Tag Archives: Espiritu Santo

Tropical Storm Lola Rapidly Intensifies to Equivalent of a Major Hurricane

Tropical Cyclone Lola rapidly intensified to the equivalent of a major hurricane over the South Pacific Ocean northeast of Vanuatu on Monday morning. At 11:00 a.m. EDT on Monday the center of Tropical Cyclone Lola was located at latitude 13.7°S and longitude 169.6°E which put it about 120 miles (195 km) east of Sola, Vanuatu. Lola was moving toward the south-southeast at 6 m.p.h. (10 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 948 mb.

Tropical Cyclone Lola rapidly intensified to the equivalent of a hurricane/typhoon on Monday morning. A circular eye with a diameter of 35 miles (55 km) was at the center of Lola’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 were revolving around the core of Tropical Cyclone Lola. Storms near the core generated strong upper level divergence that large quantities of pumped mass away from the tropical cyclone. The removal of large amounts of mass caused the surface pressure to decrease rapidly.

Winds to hurricane/typhoon force extended out 30 miles (50 km) from the center of Tropical Cyclone Lola. Winds to tropical storm force extended out 160 miles (260 km) from the center of circulation. The Hurricane Intensity Index (HII) for Tropical Cyclone Lola was 25.1. The Hurricane Size Index (HSI) was 10.6 and the Hurricane Wind Intensiy Size Index (HWISI) was 35.7. Tropical Cyclone Lola was similar in size and intensity to Hurricane Harvey when Harvey hit Texas in 2017.

Tropical Cyclone Lola will move through an environment favorable for intensification during the next 12 hours. Lola 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. Tropical Cyclone Lola could continue to intensify during the next 12 hours. An upper level trough over the Coral Sea will approach Lola from the west later today. The upper level trough will produce westerly winds that will blow toward the top of Lola’s circulation. Those winds will cause the vertical wind shear to increase. Tropical Cyclone Lola could start to weaken when the wind shear increases.

Tropical Cyclone Lola will move around the northwestern part of a high pressure system centered northeast of New Zealand. The high pressure system will steer Lola toward the southwest during the next 24 hours. On its anticipated track, Tropical Cyclone Lola will approach Vanuatu during the next 24hours. Lola will bring strong, gusty winds and locally heavy rain to Espiritu Santo, Maewo, Ambae, Pentecost, Ambrym and Malekula. Tropical Cyclone Lola will be capable of causing regional major damage. Heavy rain is likely to cause flash floods in some locations. Tropical Cyclone Lola could cause a storm surge of up to ten feet (three meters) in some places.

Tropical Cyclone Lola Rapidly Intensifies to Equivalent of Hurricane/Typhoon

Tropical Cyclone Lola rapidly intensified to the equivalent of a hurricane/typhoon over the South Pacific Ocean northeast of Vanuatu on Sunday evening. At 11:00 p.m. EDT on Sunday the center of Tropical Cyclone Lola was located at latitude 12.7°S and longitude 169.3°E which put it about 160 miles (260 km) east-northeast of Sola, Vanuatu. Lola was moving toward the south-southeast 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 105 m.p.h. (165 km/h). The minimum surface pressure was 979 mb.

Tropical Cyclone Lola rapidly intensified to the equivalent of a hurricane/typhoon on Sunday evening. A circular eye with a diameter of 35 miles (55 km) formed at the center of Lola’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 were revolving around the core of Tropical Cyclone Lola. Storms near the core generated upper level divergence that pumped mass away from the tropical cyclone. Winds to hurricane/typhoon force extended out 15 miles (25 km) from the center of Lola’s circulation. Winds to tropical storm force extended out 100 miles (160 km) from the center of circulation.

Tropical Cyclone Lola will move through an environment favorable for intensification during the next 24 hours. Lola 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. Tropical Cyclone Lola will intensify during the next 24 hours. Lola could intensify rapidly to the equivalent of a major hurricane.

Tropical Cyclone Lola will move around the northwestern part of a high pressure system centered northeast of New Zealand. The high pressure system will steer Lola toward the south during the next 24 hours. On its anticipated track, Tropical Cyclone Lola will move just to the east of northern Vanuatu. Lola will bring gusty winds and locally heavy rain to Vanua Lava, Mota Lava, Mota, Ureparapara and Gaua. Heavy rain is likely to cause flash floods in some locations. Tropical Cyclone Lola could cause a storm surge of seven feet (two meters) in some places. Lola could be near Espiritu Santo in 36 hours.

