(ONENA) in the South Pacific to Make Them Count in Global Health
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2016 Census Data Seminar – Norfolk Island
2016 Census Data Seminar – Norfolk Island Norfolk Island enumeration Local media to communicate key Census messages Special field procedures Team of local people to conduct enumeration Engagement with key Tailored materials stakeholders Norfolk Island – letter to residents Norfolk Island – fact sheet Norfolk Island – fact sheet Norfolk Island – place of birth Norfolk Island – fact sheet Norfolk Island – geography Norfolk Island consists of 1 SA2 and 8 SA1s High quality Census 95.1% Overall response rate Norfolk Island response 95.6% rate Overall online response 63.3% rate Norfolk Island online 5.4% response rate Census data - from forms to statistics 700 coding & 68.9 million Wide range of processing pieces of products and staff data services 2.8 million 8.45 million 5.3 billion tables household forms transactions and 750 thousand of data personal forms 2016 Census Data Summary Snapshot of Australia Population growth 8.9% 3.4 m Where do we live? Christmas Island 1 843 Cocos (Keeling) Islands 544 Norfolk Island 1 748 Norfolk Island population Norfolk Island population, 2001 - 2016 3000 2500 2000 1500 1000 500 0 2001 2006 2011 2016 Norfolk Island population Counted on Census night Usual residents* *Definition of usual residents differs between 2016 and previous years Norfolk Island population Norfolk Island At a glance – key characteristics Norfolk Island Australia 1,748 Population 23.4 million 46.8 / 53.2 Male / Female % 49.3 / 51.7 49 Median Age 38 1,080 Private dwellings 9.9 million 2.2 People per household 2.6 491 Families 6.1 million -
ISO Country Codes
COUNTRY SHORT NAME DESCRIPTION CODE AD Andorra Principality of Andorra AE United Arab Emirates United Arab Emirates AF Afghanistan The Transitional Islamic State of Afghanistan AG Antigua and Barbuda Antigua and Barbuda (includes Redonda Island) AI Anguilla Anguilla AL Albania Republic of Albania AM Armenia Republic of Armenia Netherlands Antilles (includes Bonaire, Curacao, AN Netherlands Antilles Saba, St. Eustatius, and Southern St. Martin) AO Angola Republic of Angola (includes Cabinda) AQ Antarctica Territory south of 60 degrees south latitude AR Argentina Argentine Republic America Samoa (principal island Tutuila and AS American Samoa includes Swain's Island) AT Austria Republic of Austria Australia (includes Lord Howe Island, Macquarie Islands, Ashmore Islands and Cartier Island, and Coral Sea Islands are Australian external AU Australia territories) AW Aruba Aruba AX Aland Islands Aland Islands AZ Azerbaijan Republic of Azerbaijan BA Bosnia and Herzegovina Bosnia and Herzegovina BB Barbados Barbados BD Bangladesh People's Republic of Bangladesh BE Belgium Kingdom of Belgium BF Burkina Faso Burkina Faso BG Bulgaria Republic of Bulgaria BH Bahrain Kingdom of Bahrain BI Burundi Republic of Burundi BJ Benin Republic of Benin BL Saint Barthelemy Saint Barthelemy BM Bermuda Bermuda BN Brunei Darussalam Brunei Darussalam BO Bolivia Republic of Bolivia Federative Republic of Brazil (includes Fernando de Noronha Island, Martim Vaz Islands, and BR Brazil Trindade Island) BS Bahamas Commonwealth of the Bahamas BT Bhutan Kingdom of Bhutan -
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. -
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. -
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. -
3. Quaternary Vertical Tectonics of the Central New Hebrides Island Arc1
Collot, J.-Y., Greene, H. G., Stokking, L. B., et al., 1992 Proceedings of the Ocean Drilling Program, Initial Reports, Vol. 134 3. QUATERNARY VERTICAL TECTONICS OF THE CENTRAL NEW HEBRIDES ISLAND ARC1 Frederick W. Taylor2 ABSTRACT Hundreds of meters of uplift of both the frontal arc and backarc characterize the late Quaternary vertical tectonic history of the central New Hebrides Island Arc. This vertical deformation is directly related to large, shallow earthquakes on the interplate thrust zone postulated on the basis of coral emergence data. This chapter presents evidence from the best documented and illustrated examples of uplifted coral reefs from the central New Hebrides Island Arc for the pattern and rates of vertical deformation caused by subduction of the d'Entrecasteaux Zone and the West Torres Massif over the past few 100 k.y. The pattern of vertical movement based on upper Quaternary coral reef terraces documents that the islands of Espiritu Santo, Malakula, Pentecost, and Maewo have risen hundreds of meters during the late Quaternary. This history suggests that the present pattern and rates of vertical deformation should be extrapolated back to at least 1 Ma, which would indicate that the total amount of structural and morphological modification of the arc during the present phase of deformation is more significant than previously assumed. The morphology of the central New Hebrides Island Arc may have resembled a more typical arc-trench area only 1-2 Ma. If the late Quaternary patterns and rates of vertical deformation have affected the central New Hebrides Island Arc since 1-2 Ma, then virtually all of the anomalous morphology that characterizes the central New Hebrides Island Arc can be attributed to the subduction of the d'Entrecasteaux Zone and the West Torres Massif. -
