Tag Archives: Brisbane

Tropical Cyclone Gabrielle Intensifies to Equivalent of a Hurricane/Typhoon

Tropical Cyclone Gabrielle intensified to the equivalent of a hurricane/typhoon over the Coral Sea on Thursday morning. At 10:00 a.m. EST on Thursday the center of Tropical Cyclone Gabrielle was located at latitude 20.1°S and longitude 155.6°E which put it about 565 miles (910 km) north-northeast of Brisbane, Australia. Gabrielle was moving toward the southeast at 13 m.p.h. (20 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 971 mb.

Tropical Cyclone Gabrielle intensified over the Coral Sea on Thursday morning. The inner end of a rainband wrapped around the center of Gabrielle’s circulation. A small eye appeared to be forming at the center of circulation. Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Gabrielle. Storms near the core generated upper level divergence that pumped mass away to the southeast of the tropical cyclone. Winds to hurricane/typhoon force extended out 45 miles (75 km) from the center of Gabrielle’s circulation. Winds to tropical storm force extended out 200 miles (320 km) from the center of circulation.

Tropical Cyclone Gabrielle will move through an environment favorable for intensification during the next 24 hours. Gabrielle will move over over water where the Sea Surface Temperatures are near 27˚C. An upper level trough near the east coast of Australia will produce northwesterly winds that will blow toward the top of Gabrielle’s circulation. Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification. Tropical Cyclone Gabrielle is likely to intensify during the next 24 hours.

The upper level trough near the east coast of Australia will steer Tropical Cyclone Gabrielle toward the southeast during the next 48 hours. On its anticipated track Gabrielle will move between Australia and New Caledonia. Bands in the eastern side of Tropical Cyclone Gabrielle could bring gusty winds and locally heavy rain to New Caledonia. Gabrielle will move over cooler water during the weekend and the vertical wind shear will increase. Cooler water and more wind shear will cause Tropical Cyclone Gabrielle to make a transition to an extratropical cyclone. Gabrielle could affect northern New Zealand as a strong extratropical cyclone in a few days.

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 Cyclone Uesi Weakens East of Australia

Tropical Cyclone Uesi weakened east of Australia on Wednesday.  At 1:00 p.m. EST on Wednesday the center of Tropical Cyclone Uesi was located at latitude 25.9°S and longitude 161.7°E which put it about 500 miles (805 km) east-northeast of Brisbane, Australia.  Uesi was moving toward the south-southwest at 13 m.p.h. (20 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 977 mb.

Tropical Cyclone Uesi weakened steadily on Wednesday as it moved into a more unfavorable environment.  An upper level low over eastern Australia and an upper level ridge over the South Pacific Ocean interacted to produce strong northerly winds which blew across the top of Uesi.  Those winds caused strong vertical wind shear and they pushed the upper part of the circulation to the south of the lower level circulation.  Thunderstorms were only occurring in bands south of the center of Tropical Cyclone Uesi.  Bands in other parts of the tropical cyclone consisted primarily of showers and lower clouds.

Tropical Cyclone Uesi will continue to weaken as it moves into an even more unfavorable environment.  The upper low over eastern Australia and the upper ridge over the South Pacific will steer Uesi toward the south.  Tropical Cyclone Uesi will move over colder water.  The trough and the ridge will also continue to cause strong vertical wind shear.  The combined effects of colder water and strong wind shear will cause Tropical Cyclone Uesi to weaken during the next several days.

Wutip Intensifies Into a Typhoon Southeast of Guam

Former Tropical Storm Wutip intensified into a typhoon southeast of Guam on Wednesday.  At 10:00 p.m. EST on Wednesday the center of Typhoon Wutip was located at latitude 6.5°N and longitude 150.0°E which put it about 640 miles (1035 km) southeast of Guam.  Wutip was moving toward the west-northwest at 13 m.p.h. (20 km/h).  The maximum sustained wind speed was 75 m.p.h. (120 km/h) and there were wind gusts to 90 m.p.h. (145 km/h).  The minimum surface pressure was 979 mb.

