Category Archives: Indian Ocean

Tropical Cyclone Ditwah Weakens

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Tropical Cyclone Ditwah was weakening on Sunday as it moved slowly over the southwestern Bay of Bengal east of southern India.  At 10:00 a.m. EST on Sunday the center of Tropical Cyclone Ditwah was located at latitude 11.8°N and longitude 80.6°E which put the center about 55 miles (90 km) east-southeast of Puducherry, India.  Ditwah was moving toward the north at 2 m.p.h. (3 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 1004 mb.

Tropical Cyclone Ditwah was weakening slowly on Sunday.  A few new thunderstorms developed near the center of Ditwah’s circulation.  However, most of the bands revolving around the center of Tropical Cyclone Ditwah consisted of showers and lower clouds.  Thunderstorms were occurring in a couple of bands in the northeastern periphery of Ditwah’s circulation.

Tropical Cyclone Ditwah will move through an environment mostly unfavorable for intensification during the next 24 hours.  Ditwah will move over water where the Sea Surface Temperatures are near 29°C.  It will move under the western part of an upper level ridge that is over Southeast Asia and the Bay of Bengal.  The upper level ridge will produce southeasterly winds that will blow toward the top of Ditwah’s circulation.  Those winds will cause moderate vertical wind shear.  The moderate vertical wind shear will inhibit intensification.  In addition, drier air being pulled into Ditwah’s circulation is likely to limit the formation of new thunderstorms.  Tropical Cyclone Ditwah is likely to continue to weaken slowly during the next 24 hours because of the moderate vertical wind shear and the effects of the drier air.

Tropical Cyclone Ditwah will move around the southwestern part of a high pressure system over the Bay of Bengal.  The high pressure system will steer Ditwah slowly toward the north during the next 24 hours.  On its anticipated track, Tropical Cyclone Ditwah will move nearly parallel to the coast of southeast India.

Tropical Cyclone Ditwah will bring gusty winds and isolated heavy rain to parts of Tamil Nadu and Puducherry.

Tropical Cyclone Ditwah Moves North of Sri Lanka

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Tropical Cyclone Ditwah moved north of Sri Lanka on Saturday.  At 10:00 a.m. EST on Saturday the center of Tropical Cyclone Ditwah was located at latitude 10.2°N and longitude 80.8°E which put the center about 150 miles (240 km) southeast of Puducherry, India.  Ditwah was moving toward the north at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 40 m.p.h. (50 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 1004 mb.

The circulation around Tropical Cyclone Ditwah was pulling in drier air from over India.  The drier air caused the thunderstorms near the center of Ditwah’s circulation to weaken.  Thunderstorms were still occurring in bands in the northern and eastern periphery of Tropical Cyclone Ditwah.  Bands in the other parts of Ditwah’s circulation consisted primarily of showers and lower clouds.

Even though the thunderstorms near the center of Tropical Cyclone Ditwah weakened, Ditwah was still producing winds to tropical storm force.  Winds to tropical storm force extended out 140 miles (225 km) from the center of Ditwah’s circulation.

Tropical Cyclone Ditwah will move through an environment marginally favorable for intensification during the next 24 hours.  Ditwah will move over water where the Sea Surface Temperatures are near 29°C.  It will move under the western part of an upper level ridge that is over Southeast Asia and the Bay of Bengal.  The upper level ridge will produce southeasterly winds that will blow toward the top of Ditwah’s circulation.  Those winds will cause moderate vertical wind shear.  The vertical wind shear will inhibit intensification but the shear may not be enough to prevent some intensification.  However, the drier air being pulled into Ditwah’s circulation is likely to inhibit the formation of new thunderstorms.  Tropical Cyclone Ditwah could maintain its intensity during the next 24 hours.  However, the drier air is likely to cause Ditwah to weaken slowly during the next several days.

Tropical Cyclone Ditwah will move around the southwestern part of a high pressure system over the Bay of Bengal.  The high pressure system will steer Ditwah toward the north during the next 24 hours.  On its anticipated track, Tropical Cyclone Ditwah will move nearly parallel to the coast of southeast India.

Tropical Cyclone Ditwah will bring gusty winds and isolated heavy rain to parts of Tamil Nadu and Puducherry.

Tropical Cyclone Ditwah Spins Near Sri Lanka

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Tropical Cyclone Ditwah continued to spin near Sri Lanka on Friday.  At 10:00 a.m. EST on Friday the center of Tropical Cyclone Ditwah was located at latitude 8.8°N and longitude 80.8°E which put the center about 85 miles (135 km) south-southeast of Jaffna, Sri Lanka.  Ditwah was moving toward the north-northwest at 4 m.p.h. (6 km/h).  The maximum sustained wind speed was 40 m.p.h. (50 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 1004 mb.

The center of Tropical Cyclone Ditwah was still over northern Sri Lanka on Friday morning.  The fact that the center of Ditwah’s circulation was still over land combined with the effects of vertical wind shear to cause the distribution of thunderstorms to be asymmetrical.  Thunderstorms were occurring in bands in the northern and western parts of Tropical Cyclone Ditwah.  Bands in the southern and eastern parts of Ditwah’s circulation consisted primarily of showers and lower clouds.

The strongest winds in Tropical Cyclone Ditwah were occurring over the southwestern Bay of Bengal.   Winds to tropical storm force extended out 110 miles (175 km) from the center of Ditwah’s circulation.  The winds were much weaker over land.

Tropical Cyclone Ditwah will move through an environment somewhat favorable for intensification when the center of its circulation moves back over the southwestern Bay of Bengal in a few hours.  Ditwah will move over water where the Sea Surface Temperatures are near 29°C.  It will move under the western part of an upper level ridge that is over Southeast Asia and the Bay of Bengal.  The upper level ridge will produce southeasterly winds that will blow toward the top of Ditwah’s circulation.  Those winds will cause moderate vertical wind shear.  The vertical wind shear will inhibit intensification but the shear may not be enough to prevent some intensification.  Tropical Cyclone Ditwah could intensify a little during the next 24 hours even with moderate vertical wind shear, when the center of its circulation moves back over water.

Tropical Cyclone Ditwah will move around the southwestern part of a high pressure system over the Bay of Bengal.  The high pressure system will steer Ditwah toward the north-northwest during the next 24 hours.  On its anticipated track, the center of Tropical Cyclone Ditwah will move north of Sri Lanka in a few hours.  Ditwah could reach the coast of Tamil Nadu during the weekend.

Tropical Cyclone Ditwah will continue to affect Sri Lanka and southern India.  Ditwah will bring strong winds and heavy rain to parts of Sri Lanka and Tamil Nadu.  Heavy rain could cause flash floods in some locations.  There were reports that flooding in Sri Lanka had already caused fatalities.

Tropical Cyclone Ditwah Forms Near Sri Lanka

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Tropical Cyclone Ditwah formed over the southwestern Bay of Bengal on Thursday.  At 10:00 a.m. EST on Thursday the center of Tropical Cyclone Ditwah was located at latitude 7.8°N and longitude 81.6°E which put the center about 10 miles (15 km) northwest of Batticaloa, Sri Lanka.  Ditwah was moving toward the northwest at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 40 m.p.h. (50 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 southwestern Bay of Bengal near Sri Lanka intensified on Thursday and the India Meteorological Department designated the system as Tropical Cyclone Ditwah.

The center of Tropical Cyclone Ditwah was near the east coast of Sri Lanka.  About half of Ditwah’s circulation was over Sri Lanka.  A band of thunderstorms was wrapped around the northern and western sides of the center of Tropical Cyclone Ditwah.  Other bands of showers and thunderstorms were revolving around the center of Ditwah’s circulation.  Storms near the center of Ditwah 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 slowly.

The distribution of wind speeds in Tropical Cyclone Ditwah was asymmetrical.  Winds to tropical storm force extended out 175 miles (280 km) in the southern half of Ditwah’s circulation.  Winds to tropical storm force extended out 80 miles (130 km) in the northern side of Tropical Cyclone Ditwah.

