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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. -
6. Annual Review and Significant Events
6. Annual Review and Significant Events January-April: wet in the tropics and WA, very hot in central to eastern Australia For northern Australia, the tropical wet season (October 2005 – April 2006) was the fifth wettest on record, with an average of 674 mm falling over the period. The monsoon trough was somewhat late in arriving over the Top End (mid-January as opposed to the average of late December), but once it had become established, widespread heavy rain featured for the next four months, except over the NT and Queensland in February. One particularly noteworthy event occurred towards the end of January when an intense low (central pressure near 990 hPa) on the monsoon trough, drifted slowly westward across the central NT generating large quantities of rain. A two-day deluge of 482 mm fell at Supplejack in the Tanami Desert (NT), resulting in major flooding over the Victoria River catchment. A large part of the central NT had its wettest January on record. Widespread areas of above average rain in WA were mainly due to the passages of several decaying tropical cyclones, and to a lesser extent southward incursions of tropical moisture interacting with mid-latitude systems. Severe tropical cyclone Clare crossed the Pilbara coast on 9t h January and then moved on a southerly track across the western fringes of WA as a rain depression. Significant flooding occurred around Lake Grace where 226 mm of rain fell in a 24-hour period from 12 t h to 13 t h January. Tropical cyclone Emma crossed the Pilbara coast on 28 th February and moved on a southerly track; very heavy rain fell in the headwaters of the Murchison River on 1s t March causing this river’s highest flood on record. -
Summary of 2005/6 Australian-Region Tropical Storm Season and Verification of Authors’ Seasonal Forecasts
Summary of 2005/6 Australian-Region Tropical Storm Season and Verification of Authors’ Seasonal Forecasts Issued: 15th May 2006 by Professor Mark Saunders and Dr Adam Lea Benfield Hazard Research Centre, UCL (University College London), UK. Summary ¢¡¤£¦¥¨§¨§¨© £¨¨ £¨£¨ ¨£"!$#%¨&('(¨)¨'*+%,¨-'(.¨&/%¨01¨.%'23'(%546¨7+£¨ ¤£¨ ¨£8!$#%¨&('(¨9&*¨¤7:¨&(&*'( ;¨.%'23'*%54=<3 ¢¡¤'*>.¨¤%¨%?@'(%¡9%¡£A:B¨#A-,£C3'(¨#/!$#%¨&('(¨ %,¨-¤'*.¨&%¨0D£¨¨E@¡'(.¡F¨&(&3¡¤¨7F)£&(,@£¨ ¨£"¨.%'23'(%54¨<G ¢¡£" ¢HIJ%£,.'(&(£K-,¨)¤¨)'(&*'(%54 :B¨,£.¨%¦:L¨M%¡¤£¥¨§¨§¨© N £¨¨O¡,@£7P£Q¨.£&*&(£%$R¤'*&(&(ST-,£7'(.%'( :,¨0VUW 4X¥¨§¨§¨©+%¡¨% !K#%¨&('*¨ )¨'( ¨7 &(¨7¤:¨&*&('( Y¨.%'Z3'(%54Y[¨#&(7 )£\.&*¨£\%Y£¨ ¨£<X ¢¡¤£] ¢H¤I 7¤£%£0^'*¤'*%'*.¦:B¨,£.¨%A¡,@£76 ¨¨¨76R¤'*&(&_:B¨;)¤¨'(`¨.%'23'(%54a¨76:B¨¦&*¨¤7:¨&(&*'( M%,¨-'(.¨& %¨0b¤#0^)£_:,¨0bUc 4d¥¨§¨§¨©¨< egf3hejilk m3n(opqsr=t k iu1vKn(wyxOze{r|vK}$ok ~3wk it nZ¨u1m¨ilhwh~¨tNw@pFwy¨u[upiOk¨st(f3h¨¨¨ ^"3wyt(ilpq(n*p~3 ilh,¨n(k ~;t*ilk m3n(opqwtNk iyuwhpwk ~9p~3¦p8gpq(n(¨pt n(k ~k¨t(f3hniwhpwk ~3pqm¨ilk 3p3n(q*n(wyt n(oAp~3¦¨ht hiunZ~3n(wyt n*o k ilhopwyt w>k i?t(f3n(w>potNn 3nZt*¨¤egf3hwh$k ilhopwyt w{@hilh$n*wwy3hKuk ~¨t(f3qZ95ilk ut*f3h$ t(f¦Wp9¨¨¨ "tNk"t*f3h t(f@hohu[3hi8¨¨¨ p~3nZ~3oqZ3¨hKwhm3pilptNhTm¨ilh¨n(otNn(k ~3wsk i{~¨¨u3hilwsk¨¤t*ilk m3n(opqwyt k iuw~¨¨u[3hilw k¨¢wh¤hilh t(ilk m3n(opq¡oC3oq(k ~3hw"p~3¢t(f3h A£E¤¥z5@oo¨u3q(ptNh^£E3oq*k ~3h¦¤¡~3hi 3}snZ~3¨h§3egf3h[q*pt(tNhiKn(w ¨n ¤h~dk i¨t*f3h/"f3k¨q(h/"3wyt(ilpq*n(p~35ilh ¨n(k ~3 Features of the 2005/6 Australian-Region Season • The 2005/6 Australian-region tropical storm season featured 11 storms of which 7 made severe tropical cyclone strength (U.S. -
Local Disaster Management Plan (LDMP) Has Been Prepared to Ensure There Is a Consistant Approach to Diaster Management in the Livingstone Shire
