Monthly Archives: August 2025

Tropical Storm Erin Forms West of Cabo Verde

Tropical Storm Erin formed over the eastern Atlantic Ocean west of the Cabo Verde Islands on Monday morning.  At 11:00 a.m. EDT on Monday the center of Tropical Storm Erin was located at latitude 17.4°N and longitude 28.0°W which put the center about 280 miles (455 km) west-northwest of the Cabo Verde Islands.  Erin was moving toward the west at 20 m.p.h. (32 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 1004 mb.

A low pressure system over the eastern Atlantic Ocean west of the Cabo Verde Islands strengthened on Monday morning and the U.S. National Hurricane Center designated the system as Tropical Storm Erin.

The circulation around Tropical Storm Erin exhibited more organization on Monday morning.  More thunderstorms formed near the center of Erin’s circulation.  Thunderstorms were also occurring in bands revolving around the center of Tropical Storm Erin.  Storms near the center of Erin started to generate upper level divergence that was pumping mass away from the tropical storm.

The strongest winds were occurring in the northern part of Tropical Storm Erin.  Winds to tropical storm force extended out 35 miles (55 km) in the northern half of Erin’s circulation.  The winds in the southern side of Tropical Storm Erin were blowing at less than tropical storm force.

Tropical Storm Erin will move through an environment somewhat favorable for intensification during the next 24 hours.  Erin will move over water where the Sea Surface Temperatures are near 26°C.  It will move under the southern part of an upper level ridge over the eastern Atlantic Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Erin’s circulation.  The winds in the lower levels of the atmosphere will also blow from the east.  So, there will be little vertical wind shear.  Erin will move through a region of drier air later today.  The drier air will inhibit intensification in the short term.  Tropical Storm Erin could intensify slowly during the next 24 hours.  Erin will move over warmer water later this week.  Tropical Storm Erin is likely to strengthen to a hurricane later this week.

Tropical Storm Erin will move around the southern side of a high pressure system over the eastern Atlantic Ocean.  The high pressure system will steer Erin toward the west during the next 24 hours.  On its anticipated track, Tropical Storm Erin will move away from the Cabo Verde Islands.

Tropical Storm Podul Churns Westward

Tropical Storm Podul churned westward over the Western North Pacific Ocean on Sunday.  At 11:00 p.m. EDT on Sunday the center of Tropical Storm Podul was located at latitude 21.2°N and longitude 132.7°E which put the center about 510 miles (820 km) southeast of Okinawa.  Podul was moving toward the west at 14 m.p.h. (22 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 structure of Tropical Storm Podul did not change much on Sunday.  An upper level ridge over China and Japan continue to produce northeasterly winds that blew toward the top of Podul’s circulation.  Those winds caused moderate vertical wind shear.  The wind shear was caused the distribution of thunderstorms in Tropical Storm Podul to be asymmetrical.  Thunderstorms were occurring in bands in the southern half of Podul’s circulation.  Bands in the northern side of Tropical Storm Podul consisted primarily of showers and lower clouds.

The circulation around Tropical Storm Podul was small.  Winds to tropical storm force extended out 75 miles (120 km) from the center of Podul’s circulation.

Tropical Storm Podul will move through an environment that will be somewhat favorable for intensification during the next 24 hours.  Podul will move over water where the Sea Surface Temperatures are near 29°C.  However, the upper level ridge over China and Japan will continue to cause vertical wind shear.  The vertical wind shear will continue to  inhibit intensification.  Tropical Storm Podul could intensify slowly during the next 24 hours if the wind shear does not get any stronger.  Podul could strengthen to a typhoon on Monday.

Tropical Storm Podul will move around the southern side of a high pressure system that is south of Japan. The high pressure system will steer Podul toward the west during the next 24 hours.  On its anticipated track, Tropical Storm Podul will approach the southern Ryukyu Islands in 36 hours.  Podul could approach Taiwan in 48 hours.

Henriette Rapidly Intensifies to a Hurricane

Former Tropical Storm Henriette rapidly intensified to a hurricane northeast of Hawaii on Sunday.  At 5:00 p.m. EDT on Sunday the center of Hurricane Henriette was located at latitude 25.7°N and longitude 152.5°W which put the center about 455 miles (735 km) northeast of Honolulu, Hawaii.  Henriette was moving toward the northwest at 17 m.p.h. (28 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 990 mb.

Former Tropical Storm Henriette rapidly intensified to a hurricane northeast of Hawaii on Sunday.  The inner end of a rainband wrapped around the center of Henriette’s circulation.  A circular eye with a diameter of 15 miles (24 km) formed at the center of Hurricane Henriette.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that rings of storms.  Bands of showers and thunderstorms were revolving around the center of Henriette’s circulation.  Storms near the center of Henriette generated upper level divergence that pumped mass away from the hurricane.  The removal of mass caused the surface pressure to decrease.

