5 Tourism, Disasters and Vulnerability
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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. -
Tropical Cyclone Tessi, April 2000
CASE STUDY: Tropical Cyclone Tessi, April 2000 Introduction Like tropical cyclone Steve, Tessi underwent extremely rapid development near the coast as it passed close to Townsville, Australia’s largest tropical population centre. Tropical Cyclone Tessie was named at 1800 UTC 1 April 2000 (4 am local time 2nd ) and almost reached hurricane force intensity near the coast 21 hours later. An Australian Institute of Marine Science (AIMS) automatic weather station (AWS) on Magnetic Island (15 km northeast oF the Townsville Meteorological OFFice) recorded 10 minute average wind speeds to 59 knots. The mean sea level sequence (MSL) (Figure 1) show a tropical low, with an absence oF any monsoon flow, moving towards the northeastern Australian coast (top panel). By 2300 UTC 1 April (centre panel in Figure 1) the low had become a tropical cyclone and note how the 1008 hPa isobar decreased in radius (indicating rising pressures around the system). At 2000 UTC 2 April 2000 (lower panel) it was a very small “midget” cyclone with the pressure continuing to rise around it. Impact of Tessi The cyclone Formed a small compact radar eye (diameter 10 to15 km) near the coast after 1800 UTC 2 April 2000. It appears the worst wind damage was just outside this eye in the area around Mutarnee (a small village 60 km northwest of Townsville). Here many large trees were uprooted and the roof of a farmhouse was lifted off, battens and all, and deposited 50 metres away in a cane field. The most extensive tree damage was Further east in the normally uninhabited beach areas where some isolated beach huts were unrooFed. -
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. -
NASA Sees Ex-Tropical Cyclone Gillian's Remnants Persist 20 March 2014
NASA sees ex-Tropical Cyclone Gillian's remnants persist 20 March 2014 (PR) instrument revealed that intense convective storms in this area were still dropping rain at a rate of over 97 mm/3.8 inches per hour and returning radar reflectivity values of over 51dBZ. TRMM PR data were used to create a simulated 3-D view that showed the vertical structure of precipitation within the stormy area contained towering thunderstorms. The Joint Typhoon Warning Center noted that animated enhanced satellite imagery on March 20 showed flaring deep convection associated with a slowly-consolidating low-level circulation center. On March 20, the Tropical Cyclone Warning Centre in Jakarta noted that Gillian's remnants had maximum sustained winds near 25 knots/28.7 mph/46.3 kph. It was centered near 9.4 south and 119.0 east, about 233 nautical miles/ 268.1 miles/431.5 km east of South Kuta, Bali, Indonesia. TRMM passed above Gillian's remnants on March 20, TCWC issued watches and warnings for parts of 2014, and this 3-D simulation of TRMM data showed the Indonesia archipelago in Bahasa. several of the tallest thunderstorms in Gillian's remnants were reaching heights of over 15.75 km/9.8 miles. Credit: NASA/SSAI, Hal Pierce NASA's TRMM satellite continues to follow the remnants of former Tropical Cyclone Gillian as it moved from the Southern Pacific Ocean into the Southern Indian Ocean where it appears to be re- organizing. The persistent remnants of tropical cyclone Gillian have moved westward over 2,700 km/1,674 miles since forming in the Gulf of Carpentaria on March 8, 2014. -
Tropical Cyclone Justin 6 - 24 March 1997
Severe Tropical Cyclone Justin 6 - 24 March 1997 Queensland Tropical Cyclone Warning Centre Bureau of Meteorology A. Summary Severe Tropical Cyclone Justin was a large, long-lived Coral Sea cyclone that crossed the Queensland coast as a category two cyclone northwest of Cairns on 22 March. Two lows that merged in a very active monsoon trough in the Coral Sea developed into Tropical Cyclone Justin on 7 March, reaching maximum intensity on 9 March as a very large system. Justin remained almost stationary and due to cooling SST’s it was downgraded to a tropical low on 13 March. Justin then drifted north over warmer SST’s and re-intensified to tropical cyclone strength on 14 March, reaching a peak intensity on 17 March before weakening and crossing the coast northwest of Cairns on 22 March. The combined effects of heavy rain, large seas and gale to storm force winds caused widespread damage in the region between Cairns and Townsville and the loss of two lives. Earlier in Justin’s lifecycle 30 people were killed in Papua New Guinea and five people died when their yacht was destroyed. Justin was reportedly responsible for an estimated loss of $150 million to the agricultural industry alone. B. Meteorological Description Intensity Analysis The monsoon trough was characterised at 2300 UTC 3 March by a series of MSL low pressure centres below 1000 hPa extending from northeast Australia across the Coral Sea and by 2300 UTC 5 March one centre had developed in the Coral Sea. This low intensified and was named Justin at 1900 UTC 6 March. -
