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TROPICAL CYCLONE WINSTON SITUATION REPORT 30 of 26/02/2016
NATIONAL EMERGENCY OPERATION CENTER TROPICAL CYCLONE WINSTON SITUATION REPORT 30 of 26/02/2016 This Situation Report is issued by the National Emergency Operation Centre and covers the period from 0800 hours to 1600hours on 26/02/2016. The purpose of this report is to provide the update on the current operations undertaken after TC Winston. 1. STATUS SUMMARY EVENT REMARKS TOTAL CENTRAL WEST EAST NORTH TOTAL Death(s) 9 11 20 2 42 Missing - - - - - Hospitalised 5 17 7 4 33 Injured 24 24 68 10 126 Evacuation 160 339 335 101 935 Centres Evacuees 13,282 33,963 6999 6095 60,339 2. WEATHER OUTLOOK NEOC SITREP 28 / 1 6 P a g e 1 | 29 Issued from the National Weather Forecasting Centre Nadi at 2.30 pm on Friday the 26th of February 2016 A strong wind warning remains in force for Kadavu passage, southern Koro sea and southern Lau waters. Situation: A weak of trough of low pressure with clouds and showers remains low moving over the eastern part of Fiji. It is expected to gradually move west wards and affect the rest of the group till later today. Meanwhile a moist north east wind flow prevails over Fiji. Forecast to midnight for Fiji waters for Kadavu passage southern Koro sea and southern Lau waters, north east winds 20 to 25 knots. Rough seas. Moderate north east swells. Poor visibility in areas of showers and thunderstorm. Further outlook:: East to north east winds 20 to 25 knots, Rough seas. For the rest of Fiji waters north to north east winds, 15 to 20 knots, moderate to rough seas. -
2020 Cruise Directory Directory 2020 Cruise 2020 Cruise Directory M 18 C B Y 80 −−−−−−−−−−−−−−− 17 −−−−−−−−−−−−−−−
2020 MAIN Cover Artwork.qxp_Layout 1 07/03/2019 16:16 Page 1 2020 Hebridean Princess Cruise Calendar SPRING page CONTENTS March 2nd A Taste of the Lower Clyde 4 nights 22 European River Cruises on board MS Royal Crown 6th Firth of Clyde Explorer 4 nights 24 10th Historic Houses and Castles of the Clyde 7 nights 26 The Hebridean difference 3 Private charters 17 17th Inlets and Islands of Argyll 7 nights 28 24th Highland and Island Discovery 7 nights 30 Genuinely fully-inclusive cruising 4-5 Belmond Royal Scotsman 17 31st Flavours of the Hebrides 7 nights 32 Discovering more with Scottish islands A-Z 18-21 Hebridean’s exceptional crew 6-7 April 7th Easter Explorer 7 nights 34 Cruise itineraries 22-97 Life on board 8-9 14th Springtime Surprise 7 nights 36 Cabins 98-107 21st Idyllic Outer Isles 7 nights 38 Dining and cuisine 10-11 28th Footloose through the Inner Sound 7 nights 40 Smooth start to your cruise 108-109 2020 Cruise DireCTOrY Going ashore 12-13 On board A-Z 111 May 5th Glorious Gardens of the West Coast 7 nights 42 Themed cruises 14 12th Western Isles Panorama 7 nights 44 Highlands and islands of scotland What you need to know 112 Enriching guest speakers 15 19th St Kilda and the Outer Isles 7 nights 46 Orkney, Northern ireland, isle of Man and Norway Cabin facilities 113 26th Western Isles Wildlife 7 nights 48 Knowledgeable guides 15 Deck plans 114 SuMMER Partnerships 16 June 2nd St Kilda & Scotland’s Remote Archipelagos 7 nights 50 9th Heart of the Hebrides 7 nights 52 16th Footloose to the Outer Isles 7 nights 54 HEBRIDEAN -
Data Structure
Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference. -
Zeszyt 10. Morza I Oceany