Tropical Cyclone Ditwah will move through an environment somewhat favorable for intensification during the next 24 hours.  Ditwah will move over water where the Sea Surface Temperatures are near 29°C.  It will move under the western part of an upper level ridge that is over Southeast Asia and the Bay of Bengal.  The upper level ridge will produce southeasterly winds that will blow toward the top of Ditwah’s circulation.  Those winds will cause moderate vertical wind shear.  The vertical wind shear will inhibit intensification.  The fact that almost half of Ditwah’s circulation is over Sri Lanka will also inhibit intensification.  Tropical Cyclone Ditwah could intensify during the next 24 hours even with moderate vertical wind shear, if the center of its circulation remains over water.

Tropical Cyclone Ditwah will move around the southwestern part of a high pressure system over the Bay of Bengal.  The high pressure system will steer Ditwah toward the northwest during the next 24 hours.  On its anticipated track, the center of Tropical Cyclone Ditwah will move along the coast of northeastern Sri Lanka.  Ditwah could approach the coast of India near Chennai within 72 hours.

Tropical Cyclone Ditwah will produce strong winds and heavy rain over Sri Lanka.  Heavy rain will cause flash floods in some locations.

Tropical Cyclone Senyar Brings Wind and Rain to Northern Sumatra

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Tropical Cyclone Senyar brought wind and rain to northern Sumatra on Wednesday.  At 4:00 a.m. EST on Wednesday the center of Tropical Cyclone Senyar was located at latitude 3.8°N and longitude 98.3°E which put the center about 30 miles (50 km) northwest of Medan, Indonesia.  Senyar was moving toward the south-southeast at 4 m.p.h. (6 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 999 mb.

Tropical Cyclone Senyar was located at latitude 3.8°N which once again proves that tropical cyclones can occur near the Equator.

Tropical Cyclone Senyar continued to be in an environment characterized by strong vertical wind shear.  An upper level ridge over the Western North Pacific Ocean was causing strong easterly winds that were blowing toward the top of Senyar’s circulation.  Those winds were causing strong vertical wind shear.  The strong winds were causing the distribution of thunderstorms in Tropical Cyclone Senyar to be asymmetrical.  Thunderstorms were occurring in bands in the western side of Senyar’s circulation.  Bands in the eastern side of Tropical Cyclone Senyar consisted primarily of showers and lower clouds.

he circulation around Tropical Cyclone Senyar was small.  Winds to tropical storm force extended out 60 miles (95 km) from the center of Senyar’s circulation.

Tropical Cyclone Senyar will move through an environment that will be marginally favorable for intensification during the next 24 hours.  Senyar will move over water where the Sea Surface Temperatures are near 29°C.  However, the upper level ridge over the Western North Pacific Ocean will continue to cause strong vertical wind shear.  The strong vertical wind shear will seriously inhibit intensification, but the shear may not be enough to prevent some intensification.  In addition, the center of Senyar’s circulation will be near the coast of northeastern Sumatra.  Tropical Cyclone Senyar could maintain its intensity during the next 24 hours.

Tropical Cyclone Senyar will move through along trough of low pressure that is near the Equator. The trough of low pressure will steer Senyar toward the southeast during the next 24 hours.  On its anticipated track, Tropical Cyclone Senyar will move along the northeastern coast of Sumatra during the next 24 hours.

Tropical Cyclone Senyar will continue to bring strong winds and heavy rain to Aceh province in northern Sumatra.  Heavy rain is likely to cause floods in some locations.  There are already reports of flooding and casualties in northern Sumatra.

Tropical Cyclone 04B Forms Over Malacca Strait

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Tropical Cyclone 04B formed over the Malacca Strait on Tuesday.  At 10:00 a.m. EST on Tuesday the center of Tropical Cyclone 04B was located at latitude 4.8°N and longitude 98.6°E which put the center about 35 miles (55 km) east-northeast of Langsa, Indonesia.  Tropical Cyclone 04B was moving toward the west-northwest at 4 m.p.h. (6 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 999 mb.

A low pressure system over the Malacca Strait strengthened on Tuesday and the U.S. Joint Typhoon Warning Center designated the system as Tropical Cyclone 04B.  The India Meteorological Department was classifying Tropical Cyclone 04B as a Depression.  It could be the first Tropical Cyclone observed to form over the Malacca Strait in the modern era.

