DOCSLIB.ORG

Tuvalu - Funafuti 2021 Tide Predictions Calendar Climate and Oceans Support Program in the Pacific

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Tuvalu - Funafuti 2021 Tide Predictions Calendar Climate and Oceans Support Program in the Pacific Tuvalu - Funafuti 2021 Tide Predictions Calendar Climate and Oceans Support Program in the Pacific A Pacific Islands Program supported by the Australian Government Tuvalu - Funafuti Paara Fualefeke Mulitefala Te Afualiku Amatuku Tengako Tepuka Tide Gauge Location Fualopa Fualopa Fuafatu Fongafale Te Namo Fatato Vasafua Funamanu Papa Elise Fuagea Fale Fatu Tefala Mateiko Falaolgo Funafala FUNAFUTI Tutanga Tengasu Tefota Teafuafou Telele Awalau Motuloa Motugie Meteorological and seasonal effects 10 highest tides for 2021 10 lowest tides for 2021 Tide predictions are based on the effects Date Time Height (m) Date Time Height (m) of the gravitational forces exerted by the 28-Apr 5:30 3.21 5-Nov 23:22 1.02 moon, the sun, and the rotation of the earth, as well as average seasonal changes. 29-Mar 17:31 3.2 24-Jul 11:24 1.03 The actual tide height will be a combination 27-Apr 4:49 3.19 4-Dec 23:13 1.03 of these effects and the weather conditions 28-May 16:52 3.19 25-Jun 11:33 1.04 at the time. The effects of the weather are not included in tide predictions. 28-Feb 17:53 3.19 27-May 11:39 1.04 30-Mar 5:53 3.18 4-Nov 22:38 1.04 4-Dec 16:46 3.18 26-May 10:50 1.04 5-Nov 17:01 3.17 7-Oct 11:15 1.04 Map courtesy of the Pacific Community. Some rights reserved. 27-Feb 17:15 3.17 27-Apr 11:04 1.05 Front cover photo courtesy of Gary Lee. 5-Dec 17:34 3.15 25-Jul 12:07 1.05 Some rights reserved. Tides and Extreme Tide Events What causes tides? What are king tides? Tides are the daily rise and fall of sea levels, caused The term king tide is commonly used to describe an mainly by the gravitational pull of the moon as it revolves especially high spring tide. King tides occur a few times around the earth. Tides are also affected by the earth’s every year, when the gravitational pull of the sun and rotation and the gravitational pull of the sun. moon upon the earth is strongest. This happens when the moon is closest to the earth in its monthly orbit. When this coincides with a spring tide, it will produce an especially high tide, or king tide. In the Pacific, the highest king tides often occur during the months from November to March, when the earth is also closest to the sun in its annual orbit. What do I need to know about king tides? King tides are a natural part of the tidal cycle and are Figure 1. Low and high tide in Suva, Fiji. Photo: Molly Powers-Tora (201 8). predictable. A king tide can cause coastal flooding, even on a clear, sunny day. What are spring tides and neap tides? When king tides coincide with cyclones, floods or storms, water levels can rise significantly, potentially Spring and neap tides are part of the normal tidal cycle causing damage to property and the coastline. The and occur regularly, usually twice per month. actual height reached by a king tide will depend on the Spring tides are very high tides and very low tides that local weather and ocean conditions on the day. occur during full and new moon phases, when the It is also important to know that king tides have always gravitational forces of the sun and moon combine to occurred and are not a result of sea level rise. exert a stronger pull on the oceans. During the moon’s quarter phases each month, the sun and moon are at right angles, and the gravitational forces cancel each other out, resulting in lower high tides and higher low tides called neap tides. Figure 3. Strong southeasterly winds and currents combine to create higher than normal tides in Levuka, Fiji. Photo: Molly Powers-Tora (2013). Figure 2. Spring and neap tides occur every month and correspond with the phases of the moon. Source: www.moononly.com Climate and Oceans Support program in the Pacific Tides and Extreme Tide Events How are tides predicted? Why are some tides higher or lower The time and approximate heights of tides are very than predicted? predictable. They follow the laws of physics and can be Tide levels can vary from predicted levels for a number of calculated with mathematical formulas. reasons, including: By observing and recording tides at a single location over 1. Geography: The shape of bays and other coastal many years, we can gain a better understanding of