F Document Set ID: 8554803 Version: 1, Version Date: 17/09/2020 FOREWORD Foreword by the Chair, Andrew Ireland of the Livingstone Shire Local Disaster Management Group. The Livingstone Shire Local Disaster Management Plan (LDMP) has been prepared to ensure there is a consistant approach to Diaster Management in the Livingstone Shire. This plan is an important tool for managing potential disasters and is a demonstrated commitment towards enhancing the safety of the Livingstone Shire community. The plan identifies potential hazards and risks in the area, identifies steps to mitigate these risks and includes strategies to enact should a hazard impact and cause a disaster. This plan has been developed to be consistant with the Disaster Management Standards and Guidelines and importantly to intergrate into the Queensland Disaster Management Arrangements (QDMA). The primary focus is to help reduce the potential adverse effect of an event by conducting activities before, during or after to help reduce loss of human life, illness or injury to humans, property loss or damage, or damage to the environment. I am confident the LDMP provides a comprehensive framework for our community, and all residents and vistors to our region can feel secure that all agenices involved in the Livingstone Shire LDMP are dedicated and capable with a shared responsibility in disaster management. On behalf of the Livingstone Shire Local Disaster Management Group, I would like to thank you for taking the time to read this important plan. Livingstone Shire Council Mayor Andrew Ireland Chair, Local Disaster Management Group Dated: 26 August 2020 Page 2 of 175 ECM # xxxxxx Version 6 Document Set ID: 8554803 Version: 1, Version Date: 17/09/2020 ENDORSEMENT This Local Disaster Management Plan (LDMP) has been prepared by the Livingstone Shire Local Disaster Management Group for the Livingstone Shire Council as required under section 57 of the Disaster Management Act 2003 (the Act). -
The Cyclone As Trope of Apocalypse and Place in Queensland Literature
ResearchOnline@JCU This file is part of the following work: Spicer, Chrystopher J. (2018) The cyclone written into our place: the cyclone as trope of apocalypse and place in Queensland literature. PhD Thesis, James Cook University. Access to this file is available from: https://doi.org/10.25903/7pjw%2D9y76 Copyright © 2018 Chrystopher J. Spicer. The author has certified to JCU that they have made a reasonable effort to gain permission and acknowledge the owners of any third party copyright material included in this document. If you believe that this is not the case, please email [email protected] The Cyclone Written Into Our Place The cyclone as trope of apocalypse and place in Queensland literature Thesis submitted by Chrystopher J Spicer M.A. July, 2018 For the degree of Doctor of Philosophy College of Arts, Society and Education James Cook University ii Acknowledgements of the Contribution of Others I would like to thank a number of people for their help and encouragement during this research project. Firstly, I would like to thank my wife Marcella whose constant belief that I could accomplish this project, while she was learning to live with her own personal trauma at the same time, encouraged me to persevere with this thesis project when the tide of my own faith would ebb. I could not have come this far without her faith in me and her determination to journey with me on this path. I would also like to thank my supervisors, Professors Stephen Torre and Richard Landsdown, for their valuable support, constructive criticism and suggestions during the course of our work together. -
Polarimetric Radar Observations of the Persistently Asymmetric Structure of Tropical Cyclone Ingrid
616 MONTHLY WEATHER REVIEW VOLUME 136 Polarimetric Radar Observations of the Persistently Asymmetric Structure of Tropical Cyclone Ingrid PETER T. MAY,J.D.KEPERT, AND T. D. KEENAN Bureau of Meteorology Research Centre, Melbourne, Australia (Manuscript received 3 November 2006, in final form 3 May 2007) ABSTRACT Tropical Cyclone Ingrid had a distinctly asymmetric reflectivity structure with an offshore maximum as it passed parallel to and over an extended coastline near a polarimetric weather radar located near Darwin, northern Australia. For the first time in a tropical cyclone, polarimetric weather radar microphysical analyses are used to identify extensive graupel and rain–hail mixtures in the eyewall. The overall micro- physical structure was similar to that seen in some other asymmetric storms that have been sampled by research aircraft. Both environmental shear and the land–sea interface contributed significantly to the asymmetry, but their relative contributions were not determined. The storm also underwent very rapid changes in tangential wind speed as it moved over a narrow region of open ocean between a peninsula and the Tiwi Islands. The time scale for changes of 10 m sϪ1 was of the order of 1 h. There were also two distinct types of rainbands observed—large-scale principal bands with embedded deep convection and small-scale bands located within 50 km of the eyewall with shallow convective cells. 1. Introduction larimetric radar (Keenan et al. 1998). Ingrid was a long- lived storm that reached Australian category 5 intensity The structure and intensity of tropical cyclones (TCs) twice—initially before it crossed the North Queensland around landfall are a major topic of research because of coast, and then again as it reintensified over the Gulf of the potential impact on human populations and prop- Carpentaria, where the eye structure was quite sym- erty. -
Severe Tropical Cyclone Marcia: an Examination of Information and Warnings Broadcasted to Inform Mitigation and Community Preparedness
Severe Tropical Cyclone Marcia: an examination of information and warnings broadcasted to inform mitigation and community preparedness Kevin Ronan CQ University, Bushfire and Naturual Hazards CRC Bruce Gunn Bureau of Meteorology Deanne Bird Risk Frontiers, University of Iceland AFAC16 CONFERENCE PAPER Severe Tropical Cyclone Marcia: An examination of information and warnings broadcasted to inform mitigation and community preparedness Deanne Bird1, 2, Shannon Panchuk3, Kevin Ronan4, Linda Anderson-Berry3, Christine Hanley5, Shelby Canterford6, Ian Mannix7, Bruce Gunn3 1 Risk Frontiers, Macquarie University, Melbourne 2 Institute of Life and Environmental Sciences, University of Iceland, Reykjavik 3 Hazards Warnings and Forecasts Division, Bureau of Meteorology 4 Clinical Psychology, School of Human, Health and Social Sciences, Central Queensland University, Rockhampton 5 Population Research Lab, School of Human, Health and Social Sciences, Central Queensland University, Rockhampton 6 Community Safety Branch, Community Safety and Earth Monitoring Division, Geoscience Australia 7 ABC Radio Emergency Broadcasting Abstract The event of severe Tropical Cyclone Marcia is particularly interesting for two reasons. Firstly, it is the most intense cyclone to make landfall so far south on the east coast of Australia during the satellite era. Secondly, it rapidly intensified from a Category 2 to a Category 5 system in 36 hours. While coastal residents of the region, including Yeppoon and Byfield are accustomed to receiving cyclone forecasts and warnings, many were taken by surprise by the intensity of Marcia and the fact that it wasn’t another ‘near miss’. Being situated further inland, the residents of Rockhampton were even more surprised. Given the rapid escalation in intensity of this event, the effective transmission of warnings and how these were used to inform mitigation and community preparedness was particularly important. -
Developing Impact-Based Thresholds for Coastal Inundation from Tide Gauge Observations
CSIRO PUBLISHING Journal of Southern Hemisphere Earth Systems Science, 2019, 69, 252–272 https://doi.org/10.1071/ES19024 Developing impact-based thresholds for coastal inundation from tide gauge observations Ben S. HagueA,B,C, Bradley F. MurphyA, David A. JonesA and Andy J. TaylorA ABureau of Meteorology, GPO Box 1289, Melbourne, Vic. 3001, Australia. BSchool of Earth, Atmosphere and Environment, Monash University, Clayton, Vic., Australia. CCorresponding author. Email: [email protected] Abstract. This study presents the first assessment of the observed frequency of the impacts of high sea levels at locations along Australia’s northern coastline. We used a new methodology to systematically define impact-based thresholds for coastal tide gauges, utilising reports of coastal inundation from diverse sources. This method permitted a holistic consideration of impact-producing relative sea-level extremes without attributing physical causes. Impact-based thresh- olds may also provide a basis for the development of meaningful coastal flood warnings, forecasts and monitoring in the future. These services will become increasingly important as sea-level rise continues.The frequency of high sea-level events leading to coastal flooding increased at all 21 locations where impact-based thresholds were defined. Although we did not undertake a formal attribution, this increase was consistent with the well-documented rise in global sea levels. Notably, tide gauges from the south coast of Queensland showed that frequent coastal inundation was already occurring. At Brisbane and the Sunshine Coast, impact-based thresholds were being exceeded on average 21.6 and 24.3 h per year respectively. In the case of Brisbane, the number of hours of inundation annually has increased fourfold since 1977. -
Annual Report 2 0 0 8 - 0 9 FIRE and EMERGENCY SERVICES AUTHORITY of WESTERN AUSTRALIA
Government of Western Australia Government of Western Australia Fire & Emergency Services Authority Fire & Emergency Services Authority Fire and Emergency Services Authority of Western Australia Annual Report 2 0 0 8 - 0 9 FIRE AND EMERGENCY SERVICES AUTHORITY OF WESTERN AUSTRALIA CONTACT DETAILS In line with State Government requirements, this annual report is published in electronic format. In order to minimise download times and reduce printing, we have developed the report into chapters. We encourage people to use recycled paper and to print double sided if they print a copy of the report or sections of it. Hard copies of this report have been digitally printed on chlorine free paper made from plantation grown timber. The paper manufacturer is certified to ISO 14001, the international standard for environmental management. Limited hard copies are available from the Manager Corporate Planning and Reporting. CONTACT DETAILS POSTAL ADDRESS STREET ADDRESS ELECTRONIC GPO Box P1174 FESA House Telephone: [08] 9323 9300 Perth WA 6844 480 Hay Street Facsimile: [08] 9323 9470 Perth WA 6000 Email: [email protected] Website: www.fesa.wa.gov.au ISSN 1442-8288 2 FIRE AND EMERGENCY SERVICES AUTHORITY OF WESTERN AUSTRALIA CONTENTS CONTACT DETAILS 2 OUR ROLES AND RESPONSIBILITIES 14 Organisational Chart AS AT 30 JUNE 2009 15 CONTENTS 3 THE FESA BOARD 16 Corporate EXECUTIVE 16 GLOSSARY 6 ADMINISTERED Legislation 17 STATEMENT OF LEGISLATIVE COMPLIANCE 7 OTHER KEY Legislation Impacting ON FESA ACTIVITIES 17 PERFORMANCE MANAGEMENT FRAMEWORK 18 1 OVERVIEW -
Surveys of the Sea Snakes and Sea Turtles on Reefs of the Sahul Shelf
Surveys of the Sea Snakes and Sea Turtles on Reefs of the Sahul Shelf Monitoring Program for the Montara Well Release Timor Sea MONITORING STUDY S6 SEA SNAKES / TURTLES Dr Michael L Guinea School of Environment Faculty of Engineering, Health, Science and the Environment Charles Darwin University Darwin 0909 Northern Territory Draft Final Report 2012-2013 Acknowledgements: Two survey by teams of ten and eleven people respectively housed on one boat and operating out of three tenders for most of the daylight hours for 20 days and covering over 2500 km of ocean can only succeed with enthusiastic members, competent and obliging crew and good organisation. I am indebted to my team members whose names appear in the personnel list. I thank Drs Arne Rasmussen and Kate Sanders who gave their time and shared their knowledge and experiences. I thank the staff at Pearl Sea Coastal Cruises for their organisation and forethought. In particular I thank Alice Ralston who kept us on track and informed. The captains Ben and Jeff and Engineer Josh and the coxswains Riley, Cam, Blade and Brad; the Chef Stephen and hostesses Sunny and Ellen made the trips productive, safe and enjoyable. I thank the Department of Environment and Conservation WA for scientific permits to enter the reserves of Sandy Islet, Scott Reef and Browse Island. I am grateful to the staff at DSEWPaC, for facilitating and providing the permits to survey sea snakes and marine turtles at Ashmore Reef and Cartier Island. Activities were conducted under Animal Ethics Approval A11028 from Charles Darwin University. Olive Seasnake, Aipysurus laevis, on Seringapatam Reef. -
Storm Surge Flood Level Modelling During Cyclones for Port Hedland
6/19/2012 Storm surge flood level modelling during cyclones for Port Hedland Paul Branson David Taylor Insert footer here for cover slide if required. Go to View / Slide Master to adjust or remove Acknowledgements Cardno team Landcorp and Department of Planning who funded the Port Hedland Coastal Vulnerability Study Organizations who contributed data > Port Hedland Port Authority > Department of Transport > Bureau of Meteorology > Department of Water > Town of Port Hedland Engineers Australia - NSW Coastal, Ocean and Port Engineering Panel 1 6/19/2012 Presentation Overview Overview of Port Hedland and context of cyclone risk Definition of the study aims Overview of modelling approaches for cyclones in the context of determining cyclonic design water levels Description of Monte Carlo cyclone track model developed for the Pilbara coast Application of Monte Carlo cyclone track database in a numerical model system to determine design water levels Conclusions and areas for further development Engineers Australia - NSW Coastal, Ocean and Port Engineering Panel Study Site Pilbara coast has complex physical oceanography Large tide range ≈ 7.5m at Port Hedland Port Hedland is the world’s largest bulk export port 200 Mta exported in 2011 Export value in 2011 ≈ $40 billion “The Pilbara coast experiences more cyclones than any other part of Australia” (BoM) Engineers Australia - NSW Coastal, Ocean and Port Engineering Panel 2 6/19/2012 Port Hedland Engineers Australia - NSW Coastal, Ocean and Port Engineering Panel Port Hedland Port Developments -
TROPICAL CYCLONE INFORMATION SERVICE Prepared by Coastal Services Unit, Environmental Sciences Division
TROPICAL CYCLONE INFORMATION SERVICE Prepared by Coastal Services Unit, Environmental Sciences Division Interim report on severe tropical cyclone Ingrid Issued April 2005. • Category 5 cyclone with wind gusts to 320 kilometres per hour near the centre. • Cyclone crossed the Queensland east coast as category 4, 57km south east of Lockhart River. • Estimated peak water level reached 4.0 metres above Australian height Datum (AHD) near Voaden Point (at the southern end of the Lockhart River Aboriginal Reserve). • Extensive environmental damage in vicinity of landfall location. • Cyclone recrossed Queensland west coast into Gulf of Carpentaria 70km south of Weipa. • Storm tide exceeded the Highest Astronomical Tide (HAT) at Cooktown by 0.28m. • National Disaster Relief Funding activated by Queensland Emergency Services Minister. Figure 1 –Track of severe tropical cyclone Ingrid (based on Tropical Cyclone Advices from Bureau of Meteorology). Summary Severe tropical cyclone Ingrid formed in the Coral Sea some time around 14:00 (AEST) on Sunday 6 March 2005 after drifting eastwards across Cape York along a monsoon trough line extending through northern Australia. The first Tropical Cyclone Advice was issued by the Bureau of Meteorology in Brisbane at 15:56 (AEST) on Monday 7 March, at which time Ingrid had deepened into a Category 3 cyclone (on a scale of 1 to 5). The timing of the cyclone corresponded to high spring tides, at or near the Highest Astronomical Tide (HAT), along the east coast of Cape York Peninsula, between Cairns and Thursday Island. Environmental Protection Agency (EPA) storm tide advisers reported to the Department of Emergency Services, State Disaster Coordination Centre at 13:00 (AEST) on Tuesday 8 March.