Competition, Cooperation and Security in the Red Sea Omar S Mahmood
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This Keyword List Contains Indian Ocean Place Names of Coral Reefs, Islands, Bays and Other Geographic Features in a Hierarchical Structure
CoRIS Place Keyword Thesaurus by Ocean - 8/9/2016 Indian Ocean This keyword list contains Indian Ocean place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. For example, the first name on the list - Bird Islet - is part of the Addu Atoll, which is in the Indian Ocean. The leading label - OCEAN BASIN - indicates this list is organized according to ocean, sea, and geographic names rather than country place names. The list is sorted alphabetically. The same names are available from “Place Keywords by Country/Territory - Indian Ocean” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. For example, the first place name “Bird Islet” has a unique identifier of “00S073E0013”. From that we see that Bird Islet is located at 00 degrees south (S) and 073 degrees east (E). It is place number 0013 at that latitude and longitude. (Note: some long lines wrapped, placing the unique identifier on the following line.) This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Indian Ocean OCEAN BASIN > Indian Ocean > Addu Atoll > Bird Islet (00S073E0013) OCEAN BASIN > Indian Ocean > Addu Atoll > Bushy Islet (00S073E0014) OCEAN BASIN > Indian Ocean > Addu Atoll > Fedu Island (00S073E0008) -
This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Quaternary Science Reviews 29 (2010) 3843e3860 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev North Atlantic influence on 19the20th century rainfall in the Dead Sea watershed, teleconnections with the Sahel, and implication for Holocene climate fluctuations Yochanan Kushnir a,*, Mordechai Stein a,b a Lamont-Doherty Earth Observatory, The Earth Institute, Columbia University, 61 Route 9W, Palisades, NY 10964, USA b Geological Survey of Israel, 30 Malkhe Israel Street, 95501 Jerusalem, Israel article info abstract Article history: The importance of understanding processes that govern the hydroclimate of the Mediterranean Basin is Received 14 February 2010 highlighted by the projected significant drying of the region in response to the increase in greenhouse Received in revised form gas concentrations. Here we study the long-term hydroclimatic variability of the central Levant region, 3 August 2010 situated in the eastern boundary of the Basin, as reveled by instrumental observations and the Holocene Accepted 9 September 2010 record of Dead Sea level variations. -
000000548.Sbu.Pdf
SSStttooonnnyyy BBBrrrooooookkk UUUnnniiivvveeerrrsssiiitttyyy The official electronic file of this thesis or dissertation is maintained by the University Libraries on behalf of The Graduate School at Stony Brook University. ©©© AAAllllll RRRiiiggghhhtttsss RRReeessseeerrrvvveeeddd bbbyyy AAAuuuttthhhooorrr... Archaeological Investigation of the Buri Peninsula and Gulf of Zula, Red Sea Coast of Eritrea A Dissertation Presented by Amanuel Yosief Beyin to The Graduate School in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Anthropology (Archaeology) Stony Brook University May 2009 Stony Brook University The Graduate School Amanuel Yosief Beyin We, the dissertation committee for the above candidate for the Doctor of Philosophy degree, hereby recommend acceptance of this dissertation. John J. Shea Associate Professor, Anthropology David J. Bernstein Associate Professor, Anthropology John G. Fleagle Distinguished Professor, Anatomical Sciences Steven A. Brandt Associate Professor, Anthropology University of Florida, Gainesville This dissertation is accepted by the Graduate School Lawrence Martin Dean of the Graduate School ii Abstract of the Dissertation Archaeological Investigation of the Buri Peninsula and Gulf of Zula, Red Sea Coast of Eritrea by Amanuel Yosief Beyin Doctor of Philosophy in Anthropology (Archaeology) Stony Brook University 2009 This dissertation reports the results of archaeological survey and excavations on the Buri Peninsula and Gulf of Zula, Red Sea coast of Eritrea. Its primary goals were to seek evidence for prehistoric human settlement, and to define the geological, chronological and cultural contexts of the sites. The Red Sea Coast of Africa is thought to be an important refugium for humans dispersing from the interior of East Africa into Arabia and the Levant. -
West Africa Part III: Central Africa Part IV: East Africa & Southern Africa Name: Date