Tropical Storm Watches have been issued for Guam, Rota, Tinian and Saipan.  A Typhoon Warning is in effect for Satawal and Puluwat.  A Tropical Storm Warning and a Typhoon Watch are in effect for Ulul and Faraulep.

Typhoon Wutip continued to exhibit better organization on Wednesday.  A cluster of thunderstorms remained near the center of circulation.  A band of storms wrapped around the southern side of the center, which could indicate the start of the formation of an eyewall.  Other bands of showers and thunderstorms were revolving around the core of Typhoon Wutip.  Storms near the core were generating upper level divergence which was pumping mass away from the typhoon.  Winds to typhoon force extended out about 35 miles (55 km) from the center of circulation.  Winds to tropical storm force extended out about 160 miles (260 km) from the center.

Typhoon Wutip will move through an environment favorable for intensification for several more days.  Wutip will move over water where the Sea Surface Temperature is near 30°C.  Typhoon Wutip will move around the western end of an upper level ridge.  The ridge will produce easterly winds which will blow toward the top of the circulation.  Those winds will create some vertical wind shear, but the wind shear will not be great enough to prevent intensification.  Typhoon Wutip will continue to intensify and it could strengthen into the equivalent of a major hurricane within 36 hours.

The ridge will steer Typhoon Wutip in a northwesterly direction during the next 48 hours.  Wutip is likely to turn more toward the north-northwest when it approaches the western end of the ridge.  On its anticipated track Typhoon Wutip could be south of Guam in 36 to 48 hours.  Wutip could be the equivalent of a major hurricane at that time.

Elsewhere, Tropical Cyclone Oma continued to spin over the Coral Sea between New Caledonia and Australia.  At 10:00 p.m. EST on Wednesday the center of Tropical Cyclone Oma was located at latitude 22.7°S and longitude159.8°E which put it about 560 miles (905 km) northeast of Brisbane, Australia.  Oma was moving toward the southwest at 6 m.p.h. (10 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 981 mb.

Tropical Cyclone 13P Develops Over the Coral Sea

Tropical Cyclone 13P developed over the Coral Sea northwest of New Caledonia on Monday.  At 5:00 p.m. EDT on Monday the center of Tropical Cyclone 13P was located at latitude 17.2°S and longitude 159.7°E which put it about 550 miles (885 km) northwest of Noumea, New Caledonia.  It was moving toward the south at 11 m.p.h. (17 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.

A distinct low level center of circulation developed within an area of showers and thunderstorms over the Coral Sea on Monday.  The strongest rainband extended from northeast of the center, south of the the center and then west of the center.  Additional rainbands were forming in other part of the circulation.  Storms near the center of circulation were beginning to generate upper level divergence which was pumping mass away to the south of the tropical cyclone.

Tropical Cyclone 13P will move through an environment favorable for intensification on Tuesday.  It will move over water where the Sea Surface Temperature is near 29°C.  An upper level trough near the east coast of Australia is producing northerly winds which are blowing toward the top of the circulation.  The core of Tropical Cyclone 13P is east of the strongest upper level winds, but the winds are causing moderate vertical wind shear.  Despite the vertical shear, the tropical cyclone is forecast to intensify during the next 24 hours.

Tropical Cyclone 13P is moving around the western end of a subtropical ridge which is steering it toward the south.  There is some variability in the guidance from the numerical models about the future strength of the ridge.  Some models do not strengthen the ridge much and those model predict that Tropical Cyclone 13P will move almost straight southward.  Other models increase the strength of the ridge and steer the tropical cyclone more toward the south-southwest.  A general motion toward the south or south-southwest seems most likely during the next 24 to 36 hours.  On its anticipated track the core of Tropical Cyclone 13P would pass west of New Caledonia, but it could move closer to the east coast of Australia.