Tag Archives: Australia

Two Tropical Lows Form over South Pacific

Two tropical lows formed over the South Pacific Ocean on Saturday morning. The first Tropical Low formed over the Coral Sea east of the Cape York Peninsula. At 7:00 a.m. EST on Saturday the center of that Tropical Low was located at latitude 13.0°S and longitude 147.8°E which put it about 240 miles (350 km) northeast of Cooktown, Australia. The Tropical Low was nearly stationary. The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were wind gusts to 40 m.p.h. (65 km/h). The minimum surface pressure was 1004 mb.

A well defined low level center of circulation formed in a small low pressure system over the Coral Sea on Saturday morning and the Australian Bureau of Meteorology designated the system as a Tropical Low. A Watch was issued for the portion of the east coast of the Cape York Peninsula from Cape Grenville to Cape Tribulation. The distribution of thunderstorms around the Tropical Low was asymmetrical. The distribution of thunderstorms around the Tropical Low was asymmetrical. The strongest thunderstorms were occurring in bands in the northwestern quadrant of the circulation. Bands in other parts of the circulation consisted primarily of showers and lower clouds. Storms near the center began to generate upper level divergence that pumped mass away from the Tropical Low.

The Tropical Low will move through an environment somewhat favorable for intensification during the next 24 hours. The Tropical Low will move over water where the Sea Surface Temperatures are near 30˚C. It will move under the northwestern part of an upper level ridge centered east of Australia. The ridge will produce easterly winds that will blow toward the top of the Tropical Low’s circulation. Those winds will cause some vertical wind shear and the shear will inhibit intensification. The Tropical Low could intensify gradually during the next 24 hours.

The Tropical Low will move north of a high pressure system centered east of Australia. The high pressure system will steer the Tropical Low toward the west during the next 24 hours. On its anticipate track the Tropical Low could approach the eastern Cape York Peninsula between Lockhart River and Cooktown in 36 hours. It could be a named tropical cyclone when it approaches the coast.

The second Tropical Low developed over the South Pacific Ocean west of Fiji. At 10:00 a.m. EST on Saturday the center of the second Tropical Low was located at latitude 18.6°S and longitude 173.3°E which put it about 320 miles (515 km) west-southwest of Nadi, Fiji. That Tropical Low was moving toward the 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 1000 mb.

A distinct low level center of circulation developed in a large low pressure system over the South Pacific Ocean west of Fiji and the Fiji Meteorological Service designated the system as a tropical low. The circulation around the second Tropical Low was much larger than the one over the Coral Sea, but the distribution of thunderstorms was also asymmetrical. The strongest thunderstorms were occurring in bands north and east of the center of circulation. Bands south and west of the center consisted primarily of showers and lower clouds. Storms near the center generated upper level divergence that pumped mass away from Tropical Low.

The second Tropical Low will move through an environment favorable for intensification during the next 24 hours. The Tropical Low will move over water where the Sea Surface Temperatures are near 30˚C. It will move through an area where the upper level winds are weak and there will be little vertical wind shear. The Tropical Low is likely to intensify into a named tropical cyclone during the next 24 hours.

The second Tropical Low will be in an area where the steering currents are weak during the next 24 hours. It is likely to meander slowly over the South Pacific Ocean between Fiji and Vanuatu during the next day or so.

Tropical Cyclone Seth Speeds South

Tropical Cyclone Seth sped toward the south over the Coral Sea east of Australia on Saturday night. At 7:00 p.m. EST on Saturday the center of Tropical Cyclone Seth was located at latitude 25.8°S and longitude 159.0°E which put it about 385 miles (620 km) east-northeast of Brisbane, Australia. Seth was moving toward the south at 25 m.p.h. (41 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 987 mb.

An upper level trough over eastern Australia and an upper level ridge east of the Coral Sea were combining to steer Tropical Cyclone Seth quickly toward the south on Saturday night. The structure of Seth’s circulation was beginning to resemble a subtropical cyclone. The strongest thunderstorms were occurring in bands south of the center of circulation. Bands in the northern half of Tropical Cyclone Seth consisted primarily of showers and lower clouds. The upper level trough and upper level ridge were producing strong northerly winds that were blowing toward the top of Seth’s circulation. Those winds were causing strong vertical wind shear. Drier air was wrapping around the northern side of Tropical Cyclone Seth. The strong vertical wind shear and drier air were causing the asymmetrical distribution of thunderstorms. The distribution of winds around Seth was also asymmetrical. Winds to tropical storm force extended out 205 miles (335 km) in the southern half of Tropical Cyclone Seth. Winds to tropical storm force extended out 90 miles (150 km) in the northern half of Seth’s circulation.

