Tag Archives: Iwo To

Typhoon Maysak Strengthens to Equivalent of Major Hurricane Near Okinawa

Typhoon Maysak strengthened to the equivalent of a major hurricane near Okinawa on Monday.  At 11:00 a.m. EDT on Monday the center of Typhoon Maysak was located at latitude 25.5°N and longitude 127.0°E which put it about 110 miles (180 km) south-southwest of Kadena AFB, Okinawa.  Maysak was moving toward the north-northwest at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 125 m.p.h. (200 km/h) and there were wind gusts to 155 m.p.h. (250 km/h).  The minimum surface pressure was 936 mb.

Typhoon Maysak strengthened to the equivalent of a major hurricane on Monday as it approached Okinawa.  A circular eye with a diameter of 30 miles (50 km) was at the center of Maysak.  The eye was surrounded 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 Maysak.  Storms near the core were generating upper level divergence which was pumping mass away from the typhoon.

Typhoon Maysak had a large circulation.  Winds to typhoon force extended out 70 miles (110 km) from the center of Maysak.  Winds to tropical storm force extended out 200 miles (320 km) from the center.  The Hurricane Intensity Index (HII) for Typhoon Maysak was 23.6.  The Hurricane Size Index (HSI) was 24.1 and the Hurricane Wind Intensity Size Index (HWISI) was 47.7.  Typhoon Maysak was capable of causing widespread major damage.

Typhoon Maysak will move through an environment favorable for intensification during the next 12 to 24 hours.  Maysak will move over water where the Sea Surface Temperature is near 30°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Typhoon Maysak could strengthen further and it could intensify into the equivalent of a Category 4 hurricane on the Saffir-Simpson Scale.

Typhoon Maysak will move around the western end of a subtropical high pressure system over the Western North Pacific Ocean.  The high will steer Maysak toward the north during the next several days.  On its anticipated track the center of Typhoon Maysak will pass west of Okinawa during the next few hours.  Maysak will bring strong winds and heavy rain to Okinawa.  Typhoon Maysak could approach South Korea in about 48 hours.

Elsewhere over the Western North Pacific Ocean, Tropical Depression 11W formed east-southeast of Iwo To.  At 11:00 a.m. EDT on Monday the center of Tropical Depression 11W was located at latitude 25.5°N and longitude 127.0°E which put it about 315 miles (515 km) east-southeast of Iwo To.  the depression was moving toward the southwest at 14 m.p.h. (22 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 1008 mb.

Tropical Storm Kalmaegi Strengthens East of Luzon

Tropical Storm Kalmaegi strengthened east of Luzon on Saturday night.  At 10:00 p.m. EST on Saturday the center of Tropical Storm Kalmaegi was located at latitude 15.7°N and longitude 125.2°E which put it about 300 miles (185 km) east-southeast of Aparri, Philippines.  Kalmaegi was moving toward the west-northwest at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 50 m.p.h. (80 km/h) and there were wind gusts to 65 m.p.h. (105 km/h).  The minimum surface pressure was 996 mb.

After meandering for days east of Luzon, Tropical Storm Kalmaegi began to strengthen on Saturday night.  Bands of showers and thunderstorms strengthened and wrapped around the eastern and northern sides of the center of circulation.   Storms near the center began to generate upper level divergence which pumped mass away to the northeast of the tropical storm.  Bands in the western half of the circulation still consisted primarily of showers and lower clouds.  Winds to tropical storm force extended out 120 miles (195 km) from the center.

Tropical Storm Kalmaegi will move through an environment favorable for intensification during the next 24 to 36 hours.  Kalmaegi will move over water where the Sea Surface Temperature is near 29°C.  It will move south of an upper level ridge over the Western North Pacific Ocean.  The ridge will produce easterly winds which will cause some vertical wind shear.  The shear will slow the rate of intensification, but it will not be strong enough to prevent intensification.  Tropical Storm Kalmaegi could strengthen into a typhoon during the next 36 hours.

The ridge over the Western Pacific Ocean will steer Tropical Storm Kalmaegi toward the northwest during the next 36 hours.  On its anticipated track Tropical Storm Kalmaegi could approach northern Luzon in about 36 hours.  Kalmaegi could be a typhoon by that time.

