Category Archives: Australian Region

Tropical Cyclone Stan Intensifying As It Nears Western Australia

Tropical Cyclone Stan intensified on Friday as it moved closer to the coast of Western Australia.  At 4:00 p.m. EDT on Friday the center of Tropical Cyclone Stan was located near latitude 18.6°N and longitude 118.9°E which put it about 120 miles (195 km) north of Port Hedland, Australia.  Stan was moving toward the east-southeast at 6 m.p.h. (10 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 982 mb.

The circulation of Tropical Cyclone Stan is much more well organized than it was 24 hours ago.  A primary rainband has wrapped about two thirds of the way around a distinct center of circulation.  There are many more thunderstorms in the core of the circulation and the structure is more symmetrical.  Thunderstorms in the core of Tropical Cyclone Stan are beginning to generate more upper level divergence which is pumping out mass in all directions.

The environment surrounding Tropical Cyclone Stan is now more favorable for intensification.  Stan has moved closer to the center of an upper level ridge that is located east of the tropical cyclone.  As a result, the upper level winds are not as strong and there is less vertical wind shear.  Since Tropical Cyclone Stan is over water where the Sea Surface Temperature is near 29°C, the reduced wind shear allowed it to intensify significantly today.  The environment will be favorable for intensification until Tropical Cyclone Stan makes landfall, and it could become the equivalent of a hurricane within 12 hours.  A period of rapid intensification may be possible.

As Tropical Cyclone Stan moved into an area where the easterly winds in the middle and upper levels were not as strong, it jogged eastward on Friday.  Stan is moving around the western end of a subtropical ridge and it is expected to begin to move more toward the southeast during the next 12 to 24 hours.  The eastward jog today also moved the most likely landfall location to the east.  On its anticipated track Tropical Cyclone Stan is expected to make landfall on the coast of Western Australia in 12 to 24 hours.  The highest probability of landfall is between Broome and Port Hedland near Pardoo Station.

Tropical Cyclone Stan will likely be the equivalent of a hurricane when it makes landfall.  It will be capable of causing wind damage.  Stan will also bring locally heavy rain and a chance for flash floods.  Tropical Cyclone Stan could generate a significant storm surge along the coast near where the center makes landfall.

Tropical Cyclone Stan Heading for Western Australia

A tropical low intensified into Tropical Cyclone Stan on Thursday and it is moving toward Western Australia.  At 10:00 p.m. EST on Thursday the center of Tropical Cyclone Stan was located at latitude 17.7°N and longitude 117.8°E which put it about 190 miles (305 km) north-northwest of Port Hedland, Australia.  Stan was moving toward the south-southeast 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 995 mb.

Tropical Cyclone Stan is not particularly well organized.  A primary rainband curves around the western side of the circulation, but there are not many thunderstorms in the eastern half of the cyclone.  Upper level divergence is occurring to the west of the center, but not to the east of the center.

The environment is marginally favorable for further intensification.  Tropical Cyclone Stan is over water where the Sea Surface Temperature is near 29°C.  However, an upper level ridge east of Stan is generating easterly winds over the top of the tropical cyclone.  The resulting vertical wind shear is inhibiting upper level divergence to the east of Stan.  The tropical cyclone is extracting enough energy from the ocean to intensify but the vertical wind shear is slowing the rate of intensification.  Tropical Cyclone Stan is expected to continue to intensify until it makes landfall.

Tropical Cyclone Stan is moving around the western end of a subtropical ridge which is steering it toward the south-southeast.  The south-southeast motion is expected to continue for another 24 to 36 hours.  On its anticipated track Tropical Cyclone Stan will make landfall on the coast of Western Australia near Port Hedland in about 24 hours.

Tropical Cyclone Stan could be near hurricane intensity when it makes landfall.  It will be capable of causing some wind damage.  Stan could also produce locally heavy rain and flooding.  It will also cause some storm surge near where the center makes landfall.

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.

Tropical Low Forms Over Northern Australia

A distinct center of circulation consolidated within a broader area of low pressure near the northern coast of Australia.  The Australian Bureau of Meteorology designated the system as a Tropical Low.  At 10:00 p.m. EST on Saturday the center of the Tropical Low was located at latitude 14.7°N and longitude 132.7°E which put it about 35 miles (55 km) east-southeast of Katherine, Australia and about 135 miles (220 km) west of Ngukurr.  The Tropical Low was moving toward the east at 3 m.p.h. (5 km).  The maximum sustained wind speed was 30 m.p.h. (45 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 1005 mb.

The atmospheric environment around the Tropical Low would be favorable for the development of a tropical cyclone.  The upper level winds are light and there is not much vertical wind shear.  An upper level anticyclone over the Tropical Low is providing a source of upper level divergence, which is pumping out mass.  However, the Tropical Low is over land which is preventing the development of a tropical cyclone.  As long as the Tropical Low remains over land, it will not develop into a tropical cyclone.  However, if the Tropical Low emerges over the Gulf of Carpentaria in a day or so, it could develop into a tropical cyclone.