Tropical Cyclone Seth will move through an environment unfavorable for intensification during the next 24 hours. Seth will move over water where the Sea Surface Temperatures are near 26˚C. However, the upper level trough and upper level ridge will continue to cause strong vertical wind shear. Drier air in the northern half of Seth’s circulation will inhibit the formation of thunderstorms. Tropical Cyclone Seth could make a transition to a subtropical cyclone during the next 24 hours. Seth could maintain its intensity during the transition, but it is likely to weaken during the next few days.

The upper level trough will steer Tropical Cyclone Seth quickly toward the south during the next 12 hours. The upper trough could make a transition to a cutoff low during the next day or so. The center of Seth could move under the cutoff low, which would cause Seth to move more slowly. The cutoff low and Tropical Cyclone Seth could drift west toward Australia during the next several days. On its anticipated track Tropical Cyclone Seth could move slowly toward Australia as a subtropical cyclone.

Tropical Cyclone Seth Spins Northeast of Brisbane

Tropical Cyclone Seth was spinning northeast of Brisbane, Australia on Friday night. At 10:00 p.m. EST on Friday the center of Tropical Cyclone Seth was located at latitude 22.6°S and longitude 157.7°E which put it about 465 miles (745 km) northeast of Brisbane, Australia. Seth was moving toward the southeast at 13 m.p.h. (20 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 992 mb.

Tropical Cyclone Seth strengthened on Friday morning, but then it weakened later in the day. An upper level ridge centered northeast of Australia and an upper level trough over eastern Australia were interacting to produce strong northwesterly winds over the Coral Sea on Friday night. Those winds were blowing toward the top of Seth’s circulation and they were causing moderate vertical wind shear. The wind shear was causing an asymmetric distribution of thunderstorms around Tropical Cyclone Seth. The strongest thunderstorms were occurring in bands southeast of the center of Seth. Bands in the northwestern half of the tropical cyclone consisted primarily of showers and lower clouds. Winds to tropical storm force extended out 155 miles (250 km) in the southern half of Tropical Cyclone Seth. Winds to tropical storm force extended out 100 miles (160 km) in the northern half of the circulation.

Tropical Cyclone Seth will move through an environment unfavorable for intensification during the next 24 hours. Seth will move over water where the Sea Surface Temperatures are near 28˚C. However, the upper level trough over eastern Australia and the upper level ridge over the Coral Sea will continue to produce strong northwesterly winds. Those winds will continue to cause strong vertical wind shear. The wind shear is likely to prevent Tropical Cyclone Seth from intensifying during the next 24 hours. There is a chance that the upper level winds could weaken in 24 hours, which might allow Seth to strengthen at that time.

The upper level trough and ridge will steer Tropical Cyclone Seth toward the south-southeast during the next 24 hours. The upper level trough could evolve into a cutoff low, which could pull Seth back toward the west during the second half of the weekend. On its anticipated track Tropical Cyclone Seth could be east of Brisbane in 36 hours.

Tropical Cyclone Seth Forms over Coral Sea

Tropical Cyclone Seth formed east of Australia over the Coral Sea on Thursday night. At 10:00 p.m. EST on Thursday the center of Tropical Cyclone Seth was located at latitude 19.7°S and longitude 153.7°E which put it about 305 miles (495 km) east-northeast of Mackay, Australia. Seth was moving toward the southeast at 17 m.p.h. (27 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 992 mb.

Tropical Cyclone Seth formed from a tropical low that initially developed northwest of Darwin, Australia almost a week ago. The tropical low made landfall southwest of Darwin and then moved east across northern Australia. The tropical low weakened as it passed over land, but then it regained some organization when it passed over the southern Gulf of Carpentaria. The circulation around the tropical low began to strengthen after it moved over the Coral Sea east of Cairns. The inner end of a rainband wrapped around the southern side of center of circulation on Thursday night and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Seth.

The strongest thunderstorms were occurring in the southern and eastern parts of Tropical Cyclone Seth. Bands in the northern and western parts of Seth’s circulation consisted primarily of showers and lower clouds. Storms near the center of Seth generated upper level divergence that pumped mass away to the southeast of the tropical cyclone. Winds to tropical storm force extended out 160 miles (260 km) to the southeast of the center of Tropical Cyclone Seth.

