Cyclone Debbie's Impact on Parks
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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. -
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. -
Indigenous Cultural Heritage Investigation Shute Harbour Marina Development Project Shute Bay, Whitsunday Shire
1 INDIGENOUS CULTURAL HERITAGE INVESTIGATION SHUTE HARBOUR MARINA DEVELOPMENT PROJECT SHUTE BAY, WHITSUNDAY SHIRE MARCH 2008 Prepared by Michele Bird Northern Archaeology Consultancies Pty Ltd PO Box 118 Castletown, Hyde Park QLD 4812 In Conjunction with GIA AND NGARO/GIA ABORIGINAL PARTIES For SHUTE HARBOUR MARINA DEVELOPMENT PTY LTD 292 Water Street Spring Hill QLD 4006 2 TABLE OF CONTENTS 1. INTRODUCTION 1 1.1 Terms of Reference 2 2. PROJECT LOCATION AND DESCRIPTION 4 3. CULTURAL HERITAGE LEGISLATION 7 4. TRADITIONAL OWNER CONSULTATION 15 4.1 Identification of Aboriginal Parties 15 4.2 Consultative Framework 16 5. ENVIRONMENTAL BACKGROUND 19 6. HISTORICAL AND ARCHAEOLOGICAL BACKGROUND 24 6.1 Pre- and Post-Contact History 24 6.2 Cultural Heritage Register and Database Searches 30 6.3 Previous Archaeological Research 32 6.4 Aboriginal Oral History 40 7. CULTURAL FIELDWORK: METHODS AND RESULTS 42 8. ABORIGINAL CULTURAL VALUES OF THE PROJECT AREA 47 8.1 Feedback from Aboriginal Stakeholders 47 8.2 Identified Aboriginal Cultural Values 50 9. ASSESSMENT OF POTENTIAL CULTURAL HERITAGE IMPACTS 53 10. PROJECT RECOMMENDATIONS 57 10.1 Cultural and Environmental Aspects 57 10.2 Cultural Aspirations and Other Issues 61 11. REFERENCES 63 3 FIGURES 1. Cadastral map showing the Shute Harbour Marina project area. 2. Concept master plan showing the Shute Harbour Marina project. PLATES Front Cover: View across Shute Bay from Shute Harbour Road. 1. Gia Aboriginal Party. 2. Ngaro/Gia Aboriginal Party. 3. Coastal fringe between Shute Harbour Road and Shute Bay. 4. Coastal fringe between Shute Harbour Road and Shute Bay. 5. Fringing mangroves along Shute Bay intertidal zone. -
Cyclone Factsheet UPDATE
TROPICAL CYCLONES AND CLIMATE CHANGE: FACTSHEET CLIMATECOUNCIL.ORG.AU TROPICAL CYCLONES AND CLIMATE CHANGE: FACT SHEET KEY POINTS • Climate change is increasing the destructive power of tropical cyclones. o All weather events today, including tropical cyclones, are occurring in an atmosphere that is warmer, wetter, and more energetic than in the past. o It is likely that maximum windspeeds and the amount of rainfall associated with tropical cyclones is increasing. o Climate change may also be affecting many other aspects of tropical cyclone formation and behaviour, including the speed at which they intensify, the speed at which a system moves (known as translation speed), and how much strength is retained after reaching land – all factors that can render them more dangerous. o In addition, rising sea levels mean that the storm surges that accompany tropical cyclones are even more damaging. • While climate change may mean fewer tropical cyclones overall, those that do form can become more intense and costly. In other words, we are likely to see more of the really strong and destructive tropical cyclones. • A La Niña event brings an elevated tropical cyclone risk for Australia, as there are typically more tropical cyclones in the Australian region than during El Niño years. BACKGROUND Tropical cyclones, known as hurricanes in the North Atlantic and Northeast Pacific, typhoons in the Northwest Pacific, and simply as tropical cyclones in the South Pacific and Indian Oceans, are among the most destructive of extreme weather events. Many Pacific Island Countries, including Fiji, Vanuatu, Solomon Islands and Tonga, lie within the South Pacific cyclone basin. -
The Bathurst Bay Hurricane: Media, Memory and Disaster
The Bathurst Bay Hurricane: Media, Memory and Disaster Ian Bruce Townsend Bachelor of Arts (Communications) A thesis submitted for the degree of Doctor of Philosophy at The University of Queensland in 2019 School of Historical and Philosophical Inquiry Abstract In 1899, one of the most powerful cyclones recorded struck the eastern coast of Cape York, Queensland, resulting in 298 known deaths, most of whom were foreign workers of the Thursday Island pearling fleets. Today, Australia’s deadliest cyclone is barely remembered nationally, although there is increasing interest internationally in the cyclone’s world record storm surge by scientists studying past cyclones to assess the risks of future