Category Archives: Indian Ocean

Tropical Cyclone Faida Brings Wind and Rain to Madagascar

Tropical Cyclone Faida brought wind and rain to Madagascar on Monday night.  At 10:00 p.m. EST on Monday the center of Tropical Cyclone Faida was located at latitude 18.5°S and longitude 49.7°E which put the center about 35 miles (55 km) southeast of the Toamasina, Madagascar.  Faida was moving toward the west at 10 m.p.h. (16 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 998 mb.

Even though the center of Tropical Cyclone Faida was just off the east coast of Madagascar on Monday night, bands in the western side of of Faida’s circulation were already over land.  Those bands brought strong winds and locally heavy rain to parts of northern and central Madagascar.

The strongest winds and heaviest rain were in the western half of Tropical Cyclone Faida.  Winds to tropical storm force extended out 70 miles (110 km) in the western side of Faida’s circulation.  The winds in the eastern half of Tropical Cyclone Faida were blowing at less than tropical storm force.

Tropical Cyclone Faida will move around the northern part of a high pressure system over the Southwest Indian Ocean and southern Africa.  The high pressure system will steer Faida toward the west during the next 24 hours.  On its anticipated track, Tropical Cyclone Faida will move across Madagascar during the next 36 hours.  The center of Faida’s circulation will pass near Toamasina and Antananarivo.

Tropical Cyclone Faida will continue to drop heavy rain over parts of northern and central Madagascar.  Heavy rain is likely to cause floods in some locations.

Elsewhere, Tropical Cyclone Vince intensified southwest of the Cocos Islands and Tropical Cyclone Taliah continued to spin northwest of Australia.

At 4:00 p.m. EST on Monday the center of Tropical Cyclone Vince was located at latitude 17.3°S and longitude 91.5°E which put the center about 465 miles (750 km) southwest of the Cocos Islands.  Vince was moving toward the west-southwest 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 978 mb.

At 4:00 p.m. EST on Monday the center of Tropical Cyclone Taliah was located at latitude 15.5°S and longitude 112.4°E which put the center about 485 miles (780 km) north of Exmouth, Australia.  Taliah was moving toward the west at 12 m.p.h. (19 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 972 mb.

Tropical Cyclone Faida Develops Just East of Madagascar

Tropical Cyclone Faida developed just east of Madagascar on Monday morning.  At 10:00 a.m. EST on Monday the center of Tropical Cyclone Faida was located at latitude 18.1°S and longitude 50.3°E which put the center about 70 miles (110 km) east of the Toamasina, Madagascar.  Faida 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 998 mb.

A low pressure system just to the east of Madagascar strengthened on early on Monday and Meteo France La Reunion designated the system as Tropical Cyclone Faida.  The distribution of thunderstorms in Tropical Cyclone Faida was asymmetrical.  Thunderstorms were occurring mainly in bands in the western side of Faida’s circulation.  Bands in the eastern part of Tropical Cyclone Faida consisted primarily of showers and lower clouds.  Storms near the center of Faida generated upper level divergence that pumped mass away to the west of the tropical cyclone.

The distribution of wind speed in Tropical Cyclone Faida was also asymmetrical.  Winds to tropical storm force extended out 70 miles (110 km) in the western half of Faida’s circulation.  The winds in the eastern side of Tropical Cyclone Faida were blowing at less than tropical storm force.

Tropical Cyclone Faida will move through an environment favorable for intensification during the next 12 hours.  Faida will move over water where where the Sea Surface Temperatures are near 29°C.  It will move under the northern part of an upper level ridge over the Southwest Indian Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Faida’s circulation.  Those winds will cause moderate vertical wind shear.  The vertical wind shear will inhibit intensification, but Tropical Cyclone Faida could intensity during the next 12 hours.

Tropical Cyclone Faida will move around the northern part of a high pressure system over the Southwest Indian Ocean.  The high pressure system will steer Faida toward the west during the next 24 hours.  On its anticipated track, Tropical Cyclone Faida will make landfall on the northern coast of Madagascar near Toamasina in 12 hours.

Tropical Cyclone Faida will bring strong winds and locally heavy rain to northern Madagascar.  Heavy rain is likely to cause floods in some locations.

