Tag Archives: Honshu

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.

Dujuan Strengthens to a Typhoon

Former Tropical Storm Dujuan strengthened to a typhoon on Friday as it moved over the Western North Pacific Ocean northwest of Iwo To.  At 11:00 p.m. EDT on Friday the center of Typhoon Dujuan was located at latitude 26.5°N and longitude 139.4°E which put the center about 140 miles (225 km) northwest of Iwo To.  Dujuan was moving toward the west-northwest at 9 m.p.h. (15 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 978 mb.

Former Tropical Storm Dujuan strengthened to a typhoon on Friday.  The inner end of a rainband wrapped around the southern and eastern side of the center of Typhoon Dujuan.  Thunderstorms were occurring in bands in the northern side of Dujuan’s circulation.  Bands in the southern side of Typhoon Dujuan consisted primarily of showers and lower clouds.  Storms near the center of Dujuan generated upper level divergence that pumped mass away from the typhoon.  The removal of mass caused the surface pressure to decrease.

The strongest winds were occurring close to the center of Typhoon Dujuan.  Winds to typhoon force extended out 20 miles (30 km) from the center of Dujuan’s circulation.  Winds to tropical storm force extended out 250 miles (400 km) in the northern side of Typhoon Dujuan.  Winds to tropical storm force extended out 140 miles (225 km) in the southern half of Dujuan’s circulation.

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 western part of an upper level ridge that is southeast of Japan.  The upper level ridge will produce southerly 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 24 hours.

Typhoon Dujuan will move around the western part of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Dujuan toward the northwest during the next 24 hours.  On its anticipated track, Typhoon Dujuan will move closer to Honshu during the weekend.

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.

Tropical Storm Mekkhala Passes West of Okinawa

The center of Tropical Storm Mekkhala passed west of Okinawa on Thursday.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Mekkhala was located at latitude 27.9°N and longitude 127.5°E which put the center about 80 miles (130 km) northwest of Okinawa.  Mekkhala was moving toward the north-northeast at 9 m.p.h. (15 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 983 mb.

Tropical Storm Mekkhala continued to weaken as it passed west of Okinawa on Thursday.  Mekkhala moved under the southern part of an upper level trough that was over South Korea,  The upper level trough produced westerly winds that blew toward the top of Mekkhala’s circulation.  Those winds caused strong vertical wind shear.  The strong vertical wind shear blew the tops off of most of the thunderstorms in Tropical Storm Mekkhala.  Bands revolving around the center of Mekkhala’s circulation consisted primarily of showers and lower clouds.

The distribution of wind speeds in Tropical Storm Mekkhala became more asymmetrical on Thursday.  Winds to tropical storm force extended out 140 miles (225 km) in the eastern side of Mekkhala’s circulation.  Winds to tropical storm force extended out 90 miles (145 km) in the western side of Tropical Storm Mekkhala.

Tropical Storm Mekkhala will move through an environment that will be unfavorable for intensification during the next 24 hours.  Mekkhala will move over water where the Sea Surface Temperatures are near 26°C.  However, the upper level trough over South Korea will continue to cause strong vertical wind shear.  Tropical Storm Mekkhala could weaken to a tropical depression during the next 24 hours.

Tropical Storm Mekkhala will move around the northwestern part of a high pressure system over the Western North Pacific Ocean.  The high pressure system will steer Mekkhala toward the east-northeast during the next 24 hours.  On its anticipated track, Tropical Storm Mekkhala will be near Tokyo in 36 hours.

Tropical Storm Mekkhala could bring gusty winds to the southern coast of Honshu including Tokyo during the next 48 hours.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Higos strengthened south of Japan.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Higos was located at latitude 26.3°N and longitude 133.9°E which put the center about 155 miles (250 km) east-southeast of Minamidaitojima, Japan.  Higos was moving toward the north at 30 m.p.h. (48 km/h). The maximum sustained wind speed was 65 m.p.h. (105 km/h) and there were wind gusts to 80 m.p.h. (130 km/h).  The minimum surface pressure was 986 mb.

Tropical Storm Jangmi Brings Wind and Rain to Japan

Tropical Storm Jangmi brought wind and rain to parts of Japan on Tuesday.  At 11:00 a.m. EDT on Tuesday the center of Tropical Storm Jangmi was located at latitude 32.8°N and longitude 134.3°E which put the center about 135 miles (215 km) southwest of Osaka, Japan.  Jangmi was moving toward the northeast at 29 m.p.h. (46 km/h).  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were wind gusts to 80 m.p.h. (130 km/h).  The minimum surface pressure was 984 mb.

Tropical Storm Jangmi was bringing wind and rain to parts of Honshu on Tuesday.  A weather station at Kansai International Airport in Osaka (RJBB) reported a sustained wind speed of 43 m.p.h. (68 km/h) and a wind gust of 55 m.p.h. (89 km/h).

Tropical Storm Jangmi was making a transition to an extratropical cyclone on Tuesday.  The circulation around Jangmi was interacting with a stationary front that was just south of Japan.  The interaction with the front was causing the distribution of thunderstorms in Tropical Storm Jangmi to become more asymmetrical.  Thunderstorms were occurring in bands in the eastern and northern parts of Jangmi’s circulation.  Bands in the western and southern parts of Tropical Storm Jangmi consisted primarily of showers and lower clouds.

The circulation around Tropical Storm Jangmi was still large. Winds to tropical storm force extended out 240 miles (390 km) from the center of Jangmi’s circulation.