Tropical Cyclone 04B formed in an environment characterized by strong vertical wind shear.  An upper level ridge over the Western North Pacific Ocean was causing strong easterly winds that were blowing toward the top of the tropical cyclone.  Those winds were causing strong vertical wind shear.  The strong winds were causing the distribution of thunderstorms in Tropical Cyclone 04B to be asymmetrical.  Thunderstorms were occurring in bands in the western side of the tropical cyclone.  Bands in the eastern side of Tropical Cyclone 04B consisted primarily of showers and lower clouds.

The circulation around Tropical Cyclone 04B was small.  Winds to tropical storm force extended out 60 miles (95 km) from the center of circulation.

Tropical Cyclone 04B will move through an environment that will be marginally favorable for intensification during the next 12 hours.  Tropical Cyclone 04B will move over water where the Sea Surface Temperatures are near 29°C.  However, the upper level ridge over the Western North Pacific Ocean will continue to cause strong vertical wind shear.  The strong vertical wind shear will seriously inhibit intensification, but the shear may not be enough to prevent some  intensification.  Tropical Cyclone 04B could intensity a little during the next 12 hours.

Tropical Cyclone 04B will move around the southwestern end of a high pressure system that is over the Western North Pacific Ocean and Southeast Asia.  The high pressure system will steer the tropical cyclone toward the west-northwest during the next 24 hours.  On its anticipated track, Tropical Cyclone 04B will make landfall in northern Sumatra near Idi in 12 hours.

Tropical Cyclone 04B will bring strong winds and heavy rain to Aceh province in northern Sumatra.  Heavy rain is likely to cause flash floods in some locations.

Tropical Cyclone Fina Hits Kimberley Coast

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Tropical Cyclone Fina hit the northeast Kimberley coast of Australia on Monday.  At 10:00 a.m. EST on Monday the center of Tropical Cyclone Fina was located at latitude 14.3°S and longitude 127.9°E which put the center about 80 miles (130 km) east of Kalumburu, Australia.  Fina was moving toward the southwest at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 125 m.p.h. (200 km/h) and there were wind gusts to 155 m.p.h. (250 km/h).  The minimum surface pressure was 946 mb.

Tropical Cyclone Fina hit the northeast Kimberley coast of Australia near the Mouth of the Berkeley River on Monday.  Fina was the equivalent of a major hurricane at the time of landfall.  Tropical Cyclone Fina was bringing strong destructive winds and heavy rain to the region near the Mouth of the Berkeley River.  Fina was also causing a strong storm surge in the small area near the center of its circulation.

The circulation around Tropical Cyclone Fina was very small.  Winds to hurricane/typhoon force extended out 20 miles (30 km) from the center of Fina’s circulation.  Winds to tropical storm force extended out 70 miles (110 km) from the center of Tropical Cyclone Fina.

The Hurricane Intensity Index (HII) for Tropical Cyclone Fina was 23.6.  The Hurricane Size Index (HSI) was 6.0 and the Hurricane Wind Intensity Size Index (HWISI) was 29.6.  Tropical Cyclone Fina was similar in intensity to Hurricane Dennis when Dennis hit Northwest Florida in 2005.  Fina was not as large as Dennis was.

Tropical Cyclone Fina will move around the western end of a high pressure system over northern Australia.  The high pressure system will steer Fina toward the southwest during the next 24 hours. On its anticipated track, Tropical Cyclone Fina will move inland over the Kimberley Plateau.

Tropical Cyclone Fina will weaken quickly because of its small size as it moves over the Kimberley Plateau.  Fina will continue to produce strong winds and to drop locally heavy rain as it moves inland.  Heavy rain is likely to cause flash floods in some locations.

 

Tropical Cyclone Fina Moves Over Timor Sea

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Tropical Cyclone Fina was moving over the Timor Sea on Sunday after it caused wind damage and electricity outages in Darwin.  At 10:00 a.m. EST on Sunday the center of Tropical Cyclone Fina was located at latitude 13.7°S and longitude 128.8°E which put the center about 155 miles (250 km) west-southwest of Darwin, Australia.  Fina was moving toward the southwest at 7 m.p.h. (11 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 960 mb.

