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Addressing the Atlantic's Emerging Security Challenges
34 Addressing the Atlantic’s Emerging Security Challenges Bruno Lété The German Marshall Fund of the United States ABSTRACT As the Atlantic space is expected to continue to play a global role, it is not surprising that nations around the Atlantic have become increasingly concerned about securing the region’s commons at land, at sea, and in the air. In much contrast to the territorial disputes and military tensions defining the Pacific Rim, the Atlantic remains a relatively stable geo-political sphere, largely due to the lack of great power conflict. But the prominence of the region in security and military considerations is rising, especially with the aim to combat illegal activities. This paper identifies three emerging security challenges that may jeopardize the future peace and prosperity of all the countries surrounding the Atlantic Ocean if they are left unresolved. The first draft of this Scientific Paper was presented at the ATLANTIC FUTURE Seminar, Lisbon, 24 April 2015 ATLANTIC FUTURE SCIENTIFIC PAPER 34 Table of contents 1. Introduction ..................................................................................................... 3 2. The Atlantic remains a key region in a rapidly changing global system ...................................................................................................... 3 3. Three emerging challenges affect security in the Atlantic ....... 4 4. A pan-Atlantic approach is lacking ...................................................... 9 5. Conclusion .................................................................................................. -
THE DEVELOPMENT of MESOZOIC SEDIMENTARY IBASINS AROUND the MARGINS of the NORTH ATLANTIC and THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R
INTERNAL DOCUMENT IIL THE DEVELOPMENT OF MESOZOIC SEDIMENTARY IBASINS AROUND THE MARGINS OF THE NORTH ATLANTIC AND THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R. Miles Internal Document No. 195 December 1983 [This document should not be cited in a published bibliography, and is supplied for the use of the recipient only]. iimsTit\jte of \ OCEANOGRAPHIC SCIENCES % INSTITUTE OF OCEANOGRAPHIC SCIENCES Wormley, Godalming, Surrey GU8 5UB (042-879-4141) (Director: Dr. A. S. Laughton, FRS) Bidston Observatory, Crossway, Birkenhead, Taunton, Mersey side L43 7RA Somerset TA1 2DW (051-653-8633) (0823-86211) (Assistant Director: Dr. D. E. Cartwright) (Assistant Director: M.J. Tucker) THE DEVELOPMENT OF MESOZOIC SEDIMENTARY BASINS AROUND THE MARGINS OF THE NORTH ATLANTIC AND THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R. Miles Internal Document No. 195 December 1983 Work carried out under contract to the Department of Energy This document should not be cited in a published bibliography except as 'personal communication', and is supplied for the use of the recipient only. Institute of Oceanographic Sciences, Brook Road, Wormley, Surrey GU8 SUB ABSTRACT The distribution of Mesozoic basins around the margins of the North Atlantic has been summarised, and is discussed in terms of a new earliest Cretaceous palaeogeographic reconstruction for the North Atlantic area. The Late Triassic-Early Jurassic rift basins of Iberia, offshore eastern Canada and the continental shelf of western Europe are seen to be the fragments of a formerly coherent NE trending rift system which probably formed as a result of tensional stress between Europe, Africa and North America. The separation of Europe, North America and Iberia was preceded by a Late Jurassic-Early Cretaceous rifting phase which is clearly distinct from the earlier Mesozoic rifting episode and was little influenced by it. -
O C E a N O C E a N C T I C P a C I F I C O C E a N a T L a N T I C O C E a N P a C I F I C N O R T H a T L a N T I C a T L