Elsewhere over the Western North Pacific Ocean, Typhoon Fengshen was speeding away from Iwo To.  At 10:00 p.m. EST on Saturday the center of Typhoon Fengshen was located at latitude 26.4°N and longitude 153.1°E which put it about 690 miles (1110 km) east-northeast of Iwo To.  Fengshen was moving toward the east at 31 m.p.h. (50 km/h).  The maximum sustained wind speed was 105 m.p.h. (165 km/h) and there were wind gusts to 125 m.p.h. (200 km/h).  The minimum surface pressure was 962 mb.

Typhoon Fengshen Strengthens into Equivalent of a Major Hurricane

Typhoon Fengshen strengthened into the equivalent of a major hurricane on Friday.  At 4:00 p.m. EST on Friday the center of Typhoon Fengshen was located at latitude 23.0°N and longitude 142.9°E which put it about 175 miles (285 km) south-southeast of Io To.  Fengshen was moving toward the north at 16 m.p.h. (26 km/h).  The maximum sustained wind speed was 125 m.p.h. (200 km/h) and there were wind gusts to 155 m.p.h. (250 km/h).  The minimum surface pressure was 949 mb.

Typhoon Fengshen strengthened quickly into the equivalent of a major hurricane on Friday.  An eye with a diameter of 25 miles (40 km) developed at the center of Fengshen.  The eye was surrounded 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 Fengshen.  Storms near the core were generating strong upper level divergence which was pumping mass away to the northeast of the typhoon.

The circulation around Typhoon Fengshen increased in size on Friday.  Winds to typhoon force extended out 40 miles (65 km) from the center of circulation.  Winds to tropical storm force extended out 140 miles (225) km from the center.  The Hurricane Intensity Index (HII) for Typhoon Fengshen was 23.6.  The Hurricane Size Index (HSI) was 11.2 and the Hurricane Wind Intensity Size Index (HWISI) was 34.8.

Typhoon Fengshen may have reached its peak intensity.  Fengshen will move over water where the Sea Surface Temperature is near 28°C.  So, there will be suffiicient energy in the upper levels of the Western Pacific to support intensification.  However, a large upper level trough southwest of Japan will move toward Fengshen.  The trough will produce strong southwesterly winds which will blow toward the top of the typhoon.  Those winds will cause moderate to strong vertical wind shear and the shear will cause Typhoon Fengshen to being to weaken.

A ridge of high pressure east of Typhoon Fengshen and the upper level trough southwest of Japan will interact to steer the typhoon toward the northeast during the weekend.  On its anticipated track the core of Typhoon Fengshen which contains the strongest winds will pass southeast of Iwo To.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Kalmaegi moved very slowly toward northern Luzon.  At 4:00 p.m. EST on Friday the center of Tropical Storm Kalmaegi was located at latitude 16.0°N and longitude 125.9°E which put it about 345 miles (555 km) southeast of Aparri, Philippines.  Kalmaegi was moving toward the west at 2 m.p.h. (3 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 1002 mb.

Typhoon Fengshen Brings Wind and Rain to Northern Marianas

Typhoon Fengshen brought wind and rain to the Northern Marianas on Thursday.  At 10:00 p.m. EST on Thursday the center of Typhoon Fengshen was located at latitude 19.6°N and longitude 143.3°E which put it about 385 miles (620 km) south-southeast of Iwo To.  Fengshen was moving toward the northwest at 18 m.p.h. (30 km/h).  The maximum sustained wind speed was 85 m.p.h. (135 km/h) and there were wind gusts to 105 m.p.h. (165 km/h).  The minimum surface pressure was 974 mb.

Typhoon Fengshen intensified rapidly into a typhoon on Thursday as it moved over the Northern Marianas.  Fengshen brought strong, gusty winds and heavy rain to Alamagan, Agrihan and Pagan.  There was a small circular eye at the center of Typhoon Fengshen.  The eye was surrounded 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 Fengshen.  Storms near the core were generating upper level divergence which was pumping mass away from the typhoon.  Winds to typhoon force extended out 30 miles from the center of circulation.  Winds to tropical storm force extended out 85 miles (135 km) from the center.

Typhoon Fengshen will move through an environment favorable for intensification during the next day or so.  Fengshen will move over water where the Sea Surface Temperature is near 29°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Typhoon Fengshen could strengthen into the equivalent of a major hurricane on Friday.

