NERMN Beach Profile Monitoring 2011
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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. -
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. -
Backwash Sediment Record of the 2009 South
Backwash sediment record of the 2009 South Pacific Tsunami and 1960 Great Chilean Earthquake Tsunami Brieuc Riou, Eric Chaumillon, Catherine Chagué, Pierre Sabatier, Jean-Luc Schneider, John-Patrick Walsh, Atun Zawadzki, Daniela Fierro To cite this version: Brieuc Riou, Eric Chaumillon, Catherine Chagué, Pierre Sabatier, Jean-Luc Schneider, et al.. Back- wash sediment record of the 2009 South Pacific Tsunami and 1960 Great Chilean Earthquake Tsunami. Scientific Reports, Nature Publishing Group, 2020, 10, pp.4149. 10.1038/s41598-020-60746-4. hal- 02544141 HAL Id: hal-02544141 https://hal.archives-ouvertes.fr/hal-02544141 Submitted on 12 Mar 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - NoDerivatives| 4.0 International License www.nature.com/scientificreports OPEN Backwash sediment record of the 2009 South Pacifc Tsunami and 1960 Great Chilean Earthquake Tsunami Brieuc Riou1,2*, Eric Chaumillon1, Catherine Chagué3, Pierre Sabatier4, Jean-Luc Schneider2, John-Patrick Walsh5, Atun Zawadzki6 & Daniela Fierro6 Following recent tsunamis, most studies have focused on the onshore deposits, while the ofshore backwash deposits, crucial for a better understanding of the hydrodynamic processes during such events and ofering an opportunity for sedimentary archives of past tsunamis, have mostly been omitted. -
Pacific Study (Focusing on Fiji, Tonga and Vanuatu
1 EXECUTIVE SUMMARY 1.1 Hazard exposure 1.1. Pacific island countries (PICs) are vulnerable to a broad range of natural disasters stemming from hydro-meteorological (such as cyclones, droughts, landslide and floods) and geo-physical hazards (volcanic eruptions, earthquakes and tsunamis). In any given year, it is likely that Fiji, Tonga and Vanuatu are either hit by, or recovering from, a major natural disaster. 1.2. The impact of natural disasters is estimated by the Pacific Catastrophe Risk Assessment and Financing Initiative as equivalent to an annualized loss of 6.6% of GDP in Vanuatu, and 4.3% in Tonga. For Fiji, the average asset losses due to tropical cyclones and floods are estimated at more than 5%. 1.3. In 2014, Tropical Cyclone (TC) Ian caused damage equivalent to 11% to Tonga's GDP. It was followed in 2018 by damage close to 38% of GDP from TC Gita. In 2015, category five TC Pam displaced 25% of Vanuatu's population and provoked damage estimated at 64% of GDP. In Fiji, Tropical Cyclone Winston affected 62% of the population and wrought damage amounting to 31% of GDP, only some three and a half years after the passage of Tropical Cyclone Evan. 1.4. Vanuatu and Tonga rank number one and two in global indices of natural disaster risk. Seismic hazard is an ever-present danger for both, together with secondary risks arising from tsunamis and landslides. Some 240 earthquakes, ranging in magnitude between 3.3 and 7.1 on the Richter Scale, struck Vanuatu and its surrounding region in the first ten months of 2018. -
Evers C Thesis 2005.Pdf (PDF, 10.47MB)
IlARE BOOKS all The University of Sydney Copyright in relation to this thesis. Under the Copyright Act 1968 (several provision of which are referred to below). this thesis must be used only under the normal conditions of scholarly fair dealing for the purposes of research. criticism or review. In particular no results or conclusions should be extracted from it, nor should it be copied or closely paraphrased in whole or in part without the written consent of the author. Proper written acknowledgement should be made for any assistance obtained from this thesis. Under Section 35(2) of the Copyright Act 1968 'the author of a literary, dramatic. musical or artistic work is the owner of any copyright subsisting in the work', By virtue of Section 32( I) copyright 'subsists in an original literary, dramatic, musical or artistic work that is unpublished' and of which the author was anAustralian citizen,anAustralian protected person or a person resident inAustralia. The Act, by Section 36( I) provides: 'Subject to this Act, the copyright in a literary, dramatic, musical or artistic work is infringed by a person who, not being the owner of the copyright and without the licence of the owner of the copyright. does in Australia, or authorises the doing in Australia of, any act comprised in the copyright', Section 31(I )(.)(i) provides that copyright includes the exclusive right to 'reproduce the work in a material form'.Thus.copyright is infringed by a person who, not being the owner of the copyright, reproduces or authorises the reproduction of a work, or of more than a reasonable part of the work, in a material form. -
Our Freshwater
