Onslow Townsite Strategy Background Report
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Severe Tropical Cyclone Glenda 27 - 31 March 2006
Severe Tropical Cyclone Glenda 27 - 31 March 2006 Perth Tropical Cyclone Warning Centre Bureau of Meteorology A. Summary Severe Tropical Cyclone Glenda was a small and intense system that developed very rapidly after moving off the northwest Kimberley coast. Glenda reached category 5 intensity but weakened as it approached the Pilbara coast. Although threatening to cross the coast near the populated Dampier/Karratha region as a Category 4 system close to the time of high tide, Glenda took a more SW course towards Onslow and weakened before finally crossing the coast near Onslow at 2200 WST 30 March as a marginal category 3 system. Very destructive winds were recorded on the coast at Mardie prior to crossing. A total of 206 mm of rain fell at Onslow in the 24 hours to 0900 WST 31 March, representing the sixth wettest day on record for the town. Other centres in the Pilbara also recorded cumulative totals of over 200mm, and although in general Glenda produced less than average rainfall for a landfalling tropical cyclone, rainfall was sufficient to cause problems for transport. The weakening of TC Glenda prior to impact on Onslow, together with the preparedness of the town helped to avert major damage. B. Meteorological Description A weak low developed in the Gulf of Carpentaria during the middle of March and slowly progressed westwards over the Northern Territory. On 24 March it moved temporarily into the Joseph Bonaparte Gulf north of Wyndham, then accelerated across the Kimberley overnight. On 26 March vertical wind shear eased and by about 1200 UTC the system moved off the coast and developed rapidly. -
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. -
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. -
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. -
Western Australia Cyclone Preparedness Guide
Is your property ready? Western Australia Cyclone Preparedness Guide Cyclone Preparedness Guide This Guide has been prepared for WA property owners to provide information on tropical cyclones and their effect on buildings. It provides recommendations about things you can do before the cyclone season to minimise damage to your property from severe winds and rain during a cyclone. The key to preparing your property is regular inspection and continued maintenance. The checklists at the back of this Guide will help you identify any potential problems with your property and ensure that it is kept in good condition. Seek advice from a building professional to address any issues if required. TABLE OF CONTENTS WHAT IS A CYCLONE? ............................................................................................................................... 3 What are the Characteristics of a Cyclone? .............................................................................................. 3 Strong winds and rain ............................................................................................................................ 3 Storm surge and storm tide ................................................................................................................... 3 WHEN AND WHERE DO CYCLONES OCCUR? ......................................................................................... 4 Wind Loading Regions ............................................................................................................................. -
Tropical Cyclone Vance 18 – 24 March 1999
Tropical Cyclone Vance 18 – 24 March 1999 Perth Tropical Cyclone Warning Centre Bureau of Meteorology A. Summary Severe tropical cyclone Vance was one of the strongest cyclones ever to affect mainland Australia. After developing off Darwin on 17-18 March, Vance gradually intensified as it tracked to the west southwest then to the south before crossing the coast near Exmouth on 22 March as a category 5 system. Vance caused severe structural damage to about 10 per cent of buildings in the town though many more experienced less obvious damage due to intrusion of rainwater. A high storm tide caused coastal erosion and damage between Exmouth and Onslow - the estimated peak storm surge west of Onslow was estimated at over 5 m. In addition to damage in the far west Pilbara, water and power supplies throughout the Gascoyne and Goldfields were disrupted and many homesteads sustained wind or flooding damage. The