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Tropical Cyclone Vernon Forms Southwest of Cocos Island

Tropical Cyclone Vernon formed over the South Indian Ocean southwest of Cocos Island on Thursday night. At 10:00 p.m. EST on Thursday the center of Tropical Cyclone Vernon was located at latitude 13.5°S and longitude 95.3°E which put it about 140 miles (220 km) southwest of Cocos Island. Vernon was moving toward the west-southwest 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 995 mb.

The circulation around a low pressure system over the South Indian Ocean southwest of Cocos Island strengthened on Thursday night and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Vernon. More thunderstorms formed near the center of Tropical Cyclone Vernon. Storms near the center of circulation generated upper level divergence that pumped mass away from the tropical cyclone. Bands of showers and thunderstorms were revolving around the core of Vernon’s circulation. Winds to tropical storm force extended out 60 miles (95 km) from the center of circulation.

Tropical Cyclone Vernon will move through an environment favorable for intensification during the next 24 hours. Vernon will move over water where the Sea Surface Temperatures are near 29˚C. It will move under the axis of an upper level ridge that is west of Australia. The upper level winds are weak near the axis of the ridge and there will be little vertical wind shear. Tropical Cyclone Vernon will intensify during the next 24 hours and it could strengthen to the equivalent of a hurricane/typhoon during the weekend.

Tropical Cyclone Vernon will move north of a high pressure system over the South Indian Ocean. The high pressure system will steer Vernon toward the west during the next few days. On its anticipated track Tropical Cyclone Vernon will move farther away from Cocos Island.

Tropical Cyclone Hilda Develops on Coast of Western Australia

A Tropical Low near the coast of Western Australia strengthened and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Hilda. At 10:00 a.m. EST on Wednesday the center of Tropical Cyclone Hilda was located at latitude 18.0°S and longitude 122.1°E which put it about 10 miles (15 km) west-southwest of Broome, Australia.  Hilda was moving toward the south-southwest at 8 m.p.h. (12 km/h).  The maximum sustained wind speed was 50 m.p.h. (85 km/h) and there were wind gusts to 85 m.p.h. (140 km/h).  The minimum surface pressure was 985 mb.  Broome Port reported a wind gust to 86 m.p.h. (139 km/h).

The center of the Tropical Low moved off the coast of Western Australia and the core of the circulation strengthened.  Thunderstorms in the core of Tropical Cyclone Hilda generated strong upper level divergence which pumped mass away from the center of circulation.  The removal of mass allowed the surface pressure to decrease quickly and the wind speeds increased.  The strongest winds were occurring over water near the center of circulation.  Additional bands of showers and thunderstorms were revolving around the core of the circulation.  Hilda is a small tropical cyclone.  Winds to tropical storm force only extend out about 35 miles (55 km) from the center of circulation.

Tropical Cyclone Hilda will be moving through an environment that will support further intensification during the next 12 hours.  The Sea Surface Temperature of the water near the coast of Western Australia is near 30°C.  Tropical Cyclone Hilda is underneath an upper level ridge and the upper level winds are weak.  There is little vertical wind shear.  The proximity to land is the only factor preventing rapid intensification of Tropical Cyclone Hilda.  Almost half of the circulation is over land and the increased friction is reducing the wind speeds in that part of Tropical Cyclone Hilda.

Tropical Cyclone Hilda is moving around the western end of a subtropical ridge, which is steering the tropical cyclone toward the south-southwest.  A general motion toward the south-southwest is expected to continue for another 12 to 24 hours.  On its anticipated track the center of Tropical Cyclone Hilda could pass near Bidyadanga during the next 6 to 12 hours.  Hilda will bring gusty winds capable of producing localized minor wind damage.  A Warning is in effect for the portion of the coast from Beagle Bay to Pardoo Roadhouse.  The core of Tropical Cyclone Hilda will drop locally heavy rain near the coast of Western Australia and flash flooding is possible.

Tropical Low Develops Near Coast of Western Australia

A distinct low level center of circulation developed in an area of thunderstorms near the coast of Western Australia on Tuesday and the Australian Bureau of Meteorology classified the system as a Tropical Low.  At 10:00 p.m. EST on Tuesday the center of the Tropical Low as located at latitude 17.2°N and 122.3°E which put it just inland east of Coulomb Point and about 55 miles (85 km) north of Broome, Australia.  The Tropical Low was moving toward the southwest at 8 m.p.h. (13 km/h).  The maximum sustained wind speed was 35 m.p.h. (55 km/h) and there were gusts to 45 m.p.h. (75 km/h).  The minimum surface pressure was 998 mb.

