Typhoon Champi Brings Wind and Rain to Southern Ryukyu Islands

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Typhoon Champi brought wind and rain to the southern Ryukyu Islands and to northeastern Taiwan on Friday.  At 11:00 a.m. EDT on Friday the center of Typhoon Champi was located at latitude 25.3°N and longitude 122.6°E which put the center about 75 miles (120 km) east of Taipei, Taiwan.  Champi was moving toward the north-northwest at 16 m.p.h. (16 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 949 mb.

A weather station on Ishigakijima Island reported a sustained wind speed of 78 m.p.h. (125 km/h).  The weather station also reported 4.94 inches (154.0 mm) of rain.

A weather station in Ohara, Japan reported a sustained wind speed of 75 m.p.h. (121 km/h).

A weather station on Yonagunijima Island reported a sustained wind speed of 66 m.p.h. (107 km/h).  The weather station also reported 8.33 inches (211.5 mm) of rain.

Typhoon Champi was the equivalent of a major hurricane on Friday morning.  Winds to typhoon force extended out 85 miles (135 km) from the center of Champi’s circulation.  Winds to tropical storm force extended out 250 miles (400 km) from the center of Typhoon Champi.

The Hurricane Intensity Index (HII) for Typhoon Champi was 20.6.  The Hurricane Size Index (HSI) was 31.8 and the Hurricane Wind Intensity Size Index (HWISI) was 52.4.  Typhoon Champi was similar in intensity to Hurricane Irma when Irma hit south Florida in 2017.  Champi is larger than Irma was.

Typhoon Champi will move around the western end of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Champi toward the north during the next 24 hours.  On its anticipated track, Typhoon Champi will remain east of China.

Typhoon Champi will move through an environment that will be unfavorable for intensification during the next 24 hours.  Champi 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 near the east coast of China.  The upper level trough will produce strong southwesterly winds that will blow toward the top of Champi’s circulation.  Those winds will cause strong vertical wind shear.  Champi will also continue to move through a mass of drier air.  Typhoon Champi is likely to weaken steadily during the next 24 hours because of the effects of strong vertical wind shear and drier air.

Elsewhere over the Western North Pacific Ocean, Tropical Depression 30W formed northwest of Kwajalein.  At 11:00 a.m. EDT on Friday the center of Tropical Depression 30W was located at latitude 10.9°N and longitude 166.3°E which put the center about 185 miles (300 km) northwest of Kwajalein.  The tropical depression moving toward the northwest at 2 m.p.h. (3 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 1004 mb.

Vance Strengthens to a Hurricane

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Former Tropical Storm Vance strengthened to a hurricane as it moved over the Eastern North Pacific Ocean south of Mexico on Thursday night.  At 5:00 a.m. EDT on Friday the center of Hurricane Vance was located at latitude 10.9°N and longitude 102.1°W which put the center about 580 miles (930 km) south-southeast of Manzanillo, Mexico.  Vance was moving toward the north-northwest at 6 m.p.h. (10 km/h).  The maximum sustained wind speed was 85 m.p.h. (135 km/h) and there were wind gusts to 100 m.p.h. (160 km/h).  The minimum surface pressure was 982 mb.

Former Tropical Storm Vance strengthened to a hurricane on Thursday night.

The inner end of a rainband wrapped around the center of Hurricane Vance.  An eye appeared to be forming at the center of Vance’s circulation.  Bands of showers and thunderstorms were revolving around the center of Hurricane Vance.  Storms near the center generated upper level divergence that pumped mass away from the hurricane.  The removal of mass caused the surface pressure to decrease.

The strongest winds were occurring in the northern side of Hurricane Vance.  Winds to hurricane force extended out 35 miles (55 km) in the northern half of Vance’s circulation.  Winds to tropical storm force extended out 200 miles (320 km) from the center of Hurricane Vance.

Hurricane Vance will move through an environment favorable for intensification during the next 24 hours.  Vance will move over water where the Sea Surface Temperatures are near 30°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Hurricane Vance will intensify during the next 24 hours.  Vance could intensify rapidly at times.  Vance could strengthen to a major by the weekend.