Taliah Strengthens to Equivalent of Hurricane/Typhoon

Tropical Cyclone Taliah strengthened to the equivalent of a hurricane/typhoon over the South Indian Ocean northwest of Australia on Monday.  At 4:00 a.m. EST on Monday the center of Tropical Cyclone Taliah was located at latitude 15.2°S and longitude 113.9°E which put the center about 500 miles (800 km) north of Exmouth, Australia.  Taliah was moving toward the west at 9 m.p.h. (15 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 975 mb.

Tropical Cyclone Taliah strengthened to the equivalent of a hurricane/typhoon on Monday.  The inner end of a rainband wrapped around the western and northern sides of the center of Taliah’s circulation.  Even though Tropical Cyclone Taliah strengthened, the distribution of thunderstorms was asymmetrical.  Most thunderstorms were occurring in bands in the western and northern parts of Taliah’s circulation.  Bands in the eastern and southern parts of Tropical Cyclone Taliah consisted primarily of showers and lower clouds.  Storms near the center of Taliah 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.

Winds to hurricane/typhoon force extended out 60 miles (95 km/h) in the northern side of Tropical Cyclone Taliah.  Winds to hurricane/typhoon force extended out 30 miles (50 km) in the southern part of Taliah’s circulation.  Winds to tropical storm force extended out 160 miles (260 km) from the center of Tropical Cyclone Taliah.

Tropical Cyclone Taliah will move through an environment favorable for intensification during the next 24 hours. Taliah will move over water where where the Sea Surface Temperatures are near 30°C.  It will move under the northern part of an upper level ridge west of Australia.  The upper level ridge will produce easterly winds that will blow toward the top of Taliah’s circulation.  Those winds will cause some vertical wind shear.  The vertical wind shear will inhibit intensification, but the wind shear will not be enough to prevent intensification.  Tropical Cyclone Taliah is likely to intensify during the next 24 hours.

Tropical Cyclone Taliah will move around the northern side of a high pressure system that extends from Australia to the South Indian Ocean.  The high pressure system will steer Talia toward the west during the next 24 hours.  On its anticipated track, Tropical Cyclone Taliah will move farther away from Western Australia.

Elsewhere, Tropical Cyclone Vince intensified south of the Cocos Islands.  4:00 a.m. EST on Monday the center of Tropical Cyclone Vince was located at latitude 16.7°S and longitude 94.3°E which put the center about 355 miles (525 km) south-southwest of the Cocos Islands.  Vince was moving toward the west-southwest at 17 m.p.h. (28 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 983 mb.

Tropical Cyclone Taliah Forms Northwest of Australia

Tropical Cyclone Taliah formed over the South Indian Ocean northwest of Australia on Sunday.  At 4:00 a.m. EST on Sunday the center of Tropical Cyclone Taliah was located at latitude 14.6°S and longitude 115.8°E which put the center about 445 miles (720 km) north of Karratha, Australia.  Taliah was moving toward the west at 7 m.p.h. (11 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 988 mb.

A low pressure system over the South Indian Ocean northwest of Australia strengthened on Sunday and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Taliah.  The circulation around Tropical Cyclone Taliah was organizing rapidly.  The inner end of a rainband wrapped around the center of Taliah’s circulation and an eye appeared to be forming at the center of Taliah.  The strongest wind were occurring in the part of the rainband around the center of circulation.  Storms near the center of Taliah 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 Taliah was fairly large.  Winds to tropical storm force extended out 160 miles (260 km) from the center of Taliah’s circulation.

Tropical Cyclone Taliah will move through an environment very favorable for intensification during the next 24 hours.  Taliah will move over water where where the Sea Surface Temperatures are near 30°C.  It will move under the axis of an upper level ridge west of Australia.  The upper level winds are weak near the axis of the ridge and there will be little vertical wind shear.  Tropical Cyclone Taliah will intensify during the next 24 hours.  Taliah is likely to intensify rapidly to the equivalent of a hurricane/typhoon.

