari is moving around the western end of a subtropical ridge over the Western North Pacific and the ridge is steering Jongdari toward the northeast.  A general motion toward the northeast is forecast for the next 12 to 24 hours.  The upper low southeast of Honshu will move slowly toward the west.  When Jongdari moves farther north, it will begin to be steered more by the upper level low.  Typhoon Jongdari is forecast to turn more toward the north on Friday.  Jongdari will start to move toward the northwest in about 36 hours, when it moves northeast of the upper level low.

On its anticipated track Typhoon Jongdari will move over Iwo To in a few hours.  It will bring gusty winds and heavy rain.  Typhoon Jongdari could approach Honshu in about 48 hours and it could cause flooding in addition to strong winds and heavy rain.

Elsewhere over the Western North Pacific, Tropical Storm Wokung was weakening east of northern Japan.  At 11:00 a.m. EDT on Thursday the center of Tropical Storm Wokung was located at latitude 42.2°N and longitude 152.5°E which put it about 600 miles (960 km) east of Misawa, Japan.  Wokung was moving toward the north-northwest at 19 m.p.h. (31 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 995 mb.

Tropical Storm Jongdari Forms Southwest of Iwo To

Tropical Storm Jongdari formed southwest of Iwo To on Tuesday.  At 5:00 p.m. EDT on Tuesday the center of Tropical Storm Jongdari was located at latitude 20.9°N and longitude 136.9°E which put it about 410 miles (665 km) southwest of Iwo To.  Jongdari was moving toward the north at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 996 mb.

A distinct low level center of circulation developed within former Tropical Depression 15W on Tuesday afternoon and the Japan Meteorological Agency designated the system as Tropical Storm Jongdari.  The circulation of Jongdari was asymmetrical.  Most of the stronger thunderstorms were forming in bands north of the center.  Bands south of the center consisted primarily of showers and lower clouds.  Stronger storms near the center were beginning to generate upper level divergence which was pumping mass away from the core of the circulation.

Tropical Storm Jongdari will move through an environment favorable for intensification during the next several days.  Jongdari will move over water where the Sea Surface Temperature is near 28°C.  So, there will be sufficient energy in the upper ocean to support intensification.  It will move under the middle of an upper level ridge where the winds are weaker and there will be little vertical wind shear.  Intensification could be slow at first while the circulation becomes more organized, but Jongdari could strengthen more quickly when the inner core becomes more well developed.  Tropical Storm Jongari could strengthen to a typhoon with 48 hours.  It could eventually intensify into the equivalent of a major hurricane.

Tropical Storm Jongari will move around the western end of a subtropical ridge which will steer Jongari toward the northeast during the next two or three days.  When Jongari moves farther north, it will be affected by a second ridge located farther to the north.  The second ridge is forecast to strengthen and push Jongari more toward the northwest.  On its anticipated track Jongari could reach Iwo To in about 48 hours.  It could be a typhoon at that time.  Jongari could approach Tokyo in about four days and it is likely to be a typhoon when it reaches Honshu.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Wokung was churning well southeast of Japan.  At 5:00 p.m. EDT on Tuesday the center of Tropical Storm Wokung was located at latitude 32.3°N and longitude 158.0°E which put it about 1250 miles (2015 km) east-southeast of Tokyo, Japan.  Wokung was moving toward the north-northwest at 11 m.p.h. (17 km/h).  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were wind gusts to 75 m.p.h. (120 km/h).  The minimum surface pressure was 984 mb.

Tropical Storm Wukong Forms Southeast of Japan

Tropical Storm Wukong formed southeast of Japan on Monday.  At 5:00 p.m. EDT on Monday the center of Tropical Storm Wukong was located at latitude 29.0°N and longitude 159.0°E which put it about 1370 miles (2210 km) east-southeast of Tokyo, Japan.  Wukong was moving toward the north at 24 m.p.h. (39 km/h).  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and the were wind gusts to 75 m.p.h. (120 km/h).  The minimum surface pressure was 984 mb.

A cluster of thunderstorms developed southeast of Japan during the weekend and a low level center of circulation formed near the southwestern edge of the cluster of storms.  However, strong upper level winds blowing from the southwest kept blowing the top of the circulation northeast of the low level center and the system was unable to develop.  The upper level winds slowed on Monday and a band of showers and thunderstorms wrapped around the northern and western sides of the center of circulation.  The Japan Meteorological Agency designated the system as Tropical Storm Wukong.

The circulation of Tropical Storm Wukong organized quickly after the upper level winds weakened.   As mentioned above, a primary rainband wrapped around the northern and western sides of the center of circulation.  Storms in the primary rainband generated upper level divergence which was pumping mass away to the north of the tropical storm.  Several other bands of showers and thunderstorms developed in the eastern half of the circulation.  Bands south and west of the center consisted primarily of showers and lower clouds.