Hurricane Vance will move around the southwestern part of a high pressure system that is over southern Mexico.  The high pressure system will steer Vance toward the north-northwest during the next 24 hours.  On its anticipated track, Hurricane Vance will gradually move closer to the west coast of Mexico.

Typhoon Champi Approaches Southern Ryukyu Islands

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Typhoon Champi was approaching the southern Ryukyu Islands on Wednesday evening.  At 11:00 p.m. EDT on Wednesday the center of Typhoon Champi was located at latitude 20.6°N and longitude 125.7°E which put the center about 295 miles (475 km) south-southeast of Ishigakijima, Japan.  Champi was moving toward the west-northwest at 11 m.p.h. (17 km/h).  The maximum sustained wind speed was 130 m.p.h. (210 km/h) and there were wind gusts to 160 m.p.h. (260 km/h).  The minimum surface pressure was 940 mb.

Typhoon Champi weakened on Wednesday.  Even though Champi weakened, it was still a very well organized typhoon.  A circular eye with a diameter of 35 miles (55 km) was at the center of Champi’s circulation.  Bands of showers and thunderstorms were revolving around the the center of Typhoon Champi.  Storms near the center of Champi 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 Wednesday.

The circulation around Typhoon Champi was large.  Winds to typhoon force extended out 100 miles (160 km) from the center of Champi’s circulation.  Winds to tropical storm force extended out 345 miles (555 km) from the center of Typhoon Champi.

The Hurricane Intensity Index (HII) for Typhoon Champi is 25.1.  The Hurricane Size Index (HSI) is 34.2 and the Hurricane Wind Intensity Size Index (HWISI) is 59.3.  Typhoon Champi is similar in size to Hurricane Ivan when Ivan hit the northern Gulf Coast in 2004.  Champi is stronger than Ivan was.

Typhoon Champi will move through an environment that will be unfavorable for intensification during the next 24 hours.  Champi 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 near the east coast of China.  The upper level trough will produce southwesterly winds that will blow toward the top of Champi’s circulation.  Those winds will cause the vertical wind shear to increase.   Champi will also move into a region of drier air on Thursday.  Typhoon Champi is likely to weaken during the next 24 hours because of more vertical wind shear and drier air.

Typhoon Champi 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 Champi toward the north-northwest during the next 24 hours.  On its anticipated track, the center of Typhoon Champi will be near Ishigakijima in 24 hours.

Typhoon Champi will bring strong winds and heavy rain to the southern Ryukyu Islands.  Heavy rain is likely to cause flash floods in some locations.

Typhoon Champi could also bring strong winds and heavy rain to parts of Taiwan.

Tropical Cyclone Agueda Passes North of Madagascar

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Tropical Cyclone Agueda passed north of Madagascar on Wednesday.  At 5:00 p.m. EDT on Wednesday the center of Tropical Cyclone Agueda was located at latitude 6.1°S and longitude 50.7°E which put the center about 400 miles (645 km) north of Antsiranana, Madagascar.  Agueda was moving toward the west-southwest 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 997 mb.

Tropical Cyclone Agueda strengthened on Wednesday.  Thunderstorms were occurring near the center of Agueda’s circulation.  Bands of showers and thunderstorms were revolving  around the center of Tropical Cyclone Agueda.  Storms near the center of Agueda generated upper level divergence that pumped mass away from the tropical cyclone.  The removal of mass caused the surface pressure to decrease.

The circulation around Tropical Cyclone Agueda was small.  Winds to tropical storm force extended out 40 miles (65 km) from the center of Agueda’s circulation.

Tropical Cyclone Agueda will move through an environment that will become unfavorable for intensification during the next 24 hours.  Agueda will move over water where the Sea Surface Temperatures are near 27°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  However, Agueda will move into a region of drier air on Thursday.  Tropical Cyclone Agueda is likely to weaken when it moves into the region of drier air.

Tropical Cyclone Agueda will move around the northern side of a high pressure system that is over the South Indian Ocean.  The high pressure system will steer Agueda toward the west-southwest during the next 24 hours.  On its anticipated track, Tropical Cyclone Agueda will move northwest of Madagascar on Thursday.