Uwaga: Niniejsza publikacja została opracowana według stanu na 2008 rok i nie jest aktualizowana. Zamieszczony na stronie internetowej Komisji Standaryzacji Nazw Geograficznych poza Granica- mi Rzeczypospolitej Polskiej plik PDF jest jedynie zapisem cyfrowym wydrukowanej publikacji. Wykaz zalecanych przez Komisję polskich nazw geograficznych świata (Urzędowy wykaz polskich nazw geograficznych świata), wraz z aktualizowaną na bieżąco listą zmian w tym wykazie, zamieszczo- ny jest na stronie internetowej pod adresem: http://ksng.gugik.gov.pl/wpngs.php. KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju NAZEWNICTWO GEOGRAFICZNE ŚWIATA Zeszyt 10 Morza i oceany GŁÓWNY URZĄD GEODEZJI I KARTOGRAFII Warszawa 2008 KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju Waldemar Rudnicki (przewodniczący), Andrzej Markowski (zastępca przewodniczącego), Maciej Zych (zastępca przewodniczącego), Katarzyna Przyszewska (sekretarz); członkowie: Stanisław Alexandrowicz, Andrzej Czerny, Janusz Danecki, Janusz Gołaski, Romuald Huszcza, Sabina Kacieszczenko, Dariusz Kalisiewicz, Artur Karp, Zbigniew Obidowski, Jerzy Ostrowski, Jarosław Pietrow, Jerzy Pietruszka, Andrzej Pisowicz, Ewa Wolnicz-Pawłowska, Bogusław R. Zagórski Opracowanie Kazimierz Furmańczyk Recenzent Maciej Zych Komitet Redakcyjny Andrzej Czerny, Joanna Januszek, Sabina Kacieszczenko, Dariusz Kalisiewicz, Jerzy Ostrowski, Waldemar Rudnicki, Maciej Zych Redaktor prowadzący Maciej -
Setting Priorities for Marine Conservation in the Fiji Islands Marine Ecoregion Contents
Setting Priorities for Marine Conservation in the Fiji Islands Marine Ecoregion Contents Acknowledgements 1 Minister of Fisheries Opening Speech 2 Acronyms and Abbreviations 4 Executive Summary 5 1.0 Introduction 7 2.0 Background 9 2.1 The Fiji Islands Marine Ecoregion 9 2.2 The biological diversity of the Fiji Islands Marine Ecoregion 11 3.0 Objectives of the FIME Biodiversity Visioning Workshop 13 3.1 Overall biodiversity conservation goals 13 3.2 Specifi c goals of the FIME biodiversity visioning workshop 13 4.0 Methodology 14 4.1 Setting taxonomic priorities 14 4.2 Setting overall biodiversity priorities 14 4.3 Understanding the Conservation Context 16 4.4 Drafting a Conservation Vision 16 5.0 Results 17 5.1 Taxonomic Priorities 17 5.1.1 Coastal terrestrial vegetation and small offshore islands 17 5.1.2 Coral reefs and associated fauna 24 5.1.3 Coral reef fi sh 28 5.1.4 Inshore ecosystems 36 5.1.5 Open ocean and pelagic ecosystems 38 5.1.6 Species of special concern 40 5.1.7 Community knowledge about habitats and species 41 5.2 Priority Conservation Areas 47 5.3 Agreeing a vision statement for FIME 57 6.0 Conclusions and recommendations 58 6.1 Information gaps to assessing marine biodiversity 58 6.2 Collective recommendations of the workshop participants 59 6.3 Towards an Ecoregional Action Plan 60 7.0 References 62 8.0 Appendices 67 Annex 1: List of participants 67 Annex 2: Preliminary list of marine species found in Fiji. 71 Annex 3 : Workshop Photos 74 List of Figures: Figure 1 The Ecoregion Conservation Proccess 8 Figure 2 Approximate -
HEBRIDEAN MARINE MAMMAL ATLAS Part 1: Silurian, 15 Years of Marine Mammal Monitoring in the Hebrides 2 CONTENTS CONTENTS 3
HEBRIDEAN MARINE MAMMAL ATLAS Part 1: Silurian, 15 years of marine mammal monitoring in the Hebrides 2 CONTENTS CONTENTS 3 CONTENTS 1 2 3 4 5 6 INTRODUCTION SILURIAN HEBRIDES SPECIES FUTURE CONTRIBUTORS 4 8 22 26 56 58 Foreword About our Extraordinary Harbour Porpoise On the Horizon Acknowledgements Research Vessel Biodiversity 5 29 59 About Us 10 Minke Whale References Survey Protocol 5 33 A Message from 14 Basking Shark our Patron Data Review 37 6 Short-Beaked About the Atlas Common Dolphin 40 Bottlenose Dolphin 43 White-Beaked Dolphin 46 Risso’s Dolphin 49 Killer Whale (Orca) 53 Humpback Whale Suggested citation; Hebridean Whale and Dolphin Trust (2018). Hebridean Marine Mammal Atlas. Part 1: Silurian, 15 years of marine mammal monitoring in the Hebrides. A Hebridean Whale and Dolphin Trust Report (HWDT), Scotland, UK. 