Part I: North Africa Part II: West Africa Part III: Central Africa Part IV: East Africa & Southern Africa Name: Date: AFRI CA Overview RICA lies at the heart of the earth's land Then, during the nineteenth century, masses. It sits astride the equator, with European traders began setting up trading sta . almost half the continent to the north tions along the coast of West Africa. The of the equator, and half to the south. It con traders, and their governments, soon saw great tains some of the world's greatest deserts, as opportunity for profit in Africa. Eventually, well as some of the world's greatest rivers. It many European countries took control of the has snow-capped mountains, and parched, arid land and divided it into colonies. plains. The first humans came from Africa. By the middle of the twentieth century, peo And in the millennia since those fust humans ple all across Africa had demanded indepen walked the plains of Africa, many different cul dence from colonial rule. By the end of the tures have arisen there. century, government had passed firmly into Physically, Africa is one enormous plateau. It African hands. However, the newly independ has no continental-scale mountain chains, no ent nations must still deal with the legacy of peninsulas, no deep fjords. Most of the conti colonialism. The boundaries the European nent is more than 1000 feet (300m) above sea powers created often cut across ethnic and cul level; over half is above 2500 feet (800 m). tural groups. Many African nations today are Africa's early history reflects the wide stretch still struggling to reconcile the different cul of the continent. -
Field Identification Guide to the Sharks and Rays of the Red Sea and Gulf of Aden
FAO SPECIES IDENTIFICATION GUIDE FOR FISHERY PURPOSES ISSN 1020-6868 FIELD IDENTIFICATION GUIDE TO THE SHARKS AND RAYS OF THE RED SEA AND GULF OF ADEN PERSGA FAO SPECIES IDENTIFICATION GUIDE FOR FISHERY PURPOSES FIELD IDENTIFICATION GUIDE TO THE SHARKS AND RAYS OF THE RED SEA AND GULF OF ADEN by Ramón Bonfil Marine Program Wildlife Conservation Society Bronx, New York, USA and Mohamed Abdallah Strategic Action Program Regional Organization for the Conservation of the Environment of the Red Sea and Gulf of Aden Jeddah, Saudi Arabia FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2004 iii PREPARATION OF THIS DOCUMENT This document was prepared under the coordination of the Species Identification and Data Programme of the Marine Resources Service, Fishery Resources and Environment Division, Fisheries Department, Food and Agriculture Organization of the United Nations (FAO). This field guide is largely based on material prepared for training courses on elasmobranch identification delivered in the region by the first author, and promoted by the Regional Organization for the Conservation of the Environment of the Red Sea and Gulf of Aden (PERSGA), as an activity of PERSGA’s Strategic Action Programme (SAP) towards capacity building and technical assistance in the Red Sea and Gulf of Aden region. Printing was supported by Japanese Government funds. The increasing recognition of the significance of sharks and batoid fishes as ecosystem health indicators, as well as their particular importance in exploited ecosystems in the Red Sea and the Gulf of Aden, have been key considerations to promote the preparation of this Field Guide. Furthermore, in recent years the reported catches of elasmobranchs in the Red Sea and the Gulf of Aden showed a marked increase. -
Directional Storm Surge in Enclosed Seas: the Red Sea, the Adriatic, and Venice
J. Mar. Sci. Eng. 2015, 3, 356-367; doi:10.3390/jmse3020356 OPEN ACCESS Journal of Marine Science and Engineering ISSN 2077-1312 www.mdpi.com/journal/jmse Article Directional Storm Surge in Enclosed Seas: The Red Sea, the Adriatic, and Venice Carl Drews Atmospheric Chemistry Observations & Modeling, National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307, USA; E-Mail: [email protected]; Tel.: +1-303-497-1429; Fax: +1-303-497-1400 Academic Editor: Rick Luettich Received: 30 March 2015 / Accepted: 25 May 2015 / Published: 29 May 2015 Abstract: Storm surge is dependent on wind direction, with maximum surge heights occurring when strong winds blow onshore. It is less obvious what happens when a port city is situated at the end of a long narrow gulf, like Venice at the northwestern end of the Adriatic Sea. Does the narrow marine approach to the port city limit the dangerous wind direction to a span of only a few degrees? This modeling study shows that the response in surge height to wind direction is a sinusoidal curve for port cities at the end of a long inlet, as well as for cities exposed along a straight coastline. Surge height depends on the cosine of the angle between the wind direction and the major axis of the narrow gulf. There is no special protection from storm surge afforded by a narrow ocean-going approach to a port city. Keywords: storm surge; Red Sea; Adriatic Sea; Venice; COAWST; ROMS; wind direction; wind setdown 1. Introduction Wind-driven storm surge can cause great damage and loss of life in coastal regions. -