main rail and road links to the eastern states were cut. B. Meteorological Description As the circulation associated with tropical cyclone Elaine moved slowly west, another low within the monsoon trough, which persisted over the north coast of Australia near Darwin for several days, moved into the Timor Sea. The low- level circulation, favourably situated beneath the upper ridge in a region of weak wind shear quickly intensified to cyclone intensity. Vance moved quite steadily west-southwest at first, then towards the southwest during 20-21 March. It intensified steadily and was declared a severe Category 3 cyclone late on 19 March. It was further upgraded to a Category 5 overnight on 20 March. -
When Disaster Strikes … How Communities Cope and Adapt: a Social Capital Perspective
In: Social Capital: Theory, Measurement and Outcomes ISBN: 978-1-62417-822-1 Editor: C. Douglas Johnson © 2013 Nova Science Publishers, Inc. No part of this digital document may be reproduced, stored in a retrieval system or transmitted commercially in any form or by any means. The publisher has taken reasonable care in the preparation of this digital document, but makes no expressed or implied warranty of any kind and assumes no responsibility for any errors or omissions. No liability is assumed for incidental or consequential damages in connection with or arising out of information contained herein. This digital document is sold with the clear understanding that the publisher is not engaged in rendering legal, medical or any other professional services. Chapter 6 WHEN DISASTER STRIKES … HOW COMMUNITIES COPE AND ADAPT: A SOCIAL CAPITAL PERSPECTIVE Lisa J. Wood, Bryan J. Boruff and Helen M. Smith The University of Western Australia, Crawley, WA, Australia ABSTRACT Human beings have had to co-exist with natural disasters and environmental calamity since the dawn of time, and our vulnerability to disasters is potentially increased in the 21st century as we contend with exponential population growth and the volatilities of climate change. When a disaster strikes, a community has no choice but to respond and cope with the event. But why is it that some communities cope and adapt better than others in the face of adversity? Underlying a well-integrated, resilient community is social capital, which can play an important role in enabling communities to work together to recover from a disaster. Social capital also provides a useful framework for assessing a community’s mechanisms for preventing or preparing for disasters before they occur. -
Identification of Climate Change Adaptation Best Practices in the Waste Management Sector ______
Identification of climate change adaptation Best Practices in the Waste Management Sector ___________________________________________ Disaster Waste Management Best practices FINAL REPORT – SEPTEMBER 4TH , 2013 IDENTIFICATION OF CLIMATE CHANGE ADAPTATION BEST PRACTICES IN THE WASTE MANAGEMENT SECTOR PART I REVISIONS VERSION DATE COMMENTS AUTHOR : CHECKED Final document incl. 2 02/09/2013 MLL ThM comments from client 1 19/08/2013 Final document MLL & JW ThM 0 09/08/2013 Draft document part I MLL & JW ThM This document is submitted by Pöyry France – Pöyry France becomes Naldeo Contact : Thierry Martin Manager International Department Naldeo France Phone + 33.4.91.13.97.56 Mobile + 33.6.82.56.92.94 55 rue de la Villette 69425 Lyon cedex 03 - France E-mail : [email protected] Page 2 NALDEO- PÖYRY 2013 IDENTIFICATION OF CLIMATE CHANGE ADAPTATION BEST PRACTICES IN THE WASTE MANAGEMENT SECTOR PART I CONTENTS PART I 1 IDENTIFICATION OF GEOGRAPHIC AREAS AFFECTED BY DESTRUCTIVE EVENTS LINKED TO CLIMATE CHANGE ................................................................................................................ 11 1.1 Effects of climat change .............................................................................................................. 11 1.1.1 Effects of climate change in the Pacific Region .....................................................................................................................11 1.1.2 Affected geographic areas ......................................................................................................................................................13 -
The Age Natural Disaster Posters