Typhoon Fengshen will move around the western end of a ridge of high pressure over the Western North Pacific Ocean.  The ridge will steer Fengshen toward the north during the next 24 hours.  The typhoon will move toward the northeast on Saturday after it moves around the end of the ridge.  On its anticipated track Typhoon Fengshen will be south of Iwo To in about 24 hours.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Kalmaegi move closer to northern Luzon.  At 10:00 p.m. EST on Thursday the center of Tropical Storm Kalmaegi was located at latitude 16.6°N and longitude 125.0°E which put it about 250 miles (400 km) southeast of Aparri, Philippines.  Kalmaegi was moving toward the west-northwest at 12 m.p.h. (19 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 1002 mb.

Halong Strengthens into a Typhoon East of the Northern Marianas

Former Tropical Storm Halong strengthened into a typhoon east of the Northern Marianas on Sunday.  At 4:00 p.m. EDT on Sunday the center of Typhoon Halong was located at latitude 17.0°N and longitude 153.3°E which put it about 520 miles (840 km) east-northeast of Saipan.  Halong was moving toward the northwest at 12 m.p.h. (19 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.

The circulation around former Tropical Storm Halong exhibited much better organization on Sunday.  An eye with a diameter of approximately 12 miles (19 km) formed at the center of Halong.  A ring of strong thunderstorms surrounded the eye and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Typhoon Halong.  The strongest rainbands were north and east of the center of circulation.  Bands in the western half of Halong consisted primarily of showers and lower clouds.  Typhoon Halong may have been pulling sinking, drier air into the western half of the circulation, which may be why the bands were weaker in that part of the typhoon.  Storms around the core of Halong were generating strong upper level divergence which was pumping mass away from the typhoon.  Winds to typhoon force extended out 10 miles (15 km) from the center of circulation.  Winds to tropical storm force extended out 175 miles (280 km) from the center.

Typhoon Halong will move through an environment favorable for intensification during the next 36 to 48 hours.  Halong will move over water where the Sea Surface Temperature is near 29°C.  It will move under the western part of an upper level ridge where the winds are weak.  So, there will not be a lot of vertical wind shear.  Typhoon Halong will continue to intensify and it could strengthen into the equivalent of a major hurricane.

Typhoon Halong will move around the western end of a ridge of high pressure over the Western North Pacific Ocean.  The ridge will steer Halong toward the northwest during the next 24 hours.  After that time Typhoon Halong will move more toward the north while it moves around the western end of the ridge.  Halong will move northeastward after it moves around the end of the ridge.  On its anticipated track Typhoon Halong is forecast to remain northeast of the Northern Marianas.  Halong is expected to pass between Iwo To and Wake Island later next week.

Typhoon Bualoi Brings Wind and Rain to Ogasawara Islands

Typhoon Bualoi brought wind and rain to the Ogasawara Islands on Wednesday.  At 11:00 p.m. EDT on Wednesday the center of Typhoon Bualoi was located at latitude 27.6°N and longitude 142.2°E which put it about 30 miles (50 km) north of Chichijima, Japan.  Bualoi was moving toward the north at 19 m.p.h. (31 km/h).  The maximum sustained wind speed was 110 m.p.h. (175 km/h) and there were wind gusts to 130 m.p.h. (210 km/h).  The minimum surface pressure was 963 mb.

Typhoon Bualoi moved over the Ogasawara Islands on Wednesday.  The core of Bulaoi and the strongest winds moved just to the east of Iwo To.  The international airport on Iwo To reported winds to near typhoon force.  The center of Typhoon Bualoi passed very close to Hahajima and Chichijima.  Bualoi produced gusty winds on Iwo To, Hahajima and Chichijima.  The typhoon also dropped locally heavy rain over some of the Ogasawara Islands.

Typhoon Bualoi weakened slowly on Wednesday.  There was a circular eye at the center of circulation.  The eye was surrounded by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were occurring in the northern half of Bualoi.  Bands in the southern half of the typhoon consisted primarily of showers and lower clouds.  An upper level trough west of Japan produced southwesterly winds which were blowing toward the top of the circulation.  Those winds were causing vertical wind shear and they were the probable reason for the weaker bands in the southern half of the circulation.