Tropical Cyclone Kevin Strengthens to Equivalent of a Hurricane/Typhoon

Tropical Cyclone Kevin strengthened to the equivalent of a hurricane/typhoon over the Coral Sea west of Vanuatu on Thursday. At 4:00 p.m. EST on Thursday the center of Tropical Cyclone Kevin was located at latitude 16.7°S and longitude 166.1°E which put it about 195 miles (310 km) west-northwest of Port Vila, Vanuatu. Kevin was moving toward the southeast at 14 m.p.h. (22 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 978 mb.

Tropical Cyclone Kevin strengthened west of Vanuatu on Thursday. The inner end of a rainband wrapped around the center of Kevin’s circulation. A circular eye with a diameter of 25 miles (40 km) formed at the center of circulation. The eye was surrounded by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms. Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Kevin. Storms near the core generated upper level divergence that pumped mass away from the tropical cyclone. Winds to hurricane/typhoon force extended out 70 miles (110 km) in the the northern side of Kevin’s circulation. Winds to tropical storm force extended out 190 miles (305 km) from the center of circulation.

Tropical Cyclone Kevin will move through an environment favorable for intensification during the next 24 hours. Kevin will move over over water where the Sea Surface Temperatures are near 30˚C. It will move under the middle of an upper level ridge over the eastern Coral Sea. The upper level winds are weak near the middle of the ridge and there will be little vertical wind shear. Tropical Cyclone Kevin will intensify the next 24 hours. Kevin could strengthen to the equivalent of a major hurricane.

An upper level trough east of Australia will steer Tropical Cyclone Kevin toward the southeast during the next 24 hours. On its anticipated track, the center of Tropical Cyclone Kevin will pass west of Espiritu Santo and Malekula during the next few hours. Kevin will bring gusty winds and locally heavy rain to Espiritu Santo and Malekula. Heavy rain could cause flash floods in some locations. The center of Tropical Cyclone Kevin will pass near Port Vila, Vanuatu in 12 hours. Kevin will bring strong winds and locally heavy rain to Port Vila and Efate. Port Vila and Efate were just hit by Tropical Cyclone Judy. Tropical Cyclone Kevin will hinder efforts to recover from Tropical Cyclone Judy. Tropical Cyclone Kevin will bring wind and rain to Erromango, Tanna and Aneityum on Friday.

Elsewhere over the South Pacific Ocean, Tropical Cyclone Judy was passing south-southwest of Fiji. At 4:00 p.m. EST on Thursday the center of Tropical Cyclone Judy was located at latitude 25.4°S and longitude 177.3°E which put it about 495 miles (795 km) south-southwest of Suva, Fiji. Judy was moving toward the east-southeast at 20 m.p.h. (32 km/h). The maximum sustained wind speed was 90 m.p.h. (145 km/h) and there were wind gusts to 115 m.p.h. (185 km/h). The minimum surface pressure was 969 mb.

Tropical Cyclone Kevin Forms West of Vanuatu

Tropical Cyclone Kevin formed over the Coral Sea west of Vanuatu on Wednesday. At 10:00 p.m. EST on Wednesday the center of Tropical Cyclone Kevin was located at latitude 14.8°S and longitude 163.2°E which put it about 430 miles (695 km) west-northwest of Port Vila, Vanuatu. Kevin was moving toward the east-southeast at 12 m.p.h. (19 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.

A low pressure system over the Coral Sea west of Vanuatu strengthened on Wednesday and the Fiji Meteorological Service designated the system as Tropical Cyclone Kevin. The circulation Tropical Cyclone Kevin organized quickly. The inner end or a rainband wrapped around the northern and eastern sides of the center of Kevin’s circulation. Other bands of showers and thunderstorms were revolving around the center of Tropical Cyclone Kevin. Storms near the center of circulation generated upper level divergence that pumped mass away from the tropical cyclone. Winds to tropical storm force extended out 130 miles (210 km) from the center of Kevin.

