Tropical Cyclone Cilida Forms North of Mauritius

Tropical Cyclone Cilida formed north of Mauritius on Wednesday.  At 10:00 p.m. EST on Wednesday the center of Tropical Cyclone Cilida was located at latitude 12.2°S and longitude 59.8°E which put it about 585 miles (945 km) north-northeast of Port Louis, Mauritius.  Cilida was moving toward the southwest at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 55 m.p.h. (90 km/h) and there were wind gusts to 70 m.p.h. (110 km/h).  The minimum surface pressure was 989 mb.

The circulation around Tropical Cyclone Cilida organized quickly on Wednesday. A small circular eye formed at the center of circulation.  A ring of strong thunderstorms formed around the eye and the strongest winds were occurring in that ring of storms.  A strong band of storms wrapped around the western and northern sides of Cilida.  Other bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Cilida.  Winds to tropical storm force extended out about 100 miles (160 km) from the center of circulation.

Tropical Storm Cilida will move through an environment favorable for intensification during the next 48 to 72 hours.  Cilida will move over water where the Sea Surface Temperature is near 27°C.  It will move through an area where the upper level winds are weak and there will be little vertical wind shear.  Cilida is likely to strengthen into the equivalent of a hurricane/typhoon on Thursday and it could intensify rapidly.  Tropical Cyclone Cilida could intensify into the equivalent of a major hurricane in two or three days.

Tropical Cyclone Cilida will move around the western end of a subtropical ridge.  The ridge will steer Cilida toward the south during the next several days.  On its anticipated track Tropical Cyclone Cilida could approach Mauritius from the north in about 48 hours.

Elsewhere over the South Indian Ocean Tropical Cyclone Kenanga drifted southeast of Diego Garcia.  At 10:00 p.m. EST on Wednesday the center Tropical Cyclone Kenanga was located at latitude 16.5°S and longitude 81.9°E which put it about 910 miles (1470 km) southeast of Diego Garcia.  Kenanga was stationary.  The maximum sustained wind speed was 125 m.p.h. (205 km/h) and there were wind gusts to 155 m.p.h. (250 km/h).  The minimum surface pressure was 947 mb.

Tropical Cyclone Kenanga Intensifies Into Equivalent of a Major Hurricane

Tropical Cyclone Kenanga intensified into the equivalent of a major hurricane on Tuesday.  At 10:00 p.m. EST on Tuesday the center of Tropical Cyclone Kenanga was located at latitude 15.9°S and longitude 82.6°E which put it about 920 miles (1485 km) southeast of Diego Garcia.  Kenanga was moving toward the southwest at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 130 m.p.h. (215 km/h) and there were wind gusts to 160 m.p.h. (260 km/h).  The minimum surface pressure was 944 mb.

Tropical Cyclone Kenanga intensified quickly into the equivalent of a major hurricane on Tuesday.  A large circular eye with a diameter of 50 miles (80 km) formed at the center of circulation.  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 Kenanga.  Storms around the core of Kenanga were generating upper level divergence which was pumping mass away to the west and north of the tropical cyclone.  Winds to hurricane/typhoon force extended out about 60 miles (95 km) from the center of circulation.  Winds to tropical storm force extended out about 200 miles (320 km) from the center.

Tropical Cyclone Kenanga may be near its peak intensity.  Kenanga is over water where the Sea Surface Temperature is near 28°C, but it will start to move over slightly cooler water during the next day or two.  Tropical Cyclone Kenanga is in an area where the upper level winds are weak and there is little vertical wind shear.  However, Kenanga will move closer to upper level westerly winds in the middle latitudes later this week and the vertical wind shear will increase.  Tropical Cyclone Kenanga could maintain its intensity or weaken slowly during the next day or so.  Kenanga could weaken more quickly later this week.

Tropical Cyclone Kenanga will move south of a subtropical ridge over the South Indian Ocean.  The ridge will continue to steer Kenanga toward the southwest.  On its anticipated track Tropical Cyclone Kenanga will pass well to the south of Diego Garcia.