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. -
4. the TROPICS—HJ Diamond and CJ Schreck, Eds
4. THE TROPICS—H. J. Diamond and C. J. Schreck, Eds. Pacific, South Indian, and Australian basins were a. Overview—H. J. Diamond and C. J. Schreck all particularly quiet, each having about half their The Tropics in 2017 were dominated by neutral median ACE. El Niño–Southern Oscillation (ENSO) condi- Three tropical cyclones (TCs) reached the Saffir– tions during most of the year, with the onset of Simpson scale category 5 intensity level—two in the La Niña conditions occurring during boreal autumn. North Atlantic and one in the western North Pacific Although the year began ENSO-neutral, it initially basins. This number was less than half of the eight featured cooler-than-average sea surface tempera- category 5 storms recorded in 2015 (Diamond and tures (SSTs) in the central and east-central equatorial Schreck 2016), and was one fewer than the four re- Pacific, along with lingering La Niña impacts in the corded in 2016 (Diamond and Schreck 2017). atmospheric circulation. These conditions followed The editors of this chapter would like to insert two the abrupt end of a weak and short-lived La Niña personal notes recognizing the passing of two giants during 2016, which lasted from the July–September in the field of tropical meteorology. season until late December. Charles J. Neumann passed away on 14 November Equatorial Pacific SST anomalies warmed con- 2017, at the age of 92. Upon graduation from MIT siderably during the first several months of 2017 in 1946, Charlie volunteered as a weather officer in and by late boreal spring and early summer, the the Navy’s first airborne typhoon reconnaissance anomalies were just shy of reaching El Niño thresh- unit in the Pacific. -
Social Policy in the Post-Crisis Context of Small Island Developing States: a Synthesis
A Service of Leibniz-Informationszentrum econstor Wirtschaft Leibniz Information Centre Make Your Publications Visible. zbw for Economics Perch, Leisa; Roy, Rathin Working Paper Social policy in the post-crisis context of small island developing states: A synthesis Working Paper, No. 67 Provided in Cooperation with: International Policy Centre for Inclusive Growth (IPC-IG) Suggested Citation: Perch, Leisa; Roy, Rathin (2010) : Social policy in the post-crisis context of small island developing states: A synthesis, Working Paper, No. 67, International Policy Centre for Inclusive Growth (IPC-IG), Brasilia This Version is available at: http://hdl.handle.net/10419/71774 Standard-Nutzungsbedingungen: Terms of use: Die Dokumente auf EconStor dürfen zu eigenen wissenschaftlichen Documents in EconStor may be saved and copied for your Zwecken und zum Privatgebrauch gespeichert und kopiert werden. personal and scholarly purposes. Sie dürfen die Dokumente nicht für öffentliche oder kommerzielle You are not to copy documents for public or commercial Zwecke vervielfältigen, öffentlich ausstellen, öffentlich zugänglich purposes, to exhibit the documents publicly, to make them machen, vertreiben oder anderweitig nutzen. publicly available on the internet, or to distribute or otherwise use the documents in public. Sofern die Verfasser die Dokumente unter Open-Content-Lizenzen (insbesondere CC-Lizenzen) zur Verfügung gestellt haben sollten, If the documents have been made available under an Open gelten abweichend von diesen Nutzungsbedingungen die in -
National Climate Change Risk Assessment for New Zealand: Technical Report
National Climate Change Risk Assessment for New Zealand Arotakenga Tūraru mō te Huringa Āhuarangi o Āotearoa Technical report Pūrongo Whaihanga This document may be cited as: Ministry for the Environment. 