disasters, particularly from a changing climate. The 1899 pearling fleet disaster, attributed by Queensland Government meteorologist Clement Wragge to a cyclone he named Mahina, has not until now been the subject of scholarly historical inquiry. This thesis examines the evidence, as well as the factors that influenced how the cyclone and its disaster have been remembered, reported, and studied. Personal and public archives were searched for references to, and evidence for, the event. A methodology was developed to test the credibility of documents and the evidence they contained, including the data of interest to science. Theories of narrative and memory were applied to those documents to show how and why evidence changed over time. Finally, the best evidence was used to reconstruct aspects of the event, including the fate of several communities, the cyclone’s track, and the elements that contributed to the internationally significant storm tide. The thesis concludes that powerful cultural narratives were responsible for the nation forgetting a disaster in which 96 percent of the victims were considered not to be citizens of the anticipated White Australia. -
In the Aftermath of Cyclone Yasi: AIR Damage Survey Observations
AIRCURRENTS By IN THE AFTERMATH OF CYCLONE YaSI: AIR DAMAGE SURVEY OBSERVATIONS EDITOR’S NOTE: In the days following Yasi’s landfall, AIR’s post-disaster survey team visited areas in Queensland affected by the storm. This article 03.2011 presents their findings. By Dr. Kyle Butler and Dr. Vineet Jain Edited by Virginia Foley INTRODUCTION Severe Cyclone Yasi began as a westward-moving depression In addition to the intense winds, Yasi brought 200-300 off Fiji that rapidly developed into a tropical storm before millimeters of precipitation in a 24 hour period and a storm dawn on January 30, 2011. Hours later, Yasi blew across the surge as high as five meters near Mission Beach. northern islands of Vanuatu, continuing to grow in intensity and size and prompting the evacuation of more than 30,000 residents in Queensland, Australia. By February 2 (local time), the storm had achieved Category 5 status on the Australian cyclone scale (a strong Category 4 on the Saffir-Simpson scale). At its greatest extent, the storm spanned 650 kilometers. By the next day, it became clear that Yasi would spare central Queensland, which had been devastated by heavy flooding in December. But there was little else in the way of good news. Yasi made landfall on the northeast coast of Queensland on February 3 between Innisfail and Cardwell with recorded gusts of 185 km/h. Satellite-derived sustained Figure 1. Satellite-derived 10-minute sustained wind speeds in knots just after wind speeds of 200 km/h were estimated near the center Cyclone Yasi made landfall. -
Results for the Mackay-Whitsunday 2018 Report Card
RESULTS FOR THE MACKAY-WHITSUNDAY-ISAAC 2018 REPORT CARD ENVIRONMENTAL INDICATORS Authorship statement The Mackay-Whitsunday-Isaac Healthy Rivers to Reef Healthy Partnership (Partnership) Results for Environmental Indicators for the Mackay-Whitsunday-Isaac 2018 Report Card technical report was compiled by the Partnership’s Technical Officers, Alysha Lee and Jessica Gillespie. Substantial input was received from the Regional Report Cards Technical Working Group (TWG) members. Some content was also drawn from technical reports from earlier Mackay-Whitsunday report cards. Regional Report Cards Technical Working Group members Diane Tarte (TWG Chair July 2018 onwards) Adam Fletcher Paulina Kaniewska Nicola Stokes Richard Hunt Reinier Mann Tegan Whitehead Angus Thompson Emma Maxwell Nathan Waltham Alysha Lee Alex Carter Jessica Gillespie Michael Rasheed Carl Mitchell Glynis Orr Nyssa Henry Luke Galea Michael Holmes Eddie Jebreen David Moffatt Ken Rhode Andrew Moss Travis Sydes Lynne Powell Lyndon Llewellyn Judith Wake Nadine Marshall Donna Audas Paul Groves Chris Dench Stephen Lewis Michael Nash Chris Manning Melinda Louden Adam Folkers Acknowledgements The authors also thank Phillip Trendell, Bernie Cockayne, Bronwyn Houlden, Carol Honchin, Len McKenzie, Jamie Corfield and Matt Curnock for their technical input into various aspects of document development and/or their review of the document. Members of the Reef Independent Science Panel are also gratefully acknowledged for their advice and review of this document. Suggested citation Mackay-Whitsunday-Isaac Healthy Rivers to Reef Partnership (2019). Results for the Mackay- Whitsunday-Isaac 2018 Report Card: Environmental Indicators, Technical Report. Mackay- Whitsunday-Isaac Healthy Rivers to Reef Partnership, Mackay. This technical report was finalised and released online in November 2019. -