Typhoon Bualoi will continue to weaken.  Bualoi will move over water where the Sea Surface Temperature is near 28°C.  However, the upper level trough west of Japan will continue to cause wind shear which will weaken the typhoon.  In addition, the circulation around Typhoon Bualoi will pull drier air around the southern side of the typhoon.  The drier air will make Bualoi start to weaken more quickly.

The upper level trough west of Japan will turn Typhoon Bualoi toward the northeast on Thursday.  On its anticipated track Typhoon Bualoi will move away from the Ogasawara Islands during the next 24 hours.  The wind speeds should gradually decrease and rainfall will end quickly as Bualoi moves away from those islands.  Typhoon Bualoi is forecast to pass well to the southeast of Honshu.

Powerful Typhoon Bualoi Approaches Iwo To

Powerful Typhoon Bualoi approached Iwo To on Tuesday night.  At 11:00 p.m. EDT on Tuesday the center of Typhoon Bualoi was located at latitude 22.3°N and longitude 142.1°E which put it about 220 miles (360 km) south-southeast of Iwo To.  Bualoi was moving toward the north-northwest at 18 m.p.h. (30 km/h).  The maximum sustained wind speed was 140 m.p.h. (220 km/h) and there were wind gusts of 165 m.p.h. (270 km/h).  The minimum surface pressure was 942 mb.

Concentric eyewalls appeared to be at the center of Typhoon Bualoi.  The small inner eye and eyewall were still evident on visible and microwave satellite images.  A second outer eyewall completely encircled the inner eyewall.  The strongest winds were occurring in the inner eyewall.  Eventually, low level convergence will occur mainly in the outer eyewall and the inner eyewall will begin to weaken.  The maximum wind speed will decrease as the inner eyewall weakens.  However, the eyewall replacement cycle will cause the circulation around Typhoon Bualoi to increase in size.

Winds to typhoon force extended out 40 miles (65 km) from the center of Typhoon Bualoi.  Winds to tropical storm force extended out 140 miles (220 km) from the center of circulation.  The Hurricane Intensity Index (HII) for Typhoon Bualoi was 28.3.  The Hurricane Size Index (HSI) was 12.2 and the Hurricane Wind Intensity Size Index (HWISI) was 40.5.  Bualoi was capable of causing significant damage.

Typhoon Bualoi will move through an environment capable of supporting a strong typhoon during the next 24 to 36 hours.  Bualoi will move over water where the Sea Surface Temperature is near 29°C.  It will move through an area where the upper level winds are weak during the next 24 hours and there will be little vertical wind shear during the next days or so.  Even though Typhoon Bualoi will move through an environment capable of supporting a strong typhoon, the eyewall replacement cycle will cause Bualoi to weaken.  Typhoon Bualoi will move into a region where the upper level winds will be stronger on Thursday.  Increased wind shear will cause Bualoi to weaken more quickly when that happens.

Typhoon Bualoi will move around the western end of a high pressure system over the Western North Pacific Ocean during the next 36 to 48 hours.  The high will steer Bualoi toward the north during the next 24 hours.  The typhoon will move more toward the northeast on Thursday.  On its anticipated track Typhoon Bualoi could reach Iwo To in about 12 hours.  Bualoi will bring very strong winds to Iwo To.  It will be capable of causing major damage.  Typhoon Bualoi will also drop heavy rain on Iwo To and flash floods will be likely.

Typhoon Bualoi Strengthens to Equivalent of Major Hurricane over Marianas

Typhoon Bualoi strengthened to the equivalent of a major hurricane over the Marianas on Monday.  At 5:00 p.m. EDT on Monday the center of Typhoon Bualoi was located at latitude 16.7°N and longitude 145.5°E which put it about 660 miles (1060 km) south-southeast of Iwo To.  Bualoi was moving toward the northwest at 14 m.p.h. (22 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 949 mb.

Typhoon Bualoi continued to intensify quickly on Monday.  There was a small eye at the center of Bualoi.  The eye was surrounded 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 Bualoi.  Storms near the core were generating upper level divergence which was pumping mass away from the typhoon in all directions.

The circulation around Typhoon Bualoi was small.  Winds to typhoon force extended out 30 miles (50 km) from the center of circulation.  Winds to tropical storm force extended out 115 miles (185 km) from the center.  The Hurricane Intensity Index (HII) for Typhoon Bualoi was 25.1.  The Hurricane Size Index (HSI) was 10.0 and the Hurricane Wind intensity Size Index (HWISI) was 35.1.  Typhoon Bualoi was capable of causing localized major damage.  The core of Bualoi where the strongest winds were occurring passed north of Saipan.