Elsewhere over the South Indian Ocean Tropical Cyclone 07S developed north-northeast of Mauritius.  At 10:00 p.m. EST on Tuesday the center of Tropical Cyclone 07S was located at latitude 10.9°S and longitude 60.8°E which put it about 690 miles (1115 km) north-northeast of Port Louis, Mauritius.  It was moving toward the south-southwest at 3 m.p.h. (5 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 998 mb

Tropical Cyclone Phethai Brings Wind and Rain to India

Tropical Cyclone Phethai brought wind and rain to parts of eastern India on Sunday night.  The center of Phethai made landfall southwest of Visakhapatnam, India near the Mouths of the Godavari.  At 10:00 p.m. EST on Sunday the center of Tropical Cyclone Phethai was located at latitude 15.7°N and longitude 82.4°E which put it about 150 miles (240 km) southwest of Visakhapatnam.  Phethai was moving toward the north at 11 m.p.h. (17 km/h).  The maximum sustained wind speed was 55 m.p.h. (90 km/h) and there were wind gusts to 75 m.p.h. (120 km/h).  The minimum surface pressure was 989 mb.

Tropical Cyclone Phethai strengthened earlier on Sunday, but it started to weaken slightly when it approached the east coast of India.  Phethai moved over slightly cooler water as it moved farther north over the western Bay of Bengal.  Tropical Cyclone Phethai moved closer to upper level westerly winds in the middle latitudes and the vertical wind shear increased.  Cooler water and more wind shear caused Phethai to start to weaken when it approached the coast.

Even though Tropical Cyclone Phethai started to weaken when it approached the coast of India, the circulation remained well organized.  There was a distinct center of circulation.  Stronger thunderstorms were occurring just to the west of the center.  Additional bands of showers and thunderstorms were located north and east of the center of Tropical Cyclone Phethai.  Winds to tropical storm force extended out about 140 miles (225 km) from the center of circulation.

Tropical Cyclone Phethai is moving around the western end of a ridge of high pressure over southeast Asia.  The ridge will steer Phethai in a north-northeasterly direction.  On its anticipated track Tropical Cyclone Phethai will move over eastern Andhra Pradesh and southern Orissa.  Phethai will drop locally heavy rain as it moves inland and flash flooding could occur in some locations.

Elsewhere, Tropical Cyclone Kenanga strengthened over the South Indian Ocean.  At 10:00 p.m. EST on Sunday the center of Tropical Cyclone Kenanga was located at latitude 12.7°S and longitude 83.7°E which put it about 1095 miles (1770 km) east-southeast of Diego Garcia.  Kenanga was moving toward the southwest at 20 m.p.h. (32 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 987 mb.

Tropical Cyclone Phethai Forms Over Southwest Bay of Bengal

Tropical Cyclone Phethai formed over the southwest Bay of Bengal on Saturday.  At 4:00 p.m. EST on Saturday the center of Tropical Cyclone Phethai was located at latitude 11.1°N and longitude 84.5°E which put it about 480 miles (775 km) south-southeast of Visakhapatnam, India.  Phethai was moving toward the northwest 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 994 mb.

More thunderstorms developed closer to the center of a low pressure system over the southwestern Bay of Bengal and the Indian Meteorological Department designated the system as Tropical Cyclone Phethai.  The distribution of thunderstorms was asymmetrical.  Most of the stronger thunderstorms were occurring northwest of the center of circulation.  There were fewer thunderstorms southeast of the center, although several bands of thunderstorms were developing on the eastern periphery of the circulation.  Storms northwest of the center were generating upper level divergence which was pumping mass away to the north of the tropical cyclone.

Tropical Cyclone Phethai will move through an environment somewhat favorable for intensification.  Phethai will move over water where the Sea Surface Temperature is near 27°C.  It will move around the eastern end of an upper level ridge over southeast Asia.  The ridge is already producing southeasterly winds which are blowing toward the top of the circulation.  Those winds are causing moderate vertical wind shear and the shear is the reason for the asymmetrical distribution of thunderstorms.  The wind shear will continue and it will inhibit the intensification of Tropical Cyclone Phethai.  Phethai could strengthen during the next 24 to 36 hours, but the rate of intensification is likely to be slow.

The ridge over southeast Asia will steer Tropical Cyclone Phethai north-northwest during the next several days.  On its anticipated track Phethai will move toward the east coast of India.  Tropical Cyclone Phethai could approach the coast near Visakhaptnam in about 48 hours.  Phethai will bring gusty winds but heavy rain and flooding will be greater risks.