tides geography can magnify or otherwise influence water and sea level changes over time. levels. The Pacific Sea Level and Geodetic Monitoring Project 2. Weather: Wind speed and direction, air temperature, has been recording sea level and weather statistics at barometric pressure and other weather conditions can 13 Pacific countries for more than 25 years. greatly affect water levels. These observations tell a story about the sea levels at 3. Waves: Both nearby and faraway events such as these locations, such as: How high was the highest tide storms, landslides and earthquakes can create large in Apia? What effect does El Niño have on sea levels in waves that lead to coastal flooding. Kiribati? All of this information is also used to verify and 4. Climate drivers: El Niño or La Niña conditions in the improve tide predictions. Pacific can raise or lower sea level by as much as 50 cm. 5. Sea-level rise: Through assessing observations and research, the Intergovernmental Panel on Climate Change (IPCC) concluded that global average sea levels have been rising at a rate of about 3 mm per year since 1993. Levels were 225 mm higher in 2012 compared to 1880. Sea-level rise can contribute to higher tides, but the rates are not the same at all locations. Figure 4. Technicians working on the recently-refurbished Cook Figure 5. Predicted vs actual sea level at the Apia tide gauge Islands tide gauge, which has been monitoring sea level and Samoa, 3 May 2018. weather conditions in Rarotonga for over 25 years. Photo: Stamy Criticos (2012). The Pacific Sea Level and Geodetic Monitoring Project provides sea level and meteorological information for 13 countries and tide predictions for 20 locations in the Pacific region. It is an important resource for those involved in disaster mitigation and adaptation planning, coastal development, and the shipping, fishing and tourism industries. To access tide calendars, wave and weather maps, and climate data for your location visit: www.bom.gov.au/pacific/index.shtml For Real-Time Display of tide gauge data, visit: http://www.bom.gov.au/cosppac/rtdd/q1c7o0hj48yu/ © Commonwealth of Australia 2014 0047 1.08 0134 1.08 0220 1.09 6 0635 0.56 7 0724 0.57 8 0815 0.57 9 1248 1.14 1337 1.13 1425 1.12 Tides and Sea Level 1919for 0.50 Coastal2006 0.50 2051 0.51 1.5m Development and1m Safe Navigation 0.5m What is a Tide Datum? 0 6 12 18 0 6 12 18 0 6 12 18 0 A Tide Datum is a fixed level against which sea level 0552 1.23 0020 0.45 0114 0.42 can be measured in a given location. A tide station 13 1212 0.44 14 0642 1.28 15 0733 1.33 16 datum was established when the sea level monitoring 1815 1.19 1304 0.38 1400 0.34 1908 1.21 2003 1.23 station featured in this calendar was first installed. The MSL tide predictions in this calendar are all relative to Tide Prediction Datum. 1.5m NEAP RANGE SPRING RANGE Why do we need a Tide Datum? 1m Tide records must be referenced to a common datum 0.5m to ensure consistency. This is important if the tide CHARTED CD DEPTH gauges are moved or in the event they are damaged or 0 6 12 18 0 6 12 18 0 6 12 18 0 destroyed. In this case, tide readings from replacement gauges can be referenced to the same datum as Figure 1. How0000 does THIS............. 1.24 relate0100 to THIS? 1.24 0158 1.24 before and continue to contribute to our understanding 20 0603 0.40 21 0704 0.41 22 0805 0.42 23 of tides. 1220 1.32 1321 1.29 1423 1.27 1846 0.31 1945 0.33 2043 0.35 What is the relationship between tides 1.5mand sea level? 1mWhen the range of highest and lowest tides are averaged over a long period (usually at least 19 years), we can establish 0.5mMean Sea Level. Mean Sea Level (MSL) is an important reference level, as all heights on land are measured in metres or 0feet above 6 12 mean18 sea level 0 as 6 in Figu12 re 182. 0 6 12 18 0 All sea level monitoring stations are tide gauges, but not all 0007 0.44 0054 0.46 0139 0.47 tide 27gauges 0625can accurately 1.24 28 measu0711re changes 1.24 in 29sea level.0755 1.22 30 The Pacific 1248Sea Level 0.41 and Geodetic1336 Monitoring 0.41 stations1422 0.40 include specialised1857 1.16weather, ocean,1943 and 1.13land monitoring2027 1.11 sensors that have been operating since 1991, allowing us to measure the extent to which sea level is affected by natural 1.5m Figure 2. An elevation sign from Tarawa, Kiribati variability and man-made climate change at those locations. Photo: Wandering Ken, 2011.