Typhoon Bualoi will move through an environment capable of supporting a strong typhoon for another 24 to 36 hours.  Bualoi will move over water where the Sea Surface Temperature is near 29°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Bualoi could strengthen during the next 24 hours.  If an inner rainband wraps around the existing eye and eyewall, then an eyewall replacement cycle could cause the typhoon to start to weaken.

Typhoon Bualoi will move around the western end of high pressure system over the Western North Pacific Ocean.  The high will steer Bualoi toward the northwest during the next 24 hours.  The typhoon will move more toward the north when it reaches the western end of the high pressure system.  On its anticipated track Typhoon Bualoi will move away from the Northern Marianas.  Conditions should improve when Bualoi gets farther away.  Typhoon Bualoi could be near Iwo To in about 60 hours.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Neoguri was moving south of Honshu.  At 5:00 p.m. EDT on Monday the center of Tropical Storm Neoguri was located at latitude 32.4°N and longitude 137.6°E which put it about 285 miles (460 km) southwest of Tokyo, Japan.  Neoguri was moving toward the east-northeast at 14 m.p.h. (22 km/h).  The maximum sustained wind speed was 50 m.p.h. (80 km/h) and there were wind gusts to 65 m.p.h. (105 km/h).  The minimum surface pressure was 997 mb.  The center of Tropical Storm Neoguri is likely to pass south of Tokyo during in about 12 hours.

Neoguri Strengthens to Typhoon South of Okinawa, Bualoi Prompts Watches for Marianas

Former Tropical Storm Neoguri strengthened into a typhoon south of Okinawa on Saturday and Tropical Storm Bualoi prompted watches for the Marianas.  At 11:00 p.m. EDT on Saturday the center of Typhoon Neoguri was located at latitude 23.9°N and longitude 128.1°E which put it about 200 miles (320 km) south of Okinawa.  Neoguri was moving toward the north-northeast at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 105 m.p.h. (165 km/h) and there were wind gusts to 125 m.p.h. (200 km/h).  The minimum surface pressure was 965 mb.

Typhoon Neoguri strengthened rapidly on Saturday.  An eye formed at the center of circulation and a ring of strong thunderstorms surrounded the eye.  The strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Neoguri.  There were more bands of thunderstorms in the northern half of the typhoon.  The circulation around Typhoon Neoguri was small.  Winds to typhoon force extended out 20 miles (30 km) from the center of circulation.  Winds to tropical storm force extended out 85 miles (135 km) from the center.

Typhoon Neoguri will move through an environment unfavorable for intensification during the next several days.  Neoguri will move over water where the Sea Surface Temperature is near 28°C.  So, there will be enough energy in the ocean to support intensification.  However, an upper level trough over China will produce southwesterly winds which will blow toward the top of Typhoon Neoguri.  Those winds will produce moderate vertical wind shear and the shear will be strong enough to cause Neoguri to weaken.  Since the circulation around the typhoon is small, it could weaken more rapidly if the upper level winds get stronger.

The upper level trough over China will steer Typhoon Neoguri toward the northeast during the next few days.  On its anticipated track Neoguri will pass east of the Ryukyu Islands including Okinawa during the next 36 hours.  It could approach Honshu in about 48 hours.  Typhoon Neoguri will likely be a tropical storm by the time it approaches Honshu.

Elsewhere over the Western North Pacific Ocean, former Tropical Depression 22W rapidly strengthened into Tropical Storm Bualoi.  Bualoi had almost strengthened into a typhoon by Saturday evening.  At 11:00 p.m. EDT on Saturday the center of Tropical Storm Bualoi was located at latitude 11.8°N and longitude 150.8°E which put it about 455 miles (730 km) east of Guam.  Bualoi was moving toward the west-northwest at 13 m.p.h. (20 km/h).  The maximum sustained wind speed was 70 m.p.h. (110 km/h) and there were wind gusts to 85 m.p.h. (135 km/h).  The minimum surface pressure was 985 mb.

Typhoon Watches were in effect for Rota, Tinian and Saipan.  A Tropical Storm Watch was in effect for Guam.