Elsewhere, Tropical Cyclone 06S formed over the South Indian Ocean on Saturday.  At 4:00 p.m. EST on Saturday the center of Tropical Cyclone 06S was located at latitude 9.1°S and longitude 91.2°E which put it about 1285 miles (2070 km) east of Diego Garcia.  It was moving toward the south-southeast at 3 m.p.h. (5 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 998 mb.

Tropical Cyclone Owen Makes Landfall in Queensland

After making landfall on the southwest coast of the Gulf of Carpentaria, Tropical Cyclone Owen reversed course and it is now making landfall on the coast of Queensland between Kowanyama and the Gilbert River Mouth.  At 1:00 p.m. EST on Friday the center of Tropical Cyclone Owen was located at latitude 16.2°S and longitude 141.4°E which put it about 55 miles (85 km) south-southwest of Kowanyama, Australia.  Owen was moving toward the southeast 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 975 mb.

A Tropical Storm Warning was in effect for the portion of the coast from Karumba to Cape Keerweer, Queensland and adjacent coastal areas including Kowanyama, Pormpuraaw, Croydon and Palmerville.

Tropical Cyclone Owen moved quickly across the southern Gulf of Carpentaria during the past 24 hours.  The circulation around Owen reorganized after the center of circulation moved away from the southwest coast of the Gulf of Carpentaria.  An eye reformed at the center of circulation and more thunderstorms developed.  Tropical Cyclone Owen strengthened back into the equivalent of a hurricane/typhoon.  The circulation around Owen is small.  Winds to hurricane/typhoon force only extend out about 20 miles (35 km) from the center of circulation.  Winds to tropical storm force extend out about 100 miles (160 km) from the center.

Tropical Cyclone Owen will be capable of causing minor wind damage over a localized area near the center of circulation.  Locally heavy rain will fall along the track of Owen as it moves inland across Queensland.  On its anticipated track the center of Tropical Cyclone Owen is forecast to pass south of Cairns and it could be near Townsville in about 36 hours.  The rain will likely cause flooding in some locations.  A Flood Warning has been issued for the Jordan River.  Flood Watches have been issued for the Gulf of Carpentaria, south Cape York Peninsula and coastal catchments from Cape Tribulation to Rainbow Beach in Queensland.

Tropical Cyclone Owen Near Coast of Australia

The center of Tropical Cyclone Owen was near the coast of Australia on Wednesday.  At 4:00 p.m. EST on Wednesday the center of Tropical Cyclone Owen was located at latitude 15.2°S and longitude 136.1°E which put it about 55 miles (90 km) northwest of Port McArthur, Australia.  Owen was moving toward the southwest at 5 m.p.h. (8 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.  Tropical Cyclone Owen was the equivalent of a hurricane/typhoon.

The center of Tropical Cyclone Owen was near the portion of the coast between Port Roper and Port McArthur in the Northern Territory of Australia.  Owen was producing winds to near hurricane/typhoon force.  It was dropping locally heavy rain over the southeastern coastal portions of the Northern Territory.

A Tropical Cyclone Warning was in effect for the portion of the coast between Alyangula, Northern Territory and Burketown, Queensland  including Groote Eylandt, Mornington Island and Borroloola.  A Tropical Cyclone Watch was in effect for the portion of the coast from Burketown to Aurukun, Northern Territory and adjacent inland areas including Pormpuraaw, Kowanyama and Karumba.  Flood Watches were in effect for the Gulf of Carpentaria, south Cape York Peninsula and North Tropical Coast catchments in Queensland.

Tropical Cyclone Owen strengthened and exhibited greater organization on Wednesday.  A small circular eye developed at the center of circulation.  A ring of strong thunderstorms surrounded the eye and the strongest winds were occurring in that ring of storms.  Several bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Owen.  The strongest rainbands were over the Gulf of Carpentaria.  Storms around the core of Owen were generating upper level divergence which was pumping mass away to the southeast of the tropical cyclone.

The circulation around Tropical Cyclone Owen was relatively small.  Winds to hurricane/typhoon force extended out only about 20 miles (30 km) from the center of circulation.  Winds to tropical storm force extended out about 80 miles (130 km) from the center.