Tropical Cyclone Kevin will move through an environment favorable for intensification during the next 36 hours. Kevin will move over over water where the Sea Surface Temperatures are near 30˚C. It will move under the middle of an upper level ridge over the Coral Sea. The upper level winds are weak near the middle of the ridge and there will be little vertical wind shear. Tropical Cyclone Kevin will rapidly intensify to the equivalent of a hurricane/typhoon during the next 24 hours. Kevin could strengthen to the equivalent of a major hurricane within 36 hours.

An upper level trough east of Australia will steer Tropical Cyclone Kevin toward the east-southeast during the next 36 hours. On its anticipated track, the center of Tropical Cyclone Kevin will pass west of Espiritu Santo and Malekula during the next 24 hours. Kevin will bring gusty winds and locally heavy rain to Espiritu Santo and Malekula. Heavy rain could cause flash floods in some locations. The center of Tropical Cyclone Kevin could pass near Port Vila, Vanuatu within 36 hours. Kevin could be the equivalent of a major hurricane when it passes near Port Vila. Tropical Cyclone Kevin could bring strong winds and locally heavy rain to Port Vila and Efate. Port Vila and Efate were just hit by Tropical Cyclone Judy. Tropical Cyclone Kevin will hinder efforts to recover from Tropical Cyclone Judy.

Elsewhere over the South Pacific Ocean, Tropical Cyclone Judy moved quickly away from Vanuatu. At 10:00 p.m. EST on Wednesday the center of Tropical Cyclone Judy was located at latitude 22.9°S and longitude 172.9°E which put it about 450 miles (650km) east of Noumea, New Caledonia. Judy was moving toward the southeast at 16 m.p.h. (26 km/h). The maximum sustained wind speed was 105 m.p.h. (165 km/h) and there were wind gusts to 125 m.p.h. (200 km/h). The minimum surface pressure was 964 mb.

Tropical Cyclone Harold Strengthens to Equivalent of Cat. 5 Hurricane

Tropical Cyclone Harold strengthened to the equivalent of a Category 5 hurricane on Monday.  After weakening while the eye crossed the southern end of Espiritu Santo, the core of Harold rapidly intensified and the tropical cyclone became even more powerful.  At 11:00 a.m. EDT on Monday the center of Tropical Cyclone Harold was located at latitude 16.2°S and longitude 169.4°E which put it about 120 miles (195 km) north-northeast of Port Vila, Vanuatu.  Harold was moving toward the east-southeast at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 165 m.p.h.  and there were wind gusts to 200 m.p.h. (320 km/h).  The minimum surface pressure was 912 mb.

The inner core of Tropical Cyclone Harold weakened when the eye moved across the southern end of Espiritu Santo.  For a time the eye was less distinct of satellite images.  However, the eye cleared out quickly after it moved back over water and the core of Harold strengthened further.  By Monday a small, well formed eye was evident infrared satellite images.  The eye had a diameter of 12 miles (19 km).  A ring of strong thunderstorms surrounded the eye and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Harold.  Storms near the core were generating strong upper level divergence which was pumping mass away from the tropical cyclone.

Winds to hurricane/typhoon force extended out 40 miles (65 km) from the center of Tropical Cyclone Harold.  Winds to tropical storm force extended out 190 miles (305 km) from the center of circulation.  The Hurricane Intensity Index (HII) for Tropical Cyclone Harold was 36.8.  The Hurricane Size Index (HSI) was 16.0 and the Hurricane Wind Intensity Size Index (HWISI) was 52.8.  Harold was capable of causing catastrophic damage.

The core of Tropical Cyclone Harold passed over the southern end of Espiritu Santo.  It then passed near the northern end of Malekula before battering Pentecost and Ambrym.  Harold likely caused catastrophic wind damage in those locations.  Tropical Cyclone Harold also dropped locally heavy rain over Espiritu Santo, Malekula, Pentecost, Maewo, and Ambrym.  Flash flooding probably occurred on those islands.

Tropical Cyclone Harold will move through an environment capable of support an intense tropical cyclone during the next several days.  Harold will move over water where the Sea Surface Temperature is near 30°C.  It will move under the southwestern part of an upper level ridge over the South Pacific Ocean.  The ridge will produce northwesterly winds which will blow toward the top of the circulation.  Those winds will cause some vertical wind shear.  If a rainband wraps around the existing eye and eyewall, then an eyewall replacement cycle could cause Tropical Cyclone Harold to weaken.  Tropical cyclones generally do not maintain Category 5 intensity for an extended period of time.  So, Tropical Cyclone Harold is likely to start to weaken within 24 hours.

