Farewell to the Carteret Islands”
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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. -
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. -
To View More Samplers Click Here
This sampler file contains various sample pages from the product. Sample pages will often include: the title page, an index, and other pages of interest. This sample is fully searchable (read Search Tips) but is not FASTFIND enabled. To view more samplers click here www.gould.com.au www.archivecdbooks.com.au · The widest range of Australian, English, · Over 1600 rare Australian and New Zealand Irish, Scottish and European resources books on fully searchable CD-ROM · 11000 products to help with your research · Over 3000 worldwide · A complete range of Genealogy software · Including: Government and Police 5000 data CDs from numerous countries gazettes, Electoral Rolls, Post Office and Specialist Directories, War records, Regional Subscribe to our weekly email newsletter histories etc. FOLLOW US ON TWITTER AND FACEBOOK www.unlockthepast.com.au · Promoting History, Genealogy and Heritage in Australia and New Zealand · A major events resource · regional and major roadshows, seminars, conferences, expos · A major go-to site for resources www.familyphotobook.com.au · free information and content, www.worldvitalrecords.com.au newsletters and blogs, speaker · Free software download to create biographies, topic details · 50 million Australasian records professional looking personal photo books, · Includes a team of expert speakers, writers, · 1 billion records world wide calendars and more organisations and commercial partners · low subscriptions · FREE content daily and some permanently This sampler file includes the title page, index and various sample pages from this volume. This file is fully searchable (read search tips page) Archive CD Books Australia exists to make reproductions of old books, documents and maps available on CD to genealogists and historians, and to co-operate with family history societies, libraries, museums and record offices to scan and digitise their collections for free, and to assist with renovation of old books in their collection. -
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. -
Comparing the Role of Absolute Sea-Level Rise and Vertical Tectonic Motions in Coastal Flooding, Torres Islands (Vanuatu), V
Comparing the role of absolute sea-level rise and vertical tectonic motions in coastal flooding, Torres Islands (Vanuatu), V. Ballu, Marie-Noëlle Bouin, Patricia Simeoni, Wayne Crawford, Stéphane Calmant, Jean-Michel Bore, Tony Kanas, Bernard Pelletier To cite this version: V. Ballu, Marie-Noëlle Bouin, Patricia Simeoni, Wayne Crawford, Stéphane Calmant, et al.. Com- paring the role of absolute sea-level rise and vertical tectonic motions in coastal flooding, Torres Islands (Vanuatu),. Proceedings of the National Academy of Sciences of the United States of America , National Academy of Sciences, 2011, 108 (32), pp.13019-13022. 10.1073/pnas.1102842108. hal- 00812620 HAL Id: hal-00812620 https://hal.archives-ouvertes.fr/hal-00812620 Submitted on 22 Apr 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. Comparing the role of absolute sea-level rise and vertical tectonic motions in coastal flooding, Torres Islands (Vanuatu) Valérie Ballua,b,1, Marie-Noëlle Bouinc, Patricia Siméonid, Wayne C. Crawforda,b, Stephane Calmante, Jean-Michel Boréf, Tony Kanasg, and Bernard Pelletiera,f aGéoazur, Unité Mixte de Recherche 6526, Institut de Recherche pour le Developpement, Port Vila, Vanuatu; bInstitut de Physique du Globe—Sorbonne Paris Cité, Université Paris Diderot, Unité Mixte de Recherche, Centre National de la Recherche Scientifique 7154, 1 rue Cuvier, 75238 Paris Cedex 05, France; cCentre National de Recherches Météorologiques, Météo France. -
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. -
TORBA Provincial Disaster & Climate Response Plan
PROVINCIAL GOVERNMENT COUNCIL PROVINCIAL GOVERNMENT NATIONAL DISASTER MANAGEMENT OFFICE NATIONAL TORBA ADVISORY BOARD Provincial Disaster & Climate ON CC & DRR Response Plan 2016 Province of TORBA – 2016 PLAN AUTHORIZATION This Plan has been prepared by TORBA Provincial Government Councils in pursuance of Section 11(1) of the National Disaster Act of 2000 and the National Climate Change & Disaster Risk Reduction Policy. ENDORSED BY: _______________________ Date: / / 2016 Mr. Judas Silas Chairperson Provincial Disaster & Climate Change Committee This Plan is approved in accordance with Section 11(2) of the National Disaster Act 2000 and is in-line with the National Climate Change & Disaster Risk Reduction Policy 2015-2030. APPROVED BY: ___________________ Date: / / 2016 Mr. Shadrack Welegtabit Director National Disaster Management Office Ministry Of Climate Change and Disasters ___________________ Date: / / 2016 Mr. David Gibson Director VMGD Office Ministry Of Climate Change and Disasters ___________________ Date: / / 2016 Ms Anna Bule Secretariat National Advisory Board on Climate Change & Disaster Risk Reduction ___________________ Date: / / 2016 Ms Ketty Napwatt Secretary General TORBA Provincial Government i | Province of TORBA – 2016 PREFACE Disaster Risk Management (DRM) Provincial level is a dynamic process. In order to adequately respond to disasters, there must be a comprehensive and coordinated approach between national, provincial and community levels. This plan has been developed to provide guidelines on how to manage different risks in the province, taking into account the effects of the climate change that increase the strength of the hazard and potential impacts of future disasters. This Provincial Disaster & Climate Response Plan provides directive to all agencies on the conduct of Disaster Preparedness and Emergency operations. -
