Ocean Hazards Assessment
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Wave Data Recording Program
Wave data recording program Weipa Region 1978–2004 Coastal Sciences data report No. W2004.5 ISSN 1449–7611 Abstract This report provides summaries of primary analysis of wave data recorded in water depths of approximately 5.2m relative to lowest astronomical tide, 10km west of Evans Landing in Albatross Bay, west of Weipa. Data was recorded using a Datawell Waverider buoy, and covers the periods from 22 December, 1978 to 31 January, 2004. The data was divided into seasonal groupings for analysis. No estimations of wave direction data have been provided. This report has been prepared by the EPA’s Coastal Sciences Unit, Environmental Sciences Division. The EPA acknowledges the following team members who contributed their time and effort to the preparation of this report: John Mohoupt; Vince Cunningham; Gary Hart; Jeff Shortell; Daniel Conwell; Colin Newport; Darren Hanis; Martin Hansen; Jim Waldron and Emily Christoffels. Wave data recording program Weipa Region 1978–2004 Disclaimer While reasonable care and attention have been exercised in the collection, processing and compilation of the wave data included in this report, the Coastal Sciences Unit does not guarantee the accuracy and reliability of this information in any way. The Environmental Protection Agency accepts no responsibility for the use of this information in any way. Environmental Protection Agency PO Box 15155 CITY EAST QLD 4002. Copyright Copyright © Queensland Government 2004. Copyright protects this publication. Apart from any fair dealing for the purpose of study, research, criticism or review as permitted under the Copyright Act, no part of this report can be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise without having prior written permission. -
SOPAC Coastal Protection Feasibility Study
SOPAC Coastal Protection Feasibility Study Final Report August 2005 Executive Summary i 1. Introduction 1 2. Cyclone Design Condition Methodology Overview 3 2.1 Overall Philosophy 3 2.2 Detailed Methodology 4 2.3 Assessment of Recorded Data 4 2.3.1 Deterministic Model Checks 4 2.3.2 Simulation Production Modelling 5 3. Regional Tropical Cyclone Climatology 6 3.1 Statistical Assessment of the Tropical Cyclone Hazard 6 3.2 Parameterisation for Modelling Purposes 12 3.3 Regional Wind Speed and Pressure Data 15 3.4 Selection of Hindcast Storms 19 4. Numerical Modelling 21 4.1 Representation of Localities 21 4.2 Wind and Pressure Field Modelling 22 4.2.1 Wind and Pressure Calibration 22 4.3 Spectral Wave Modelling 31 4.3.1 Wave Model Details 31 4.3.2 Wave Model Calibration 31 4.4 Parametric Wave Model Performance 35 4.5 Tide, Surge and Wave Setup Modelling 37 4.5.1 TC Sally 1987 38 4.5.2 TC Gene 1992 41 4.5.3 TC Pam 1997 42 4.5.4 Commentary 42 4.6 Statistical Model Validation 46 4.6.1 Astronomical Tide 46 4.6.2 Wind 46 4.7 Statistical Storm Tide Model Estimates 49 4.8 Limitations of the Numerical Modelling 51 5. Coastal Protection Issues 52 5.1 Reef Top Conditions 52 5.2 Reef Opening Conditions 54 41/13806/316133 Coastal Protection Feasibility Study Final Report ii 5.3 Factors affecting Reef Setup and their influence on coastal protection choices. 55 5.3.1 Drainage 55 5.3.2 Barriers 55 5.3.3 Incremental Protection 55 5.4 Influence of Sea Level Rise and Climate Change 56 5.4.1 Sea Level Rise 56 5.4.2 Climate Change 56 6. -
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. -
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. -
Wave Data Recording Program Dunk Island 1998-2002
Wave data recording program Dunk Island 1998–2002 Coastal Services data report No. W2004.2 ISSN 1449–7611 Abstract This report provides summaries of primary analysis of wave data recorded in water depths of approximately 20m relative to lowest astronomical tide, 12.7km north of Dunk Island and 8km northeast of Clump Point in north Queensland. Data was recorded using a Datawell Waverider buoy, and covers the periods from 18 December 1998 to 12 November 2002. The data was divided into seasonal groupings for analysis. No estimations of wave direction data have been provided. This report has been prepared by the EPA’s Coastal Services Unit, Environmental Sciences Division. The EPA acknowledges the following team members who contributed their time and effort to the preparation of this report: John Mohoupt; Vince Cunningham; Gary Hart; Jeff Shortell; Daniel Conwell; Colin Newport; Darren Hanis; Martin Hansen and Jim Waldron. Wave data recording program Dunk Island 1998–2002 Disclaimer While reasonable care and attention have been exercised in the collection, processing and compilation of the wave data included in this report, the Coastal Services Unit does not guarantee the accuracy and reliability of this information in any way. The Environmental Protection Agency accepts no responsibility for the use of this information in any way. Environmental Protection Agency PO Box 155 BRISBANE ALBERT ST QLD 4002. Copyright Copyright Queensland Government 2004. Copyright protects this publication. Apart from any fair dealing for the purpose of study, research, criticism or review as permitted under the Copyright Act, no part of this report can be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise without having prior written permission. -