The circulation around Tropical Storm Bualoi organized quickly on Saturday.  The inner end of a rainband wrapped around the center of circulation.  Microwave satellite images indicated that an eye could be forming.  Bands of showers and thunderstorms were revolving around the core of Bualoi.  Storms near the core were generating upper level divergence which was pumping mass away from the tropical storm.  Winds to tropical storm force extended out about 90 miles (145 km) from the center of circulation.

Tropical Storm Bualoi will move through an environment favorable for intensification during the next several days.  Bualoi will move over water where the Sea Surface Temperature is near 29°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Bualoi will strengthen into a typhoon on Sunday and it could eventually intensify into the equivalent of a major hurricane.

Tropical Storm Bualoi will move south of a high pressure system over the Western North Pacific Ocean.  The high will steer Bualoi toward the west-northwest during the next day or two.  On its anticipated track Tropical Storm Bualoi could reach the Marianas in 36 hours.  Bualoi will very likely be a typhoon when it reaches the Marianas.  The center of Bualoi could pass near Tinian and Saipan.  It could be near Iwo To in about four days.

Powerful Typhoon Hagibis Continues Toward Honshu

Powerful Typhoon Hagibis continue to move toward Honshu on Wednesday.  At 11:00 p.m. EDT on Wednesday the center of Typhoon Hagibis was located at latitude 23.7°N and longitude 139.5°E which put it about 140 miles (225 km) west-southwest of Iwo To.  Hagibis was moving toward the north at 14 m.p.h. (22 km/h).  The maximum sustained wind speed was 160 m.p.h. (260 km/h) and there were wind gusts to 195 m.p.h. (315 km/h).  The minimum surface pressure was 918 mb.

Typhoon Hagibis continued to have a powerful, large circulation on Wednesday.  A circular eye with a diameter of 25 miles (40 km) was at the center of circulation.  The eye was surrounded 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 Hagibis.  The rainbands in the northwestern quadrant of Hagibis were a little weaker than the bands in other parts of the typhoon.  Some drier air may have been being pulled into the the northwestern quadrant of the circulation.  Storms around the core of the typhoon continue to generate strong upper level divergence.

The strength of the winds around Typhoon Hagibis exhibited more asymmetry on Wednesday.  Winds to typhoon force extended out 150 miles (240 km) from the center of circulation in the northeastern part of Hagibis.  Winds to typhoon force were occurring within 100 miles (160 km) of the center in the other parts of Typhoon Hagibis.  Winds to tropical storm force extended out 370 miles (565 km) from the center.  The Hurricane Intensity Index (HII) for Typhoon Hagibis was 35.0.  The Hurricane Size Index (HSI) was 39.9 and he Hurricane Wind Intensity Size Index (HWISI) was 74.9.  Typhoon Hagibis was capable of causing extensive catastrophic damage.

Typhoon Habigis will continue to move through an environment capable of supporting strong  typhoons, but Hagibis is likely to start to weaken on Thursday.  Typhoon Hagibis will move over water where the Sea Surface Temperature is near 29°C, but that is slightly cooler than the water Hagibis has been over.  Typhoon Hagibis will move through a region where the upper level winds are weak during the next 24 hours.  There will be little vertical wind shear on Thursday, and so Hagibis will likely weaken slowly.  Typhoon Hagibis will move closer to upper level westerly winds in the middle latitudes on Friday.  When Hagibis gets closer to the stronger upper level winds, vertical wind shear will increase and the typhoon will weaken more quickly.  The large circulation around Typhoon Hagibis will slow the rate of weakening even when the wind shear increases.

Typhoon Hagibis will move around the western end of a subtropical high pressure system over the Western North Pacific Ocean during the next 24 hours.  The high will steer Hagibis toward the north on Thursday.  Typhoon Hagibis will move toward the northeast on Friday when it reaches the upper level westerly winds.  On its anticipated track the center of Typhoon Hagibis will move west of Iwo To during the next 24 hours.  Hagibis will bring winds to tropical storm force to Iwo To and there is a chance that the winds could reach typhoon force at times.  Rainbands on the eastern side of the typhoon will drop heavy rain on Iwo To.  Typhoon Hagibis could approach the coast of Honshu near Tokyo in a little over 48 hours.  Hagibis will still be a typhoon when it approaches Tokyo.  It will bring strong winds and heavy rain to parts of Honshu.  Typhoon Hagibis could also produce winds to tropical storm force on Shikoku.