Historical Ties: India’S Relations with Africa Date Back Several Centuries
EDITORIAL 30TH JULY 2019 GREAT GAME IN AFRICA Context Defence Minister’s recent visit to Mozambique, which is a good moment to reflect on the growing significance of the East African coastal countries and the islands off it for the geopolitics of the Indo-Pacific. Introduction: During the visit to Mozambique, he is expected to sign a number of agreements, including on hydrographic survey, sharing of white shipping information and the monitoring of its exclusive zone. He is also expected to deliver two fast patrol naval craft to the country as part of India’s expanding security cooperation with Mozambique. India and Africa - Historical Ties: India’s relations with Africa date back several centuries. The presence of Indians in East Africa is documented in the 'Periplus of the Erythraean Sea' or Guidebook of the Red Sea by an ancient Greek author written in 60 AD. The geographical proximity and easy navigability in Indian Ocean resulted in well- established trade network between India and the Swahili Coast predating European exploration. More concrete relation between India and Africa begins to emerge during the Islamic age which is evident through the accounts of Venetian traveller Marco Polo. Political connection during the colonial era was linked through M.K Gandhi who began his political career in South Africa, became the leader of colonized and established Indian Natal Congress in 1894. After India got independent, it raised voice for African liberation taking their case to all the available international forums. End of racial struggle and decolonization became the rallying point of India–Africa relations. India was a forerunner as a champion of the interests of the developing countries from Africa, particularly through the Bandung Declaration of 1955, the Group of 77, and the Non-Aligned Movement (NAM). -
Geog 120: World Geography American University of Phnom Penh
Geog 120: World Geography American University of Phnom Penh Map Quizzes: List of physical features 1. Africa Atlas Drakensberg Seas and Oceans Deserts Mediterranean Atlantic Kalahari Strait of Gibraltar Namib Suez Canal Sahara Mozambique Channel Ogaden Red Sea Libyan Gulf of Suez 2. Asia Lakes Lake Chad Seas and Oceans Lake Malawi (Nyasa) Lake Tanganyika Andaman Sea Lake Victoria Arabian Sea Lake Albert Aral Sea Lake Rudolph Arctic Ocean Atlantic Ocean Rivers Black Sea Caspian Sea Congo East China Sea Limpopo Indian Ocean Niger Inland Sea (also know as Setonaikai, Zambezi Japan) Nile Mediterranean Sea Orange Pacific Ocean Vaal Red Sea Sea of Japan Mountains Sea of Okhotsk 2 South China Sea Mountain Ranges Yellow Sea Caucuses Elburz Straits, Channels, Bays and Gulfs Himalayas Hindu Kush Bay of Bengal Ural Bosporus Zagros Dardanelles Gulf of Aden Gulf of Suez Deserts Gulf of Thailand Arabian Gulf of Tonkin Dasht-E-Kavir Persian Gulf Gobi Strait of Taiwan Negev Strait of Malacca Takla Makan Strait of Hormuz Strait of Sunda Suez Canal 3. The Americas Lakes Seas and Oceans Baykal Bering Tonle Sap Caribbean Sea Atlantic Ocean Pacific Ocean Rivers Straits, Channels, Bays and Gulfs Amur Brahmaputra Gulf of Mexico Chang Jiang Hudson Bay Euphrates Panama Canal Ganges Strait of Magellan Huang He (Yellow) Indus Lakes Irrawaddy Mekong Great Salt Tigris Great Lakes (Lakes Tonle Sap (River and Lake) Superior, Michigan, Huron, 3 Erie, and Ontario) 4. Australia and the Pacific Manitoba Titicaca Winnipeg Seas and Oceans Coral Sea Rivers Tasman Sea Pacific Ocean Amazon Indian Ocean Colorado Columbia Hudson Straits, Channels, Bays and Gulfs Mississippi Bass Strait Missouri Cook Strait Ohio Gulf of Carpentaria Orinoco Torres Strait Paraguay Plata Parana Rivers Rio Grande Darling St. -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
Intefwaitional EXPLORATIWWTS O Meetlnq-NO~~R Sketch
