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Typhoon Koguma Continues to Weaken

Typhoon Koguma continued to weaken on Monday as it moved over the Western North Pacific Ocean east of Japan.  At 11:00 p.m. EDT on Monday the center of Typhoon Koguma was located at latitude 34.6°N and longitude 152.6°E which put the center about 690 miles (1110 km) east of Tokyo, Japan.  Koguma was moving toward the northeast at 28 m.p.h. (45 km/h).  The maximum sustained wind speed was 80 m.p.h. (130 km/h) and there were wind gusts to 100 m.p.h. (160 km/h).  The minimum surface pressure was 979 mb.

Typhoon Koguma started to make a transition to a strong extratropical cyclone on Monday.  Thunderstorms were still occurring in bands in the eastern and northern parts of Koguma’s circulation.  Bands in the western and southern parts of Typhoon Koguma consisted primarily of showers and lower clouds.  Storms near the center of Koguma generated upper level divergence that pumped mass away to the northeast of the typhoon.  The removal of mass in the upper levels was less than the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure increased on Monday.

Even though Typhoon Koguma started a transition to an extratropical cyclone on Monday, the distribution of wind speeds was still fairly symmetrical.  Winds to typhoon force extended out 60 miles (95 km) from the center of Koguma’s circulation.  Winds to tropical storm force extended out 140 miles (225 km) from the center of Typhoon Koguma.

Typhoon Koguma will move through an environment that will be unfavorable for intensification of a typhoon during the next 24 hours.  Koguma will move over water where the Sea Surface Temperatures are near 22°C.  It will move under the eastern side of an upper level trough that is east of Japan.  The upper level trough will produce southwesterly winds that will blow toward the top of Koguma’s circulation.  Those winds will cause strong vertical wind shear.  Typhoon Koguma will continue to weaken on Tuesday as it makes a transition to a strong extratropical cyclone.

The upper level trough that is east of Japan will steer Typhoon Koguma quickly toward the northeast during the next 24 hours.  On its anticipated track, Typhoon Koguma will move farther away from Japan.

Typhoon Koguma Weakens

Typhoon Koguma weakened on Sunday as it moved over the Western North Pacific Ocean southeast of Japan.  At 11:00 p.m. EDT on Sunday the center of Typhoon Koguma was located at latitude 29.0°N and longitude 147.6°E which put the center about 655 miles (1060 km) southeast of Tokyo, Japan.  Koguma was moving toward the north at 14 m.p.h. (22 km/h).  The maximum sustained wind speed was 115 m.p.h. (1850 km/h) and there were wind gusts to 145 m.p.h. (235 km/h).  The minimum surface pressure was 954 mb.

Typhoon Koguma weakened on Sunday, but the structure of Koguma was still intact.  A large circular eye with a diameter of 45 miles (75 km) was at the center of Koguma’s circulation.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms revolved around the center of Koguma’s circulation.  Storms near the center of Koguma generated upper level divergence that pumped mass away from the typhoon.  The removal of mass in the upper levels was less than the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure increased on Sunday.

The distribution of wind speeds in Typhoon Koguma was fairly symmetrical.  Winds to typhoon force extended out 65 miles (105 km) from the center of Koguma’s circulation.  Winds to tropical storm force extended out 130 miles (210 km) from the center of Typhoon Koguma.

The Hurricane Intensity Index (HII) for Typhoon Koguma is 20.6. The Hurricane Size Index (HSI) is 19.6 and the Hurricane Wind Intensity Size Index (HWISI) is 40.2. Typhoon Koguma is similar in intensity to Hurricane Rita when Rita hit southwest Louisiana in 2005.  Koguma is not as large as Rita was.

Typhoon Koguma will move through an environment that will be unfavorable for intensification during the next 24 hours.  Koguma will move over water where the Sea Surface Temperatures are near 26°C.  It will move under the eastern side of an upper level trough that is over Japan.  The upper level trough will produce southwesterly winds that will blow toward the top of Koguma’s circulation.  Those winds will cause moderate vertical wind shear.  Moderate vertical wind shear and cooler Sea Surface Temperature will cause Typhoon Koguma to continue to weaken on Monday.

The upper level trough over Japan will steer Typhoon Koguma toward the northeast during the next 24 hours.  On its anticipated track, Typhoon Koguma will stay far to the east of Japan.