Tropical Cyclone Taliah will move around the northern side of a high pressure system that extends from Australia to the South Indian Ocean.  The high pressure system will steer Talia toward the west during the next 24 hours.  On its anticipated track, Tropical Cyclone Taliah will move farther away from Western Australia.

 

Tropical Cyclone Elvis Spins Near Southwest Madagascar

Tropical Cyclone Elvis continued to spin near southwestern Madagascar on Wednesday.  At 4:00 p.m. EST on Wednesday the center of Tropical Cyclone Elvis was located at latitude 26.0°S and longitude 43.3°E which put the center about 115 miles (185 km) southwest of Beloha, Madagascar.  Elvis was moving toward the south-southeast at 13 m.p.h. (21 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 989 mb.

Although Tropical Cyclone Elvis strengthened on Wednesday, drier air appeared to be getting pulled into Elvis’ circulation.  Many of the thunderstorms near the center of Tropical Cyclone Elvis dissipated. Thunderstorms were still occurring in bands in the southeastern part of Elvis’ circulation.  Bands in the other parts of Tropical Cyclone Elvis consisted primarily of showers and lower clouds.  The few remaining thunderstorms near the center of Elvis were not generating much upper level divergence

The distribution of wind speeds in Tropical Cyclone Elvis was asymmetrical.  Winds to tropical storm force extended out 140 miles (220 km) in the southeastern part of Elvis’s circulation.  Winds to tropical storm force only extended out 50 miles in the northern side of Tropical Cyclone Elvis.

Tropical Cyclone Elvis will move through an environment marginally favorable for intensification during the next 24 hours.  Elvis will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the eastern side of an upper level trough near southern Africa.  The upper level trough will produce northwesterly winds that will blow toward the top of Elvis’ circulation.  Those winds will cause moderate to strong vertical wind shear. The vertical wind shear will inhibit intensification of Tropical Cyclone Elvis.  Drier air will also inhibit the intensification of Elvis.  The vertical wind shear and the drier air are likely to cause Tropical Cyclone Elvis to weaken during the next 24 hours.

The upper level trough near southern Africa will steer Tropical Cyclone Elvis toward the southeast during the next 24 hours.  On its anticipated track, the center of Tropical of Cyclone Elvis will pass south of southern Madagascar.  Elvis will move away from Madagascar on Friday.

Tropical Cyclone Elvis Forms Near Southwest Madagascar

Tropical Cyclone Elvis formed near southwestern Madagascar on Tuesday night.  At 10:00 p.m. EST on Tuesday the center of Tropical Cyclone Elvis was located at latitude 25.1°S and longitude 42.8°E which put the center about 75 miles (120 km) southwest of Toliara, Madagascar.  Elvis was moving toward the southeast 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 995 mb.

A low pressure system over the Southwest Indian Ocean near southwestern Madagascar strengthened on Tuesday evening and Meteo France La Reunion designated the system as Tropical Cyclone Elvis.  The distribution of thunderstorms in Tropical Cyclone Elvis was asymmetrical.  Thunderstorms were occurring in bands in the eastern and southern parts of Elvis’ circulation.  Bands in the northern and western parts of Tropical Cyclone Elvis consisted primarily of showers and lower clouds.  Storms near the center of Elvis generated upper level divergence that pumped mass away to the southeast of the tropical cyclone.

Tropical Cyclone Elvis will move through an environment marginally favorable for intensification during the next 24 hours.  Elvis will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the eastern side of an upper level trough over southern Africa.  The upper level trough will produce northwesterly winds that will blow toward the top of Elvis’ circulation.  Those winds will cause moderate to strong vertical wind shear.  The vertical wind shear will inhibit intensification of Tropical Cyclone Elvis.  Elvis could intensify a little if the vertical wind shear does not increase.  However, if the wind shear does increase then Elvis is likely to weaken.

Tropical Cyclone Elvis will move around the southwestern part of a high pressure system over the South Indian Ocean.  The high pressure system will steer Elvis slowly toward the southeast during the next 24 hours.  On its anticipated track, the center of Tropical of Cyclone Elvis will pass just to the south of southern Madagascar.

Bands in the northern part of Tropical Cyclone Elvis could bring gusty winds and locally heavy rain to southern Madagascar.  Heavy rain could cause flash floods in some locations.

