Torres Strait Islands and Climate Displacement
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CYI Submission on Aurukun Shire Council's Proposal for a Trial
CYI submission on Aurukun Shire Council’s Proposal for a Trial Alcohol Event 24 May 2019 1 Contents Introduction ............................................................................................................................... 3 The Gap is at its widest in Aurukun ........................................................................................... 4 It hasn’t always been this way: an ignoble history .................................................................... 6 State Violence: the Queensland Government Takeover of Aurukun .................................... 6 The forced imposition of the alcohol canteen ....................................................................... 6 Two decades of grog: the cycle is embedded ........................................................................ 7 A shameful response .............................................................................................................. 9 Beattie and Bligh enable restrictions of alcohol .................................................................. 10 Alcohol restrictions have changed the trajectory .................................................................... 10 Reducing alcohol abuse must remain the top long-term priority ........................................... 11 Harmful policy drift—no clear policy ....................................................................................... 13 A plan is urgently required ...................................................................................................... -
Torresstrait Islander Peoples' Connectiontosea Country
it Islander P es Stra eoples’ C Torr onnec tion to Sea Country Formation and history of Intersection of the Torres Strait the Torres Strait Islands and the Great Barrier Reef The Torres Strait lies north of the tip of Cape York, Torres Strait Islanders have a wealth of knowledge of the marine landscape, and the animals which inhabit it. forming the northern most part of Queensland. Different marine life, such as turtles and dugong, were hunted throughout the Torres Strait in the shallow waters. Eighteen islands, together with two remote mainland They harvest fish from fish traps built on the fringing reefs, and inhabitants of these islands also embark on long towns, Bamaga and Seisia, make up the main Torres sea voyages to the eastern Cape York Peninsula. Although the Torres Strait is located outside the boundary of the Strait Islander communities, and Torres Strait Islanders Great Barrier Reef Marine Park, it is here north-east of Murray Island, where the Great Barrier Reef begins. also live throughout mainland Australia. Food from the sea is still a valuable part of the economy, culture and diet of Torres Strait Islander people who have The Torres Strait Islands were formed when the land among the highest consumption of seafood in the world. Today, technology has changed, but the cultural use of bridge between Australia and Papua New Guinea the Great Barrier Reef by Torres Strait Islanders remains. Oral and visual traditional histories link the past and the was flooded by rising seas about 8000 years ago. present and help maintain a living culture. -
Physical Geography of Southeast Asia
Physical Geography of Southeast Asia Creating an Annotated Sketch Map of Southeast Asia By Michelle Crane Teacher Consultant for the Texas Alliance for Geographic Education Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 Guiding Question (5 min.) . What processes are responsible for the creation and distribution of the landforms and climates found in Southeast Asia? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 2 Draw a sketch map (10 min.) . This should be a general sketch . do not try to make your map exactly match the book. Just draw the outline of the region . do not add any features at this time. Use a regular pencil first, so you can erase. Once you are done, trace over it with a black colored pencil. Leave a 1” border around your page. Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 3 Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 4 Looking at your outline map, what two landforms do you see that seem to dominate this region? Predict how these two landforms would affect the people who live in this region? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 5 Peninsulas & Islands . Mainland SE Asia consists of . Insular SE Asia consists of two large peninsulas thousands of islands . Malay Peninsula . Label these islands in black: . Indochina Peninsula . Sumatra . Label these peninsulas in . Java brown . Sulawesi (Celebes) . Borneo (Kalimantan) . Luzon Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 6 Draw a line on your map to indicate the division between insular and mainland SE Asia. -
Australian Aborigines & Cultural Tourism