Load more

Recommended publications
  • 2017 Tuvalu Mini CPH Form 3
    Generated by winston, Apr 09, 2019 16:09 Sections: 4, Sub-sections: 17, Questionnaire created by togar, Mar 04, 2019 14:56 Questions: 209. Last modified by togar, Mar 04, 2019 14:56 Questions with enabling conditions: 123 Questions with validation conditions:66 Shared with: Rosters: 10 luisr (never edited) Variables: 3 winston (never edited) 2017 Tuvalu Mini CPH Form 3 SURVEY IDENTIFICATION INFORMATION QUESTIONNAIRE DESCRIPTION IDENTIFICATION No sub-sections, No rosters, Questions: 21, Static texts: 1. HOUSEHOLD No sub-sections, Rosters: 6, Questions: 71, Static texts: 1. PERSON Sub-sections: 17, Rosters: 4, Questions: 110, Static texts: 4, Variables: 3. ENDING No sub-sections, No rosters, Questions: 7. APPENDIX A — ENABLING CONDITIONS APPENDIX B — VALIDATION CONDITIONS AND MESSAGES APPENDIX C — INSTRUCTIONS APPENDIX D — CATEGORIES APPENDIX E — CATEGORIES FILTERS LEGEND 1 / 49 SURVEY IDENTIFICATION INFORMATION QUESTIONNAIRE DESCRIPTION Basic information Title 2017 Tuvalu Mini CPH Form 3 SURVEY IDENTIFICATION INFORMATION QUESTIONNAIRE DESCRIPTION 2 / 49 IDENTIFICATION C1. CENSUS ID TEXT censusID SCOPE: IDENTIFYING E1 $censIdOk M1 The Census ID entered is invalid. Please double check the entered valu es match the Census ID in CPH Form 1. C2. ISLAND SINGLE-SELECT: COMBO BOX Island_code SCOPE: IDENTIFYING E1 ((censusID.ToLower().Left(1) == "x" && self == 0)?true:f 00 Test Island alse) || ((censusID.ToLower().Left(1) == "a" && self == 1)?true:false) || ((censusID.ToLower().Left(1) == "b" && 01 Nanumea self == 2)?true:false) || (( And 457 other symbols [1] 02 Nanumaga M1 The Island entered is not associated with the Census ID. 03 Niutao 04 Nui 05 Vaitupu 06 Nukufetau 07 Funafuti 08 Nukulaelae 09 Niulakita STATIC TEXT Census ID: %censusID% C3.
    [Show full text]
  • Towards Fatele Theology: a Contextual Theological Response in Addressing Threats of Global Warming in Tuvalu
    Towards Fatele Theology: A Contextual Theological Response in Addressing Threats of Global Warming in Tuvalu A Thesis Submitted to the Faculty of Theology In Partial Fulfillment of the Requirements For The Degree of Master of Theology By Maina Talia Advisor: Prof, Dr. M.P. Joseph Tainan Theological College and Seminary Tainan, Taiwan May 2009 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 2009 Maina Talia ALL RIGHTS RESERVED ! ! ! ! ! ! This thesis is dedicated to the followings: My parents Talia Maina Salasopa and the late Lise Moeafu Talia, OBE. Mum, your fatele’s will remains as living text for the Tuvaluan generations in their search for the presence of the Divine. And my grandma Silaati Telito, in celebrating her 90th Birthday. ! ! i ACKNOWLEDGEMENT “So you also, when you have done everything you were told to do, should say, ‘We are unworthy servants; we have only done our duty.” (Luke 17:10) The completion of this thesis is not an individual achievement. Without the help of many, it would never have come to a final form. Because I was not endorsed by the Ekalesia Kelisiano Tuvalu, it remains dear to me. Rev. Samuelu Tialavea Sr the General Secretary of the Congregational Christian Church in American Samoa (CCCAS) offered his church’s sponsorship. I owe a big fa’afetai tele to the CCCAS and the Council for World Mission for granting me a scholarship. Fakafetai lasi kii to my thesis advisor Prof, Dr. M.P. Joseph great theologian, who helped me through the process of writing, especially giving his time for discussion. His constructive advice and words of encouragement contributed in many ways to the formation of fatele theology.