Tropical Storm Jangmi will move through an environment that will be unfavorable for intensification of a tropical cyclone during the next 24 hours.  Jangmi will move over water where the Sea Surface Temperatures are near 23°C.  It will move under the eastern part of an upper level trough that is over South Korea.  The upper level trough will produce strong southwesterly winds that will blow toward the top of Jangmi’s circulation.  Those winds will cause strong vertical wind shear.  The cool Sea Surface Temperature and the strong vertical wind shear will cause Tropical Storm Jangmi to continue to make a transition to an extratropical cyclone during the next 24 hours.

The upper level trough over South Korea will steer Tropical Storm Jangmi toward the east-northeast during the next 24 hours.  On its anticipated track, the center of Tropical Storm Jangmi will pass near Tokyo in 18 hours.

Tropical Storm Jangmi will continue to bring strong winds and locally heavy rain to parts of Honshu.  Heavy rain could cause flash floods in some locations.

Jangmi Brings Wind and Rain to Okinawa

Tropical Storm Jangmi brought wind and rain to Okinawa on Monday.  At 11:00 a.m. EDT on Monday the center of Tropical Storm Jangmi was located at latitude 27.3°N and longitude 128.0°E which put the center about 25 miles (40 km) northwest of Okinawa.  Jangmi was moving toward the north at 13 m.p.h. (21 km/h).  The maximum sustained wind speed was 65 m.p.h. (105 km/h) and there were wind gusts to 85 m.p.h. (130 km/h).  The minimum surface pressure was 982 mb.

Tropical Storm Jangmi brought wind and rain to Okinawa on Monday.  A weather station at Kadena Air Force Base in Okinawa (RODN) reported a sustained wind speed of 52 m.p.h. (84 km/h) and a wind gust of 71 m.p.h. (115 km/h).

Former Typhoon Jangmi weakened back to a tropical storm Monday.  A large eye with a diameter of 60 miles (95 km) was still present at the center of Tropical Storm Jangmi.  The eye was surrounded by a broken ring of thunderstorms and the strongest winds were occurring in that ring of storms.

The circulation around Tropical Storm Jangmi was pulling drier air around the western and southern parts of Jangmi’s circulation.  Thunderstorms were still occurring in bands in the eastern and northern parts of Tropical Storm Jangmi.  Bands in the western and southern sides of Jangmi’s circulation consisted primarily of showers and lower clouds.

Storms near the center of Jangmi generated upper level divergence that pumped mass away to the northeast of the tropical storm.  However, the removal of mass in the upper levels of the atmosphere was less than the convergence of mass in the lower levels.  So, the surface pressure increased gradually.

The circulation around Tropical Storm Jangmi was still large.  Winds to tropical storm force extended out 205 miles (330 km) from the center of Jangmi’s circulation.

Tropical Storm Jangmi will move through an environment that will be unfavorable for intensification during the next 24 hours.  Jangmi will move over water where the Sea Surface Temperatures are near 26°C. It will move under the eastern part of an upper level trough that is over the east coast of China.  The upper level trough will produce southwesterly winds that will blow toward the top of Jangmi’s circulation.  Those winds will cause the moderate vertical wind shear. Tropical Storm Jangmi will continue to weaken slowly during the next 24 hours.

The upper level trough over the east coast of China will steer Tropical Storm Jangmi toward the northeast during the next 24 hours.  On its anticipated track, the center of Jangmi will move over the northern Ryukyu Islands.  The center of Tropical Storm Jangmi will be southeast of Kyushu in 18 hours.

Tropical Storm Jangmi will bring strong winds and locally heavy rain to the northern Ryukyu Islands.  Heavy rain could cause flash floods in some locations. Jangmi will also bring strong winds and heavy rain to parts of Kyushu, Shikoku, and Honshu.

Tropical Storm Nakri Moves South of Japan

Tropical Storm Nakri moved south of Japan on Saturday.  At 11:00 a.m. EDT on Saturday the center of Tropical Storm Nakri was located at latitude 29.1°N and longitude 132.0°E which put the center about 320 miles (515 km) south-southwest of Kochi, Japan.  Nakri was moving toward the north-northeast at 13 m.p.h. (21 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.

Tropical Storm Nakri started to strengthen on Saturday as it moved south of Japan.  The inner end of a rainband wrapped around the center of Nakri’s circulation.  An eye appeared to be forming at the center of Tropical Storm Nakri.  Bands of showers and thunderstorms were revolving around the center of Nakri’s circulation.  Storms near the center of Nakri generated upper level divergence that pumped mass away to the east of the tropical storm.  The removal of mass caused the surface pressure to decrease.

The size of the circulation around Tropical Storm Nakri was relatively small.  Winds to tropical storm force extended out 105 miles (165 km) from the center of Nakri’s circulation.

Tropical Storm Nakri will move through an environment favorable for intensification during the next 24 hours.  Nakri will move over water where the Sea Surface Temperatures are near 28°C.  It will move under the eastern side of an upper level trough that is west of Japan.  The upper level trough will produce southwesterly winds that will blow toward the top of Nakri’s circulation.  However, the winds in the lower atmosphere will also blow from the west.  So, there will not be a lot of vertical wind shear.  Tropical Storm Nakri will intensify during the next 24 hours.  Nakri could strengthen to a typhoon on Sunday.

The upper level trough that is west of Japan will steer Tropical Storm Nakri toward the northeast during the next 24 hours.  On its anticipated track, Tropical Storm Nakri will move south of Honshu on Sunday.