2020. National Climate Change Risk Assessment for New Zealand – Arotakenga Tūraru mō te Huringa Āhuarangi o Āotearoa: Technical report – Pūrongo whaihanga. Wellington: Ministry for the Environment. Disclaimer The information in this publication is, according to the Ministry for the Environment’s best efforts, accurate at the time of publication. The information provided does not alter the laws of New Zealand and other official guidelines or requirements. Users should take specific advice from qualified professional people before undertaking any action, as a result of information obtained from this publication. The Ministry for the Environment does not accept any responsibility or liability whether in contract, tort, equity or otherwise, for any action taken as a result of reading, or reliance placed on the Ministry for the Environment because of having read any part, or all, of the information in this publication or for any error, or inadequacy, deficiency, flaw in or omission from the information provided in this publication. Acknowledgements Prepared for the Ministry for the Environment by a consortium led by AECOM, including Tonkin + Taylor Ltd, NIWA and Latitude and a number of independent contractors. Published in July 2020 by the Ministry for the Environment Manatū Mō Te Taiao PO Box 10362, Wellington 6143, New Zealand ISBN: 978-1-98-857995-5 (online) Publication number: ME 1508 © Crown copyright New Zealand 2020 This document is available on the Ministry for the Environment website: www.mfe.govt.nz. -
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. -
Solomon Islands
Climate Risk and Adaptation Country Profile April 2011 N Ontong Java Atol Choiseul Malloco Bay Santa Isabel Buala New Yiru Georgia Auki Malaita Harbour Honiara Guadalcanal Kirakira Elevation San Nendo meters above sea-level Cristobal Lata 7088 m Bellona Rennell Utupua Vanikolo -416 m Key to Map Symbols Capital City/Town 0 50 100 200 Kilometers Vulnerability, Risk Reduction, and Adaptation to CLIMATE Climate Change DISASTER RISK ADAPTATION REDUCTION SOLOMON ISLANDS Climate Change Team ENV t Solomon Climate Risk and Adaptation Country Profiles Islands COUNTRY OVERVIEW The Solomon Islands are an archipelago located in the Melanesian region of the Pacific, south-east of Papua New Guinea. The Archipelago consists of 992 small islands that cover approximately 27,000 square kilometers (km2), and a sea area of 1.35 million km2 dispersed between 7 and 12 degrees south of the equator and 156 and 170 degrees longitude. Considered the “Amazon of the Seas”, the country’s 30.00 expansive area covers a unique geographical environment of atolls, mountains, and salt-water 25.00 Thousands lagoons, and has one of the world’s richest marine diversity, including 75% of the known coral species, 20.00 more than 30% of the world’s coral reefs, 40% of the 15.00 coral reef species, and the largest mangrove forest in km2 the world1. Of the 523,170 inhabitants, most live in 10.00 rural areas (~80%)2, in contrast to the rest of East Asia and the Pacific (with rural populations of 60%). 5.00 Agriculture, forestry, and fishing are the mainstay of the economy, with agriculture contributing nearly 0.00 36% of GDP in 2006. -
Natural Hazard Resilient Communities and Land Use Planning: the Limitations of Planning Governance in Tropical Australia
Harwood et al., J Geogr Nat Disast 2014, 4:2 Geography & Natural Disasters http://dx.doi.org/10.4172/2167-0587.1000130 ResearchResearch Article Article OpenOpen Access Access Natural Hazard Resilient Communities and Land Use Planning: The Limitations of Planning Governance in Tropical Australia Sharon Harwood1*, Dean Carson2, Ed Wensing3 and Luke Jackson4 1School of Earth and Environmental Sciences, James Cook University, PO Box 6811, Cairns QLD 4870, Australia 2Professor of Rural and Remote Research, Flinders University Rural Clinical School , PO Box 889, Nuriootpa SA 5355, Australia 3National Centre for Indigenous Studies, The Australian National University, Canberra ACT 0200 4School of Earth and Environmental Sciences, James Cook University, PO Box 6811, Cairns QLD, 4870, Australia Abstract This paper examines how two Australian land use planning systems address the creation of hazard resilient communities in tropical areas. The application of substantive hazard knowledge and how this influences the associated procedures within the planning system is examined. The case studies of Darwin the capital of the Northern Territory, and the beachside suburb of Machans Beach within the Cairns Regional Council in far north Queensland are investigated. Both case study locations have experienced tropical cyclones since settlement and despite their hazard prone locations, both have intensified over their 120 year existence. Moreover, it is predicted that cyclones in tropical Australia will decrease in number, but increase in intensity. It would be rational to assume that industry, community and government would actively pursue planning strategies to negate the risks of natural hazards and the corresponding level of vulnerability to a hazard event. However, neither communities nor planning are driven by rational technical decision making processes.