INTEfWAiTIONAL EXPLORATIWWTS Om sparsrs to have been sutured onto the Brazilian Shield near MEETlNQ-NO~~R14,laMJ the end of the Paleozoic. There is considerable controverav concerning is origin and original Iffietion, as well as the THOMAS E. O'CONNOR-Biographical Sketch nature of the suturina of the two maasifa. ~h~~..F nTnnnnr ie Asaocisted withthe Brazilian Shield ars two marine Vice President of Aminoil Paleozoic basins in the northern portion of the country. The Internationel, Incorporated. Tarija Basin is largely represented in BollrEa where it is the developing international ex- cemer of considerable exploration for and prdwtion of ptoration opportunltiea. Tom natural gas. Farther east is the large, imacmtonlc Cham- overviews three production Parena Basin which extends wuthweatdy from Paraguay areas (Indonesia, North Sea and Brazil. To date it has proved to be WenBf hydrocarbons. and Argentine) and directdl Along the western and southern margins of thesnlarged the exploration activity in lulesozoic continental mass of Argentina ie a saries of marina nine exploration contract basins which were present prior to We EoHloian and onset of areas. He received a B.S. subduction of the PeciPicplataduriw(hp Ladr hawob/Early degree ingedogyfromSfan- Tertiary. These western, leading kjnawere wiginally ford University in 1968 and simple in format end structural sQde untll zheowrpfimdf the an M.S. degree in geology Andean Orogeny and associated -rd-verging over- from the University of thrusts deformed their wastern margins. To varying degrees. Colorado in 1961. Since all of the marginal cretonic beaina have proved lo be hydro- 1983. he has been Adjunct Research Professor in the Earth carbon-bearing, inclwlingrecentdiawverieain the Megallanas/ Sciences and Resources Institute at the University of South Malvinas area. -
In the Mediterranean
Project FAO-COPEMED / Grandes Pelágicos’2000 SUBSCRIPT OBJETIVE 1 OBJECTIVE 1 : HIDROGRAPHICAL DESCRIPTION ......................................................2 GENERAL CIRCULATION IN THE MEDITERRANEAN................................................2 1. Circulation of Atlantic water ......................................................................................3 2. Circulation of Levantine Intermediate Water.............................................................6 STRAIT HIDROLOGY .....................................................................................................8 1. Salinity........................................................................................................................8 2. Temperature................................................................................................................8 3. Currents ......................................................................................................................9 4. Tide.............................................................................................................................9 ALBORAN SEA ..............................................................................................................12 CATALAN-BALEARIC..................................................................................................14 NORTH TUNISIAN COASTS ........................................................................................15 1. The Gulf of Tunis .....................................................................................................16 -
Investment Opportunities in Africa
A PUBLICATION BY THE AFRICAN AMBASSADORS GROUP IN CAIRO INVESTMENT OPPORTUNITIES IN AFRICA In collaboration with the African Export-Import Bank (Afreximbank) A PUBLICATION BY THE AFRICAN AMBASSADORS GROUP IN CAIRO INVESTMENT OPPORTUNITIES IN AFRICA © Copyright African Ambassadors Group in Cairo, 2018. All rights reserved. African Ambassadors Group in Cairo Email: [email protected] This publication was produced by the African Ambassadors Group in Cairo in collaboration with the African Export-Import Bank (Afreximbank) TABLE OF CONTENTS FOREWORD 8 VOTE OF THANKS 10 INTRODUCTION 12 THE PEOPLE’S DEMOCRATIC REPUBLIC OF ALGERIA 14 THE REPUBLIC OF ANGOLA 18 BURKINA FASO 22 THE REPUBLIC OF BURUNDI 28 THE REPUBLIC OF CAMEROON 32 THE REPUBLIC OF CHAD 36 THE UNION OF COMOROS 40 THE DEMOCRATIC REPUBLIC OF THE CONGO 44 THE REPUBLIC OF CONGO 50 THE REPUBLIC OF CÔTE D’IVOIRE 56 THE REPUBLIC OF DJIBOUTI 60 THE ARAB REPUBLIC OF EGYPT 66 THE STATE OF ERITREA 70 THE FEDERAL DEMOCRATIC REPUBLIC OF ETHIOPIA 74 THE REPUBLIC OF EQUATORIAL GUINEA 78 THE GABONESE REPUBLIC 82 THE REPUBLIC OF GHANA 86 THE REPUBLIC OF GUINEA 90 THE REPUBLIC OF KENYA 94 THE REPUBLIC OF LIBERIA 98 THE REPUBLIC OF MALAWI 102 THE REPUBLIC OF MALI 108 THE REPUBLIC OF MAURITIUS 112 THE KINGDOM OF MOROCCO 116 THE REPUBLIC OF MOZAMBIQUE 120 THE REPUBLIC OF NAMIBIA 126 THE REPUBLIC OF NIGER 130 THE FEDERAL REPUBLIC OF NIGERIA 134 THE REPUBLIC OF RWANDA 138 THE REPUBLIC OF SIERRA LEONE 144 THE FEDERAL REPUBLIC OF SOMALIA 148 THE REPUBLIC OF SOUTH AFRICA 152 THE REPUBLIC OF SOUTH SUDAN 158 THE REPUBLIC OF THE SUDAN 162 THE UNITED REPUBLIC OF TANZANIA 166 THE REPUBLIC OF TUNISIA 170 THE REPUBLIC OF UGANDA 174 THE REPUBLIC OF ZAMBIA 178 THE REPUBLIC OF ZIMBABWE 184 ABOUT AFREXIMBANK 188 FOREWORD Global perception on Africa has positively evolved.