189930408.Pdf
© The University of Queensland and James Cook University, 2018 Published by the Great Barrier Reef Marine Park Authority ISSN: 2208-4134 Marine Monitoring Program: Annual report for inshore pesticide monitoring 2016-2017 is licensed for use under a Creative Commons By Attribution 4.0 International licence with the exception of the Coat of Arms of the Commonwealth of Australia, the logos of the Great Barrier Reef Marine Park Authority, The University of Queensland and James Cook University, any other material protected by a trademark, content supplied by third parties and any photographs. For licence conditions see: http://creativecommons.org/licences/by/4.0 This publication should be cited as: Grant, S., Thompson, K., Paxman, C., Elisei, G., Gallen C., Tracey, D., Kaserzon, S., Jiang, H., Samanipour, S. and Mueller, J. 2018, Marine Monitoring Program: Annual report for inshore pesticide monitoring 2016-2017. Report for the Great Barrier Reef Marine Park Authority, Great Barrier Reef Marine Park Authority, Townsville, 128 pp. A catalogue record for this publication is available from the National Library of Australia Front cover image: Turbid river plume emerging from the Russell-Mulgrave river mouth following several days of heavy rainfall in February 2015 © Dieter Tracey, 2015 DISCLAIMER While reasonable efforts have been made to ensure that the contents of this document are factually correct, UQ and JCU do not make any representation or give any warranty regarding the accuracy, completeness, currency or suitability for any particular purpose of the information or statements contained in this document. To the extent permitted by law UQ and JCU shall not be liable for any loss, damage, cost or expense that may be occasioned directly or indirectly through the use of or reliance on the contents of this document. -
Escape Succumb to Nature
ESCAPE SUCCUMB TO NATURE RELAX & RECHARGE Worlds away from the unrelenting hum of While we love our coastline, every now and the everyday, the expanse of our botanic then we trade our salty air and surf to binge backyard is a welcome surprise and one well on fresh mountain air and waterfalls. worth slowing down for. If the urge to reset befalls you, hit the road and head west along ribbon-like roads SPRINGBROOK NATIONAL PARK winding through a canvas of verdant hills Nestled in the untouched World Heritage dotted with vineyards and roadside produce area, Purling Brook Falls is a must for any stalls. The yin to the coastal yang, the Gold visit. You’ll hear it before you see it with fresh NATURAL BRIDGE Coast Hinterland is a definite sojourn for water falling over 100 meters to the rock pool the well-informed traveller and a revelation below. Let the night birds be your soundtrack to those lucky enough to stumble across it. at 850m above sea-level at Mouses House Just a 40-minute drive inland from Surfers Rainforest Retreat. If a cosy cedar chalet isn’t Paradise and Broadbeach sees the scenery enough to pull on the heart strings, the sound change from surf to serenity; where the air of a mountain stream cascading beside is crisper and the stars shine brighter. Stand the chalet and hard wood crackling in the hundreds of meters above sea level and drink fireplace just might. in the infinite views that stretch across an ancient realm. MOUNT TAMBORINE Can’t make it to the hinterland? Salute the Mount Tamborine boasts 12 walking trails sun with a beach side yoga session, work up each no longer than around 3km. -
Gold Coast Hinterland Great Walk Map Please Use Only As a Guide to Plan Your Great Walk