Tropical Cyclone Seth will move through an environment that is somewhat favorable for intensification during the next 36 hours. Seth will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the southwestern part of an upper level ridge centered northeast of Australia. The ridge will produce southwesterly winds that will blow toward the top of Tropical Cyclone Seth’s circulation. Those winds will cause moderate vertical wind shear. The wind shear will inhibit intensification, but it may not be strong enough to keep Seth from getting stronger. Tropical Cyclone Seth could intensify during the next 36 hours.

Tropical Cyclone Seth will move around the southwestern part of a high pressure system over the Coral Sea. The high pressure system will steer Seth toward the southeast during the next 36 hours. On its anticipated track Tropical Cyclone Seth will move over the Coral Sea parallel to the east coast of Australia. Seth could be located northeast of Brisbane in 36 hours. The steering currents could weaken during the weekend and Tropical Cyclone Seth could stall.

Tropical Low Drops Rain on Darwin

A Tropical Low dropped rain on the area around Darwin, Australia on Saturday. At 1:00 p.m. EST on Saturday the center of the Tropical Low was located at latitude 12.9°S and longitude 130.4°E which put it about 45 miles (75 km) southwest of Darwin, Australia. The Tropical Low was moving toward the east-southeast at 6 m.p.h. (10 km/h). The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were wind gusts to 50 m.p.h. (65 km/h). The minimum surface pressure was 988 mb.

A Tropical Low that developed over the Timor Sea late last week made landfall on the coast of Australia near Dundee Beach on Saturday. Bands revolving around the center of the Tropical Low brought gusty winds and locally heavy rain to the area around Darwin. A weather station at the airport in Darwin reported a sustained wind speed of 27 m.p.h. (44 km/h) and a wind gust of 38 m.p.h. (61 km/h). The weather stationed measured 2.2 inches (56 mm) of rain. A station in Batchelor measured 5.7 inches (144.8 mm) of rain and a station in Dum In Mirrie measured 7.1 inches (180.6 mm) of rain. Flood Watches were in effect for portions of northern Australia.

The Tropical Low is forecast to move toward the east-southeast during the next several days. On its anticipated track the Tropical Low will move across northern Australia. It will continue to drop heavy rain over the northern part of the Northern Territory. The Tropical Low could move over the Gulf of Carpentaria in 48 hours. If the Tropical Low moves back over water, there is a chance it could strengthen to a tropical cyclone.

Tropical Low Forms over Timor Sea

A Tropical Low formed over the Timor Sea north of Darwin, Australia on Thursday night. At 10:00 p.m. EST on Thursday the center of the Tropical Low was located at latitude 9.8°S and longitude 129.6°E which put it about 200 miles (325 km) north-northwest of Darwin, Australia. The Tropical Low was moving toward the south-southwest at 7 m.p.h. (11 km/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 1007 mb.

A Watch was issued for the portion of the coast from Point Stuart, Northern Territory to Kalumburu, Western Australia including Darwin and the Tiwi Islands.

A low pressure system over the Timor Sea north of Darwin, Australia exhibited more organization on Thursday night and the Australian Bureau of Meteorology designated the system as a Tropical Low. More thunderstorms formed in bands revolving around the center of the Tropical Low. The strongest rainbands were occurring in the western half of the circulation. Storms near the center began to generate upper level divergence that pumped mass away from the Tropical Low.

The Tropical Low will move through an environment favorable for intensification during the next 24 hours. It will will move over water where the Sea Surface Temperatures are near 30˚C. The Tropical Low will move under the southwestern part of an upper level ridge centered north of Australia. The ridge will produce northwesterly winds that will blow toward the top of the Tropical Low’s circulation. Those winds will cause some vertical wind shear, but the shear will not be strong enough to prevent intensification. The Tropical Low is likely to strengthen during the next 24 hours.

The Tropical Low will move around the western side of a high pressure system centered north of Australia during the next 24 hours. The high pressure system will steer the Tropical Low toward the south during the next day or so. On its anticipated track the Tropical Low could approach Bathurst Island and Melville Island within 24 hours. The Tropical Low could bring gusty winds and locally heavy rain to a portion of the coast of the Northern Territory during the weekend.