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. -
Monthly Catalogue, United States Public Documents, July 1914
Monthly Catalogue United States Public Documents Nos. 235-246 July, 1914-June, 1915 ISSUED BY THE SUPERINTENDENT OF DOCUMENTS WASHINGTON 1914-1915 Monthly Catalogue United States Public Documents No. 235 July, 1914 ISSUED BY THE SUPERINTENDENT OF DOCUMENTS WASHINGTON 1914 Abbreviations Appendix......................................................app. Part, parts...............................................pt., pts. Congress............... Cong. Plate, plates..................................................... pl. Department.................................................Dept. Portrait, portraits.......................................... por. Document......................................................doc. Quarto.............................................. 4- Facsimile, facsimiles...................................facsim. Report.............................................................rp. Folio................................................................. f° Saint................................................................St. House.............................................................. H. Section, sections.............................................. seo. House concurrent resolution.....................H. C. R. Senate............................................................... S. House document........................................H. doc. Senate concurrent resolution.................... S. C. R. House executive document...................H. ex. doc. Senate document....................................... S. -
HEAVY MINERAL CONCENTRATION in a MARINE SEDIMENT TRANSPORT CONDUIT, BERING STRAIT, ALASKA by James C
Alaska Division of Geological & Geophysical Surveys PRELIMINARY INTERPRETIVE REPORT 2016-4 HEAVY MINERAL CONCENTRATION IN A MARINE SEDIMENT TRANSPORT CONDUIT, BERING STRAIT, ALASKA by James C. Barker, John J. Kelley, and Sathy Naidu June 2016 Released by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES Division of Geological & Geophysical Surveys 3354 College Rd., Fairbanks, Alaska 99709-3707 Phone: (907) 451-5010 Fax (907) 451-5050 [email protected] www.dggs.alaska.gov $3.00 Contents INTRODUCTION .................................................................................................................................................. 1 REGIONAL SETTING ............................................................................................................................................ 2 MATERIALS AND METHODS ................................................................................................................................ 3 RESULTS .............................................................................................................................................................. 5 Heavy Mineral Deposition in the Bering Strait Area .................................................................................... 5 Heavy Mineral Composition ......................................................................................................................... 8 Mineralogy .................................................................................................................................................. -
VII the Eastern Islands (Nuguria, Tauu and Nukumanu)
THE EASTERN ISLANDS (NUGURIA, TAUU AND NUKUMANU) VII The Eastern Islands (Nuguria, Tauu and Nukumanu) ast of the large Melanesian islands extends a For years the population has been in the process Elong chain of small islands, mostly raised of dying out. The current number is about fifteen. coral reefs or atolls, belonging geographically to In 1902 alone, sixteen died, particularly as a result Melanesia, but occupying a quite special position of influenza. The natives’ physical resistance seems ethnographically. to be very low, and it will not be many more years Three of these small atolls, Nuguria, Tauu and before none of the present population exists. In Nukumanu, have been annexed by the German 1885 when I first visited this small group I esti- protectorate. A fourth group, Liueniua or Ong mated the population to be at least 160 people. tong Java, by far the most significant, was Ger - Tauu, pronounced Tau’u’u (Mortlock or Mar- man for a time but then by treaty passed into queen Islands; Dr Thilenius names it incorrectly as English hands. Taguu), is likewise an atoll structure. It lies at ap- Although the three German groups are of no proximately 157ºE longitude and 4º50’S latitude, great interest commercially and probably never and the total land area of the islands is no greater will be, ethnographically they are of no small im- than 200 hectares. The distance from Nuguria is portance because in spite of being in a Melanesian about 150 nautical miles. The nearest point in the neighbourhood, they are inhabited by Polynesians.