University of Wollongong Research Online Centre for Multicultural Studies Working Papers Faculty of Law, Humanities and the Arts 1991 Australian Aborigines & cultural tourism: case studies of Aboriginal involvement in the tourist industry Julie Finlayson Recommended Citation Finlayson, Julie, Australian Aborigines & cultural tourism: case studies of Aboriginal involvement in the tourist industry, Centre for Multicultural Studies, University of Wollongong, Working Paper 15, 1991, 127. http://ro.uow.edu.au/cmsworkpapers/13 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Australian Aborigines & cultural tourism: case studies of Aboriginal involvement in the tourist industry Abstract The principal focus of this report has been with issues of direct concern to Aboriginal people and communities involved with cultural tourism. Report recommendations stress the need for greater consideration of Aboriginal cultural perspectives in the development and implementation of government policies. A central question to emerge from the study is whether cultural tourism is merely a novel angle within current developments in tourism and enjoying a good deal of attention and enthusiasm from tourist organisations and operators, or whether it is primarily a context for commercial enterprise development by Aboriginal people? A related matter is the question of what purpose Aboriginal ventures in cultural tourism are designed to serve and in whose interests they are developed? Answers to these issues were not always obvious to Aboriginal people involved in the ventures surveyed nor was it necessarily apparent to some of the non-Aboriginal participants. The purpose of Aboriginal tourism ventures is problematic in public policy and in bureaucratic practice. -
Navigating Boundaries: the Asian Diaspora in Torres Strait
CHAPTER TWO Tidal Flows An overview of Torres Strait Islander-Asian contact Anna Shnukal and Guy Ramsay Torres Strait Islanders The Torres Strait Islanders, Australia’s second Indigenous minority, come from the islands of the sea passage between Queensland and New Guinea. Estimated to number at most 4,000 people before contact, but reduced by half by disease and depredation by the late-1870s, they now number more than 40,000. Traditional stories recount their arrival in waves of chain migration from various islands and coastal villages of southern New Guinea, possibly as a consequence of environmental change.1 The Islanders were not traditionally unified, but recognised five major ethno-linguistic groups or ‘nations’, each specialising in the activities best suited to its environment: the Miriam Le of the fertile, volcanic islands of the east; the Kulkalgal of the sandy coral cays of the centre; the Saibailgal of the low mud-flat islands close to the New Guinea coast; the Maluilgal of the grassy, hilly islands of the centre west; and the Kaurareg of the low west, who for centuries had intermarried with Cape York Aboriginal people. They spoke dialects of two traditional but unrelated languages: in the east, Papuan Meriam Mir; in the west and centre, Australian Kala Lagaw Ya (formerly called Mabuiag); and they used a sophisticated sign language to communicate with other language speakers. Outliers of a broad Melanesian culture area, they lived in small-scale, acephalous, clan-based communities and traded, waged war and intermarried with their neighbours and the peoples of the adjacent northern and southern mainlands. -
Torres Strait Regional Economic Investment Strategy, 2015-2018 Phase 1: Regional Business Development Strategy
Page 1 Torres Strait Regional Economic Investment Strategy, 2015-2018 Phase 1: Regional Business Development Strategy A Framework for Facilitating Commercially-viable Business Opportunities in the Torres Strait September 2015 Page 2 This report has been prepared on behalf of the Torres Strait Regional Authority (TSRA). It has been prepared by: SC Lennon & Associates Pty Ltd ACN 109 471 936 ABN 74 716 136 132 PO Box 45 The Gap Queensland 4061 p: (07) 3312 2375 m: 0410 550 272 e: [email protected] w: www.sashalennon.com.au and Workplace Edge Pty Ltd PO Box 437 Clayfield Queensland 4011 p (07) 3831 7767 m 0408 456 632 e: [email protected] w: www.workplaceedge.com.au Disclaimer This report was prepared by SC Lennon & Associates Pty Ltd and Workplace Edge Pty Ltd on behalf of the Torres Strait Regional Authority (TSRA). It has been prepared on the understanding that users exercise their own skill and care with respect to its use and interpretation. Any representation, statement, opinion or advice expressed or implied in this publication is made in good faith. SC Lennon & Associates Pty Ltd, Workplace Edge Pty Ltd and the authors of this report are not liable to any person or entity taking or not taking action in respect of any representation, statement, opinion or advice referred to above. Photo image sources: © SC Lennon & Associates Pty Ltd Page 3 TABLE OF CONTENTS EXECUTIVE SUMMARY A New Approach to Enterprise Assistance in the Torres Strait i A Plan of Action i Recognising the Torres Strait Region’s Unique Challenges ii -
Cultural Heritage Series