Gold Coast Hinterland Great Walk map Please use only as a guide to plan your Great Walk To Nerang To Nerang To Beechmont Pine To Mudgeeraba To Canungra Numinbah Legend Springbrook National park and Creek Road Gold Coast QPWS tenure NP Springbrook Road Conservation park City of Gold Coast Council Little conservation area, reserves Nerang and refuges Kamarun Dam Seqwater lookout Priems Numinbah Correctional Centre Crossing Restricted access area d Woonoongoora Waterways a Numinbah o walkers’ camp R Waterfall Correctional k r Centre Ner Built up area a Apple Tree Park P (No l ang–Murwill Sealed road a a Road n Access) io Unsealed road t a N Great Walk n Egg o umbah Walking track t Binna Burr Rock g (Kurraragin) State border in Lamington Warringa m Binna Burra ingbrook Road a Pool Springbrook Horse riding trail L National Turtle Rock Springbrook Mountain Lodge Road Spr Walkers’ camp Park (Yowgurrabah) NP National Kooloobano ks Rd Park Camping area ic lookout Springbrook Milleribah Camping area—car access Carr lookout Purling Brook Falls Accommodation Gorooburra lookout Gwongorella Dar Information picnic area The Settlement Yangahla Road Bochow Park camping area lington lookout Kiosk Green Gwongoorool (pool) Lookout (fenced) Mountains Kweebani Cave Range section Koolanbilba Gauriemabah Drinking water Range lookout Hardys Water collection point— yrebird Ballunjui L lookout treat all water before drinking Yerralahla (pool) Falls Tracks do Gooroolba Falls No water Tullawallal not connect Repeater Canyon No swimming Darraboola Binna Burra lookout -
Lessons Learned from Cyclones in Northern Australia
Lessons Learned from Cyclones in Northern Australia SEPTEMBER 2013 RIRDC Publication No. 13/071 Lessons Learned from Cyclones in Northern Australia By Rhonda Sorensen September 2013 RIRDC Publication No. 13/071 RIRDC Project No. PRJ-008498 © 2013 Rural Industries Research and Development Corporation. All rights reserved. ISBN 978-1-74254-564-6 ISSN 1440-6845 Lessons Learned from Cyclones in Northern Australia Publication No. 13/071 Project No. PRJ-008498 The information contained in this publication is intended for general use to assist public knowledge and discussion and to help improve the development of sustainable regions. You must not rely on any information contained in this publication without taking specialist advice relevant to your particular circumstances. While reasonable care has been taken in preparing this publication to ensure that information is true and correct, the Commonwealth of Australia gives no assurance as to the accuracy of any information in this publication. The Commonwealth of Australia, the Rural Industries Research and Development Corporation (RIRDC), the authors or contributors expressly disclaim, to the maximum extent permitted by law, all responsibility and liability to any person, arising directly or indirectly from any act or omission, or for any consequences of any such act or omission, made in reliance on the contents of this publication, whether or not caused by any negligence on the part of the Commonwealth of Australia, RIRDC, the authors or contributors. The Commonwealth of Australia does not necessarily endorse the views in this publication. This publication is copyright. Apart from any use as permitted under the Copyright Act 1968, all other rights are reserved. -
Circulation and Suspended Sediment Transport in a Coral
Marine Pollution Bulletin Archimer 2010, Volume 61, Issues 7-12, Pages 269-296 http://archimer.ifremer.fr http://dx.doi.org/10.1016/j.marpolbul.2010.06.023 © 2010 Elsevier Ltd All rights reserved. ailable on the publisher Web site Circulation and suspended sediment transport in a coral reef lagoon: The south-west lagoon of New Caledonia S. Ouillona,b,*, P. Douilletc, J.P. Lefebvrec, R. Le Gendred, A. Jouone, P. Bonnetone, J.M. Fernandezd, C. Chevillond, O. Magandf, J. Lefèvred, P. Le Hirg, R. Laganierh, F. Dumasg, P. Marchesielloa,d, A. Bel Madanii, S. Andréfouëtd, J.Y. Panchéd, R. Fichezc a Université de Toulouse, UPS (OMP-PCA), LEGOS, 14 av. Edouard Belin, Toulouse F-31400, France b IRD, LEGOS, 14 av. Edouard Belin, Toulouse F-31400, France c IRD, UAM, Dpt Hidrobio – DIV de Ciencas Bio y Salud, AV. San Rafael Atlixco 186 – Col. Vicentina 09340, Mexico DF, Mexico blisher-authenticated version is av d IRD Nouméa, BP A5, 98848 Nouméa cedex, New Caledonia e Université de Bordeaux, CNRS, UMR 5805, Bordeaux F-33000, France f LGGE, CNRS, Université Joseph Fourier, 54 rue Molière, Saint Martin d’Hères cedex F-38402, France g DYNECO/PHYSED, Ifremer, BP 70, Plouzané F-29280, France h Université Paris Diderot – Paris 7, Case 7001, 75205 Paris cedex 13, France i IRD, IMARPE/CIMOBP, Instituto del Mar del Perù, Esquina de Gamarra y General Valle S/N Chucuito, Callao, Peru *: Corresponding author : S. Ouillon, Tel.: +33 5 61 33 29 02, email address : [email protected] Abstract: The south-west lagoon of New Caledonia is a wide semi-open coral reef lagoon bounded by an intertidal barrier reef and bisected by numerous deep inlets.