Tropical Cyclone Owen will move through an environment favorable for intensification for another 24 to 36 hours.  Owen will move over water where the Sea Surface Temperature is near 30°C.  An upper level trough over Western Australia and an upper level ridge northeast of Australia will combine to produce northwesterly winds which 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 further intensification.  The center of Tropical Cyclone Own is close to the coast and part of the circulation is over land.  Owen could weaken during the next few hours, while the center is near land.  It should strengthen when the center moves back over the Gulf of Carpentaria.

Tropical Cyclone Owen is an area where the steering currents are weak and it is moving slowly toward the southwest.  The trough over Western Australia will start to steer Owen toward the east-southeast during the next 12 hours.  On its anticipated track the center of Tropical Cyclone Owen could pass just north of Port McArthur in about 12 hours.  Owen could pass north of Mornington Island in about 18 hours.  Tropical Cyclone Owen could approach the southeast of coast of the Gulf of Carpentaria in about 36 hours.  Owen is likely to be the equivalent of a hurricane/typhoon at that time.

Tropical Cyclone Owen will bring gusty winds and locally heavy rain to the southern portions of the Gulf of Carpentaria.  Owen will be capable of causing minor wind damage while it lingers near the southeast coast of the Northern Territory.  It will also drop locally heavy rain in coastal areas and flooding could occur.  Tropical Cyclone Owen will be stronger when it brings wind and rain to parts of Queensland.

Tropical Cyclone Owen Redevelops Over Gulf of Carpentaria

After meandering westward over the Coral Sea last week and crossing northern Queensland, Tropical Cyclone Owen redeveloped over the Gulf of Carpentaria on Tuesday.  At 10:00 a.m. EST on Tuesday the center of Tropical Cyclone Owen was located at latitude 14.9°S and longitude 138.4°E which put it about 135 miles (215 km) north-northwest of Mornington Island, Australia.  Owen was moving toward the west-northwest 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 993 mb.

The circulation around Tropical Cyclone Owen exhibited increased organization after it moved over the Gulf of Carpentaria and the Australian Bureau of Meteorology reclassified the system as a tropical cyclone on Tuesday.  A band of showers and thunderstorms was wrapping around the southern and western sides of the center of circulation and the strongest winds were occurring in that band of storms.  Other bands of showers and thunderstorms were strengthening over the Gulf of Carpentaria.  Storms near the center of circulation started to generate upper level divergence which was pumping mass away from the tropical cyclone.

A Tropical Cyclone Warning is in effect for the portion of the coast from Cape Shield, Northern Territory to Burketown, Queensland including Groote Eylandt and Mornington Island.

Tropical Cyclone Owen will move through an environment favorable for intensification during the next several days.  Owen will move over water where the Sea Surface Temperature is near 30°C.  It will move in an area between an upper level ridge north of Australia and a larger upper level ridge over the South Pacific Ocean where the upper level winds are weaker.  There will be some vertical wind shear, but the wind shear will not be strong enough to prevent intensification.  Tropical Cyclone Owen will intensify during the next two days and it could strengthen into the equivalent of a hurricane/typhoon.

The ridge north of Australia will steer Tropical Cyclone Owen toward the west-northwest during the next 24 hours.  On its anticipated track Tropical Cyclone Owen could be near Groote Eylandt in about 24 hours.  An upper level trough over Western Australia will move eastward and the trough will cause the winds in the steering levels to weaken in a day or so.  Owen could drift slowly southward for 12 to 24 hours when that happens.  Eventually, westerly winds blowing around the northern end of the trough are forecast to turn Tropical Cyclone Owen back toward the east.

Tropical Cyclone Owen could bring gusty winds and drop locally heavy rain over Groote Eylandt when it passes nearby.  If Owen drifts southward as expected, it could also bring gusty winds and heavy rain to the western coast of the Gulf of Carpentaria near Port McArthur.

Former Tropical Cyclone Owen Drops Rain on Northern Queensland

After meandering westward across the Coral Sea during the past week a low pressure system formerly designated as Tropical Cyclone Owen dropped rain on northern Queensland on Sunday.  At 7:00 p.m. EST on Sunday the center of former Tropical Cyclone Owen was located at latitude 15.7°S and longitude 144.5°E which put it about 75 miles (120 km) west of Cairns, Australia.  Owen was moving toward the west-northwest at 7 m.p.h.  The maximum sustained wind speed was 25 m.p.h. (40 km/h) and there were wind gusts to 35 m.p.h. (55 km/h).  The minimum surface pressure was 1006 mb.