Tropical Storm Vance Forms South of Mexico

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Tropical Storm Vance formed over the Eastern North Pacific Ocean south of Mexico on Wednesday.  At 5:00 p.m. EDT on Wednesday the center of Tropical Storm Vance was located at latitude 9.4°N and longitude 99.8°W which put the center about 520 miles (835 km) south of Acapulco, Mexico.  Vance was moving toward the west at 7 m.p.h. (11 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.

A low pressure system over the Eastern North Pacific Ocean south of Mexico strengthened on Wednesday and the U.S. National Hurricane Center designated the system as Tropical Storm Vance.

More thunderstorms developed in bands revolving around the center of Tropical Storm Vance on Wednesday afternoon.  Storms near the center of Vance’s circulation began to generate upper level divergence that pumped mass away from the tropical storm.  The removal of mass caused the surface pressure to decrease.

The strongest winds were occurring in the northern side of Tropical Storm Vance.  Winds to tropical storm force extended out 70 miles (110 km) in the northern side of Vance’s circulation.  The winds in the southern part of Tropical Storm Vance were blowing at less than tropical storm force.

Tropical Storm Vance will move through an environment favorable for intensification during the next 24 hours.  Vance will move over water where the Sea Surface Temperatures are near 30°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Tropical Storm Vance will intensify during the next 24 hours.  Vance could strengthen to a hurricane on Thursday.

Tropical Storm Vance will move around the southwestern part of a high pressure system that is over southern Mexico.  The high pressure system will steer Vance toward the northwest during the next 24 hours.  On its anticipated track, Tropical Storm Vance will start to move closer to the west coast of Mexico on Thursday.

Subtropical Storm Josephine Develops Off East Coast

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Subtropical Storm Josephine developed off the East Coast of the U.S. on Wednesday.  At 5:00 p.m. EDT on Wednesday the center of Subtropical Storm Josephine was located at latitude 37.4°N and longitude 69.5°W which put the center about 265 miles (425 km) south of Nantucket, Massachusetts.  Josephine was moving toward the north at 6 m.p.h. (10 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 990 mb.

The U.S. National Hurricane Center designated a low pressure system off the East Coast of the U.S. as Subtropical Storm Josephine on Wednesday afternoon.

Subtropical Storm Josephine made a transition from an extratropical cyclone to a subtropical cyclone on Wednesday.  The warm front and cold front that had been attached to the low pressure system dissipated.  Even though the fronts had dissipated, the distribution of thunderstorms in Subtropical Storm Josephine was asymmetrical.  Thunderstorms were occurring in bands in the northern and western parts of Josephine’s circulation.  Bands in the eastern and southern parts of Josephine consisted primarily of showers and lower clouds.

The distribution of wind speeds in Subtropical Storm Josephine was also asymmetrical.  Winds to tropical storm force extended out 415 miles (665 km) in the northern half of Josephine’s circulation.  Winds to tropical storm force extended out 150 miles (240 km) in the southern half of Subtropical Storm Josephine.

Subtropical Storm Josephine will move through an environment favorable for the intensification of a subtropical storm during the next 24 hours.  Josephine will move over water where the Sea Surface Temperatures are near 24°C.  It will move under the southeastern part of an upper level trough that will be over the Great Lakes.  The upper level trough will produce southwesterly winds that will blow toward the top of Josephine’s circulation.  Those winds will cause strong vertical wind shear.  However, the upper level winds may also contribute to upper level divergence.  Subtropical Storm Josephine could intensify on Thursday because of the upper level divergence.

The upper level trough over the Great Lakes will steer Subtropical Storm Josephine toward the northeast during the next 24 hours.  On its anticipated track, Subtropical Storm Josephine will pass south of Nova Scotia on Thursday.