Tropical Storm Wukong will move through an environment favorable for intensification during the next day or so.  Wukong will move over water where the Sea Surface Temperature is near 27°C.  Wukong is moving along the eastern portion of an upper level trough.  The trough is producing southwesterly winds which are blowing toward the top of the circulation.  However, those winds weakened on Monday and they will not cause enough vertical wind shear to prevent further intensification.  Tropical Storm Wukong could strengthen into a typhoon during the next 24 to 36 hours.  Eventually, Wukong will move over cooler water and it will begin to weaken.

Tropical Storm Wukong is moving between an upper level trough to the west and an upper level ridge to the east.  The trough and ridge were combining to steer Wukong toward the north and a general northerly motion is expected to continue.  On its anticipated track Tropical Storm Wukong will stay west of the larger islands of Japan.  Wukong could approach the Kuril Islands in about three days.

Elsewhere over the Western North Pacific former Tropical Storm Ampil weakened to a tropical depression over land southeast of Beijing, China, Tropical Storm Son-tinh meandered near the coast of southeastern China and Tropical Depression 15W organized southwest of Iwo To, Japan.  At 5:00 p.m. EDT on Monday the center of Tropical Depression Ampil was located at latitude 38.8°N and longitude 117.6°E which put it about 110 miles (175 km) southeast of Beijing, China.  Ampil was moving toward the north-northwest at 18 m.p.h. (29 km/h).  The maximum sustained wind speed was 35 m.p.h. (55k km/h) and there were wind gusts to 45 m.p.h. (75 km/h).  The minimum surface pressure was 998 mb.  Tropical Depression Ampil was still dropping locally heavy rain over parts of eastern China.

At 5:00 p.m. EDT on Monday the center of Tropical Storm Son-tinh was located at latitude 21.2°N and longitude 109.0°E which put it about 40 miles (65 km) southeast of Beihai, China.  Son-tinh was moving toward the west-northwest at 6 m.p.h. (10 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 996 mb.  Tropical Storm Son-tinh was dropping locally heavy rain over parts of southeastern China and Hainan Island.

At 5:00 p.m. EDT on Monday the center of Tropical Depression 15W was located at latitude 17.6°N and longitude 136.3°E which put it about 585 miles (945 km) southwest of Iwo To, Japan.  It was moving toward the north-northwest at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 35 m.p.h. (55 km/h) and there were wind gusts to 45 m.p.h. (75 km/h).  The minimum surface pressure was 998 mb.  The circulation of Tropical Depression 15W became more organized on Monday and it could eventually strengthen into a typhoon when it moves toward Iwo To later this week.

Tropical Storm Ampil Nears Landfall Southeast of Shanghai

Tropical Storm Ampil neared landfall on the coast of China southeast of Shanghai on Saturday night.  At 11:00 p.m. EDT on Saturday the center of Tropical Storm Ampil was located at latitude 31.0°N and longitude 122.3°E which put it about 60 miles (95 km) southeast of Shanghai, China.  Ampil was moving toward the west-northwest at 14 m.p.h. (22km/h).  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were wind gusts to 75 m.p.h. (120 km/h).  The minimum surface pressure was 990 mb.

Tropical Storm Ampil moved steadily toward the coast of China on Saturday with little change of structure or intensity.  Drier air continued to circulate around the tropical storm and it limited the development of taller thunderstorms in much of Ampil.  The strongest thunderstorms were occurring in the inner portion of a band northwest of center of circulation.  The strongest winds were associated with those storms.  Bands around the rest of Tropical Storm Ampil consisted of showers and lower clouds.  Winds to tropical storm force extended out about 165 miles (270 km) from the center.

Tropical Storm Ampil will make landfall on the coast of China southeast of Shanghai in a few hours.  Ampil will cause gusty winds and the strong band of thunderstorms will drop locally heavy rain.  The heavy rain could cause flash floods in parts of eastern China.

Elsewhere the tropics became more active over the Western North Pacific Ocean on Saturday.  The remnants of former Tropical Storm Son-tinh were reorganizing west of Hainan Island over the Gulf of Tongking, Tropical Depression 13W moved east of Taiwan, and Tropical Depression 14W formed northwest of Wake Island and Tropical Depression 15W formed west of Guam.

At 11:00 p.m. EDT on Saturday the center of Tropical Depression Son-tinh was located at latitude 19.2°N and longitude 108.2°E which put it about 45 miles (75 km) west of Dongfeng, China.  Son-tinh was moving toward the east-southeast at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were wind gusts to 40 m.p.h. (65 km/h).  The minimum surface pressure was 999 mb.

Former Tropical Storm Son-tinh completed a slow clockwise loop over Laos and Vietnam which during the past several days and it emerged back over the Gulf of Tongking on Saturday.  There was a distinct low level center of circulation.  Bands of showers and thunderstorms were circulating around the enter.  The rainbands were dropping heavy rain over Hainan Island and creating the potential for flash floods.