Tropical Cyclone Sean Continues to Weaken

Tropical Cyclone Sean continued to weaken steadily on Wednesday.  At 10:00 a.m. EST on Wednesday the center of Tropical Cyclone Sean was located at latitude 28.5°S and longitude 107.4°E which put the center about 440 miles (740 km) west of Geraldton, Australia.  Sean was moving toward the south-southeast at 4 m.p.h. (6 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 992 mb.

The effects of cooler Sea Surface Temperatures and strong vertical wind shear caused Tropical Cyclone Sean to continue to weaken on Wednesday.  An upper level trough over the South Indian Ocean west of Australia was producing strong northwesterly winds that were blowing across the top of Sean’s circulation.  Those winds were causing strong vertical wind shear.  The strong upper level winds also blew the tops off of thunderstorms that had been in the southeastern part of Tropical Cyclone Sean.  Bands revolving around the center of Sean’s circulation consisted primarily of showers and lower clouds.

Winds to tropical storm force extended out 130 miles (210 km) from the center of Tropical Cyclone Sean.

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

Tropical Cyclone Sean will move around the western part of a high pressure system over Australia.  The high pressure system will steer Sean toward the south-southeast during the next 24 hours.  On its anticipated track, Tropical Cyclone Sean will move parallel to the coast of Western Australia.

Tropical Cyclone Sean Weakens

Tropical Cyclone Sean weakened over the South Indian Ocean west of Australia on Tuesday.  At 10:00 a.m. EST on Tuesday the center of Tropical Cyclone Sean was located at latitude 26.7°S and longitude 107.3°E which put the center about 380 miles (610 km) west of Carnarvon, Australia.  Sean was moving toward the south-southwest at 16 m.p.h. (26 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 977 mb.

Tropical Cyclone Sean weakened on Tuesday as it moved over cooler water in the South Indian Ocean west of Australia.  An eye was no longer visible in the center of Sean’s circulation.  Thunderstorms were still occurring in bands in the southern and eastern parts of Tropical Cyclone Sean.  Bands in the northern and western parts of Sean’s circulation consisted primarily of showers and lower clouds.  Storms near the center of Sean still produced some upper level divergence that pumped mass away to the southeast of the tropical cyclone.  The removal of mass in the upper levels of the atmosphere was less than the inflow of mass in the lower levels, which caused the surface pressure to increase.

The size of the circulation around Tropical Cyclone Sean increased even though Sean was weakening.  Winds to hurricane/typhoon force extended out 30 miles (50 km) from the center of Sean’s circulation.  Winds to tropical storm force extended out 175 miles (280 km) from the center of Tropical Cyclone Sean.

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

Tropical Cyclone Sean will move around the western part of a high pressure system over Australia.  The high pressure system will steer Sean toward the south during the next 24 hours. On its anticipated track, Tropical Cyclone Sean will move parallel to the coast of Western Australia.

Tropical Cyclone Sean Rapidly Intensifies to Equivalent of Major Hurricane

Tropical Cyclone Sean rapidly intensified to the equivalent of a major hurricane over the South Indian Ocean west of Australia on Monday.  At 10:00 a.m. EST on Monday the center of Tropical Cyclone Sean was located at latitude 23.0°S and longitude 110.4°E which put the center about 210 miles (340 km) west of Exmouth, Australia.  Sean was moving toward the southwest at 13 m.p.h. (21 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 936 mb.

A Warning was in effect for the portion of the coast from Onslow to Ningaloo.  The Warning included Exmouth.

Tropical Cyclone Sean rapidly intensified to the equivalent of a major hurricane west of Australia on Monday.  A small circular eye with a diameter of 10 miles (16 km) was at the center of Sean’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 Sean.  Storms near the core of Sean generated strong upper level divergence that pumped large quantities of mass away from the tropical cyclone.  The removal of large amounts of mass caused the surface pressure to decrease rapidly.

The circulation around Tropical Cyclone Sean was relatively small.  Winds to hurricane/typhoon force extended out 35 miles (55 km) from the center of Sean’s circulation.  Winds to tropical storm force extended out 110 miles (175 km) from the center of Tropical Cyclone Sean.