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. -
Issues and Events, I992
.1 , • , Melanesia in Review: Issues and Events, I992 FIJI Fijians and non-Indo-Fijians, won all The year 1992 may well be remembered the 5 seats allocated to that community. in Fiji as one of unexpected develop In an unexpectedly close contest, the ments in the political arena, dominated National Federation Party won 14 of by the general election in May. The the 27 seats allocated to the Indo-Fijian first half of the year was consumed by community, with the Fiji Labour Party the election campaign and the second securing 13. The Soqosoqo ni Vakavu half by its problematic reverberations. lewa ni Taukei was able to form a gov It ended with a promise to take Fiji ernment after entering into a coalition away from the politics ofracial divi with the General Voters Party and with sion toward a multiracial government the support of the Fijian National ofnational unity. Whether, and if, that United Front. Sitiveni Rabuka became occurs will be the challenge of1993. prime minister after Labour threw its The general election, the sixth since support behind him rather than Kami independence in 1970 and the first since kamica, who was backed by the the coups of1987, was preceded by a National Federation Party. long and sometimes bitter campaign Labour's strategy took supporters (see my article, this issue). Political completely by surprise. Its leaders fragmentation in the Fijian community argued that Rabuka was a changed accompanied the emergence of a num man who appeared to be a genuine ber ofpolitical parties and the rise of friend ofthe poor of all races. -
Guidelines for Converting Between Various Wind Averaging Periods in Tropical Cyclone Conditions
GUIDELINES FOR CONVERTING BETWEEN VARIOUS WIND AVERAGING PERIODS IN TROPICAL CYCLONE CONDITIONS For more information, please contact: World Meteorological Organization Communications and Public Affairs Office Tel.: +41 (0) 22 730 83 14 – Fax: +41 (0) 22 730 80 27 E-mail: [email protected] Tropical Cyclone Programme Weather and Disaster Risk Reduction Services Department Tel.: +41 (0) 22 730 84 53 – Fax: +41 (0) 22 730 81 28 E-mail: [email protected] 7 bis, avenue de la Paix – P.O. Box 2300 – CH 1211 Geneva 2 – Switzerland www.wmo.int D-WDS_101692 WMO/TD-No. 1555 GUIDELINES FOR CONVERTING BETWEEN VARIOUS WIND AVERAGING PERIODS IN TROPICAL CYCLONE CONDITIONS by B. A. Harper1, J. D. Kepert2 and J. D. Ginger3 August 2010 1BE (Hons), PhD (James Cook), Systems Engineering Australia Pty Ltd, Brisbane, Australia. 2BSc (Hons) (Western Australia), MSc, PhD (Monash), Bureau of Meteorology, Centre for Australian Weather and Climate Research, Melbourne, Australia. 3BSc Eng (Peradeniya-Sri Lanka), MEngSc (Monash), PhD (Queensland), Cyclone Testing Station, James Cook University, Townsville, Australia. © World Meteorological Organization, 2010 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspondence and requests to publish, reproduce or translate these publication in part or in whole should be addressed to: Chairperson, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0) 22 730 84 03 P.O. Box 2300 Fax: +41 (0) 22 730 80 40 CH-1211 Geneva 2, Switzerland E-mail: [email protected] NOTE The designations employed in WMO publications and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of WMO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
Climate Change and Health
Climate Change and Health Climate Change and Health CO2Coalition.org Table of Contents Introduc on .........................................................................................................................................................................2 Warmth, Wealth and Health ................................................................................................................................................2 Figure 1: The Preston curve of Life Expectancy at birth increasing with GDP per capita ..............................................3 Figure 2: Projected economic impact of global warming of 1⁰C, 2.5⁰C and 3⁰C over the 21st century .........................4 Temperature and Disease ..........................................................................................................................................4 Figure 3: Nocturnal temperature trends for 1910-39 (Top) and 1970-97 (Bo om): trends plo ed for the coldest nights from the le (No. 1) to the warmest (No. 365) ...............................................................................................5 Figure 4: Distribu on of cholera in 2016 as reported to the World Health Organisa on ...............................................7 Figure 5: Projected changes in cold-related and heat-related excess mortality over the 21st century for nine regions and three emissions scenarios: RCP2.6, RCP4.5 and RCP8.5 .......................................................................9 Disease Vectors ..................................................................................................................................................................10 -