    [Show full text]
  • The Project for Pilot Gravel Beach Nourishment Against Coastal Disaster on Fongafale Island in Tuvalu
    MINISTRY OF FOREIGN AFFAIRS, TRADES, TOURISM, ENVIRONMENT AND LABOUR THE GOVERNMENT OF TUVALU THE PROJECT FOR PILOT GRAVEL BEACH NOURISHMENT AGAINST COASTAL DISASTER ON FONGAFALE ISLAND IN TUVALU FINAL REPORT (SUPPORTING REPORT) April 2018 JAPAN INTERNATIONAL COOPERATION AGENCY NIPPON KOEI CO., LTD. FUTABA INC. GE JR 18-058 MINISTRY OF FOREIGN AFFAIRS, TRADES, TOURISM, ENVIRONMENT AND LABOUR THE GOVERNMENT OF TUVALU THE PROJECT FOR PILOT GRAVEL BEACH NOURISHMENT AGAINST COASTAL DISASTER ON FONGAFALE ISLAND IN TUVALU FINAL REPORT (SUPPORTING REPORT) April 2018 JAPAN INTERNATIONAL COOPERATION AGENCY NIPPON KOEI CO., LTD. FUTABA INC. Table of Contents Supporting Report-1 Study on the Quality and Quantity of Materials in Phase-1 (quote from Interim Report 1) .............................................................. SR-1 Supporting Report-2 Planning and Design in Phase-1 (quote from Interim Report 1) ............ SR-2 Supporting Report-3 Design Drawing ..................................................................................... SR-3 Supporting Report-4 Project Implementation Plan in Phase-1 (quote from Interim Report 1)................................................................................................. SR-4 Supporting Report-5 Preliminary Environmental Assessment Report (PEAR) ....................... SR-5 Supporting Report-6 Public Consultation in Phase-1 (quote from Interim Report 1) .............. SR-6 Supporting Report-7 Bidding Process (quote from Progress Report) ...................................... SR-7 Supporting
    [Show full text]
  • Coastal Erosion and Management of Amatuku Island, Funafuti Atoll, Tuvalu
    COASTAL EROSION AND MANAGEMENT OF AMATUKU ISLAND, FUNAFUTI ATOLL, TUVALU Chunting Xue SOPAC Secretariat August 1996 SOPAC Technical Report 234 This project was funded by the Government of the People's Republic of China [3] TABLE OF CONTENTS Page SUMMARY.................................................................................................................................. 6 ACKNOWLEDGMENTS............................................................................................................. 7 INTRODUCTION........................................................................................................................ 7 STUDY METHODS .................................................................................................................. 11 DEVELOPMENT HISTORY ..................................................................................................... 11 REEF FLAT AND BEACH........................................................................................................ 12 COASTAL EROSION............................................................................................................... 19 BORROW PIT AND CHANNEL ............................................................................................... 27 COASTAL MANAGEMENT ....................................................................................................... 31 CONCLUSIONS ....................................................................................................................... 31 RECOMMENDATIONS
    [Show full text]
  • Terminal Evaluation of the Global Environment Facility/UN
    Terminal Evaluation of the Global Environment Facility/UN Environment Project Low Carbon-Energy Islands: Accelerating the Use of Energy Efficient and Renewable Energy Technologies in Tuvalu, Niue and Nauru Final Report Evaluation Office of UN Environment March 2018 Evaluation Office of UN Environment Photos Credits: Front cover: Alfredo Caprile Team Leader, UN Environment Evaluation Mission (2017) Page 55: Sirikul Prasitpianchai, Support Consultant, UN Environment Evaluation Mission (2017) Page 57: Alfredo Caprile Team Leader, UN Environment Evaluation Mission (2017) This report has been prepared by Alfredo Caprile and Sirikul Prasitpianchai and is a product of the Evaluation Office of UN Environment. The findings and conclusions expressed herein do not necessarily reflect the views of Member States or the UN Environment Senior Management. For further information on this report, please contact: Evaluation Office of UN Environment P. O. Box 30552-00100 GPO Nairobi Kenya Tel: (254-20) 762 3389 Email: [email protected] Project Title: Low Carbon-Energy Islands: Accelerating the Use of Energy Efficient and Renewable Energy GEF project ID 4000 Date 03/18 All rights reserved. © (2018) Evaluation Office of UN Environment ACKNOWLEDGEMENTS This Terminal evaluation was prepared for the Evaluation Office of UN Environment by Mr. Alfredo Caprile and Ms. Sirikul Prasitpianchai, Lead and Support Consultants. The authors would like to express their gratitude to all of the UN Environment and IUCN personnel and project participants that have been interviewed during the evaluation. Their comments and opinions with regard to the results and impacts that have been accomplished by the project have been critical for the preparation of this report.
