|
||||||||||||||||||||||||||||||||||||||||||
Tropical Cyclones Affecting Inland Pilbara townsFlooding | Notable TCs | TC Olivia It may be thought that tropical cyclones only affect coastal areas of the state. While cyclones certainly weaken as they move inland, the stronger ones remain capable of causing damaging winds for some time before being downgraded below cyclone intensity. A cyclone at category five intensity near the coast capable of causing wind gusts to 300 km/h can still be rated at category three or higher producing wind gusts of over 170 km/h hundreds of kilometres inland. It is quite rare that an inland town experiences the maximum winds of a severe cyclone. The risk of damaging winds also decreases with distance from the coast. Pannawonica, for example, being just 75 kilometres from the coast is much more likely to experience damaging winds than Paraburdoo and Newman which are 300 and 350 kilometres inland respectively. Additionally cyclones weaken at a faster rate when moving over hills and mountains such as the Hamersley and Chichester Ranges compared to those moving over flatter terrain over the eastern Pilbara and Great Sandy Desert areas. Typically the greatest impact of most cyclones inland is flooding from heavy rainfall. This can cause damage to buildings and fences near watercourses in addition to road and rail networks. The added cost of transport delays can cause significant economic costs particularly to the mining industry. Some of the more remote communities may be isolated for extended periods before water levels fall and roads and bridges repaired. While most towns and communities are located away from flood-susceptible areas, some such as Nullagine often experience flooding in the town. The tracks of cyclones affecting inland Pilbara are similar to those affecting coastal communities of Port Hedland, Karratha/Dampier, and Onslow. These cyclones typically form over warm ocean waters to the north of the state and intensify before crossing the coast, by which stage they are moving in a general southerly track. The further south cyclones move the more likely they will take a southeasterly track across inland parts of the State. Tropical cyclone Olivia is one example of a severe cyclone that crosses the Pilbara coast and, while weakening, can still cause damage to inland parts. See the Interactive Tropical Cyclone Plotting web page to access tracks of historical tropical cyclones. FloodingHeavy rainfall and associated flooding is the main impact for most cyclone events in the inland Pilbara. The highest rainfall is usually found along or just east of the track for most systems. The flood potential of a system is not directly related to cyclone intensity but is associated with its track, speed, areal extent and saturation of catchments from prior rainfall. Indeed rainfall totals in excess of 100 mm are common with tropical lows that move over land. In February 1997 a slow moving low moved over the west Kimberley, Pilbara and Gascoyne causing rainfall in excess of 400 mm in parts and one of the highest ever floods along the Ashburton River. Cyclone Joan in December 1975 caused over 400 mm of rain near its track, the highest fall being 591 mm at Marandoo. Flooding is enhanced when multiple tropical lows occur within a few weeks of each other. During January and February 1961 rainfall totals exceeded 200 mm during two tropical cyclones. At Wittenoom it was described as the worst flood in memory as water levels rose to 23 m in sections of the Gorge. In both events Wittenoom was isolated. In 1980 cyclones Amy, Dean and Enid moved over the eastern Pilbara causing total rainfall to exceed 600 mm in some areas.
Some Notable Cyclones Impacting inland Pilbara towns
|
Home | About Us | Learn about Meteorology | Contacts | Search | Help | Feedback Weather and Warnings | Climate | Hydrology | Numerical Prediction | About Services | Registered Users |
|
© Copyright Commonwealth of Australia 2009, Bureau of Meteorology (ABN 92 637 533 532) Please note the Copyright Notice and Disclaimer statements relating to the use of the information on this site and our site Privacy and Accessibility statements. Users of these web pages are deemed to have read and accepted the conditions described in the Copyright, Disclaimer, and Privacy statements. Please also note the Acknowledgement notice relating to the use of information on this site. No unsolicited commercial email. |