Typhoon Koguma Intensifies to Equivalent of a Major Hurricane

Typhoon Koguma intensified to the equivalent of a major hurricane east of the Northern Marianas on Friday.  At 11:00 a.m. EDT on Friday the center of Typhoon Koguma was located at latitude 20.5°N and longitude 153.5°E which put the center about 640 miles (1035 km) east-northeast of Saipan.  Koguma was moving toward the west-northwest at 17 m.p.h. (28 km/h).  The maximum sustained wind speed was 115 m.p.h. (185 km/h) and there were wind gusts to 145 m.p.h. (235 km/h).  The minimum surface pressure was 961 mb.

Typhoon Koguma intensified to the equivalent of a major hurricane on Friday as it was completing an eyewall replacement cycle.  A new larger eye was forming at the center of Koguma’s circulation.  Bands of showers and thunderstorms were revolving around the center of Typhoon Koguma.  Storms near the center of Koguma generated upper level divergence that pumped mass away from the typhoon.  The removal of mass caused the surface pressure to decrease.

Even though Typhoon Koguma was completing an eyewall replacement cycle, the circulation around Koguma was still small for a typhoon over the Western North Pacific Ocean.  Winds to typhoon force extended out 45 miles (75 km) from the center of Koguma’s circulation.  Winds to tropical storm force extended out 105 miles (165 km) from the center of Typhoon Koguma.

The Hurricane Intensity Index (HII) for Typhoon Koguma is 20.6.  The Hurricane Size Index (HSI) is 16.2 and the Hurricane Wind Intensity Size Index (HWISI) is 36.8.  Typhoon Koguma is similar in size and intensity to Hurricane Delta when Delta hit Louisiana in 2020.

Typhoon Koguma will move through an environment that will be favorable for intensification during the next 24 hours.  Koguma will move over water where the Sea Surface Temperatures are near 29°C.  It will move under the southwestern part of an upper level ridge that is over the Central North Pacific Ocean.  The upper level ridge will produce southeasterly winds that will blow toward the top of Koguma’s circulation.  Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification.  Typhoon Koguma will intensify during the next 24 hours.

Typhoon Koguma will move around the southwestern part of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Koguma toward the northwest during the next 24 hours.  On its anticipated track, Typhoon Koguma will pass northeast of the Northern Marianas.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Nolo continued to weaken gradually far to the southeast of Japan.

At 11:00 a.m. EDT on Friday the center of Tropical Storm Nolo was located at latitude 29.7°N and longitude 147.6°E which put the center about 635 miles (1025 km) southeast of Tokyo, Japan.  Nolo was moving toward the northwest at 13 m.p.h. (21 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 991 mb.

Koguma Strengthens to a Typhoon

Former Tropical Storm Koguma strengthened to a typhoon over the Western North Pacific Ocean east of the Northern Marianas on Thursday.  At 5:00 p.m. EDT on Thursday the center of Typhoon Koguma was located at latitude 18.4°N and longitude 157.1°E which put the center about 810 miles (1310 km) east-northeast of Saipan.  Koguma was moving toward the west-northwest at 14 m.p.h. (22 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 980 mb.

Former Tropical Storm Koguma strengthened to a typhoon on Thursday.  The inner end of a rainband wrapped around the southern side of the center of Koguma’s circulation.  Other bands of showers and thunderstorms were revolving around the center of Typhoon Koguma.  Storms near the center of Koguma generated upper level divergence that pumped mass away from the typhoon.  The removal of mass caused the surface pressure to decrease.

The distribution of wind speeds in Typhoon Koguma was fairly symmetrical.  Winds to typhoon force extended out 30 miles (50 km) from the center of Koguma’s circulation.  Winds to tropical storm force extended out 105 miles (165 km) from the center of Typhoon Koguma.

Typhoon Koguma will move through an environment that will be favorable for intensification during the next 24 hours.  Koguma will move over water where the Sea Surface Temperatures are near 29°C.  It will move under the southwestern part of an upper level ridge that is over the Central North Pacific Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Koguma’s circulation.  Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification.  Typhoon Koguma will intensify during the next 24 hours.  Koguma could strengthen to the equivalent of a major hurricane during the weekend.

Typhoon Koguma will move around the southwestern part of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Koguma toward the west-northwest during the next 24 hours.  On its anticipated track, Typhoon Koguma will pass northeast of the Northern Marianas.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Nolo was weakening gradually far to the southeast of Japan.

At 5:00 p.m. EDT on Thursday the center of Tropical Storm Nolo was located at latitude 28.1°N and longitude 150.6°E which put the center about 855 miles (1380 km) east-southeast of Tokyo, Japan.  Nolo was moving toward the west-northwest at 17 m.p.h. (28 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 991 mb.

