Flood Stories from the Barron River
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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. -
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. -
Cyclone Testing Station
CYCLONE TESTING STATION Investigation of Townsville Tornado, 20 March 2012 Report: TR58 June, 2012 Cyclone Testing Station School of Engineering and Physical Sciences James Cook University Queensland, 4811, Australia www.jcu.edu.au/cts CYCLONE TESTING STATION SCHOOL of ENGINEERING and PHYSICAL SCIENCES JAMES COOK UNIVERSITY TECHNICAL REPORT NO. 58 Investigation of Townsville Tornado, 20 March 2012 By D. Henderson, J. Ginger, P. Kim, and B. Sumant June 2012 © Cyclone Testing Station, James Cook University Bibliography. ISBN 978-0-9808572-6-9 (pbk) Series: Technical report (James Cook University, Cyclone Testing Station); 58 Notes: Bibliography Henderson, D. J. (David James), 1967-. Investigation of Townsville Tornado, 20 March 2012 1. Tornado 2. Buildings – Natural disaster effects 3. Wind damage I. Ginger, John David (1959-) II. Kim, Peter (1982 -) IV. Sumant B. (1983 -) V. James Cook University. Cyclone Testing Station. VI. Title. (Series : Technical Report (James Cook University. Cyclone Testing Station); no. 58). LIMITATIONS OF THE REPORT The Cyclone Testing Station (CTS) has taken all reasonable steps and due care to ensure that the information contained herein is correct at the time of publication. CTS expressly exclude all liability for loss, damage or other consequences that may result from the application of this report. This report may not be published except in full unless publication of an abstract includes a statement directing the reader to the full report. Cyclone Testing Station TR58 Acknowledgements We acknowledge the support and assistance of the Qld Dept of Community Safety, Bureau of Meteorology, and the Mayor and officers of the Townsville City Council during this damage investigation. -
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. -
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. -
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. -
Physical Processes and Biogeochemical Engineering
Keppel Bay: physical processes and biogeochemical engineering L.C. Radke1, P.W. Ford2, I.T. Webster2, I. Atkinson1, K.Oubelkheir2 1 Geoscience Australia, Canberra, ACT 2 CSIRO Land and Water, Canberra, ACT 2006 Keppel Bay: physical processes and biogeochemical functioning Keppel Bay: physical processes and biogeochemical functioning Copyright © 2006: Cooperative Research Centre for Coastal Zone, Estuary and Waterway Management Written by: L.C. Radke P.W. Ford I,T, Webster I. Atkinson K. Oubelkheir Published by the Cooperative Research Centre for Coastal Zone, Estuary and Waterway Management (Coastal CRC) Indooroopilly Sciences Centre 80 Meiers Road Indooroopilly Qld 4068 Australia www.coastal.crc.org.au The text of this publication may be copied and distributed for research and educational purposes with proper acknowledgement. Disclaimer: The information contained in this report was current at the time of publication. While the report was prepared with care by the authors, the Coastal CRC and its partner organisations accept no liability for any matters arising from its contents. National Library of Australia Cataloguing-in-Publication data Keppel Bay: physical processes and biogeochemical functioning QNRM06356 ISBN 1 921017759 (print and online) Keppel Bay: physical processes and biogeochemical functioning Acknowledgements The work described in this report was funded by the CRC for Coastal Zone, Estuary and Waterway Management and relied on extensive inputs of data and ideas from members of other components of the Fitzroy Contaminants subproject (described in CRC Reports 34 to 37). We acknowledge and thank the following other people for their various contributions to this work: Kirrod Broadhurst, Graham Wassell, Paul Ridett and David Munro, the captain and deckhands of the Rum Rambler, managed navigation, shared local knowledge and provided assistance during the sampling. -
KUNINJKU PEOPLE, BUFFALO, and CONSERVATION in ARNHEM LAND: ‘IT’S a CONTRADICTION THAT FRUSTRATES US’ Jon Altman