The circulation around Hurricane Henriette was small.  Winds to hurricane force extended out 20 miles (30 km) from the center of Henriette’s circulation.  Winds to tropical storm force extended out 70 miles (110 km) from the center of Hurricane Henriette.

Hurricane Henriette will move through an environment favorable for intensification during the next 24 hours.  Henriette will move over water where the Sea Surface Temperatures are near 26°C.  It will move under the middle of an upper level trough that is east of Hawaii.  The upper level winds are weak near the middle of the trough and there will be little vertical wind shear. Hurricane Henriette will intensify during the next 24 hours.  Henriette could continue to intensify rapidly.

Hurricane Henriette will move around the southwestern part of a high pressure system over the central North Pacific Ocean.  The high pressure system will steer Henriette toward the northwest during the next 24 hours.  On its anticipated track, Hurricane Henriette will pass well to the north of Hawaii.

Elsewhere, Tropical Storm Ivo continued to churn west of Baja California. At 5:00 p.m. EDT on Sunday the center of Tropical Storm Ivo was located at latitude 22.1°N and longitude 117.2°W which put the center about 470 miles (755 km) west of the southern tip of Baja California.  Ivo 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 1006 mb.

Tropical Storm Henriette Passes Northeast of Hawaii

Tropical Storm Henriette was passing northeast of Hawaii on Sunday.  At 5:00 a.m. EDT on Sunday the center of Tropical Storm Henriette was located at latitude 23.8°N and longitude 150.3°W which put the center about 420 miles (675 km) northeast Hilo, Hawaii.  Henriette was moving toward the northwest 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 1006 mb.

Former Tropical Storm Henriette strengthened back to a tropical storm as it moved northeast of Hawaii on Sunday.  More thunderstorms former near the center of Henriette’s circulation.  The inner end of a rainband wrapped much of the way around the center of Tropical Storm Henriette.  A clear area was forming at the center of Henriette.  Storms near the center of Henriette generated upper level divergence that pumped mass away from the tropical storm.

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

Tropical Storm Henriette will move through an environment favorable for intensification during the next 24 hours.  Henriette will move over water where the Sea Surface Temperatures are near 26°C.  It will move under the middle of an upper level trough that is east of Hawaii.  The upper level winds are weak near the middle of the trough and there will be little vertical wind shear.  Tropical Storm Henriette will intensify during the next 24 hours.

Tropical Storm Henriette will move around the southwestern part of a high pressure system over the Eastern North Pacific Ocean.  The high pressure system will steer Henriette toward the northwest during the next 24 hours.  On its anticipated track, Tropical Storm Henriette will pass well to the north of Hawaii.

Elsewhere, Tropical Storm Ivo was weakening southwest of Baja California.  At 5:00 a.m. EDT on Sunday the center of Tropical Storm Ivo was located at latitude 21.5°N and longitude 114.9°W which put the center about 335 miles (535 km) west-southwest of the southern tip of Baja California.  Ivo was moving toward the west-northwest at 8 m.p.h. (13 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 1006 mb.

Tropical Storm Podul Passes South of Iwo To

Tropical Storm Podul passes south of Iwo To on Saturday.  At 11:00 a.m. EDT on Saturday the center of Tropical Storm Podul was located at latitude 21.6°N and longitude 140.4°E which put the center about 230 miles (370 km) south of Iwo To.  Podul was moving toward the west at 9 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 998 mb.

Tropical Storm Podul was maintaining its intensity on Saturday as it passed south of Iwo To.  An upper level ridge over China and Japan was producing northeasterly winds that were blowing toward the top of Podul’s circulation.  Those winds were causing moderate vertical wind shear.  The wind shear was causing the distribution of thunderstorms in Tropical Storm Podul to be asymmetrical.  Thunderstorms were occurring in bands in the southern half of Podul’s circulation.  Bands in the northern side of Tropical Storm Podul consisted primarily of showers and lower clouds.

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

Tropical Storm Podul will move through an environment that will be somewhat favorable for intensification during the next 24 hours.  Podul will move over water where the Sea Surface Temperatures are near 29°C.  However, the upper level ridge over China and Japan will continue to cause moderate vertical wind shear.  The wind shear will inhibit intensification.  Tropical Storm Podul could intensify slowly during the next 24 hours if the wind shear does not get any stronger.

Tropical Storm Podul will move around the southern side of a high pressure system over Japan.  The high pressure system will steer Podul toward the west during the next 24 hours.  On its anticipated track, Tropical Storm Podul will move toward the southern Ryukyu Islands.