Typhoon Dujuan Passes Southeast of Honshu

Typhoon Dujuan passed southeast of Honshu on Monday morning.  At 5:00 a.m. EDT on Monday the center of Typhoon Dujuan was located at latitude 34.3°N and longitude 140.8°E which put the center about 110 miles (175 km) south of Tokyo, Japan.  Dujuan was moving toward the northeast at 18 m.p.h. (30 km/h).  The maximum sustained wind speed was 80 m.p.h. (130 km/h) and there were wind gusts to 100 m.p.h. (160 km/h).  The minimum surface pressure was 971 mb.

Typhoon Dujuan strengthened a little more on Monday morning as it passed southeast of Honshu.  Bands of showers and thunderstorms were revolving around the center of Dujuan’s circulation.  Storms near the center of Dujuan generated upper level divergence that pumped mass away to the northeast of the typhoon.  The removal of mass caused the surface pressure to decrease.

The strongest winds were occurring in the eastern side of Typhoon Dujuan.  Winds to typhoon force extended out 35 miles (55 km) in the eastern side of Dujuan’s circulation.  Winds to tropical storm force extended out 210 miles (335 km) from the center of Typhoon Dujuan.

Typhoon Dujuan will move through an environment that will be somewhat favorable for intensification during the next 12 hours.   Dujuan will move over water where the Sea Surface Temperatures are near 27°C.  It will move under the eastern part of an upper level trough that is north of Japan.  The upper level trough will produce southwesterly winds that will blow toward the top of Dujuan’s circulation.  Those winds will cause moderate vertical wind shear. The moderate vertical wind shear will inhibit intensification, but the wind shear may not be enough to prevent intensification.  Typhoon Dujuan could intensify a little more during the next 12 hours.  Dujuan will move over cooler Sea Surface Temperatures later on Monday.  Typhoon Dujuan will also into a region where the upper level winds are stronger on Tuesday.  The cooler Sea Surface Temperatures and stronger upper level winds will cause Typhoon Dujuan to weaken.  The cooler water and stronger upper level winds will also cause Dujuan to make a transition to an extratropical cyclone.

The upper level trough that is north of Japan will steer Typhoon Dujuan toward the northeast during the next 24 hours.  On its anticipated track, Typhoon Dujuan will move away from Honshu.

Typhoon Dujuan South of Honshu

The center of Typhoon Dujuan was south of Honshu on Sunday evening.  At 11:00 p.m. EDT on Sunday the center of Typhoon Dujuan was located at latitude 33.0°N and longitude 139.5°E which put the center about 210 miles (335 km) south-southwest of Tokyo, Japan.  Dujuan was moving toward the northeast at 15 m.p.h. (24 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 974 mb.

Former Tropical Storm Dujuan strengthened back to a typhoon as it moved south of Honshu on Sunday evening.  The inner end of a rainband wrapped around the center of Typhoon Dujuan.  Other bands of showers and thunderstorms were revolving around the center of Dujuan’s circulation.  Storms near the center of Dujuan generated upper level divergence that pumped mass away to the northeast of the typhoon.  The removal of mass caused the surface pressure to decrease.

The strongest winds were occurring in the eastern side of Typhoon Dujuan.  Winds to typhoon force extended out 30 miles (50 km) in the eastern side of Dujuan’s circulation.  Winds to tropical storm force extended out 195 miles (315 km) from the center of Typhoon Dujuan.

Typhoon Dujuan will move through an environment that will be somewhat favorable for intensification during the next 24 hours.  Dujuan will move over water where the Sea Surface Temperatures are near 28°C.  It will move under the southern part of an upper level trough that is north of Japan.  The upper level trough will produce southwesterly winds that will blow toward the top of Dujuan’s circulation.  Those winds will cause moderate vertical wind shear.  The moderate vertical wind shear will inhibit intensification, but the wind shear may not be enough to prevent intensification.  Typhoon Dujuan could intensify on Monday.  Dujuan will move into a region where the upper level winds are stronger on Tuesday.  The stronger upper level winds will cause Typhoon Dujuan to start to weaken.  The stronger upper level winds will also cause Dujuan to make a transition to an extratropical cyclone.

The upper level trough that is north of Japan will steer Tropical Storm Dujuan toward the northeast during the next 24 hours.  On its anticipated track, the center of Tropical Storm Dujuan will pass just south of Tokyo in a few hours.

Tropical Storm Dujuan will bring strong winds and locally heavy rain to Tokyo and eastern Honshu.  Heavy rain could cause floods in some locations.

