Tag Archives: Tropical Cyclone Charlotte

Tropical Cyclone Halima Forms South of Diego Garcia

Tropical Cyclone Halima formed south of Diego Garcia on Wednesday. At 11:00 a.m. EDT on Wednesday the center of Tropical Cyclone Halima was located at latitude 13.4°S and longitude 75.7°E which put it about 485 miles (780 km) south-southeast of Diego Garcia. Halima was moving toward the west-southwest at 9 m.p.h (15 km/h). The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h). The minimum surface pressure was 997 mb.

The circulation around a low pressure system over the South Indian Ocean south of Diego Garcia strengthened on Wednesday and the system was designated at Tropical Cyclone Halima. More thunderstorms formed west of the center of Halima’s circulation. The strongest thunderstorms were occurring in bands in the western half of Tropical Cyclone Halima. Bands in the eastern half 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 90 miles (145 km) from the center of Halima.

Tropical Cyclone Halima will move through an environment favorable for intensification during the next 36 hours. Halima will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the northern part of an upper level ridge over the South Indian Ocean. The ridge will produce easterly winds that will blow toward the top of Halima’s circulation. Those winds will cause some vertical wind shear, but the shear will not be enough to prevent intensification. Tropical Cyclone Halima will intensify during the next 36 hours and it could strengthen to the equivalent of a hurricane/typhoon.

Tropical Cyclone Halima will move around the western end of a high pressure system over the South Indian Ocean during the next 36 hours. The high pressure system will steer Halima toward the south. On its anticipated track Tropical Cyclone Halima will move farther away from Diego Garcia.

Elsewhere over the South Indian Ocean, Tropical Cyclone Charlotte weakened gradually northwest of Australia. At 11:00 a.m. EDT on Wednesday the center of Tropical Cyclone Charlotte was located at latitude 20.4°S and longitude 107.6°E which put it about 430 miles (695 km) west-northwest of Learmonth, Australia. Charlotte was moving toward the south-southwest at 13 m.p.h (20 km/h). The maximum sustained wind speed was 75 m.p.h. (120 km/h) and there were wind gusts to 90 m.p.h. (145 km/h). The minimum surface pressure was 979 mb.

Tropical Cyclone Charlotte Spins Northwest of Australia

Tropical Cyclone Charotte was spinning over the South Indian Ocean northwest of Australia on Tuesday night. At 11:00 p.m. EDT on Tuesday the center of Tropical Cyclone Charlotte was located at latitude 18.5°S and longitude 108.7°E which put it about 435 miles (700 km) northwest of Learmonth, Australia. Charlotte was moving toward the south-southwest 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 973 mb.

Tropical Cyclone Charlotte continued to spin over over the South Indian Ocean northwest of Australia on Tuesday night. The environment around Charlotte became less favorable for a tropical cyclone on Tuesday evening and the tropical cyclone was beginning to be affected the different environment. The ring of thunderstorms around the eye weakened and the overall distribution of thunderstorms became asymmetrical. The strongest thunderstorms were occurring in bands in the southern half of the circulation around Tropical Cyclone Charlotte. Bands in the northern half of the tropical cyclone consisted primarily of showers and lower clouds. Storms near the center of circulation were still generating upper level divergence that pumped mass away to the southeast of the tropical cyclone. Winds to tropical storm force extended out 125 miles (200 km) from the center of Tropical Cyclone Charlotte.

Tropical Cyclone Charlotte will continue to be in an environment unfavorable for a tropical cyclone during the next several days. Charlotte will move over water where the Sea Surface Temperatures are near 28˚C. An upper level trough over the South Indian Ocean will approach Charlotte from the west. The trough will produce northwesterly winds that will blow toward the top of Charlotte’s circulation. Those winds will cause moderate vertical wind shear. The flow of air around Tropical Cyclone Charlotte could also pull drier air into the western and northern parts of the circulation. The wind shear and the drier air will cause Tropical Cyclone Charlotte to weaken during the next several days.

Tropical Cyclone Charlotte will move around the western part of a high pressure system over Australia during the next 36 hours. The high pressure system will steer Charlotte toward the south. On its anticipated track Tropical Cyclone Charlotte will move parallel to the coast of Western Australia. Charlotte will remain west of the coast during the next 36 hours.

Tropical Cyclone Charlotte Strengthens to Equivalent of Hurricane/Typhoon

Tropical Cyclone Charlotte strengthened to the equivalent of a hurricane/typhoon over the South Indian Ocean northwest of Australia on Monday afternoon. At 5:00 p.m. EDT on Monday the center of Tropical Cyclone Charlotte was located at latitude 16.4°S and longitude 109.6°E which put it about 500 miles (805 km) northwest of Learmonth, Australia. Charlotte was moving toward the southwest at 9 m.p.h (15 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 973 mb.

Tropical Cyclone Charlotte continued to intensify on Monday. A small circular eye formed at the center of Charlotte’s 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 small core of Tropical Cyclone Charlotte. 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 circulation. Winds to tropical storm force extended out 140 miles (225 km) from the center.

Tropical Cyclone Charlotte will move through an environment favorable for intensification during the next 24 hours. Charlotte will move over water where the Sea Surface Temperatures are near 29˚C. It will move through a region where the upper level winds are weak and there will be little vertical wind shear. Tropical Cyclone Charlotte is likely to continue to intensify during the next 24 hours. An upper level trough over the South Indian Ocean will approach Charlotte from the west in a day or so. The trough will produce northwesterly winds and those winds will cause the vertical wind shear to increase. Tropical Cyclone Charlotte will start to weaken when the wind shear increases.

Tropical Cyclone Charlotte will move around the northwestern part of a high pressure system over Australia during the next 24 hours. The high pressure system will steer Charlotte toward the southwest. On its anticipated track Tropical Cyclone Charlotte will move parallel to the coast of Western Australia during the next 24 hours. Charlotte will remain far away from the coast during the next several days.

Tropical Cyclone Charlotte Develops Quickly Northwest of Australia

Tropical Cyclone Charlotte developed quickly over the South Indian Ocean northwest of Australia on Sunday. At 11:00 p.m. EDT on Sunday the center of Tropical Cyclone Charlotte was located at latitude 14.9°S and longitude 111.5°E which put it about 550 miles (890 km) north-northwest of Learmonth,, Australia. Charlotte was moving toward the southwest at 15 m.p.h (24 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.

A low pressure system over the South Indian Ocean northwest of Australia strengthened quickly on Sunday and the Australia Bureau of Meteorology designated the system as Tropical Cyclone Charlotte. The circulation around Tropical Cyclone Charlotte organized rapidly. The inner end of a rainband wrapped around the southern and western sides of the center of circulation and an eye appeared to be forming. Bands of showers and thunderstorms were revolving around the core of Charlotte’s circulation. Storms near the core generated upper level divergence that pumped mass away from the tropical cyclone. Winds to tropical storm force extended out 140 miles (225 km) from the center of circulation.

Tropical Cyclone Charlotte will move through an environment favorable for intensification during the next 24 hours. Charlotte 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 Cyclone Charlotte is likely to continue to intensify rapidly during the next 24 hours. Charlotte is likely to strengthen to the equivalent of a hurricane/typhoon during the next 12 hours.

Tropical Cyclone Charlotte will move around the northwestern part of a high pressure system over Australia during the next 24 hours. The high pressure system will steer Charlotte toward the west-southwest. On its anticipated track Tropical Cyclone Charlotte will move parallel to the coast of Western Australia during the next 24 hours. Charlotte will remain well away from the coast on Monday.