Although it is no longer formally designated as a tropical cyclone, the low pressure center that was Tropical Cyclone Owen maintains a distinct low level center of circulation.  Bands of showers and thunderstorms are revolving around the center.  Some of those bands are moving inland over northern Queensland and they are dropping locally heavy rainfall.  Flooding could develop in areas that receive persistent heavy rain.

Flood Watches are in effect for the Mulgrave River, Russell River, Johnstone River, Murray River, Tully River, and Herbert River.

Former Tropical Storm Owen is forecast to move toward the west-northwest across the Cape York Peninsula.  It could emerge over the Gulf of Carpentaria early in the week.  There is a possibility that the low pressure system could strengthen when it moves back over water.

 

Tropical Cyclone Owen Develops Over the Coral Sea

Tropical Cyclone Owen developed over the Coral Sea on Sunday.  Thunderstorms developed near the center of a tropical low over the Coral Sea and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Owen.  At 4:00 p.m. EST on Sunday the center of Tropical Cyclone Owen was located at latitude 15.4°S and longitude 154.9°E which put it about 615 miles (990 km) east of Cairns, Australia.  Owen was moving toward the south 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 996 mb.

The circulation of Tropical Cyclone Owen became better organized on Sunday.  A band of thunderstorms wrapped around the eastern and southern sides of the center of circulation.  Additional bands of showers and thunderstorms were developing in the eastern half of the circulation.  Bands in the western half of Tropical Cyclone Owen consisted primarily of showers and lower clouds.  Storms near the center of circulation were generating upper level divergence which was pumping mass away to the east of the tropical cyclone.

Tropical Cyclone Owen will move through an environment marginally favorable for intensification during the next 24 to 36 hours.  Owen will move over water where the Sea Surface Temperature is near 29°C.  It will move through a region where the upper level winds will blow from the west.  Those winds will blow toward the top of the circulation and they are already causing moderate vertical wind shear.  The wind shear is the likely reason why most of the stronger thunderstorms are developing in the eastern half of the circulation.  The westerly winds will inhibit upper level divergence to the west of the tropical cyclone and the wind shear will limit intensification.  Tropical Cyclone Owen could strengthen during the next day or two, but the wind shear is likely to weaken Owen later this week.

Tropical Cyclone Owen will move north of a subtropical ridge in the middle troposphere.  The ridge is forecast to turn Owen toward the west and to steer the tropical cyclone toward the west during the next few days.  On its anticipated track Tropical Cyclone Owen is forecast to move slowly westward during the next several days.  Owen could be east of Willis Island in three or four days.

Tropical Storm Usagi Makes Landfall South of Ho Chi Minh City

Tropical Storm Usagi made landfall south of Ho Chi Minh City, Vietnam on Saturday night.  At 10:00 p.m. EST on Saturday the center of Tropical Storm Usagi was located at latitude 10.2°N and longitude 107.1°E which put it about 60 miles (995 km) south-southeast of Ho Chi Minh City, Vietnam.  Usagi was moving toward the west at 5 m.p.h. (8 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 984 mb.

Former Typhoon Usagi weakened as it approached the coast of southern Vietnam.  Moderate vertical wind shear caused by upper level winds blowing from the east caused Usagi to weaken slowly.  The core of Tropical Storm Usagi was still relatively intact.  A ring of strong thunderstorms surrounded the remnants of the small eye.  The strongest winds were occurring in that ring of storms.  Heavy rain was falling just to the southwest of the center of circulation.  Thunderstorms were also dropping heavy rain in a couple of bands on the northeastern periphery of the circulation.

Tropical Storm Usagi will bring gusty winds to the areas south and west of Ho Chi Minh City.  Some places in southern Vietnam and Cambodia will receive locally heavy rainfall and flash floods could occur in those areas.  Usagi will weaken slowly as it move inland over southern Vietnam.

Elsewhere over the Western North Pacific Ocean, Typhoon Man-yi was meandering slowly southeast of Okinawa.  At 10:00 p.m. EST on Saturday the center of Typhoon Man-yi was located at latitude 18.4°N and longitude 135.8°E which put it about 770 miles (1245 km) southeast of Okinawa.  Man-yi was moving toward the west at 2 m.p.h. (3 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.