State of the Environment report 2012 | Our freshwater Surface water quality OUR Northland has an extensive network of rivers flowing and muddy because the land is FRESHWATER and streams. None of them are considered dominated by deeply weathered geology and major on a national scale as Northland's fine clay soils. narrow land mass means most rivers are relatively short with small catchments. Most of Northland also has a large number of small, the major rivers flow into harbours, rather than shallow lakes and associated wetlands. Most discharging directly to the open coast which of these have been formed between stabilised means contaminants tend to take longer to sand dunes on the west coast. These dune disperse from these sheltered environments. lakes are grouped on the Aupōuri, Karikari and Poutō peninsulas. Most are between five and The Northern Wairoa River is Northland's 35 hectares in area and are generally less than largest river, draining a catchment area of 15 metres deep. However, Lake Taharoa of the 3650 square kilometres, or 29 percent of Kai Iwi group near Dargaville is one of the Northland's land area. largest and deepest dune lakes in New Zealand. It covers an area of 237ha and is 37m Flows in rivers vary considerably with rainfall deep. There are also a few volcanic and man- and high intensity storms causing flash floods, made lakes. Northland’s largest lake is Lake while prolonged dry spells lead to very low Ōmāpere, which is 1160ha in area and located flows in many smaller catchments. Northland’s to the north of Kaikohe. -
Title Layout
Disaster Risk Assessment and Recovery Utilizing Unmanned Aerial Vehicles in the Pacific Islands. The World Bank UAV4Resilience Project - Update Malcolm Archbold Consultant, World Bank 27 November 2019 Pacific Islands GIS & RS Conference 2019 Introduction Pacific Island nations are some of the most vulnerable to natural disasters • Cyclone Waka – 2001 – Tonga • Cyclone Heta – 2003 – Tonga, Niue, American Samoa • Cyclone Lin – 2008 – Fiji • Cyclone Wilma – 2010 – Solomon Islands, Tonga • Cyclone Ian – 2013 – Fiji, Tonga • Cyclone Pam – 2014 – Vanuatu • Cyclone Winston – 2016 – Fiji • Cyclone Gita – 2018 - Tonga Cyclone Ian, Vanuatu, Jan 2014 The World Bank UAV4Resilence Project • Assess the utility of UAVs in Disaster Management for the SW Pacific • Identify the potential cost-benefits of UAVs for disaster assessment • Develop Standard Operating Procedures for in country operations UAV4Resilence Project UAV Challenge Project – October 2017 Cyclone Gita – Feb 2018 – Tonga Cyclone Gita – 2018 – Tonga Cyclone Gita – 2018 – Tonga Cyclone Gita – 2018 – Tonga Cyclone Gita – 2018 – Tonga OpenAerialMap.org UAV Training and Capacity Building • Commence in May 2019 • Objectives: • Assist in procurement, training and capacity building • Involve Govt Disaster Management organisations and associated Govt Depts/Ministries • Facilitate cooperation and communication between Govt Depts and local Civil Aviation and Air Traffic Control authorities. DroneFlyer Course (2 days) Day 1 Day 2 • Civil Aviation PRAS/drone rules • Review of Day 1 • Airspace • Semi -
ST THOMAS CHURCH PH: 0273202560 (The Church on the Hill) St Thomas Church Held a Special Meeting After the Service This Month to Select a New Committee
Whiringa-a-Rangi / November 2015 Maketu, Aotearoa/ New Zealand POSSIBLE FUTURE LEADERS Stronger safer community Congratulations On Saturday October 31st , Maketu celebrated our YES (Youth in Emergency Services), at Whakaue Marae. It was the graduation ceremony for the yes programme for 15 of our youth. For the last 3 months these 15 young members of our community attended inductions & trainings with the emergency services, every week. At least 2 sessions a week and had a sce- nario weekend. They learnt emergency response skills, risk management, time Maketu Y.E.S graduates with the Y.E.S coordinator Clester Eru management, commitment and strengthened their connection to the community. The recipients of the certificates are Meteria Tapsell-Walters, Rawinia Kohu, Jack Brown, Kaea Walters, Manepo Tapsell- Wafer, Shania Thomas, Creedance Kirikiri Brown, Jalyn- Memory Rolleston, Isaiah Fata, Manaia Gourlay, Billie Hikatan- gata, Manaia Newton, Isabella Lawrence, Denny Lawrence, & Seini Maile Maketu stands in good steed as it is hoped some of the youth will be part of the future emergency services as well as potential lead- ers. It was a momentous moment for our community. Thanks to the Shane Gourlay (Maketu Fire Ministry of Youth, Minister of Social Development, Civil De- Brigade Station Officer), Sue fence Emergency Response, Western BoP District Council, St Mathews Councillor, Hon. Anne John’s, Maketu Coastguard, Tolley Ministry of Social Devel- Maketu Fire Brigade, Civil opment & Clester Eru Y.E.S Defence, Maketu Commu- nity Development, Maketu programme coordinator. Health & Social Services, Whakaue Marae, Jodie Isaiah Fata receiving his Beattie, and of course our Certificate of completion YOUTH. -
The Cyclone of 1936: the Most Destructive Storm of the Twentieth Century?
