Tag Archives: SH01

Tropical Cyclone Ancha Forms Southeast of Diego Garcia

Tropical Cyclone Ancha formed over the South Indian Ocean southeast of Diego Garcia on Tuesday night.  At 11:00 p.m. EDT on Wednesday the center of Tropical Cyclone Ancha was located at latitude 11.7°S and longitude 74.2°E which put the center about 335 miles (540 km) south-southeast of Diego Garcia.  Ancha was moving toward the south-southwest at 14 m.p.h. (22 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 994 mb.

A low pressure system over the South Indian Ocean southeast of Diego Garcia intensified on Tuesday night and Meteo France la Reunion designated the system as Tropical Cyclone Ancha.  The circulation around Tropical Cyclone Ancha exhibited more organization on Wednesday morning.  The inner end of a rainband wrapped around the southern side of the center of Ancha’s circulation.  Even though the circulation around Tropical Cyclone Ancha exhibited more organization, the distribution of thunderstorms was still asymmetrical.  Thunderstorms were occurring in bands in the eastern and southern parts of Ancha’s circulation.  Bands in the northern and western parts of the circulation consisted primarily of showers and lower clouds.  Storms near the center of Ancha generated upper level divergence that pumped mass away to the east of the tropical cyclone.

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

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

Tropical Cyclone Ancha will move around the western end of high pressure system over the South Indian Ocean.  The high pressure system will steer Ancha toward the southwest during the next 24 hours.  On its anticipated track, Tropical Cyclone Ancha will pass well to the south of Diego Garcia.

Tropical Cyclone Lola Hits Vanuatu

Tropical Cyclone Lola hit Vanuatu on Tuesday. At 5:00 p.m. EDT on Tuesday the center of Tropical Cyclone Lola was located at latitude 16.0°S and longitude 167.5°E which put it about 25 miles (40 km) east of Norsup, Vanuatu. Lola was moving toward the west-southwest 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 956 mb.

Tropical Cyclone Lola was the equivalent of a major hurricane when it hit the central part of Vanuatu on Tuesday. Winds to hurricane/typhoon force extended out 30 miles (50 km) from the center of Lola’s circulation. Winds to tropical storm force extended out 105 miles (165 km) from the center of circulation. The Hurricane Intensity Index (HII) for Tropical Cyclone Lola was 22.1. The Hurricane Size Index (HSI) was 10.6 and the Hurricane Wind Intensity Size Index (HWISI) was 32.7. Tropical Cyclone Lola was similar in size and intensity to Hurricane Dennis when Dennis hit Northwest Florida in 2005.

The center of Tropical Cyclone Lola will move across Malekula during the next few hours. The strong winds in the eastern side of Lola’s circulation will hit Malekula, Ambrym and Epi. Tropical Cyclone Lola is capable of causing regional major damage. Heavy rain will also fall on Malekula, Ambrym and Epi. Heavy rain is likely to cause flash floods in some location. Lola could cause a storm surge of up to ten feet (three meters) along the north coasts of Malekula, Ambrym and Epi, when the wind blows the water toward the land.

Tropical Cyclone Lola will move through an environment that will become unfavorable for a strong tropical cyclone during the next 24 hours. Lola will move over water where the Sea Surface Temperatures are near 27°C. An upper level trough over the Coral Sea will approach Lola from the west. 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 is likely to weaken when the wind shear increases.

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 Lola Forms North Of Vanuatu

Tropical Storm Lola formed over the South Pacific Ocean northern of Vanuatu during Saturday night. At 5:00 a.m. EDT on Sunday the center of Tropical Cyclone Lola was located at latitude 11.0°S and longitude 167.9°E which put it about 200 miles (320 km) northeast of Sola, Vanuatu. Sola was moving toward the south-southeast at 8 m.p.h. (13 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 999 mb.

A low pressure system over the South Pacific Ocean north of Vanuatu strengthened during Saturday night and the system was designated as Tropical Cyclone Lola. The circulation around Tropical Cyclone Lola was organizing quickly. Thunderstorms developed near the center of Lola’s circulation. Storms near the center generated upper level divergence that pumped mass away from the tropical cyclone. Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Lola. Winds to tropical storm force extended out 185 miles (295 km) in the southeastern quadrant of Lola’s circulation. Tropical storm force winds extended out 100 miles (160 km) in the other parts of Tropical Cyclone Lola.

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 to the equivalent of a hurricane/typhoon during the next 24 hours. Lola could intensify rapidly at times.

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 across northern Vanuatu. Lola will bring strong 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.

Rare Late Season Tropical Cyclone Forms over South Indian Ocean

A rare late season tropical cyclone formed over the South Indian Ocean on Thursday. At 5:00 p.m. EDT on Thursday the center of Tropical Cyclone 01S was located at latitude 10.7°S and longitude 95.0°E which put it about 170 miles (275 km) west-northwest of Cocos Island. Tropical Cyclone 01S was moving toward the southeast at 7 m.p.h. (11 km/h). The maximum sustained wind speed was 40 m.p.h. (65 km/h) and and there were wind gusts to 50 m.p.h. (80 km/h). The minimum surface pressure was 1002 mb.

The circulation around a low pressure system over the South Indian Ocean west-northwest of Cocos Island strengthened on Thursday and the Joint Typhoon Warning Center and the Australian Bureau of Meteorology both designated the system as a tropical cyclone. It is unusual for a tropical cyclone to form this late in the season in the southern hemisphere. It is the equivalent of a tropical cyclone forming in late January in the northern hemisphere.

The distribution of thunderstorms around Tropical Cyclone 01S was asymmetrical. The strongest thunderstorms were occurring in bands in the southern half of the tropical cyclone. Bands in the northern half of Tropical Cyclone 01S consisted primarily of showers and lower clouds. Tropical Cyclone 01S was under the southwestern part of an upper level ridge centered northwest of Australia. The upper level ridge was producing northerly winds that were blowing toward the top of the tropical cyclone’s circulation. Those winds were causing moderate vertical wind shear. The wind shear was causing the asymmetrical distribution of thunderstorms. Winds to tropical storm force extended out 170 miles (275 km) in the southeastern quadrant of Tropical Cyclone 01S. Winds in the other parts of the tropical cyclone were blowing at less than tropical storm force.

Tropical Cyclone 01S will move through an environment somewhat favorable for intensification during the next 24 hours. The tropical cyclone will move over water where the Sea Surface Temperatures are near 28˚C. However, the upper level ridge northwest of Australia will continue to cause moderate vertical wind shear. Tropical Cyclone 01S could strengthen a little more during the next 24 hours, but the moderate vertical wind shear will limit intensification.

Tropical Cyclone 01S will move north of a high pressure system over the South Indian Ocean during the next several days. The high pressure system will steer the tropical cyclone toward the west. On its anticipated track Tropical Cyclone 01S will begin to move farther away from Cocos Island.

Tropical Cyclone Paddy Weakens South of Christmas Island

Tropical Cyclone Paddy weakened over the South Indian Ocean south of Christmas Island on Wednesday. At 10:00 a.m. EST on Wednesday the center of Tropical Cyclone Paddy was located at latitude 14.5°S and longitude 105.5°E which put it about 270 miles (440 km) south of Christmas Island. Paddy was moving toward the southwest at 6 m.p.h. (10 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 1003 mb.

An upper level trough over the South Indian Ocean west of Australia was producing strong northwesterly winds that were blowing toward the top of Tropical Cyclone Paddy’s circulation. Those winds were causing strong vertical wind shear and the upper level winds were blowing the tops off of many of the thunderstorms around Paddy’s circulation. The strongest thunderstorms were occurring in bands on the southeastern side of Tropical Cyclone Paddy. Bands in the other parts of the tropical cyclone consisted primarily of showers and lower clouds. The strong vertical wind shear was causing Paddy to weaken.

Tropical Cyclone Paddy will move through an environment unfavorable for a tropical cyclone during the next several days. Paddy will move over water where the Sea Surface Temperatures are near 26˚C. However, the upper level trough west of Australia will continue to cause strong vertical wind shear. The strong wind shear will blow the tops off of any new thunderstorms that develop. The winds around Tropical Cyclone Paddy will decrease gradually during the next 48 hours.

Tropical Cyclone Paddy will move south of a high pressure system over the South Indian Ocean. The high pressure system will steer Paddy toward the west during the next several days as the tropical cyclone weakens gradually. On its anticipated track Tropical Cyclone Paddy will remain well to the south of Christmas Island.

Tropical Cyclone Paddy Develops Southeast of Christmas Island

Tropical Cyclone Paddy developed over the South Indian Ocean southeast of Christmas Island on Monday. At 10:00 a.m. EST on Monday the center of Tropical Cyclone Paddy was located at latitude 13.8°S and longitude 108.0°E which put it about 275 miles (440 km) southeast of Christmas, Island. Paddy was moving toward the southwest at 5 m.p.h. (8 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 997 mb.

A low pressure system over the South Indian Ocean south of Java strengthened on Monday and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Paddy. The strongest thunderstorms in Paddy’s circulation were occurring in bands that were southeast and northwest of the center of circulation. Bands in the northeastern and southwestern parts of the circulation consisted primarily of showers and lower clouds. 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 75 miles (120 km) from the center of Tropical Cyclone Paddy.

Tropical Cyclone Paddy will move through an environment somewhat favorable for intensification during the next 12 hours. Paddy 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. Tropical Cyclone Paddy could get a little stronger during the next 12 hours. Paddy will move under an area where there are strong northwesterly winds in the upper levels on Tuesday. Those winds will create strong vertical wind shear and the shear will cause Tropical Cyclone Paddy to weaken.

Tropical Cyclone Paddy will move around the northern side of a high pressure system over the South Indian Ocean. The high pressure system will steer Paddy toward the southwest during the next 12 to 24 hours. When Tropical Cyclone Paddy starts to weaken on Tuesday, it will be steered by winds in the lower levels of the atmosphere. Those winds will steer Paddy toward the west during the middle of this week. On its anticipated track Tropical Cyclone Paddy will remain well to the south of Christmas Island.

Tropical Cyclone Alicia Develops East of Diego Garcia

Tropical Cyclone Alicia developed east of Diego Garcia on Friday. At 10:00 p.m. EST on Friday the center of Tropical Cyclone Alicia was located at latitude 7.8°N and longitude 79.1°E which put it about 495 miles (795 km) east of Diego Garcia. Alicia was moving toward the west-southwest at 23 m.p.h. (37 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 991 mb.

The circulation around a low pressure system east of Diego Garcia exhibited more organization on Friday and the system was designated as Tropical Cyclone Alicia. The inner end of a rainband wrapped around the western and northern sides of the center of circulation. Other bands of showers and thunderstorms were revolving around the center of Alicia. Storms near the center generated upper level divergence which pumped mass away from the tropical storm. Winds to tropical storm force extended out 130 miles (210 km) from the center of circulation.

Tropical Cyclone Alicia will move through an environment that will be favorable for intensification during the next 36 hours. Alicia will move over water where the Sea Surface Temperature is near 29°C. Alicia will be under an upper level ridge where the winds are weaker and there will be little vertical wind shear. Tropical Cyclone Alicia could strengthen into the equivalent of a hurricane/typhoon within 36 hours.

Tropical Cyclone Alicia will move around the western end of a high pressure system over the southeastern Indian Ocean. The high will steer Alicia toward the south-southwest during the next several days. On its anticipated track Tropical Cyclone Alicia will pass southeast of Diego Garcia and east of Rodrigues.

Tropical Storm Kammuri Passes South of Guam

Tropical Storm Kammuri passed south of Guam on Tuesday.  At 10:00 p.m. EST on Tuesday the center of Tropical Storm Kammuri was located at latitude 11.8°N and longitude 141.8°E which put it about 225 miles (365 km) southwest of Guam.  Kammuri 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 985 mb.  The Tropical Storm Warnings for Guam, Rota, Saipan and Tinian were discontinued.

The circulation around Tropical Storm Kammuri exhibited greater organization on Tuesday.  Rainbands around the center of circulation were more circular.  Storms near the center were generating upper level divergence which was pumping mass away to the north and west of the tropical storm.  There were also more thunderstorms in bands north and west of the center of Kammuri.  Bands southeast of the center consisted primarily of showers and lower clouds.  The wind field around Tropical Storm Kammuri was also asymmetrical.  Winds to tropical storm force extended out farther in the northern half of the circulation.  Winds to tropical storm force extended out 240 miles (340 km) to the northeast of the center of Kammuri.  In contrast, tropical storm force winds only extended out 75 miles (120 km) to the southeast of the center of circulation.

Tropical Storm Kammuri will move through an environment favorable for intensification during the next few days.  Kammuri will move over water where the Sea Surface Temperature is near 29°C.  It will move under the western end of an upper level ridge.  The ridge will produce easterly winds which will blow toward the top of the circulation.  Those winds will cause some vertical wind shear.  The shear will slow the rate of intensification, but it will not be strong enough to prevent Tropical Storm Kammuri from getting stronger.  Kammuri is likely to intensify into a typhoon during the next 24 hours and it could strengthen into the equivalent of a major hurricane later this week.

Tropical Storm Kammuri will move around the western end of a subtropical high pressure system over the Western Pacific Ocean during the next 48 to 72 hours.  The ridge will steer Kammuri toward the northwest.  A second high pressure system will move eastward from Asia in about three days.  The second high will block Tropical Storm Kammuri from moving any farther toward the north and the high will steer Kammuri toward the west during the weekend.  On its anticipated track Tropical Storm Kammuri will gradually move closer to the Philippines.

Elsewhere, over the South Pacific Ocean near Vanuatu vertical wind shear weakened Tropical Cyclone Rita.  At 10:00 p.m. EST on Tuesday the center of Tropical Cyclone Rita was located at latitude 15.3°S and longitude 169.0°E which put it about 180 miles (290 km) north of Port Vila, Vanuatu.  Rita was moving toward the south at 5 m.p.h. (8 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 1000 mb.