A ridge in the middle levels of the atmosphere is steering the tropical low toward the east and that general motion is expected to continue for another 24 to 48 hours.  On its anticipated track the Tropical Low could emerge over the southwestern Gulf of Carpentaria south of Port Roper in 24 to 36 hours.

Although the Tropical Low is moving over land, it will still draw in enough moisture to be capable of producing locally heavy rain.  Flooding may be possible in some locations.

Tropical Cyclone Quang Nearing the Coast of Western Australia

Tropical Cyclone Quang is weakening as it nears the coast of Western Australia.  At 11:00 p.m. EDT on Thursday the center of Tropical Cyclone Quang was located at latitude 20.5°S and longitude 112.1°E which put it about 160 miles northwest of Exmouth and about 210 miles north-northwest of Coral Bay, Australia.  Quang was moving toward the southeast at 14 m.p.h.  The maximum sustained wind speed was 100 m.p.h. and there were gusts to 120 m.p.h.  The minimum surface pressure was 969 mb.

An upper level ridge northeast of Tropical Cyclone Quang is generating strong northwesterly winds and vertical wind shear over it.  The wind shear in combination with cooler Sea Surface Temperatures is causing Quang to weaken.  The wind shear and rate of weakening could increase as the tropical cyclone moves farther south.

The upper level ridge is also steering Quang toward the southeast.  On the projected track Quang would make landfall on the coast of Western Australia between Exmouth and Cape Cuvier in about 12 hours.  The forecast weakening means that Quang is likely to be the equivalent of a tropical storm when it makes landfall.  It will bring some wind and locally heavy rain to parts of Western Australia as it moves inland.

 

Tropical Cyclone Quang Intensified Rapidly Into Equivalent of a Major Hurricane

Tropical Cyclone Quang intensified very rapidly on Wednesday and it reached an intensity equivalent to a major hurricane.  At 10:00 p.m. EDT on Wednesday the center of Tropical Cyclone Quang was located at latitude 17.0°S and longitude 109.2°E which put it about 460 miles northwest of Exmouth and about 610 miles north-northwest of Carnarvon, Australia.  Quang was moving south-southeast at 6 m.p.h.  The maximum sustained wind speed was 130 m.p.h. and there were gusts to 160 m.p.h.  The minimum surface pressure was 940 mb.

As Quang moved across very warm Sea Surface Temperatures (SSTs), the upper level winds eased enough to allow it to intensify very rapidly.  Thunderstorms around the eyewall transported mass upward and generated upper level divergence in all directions, which allowed the surface pressure to decrease quickly.  The decrease in surface pressure generated the rapid increase in wind speed.    Quang is a small tropical cyclone and small tropical cyclones can intensify and weaken more quickly than larger storms.  Quang may have peaked in intensity.  As it moves farther south it will move over cooler SSTs.  Upper level wind speeds will increase along the projected track creating more vertical wind shear.  In addition, it appears that some drier air may be entering the northwestern part of the circulation.  The combination of cooler SSTs, more wind shear and drier air is likely to weaken Quang significantly before it reaches the coast of Western Australia.

Quang is moving around the western end of a subtropical ridge.  As it moves toward higher latitudes, westerly winds are likely to steer it more toward the southeast.  Quang could be approaching the coast of Western Australia between Onslow and Denham in about 48 to 60 hours.

 

Tropical Cyclone Quang Forms Northwest of Australia

After several quiet weeks in the tropics a low level circulation developed in an area of thunderstorms northwest of Australia and the system was classified as Tropical Cyclone Quang (24S) on Tuesday.  At 10:00 p.m. EDT on Tuesday the center of Tropical Cyclone Quang was located at latitude 15.2°S and longitude 109.7°E which put it about 550 miles northwest of Exmouth, Australia.  Quang was moving toward the southwest at 6 m.p.h.  The maximum sustained wind speed was 45 m.p.h. and there were gusts to 65 m.p.h.  The minimum surface pressure was 997 mb.

Tropical Cyclone Quang developed over an area where the Sea Surface Temperatures (SSTs) are near 30°C.  A subtropical ridge to the east of Quang is generating some northeasterly winds over the circulation in the upper levels.  The resulting vertical wind shear is slowing the intensification of the circulation.  However, satellite imagery indicates that Quang is becoming more well organized.  A primary rainband has wrapped most of the way around the center of circulation and an eye may be forming.  Thunderstorms near the center of circulation are increasing the upper level outflow, especially on the southern side of Quang.  Further intensification is likely and Quang could reach hurricane intensity in 24 to 48 hours.  Eventually, when Quang moves farther south, it will move over cooler SSTs.  Vertical wind shear is also likely to increase at the same time, and Quang is likely to weaken as it approaches Western Australia.

Tropical Cyclone Quang is moving around the western end of the subtropical ridge.  As it reaches the western end of the ridge, it is likely to take a more southerly track on Wednesday.  By Thursday westerly winds are forecast to begin to steer Quang to the southeast.  On its projected track, Quang would approach the coast of Western Australia in about three days.  If it weakens as expected, Quang would bring some wind and rain when it moves across Western Australia.