Tropical Cyclone Niran Develops over Coral Sea

Tropical Cyclone Niran developed over the Coral Sea east of Queensland on Monday. At 10:00 p.m. EST on Monday the center of Tropical Cyclone Niran was located at latitude 15.4°S and longitude 147.0°E which put it about 175 miles (285 km) northeast of Cairns, Australia. Niran was moving toward the northeast 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 991 mb.

The circulation around a low pressure system over the Coral Sea east of Queensland strengthened on Monday and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Niran. The circulation around Niran was organizing gradually. The strongest thunderstorms were occurring in bands in the western half of Tropical Cyclone Niran. Bands in the eastern half of the tropical cyclone consisted primarily of showers and lower clouds. Storms near the center of circulation began to generate upper level divergence which pumped mass away to the west of Niran. Winds to tropical storm force extended out 90 miles from the center of circulation.

Tropical Cyclone Niran will move through an environment favorable for intensification during the next 48 hours. Niran will move over water where the Sea Surface Temperatures will be near 29°C. It will move under the northern part of an upper level ridge over the Coral Sea. The ridge will produce easterly winds which will blow toward the top of Tropical Cyclone Niran. Those winds will cause some vertical wind shear and they are contributing to the current asymmetrical distribution of thunderstorms. The wind shear will slow the rate of intensification. Tropical Cyclone Niran will intensify and it could strengthen into the equivalent of a hurricane/typhoon within 48 hours.

Tropical Cyclone Niran will be in an area where the steering winds are weak during the next day or so. Niran could make a slow loop over the Coral Sea east of Queensland during the next 24 hours. A high pressure system over the tropical South Pacific Ocean will strengthen during the week. The high will start to steer Tropical Cyclone Niran toward the southeast on Wednesday. On its anticipated track Niran could approach New Caledonia during the weekend.

Tropical Cyclone Mangga Develops Northwest of Cocos Islands

Tropical Cyclone Mangga developed over the South Indian Ocean northwest of the Cocos Islands on Thursday.  At 11:00 a.m. EDT on Thursday the center of Tropical Cyclone Mangaa was located at latitude 9.4°S and longitude 93.1°E which put it about 320 miles (515 km) northwest of Cocos Island.  Mangga was moving toward the south-southeast at 7 m.p.h. (12 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 996 mb.

The Australian Bureau of Meteorology issued a Warning for the Cocos Islands.

Tropical Cyclone Mangga developed within a trough of low pressure that extended from southwest of Indonesia to western Australia.  The trough had persisted for several days and a center of low pressure gradually formed northwest of the Cocos Islands during the past 24 hours.  The Australian Bureau of Meteorology designated the system as Tropical Cyclone Mangga on Thursday.

The circulation around Tropical Cyclone Mangga was still in the process of organizing.  The strongest thunderstorms were in a band on the western side of the circulation.  Bands on the eastern side of the circulation consisted primarily of showers and lower clouds.  More thunderstorms began to develop near the center of circulation on Thursday.  Storms developing near the center started to generate upper level divergence which was pumping mass away to the west of the tropical cyclone.  Winds to tropical storm force extended out 150 miles (240 km) from the center of Mangga.

Tropical Cyclone Mangga will move through an environment somewhat favorable for intensification during the next 24 to 36 hours.  Mannga will move over water where the Sea Surface temperature is near 27°C.  It will move under the northwestern part of an upper level ridge centered over Indonesia.  The ridge will produce easterly winds which will blow toward the top of the circulation.  Those winds will produce moderate vertical wind shear.  The wind shear may be the reason why the bands on the eastern side of Tropical Cyclone Mangga are weaker.  The shear will also inhibit intensification, but it will probably not be strong enough to prevent Manga from strengthening during the next 24 hours.

Tropical Cyclone Mangga will move around the western end of a high pressure system centered north of Australia.  The high will steer Mangga toward the southeast during the next few days.  On its anticipated track Tropical Cyclone Mangga will pass near the Cocos Islands in about 24 hours.  Manga will bring gusty winds and locally heavy rain to those islands.

Tropical Cyclone Blake Makes Another Landfall in Western Australia

Tropical Cyclone Blake made another landfall on the coast of Western Australia on Tuesday.  At 4:00 p.m. EST on Tuesday the center of Tropical Cyclone Blake was located at latitude 20.1°S and longitude 120.5°E which put it about 20 miles (35 km) south-southwest of Wallal Downs, Australia.  Blake was moving toward the southwest at 6 m.p.h. (10 km/h).  The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were wind gusts to 55 m.p.h. (90 km/h).  The minimum surface pressure was 990 mb.