The Melanesian Mission, 1877–1909
4 The Melanesian Mission, 1877–1909 The heathen are always threatening us; they come with their bows and arrows again and again, and say they will kill us all and bury the school, but it is mostly words; they say they want three lives, Johnson’s, mine, and John’s (these are the three teachers). We do not go to meet them with arms, Mr. Comins has told us to seek peace with them, so we give them food and goods, and we try not to get angry with them. —Luke Masuraa, Aulu, 18961 Introduction Christianity, labour and government are three of the major influences that shaped modern Malaita before the 1940s. The fourth is an ability to be practical and incorporate change. There is nothing unique in the combination of the first three elements, which were major causes of change in many Pacific Islands societies. Yet virtually no other island experienced the same intensity of labour recruiting or had the strong link with Christian missions in Queensland. As we have seen, many early Malaitan Christians adopted their new spiritual beliefs while working on overseas plantations and attending denominational missions, the strongest links being with the QKM-SSEM and the Anglicans. This chapter further develops themes raised in the last, with a concentration 1 Quoted in the Ballarat Churchman and reproduced in OPMM, Mar 1896, 200. 183 MAKING MALA on the Anglican’s Melanesian Mission. David Lawrence, writing about the BSIP’s first resident commissioner, Charles Woodford, provides a neat summary of the interactions between the different European groups and local people: Missionaries saw themselves as pursuing a political agenda that filled the gap between fervent British colonialism and neutrality. -
Demographic Instability in the Paci C Island Territories
Durham E-Theses Demographic instability in the pacic island territories Matoto, O. A. How to cite: Matoto, O. A. (1971) Demographic instability in the pacic island territories, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/10011/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk DEMOGHAPHIC INSTABILITY Bf THE PACIFIC ISLAND TEREITORIES Thesis submitted to the Faculty of Social Sciences, University of Durham, for the degree of M.A. 'O.A. Matoto B.A. (Auckland) University of Durham, Durham City, England, 1971. The copyright of this thesis rests with the author. No quotation from it should be published without his prior written consent and information derived from it should be acknowledged. ABSTRACT The main purpose of this thesis is to show that demographic instability is a feature of the populations of the Pacific island territories. -
Pacific Island Populations
POPULATION CHARACTERISTICS / MID-YEAR POPULATION ESTIMATE / VITAL STATISTICS / POPULATION CHARACTERISTICS / ESTIMATION DE LA POPULATION EN CARACTÉRISTIQUES DE LA POPULATION STATISTIQUES VITALES CARACTÉRISTIQUES DE LA POPULATION MILIEU D’ANNÉE Crude Crude Crude Net Annual Estimated Average Land area Urban Dependency Teenage Fertility Population Average Birth Rate a Death Rate a Migration Growth Rate Annual Growth Rate b Median e Infant Mortality Rate COUNTRY/TERRITORY (km²) Last Density population at Annual Sex Ratio c Ratio Total Fertility Rate Rate f (15–19) COUNTRY/TERRITORY count at last Household (‰) (‰) Rate (‰) (%) (%) Age d (IMR, ‰) g Life Expectancy at Birth h population (persons/ last census (%) Intercensal (15–59) (TFR) 2 Size PAYS / TERRITOIRE Superficie census km ) Growth Rate 2020 2030 2050 PAYS / TERRITOIRE census Rapport de Rapport de Indice synthétique Fécondité des h (km²) Population Tx brut de Tx brut de Tx brut de Tx de Estimation du tx de c Âges f Tx de mortalité Espérance de vie à la naissance Taille a a b masculinité d e adolescentes Population Densité urbaine Tx annuel de natalité mortalité migration croissance croissance annuel médian dépendance de fécondité (ISF) infantile (TMI, ‰) g Dernier moyenne (15–19) au dernier (habitants/ au dernier croissance (‰) (‰) nette (‰) annuel (%) (%) (15–59) recensement des recensement km2) recensement intercensitaire TFR Year Year IMR Year Males Females Year ménages Total Total Total 2020 2020–30 2030–50 2020 % (%) ISF Année Année TMI Année Hommes Femmes Année MELANESIA 540,260 -
Situation Report Response Name Tropical Cyclone Donna