    [Show full text]
  • The Biology and Geology of Tuvalu: an Annotated Bibliography
    ISSN 1031-8062 ISBN 0 7305 5592 5 The Biology and Geology of Tuvalu: an Annotated Bibliography K. A. Rodgers and Carol' Cant.-11 Technical Reports of the Australian Museu~ Number-t TECHNICAL REPORTS OF THE AUSTRALIAN MUSEUM Director: Technical Reports of the Australian Museum is D.J.G . Griffin a series of occasional papers which publishes Editor: bibliographies, catalogues, surveys, and data bases in J.K. Lowry the fields of anthropology, geology and zoology. The journal is an adjunct to Records of the Australian Assistant Editor: J.E. Hanley Museum and the Supplement series which publish original research in natural history. It is designed for Associate Editors: the quick dissemination of information at a moderate Anthropology: cost. The information is relevant to Australia, the R.J. Lampert South-west Pacific and the Indian Ocean area. Invertebrates: Submitted manuscripts are reviewed by external W.B. Rudman referees. A reasonable number of copies are distributed to scholarly institutions in Australia and Geology: around the world. F.L. Sutherland Submitted manuscripts should be addressed to the Vertebrates: Editor, Australian Museum, P.O. Box A285, Sydney A.E . Greer South, N.S.W. 2000, Australia. Manuscripts should preferably be on 51;4 inch diskettes in DOS format and ©Copyright Australian Museum, 1988 should include an original and two copies. No part of this publication may be reproduced without permission of the Editor. Technical Reports are not available through subscription. New issues will be announced in the Produced by the Australian Museum Records. Orders should be addressed to the Assistant 15 September 1988 Editor (Community Relations), Australian Museum, $16.00 bought at the Australian Museum P.O.
    [Show full text]
  • Pacific Islands
    THE PACIFIC ISLANDS POLITICS, ECONOMICS, AND INTERNATIONAL RELATIONS TE'O I.J. FAIRBAIRN CHARLES E. MORRISON RICHARD W. BAKER SHEREE A. GROVES THE PACIFIC ISLANDS THE EAST-WEST CENTER was established in Hawaii in 1960 by the United States Congress "to promote better relations and understand­ ing between the United States and the nations of Asia and the Pacific through cooperative study, training, and research:' Some 2,000 research fellows, graduate students, and professionals in business and government each year work with the Center's interna­ tional staff on major Asia-Pacific issues relating to population, economic and trade policies, resources and the environment, culture and com­ munication, and international relations. Since 1960, more than 27,000 men and women from the region have participated in the Center's cooperative programs. Officially known as the Center for Cultural and Technical Inter­ change Between East and West, Inc., the Center is a public, non-profit institution with an international board of governors. Principal funding comes from the United States Congress. Support also comes from more than twenty Asian and Pacific governments, as well as private agen­ cies and corporations. THE INTERNATIONAL RELATIONS PROGRAM (JRP) became an autonomous program within the East-West Center in 1989. The Program advances the Center's overall objectives through work on foreign poli­ cy and related political, economic, and security issues. Program pri­ orities are to 1) promote research and dialogue directed toward creating a stable, peaceful Asia/Pacific community; 2) identify issues in U.S. re­ lations with the Asia/Pacific region and recommend means of strength­ ening these relations; 3) improve understanding of individual societies of the region through cooperative research; and 4) promote contact and dialogue among the region's future leaders.