The center of Tropical Cyclone Blake moved across the coast of Western Australia just to the west of Wallal Downs on Tuesday.  Blake was beginning to weaken, but winds to tropical storm force were still occurring in the northwestern part of the circulation that was still over water.  A weather station at Bedout Island which is just off the coast of Western Australia was reporting a sustained wind speed of 43 m.p.h. (69 km/h) and wind gusts to 50 m.p.h. (82 km/h).  A weather station in Mandora, Australia had already received 2.69 inches (64.4 mm) of rain from the rainbands in eastern side of the tropical cyclone.

Tropical Cyclone Blake will move around the western end of a high pressure system over Australia.  Blake will move more toward the south when it reaches the western end of the high.  On its anticipated track the center of Tropical Cyclone Blake could be near Marble Bar in about 12 hours.  Blake could approach Newman in about 24 hours.  Tropical Cyclone Blake will weaken as it moves farther inland.  Blake could drop locally heavy rain over parts of Western Australia and the potential for flash floods exists.

Elsewhere, a Tropical Low was slowly organizing over the Arafura Sea north of Australia.  At 1:00 p.m. EST on Tuesday the center of the Tropical Low was located at latitude 11.2°S and longitude 137.7°E which put it about 70 miles (115 km) north-northeast of Nhulunbuy, Australia.  The Tropical Low was moving toward the west at 3 m.p.h. (5 km/h).  The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were wind gusts to 40 m.p.h. (65 km/h).  The minimum surface pressure was 1003 mb.  The Tropical Low is forecast to move westward and to strengthen.  A Watch has been issued for the portions of the coast from Cape Don to Point Stuart and from Goulburn Island to Cape Shield.

Tropical Cyclone Blake Brings Wind and Rain to Western Australia

Tropical Cyclone Blake brought wind and rain to portions of Western Australia on Monday.  At 10:00 p.m. EST on Monday the center of Tropical Cyclone Blake was located at latitude 18.7°S and longitude 121.5°E which put it about 60 miles (95 km) southwest of Broome, Australia.  Blake was moving toward the south-southwest 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 989 mb.

The center of Tropical Cyclone Blake made landfall on the coast of Western Australia north of Broome earlier on Monday.  The center moved back out over water slightly north of Broome and then the center passed just to the west of that city.  A weather station in Broome measured sustained winds of 30 m.p.h. (50 km/h) and a wind gust to 50 m.p.h. (82 km/h).  5.83 inches (148 mm) of rain fell over Broome.  A rainband in the northeastern periphery of the circulation dropped rain over the area around the Kimberly Plateau during much of Monday.

Tropical Cyclone Blake weakened while the center was over land, but it appears to be strengthening again now that the center is back over water.  More thunderstorms developed near the center of circulation during the past few hours.  Those storms started to generated upper level divergence again.  Bands farther away from the center consisted primarily of showers and lower clouds.  Winds to tropical storm force extended out about 100 miles (160 km) from the center of circulation mainly in portions of circulation over water.

Tropical Cyclone Blake will move through an environment favorable for intensification during the next 12 hours.  Blake will move over water where the Sea Surface Temperature is 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 Blake could strengthen during the next 12 hours.

Tropical Cyclone Blake will move around the western end of a high pressure system over Australia.  The high will steer Blake toward the south-southwest during the next 24 to 36 hours.  On its anticipated track Tropical Cyclone Blake could make another landfall on the coast of Western Australia near Wallal Downs.  A Warning is in effect for the portion of the coast from Bidyadanga to De Grey.  Blake will bring gusty winds and rain to that portion of the coast.

Elsewhere, a new Tropical Low developed over the Arafura Sea north of Australia.  At 8:00 p.m. EST on Monday the center of the Tropical Low was located at latitude 10.7°S and longitude 137.7°E which put it about 120 miles (195 km) north-northeast of Nhulunbuy, Australia.  The Tropical Low was moving toward the east at 6 m.p.h. (9 km/h).  The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were wind gusts to 40 m.p.h. (65 km/h).  The minimum surface pressure was 1003 mb.  The Tropical Low is forecast to move back toward the west and to strengthen.  A Watch has been issued for the portion of the Australian coast from Cape Shield to Cape Don including Goulburn Island.  On its anticipated track the center of the Tropical Low could pass near Cape Wessel in about 24 hours.