Tropical Storm Dujuan Moves Toward Honshu

Tropical Storm Dujuan moved toward Honshu on Saturday.  At 11:00 p.m. EDT on Saturday the center of Tropical Storm Dujuan was located at latitude 29.1°N and longitude 137.5°E which put the center about 475 miles (760 km) south-southwest of Tokyo, Japan.  Dujuan was moving toward the northwest at 5 m.p.h. (8 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 978 mb.

Former Typhoon Dujuan weakened slightly on Saturday.  The circulation around Dujuan pulled some drier air into the eastern side of the tropical storm.  Some of the thunderstorms in bands in the eastern side of Tropical Storm Dujuan weakened.  Thunderstorms were still occurring in bands in the other parts of Dujuan’s circulation.  Storms near the center of Dujuan generated upper level divergence that pumped mass away to the northeast of the tropical storm.  The removal of mass in the upper levels was nearly equal to the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure did not change much on Saturday.

The circulation around Tropical Storm Dujuan was large.  Winds to tropical storm force extended out 230 miles (370 km) from the center of Dujuan’s circulation.

Tropical Storm Dujuan will move through an environment that will be somewhat favorable for intensification during the next 24 hours.  Dujuan will move over water where the Sea Surface Temperatures are near 28°C.  It will move under the southern part of an upper level trough that is north of Japan.  The upper level trough will produce southwesterly winds that will blow toward the top of Dujuan’s circulation.  Those winds will cause moderate vertical wind shear. The moderate vertical wind shear will inhibit intensification, but the wind shear may not be enough to prevent intensification.  Tropical Storm Dujuan could intensify a little on Sunday.

The upper level trough that is north of Japan will steer Tropical Storm Dujuan toward the north-northeast during the next 24 hours.  On its anticipated track, the center of Tropical Storm Dujuan will pass just south of Tokyo in a little over 24 hours.

Tropical Storm Dujuan will bring strong winds and locally heavy rain to Tokyo and eastern Honshu.  Heavy rain could cause floods in some locations.

Tropical Storm Chan-hom Brings Wind and Rain to Honshu

Tropical Storm Chan-hom brought wind and rain to central Honshu on Tuesday morning.  At 11:00 a.m. EDT on Tuesday the center of Tropical Storm Chan-hom was located at latitude 36.0°N and longitude 139.0°E which put the center about 25 miles (40 km) north of Tokyo, Japan.  Chan-hom was moving toward the west-southwest at 20 m.p.h. (32 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 994 mb.

The center of Tropical Storm Chan-hom crossed the coast of Honshu northeast of Tokyo on Tuesday morning.

The strongest winds were occurring in the northern side of Tropical Storm Chan-hom.  Winds to tropical storm force extended out 45 miles in the northern half of Chan-hom’s circulation.  The winds in the southern half of Tropical Storm Chan-hom were blowing at less than tropical storm force.

An upper level low south of Japan will steer Tropical Storm Chan-hom toward the west during the next 24 hours.  On its anticipated track, the center of Tropical Storm Chan-hom will move across central Honshu.

Tropical Storm Chan-hom will bring gusty winds and locally heavy rain to parts of central Honshu.  Heavy rain could cause floods in some locations.

Elsewhere over the Western North Pacific Ocean, Tropical Depression Peilou continued to weaken slowly northwest of Wake Island.  At 11:00 a.m. EDT on Tuesday the center of Tropical Depression Peilou was located at latitude 26.7°N and longitude 160.1°E which put the center about 645 miles (1035 km) northwest of Wake Island.  Peilou was moving toward the east-northeast at 17 m.p.h. (28 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 999 mb.

Tropical Storm Chan-hom Moves Toward Japan

Tropical Storm Chan-hom was moving toward Japan on Monday morning.  At 11:00 a.m. EDT on Monday the center of Tropical Storm Chan-hom was located at latitude 35.7°N and longitude 147.1°E which put the center about 460 miles (745 km) east of Tokyo, Japan.  Chan-hom was moving toward the northwest at 12 m.p.h. (19 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 981 mb.

The surface center of Tropical Storm Chan-hom is under the eastern part of an upper level low.  The upper level low is producing southeasterly winds that are blowing toward the top of Chan-hom’s circulation.  Those winds are causing moderate vertical wind shear.  The circulation around Tropical Storm Chan-hom is also puling drier air into the southern and eastern parts of Chan-hom’s circulation.

The combination of the moderate vertical wind shear and the drier air is causing the distribution of thunderstorms in Tropical Storm Chan-hom to be asymmetrical.  Thunderstorms are occurring in bands in the western half of Chan-hom’s circulation.  Bands in the eastern part of Tropical Storm Chan-hom consist primarily of showers and lower clouds.  Storm near the enter of Chan-hom generated upper level divergence that pumped mass away from the tropical storm.  The removal of mass caused the surface pressure to decrease.