3 KUNINJKU PEOPLE, BUFFALO, AND CONSERVATION IN ARNHEM LAND: ‘IT’S A CONTRADICTION THAT FRUSTRATES US’ Jon Altman On Tuesday 20 May 2014 I was escorting two philanthropists to rock art galleries at Dukaladjarranj on the edge of the Arnhem Land escarpment. I was there in a corporate capacity, as a direc- tor of the Karrkad-Kanjdji Trust, seeking to raise funds to assist the Djelk and Warddeken Indigenous Protected Areas (IPAs) in their work tackling the conservation challenges of maintain- ing the environmental and cultural values of 20,000 square kilometres of western Arnhem Land. We were flying low in a Robinson R44 helicopter over the Tomkinson River flood plains – Bulkay – wetlands renowned for their biodiversity. The experienced pilot, nicknamed ‘Batman’, flew very low, pointing out to my guests herds of wild buffalo and their highly visible criss-cross tracks etched in the landscape. He remarked over the intercom: ‘This is supposed to be an IPA but those feral buffalo are trashing this country, they should be eliminated, shot out like up at Warddeken’. His remarks were hardly helpful to me, but he had a point that I could not easily challenge mid-air; buffalo damage in an iconic wetland within an IPA looked bad. Later I tried to explain to the guests in a quieter setting that this was precisely why the Djelk Rangers needed the extra philanthropic support that the Karrkad-Kanjdji Trust was seeking to raise. * * * 3093 Unstable Relations.indd 54 5/10/2016 5:40 PM Kuninjku People, Buffalo, and Conservation in Arnhem Land This opening vignette highlights a contradiction that I want to explore from a variety of perspectives in this chapter – abundant populations of environmentally destructive wild buffalo roam widely in an Indigenous Protected Area (IPA) declared for its natural and cultural values of global significance, according to International Union for the Conservation of Nature criteria. -
NASA Finds Tropical Cyclone Ann Over the Great Barrier Reef 14 May 2019
NASA finds tropical cyclone Ann over the great barrier reef 14 May 2019 satellite analyzed cloud top temperatures and found cloud top temperatures of strongest thunderstorms as cold as or colder than minus 63 degrees Fahrenheit (minus 53 degrees Celsius) circling the center and in a large band of thunderstorms north of the center. Cloud top temperatures that cold indicate strong storms that have the capability to create heavy rain. On May 14, NASA's Terra satellite provided a visible image of the storm to forecasters. The Moderate Resolution Imaging Spectroradiometer or MODIS instrument aboard Terra captured the storm as it was moving over the Great Barrier Reef in the Coral Sea. Multispectral satellite imagery at the time showed that an exposed, well-defined low- On May 14, 2019 NASA's Terra satellite provided a level circulation center with a small area of visible image of Tropical Cyclone Ann as it was moving convection flaring 50 nautical miles to the south. over the Great Barrier Reef in the Coral Sea. Credit: NASA Worldview, Earth Observing System Data and Information System (EOSDIS) Ann is weakening because it has run into increased vertical wind shear, that is, winds blowing at different directions at different levels of the atmosphere tearing at the storm's structure. There Australia's world-famous Great Barrier Reef is is also dry air moving into Tropical Cyclone Ann at located in the Coral Sea, east of Queensland and low and mid-levels of the atmosphere, preventing on May 14, Tropical Cyclone Ann was moving over the development of thunderstorms that fuel the it. -
Workshop on the Impacts of Flooding
Workshop on the Impacts of Flooding Proceed/rigs of a Workshop held in Rockhamptori, Australia, 27 Septeinber 1991. , Edited by G.T. Byron Queensland Department of. ti Environment tand Heritage ’ Great Barrier Reef Marine Park Authority ‘, , ,’ @ Great Barrier Reef Marine Park Authority ISSN 0156-5842 ISBN 0 624 12044 7 Published by GBRMPA April 1992 The opinions expressed in th.is document are not necessarily those of the Great Barrier Reef Marine Park Authority or the Queensland Department of Env/ionment an!d Heritage. Great Barrier Reef Environment and P.O. Box 155 P.O. Box1379 North Quay , Townsville Queens’land 4002 Queensland 48 TABLE OF CONTENTS : PREFACE iv 1 EXECUTIVE SUMMARY V PART A: FORUM PAPERS Jim Pearce MLA Opening Address 1 Peter Baddiley Fitzroy River Basin 3 Rainfalls and The 1991 Flood Event Mike Keane Assessment of the 1991 16 Fitzroy River Flood How much water? J.P. O’Neill, G.T.Byron and Some Physical Characteristics 36 S.C.Wright and Movement of 1991 Fitzroy River flood plume PART B: WORKSHOP PAPERS GROUP A - WATER RELATED’ISSUES Jon E. Brodie and Nutrient Composition of 56 Alan Mitchell the January 1991 Fitzroy River Plume Myriam Preker The Effects of the 1991 75 Central Queensland Floodwaters around Heron Island, Great Barrier Reef i > d.T.Byron and J.P.O’Neill Flood Induced Coral Mortality 76 on Fringing Reefs in Keppel Bay J.S. Giazebrook and Effects of low salinity on 90 R. Van Woesik the tissues of hard corals Acropora spp., Pocillopora sp and Seriatopra sp from the Great Keppel region M.