The Hurricane Intensity Index (HII) for Tropical Cyclone Sean was 25.1.  The Hurricane Size Index (HSI) was 12.6 and the Hurricane Wind Intensity Size Index (HWISI) was 37.7.  Tropical Cyclone Sean was similar in size and intensity to Hurricane Harvey when Harvey hit Texas in 2017.

Tropical Cyclone Sean will move through an environment that will become unfavorable for intensification during the next 24 hours.  Sean will move over water where where the Sea Surface Temperatures are near 27°C.  It will move under the eastern part of an upper level trough over the South Indian Ocean.  The upper level trough will produce northwesterly winds are that will blow toward the top of Sean’s circulation.  Those winds will cause the vertical wind shear to increase.  The combination of cooler water and  more vertical wind shear will cause Tropical Cyclone Sean to weaken during the next 24 hours.

Tropical Cyclone Sean will move around the northwestern part of a high pressure system over Australia.  The high pressure system will steer Sean toward the southwest during the next 24 hours.  On its anticipated track, Tropical Cyclone Sean will move a little farther away from the coast of Western Australia.

Bands in the eastern side of Tropical Cyclone Sea will bring gusty winds and locally heavy rain to the coast of Western Australia.  Heavy rain could cause floods in some locations.  10.78 inches (274 mm) of rain has already fallen at the Karratha Airport.  4.37 inches (111 mm) of rain has already fallen at the Mardie Airport.

Flood Warnings were in effect for parts of the Pilbara and northern Gascoyne regions.  A Flood Warning was in effect for the Lyndon-Minilya Rivers. 

 

Tropical Cyclone Sean Intensifies to Equivalent of Hurricane/Typhoon

Tropical Cyclone Sean intensified to the equivalent of a hurricane/typhoon near the coast of Western Australia on Sunday.  At 10:00 a.m. EST on Sunday the center of Tropical Cyclone Sean was located at latitude 20.5°S and longitude 113.9°E which put the center about 125 miles (200 km) north of Exmouth, Australia.   Sean was moving toward the west-southwest at 12 m.p.h. (19 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 978 mb.

A Warning was in effect for the portion of the coast from Whim Creek to Ningaloo.  The Warning included Karratha, Damoier, Onslow, and Exmouth.

Tropical Cyclone Sea intensified to the equivalent of a hurricane/typhoon near the coast of Western Australia on Sunday.  A circular eye with a diameter of 17 miles (28 km) formed at the center of Sean’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 Sean.  Storms near the core of Sean 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 Sean was relatively small.  Winds to hurricane/typhoon force extended out 25 miles (40 km) from the center of Sean’s circulation.  Winds to tropical storm force extended out 115 miles (185 km) from the center of Tropical Cyclone Sean.

Tropical Cyclone Sean will move through an environment favorable for intensification during the next 24 hours.  Sean will move over water where where the Sea Surface Temperatures are near 30°C.  It will move under the northern part of an upper level ridge northwest of Australia.  The upper level ridge will produce easterly winds are that will blow toward the top of Sean’s circulation.  Those winds will cause some vertical wind shear.  The wind shear will inhibit intensification, but the shear will not be enough to prevent intensification.  Tropical Cyclone Sean will intensify during the next 24 hours.

Tropical Cyclone Sean will move around the northwestern part of a high pressure system over Australia.  The high pressure system will steer Sean toward the west-southwest during the next 24 hours.  On its anticipated track, Tropical Cyclone Sean will move parallel to the coast of Western Australia.  The center of Sean is forecast to remain over water.

Bands in the southern side of Tropical Cyclone Sea will bring gusty winds and locally heavy rain to the coast of Western Australia.  Heavy rain could cause flash floods in some locations.  3.74 inches (95 mm) of rain fell at the Lombadina Airstrip.

A Flood Watch was in effect for the coastal parts of the Kimberley and the Pilbara Districts.  Catchments likely to be affected include the West Kimberley Rivers, the De Grey River, the Pilbara Coastal Rivers, the Fortescue River, the Onslow Coast, and the Lyndon-Minilya Rivers.