Weather and Climate (2000) 20: 23-28 23 THE CYCLONE OF 1936: THE MOST DESTRUCTIVE STORM OF THE TWENTIETH CENTURY? Erick Brenstrum MetService In late January 1936 a weakening tropical of New Zealand on the 31st and intensified cyclone moving towards New Zealand then crossed the North Island on the 2nd of interacted with a cold front over the north February. It was not assigned a name, as the Tasman Sea to form one of the deepest practice of routinely naming tropical cyclones depressions ever to cross the country. The did not begin until 1963. meteorological aspects of the depression were described in a report published by Barnett in FLOODING 1938. He did not describe in detail the destruction caused by the storm, limiting Heavy rain fell over the entire North Island himself to the comment" Graphic descriptions bringing most of the major rivers into flood. of the effects of the storm can be found in the The Mangakahia River in Northland rose 19 daily press for the few days following the 2nd metres at Titoki. Kaitaia main-street was February." flooded a metre deep and one man was The following article is a summary of the drowned there when a house was washed accounts in the newspapers, and shows that away as he was trying to retrieve a friend's this was probably the most destructive storm belongings. Another man was killed near to affect New Zealand during the twentieth Thames in the Coromandel when his hut was century. carried into a flooded stream by a slip. The tropical cyclone formed south of the In Whangerei almost 300 mm of rain fell in Solomon Islands on January 28 then moved 24 hours and floodwater ran through the southeast to pass between New Caledonia and business district tearing up footpaths and Vanuatu. -
The Pacific Experience in Developing Policy and Legislation on Disaster Risk Reduction and Climate Change Adaptation
THE PACIFIC EXPERIENCE IN DEVELOPING POLICY AND LEGISLATION ON DISASTER RISK REDUCTION AND CLIMATE CHANGE ADAPTATION The Pacific Experience in Developing Policy and Legislation on Disaster Risk Reduction and Climate Change Adaptation 1 The Pacific Experience in Developing Policy and Legislation on Disaster Risk Reduction and Climate Change Adaptation THE PACIFIC EXPERIENCE IN DEVELOPING POLICY AND LEGISLATION ON DISASTER RISK REDUCTION AND CLIMATE CHANGE ADAPTATION Contents Glossary iv Chapter 1. Introduction 1 1.1 Scope of the study and acknowledgements 1 1.2 Background 1 1.3 Findings of the institutional and policy analysis on DRR and CCA in the Pacific 3 Chapter 2. Joint National Action Plans on Disaster Risk Management and Climate Change (JNAPs) – Regional Perspective 4 2.1 Background of the JNAPs 4 2.2 Intent to develop the JNAPs 5 2.3 Process to develop the JNAPs 6 2.4 Implementation of the JNAPs 7 Chapter 3. Country Studies – Tonga 10 3.1 Introduction 10 3.2 Joint National Action Plan on Climate Change Adaptation and Disaster Risk Management 2010-2015 10 3.3 Emergency Management Act (2007) 16 Chapter 4. Country Studies – Cook Islands 19 4.1. Introduction 19 4.2 Te Kaveinga Nui – National Sustainable Development Plan 2011-2015 19 4.3 Disaster Risk Management Act (2007) 23 Chapter 5. Country Studies – Solomon Islands 26 5.1 Introduction 26 5.2 Joint framework for resilient development 26 5.3 Process towards the joint framework for resilient development 27 Chapter 6. Conclusions 29 References 32 Annex 1: Interviewees 34 Annex 2: Interview -
Wave Data Recording Program
Wave data recording program Queensland wave climate annual summary for season 2000–01 Coastal Services data report No. 2000.3 ISSN 1449–7611 Foreword This summary of wave climate in Queensland is the earliest of the series of technical wave reports that will be prepared annually by the Coastal Services Unit. It represents a change in the way wave data is presented by the Environmental Protection Agency (EPA). Previously, the wave data recording program technical report series comprised separate reports prepared for each region, covering all data recorded at a site from deployment to date of report. Annual reports will not replace the more comprehensive regional reports. Instead, they will serve to supplement and enhance the reporting ability of the Coastal Services Unit by providing more timely information on wave climates in Queensland. Regional wave data reports will continue to provide the more thorough, long-time presentation of regional conditions. Using the information presented annually, it is hoped that in future, regional reports will be updated every five years. Annual reports will cover the year from 1 November to 31 October. The start of the reporting year therefore coincides with the start of the annual cyclone season that extends from 1 November through to 30 April. This period is also classed as summer in both this annual report and the regional technical reports. The remainder of the year (1 May to 31 October) is classed as winter in these reports. Annual reports present wave information in a similar format to the regional reports, however they also include (for the first time), plots of monthly average significant wave heights and directional wave rose (where possible). -
MASARYK UNIVERSITY BRNO Diploma Thesis
MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories.