Tag Archives: Gulf of Carpentaria

Tropical Cyclone 16P Forms Over Gulf of Carpentaria

After a quiet period of several weeks in the tropics Tropical Cyclone 16P formed over the Gulf of Carpentaria on Tuesday.  At 11:00 p.m. EDT on Tuesday the center of Tropical Cyclone 16P was located at latitude 16.4°S and longitude 140.3°E which put it about 75 miles (120 km) east-northeast of Mornington Island and about 115 miles (185 km) southwest of Kowanyama, Australia.  Tropical Cyclone 16P was moving toward the east-southeast at 12 m.p.h. (18 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.

An upper level ridge persisted over the Gulf of Carpentaria during the past few days.  The upper level ridge generated upper level divergence which enhanced rising motion and supported the development of thunderstorms.  Eventually, the upper level divergence pumped out enough mass to allow the surface pressure to decrease and the thunderstorms began to consolidate around a low level center.  The system developed enough organization on Tuesday to be classified as a tropical cyclone.

The organization of Tropical Cyclone 16P improved on Tuesday.  Spiral bands of thunderstorms wrapped around a low level center.  Strong thunderstorms near the center of circulation generated upper level divergence, especially to the east of the tropical cyclone.

The environment is favorable for intensification as long as the center of circulation remains over water.  The Sea Surface Temperatures are near 31°C in the southern Gulf of Carpentaria.  An upper level ridge to the east of the tropical cyclone is generating some vertical wind shear, but the ridge is also enhancing upper level divergence.  The primary inhibiting factor is the proximity of the center of circulation to land.  Tropical Cyclone 16P could intensify further during the next 12 hours before it makes landfall.

The upper level ridge is steering Tropical Cyclone 16P toward the southeast coast of the Gulf of Carpentaria.  On its anticipated track Tropical cyclone 16P is expected to make landfall in Queensland near the mouth of the Gilbert River in about 12 hours.  The potential track after landfall is much more uncertain.  Some guidance suggests that the tropical cyclone could move across the Cape York peninsula toward the Coral Sea.  Other guidance suggests that the tropical cyclone could turn back toward the northwest and move back out into the Gulf of Carpentaria.

Although Tropical Cyclone 16P is likely to cause minor wind damage, it could produce locally heavy rainfall and flooding when it moves over northeastern Queensland.

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 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.

Severe Tropical Cyclone Nathan Making Landfall in Queensland

The center of Severe Tropical Cyclone Nathan is very near the coast of Queensland and it is about to make landfall between Cape Flattery and Cape Melville.  At 11:00 a.m. EDT on Thursday the center of Nathan was located at latitude 14.7°S and longitude 145.6°E which put it about 20 miles northeast of Cape Flattery and about 50 miles north-northeast of Cooktown, Australia.  Nathan was moving toward the west at 11 m.p.h.  The maximum sustained wind speed was 105 m.p.h. and there were gusts to 140 m.p.h.  The minimum surface pressure was 953 mb.

A subtropical ridge is steering Nathan westward and this motion is expected to continue.  The center of Nathan will make landfall soon between Cape Flattery and Cape Melville.  It is capable of producing wind damage and a significant storm surge near where the center crosses the coast.  Nathan could also produce locally heavy rainfall and flooding in some locations.  It is possible that the circulation could emerge intact over the Gulf of Carpentaria.  In that case Nathan could re-intensify somewhat and possibly pose a risk to the western side of the Gulf.