    [Show full text]
  • Transformations of the Meeting-House in Tuvalu
    Transformations of the meeting-house in Tuvalu Michael Goldsmith My problem is this: the Tuvaluan meeting-house is displayed as a symbol of indigenous culture in many different contexts. It is therefore often assumed, by both outside commentators and Tuvaluans themselves, to be of long standing in the history of that culture. Yet the word maneapa, by which the meeting-house is generically known, is of Gilbertese origin.1 Moreover, the weight of evidence suggests that not only the word but probably even the type of building itself is a post-colonial borrowing or implantation. If, indeed, there were no maneapa as such in Tuvalu before British hegemony was es­ tablished, then questions arise as to what, if anything, existed in its place; why the maneapa was introduced or borrowed; why it has achieved its current importance and, further, why it has become a symbol of national identity. In this connection, the concept of “transformation” calls out for a strong measure of historical attention. Yet the meaning of history is not as self-evident as the traditional definitions imply, with their references to narrative, sequences of events and so on (Braudel 1980:27). Another avenue, almost a new orthodoxy, has been explored under the influence of structuralism. Bather than using sequences of events to explain structure, some anthropologists use the delineation of structure to explain events. While Lêvi-Strauss’ name is the most closely linked to this programme (1966-.passim), even historical materialists find it beguiling. Godelier, for example, reverses the con­ ventional Marxist understanding of history with his contention that it explains nothing but is the category which itself needs to be explained, once structure has been revealed (Godelier 1977:49).
    [Show full text]
  • Speaker Presentation Session 3
    Innovative Solutions for Small-Island States Mafalu Lotolua Pacific Energy Summit Auckland, 7th June 2016 RE&EE Development in Tuvalu . Guided by the RE&EE Master Plan and is directly linked to the - Tuvalu National Sustainable Development Plan (Te Kakeega III), - the Climate Change Policy (Te Kaniva) and - the Tuvalu National Energy Policy. Master Plan has identified the most possible proven technologies for Tuvalu to meet its 100% target. RE&EE Master Plan . RE TARGET – 100% by 2025 . GOAL • To generate electricity with 100% renewable energy by 2025, and • To increase energy efficiency on Funafuti by 30% Implementation Strategies . 60 – 95% - Solar . 0 – 40% - Wind . 5% - Biodiesel . 30% - Energy Efficiency • Cannot achieve 100% renewable energy with ONE Renewable Energy source and need to include other potential PROVEN and MATURED technology, and • Energy Efficiency is also important to avoid additional renewable energy generation. Renewable Energy Portfolio No Island Technology Capacity % RE Development (kW) Partners 1 Funafuti Solar PV 750 17 NZ Govt, UAE and Japan 2 Vaitupu, Niutao, Solar PV 1,032 90 NZ Govt Nanumaga and Nanumea 3 Nukulaelae, Nukufetau Solar PV 188 50 EU and Nui 4 Amatuku, TMTI Solar PV 8 2 Finland 5 Niulakita and Funafala Solar PV 100 Italian Govt. SHS Partners involved in RE & EE Space in Tuvalu No Partners RE Technology/EE Capacity Site Status (kW) 1 NZ Govt. (MFAT) Solar PV mini-grid 3,032 + 170 Outer-islands/Funafuti Operational =3,202 2 EU Solar PV mini-grid 182 Outer islands Operational 3 United Arabs Solar
    [Show full text]
  • Diagnostic Report Tuvalu
    Sustainable Integrated Water Resources and Wastewater Management in Pacific Island Countries National Integrated Water Resource Management Diagnostic Report Tuvalu Published Date: November 2007 Draft SOPAC Miscellaneous Report 647 ACRONYMS AusAID Australian Agency for International Development EU European Union FAO Food and Agriculture Organization FFA Foreign Fisheries Agency GEF Global Environment Facility HYCOS Hydrological Cycle Observing System GPA Global Programme of Action for the Protection of Marine Environment form Land Based Activities IWRM Integrated Water Resources Management IWP International Waters Programme JICA Japanese International Cooperation Agency MPWE Ministry of Public Works and Energy MNRLE Ministry of Natural Resources, Lands and Environment FCA Funafuti Conservation Area FD Fisheries Department MDG Millennium Development Goals MPA Marine Protected Areas NAFICOT National Fishing Corporation of Tuvalu NTF National Task Force NEMS National Environment Management Strategy NZAID New Zealand Overseas Development Assistance PIC Pacific Island Countries PWD Public Works Division SAP Strategic Action Programme SOPAC Pacific Islands Applied Geoscience Commission SPREP South Pacific Regional Environment Programme TANGO Tuvalu Association for Non-Government Organisation UNDP United Nations Development Programme UNESCO United Nations Economic Social and Cultural Organisation USAID United States Agency for International Development WHO World Health Organization WSSD World Summit for Sustainable Development Sustainable Integrated
    [Show full text]
  • Sustainable Development for Tuvalu: a Reality Or an Illusion?