Tropical Cyclone Harold will move around the southwestern part of a high pressure system over the South Pacific Ocean.  The high will steer Harold toward the east-southeast during the next few days.  On its anticipated track Tropical Cyclone Harold will move away from Vanuatu.  Harold could approach Fiji within 36 hours and it could still be the equivalent of a major hurricane at that time.

Tropical Cyclone Harold Batters Espiritu Santo

Tropical Cyclone Harold battered Espiritu Santo on Sunday.  The eye of Harold moved over the southwestern part of Espiritu Santo.  At 5:00 p.m. EDT on Sunday the center of Tropical Cyclone Harold was located at latitude 15.3°S and longitude 166.4°E which put it about 60 miles west-northwest of Luganville, Vanuatu.  Harold was moving toward the east at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 145 m.p.h. (230 km/h) and there were wind gusts to 175 m.p.h. (280 km/h).  The minimum surface pressure was 929 mb.

Tropical Cyclone Harold strengthened on Sunday as it slowly approached northern Vanuatu.  A circular eye with a diameter of 18 miles (29 km) was evident on satellite images.  The eye was surrounded by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Harold.  Storms near the core were generating strong upper level divergence which was pumping mass away from the tropical cyclone.

Winds to hurricane/typhoon force extended out 45 miles (75 km) from the center of Tropical Cyclone Harold.  Winds to tropical storm force extended out 120 miles (195 km) from the center of circulation.  The Hurricane Intensity Index (HII) for Tropical Cyclone Harold was 29.9.  The Hurricane Size Index (HSI) was 13.3 and the Hurricane Wind Intensity Size Index (HWISI) 43.2.  Harold was capable of causing significant damage.

Tropical Cyclone Harold will move around the southwestern part of a high pressure system over the South Pacific Ocean.  The high will steer Harold toward the east-southeast during the next few days.  On its anticipated track the center of Tropical Cyclone Harold will move across the southern end of Espiritu Santo.  The center will also pass near the northern end of Malekula, near the southern end of Pentecost and near Ambrym.  Tropical Cyclone Harold will drop heavy rain over Espiritu Santo, Malekula, Pentecost, Ambrym, Epi, Ambae and Maewo.  Harold will move slowly and the heavy rain is likely to cause flash floods.  Strong winds blowing toward the coast could produce significant storm surges on the eastern and northern coasts of some islands.

Tropical Cyclone Harold will move through an environment favorable for a strong tropical cyclone.  Harold will move over water where the Sea Surface Temperature is near 30°C.  It will move under the southwestern part of an upper level ridge over the South Pacific Ocean.  The ridge will produce northwesterly winds which will blow toward the top of the circulation.  Those winds will cause some vertical wind shear.  Since the core of Tropical Cyclone Harold will pass over the southern end of Espiritu Santo, increased friction will cause the circulation to weaken during the next 12 to 24 hours.

Major Tropical Cyclone Harold Nears Vanuatu

Major Tropical Cyclone Harold neared Vanuatu on Saturday night.  At 11:00 p.m. EDT on Saturday the center of Tropical Cyclone Vanuatu was located at latitude 15.5°S and longitude 166.0°E which put it about 80 miles (130 km) west-northwest of Unmet, Vanuatu.  Harold was moving toward the southeast at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 120 m.p.h. (195 km/h) and there were wind gusts to 150 m.p.h. (240 km/h).  The minimum surface pressure was 949 mb.

Tropical Cyclone Harold intensified into the equivalent of a major hurricane.  The original small eye dissipated but a new larger eye developed on Saturday night.  The new eye was surround by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Harold.  The strongest rainbands were in the eastern and southern parts of the circulation.  Storms near the core of Harold generated upper level divergence which pumped mass away from the center of the tropical cyclone.

Winds to hurricane/typhoon force extended out 30 miles (50 km) from the center of Tropical Cyclone Harold.  Winds to tropical storm force extended out 125 miles (200 km) from the center of circulation.  The Hurricane Intensity Index (HII) for Harold was 22.1.  The Hurricane Size Index (HSI) was 11.1 and the Hurricane Wind Intensity Size Index (HWISI) was 33.2.  Tropical Cyclone Harold was capable of causing major damage.