Situation Report Response Name Tropical Cyclone Donna Situation Report 05 Time & Date 18:30 10th May 2017 Reporting period 08/05/2017 – 10/05/2017 Provinces affected Torba, Sanma, Malampa Attachment(s) Situation overview infographic; Torres Islands reference map; NEOC Status Operational Situation Overview Tropical Cyclone Donna has passed out of the Vanuatu region and the National Disaster Management Office (NDMO) gave the all clear on the 9th of May. TC Donna moved in a westerly direction passing north of the Vanuatu group within 50-100km the Torres islands in Torba Province as a category 3 cyclone. It continued west, before turning south, gathering strength to become a category 5 and passed to the west of Sanma, Malmpa and Shefa. TC Donna passed about 200km to the west of the islands of Vanuatu. Preliminary Impact The Torres Island group in Torba Province remains the most affected area, with other areas in Torba less affected. Ongoing assessment of inaccessible areas of Samna and Malampa are ongoing and a full picture will not be known until that is complete. Information available so far is showing modest impacts in other areas. During TC Donna approximately 60 evacuation centres were activated across Vanuatu, sheltering around 2,700 people. These evacuation facilities include schools, churches, caves, private houses, community buildings and other public buildings which were identified pre-disaster. Almost all evacuees have returned to their homes, however, a small number of evacuation centres remain open in Torres and Shefa. Torba Province Preliminary assessments are showing significant damage on the Torres Islands to crops, shelter, water supply, telecommunications and schools. -
The Mosquitoes of the Banks and Torres Island Groups of the South Pacific (Diptera: Culicidae)
Vol. 17, no. 4: 511-522 28 October 1977 THE MOSQUITOES OF THE BANKS AND TORRES ISLAND GROUPS OF THE SOUTH PACIFIC (DIPTERA: CULICIDAE) By Mario Maffi1 and Brian Taylor2 Abstract: In August 1971 a total of 1003 specimens of Culicidae were collected from 2 little known island groups ofthe New Hebrides, the Banks and the Torres, 637 (39 $$, 12 S$, 148 P, 13 p, 419 L, 6 1) and 366 (46 $$, 3 $<$, 73 P, 13 p, 231 L), respectively. Of 9 species of Culicidae previously recorded, 6 are confirmed. 3 species are added: Culex (Cux.) banksensis, Culex {Cux,) sitiens, Culex (Eum.) Jemineus. The distribution (considerably wider than previously recorded) and the bionomics of the species are presented. Located at the northern end of the territory of the New Hebrides Condominium, and administratively part of it, 2 island groups, the Banks and the Torres, rise from the New- Hebrides submarine ridge and are dispersed over a wide area of the Southwest Pacific: 13°04' to 14°28' S, and 166°30' to 168°04' E. The Banks, the southern ofthe 2 groups, are more scattered and consist of 2 major islands (Gaua, Vanua Lava) and 6 minor islands (Merelava, Merig, Mo ta, Motalava, Parapara, Ro wa) with a total land area of approx imately 750 km2. The Torres group is more compact and consists of 5 small islands (Toga, Loh, Tegua, Metoma, Hiu) with less than 100km2 ofland area. There are a few off-shore islets. Except for the reef island of Rowa, the islands are of volcanic origin; however, on some of the smaller islands, particularly in the Torres, there are terraces of coral limestone. -
Norfolk Island Roadmap Submissions Feedback Summary
2011 NORFOLK ISLAND ROADMAP SUBMISSIONS FEEDBACK SUMMARY NORFOLK ISLAND ROADMAP SUBMISSIONS FEEDBACK SUMMARY Summary The Norfolk Island Roadmap was developed to inform future directions in relation to structural reform of Norfolk Island’s self-government model. The roadmap is a discussion document, and has been developed to enable targeted consultation between the Australian Government, the Norfolk Island Government (NIG) and the local community. The key Norfolk Island Roadmap reforms are: - Governance through providing a stronger, more open and transparent form of government, building on the reforms in the Territories Law Reform Act 2010. - Economic development through quick action to address barriers to tourism, particularly reform of air services, access to the Island, and facilities for cruise ships. - Enabling the Norfolk Island Public Service to provide good financial and policy advice and effective services to the Norfolk Island Government and community. - Obligation by Norfolk Island residents to contribute to the Australian tax system; - Social services including adequate health, welfare and education, support for vulnerable citizens and providing educational opportunities. - Preserving and enhancing the environment and heritage attributes of the Island including the Kingston and Arthur’s Vale Historic Area and the other natural areas of Norfolk Island and recognizing their contribution to the economy and community. - Extend Commonwealth laws to the Island to promote improved economic growth and diversification. The Roadmap was circulated for public comment by the NIG and this round of consultation closed on 20 May 2011. 153 submissions were received either by the NIG or the Department. All submissions were then collated by the Department in line with the NIG’s requested that it conduct the analysis.