Although the center of circulation was over land, the circulation of the Tropical Low became much better organized on Tuesday.  There was a well defined center of circulation and weather radar images indicated an eyelike feature at the center of the Tropical Low.  Several bands of showers and thunderstorms wrapped around the center of circulation.  Storms in the core of the Tropical Low were generating well developed upper level divergence which was pumping mass away in all directions.

The Tropical Low will move through an environment favorable for intensification during the next 24 to 36 hours.  The Sea Surface Temperature of the water off the coast of Western Australia is near 30°C.  The Tropical Low is underneath an upper level ridge and the upper level winds are not very strong.  There is little vertical wind shear.  The only factor inhibiting intensification is the fact that the center is still inland over Western Australia.  If the center moves over water as is forecast, the Tropical Low will intensify and it could intensify rapidly.

The Tropical Low is moving around the western end of a mid-level ridge which is steering it toward the southwest.  The ridge is forecast to steer the Tropical Low toward the southwest for another 12 to 24 hours.  When the Tropical Low reaches the western end of the ridge, it will move more toward the south.  On its anticipated track the center of the Tropical Low will move off the coast of Western Australia and over water during the next 6 to 12 hours.  The center of the Tropical Low is expected to pass west of Broome.  The Tropical Low could approach the coast of Western Australia between Bidyadanga and Wallal Downs in about 36 hours.

The Tropical Low will drop heavy rain along the coast of Western Australia during the next 48 hours.  It will also bring gusty winds and a Warning has been issued for the portion of the coast from Cape Leveque to De Grey.

Tropical Cyclone Organizing Over Southwest Indian Ocean

A tropical cyclone organized north of La Reunion and east of Madagascar over the Southwest Indian Ocean on Friday.  At 1:00 p.m. EST on Friday the center of the tropical cyclone was located at latitude 14.5°N and longitude 56.1°E, which put it about 435 miles (700 km) north of La Reunion.  The tropical cyclone was moving toward the south at 5 m.p.h. (8 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 1002 mb.

An area of showers and thunderstorms persisted north of La Reunion for much of the past week.  Curved bands of showers and thunderstorms began to develop on Friday and the circulation took on more of a circular shape.  Thunderstorms near the center of the circulation began to generate upper level divergence which was pumping out mass and the surface pressure started to decrease.  There is a distinct center in the low level circulation and the tropical cyclone would be the equivalent of a tropical depression if it were over the Atlantic or Pacific Oceans.

The environment surrounding the tropical cyclone is favorable for further intensification.  The tropical cyclone is over water where the Sea Surface temperature is around 28.5°C.  So, there is plenty of energy in the upper ocean.  The upper level winds over the tropical cyclone are light and there is little vertical wind shear.  The absence of vertical wind shear is allowing the upper level divergence to pump out mass in all directions.  The tropical cyclone is expected to strengthen during the next 24 hours and it could intensify quickly if the inner core continues to develop.

The winds at the steering level are weak, which is why the system did not move much during the past few days.  Weak northerly winds could push the tropical cyclone slowly toward the south toward Mauritius and La Reunion.  The tropical cyclone could be near those islands in about three or four days.

Tropical Cyclone Organizing Northwest of Australia

A tropical cyclone is organizing northwest of Australia and the Australian Bureau of Meteorology has officially designated it as a tropical low.  At 10:00 p.m. EST on Wednesday the center of the tropical low was located at latitude 15.4°S and longitude 117.7°E which put it about 345 miles (555 km) north of Port Hedland, Australia.  The tropical low was moving toward the south at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 1001 mb.

The circulation around the tropical low is still in an organizational phase and there is no well defined center of circulation.  Scattered spiral bands of thunderstorms are beginning to form and rotate around a broad center of circulation.  Much of the convection is still relatively shallow and taller thunderstorms are just beginning to form.  Some upper level divergence is beginning to occur to the west of the tropical low.

The environment is favorable for intensification.  The tropical low is over water where the Sea Surface Temperature is near 30°C.  An upper level ridge east of the tropical low is generating some easterly winds over the system, but the vertical wind shear is probably not strong enough to prevent intensification.  After more thunderstorms consolidate around a center of circulation and the organization of the tropical low improves, intensification is likely.

A subtropical ridge east of the tropical low is steering the low toward the south and that general motion is expected to continue for the next several days.  On its anticipated track, the tropical low could make landfall somewhere along the coast of Western Australia between Broome and Mardie on Friday.  The highest probability is currently for a landfall near Port Hedland in about 48 hours.  However, uncertainty exists about the future track because the tropical low is still organizing and a well defined center of circulation does not yet exist.

The tropical low is likely to bring strong winds, locally heavy rain and some storm surge to parts of the coast of Western Australia.