Intense Typhoon Champi Churns West

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Intense Typhoon Champi churned westward over the Western North Pacific Ocean on Tuesday.  At 5:00 p.m. EDT on Tuesday the center of Typhoon Champi was located at latitude 17.7°N and longitude 130.9°E which put the center about 670 miles (1080 km) south-southeast of Okinawa.  Champi was moving toward the west-northwest at 17 m.p.h. (28 km/h).  The maximum sustained wind speed was 185 m.p.h. (295 km/h) and there were wind gusts to 225 m.p.h. (360 km/h).  The minimum surface pressure was 895 mb.

Intense Typhoon Champi got even stronger on Tuesday.  A circular eye with a diameter of 35 miles (55 km) was at the center of Champi’s circulation.  Bands of showers and thunderstorms were revolving around the the center of Typhoon Champi.  Storms near the center of Champi generated upper level divergence that pumped mass away from the typhoon.  The removal of mass caused the surface pressure to decrease.

The circulation around Typhoon Champi was large.  Winds to typhoon force extended out 100 miles (160 km) from the center of Champi’s circulation.  Winds to tropical storm force extended out 290 miles (465 km) from the center of Typhoon Champi.

The Hurricane Intensity Index (HII) for Typhoon Champi is 44.1.  The Hurricane Size Index (HSI) is 30.4 and the Hurricane Wind Intensity Size Index (HWISI) is 74.5.  Typhoon Champi is similar in intensity to Hurricane Dorian when Dorian hit the Bahamas in 2019.  Champi is much larger than Dorian was.

Typhoon Champi will move through an environment that will be favorable for an intense typhoon during the next 24 hours.  Champi will move over water where the Sea Surface Temperatures are near 28°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Typhoon Champi could maintain its intensity during the next 24 hours unless the inner end of a rainband wraps around the existing eye and eyewall.  If concentric eyewalls form, then an eyewall replacement cycle would cause Champi to weaken.

Typhoon Champi 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 Champi toward the west-northwest during the next 24 hours.  On its anticipated track, Typhoon Champi will continue to move toward Taiwan and the southern Ryukyu Islands.  Champi could approach the southern Ryukyu Islands in 48 hours.

Tropical Cyclone Agueda Forms West of Seychelles

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Tropical Cyclone Agueda formed over the South Indian Ocean west of the Seychelles on Tuesday.  At 5:00 p.m. EDT on Tuesday the center of Tropical Cyclone Agueda was located at latitude 5.2°S and longitude 52.5°E which put the center about 180 miles (290 km) west of the Seychelles.  Agueda was moving toward the west at 7 m.p.h. (11 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 1003 mb.

A low pressure system over the South Indian Ocean west of the Seychelles strengthened on Tuesday and Meteo France la Reunion designated the system as Tropical Cyclone Agueda.

Thunderstorms were forming near the center of Tropical Cyclone Agueda.  Thunderstorms were also occurring in bands in the western side of Agueda’s circulation.  Bands in the eastern side of Tropical Cyclone Agueda consisted primarily of showers and lower clouds.  Storms near the center of Agueda generated upper level divergence that pumped mass away to the west of the tropical cyclone.  The removal of mass caused the surface pressure to decrease.

The circulation around Tropical Cyclone Agueda was small.  Winds to tropical storm force extended out 50 miles (80 km) from the center of Agueda’s circulation.

Tropical Cyclone Agueda will move through an environment that will be somewhat favorable for intensification during the next 24 hours.  Agueda will move over water where the Sea Surface Temperatures are near 27°C.  It will move under the northern part of an upper level ridge that is over the South Indian Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Agueda’s circulation.  Those winds will cause moderate vertical wind shear.  The vertical wind shear will inhibit intensification, but the wind shear may not be enough to prevent intensification.  Tropical Cyclone Agueda could intensify during the next 24 hours.

Tropical Cyclone Agueda will move around the northern side of a high pressure system that is over the South Indian Ocean.  The high pressure system will steer Agueda toward the west-southwest during the next 24 hours.  On its anticipated track, Tropical Cyclone Agueda will pass north of Madagascar later this week.