Tropical Cyclone Rona, 1999
CASE STUDY: Tropical Cyclone Rona, 1999 By Mr Jeff Callaghan Retired Senior Severe Weather Forecaster, Bureau of Meteorology, Brisbane Rona made landfall just to the north of Cow Bay, which is near the Daintree River Mouth. The main wind damage extended from Newell Beach to Cape Tribulation, with the major damage between Cape Kimberley and Cape Tribulation. Some trees in the Cape Tribulation area that survived the legendry 1934 cyclone fell during Rona. The maximum wind speeds were recorded by the Low Isle automatic weather station with 10- minute average winds of 71 knots and a maximum wind gust of 85 knots. The lowest pressure of 983.0 hPa (not in the eye) was recorded at Low Isle. A 1metre storm surge was recorded at Port Douglas (at low tide) and a 1.4m surge was recorded at the mouth of the Mossman River. These sites were south of the maximum wind zone where the largest storm surge would be expected. Major flooding occurred between Cairns and Townsville. Despite the confined wind fetch inside the Barrier Reef, Rona generated some large waves as indicated from wave recording stations run by the Beach Protection Authority. At the Low Isle station the peak significant wave height (the average of the one-third highest waves in a 26.6 minute period) exceeded 3.5m and the maximum wave height exceeded 6.3m. The Cairns station recorded significant wave heights to 2.49m and a peak height of 4.65m. These were record heights (since recordings commenced in 1975) for Cairns. Tropical cyclone Steve in 2000 exceeded these wave heights at Cairns. -
Storm Surge: Know Your Risk in Queensland!
Storm Surge: Know your risk in Queensland! Storm surge is a rise in sea level above the normal tide usually associated with a low pressure weather system such as a tropical cyclone. Storm surge develops due to strong winds pushing water towards the coastline as well as the low atmospheric pressure drawing up the sea surface. The Queensland coastline is highly vulnerable to storm surge. This is due to the frequency of tropical cyclones, the wide continental shelf and relatively shallow ocean floor in both the Great Barrier Reef lagoon and in the Gulf of Carpentaria, as well as the low lying nature of many coastal cities and towns. While the highest storm surges are more likely to occur in North Queensland and the Gulf of Carpentaria, they can also develop in southeast Queensland affecting the Sunshine Coast, Moreton Bay and the Gold Coast. Storm surges may reach magnitudes of 1 to 10 metres above the tide depending on the intensity of the cyclone, its size and the local characteristics of the coastline. Impacts Coral Sea Storm surge can be very dangerous and poses a critical risk Gulf of Carpentaria to human life during tropical cyclones. Great Cairns Barrier Reef The length of coastline affected by a storm surge can be Innisfail tens to hundreds of kilometres wide. The rise in sea level Cardwell Townsville can be rapid and high in velocity, inundating the ground Bowen floor of buildings, even up to the roof. Mackay Queensland Storm surge has the power to easily move cars, even Gladstone houses, can damage roads and buildings and can be Hervey Bay almost impossible to manoeuvre through. -
Notable Tropical Cyclones and Unusual Areas of Tropical Cyclone Formation
A flood is an overflow of an expanse of water that submerges land.[1] The EU Floods directive defines a flood as a temporary covering by water of land not normally covered by water.[2] In the sense of "flowing water", the word may also be applied to the inflow of the tide. Flooding may result from the volume of water within a body of water, such as a river or lake, which overflows or breaks levees, with the result that some of the water escapes its usual boundaries.[3] While the size of a lake or other body of water will vary with seasonal changes in precipitation and snow melt, it is not a significant flood unless such escapes of water endanger land areas used by man like a village, city or other inhabited area. Floods can also occur in rivers, when flow exceeds the capacity of the river channel, particularly at bends or meanders. Floods often cause damage to homes and businesses if they are placed in natural flood plains of rivers. While flood damage can be virtually eliminated by moving away from rivers and other bodies of water, since time out of mind, people have lived and worked by the water to seek sustenance and capitalize on the gains of cheap and easy travel and commerce by being near water. That humans continue to inhabit areas threatened by flood damage is evidence that the perceived value of living near the water exceeds the cost of repeated periodic flooding. The word "flood" comes from the Old English flod, a word common to Germanic languages (compare German Flut, Dutch vloed from the same root as is seen in flow, float; also compare with Latin fluctus, flumen).