60 pp. Compiled by Dr Lauren Hartny-Mills, Science and Policy Manager, Hebridean Whale and Dolphin Trust 4 CONTENTS INTRODUCTION 5 FOREWORD INTRODUCTION About Us Established in 1994, the Hebridean Whale and Dolphin Based on the Isle of Mull, in the heart of the Trust (HWDT) is the trusted voice and leading source of Hebrides, HWDT is a registered charity that information for the conservation of Hebridean whales, has pioneered practical, locally based education dolphins and porpoises (cetaceans). and scientifically rigorous long-term monitoring programmes on cetaceans in the Hebrides. The Hebridean Marine Mammal Atlas is a showcase of We believe that evidence is the foundation of effective 15 years of citizen science and species monitoring in the conservation. Our research has critically advanced Hebrides. -
Current and Future Climate of the Fiji Islands
Rotuma eef a R Se at re Ahau G p u ro G a w a Vanua Levu s Bligh Water Taveuni N a o Y r th er Koro n La u G ro Koro Sea up Nadi Viti Levu SUVA Ono-i-lau S ou th er n L Kadavu au Gr South Pacific Ocean oup Current and future climate of the Fiji Islands > Fiji Meteorological Service > Australian Bureau of Meteorology > Commonwealth Scientific and Industrial Research Organisation (CSIRO) Fiji’s current climate Across Fiji the annual average temperature is between 20-27°C. Changes Fiji’s climate is also influenced by the in the temperature from season to season are relatively small and strongly trade winds, which blow from the tied to changes in the surrounding ocean temperature. east or south-east. The trade winds bring moisture onshore causing heavy Around the coast, the average night- activity. It extends across the South showers in the mountain regions. time temperatures can be as low Pacific Ocean from the Solomon Fiji’s climate varies considerably as 18°C and the average maximum Islands to east of the Cook Islands from year to year due to the El Niño- day-time temperatures can be as with its southern edge usually lying Southern Oscillation. This is a natural high as 32°C. In the central parts near Fiji (Figure 2). climate pattern that occurs across of the main islands, average night- Rainfall across Fiji can be highly the tropical Pacific Ocean and affects time temperatures can be as low as variable. On Fiji’s two main islands, weather around the world. -
Deep Structure of the Foreland to the Caledonian Orogen, Nw Scotland: Results of the Birps Winch Profile
TECTONICS, VOL. 5, NO. 2, PAGES 171-194, APRIL 1986 DEEP STRUCTURE OF THE FORELAND TO THE CALEDONIAN OROGEN, NW SCOTLAND: RESULTS OF THE BIRPS WINCH PROFILE Jonathan A. Brewer Department of Earth Sciences, University of Cambridge, Cambridge, United Kingdom David K. Smythe British Geological Survey, Edinburgh, United Kingdom Abstract. The WINCH marine deep tal velocity for the Hebridean shelf of seismic reflection profile crosses the 6.4+0.1 km s-1. The eastward-dipping Fla- Hebridean shelf, the Proterozoic foreland nnan Thrust can be mapped into the upper to the Caledonian orogen, west of Scot- mantle on three lines from about 15 to land. The data quality is very good. The 45 km depth, well into the upper mantle. upper crust is largely devoid of coherent Neither the Flannan Thrust nor the Outer seismic reflections, although this may in Isles Thrust appear to pass straight thro- part be due to acquisition techniques ugh the reflective lower crust, suggesting being inappropriate for this problem. In that the lower crust is a region of high contrast, the middle and lower crust (10- strain. The Outer Hebrides is a positive 25 km depth) exhibits good reflections; block probably formed as an isostatic the mid crust contains reflectors which response to Mesozoic normal faulting which may be relics of early Palaeozoic, Caledo- reactivated the Outer Isles Thrust. nian (or earlier Grenvillian) eastward- INTRODUCTION dipping thrust zones, which pass into an acoustically strongly layered lower crust. The Western Isles-North Channel (WINCH) The Outer Isles Thrust is mapped from the surf ace to the mid crust, and tied into deep crustal seismic reflection profile was recorded for BIRPS (British Institut- its land outcrop on north Lewis. -
Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO
An Atlas of Oceanic Internal Solitary Waves (February 2004) Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Indonesian Seas • Bali Sea • Flores Sea • Molucca Sea • Banda Sea • Java Sea • Savu Sea • Cream Sea • Makassar Strait Overview The Indonesian Seas are the regional bodies of water in and around the Indonesian Archipelago. The seas extend between approximately 12o S to 3o N and 110o to 132oE (Figure 1). The region separates the Pacific and Indian Oceans. Figure 1. Bathymetry of the Indonesian Archipelago. [Smith and Sandwell, 1997] Observations Indonesian Archipelago is most extensive archipelago in the world with more than 15,000 islands. The shallow bathymetry and the strong tidal currents between the islands give rise to the generation of internal waves throughout the archipelago. As a result there are a very 453 An Atlas of Oceanic Internal Solitary Waves (February 2004) Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO large number of internal wave sources throughout the region. Since the Indonesian Seas boarder the equator, the stratification of the waters in this sea area does not change very much with season, and internal wave activity is expected to take place all year round. Table 2 shows the months of the year during which internal waves have been observed in the Bali, Molucca, Banda and Savu Seas Table 1 - Months when internal waves have been observed in the Bali Sea. (Numbers indicate unique dates in that month when waves have been noted) Jan Feb Mar Apr May Jun Jul Aug Sept Oct Nov Dec 12111 11323 Months when Internal Waves have been observed in the Molucca Sea. -
1 Investigation of the Energy Potential from Tidal Stream
INVESTIGATION OF THE ENERGY POTENTIAL FROM TIDAL STREAM CURRENTS IN INDONESIA Kadir Orhan1, Roberto Mayerle1, Rangaswami Narayanan1 and Wahyu Widodo Pandoe2 In this paper, an advanced methodology developed for the assessment of tidal stream resources is applied to several straits between Indian Ocean and inner Indonesian seas. Due to the high current velocities up to 3-4 m/s, the straits are particularly promising for the efficient generation of electric power. Tidal stream power potentials are evaluated on the basis of calibrated and validated high-resolution, three-dimensional numerical models. It was found that the straits under investigation have tremendous potential for the development of renewable energy production. Suitable locations for the installation of the turbines are identified in all the straits, and sites have been ranked based on the level of power density. Maximum power densities are observed in the Bali Strait, exceeding around 10kw/m2. Horizontal axis tidal turbines with a cut-in velocity of 1m/s are considered in the estimations. The highest total extractable power resulted equal to about 1,260MW in the Strait of Alas. Preliminary assessments showed that the power production at the straits under investigation is likely to exceed previous predictions reaching around 5,000MW. Keywords: renewable energy; tidal stream currents; numerical model; Indonesia INTRODUCTION The global energy supply is facing severe challenges in terms of long-term sustainability, fossil fuel reserve exhaustion, global warming and other energy related environmental concerns, geopolitical and military conflicts surrounding oil rich countries, and secure supply of energy. Renewable energy sources such as solar, wind, wave and tidal energy are capable of meeting the present and future energy demands with ease without inflicting any considerable damage to global ecosystem (Asif et al. -