Tropical Cyclone Harold will move through an environment favorable for intensification during the next 24 hours.  Harold will move over water where the Sea Surface Temperature is near 30°C.  It will move around the southwestern part of an upper level ridge over the South Pacific Ocean.  The ridge will produce northwesterly winds which will blow toward the top of the circulation.  Those winds will cause some vertical wind shear and the wind shear could be strong enough to limit intensification.  Tropical Cyclone Harold could intensify further, but it may maintain its intensity on Sunday.

The ridge over the South Pacific Ocean will steer Tropical Cyclone Harold slowly toward the southeast during the next 24 hours.  On its anticipated track the core of Harold with the strongest winds will move slowly toward Malekula.  Tropical Cyclone Harold will drop heavy rain over central Vanuatu.  The slow movement of Harold could create the potential for very serious flooding on Espiritu Santo, Malekula, Ambrym and Epi.

Elsewhere in the tropics, Tropical Cyclone Irondro began to slowly weaken over the South Indian Ocean.  At 5:00 p.m. EDT on Saturday the center of Tropical Cyclone Irondro was located at latitude 23.3°S and longitude 81.5°E which put it about 1275 miles (2060 km) southwest of Cocos Island.  Irondro was moving toward the southeast at 18 m.p.h. (29 km/h).  The maximum sustained wind speed was 110 m.p.h. (175 km/h) and there were wind gusts to 130 m.p.h. (210 km/h).  The minimum surface pressure was 958 mb.

Tropical Cyclone Harold Rapidly Intensifies into Equivalent of Hurricane/Typhoon

Tropical Cyclone Harold rapidly intensified into the equivalent of a hurricane/typhoon west-northwest of Vanuatu on Friday.  At 11:00 p.m. EDT on Friday the center of Tropical Cyclone Harold was located at latitude 14.1°S and longitude 164.1°E which put it about 170 miles (275 km) west-northwest of Nokuku, Vanuatu.  Harold was moving toward the southeast at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 105 m.p.h. (170 km/h) and there were wind gusts to 125 m.p.h. (200 km/h).  The minimum surface pressure was 959 mb.

The circulation around Tropical Cyclone Harold organized quickly on Friday.  The inner end of a rainband wrapped around the center of circulation and a small eye formed.  A ring of strong thunderstorms surrounded the eye and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Harold.  The strongest rainbands were in the eastern half of the circulation.  Bands in the western half of the circulation consisted primarily of showers and lower clouds.  Storms around the core of the circulation generated strong upper level divergence which pumped mass away to the east of the tropical cyclone.

Winds to hurricane/typhoon force extend out 35 miles (55 km) from the center of Tropical Cyclone Harold.  Winds to tropical storm force extended out 140 miles (225 km) from the center of circulation.  The Hurricane Intensity Index (HII) for Tropical Cyclone Harold was 17.8.  The Hurricane Size Index (HSI) was 12.0 and the Hurricane Wind Intensity Size Index (HWISI) was 29.8.  Harold was capable of causing serious damage.

Tropical Cyclone Harold will move through an environment favorable for intensification during the next 24 to 48 hours.  Harold will move over water where the Sea Surface Temperature is near 30°C.  It will move around the southwestern part of an upper level ridge over the South Pacific Ocean.  The ridge will produce northwesterly winds which will blow toward the top of the circulation.  Those winds will cause some vertical wind shear, but the shear will not be strong enough to prevent intensification.  Tropical Cyclone Harold will strengthen into the equivalent of a major hurricane during the next 12 hours.

The upper level ridge will steer Tropical Cyclone Harold slowly toward the southeast during the weekend.  On its anticipated track Harold will gradually approach Espiritu Santo and Malekula in Vanuatu.  The core of Tropical Cyclone Harold could move across the central part of Vanuatu in 48 to 72 hours.  Harold is likely to be the equivalent of a major hurricane at that time.

Elsewhere in the tropics, Tropical Cyclone Irondro intensified into the equivalent of a hurricane/typhoon over the South Indian Ocean.  At 5:00 p.m. EDT on Friday the center of Tropical Cyclone Irondro was located at latitude 19.9°S and longitude 76.4°E which put it about 885 miles (1425 km) south-southeast of Diego Garcia.  Irondro was moving toward the east-southeast at 21 m.p.h. (33 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. (170 km/h).  The minimum surface pressure was 973 mb.