VOLUME 4 PART 2 MEMOIRS OF THE QUEENSLAND MUSEUM CULTURAL HERITAGE SERIES 17 OCTOBER 2008 © The State of Queensland (Queensland Museum) 2008 PO Box 3300, South Brisbane 4101, Australia Phone 06 7 3840 7555 Fax 06 7 3846 1226 Email [email protected] Website www.qm.qld.gov.au National Library of Australia card number ISSN 1440-4788 NOTE Papers published in this volume and in all previous volumes of the Memoirs of the Queensland Museum may be reproduced for scientific research, individual study or other educational purposes. Properly acknowledged quotations may be made but queries regarding the republication of any papers should be addressed to the Editor in Chief. Copies of the journal can be purchased from the Queensland Museum Shop. A Guide to Authors is displayed at the Queensland Museum web site A Queensland Government Project Typeset at the Queensland Museum CHAPTER 4 HISTORICAL MUA ANNA SHNUKAL Shnukal, A. 2008 10 17: Historical Mua. Memoirs of the Queensland Museum, Cultural Heritage Series 4(2): 61-205. Brisbane. ISSN 1440-4788. As a consequence of their different origins, populations, legal status, administrations and rates of growth, the post-contact western and eastern Muan communities followed different historical trajectories. This chapter traces the history of Mua, linking events with the family connections which always existed but were down-played until the second half of the 20th century. There are four sections, each relating to a different period of Mua’s history. Each is historically contextualised and contains discussions on economy, administration, infrastructure, health, religion, education and population. Totalai, Dabu, Poid, Kubin, St Paul’s community, Port Lihou, church missions, Pacific Islanders, education, health, Torres Strait history, Mua (Banks Island). -
A Synthesis of Climate Change and Coastal Science to Support Adaptation in the Communities of the Torres Strait
MTSRF Synthesis Report A Synthesis of Climate Change and Coastal Science to Support Adaptation in the Communities of the Torres Strait Stephanie J. Duce, Kevin E. Parnell, Scott G. Smithers and Karen E. McNamara School of Earth and Environmental Sciences, James Cook University Supported by the Australian Government’s Marine and Tropical Sciences Research Facility Project 1.3.1 Traditional knowledge systems and climate change in the Torres Strait © James Cook University ISBN 978-1-921359-53-8 This report should be cited as: Duce, S.J., Parnell, K.E., Smithers, S.G. and McNamara, K.E. (2010) A Synthesis of Climate Change and Coastal Science to Support Adaptation in the Communities of the Torres Strait. Synthesis Report prepared for the Marine and Tropical Sciences Research Facility (MTSRF). Reef & Rainforest Research Centre Limited, Cairns (64pp.). Published by the Reef and Rainforest Research Centre on behalf of the Australian Government’s Marine and Tropical Sciences Research Facility. The Australian Government’s Marine and Tropical Sciences Research Facility (MTSRF) supports world-class, public good research. The MTSRF is a major initiative of the Australian Government, designed to ensure that Australia’s environmental challenges are addressed in an innovative, collaborative and sustainable way. The MTSRF investment is managed by the Department of the Environment, Water, Heritage and the Arts (DEWHA), and is supplemented by substantial cash and in-kind investments from research providers and interested third parties. The Reef and Rainforest Research Centre Limited (RRRC) is contracted by DEWHA to provide program management and communications services for the MTSRF. This publication is copyright. -
Erosion and Accretion on a Mudflat: the Importance of Very 10.1002/2016JC012316 Shallow-Water Effects
PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE Erosion and Accretion on a Mudflat: The Importance of Very 10.1002/2016JC012316 Shallow-Water Effects Key Points: Benwei Shi1,2 , James R. Cooper3 , Paula D. Pratolongo4 , Shu Gao5 , T. J. Bouma6 , Very shallow water accounted for Gaocong Li1 , Chunyan Li2 , S.L. Yang5 , and YaPing Wang1,5 only 11% of the duration of the entire tidal cycle, but accounted for 1Ministry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing, China, 2Department 35% of bed-level changes 3 Erosion and accretion during very of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, LA, USA, Department of Geography and 4 shallow water stages cannot be Planning, School of Environmental Sciences, University of Liverpool, Liverpool, UK, CONICET – Instituto Argentino de neglected when modeling Oceanografıa, CC 804, Bahıa Blanca, Argentina, 5State Key Laboratory of Estuarine and Coastal Research, East China morphodynamic processes Normal University, Shanghai, China, 6NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and This study can improve our understanding of morphological Delta Systems, and Utrecht University, Yerseke, The Netherlands changes of intertidal mudflats within an entire tidal cycle Abstract Understanding erosion and accretion dynamics during an entire tidal cycle is important for Correspondence to: assessing their impacts on the habitats of biological communities and the long-term morphological Y. P. Wang, evolution of intertidal mudflats. However, previous studies often omitted erosion and accretion during very [email protected] shallow-water stages (VSWS, water depths < 0.20 m). It is during these VSWS that bottom friction becomes relatively strong and thus erosion and accretion dynamics are likely to differ from those during deeper Citation: flows. -
The Contribution of Wind-Generated Waves to Coastal Sea-Level Changes