A Warning was in effect for the portion of the coast from Wadeye, Australia to the Daly River Mouth.  A Warning was also in effect for the portion of the coast from the border between the Northern Territory and Western Australia to Kalumburu.

Tropical Cyclone Fina was still a well organized tropical cyclone on Sunday.  A small circular eye was visible at the center of Fina’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 Fina.  Storms near the core of Fina 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 Fina was small.  Winds to hurricane/typhoon force extended out 20 miles (30 km) from the center of Fina’s circulation.  Winds to tropical storm force extended out 70 miles (110 km) from the center of Tropical Cyclone Fina.

The Hurricane Intensity Index (HII) for Tropical Cyclone Fina was 19.2.  The Hurricane Size Index (HSI) was 7.4 and the Hurricane Wind Intensity Size Index (HWISI) was 26.6.  Tropical Cyclone Fina was similar in size and intensity to Hurricane Zeta when Zeta hit Louisiana in 2020.

Tropical Cyclone Fina will move through an environment that will become unfavorable for intensification during the next 24 hours.  Fina will move over water where the Sea Surface Temperatures are near 30°C.  It will move under the western end of an upper level ridge over northern Australia.  The upper level ridge will produce northerly winds that will blow toward the top of Fina’s circulation.  Those winds will cause some vertical wind shear.  The vertical wind shear will inhibit intensification, but the wind shear may not be enough to prevent intensification.  However, the circulation around the eastern side of Tropical Cyclone Fina will begin to pull drier air from northwestern Australia into its circulation.  The drier air will cause thunderstorms in the eastern side of Fina’s circulation to start to weaken.  The effects of the drier air will cause Tropical Cyclone Fina to start to weaken during the next 24 hours.

Tropical Cyclone Fina will move around the western end of a high pressure system over northern Australia.  The high pressure system will steer Fina toward the west-southwest during the next 24 hours.  On its anticipated track, the center of Tropical Cyclone Fina will reach the coast of Western Australia near of the King George River Mouth in 24 hours.

Tropical Cyclone Fina will continue to bring strong winds and heavy rain to the coast of the Western Australia northeast of Kalumburu.  Heavy rain is likely to cause floods in some locations.  Tropical Cyclone Fina could also cause a storm surge of up to 7 feet (2 meters) along parts of the coast of the Western Australia.

Flood Watches are in effect for the North West Coastal Rivers and the Bonaparte Coastal Rivers.

Tropical Cyclone Fina Brings Wind and Rain to Darwin

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Tropical Cyclone Fina brought wind and rain to Darwin, Australia on Saturday.  At 10:00 a.m. EST on Saturday the center of Tropical Cyclone Fina was located at latitude 12.2°S and longitude 130.4°E which put the center about 35 miles (55 km) northwest of Darwin, Australia.  Fina was moving toward the west-southwest at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 100 m.p.h. (160 km/h) and there were wind gusts to 120 m.p.h. (195 km/h).  The minimum surface pressure was 967 mb.

A Warning is in effect for the portion of the coast from Cape Hotham to Wadeye, Australia.  The Warning includes Darwin.  A Warning is also in effect for the western and central Tiwi Islands.

A Watch is in effect for the portion of the coast from Wadeye to Troughton Island, Australia.  The Watch includes Kalumburu.

Tropical Cyclone Fina brought wind and rain to the area around Darwin, Australia on Saturday.  The core of Fina’s circulation, where the strongest winds were, was passing to the northwest of Darwin.  A weather station at the Darwin Airport reported a sustained wind speed of 37 m.p.h. (57 km/h) and a wind gust to 53 m.p.h. (85 km/h).  The weather station also measure 5.89 inches (149.6 mm) of rain.

Tropical Cyclone Fina intensified to the equivalent of a Category 2 hurricane on the Saffir-Simpson Scale as it moved over the Timor Sea.  A very small eye was present at the center of Fina’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 Fina.  Storms near the core of Fina 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 Fina was small.  Winds to hurricane/typhoon force extended out 20 miles (30 km) from the center of Fina’s circulation.  Winds to tropical storm force extended out 75 miles (120 km) from the center of Tropical Cyclone Fina.

The Hurricane Intensity Index (HII) for Tropical Cyclone Fina was 16.5.  The Hurricane Size Index (HSI) was 7.5 and the Hurricane Wind Intensity Size Index (HWISI) was 24.0.  Tropical Cyclone Fina was similar in size and intensity to Hurricane Idalia when Idalia hit Florida in 2023.

Tropical Cyclone Fina will move through an environment somewhat favorable for intensification while it moves over the Timor Sea during the next 24 hours.  Fina will move over water where the Sea Surface Temperatures are near 30°C.   It will move under the western end of an upper level ridge over northern Australia.  The upper level ridge will produce northerly winds that will blow toward the top of Fina’s circulation.  Those winds will cause some vertical wind shear.  The vertical wind shear will inhibit intensification, but the wind shear may not be enough to prevent intensification.  Tropical Cyclone Fina could intensify during the next 24 hours.  Fina could strengthen to the equivalent of a major hurricane.

Tropical Cyclone Fina will move around the western end of a high pressure system over northern Australia.  The high pressure system will steer Fina toward the southwest during the next 24 hours.   On its anticipated track, the center of Tropical Cyclone Fina will move away from Darwin during the next 24 hours.   Fina will approach the coast of Western Australia northeast of Kalumburu in 36 hours.

Tropical Cyclone Fina will continue to bring strong winds and heavy rain to the coast of the Northern Territory of Australia southwest of Darwin.  Heavy rain is likely to cause floods in some locations.  Tropical Cyclone Fina could also cause a storm surge of up to 10 feet (3 meters) along parts of the coast of the Northern Territory.

Flood Watches are in effect for the North West Coastal Rivers and the Bonaparte Coastal Rivers.

Tropical Cyclone Fina Crosses Cobourg Peninsula

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Tropical Cyclone Fina moved across the Cobourg Peninsula in northern Australia on Friday.  At 4:00 p.m. EST on Friday the center of Tropical Cyclone Fina was located at latitude 11.8°S and longitude 131.6°E which put the center about 80 miles (130 km) northeast of Darwin, Australia.   Fina was moving toward the southwest at 8 m.p.h. (13 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 979 mb.

A Warning is in effect for the portion of the coast from Daly River Mouth to Cape Don, Australia.  The Warning includes Darwin.  A Warning is also in effect for the Tiwi Islands.

A Watch is in effect for the portion of the coast from Wadeye to Daly River Mouth.

Tropical Cyclone Fina intensified a little after it crossed the Cobourg Peninsula and moved over the Van Dieman Gulf.  A small circular eye was at the center of Fina’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 Fina.  Storms near the core of Fina 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 Fina was small.  Winds to hurricane/typhoon force extended out 20 miles (30 km) from the center of Fina’s circulation.  Winds to tropical storm force extended out 70 miles (110 km) from the center of Tropical Cyclone Fina.

Tropical Cyclone Fina will move through an environment somewhat favorable for intensification while it moves over the Van Dieman Gulf during the next few hours. Fina will move over water where the Sea Surface Temperatures are near 30°C.  It will move under the western end of an upper level ridge over northern Australia.  The upper level ridge will produce northerly winds that will blow toward the top of Fina’s circulation.  Those winds will cause some vertical wind shear.  The vertical wind shear will inhibit intensification, but the wind shear may not be enough to prevent intensification.  Tropical Cyclone Fina could intensify during the next 24 hours.

Tropical Cyclone Fina will move around the western end of a high pressure system over northern Australia.  The high pressure system will steer Fina toward the southwest during the next 24 hours.   On its anticipated track, the center of Tropical Cyclone Fina will pass near Darwin in 12 hours.   Fina will move over the Timor Sea on Saturday.

Tropical Cyclone Fina will bring strong winds and heavy rain to the coast of the Northern Territory of Australia.  Heavy rain is likely to cause floods in some locations.  Tropical Cyclone Fina could also cause a storm surge of up to 7 feet (2 meters) along parts of the coast of the Northern Territory.

Flood Watches are in effect for the North West Coastal Rivers.