At 11:00 p.m. EDT on Saturday the center of Tropical Depression 13W was located at latitude 21.6°N and longitude 122.9°E which put it about 165 miles (265 km) south-southeast of Hualien, Taiwan.  It was moving toward the northwest at 18 m.p.h. (29 km/h).  The maximum sustained wind speed was 35 m.p.h. (55 km/h) and there were wind gusts to 45 m.p.h. (75 km/h).  The minimum surface pressure was 998 mb.

At 11:00 p.m. EDT on Saturday the center of Tropical Depression 14W was located at latitude 22.5°N and longitude 159.4°E which put it about 370 miles (600 km) east-southeast of Minami Tori Shima.  It was moving toward the north at 4 m.p.h. (6 km/h).  The maximum sustained wind speed was 35 m.p.h. (55 km/h) and there were wind gusts to 45 m.p.h. (75 km/h).  The minimum surface pressure was 998 mb.

At 11:00 p.m. EDT on Saturday the center of Tropical Depression 15W was located at latitude 13.2°N and longitude 138.1°E which put it about 225 miles (365 km) north-northwest of Ulithi.  It was moving toward the northwest at 15 m.p.h. (24 km/h).  The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were wind gusts to 40 m.p.h. (65 km/h).  The minimum surface pressure was 998 mb.

Banyan Rapidly Intensifies Into a Typhoon

Tropical Storm Banyan rapidly intensified into a typhoon on Saturday.  At 5:00 p.m. EDT on Saturday the center of Typhoon Banyan was located at latitude 20.8°N and longitude 164.3°E which put it about 165 miles (265 km) west-northwest of Wake Island.  Banyan was moving toward the north-northwest at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 90 m.p.h. (145 km/h) and there were wind gusts to 115 m.p.h. (185 km/h).  The minimum surface pressure was 976 mb.

Banyan intensified rapidly from a tropical storm into a typhoon in less than 36 hours.  Banyan is a small well organized typhoon.  There is a small circular eye at the center of circulation.  The eye is surrounded by a ring of strong thunderstorms.  The strongest winds are occurring in that ring of storms.  A primary band of thunderstorms wraps around the eastern and northern sides of the core of Typhoon Banyan.  Other bands of showers and storms are revolving around the core of the typhoon.  Banyan has a small circulation.  Winds to typhoon force only extend out about 25 miles (40 km) from the center of circulation.  Winds to tropical storm force only extend out about 100 miles (160 km) from the center.

Typhoon Banyan will continue to move through an environment that is favorable for intensification on Sunday.  Banyan will move over water where the Sea Surface Temperature is near 30°C.  The upper level winds are weak and there is little vertical wind shear.  Typhoon Banyan will continue to intensify during the next 24 hours and it could become the equivalent of a major hurricane.

Banyan is moving around the western end of a subtropical ridge, which is steering the typhoon toward the north-northwest.  Banyan is forecast to continue to move toward the north-northwest for another day or two.  On its anticipated track Typhoon Banyan will move away from Wake Island and the weather should improve on Sunday.

Tropical Storm Banyan Forms Near Wake Island

Tropical Storm Banyan formed quickly near Wake Island on Friday.  At 11:00 a.m. EDT on Friday the center of Tropical Storm Banyan was located at latitude 17.9°N and longitude 167.2°E which put it about 140 miles (225 km) south-southeast of Wake Island.  Banyan was moving toward the west-northwest at 16 m.p.h. (26 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 1003 mb.

The circulation of Tropical Storm Banyan organized quickly.  It developed a distinct center of circulation.  Thunderstorms formed north and south of the center, but there were more thunderstorms south of the center.  Additional bands of showers and thunderstorms began to develop in the outer parts of the circulation.  The thunderstorms in the core of Tropical Storm Banyan were generating upper level divergence which was pumping away mass.  The circulation of Tropical Storm Banyan is relatively small.  Winds to tropical storm force only extend out about 40 miles (65 km) from the center of circulation.

Tropical Storm Banyan will move through an environment that will be favorable for intensification.  Banyan will move over water where the Sea Surface Temperature is near 30.5°C.  An upper level ridge north of Banyan is producing easterly winds which are blowing toward the top of the circulation.  Those winds are weak and there is not much vertical wind shear.  Tropical Storm Banyan is likely to intensify during the next day or two and it could intensify quickly at times.

Tropical Storm Banyan is moving near the western end of a subtropical ridge to its north.  The ridge is currently steering Banyan toward the west-northwest, but the tropical storm is expected to turn more toward the north when it reaches the end of the ridge.  On its anticipated track Tropical Storm Banyan will move over Wake Island in about 12 hours.  Banyan will cause gusty winds and heavy rain when it moves over Wake Island.