new thread for the new developing system.
TROPICAL CYCLONE INFORMATION BULLETIN
Issued at 3:04 pm WST on Tuesday 24 January 2012
BY THE BUREAU OF METEOROLOGY
TROPICAL CYCLONE WARNING CENTRE
PerthA Tropical Low was located at 2 pm WST near 16.0S 112.6E,
that is 680 km north northwest of Exmouth, moving west at 25 kilometres per
hour.
The low may develop into a tropical cyclone during Wednesday as it moves
towards the west or west southwest. Late on Wednesday or on Thursday the system
may take a more southerly track, bringing it closer to the coast.
Gales are not expected in coastal communities on Wednesday or Thursday, however
there is a possibility that coastal communities near the North West Cape,
including Coral Bay, Exmouth and Onslow, will experience gales on Friday.
Rainfall is likely to increase later in the week in coastal parts of the
Pilbara and on the west coast north of Cape Cuvier.
The next Information Bulletin will be issued at 9 pm WST.
and the tech bulletin -
REMARKS:
System assigned T1.0 at 00Z. Yesterday the cloud system centre could not be
defined in an area less than 2.5 degrees. Overnight convection consolidated near
a developing low level circulation centre. ASCAT and VIS imagery show the LLCC
gradually becoming better defined but low level cloud lines are still poorly
organised.
The system has shown further improvement over the last 6 hours and FT is set at
1.5. Shear is generally low south of 15S and models indicate the system will
experience low shear for the next 72 hours. Combined with SSTs over 30 degrees
the system is expected to develop faster than the standard Dvorak rate and may
reach TC intensity by early tomorrow.
The subsequent track may develop on the rate of intensification with some models
indicating the system will take a southerly or south southeasterly track on
Thursday. On Friday the system is likely to be near 20S. SSTs decrease south of
20S and the system is likely to be slow moving which may cause upwelling and
reduce SSTs. As shear remains light, weakening in the longer term is more likely
to be due to low oceanic heat content.
The monsoon trough is expected to remain strong over the next few days,
resulting in strong northwesterly flow extending well to the east of the system
centre and bringing moderate swell and increased rainfall to coastal areas of
the Pilbara and Kimberley.