Tropical Storm Ivo Moves South of Baja California

Tropical Storm Ivo moved south of Baja California on Friday.  At 5:00 p.m. EDT on Friday the center of Tropical Storm Ivo was located at latitude 20.4°N and longitude 111.2°W which put the center about 190 miles (310 km) south-southwest of the southern tip of Baja California.  Ivo was moving toward the west 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 80 m.p.h. (130 km/h).  The minimum surface pressure was 999 mb.

Tropical Storm Ivo exhibited much more organization on Friday after it moved south of Baja California.  The inner end of a rainband wrapped around the western side of the center of Ivo’s circulation.  Other bands of showers and thunderstorms were revolving around the center of Tropical Storm Ivo.  Storms near the center of Ivo generated upper level divergence that pumped mass away from the tropical storm.  The removal of mass caused the surface pressure to decrease.

The circulation around Tropical Storm Ivo was small.  Winds to tropical storm force extended out 35 miles (55 km) from the center of Ivo’s circulation.

Tropical Storm Ivo will move through an environment mostly favorable for intensification during the next 24 hours.  Ivo will move over water where the Sea Surface Temperatures are near 27°C.  It will move under the southern side of an upper level ridge over Mexico and the Eastern North Pacific Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Ivo’s circulation.  However, the winds in the lower atmosphere will also blow from the east.  Since the winds in the upper and lower levels of the atmosphere will blow from the same direction, there will be less vertical wind shear.  Tropical Storm Ivo is likely to intensify during the next 24 hours.  Ivo could strengthen to a hurricane on Saturday.  Ivo will move over cooler water on Sunday which will cause it to weaken.

Tropical Storm Ivo will move around the southern side of a high pressure system that is over Mexico and the eastern North Pacific Ocean.  The high pressure system will steer Ivo toward the west during the next 24 hours.  On its anticipated track, Tropical Storm Ivo will move away from Baja California during the weekend.

Tropical Storm Ivo Moves Southeast of Baja California

Tropical Storm Ivo moved southeast of Baja California on Thursday evening.  At 5:00 p.m. EDT on Thursday the center of Tropical Storm Ivo was located at latitude 19.7°N and longitude 107.3°W which put the center about 275 miles (445 km) southeast of the southern tip of Baja California.  Ivo was moving toward the northwest at 22 m.p.h. (35 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 1001 mb.

Even though Tropical Storm Ivo strengthened on Thursday, its structure did not change a lot.  Thunderstorms were still forming near the center of Ivo’s circulation.  Thunderstorms were also occurring in bands in the southern and eastern parts of Tropical Storm Ivo.  Bands in the northern and western parts of Ivo’s circulation consisted primarily of showers and lower clouds.

The circulation around Tropical Storm Ivo was small.  Winds to tropical storm force extended out 45 miles (75 km) from the center of Ivo’s circulation.

Tropical Storm Ivo will move through an environment mostly favorable for intensification during the next 24 hours.  Ivo will move over water where the Sea Surface Temperatures are near 29°C.  It will move under the southern side of an upper level ridge over Mexico.  The upper level ridge will produce easterly winds that will blow toward the top of Ivo’s circulation.  However, the winds in the lower atmosphere will also blow from the east.  Since the winds in the upper and lower levels of the atmosphere will blow from the same direction, there will be less vertical wind shear.  Even though Tropical Storm Ivo will move through an environment most favorable for intensification, Ivo may not intensify a lot on Friday as long as it continues to move quickly toward the west-northwest.  If Tropical Storm Ivo starts to move more slowly, then it could intensify again.

Tropical Storm Ivo will move around the southern side of a high pressure system that is over Mexico.  The high pressure system will steer Ivo toward the west-northwest during the next 24 hours.  On its anticipated track, Tropical Storm Ivo will move south of Baja California on Friday.

Elsewhere over the Eastern North Pacific Ocean, Tropical Storm Henriette weakened slowly as it approached the Central Pacific.  At 5:00 p.m. EDT on Thursday the center of Tropical Storm Henriette was located at latitude 19.1°N and longitude 138.4°W which put the center about 1090 miles (1750 km) east Hilo, Hawaii.  Henriette was moving toward the west at 16 m.p.h. (26 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 1007 mb.

Tropical Storm Podul Forms North of Saipan

Tropical Storm Podul formed over the Western North Pacific Ocean north of Saipan on Thursday.  At 5:00 p.m. EDT on Thursday the center of Tropical Storm Podul was located at latitude 19.7°N and longitude 145.9°E which put the center about 290 miles (470 km) north of Saipan.  Podul was moving toward the northwest at 11 m.p.h. (17 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 Western North Pacific Ocean north of Saipan strengthened on Thursday and the Japan Meteorological Agency designated the system as Tropical Storm Podul.

The circulation around Tropical Storm Podul was small.  Thunderstorms were occurring in bands south and east of the center of Podul’s circulation.  Bands in the rest of Tropical Storm Podul consisted primarily of showers and lower clouds.  Storms near the center of Podul started to generate upper level divergence that was beginning to pump mass away from the tropical storm.