1 Surveys in Geophysics Archimer November 2011, Volume 40, Issue 6, Pages 1563-1601 https://doi.org/10.1007/s10712-019-09557-5 https://archimer.ifremer.fr https://archimer.ifremer.fr/doc/00509/62046/ The Contribution of Wind-Generated Waves to Coastal Sea-Level Changes Dodet Guillaume 1, *, Melet Angélique 2, Ardhuin Fabrice 6, Bertin Xavier 3, Idier Déborah 4, Almar Rafael 5 1 UMR 6253 LOPSCNRS-Ifremer-IRD-Univiversity of Brest BrestPlouzané, France 2 Mercator OceanRamonville Saint Agne, France 3 UMR 7266 LIENSs, CNRS - La Rochelle UniversityLa Rochelle, France 4 BRGMOrléans Cédex, France 5 UMR 5566 LEGOSToulouse Cédex 9, France *Corresponding author : Guillaume Dodet, email address : [email protected] Abstract : Surface gravity waves generated by winds are ubiquitous on our oceans and play a primordial role in the dynamics of the ocean–land–atmosphere interfaces. In particular, wind-generated waves cause fluctuations of the sea level at the coast over timescales from a few seconds (individual wave runup) to a few hours (wave-induced setup). These wave-induced processes are of major importance for coastal management as they add up to tides and atmospheric surges during storm events and enhance coastal flooding and erosion. Changes in the atmospheric circulation associated with natural climate cycles or caused by increasing greenhouse gas emissions affect the wave conditions worldwide, which may drive significant changes in the wave-induced coastal hydrodynamics. Since sea-level rise represents a major challenge for sustainable coastal management, particularly in low-lying coastal areas and/or along densely urbanized coastlines, understanding the contribution of wind-generated waves to the long-term budget of coastal sea-level changes is therefore of major importance. -
Shoreline Stabilisation
Section 5 SHORELINE STABILISATION 5.1 Overview of Options Options for handling beach erosion along the western segment of Shelley Beach include: • Do Nothing – which implies letting nature take its course; • Beach Nourishment – place or pump sand on the beach to restore a beach; • Wave Dissipating Seawall – construct a wave dissipating seawall in front of or in lieu of the vertical wall so that wave energy is absorbed and complete protection is provided to the boatsheds and bathing boxes behind the wall for a 50 year planning period; • Groyne – construct a groyne, somewhere to the east of Campbells Road to prevent sand from the western part of Shelley Beach being lost to the eastern part of Shelley Beach; • Offshore Breakwater – construct a breakwater parallel to the shoreline and seaward of the existing jetties to dissipate wave energy before it reaches the beach; and • Combinations of the above. 5.2 Do Nothing There is no reason to believe that the erosion process that has occurred over at least the last 50 years, at the western end of Shelley Beach, will diminish. If the water depth over the nearshore bank has deepened, as it appears visually from aerial photographs, the wave heights and erosive forces may in fact increase. Therefore “Do Nothing” implies that erosion will continue, more structures will be threatened and ultimately damaged, and the timber vertical wall become undermined and fail, exposing the structures behind the wall to wave forces. The cliffs behind the wall will be subjected to wave forces and will be undermined if they are not founded on solid rock. -
Malaysian Journal of Civil Engineering 27 Special Issue (2):325-336 (2015)
Malaysian Journal of Civil Engineering 27 Special Issue (2):325-336 (2015) EVALUATION OF THE WATER AGE IN THE WESTERN PART OF JOHOR STRAIT, MALAYSIA Ziba Kazemi*, Noor Baharim Hashim, Hossein Aslani & Khairul Anuar Mohamad 1 Faculty of Civil Engineering, Universiti Teknologi Malaysia, 81310, Skudai, Johor Bahru, Malaysia *Corresponding Author: [email protected] Abstract: The age of water is useful for understanding the fundamental mechanisms controlling the flux of substances through an estuary. Furthermore, this variable is useful indicators of the susceptibility of estuaries to eutrophication. In this paper, an application of a three-dimensional hydrodynamic model used to evaluate water age distributions for a range of inflow conditions in the Western Part of Strait of Johor, Malaysia. As a first step, the three dimensional hydrodynamic model EFDC was calibrated and then used to evaluate the spatial distribution of water age. Numerical simulations were completed under different inflow conditions. The analysis suggested considerable spatial variation in the water age under both low and high-flow conditions. The average water age in entire system is maximum 14 days under minimum inflow, 194.4 m3/s and minimum 4 days under maximum inflow, 541.3 m3/s. This analysis helped in recognition of areas of the estuary most vulnerable to oxygen depletion and eutrophication. Keywords: Water age, EFDC, hydrodynamic modeling, estuary, Johor Strait. 1.0 Introduction Estuaries are coastal area where freshwater from rivers and streams mixes with saltwater from ocean and are thus characterized by a variety of complicated and complex processes (Michaelis, 1990). One significant and typical estuarine phenomenon is the mixing zone between the saline water and freshwater.