The Age Natural Disaster Posters Wild Weather Student Activities Wild Weather 1. Search for an image on the Internet showing damage caused by either cyclone Yasi or cyclone Tracy and insert it in your work. Using this image, complete the Thinking Routine: See—Think— Wonder using the table below. What do you see? What do you think about? What does it make you wonder? 2. World faces growing wild weather threat a. How many people have lost their lives from weather and climate-related events in the last 60 years? b. What is the NatCatService? c. What does the NatCatService show over the past 30 years? d. What is the IDMC? e. Create a line graph to show the number of people forced from their homes because of sudden, natural disasters. f. According to experts why are these disasters getting worse? g. As human impact on the environment grows, what effect will this have on the weather? h. Between 1991 and 2005 which regions of the world were most affected by natural disasters? i. Historically, what has been the worst of Australia’s natural disasters? 3. Go to http://en.wikipedia.org/wiki/File:Global_tropical_cyclone_tracks-edit2.jpg and copy the world map of tropical cyclones into your work. Use the PQE approach to describe the spatial distribution of world tropical cyclones. This is as follows: a. P – describe the general pattern shown on the map. b. Q – use appropriate examples and statistics to quantify the pattern. c. E – identifying any exceptions to the general pattern. 4. Some of the worst Question starts a. -
The Effects of Tropical Cyclone Vance on Exmouth
The effects of tropical cyclone Vance on Exmouth Introduction for a category 5 cyclone in Region D is Cyclone Vance hit Exmouth on the morning by Greg Reardon (Cyclone Testing Station, James Cook University, Townsville), ‘Significant roof and structural damage. of Monday 22nd March, 1999. Exmouth is a Geoff Boughton (Curtin University of Dangerous airborne debris’, that is, the small coastal township some 1250 km north Technology, Perth), David Henderson and tabulated description for a category 4 event of Perth, and almost at the tip of Northwest John Ginger (Cyclone Testing Station, JCU) in Region C. Cape in Western Australia. It is located on Cyclone Vance the west side of the Exmouth Gulf and has a maximum gust speed expressed in both Vance formed in the Timor Sea and was population of just under 3000. It was kilometres per hour (km/h) and metres per established in the early 1960s as the service declared a Category 1 cyclone by the Bureau second (m/s). of Meteorology on 18 March. It headed west centre for the Australian–United States The damage potential listed in Tab le 1 for Communication Station. Now its main then southwest as it intensified rapidly to each category of cyclone has been based on become a Category 5 by 21 March. The fol- industry is tourism. likely performance of buildings in cyclone The township extends over an area of lowing day it was travelling almost due south Region C, as defined in the wind loading as it entered Exmouth Gulf. The Bureau’s about 4 km long by 2 km wide, and is about code. -
Air Quality Impact Assessment.Pdf
Perdaman Urea Project Cardno (WA) Pty Ltd Air Quality Impact Assessment Final | Revision 7 16 March 2020 Air Quality Impact Assessment Perdaman Urea Project Project No: IW213400 Document Title: Air Quality Impact Assessment Document No.: Final Revision: Revision 7 Date: 16 March 2020 Client Name: Cardno (WA) Pty Ltd Project Manager: Lisa Boulden Author: Matthew Pickett, Maria Murphy & Andrew Boyd File Name: Perdaman-AQ-Assessment-Rev7_issued Jacobs Group (Australia) Pty Limited ABN 37 001 024 095 Level 6, 30 Flinders Street Adelaide SA 5000 Australia T +61 8 8113 5400 F +61 8 8113 5440 www.jacobs.com © Copyright 2020 Jacobs Group (Australia) Pty Limited. The concepts and information contained in this document are the property of Jacobs. Use or copying of this document in whole or in part without the written permission of Jacobs constitutes an infringement of copyright. Limitation: This document has been prepared on behalf of, and for the exclusive use of Jacobs’ client, and is subject to, and issued in accordance with, the provisions of the contract between Jacobs and the client. Jacobs accepts no liability or responsibility whatsoever for, or in respect of, any use of, or reliance upon, this document by any third party. Document history and status Revision Date Description By Review Approved A 12 Aug 2019 Preliminary draft M Pickett, M Murphy, A Boyd S Lakmaker, L Boulden L Boulden B 6 Sep 2019 Draft report M Pickett, M Murphy, A Boyd S Lakmaker, L Boulden D Malins 0 26 Sep 2019 Draft report M Pickett, M Murphy, A Boyd L Boulden D Malins