The strongest winds in Tropical Storm Podul were occurring in the thunderstorms southeast of the center of circulation.  Winds to tropical storm force extended out 60 miles (95 km) in the southeastern quadrant of Podul’s circulation.  The winds in the other parts of Tropical Storm Podul were blowing at less than tropical storm force.

Tropical Storm Podul will move through an environment favorable for intensification during the next 24 hours.  Podul will move over water where the Sea Surface Temperatures are near 29°C.   It will move under the southern side of an upper level ridge that is south of Japan.  The upper level ridge will produce easterly winds that will blow toward the top of Podul’s circulation.  Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification.  Tropical Storm Podul will intensify during the next 24 hours.  Podul is likely to strengthen to a typhoon during the weekend.

Tropical Storm Podul will move around the southern side of a high pressure system that is south of Japan.  The high pressure system will steer Podul toward the west during the next 24 hours.  On its anticipated track, Tropical Storm Podul will move away from the Marianas.  Podul could approach Taiwan in a few days.

Tropical Cyclone Awo Forms Over South Indian Ocean

Tropical Cyclone Awo formed over the South Indian Ocean west of Diego Garcia on Thursday.  At 11:00 a.m. EDT on Thursday the center of Tropical Cyclone Awo was located at latitude 7.0°S and longitude 60.5°E which put the center about 1000 miles (1615 km) north-northeast of La Reunion.  Awo 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.

A low pressure system over the South Indian Ocean west of Diego Garcia strengthened on Thursday morning and Meteo France La Reunion designated the system as Tropical Cyclone Awo.

More thunderstorms formed near the center of Tropical Cyclone Awo on Thursday morning.  Thunderstorms were also occurring in bands in the western side of Awo’s circulation.  Bands in the eastern side of Tropical Cyclone Awo consisted primarily of showers and lower clouds.  Storms near the center of Awo generated upper level divergence that pumped mass away to the west of the tropical cyclone.

The strongest winds were blowing in the southern half of Tropical Cyclone Awo.  Winds to tropical storm force extended out 80 miles (130 km) in the southern side of Awo’s circulation. The winds in the northern half of Tropical Cyclone Awo were blowing at less that tropical storm force.

Tropical Cyclone Awo will move through an environment that will become unfavorable for intensification during the next 24 hours.  Awo will move over water where the Sea Surface Temperatures are near 25°C.  It will move under the northern part of an upper level ridge over the South Indian Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Awo’s circulation.  Those winds will cause moderate to strong vertical wind shear.  The combination of cool Sea Surface temperatures and moderate to strong wind shear will cause Tropical Cyclone Awo to weaken during the next 24 hours.

Tropical Cyclone Awo will move around the northern side of a high pressure system over the South Indian Ocean.  The high pressure system will steer Awo toward the west during the next 24hours.  On its anticipated track, Tropical Cyclone Awo will remain far to the north of La Reunion.

Tropical Storm Dexter Passes South of Newfoundland

Tropical Storm Dexter passed south of Newfoundland on Wednesday evening.  At 11:00 p.m. EDT on Wednesday the center of Tropical Storm Dexter was located at latitude 40.2°N and longitude 54.2°W which put the center about 450 miles (730 km) south of Cape Race, Newfoundland.  Dexter was moving toward the east at 17 m.p.h. (28 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 999 mb.

Tropical Storm Dexter was making a transition to an extratropical cyclone on Wednesday evening.  Dexter was move over water where the Sea Surface Temperatures are near 24°C.  It was moving under the southern part of an upper level trough that is southwest of Greenland.  The upper level trough was producing strong westerly winds that were blowing toward the top of Dexter’s circulation.  Those winds were causing strong vertical wind shear.  The cool Sea Surface Temperatures and the strong vertical wind shear were causing Tropical Storm Dexter to make a transition to an extraropical cyclone.

The transition to an extratropical cyclone was causing changes to the structure of Tropical Storm Dexter.  Thunderstorms were still developing in the eastern side of Dexter’s circulation.  Bands in the other parts of Tropical Storm Dexter consisted primarily of showers and lower clouds.

The size of the circulation around Tropical Storm Dexter increased as Dexter made its transition to an extratropical cyclone.  Winds to tropical storm force extended out 170 miles (275 km) from the center of Dexter’s circulation.

The upper level trough southwest of Greenland will steer Tropical Storm Dexter toward the east-northeast during the next 48 hours.  On its anticipated track, Tropical Storm Dexter will pass south of Greenland and Iceland.

Tropical Storm Dexter will complete the transition to a strong extratropical cyclone on Thursday.  Dexter is likely to strengthen as it completes the transition to an extratropical cyclone.