Tropical Cyclone Nathan Weakening Over Northern Australia

The center of Tropical Cyclone Nathan moved inland between Maningrida and Goulburn Island on the northern coast of Australia on Monday.  At 11:00 p.m. EDT on Monday the center of Tropical Cyclone Nathan was located at latitude 12.2°S and longitude 133.5°E which put it about 30 miles east-northeast of Gunbalanya, about 45 miles south of Goulburn Island and about 210 miles east of Darwin, Australia.  Nathan was moving toward the southwest at 8 m.p.h.  The maximum sustained wind speed was 45 m.p.h. and there were gusts to 60 m.p.h.  The minimum surface pressure was 989 mb.

A combination of factors contributed to the weakening of Nathan.  As the center of circulation moved inland, the clockwise flow pulled in drier air from the interior of Australia.  The drier air reduced the number of thunderstorms and decreased the amount of latent energy released in the remaining thunderstorms.  Since the release of latent energy drives the circulation in a tropical cyclone, the wind speed has been decreasing as well.  In addition, northerly winds in the upper levels are creating moderate vertical wind shear over the top of Nathan.  The wind shear is displacing many of the remaining thunderstorms to the south side of the circulation.  The asymmetrical development of thunderstorms has weakened the inner core of the circulation.  As long as the center of circulation remains over land, it is likely to weaken further.

A subtropical ridge to the south of Nathan is expected to steer it in a mainly westerly direction.  The projected track would take the center of Nathan south of Darwin and keep it over land for about another 36 hours.  The circulation could be fairly weak by the time it moves back over water west of Darwin.  The water west of Darwin is warm and so, it is possible that more thunderstorms could develop, if there is a coherent circulation when the system moves back over the water.

Tropical Cyclone Nathan Moving Parallel to the Northern Coast of Australia

The center of Tropical Cyclone Nathan moved across the northeastern portion of Arnhem Land and it has emerged over the Arafura Sea.  At 10:00 p.m. EDT on Sunday the center of Tropical Cyclone Nathan was located at latitude 11.6°S and longitude 134.7°E which put it about 45 miles northeast of Maningrida, about 35 miles north-northwest of Milingimbi and about 280 miles east-northeast of Darwin, Australia.  Nathan was moving toward the west at 5 m.p.h.  The maximum sustained wind speed was 75 m.p.h. and there were gusts to 95 m.p.h.  The minimum surface pressure was 974 mb.

The core of the circulation was relatively intact when the center of Nathan moved back over water and it had an apparent eye on some satellite imagery and radar displays.  The surface temperatures are quite warm in the Arafura Sea and thunderstorms continue to develop around the southern and western sides of the circulation.  Less convection is occurring on the eastern side of Nathan.  It is possible the moving across land and proximity to the coast is allowing some drier air to be entrained into the circulation.  Light westerly winds in the upper levels may also be creating some vertical wind shear.  The intact core and warm water could allow Nathan to intensify somewhat on Monday.

Nathan is being steered toward the west by a subtropical ridge located to its south.  The ridge is expected to continue to steer Nathan in a general westerly direction for another 24 hours.  The projected track would keep the center of circulation over water.  The ridge is expected to weaken a bit in a day or so, which could allow Nathan turn southwestward and make another landfall on the north coast of Australia.  The southwesterly turn could produce a landfall between Maningrida and Croker Island.

Nathan has a relatively small circulation but it is strong enough to cause wind damage and a significant storm surge near where the center makes landfall.  It could also produce locally heavy rainfall and flooding in inland areas.

Tropical Cyclone Nathan Making Landfall in Northern Australia

The center of Tropical Cyclone Nathan is moving inland near Nhulunbuy, Australia.  At 9:00 p.m. EDT on Saturday the center of Tropical Cyclone Nathan was located at latitude 12.6°S and longitude 136.8°E which put it about 25 miles south of Nhulunbuy and about 90 miles north-northeast of Alyangula, Australia.  Nathan was moving toward the northwest at 8 m.p.h.  The maximum wind speed was 75 m.p.h. and there were gusts to 90 m.p.h.  The minimum surface pressure was 979 mb.

The atmospheric environment around Tropical Cyclone Nathan is favorable for intensification.  The upper level winds are light.  The circulation is well organized and there is upper level outflow pumping out mass.  Outflow channels extend to the northwest and southeast.  However, as the center moves over land, the circulation will weaken.  The center is expected to cross the northeastern corner of Arnhem Land and move back over water in a few hours.  The potential for re-intensification will depend on how far away from the coast the center moves.

A subtropical ridge located southwest of Nathan is steering it toward the northwest.  The ridge is expected to continue to steer the tropical cyclone in that direction for another day or so.  After that time Nathan is expected to start moving more toward the west and eventually toward the southwest and make another landfall on the northern coast of Australia,

Nathan is strong enough to cause some wind damage.  It could also produce a significant storm surge near where the center is making landfall.  Locally heavy rainfall could create possible flooding at inland locations.