Typhoon Champi Strengthens to Equivalent of Cat. 5 Hurricane

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Typhoon Champi strengthened to the equivalent of a Category 5 hurricane on the Saffir-Simpson Scale as it moved over the Western North Pacific Ocean north of Yap on Sunday night.  At 5:00 a.m. EDT on Monday the center of Typhoon Champi was located at latitude 14.6°N and longitude 137.9°E which put the center about 330 miles (535 km) north of Yap.  Champi was moving toward the west-northwest at 9 m.p.h. (15 km/h).  The maximum sustained wind speed was 160 m.p.h. (260 km/h) and there were wind gusts to 105 m.p.h. (315 km/h).  The minimum surface pressure was 917 mb.

Typhoon Champi intensified to the equivalent of a Category 5 hurricane on Saturday night.  A circular eye with a diameter of 30 miles (50 km) was at the center of Champi’s circulation.  Bands of showers and thunderstorms were revolving around the the center of Typhoon Champi.  Storms near the center of Champi generated upper level divergence that pumped mass away from the typhoon.  The removal of mass caused the surface pressure to decrease.

The size of the circulation around Typhoon Champi increased on Sunday.  Winds to typhoon force extended out 65 miles (105 km) from the center of Champi’s circulation.  Winds to tropical storm force extended out 220 miles (350 km) from the center of Typhoon Champi.

The Hurricane Intensity Index (HII) for Typhoon Champi is 35.0.  The Hurricane Size Index (HSI) is 20.8 and the Hurricane Wind Intensity Size Index (HWISI) is 55.8. Typhoon Champi is similar in size and intensity to Hurricane Maria when Maria hit Puerto Rico in 2017.

Typhoon Champi will move through an environment that will be favorable for intensification during the next 24 hours.  Champi will move over water where the Sea Surface Temperatures are near 28°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Typhoon Champi could intensify during the next 24 hours unless the inner end of a rainband wraps around the existing eye and eyewall.  If concentric eyewalls form, then an eyewall replacement cycle would cause Champi to weaken.

Typhoon Champi 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 Champi toward the west-northwest during the next 24 hours.  On its anticipated track, Typhoon Champi will move toward Taiwan and the southern Ryukyu Islands.

Hurricane Trudy Rapidly Weakens

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Hurricane Trudy weakened rapidly on Sunday evening as it moved over the Eastern North Pacific Ocean west of Mexico.  At 11:00 p.m. EDT on Sunday the center of Hurricane Trudy was located at latitude 19.7°N and longitude 107.6°W which put the center about 130 miles (215 km) west-southwest of Cabo Corrientes, Mexico.  Trudy was moving toward the northwest at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 80 m.p.h. (130 km/h) and there were wind gusts to 95 m.p.h. (150 km/h).  The minimum surface pressure was 984 mb.

An upper level trough that was over Baja California was producing strong westerly winds that were blowing toward the top of Hurricane Trudy.  Those winds were causing strong vertical wind shear.  The strong vertical wind shear was causing Trudy to weaken rapidly on Sunday evening.  The strong upper level winds also blew the tops off of many of the thunderstorms in Hurricane Trudy.  There was much less upper level divergence that pumped less mass away from the hurricane.  The removal of mass in the upper levels was much less than the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure started to increase rapidly.

The size of the circulation around Hurricane Trudy was getting smaller on Sunday evening.  Winds to hurricane force extended our 25 miles (40 km) from the center of Trudy’s circulation.  Winds to tropical storm force extended out 90 miles (145 km) from the center of Hurricane Trudy.

Hurricane Trudy will move through an environment that will be unfavorable for intensification during the next 24 hours.  Trudy will move over water where the Sea Surface Temperatures are near 30°C.  However, the upper level trough over Baja California will continue to cause strong vertical wind shear.  The strong vertical wind shear will cause Hurricane Trudy to weaken to a tropical storm on Monday.

Since the strong vertical wind shear blew the tops off of many of the thunderstorms in Hurricane Trudy, Trudy will be steered by the winds lower in the atmosphere.  A high pressure system over northern Mexico will steer Trudy toward the west during the next 24 hours.  On its anticipated track, Hurricane Trudy will move farther away from Mexico on Monday.