The distribution of wind speeds in Tropical Storm Chan-hom was also asymmetrical.  Winds to tropical storm force extended out 145 miles (235 km) in the northern half of Chan-hom’s circulation.  Winds to tropical storm force only extended out 70 miles (110 km) in the southern half of Tropical Storm Chan-hom.

Tropical Storm Chan-hom will move through an environment that will be somewhat favorable for intensification during the next 24 hours.  Chan-hom will move over water where the Sea Surface Temperatures are near 26°C.  However, the upper level low just to the west of the low level center of Chan-hom’s circulation will continue to cause moderate vertical wind shear.  Tropical Storm Chan-hom could intensify a little in spite of the moderate vertical wind shear.

The upper level low just to the west of the surface center of Tropical Storm Chan-hom will steer Chan-hom toward the west during the next 24 hours.  On its anticipated track, the center of Tropical Storm Chan-hom will reach the coast of Honshu northeast of Tokyo in about 24 hours.

Tropical Storm Chan-hom will bring strong winds and locally heavy rain to parts of central Honshu.  Heavy rain is likely to cause floods in some locations.

Elsewhere, Tropical Storm Dolphin continued to drop heavy rain over parts of eastern China and former Tropical Storm Peilou weakened to a tropical depression.

At 8:00 a.m. EDT on Monday the center of Tropical Storm Dolphin was located at latitude 29.0°N and longitude 117.9°E which put the center about 60 miles (95 km) southeast of Jingdezhen, China.  Dolphin was moving toward the north-northwest at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 990 mb.

At 11:00 a.m. EDT on Monday the center of Tropical Depression Peilou was located at latitude 22.1°N and longitude 153.6°E which put the center about 195 miles (315 km) south-southwest of Minami Tori Shima.  Peilou was moving toward the northeast at 20 m.p.h. (32 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 993 mb.

Typhoon Dolphin Hits Eastern China

Typhoon Dolphin hit the coast of eastern China near Wenzhou early on Sunday.  At 5:00 a.m. EDT on Sunday the center of Typhoon Dolphin was located at latitude 28.2°N and longitude 121.4°E which put the center about 50 miles (80 km) east of Wenzhou, China.  Dolphin was moving toward the west-northwest at 14 m.p.h. (22 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 954 mb.

Typhoon Dolphin made landfall on the east coast of China near Wenzhou early on Sunday.  Dolphin was a large typhoon.  Winds to typhoon force extended out 35 miles (55 km) from the enter of Dolphin’s circulation.  Winds to tropical storm force extended out 295 miles (475 km) from the center of Typhoon Dolphin.

The Hurricane Intensity Index (HII) for Typhoon Dolphin is 12.7.  The Hurricane Size Index (HSI) is 16.7 and the Hurricane Wind Intensity Size Index (HWISI) is 29.4.  Typhoon Dolphin is similar in intensity to Hurricane Isaac when Isaac hit southeast Louisiana in 2012.  Typhoon Dolphin is much larger than Isaac was.

Typhoon Dolphin will move around the southern side of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Dolphin toward the west-northwest during the next 24 hours.  On its anticipated track, the center of Typhoon Dolphin will continue to move farther inland over eastern China during the next 24 hours.

Typhoon Dolphin will bring strong winds and heavy rain to parts of eastern China.  Dolphin will bring strong winds and heavy rain to Zhejiang, Anhui, and Jiangsu.  Heavy rain is likely to cause floods in some locations.  Typhoon Dolphin could also produce a storm surge of up to 10 feet (3 meters) along parts of the east coast of China.

Even though Typhoon Dolphin will weaken as it moves farther inland, Dolphin could also drop heavy rain over parts of Henan, Shandong, Hebei, and Shanxi as it moves farther inland.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Chan-hom was still churning east of Japan and Tropical Storm Peilou formed south of Iwo To.

At 5:00 a.m. EDT on Sunday the center of Tropical Storm Chan-hom was located at latitude 32.4°N and longitude 150.5°E which put the center about 650 miles (1050 km) east-southeast of Tokyo, Japan.  Chan-hom was moving toward the west-northwest at 4 m.p.h. (6 km/h).  The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 984 mb.

At 5:00 a.m. EDT on Sunday the center of Tropical Storm Peilou was located at latitude 21.0°N and longitude 143.6°E which put the center about 265 miles (425 km) south-southeast of Iwo To.  Peilou was moving toward the east-southeast at 15 m.p.h. (24 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 998 mb.