Cyclone Surge and Community Preparedness
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Known Impacts of Tropical Cyclones, East Coast, 1858 – 2008 by Mr Jeff Callaghan Retired Senior Severe Weather Forecaster, Bureau of Meteorology, Brisbane
ARCHIVE: Known Impacts of Tropical Cyclones, East Coast, 1858 – 2008 By Mr Jeff Callaghan Retired Senior Severe Weather Forecaster, Bureau of Meteorology, Brisbane The date of the cyclone refers to the day of landfall or the day of the major impact if it is not a cyclone making landfall from the Coral Sea. The first number after the date is the Southern Oscillation Index (SOI) for that month followed by the three month running mean of the SOI centred on that month. This is followed by information on the equatorial eastern Pacific sea surface temperatures where: W means a warm episode i.e. sea surface temperature (SST) was above normal; C means a cool episode and Av means average SST Date Impact January 1858 From the Sydney Morning Herald 26/2/1866: an article featuring a cruise inside the Barrier Reef describes an expedition’s stay at Green Island near Cairns. “The wind throughout our stay was principally from the south-east, but in January we had two or three hard blows from the N to NW with rain; one gale uprooted some of the trees and wrung the heads off others. The sea also rose one night very high, nearly covering the island, leaving but a small spot of about twenty feet square free of water.” Middle to late Feb A tropical cyclone (TC) brought damaging winds and seas to region between Rockhampton and 1863 Hervey Bay. Houses unroofed in several centres with many trees blown down. Ketch driven onto rocks near Rockhampton. Severe erosion along shores of Hervey Bay with 10 metres lost to sea along a 32 km stretch of the coast. -
Tropical Cyclone Justin 6 - 24 March 1997
Severe Tropical Cyclone Justin 6 - 24 March 1997 Queensland Tropical Cyclone Warning Centre Bureau of Meteorology A. Summary Severe Tropical Cyclone Justin was a large, long-lived Coral Sea cyclone that crossed the Queensland coast as a category two cyclone northwest of Cairns on 22 March. Two lows that merged in a very active monsoon trough in the Coral Sea developed into Tropical Cyclone Justin on 7 March, reaching maximum intensity on 9 March as a very large system. Justin remained almost stationary and due to cooling SST’s it was downgraded to a tropical low on 13 March. Justin then drifted north over warmer SST’s and re-intensified to tropical cyclone strength on 14 March, reaching a peak intensity on 17 March before weakening and crossing the coast northwest of Cairns on 22 March. The combined effects of heavy rain, large seas and gale to storm force winds caused widespread damage in the region between Cairns and Townsville and the loss of two lives. Earlier in Justin’s lifecycle 30 people were killed in Papua New Guinea and five people died when their yacht was destroyed. Justin was reportedly responsible for an estimated loss of $150 million to the agricultural industry alone. B. Meteorological Description Intensity Analysis The monsoon trough was characterised at 2300 UTC 3 March by a series of MSL low pressure centres below 1000 hPa extending from northeast Australia across the Coral Sea and by 2300 UTC 5 March one centre had developed in the Coral Sea. This low intensified and was named Justin at 1900 UTC 6 March. -
Natural Hazard Resilient Communities and Land Use Planning: the Limitations of Planning Governance in Tropical Australia
Harwood et al., J Geogr Nat Disast 2014, 4:2 Geography & Natural Disasters http://dx.doi.org/10.4172/2167-0587.1000130 ResearchResearch Article Article OpenOpen Access Access Natural Hazard Resilient Communities and Land Use Planning: The Limitations of Planning Governance in Tropical Australia Sharon Harwood1*, Dean Carson2, Ed Wensing3 and Luke Jackson4 1School of Earth and Environmental Sciences, James Cook University, PO Box 6811, Cairns QLD 4870, Australia 2Professor of Rural and Remote Research, Flinders University Rural Clinical School , PO Box 889, Nuriootpa SA 5355, Australia 3National Centre for Indigenous Studies, The Australian National University, Canberra ACT 0200 4School of Earth and Environmental Sciences, James Cook University, PO Box 6811, Cairns QLD, 4870, Australia Abstract This paper examines how two Australian land use planning systems address the creation of hazard resilient communities in tropical areas. The application of substantive hazard knowledge and how this influences the associated procedures within the planning system is examined. The case studies of Darwin the capital of the Northern Territory, and the beachside suburb of Machans Beach within the Cairns Regional Council in far north Queensland are investigated. Both case study locations have experienced tropical cyclones since settlement and despite their hazard prone locations, both have intensified over their 120 year existence. Moreover, it is predicted that cyclones in tropical Australia will decrease in number, but increase in intensity. It would be rational to assume that industry, community and government would actively pursue planning strategies to negate the risks of natural hazards and the corresponding level of vulnerability to a hazard event. However, neither communities nor planning are driven by rational technical decision making processes. -