Indonesia's Transformation and the Stability of Southeast Asia
INDONESIA’S TRANSFORMATION and the Stability of Southeast Asia Angel Rabasa • Peter Chalk Prepared for the United States Air Force Approved for public release; distribution unlimited ProjectR AIR FORCE The research reported here was sponsored by the United States Air Force under Contract F49642-01-C-0003. Further information may be obtained from the Strategic Planning Division, Directorate of Plans, Hq USAF. Library of Congress Cataloging-in-Publication Data Rabasa, Angel. Indonesia’s transformation and the stability of Southeast Asia / Angel Rabasa, Peter Chalk. p. cm. Includes bibliographical references. “MR-1344.” ISBN 0-8330-3006-X 1. National security—Indonesia. 2. Indonesia—Strategic aspects. 3. Indonesia— Politics and government—1998– 4. Asia, Southeastern—Strategic aspects. 5. National security—Asia, Southeastern. I. Chalk, Peter. II. Title. UA853.I5 R33 2001 959.804—dc21 2001031904 Cover Photograph: Moslem Indonesians shout “Allahu Akbar” (God is Great) as they demonstrate in front of the National Commission of Human Rights in Jakarta, 10 January 2000. Courtesy of AGENCE FRANCE-PRESSE (AFP) PHOTO/Dimas. RAND is a nonprofit institution that helps improve policy and decisionmaking through research and analysis. RAND® is a registered trademark. RAND’s publications do not necessarily reflect the opinions or policies of its research sponsors. Cover design by Maritta Tapanainen © Copyright 2001 RAND All rights reserved. No part of this book may be reproduced in any form by any electronic or mechanical means (including photocopying, -
1 Influence of Sea Ice Anomalies on Antarctic Precipitation Using
https://doi.org/10.5194/tc-2019-69 Preprint. Discussion started: 12 June 2019 c Author(s) 2019. CC BY 4.0 License. Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution Hailong Wang1*, Jeremy Fyke2,3, Jan Lenaerts4, Jesse Nusbaumer5,6, Hansi Singh1, David Noone7, and Philip Rasch1 (1) Pacific Northwest National Laboratory, Richland, WA 5 (2) Los Alamos National Laboratory, Los Alamos, NM (3) Associated Engineering, Vernon, British Columbia, Canada (4) Department of Atmospheric and Oceanic Sciences, University of Colorado at Boulder, Boulder, CO (5) NASA Goddard Institute for Space Studies, New York, NY (6) Center for Climate Systems Research, Columbia University, New York, NY 10 (7) Oregon State University, Corvallis, OR *Correspondence to: [email protected] 1 https://doi.org/10.5194/tc-2019-69 Preprint. Discussion started: 12 June 2019 c Author(s) 2019. CC BY 4.0 License. Abstract We conduct sensitivity experiments using a climate model that has an explicit water source tagging capability forced by prescribed composites of sea ice concentrations (SIC) and corresponding SSTs to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source– 5 receptor relationships for precipitation over Antarctica. Surface sensible heat fluxes, evaporation, and column-integrated water vapor are larger over Southern Ocean (SO) areas with lower SIC, but changes in Antarctic precipitation and its source attribution with SICs reflect a strong spatial variability. Among the tagged source regions, the Southern Ocean (south of 50°S) contributes the most (40%) to the Antarctic total precipitation, followed by more northerly ocean basins, most notably the S.