    SUSTAINABLE DEVELOPMENT FOR TUVALU: A REALITY OR AN ILLUSION? bY Petely Nivatui BA (University of the South Pacific) Submitted in partial fulfilment of the requirements for the degree of Master of Environmental Studies (Coursework) Centre for Environmental Studies University of Tasmania Hobart, Tasmania, Australia December 1991 DECLARATION This thesis contains no material that has been accepted for the award of any other higher degree or graduate diploma in any tertiary institution and, to the best of my knowledge and belief, contains no material previously published or written by another person, except when due reference is made in this thesis. Petely Nivatui ABSTRACT For development to be sustainable for Tuvalu it needs to be development which specifically sustains the needs of Tuvaluans economically, politically, ecologically and culturally without jeopardising and destroying the resources for future generations. Development needs to be of the kind which empowers Tuvaluans, gives security, self-reliance, self-esteem and respect. This is different from western perspectives which concentrate and involve a western style economy and money system in which money is the centre of everything. For Tuvaluans the economy is based on and dependent on land, coconut trees, pulaka (Cyrtosperma) and fish, as well as the exchange of these commodities. The aim of this thesis is to compare western and Tuvaluan concepts and practices of sustainable development in order to evaluate future possibilities of sustainable practices for Tuvalu. An atoll state like Tuvalu has many problems. The atolls are small, isolated, and poor in natural resources. Transport and communication are difficult and the environment is sensitive. Tuvalu is classified by the United Nations as one of the least developed countries, one dependent on foreign assistance.
    [Show full text]
  • Patterns of Island Change and Persistence Offer Alternate Adaptation Pathways for Atoll Nations
    ARTICLE DOI: 10.1038/s41467-018-02954-1 OPEN Patterns of island change and persistence offer alternate adaptation pathways for atoll nations Paul S. Kench 1, Murray R. Ford1 & Susan D. Owen1 Sea-level rise and climatic change threaten the existence of atoll nations. Inundation and erosion are expected to render islands uninhabitable over the next century, forcing human migration. Here we present analysis of shoreline change in all 101 islands in the Pacific atoll 1234567890():,; nation of Tuvalu. Using remotely sensed data, change is analysed over the past four decades, a period when local sea level has risen at twice the global average (~3.90 ± 0.4 mm.yr−1). Results highlight a net increase in land area in Tuvalu of 73.5 ha (2.9%), despite sea-level rise, and land area increase in eight of nine atolls. Island change has lacked uniformity with 74% increasing and 27% decreasing in size. Results challenge perceptions of island loss, showing islands are dynamic features that will persist as sites for habitation over the next century, presenting alternate opportunities for adaptation that embrace the heterogeneity of island types and their dynamics. 1 School of Environment, University of Auckland, Private Bag, 92010 Auckland, New Zealand. Correspondence and requests for materials should be addressed to P.S.K. (email: [email protected]) NATURE COMMUNICATIONS | (2018) 9:605 | DOI: 10.1038/s41467-018-02954-1 | www.nature.com/naturecommunications 1 ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/s41467-018-02954-1 nderstanding of human migration patterns and popula- Amid this dispiriting and forlorn consensus, recent commen- tion relocation through the Pacific, since earliest settle- tators have queried whether the loss of islands can be avoided and U 17 ment, has been informed by insights into the geologic ask whether a more optimistic prognosis exists for atoll nations .
    [Show full text]