Nagurskoye Thule (Qanaq) Longyearbyen AR CTIC OCE AN Thule Air Base LAPTEV GR EENLA ND SEA EAST Resolute KARA BAFFIN BAY Dikson SIBERIAN BARENTS SEA SEA SEA Barrow SEA BEAUFORT Tiksi Prudhoe Bay Vardo Vadso Tromso Kirbey Mys Shmidta Tuktoyaktuk Narvik Murmansk Norilsk Ivalo Verkhoyansk Bodo Vorkuta Srednekolymsk Kiruna NORWEGIAN Urengoy Salekhard SEA Alaska Oulu ICELA Anadyr Fairbanks ND Arkhangelsk Pechora Cape Dorset Godthab Tura Kitchan Umea Severodvinsk Reykjavik Trondheim SW EDEN Vaasa Kuopio Yellowknife Alesund Lieksa FINLAND Plesetsk Torshavn R U S S Yakutsk BERING Anchorage Surgut I A NORWAY Podkamennaya Tungusk Whitehorse HUDSON Nurssarssuaq Bergen Turku Khanty-Mansiysk Apuka Helsinki Olekminsk Oslo Leningrad Magadan Yurya Churchill Tallin Stockholm Okhotsk SEA Juneau Kirkwall ESTONIA Perm Labrador Sea Goteborg Yedrovo Kostroma Kirov Verkhnaya Salda Aldan BAY UNITED KINGDOM Aluksne Yaroslavl Nizhniy Tagil Aberdeen Alborg Riga Ivanovo SEA Kalinin Izhevsk Sverdlovsk Itatka Yoshkar Ola Tyumen NORTH LATVIA Teykovo Gladkaya Edinburgh DENMARK Shadrinsk Tomsk Copenhagen Moscow Gorky Kazan OF BALTIC SEA Cheboksary Krasnoyarsk Bratsk Glasgow LITHUANIA Uzhur SEA Esbjerg Malmo Kaunas Smolensk Kaliningrad Kurgan Novosibirsk Kemerovo Belfast Vilnius Chelyabinsk OKHOTSK Kolobrzeg RUSSIA Ulyanovsk Omsk Douglas Tula Ufa C AN Leeds Minsk Kozelsk Ryazan AD A Gdansk Novokuznetsk Manchester Hamburg Tolyatti Magnitogorsk Magdagachi Dublin Groningen Penza Barnaul Shefeld Bremen POLAND Edmonton Liverpool BELARU S Goose Bay NORTH Norwich Assen Berlin -
99 UPWELLING in the GULF of GUINEA Results of a Mathematical
99 UPWELLING IN THE GULF OF GUINEA Results of a mathematical model 2 2 6 5 0 A. BAH Mécanique des Fluides géophysiques, Université de Liège, Liège (Belgium) ABSTRACT A numerical simulation of the oceanic response of an x-y-t two-layer model on the 3-plane to an increase of the wind stress is discussed in the case of the tro pical Atlantic Ocean. It is shown first that the method of mass transport is more suitable for the present study than the method of mean velocity, especially in the case of non-linearity. The results indicate that upwelling in the oceanic equatorial region is due to the eastward propagating equatorially trapped Kelvin wave, and that in the coastal region upwelling is due to the westward propagating reflected Rossby waves and to the poleward propagating Kelvin wave. The amplification due to non- linearity can be about 25 % in a month. The role of the non-rectilinear coast is clearly shown by the coastal upwelling which is more intense east than west of the three main capes of the Gulf of Guinea; furthermore, by day 90 after the wind's onset, the maximum of upwelling is located east of Cape Three Points, in good agree ment with observations. INTRODUCTION When they cross over the Gulf of Guinea, monsoonal winds take up humidity and subsequently discharge it over the African Continent in the form of precipitation (Fig. 1). The upwelling observed during the northern hemisphere summer along the coast of the Gulf of Guinea can reduce oceanic evaporation, and thereby affect the rainfall pattern in the SAHEL region. -
Countries and Their Capital Cities Cheat Sheet by Spaceduck (Spaceduck) Via Cheatography.Com/4/Cs/56
Countries and their Capital Cities Cheat Sheet by SpaceDuck (SpaceDuck) via cheatography.com/4/cs/56/ Countries and their Captial Cities Countries and their Captial Cities (cont) Countries and their Captial Cities (cont) Afghani stan Kabul Canada Ottawa Federated States of Palikir Albania Tirana Cape Verde Praia Micronesia Algeria Algiers Cayman Islands George Fiji Suva American Samoa Pago Pago Town Finland Helsinki Andorra Andorra la Vella Central African Republic Bangui France Paris Angola Luanda Chad N'Djamena French Polynesia Papeete Anguilla The Valley Chile Santiago Gabon Libreville Antigua and Barbuda St. John's Christmas Island Flying Fish Gambia Banjul Cove Argentina Buenos Aires Georgia Tbilisi Cocos (Keeling) Islands West Island Armenia Yerevan Germany Berlin Colombia Bogotá Aruba Oranjestad Ghana Accra Comoros Moroni Australia Canberra Gibraltar Gibraltar Cook Islands Avarua Austria Vienna Greece Athens Costa Rica San José Azerbaijan Baku Greenland Nuuk Côte d'Ivoire Yamous‐ Bahamas Nassau Grenada St. George's soukro Bahrain Manama Guam Hagåtña Croatia Zagreb Bangladesh Dhaka Guatemala Guatemala Cuba Havana City Barbados Bridgetown Cyprus Nicosia Guernsey St. Peter Port Belarus Minsk Czech Republic Prague Guinea Conakry Belgium Brussels Democratic Republic of the Kinshasa Guinea- Bissau Bissau Belize Belmopan Congo Guyana Georgetown Benin Porto-Novo Denmark Copenhagen Haiti Port-au -P‐ Bermuda Hamilton Djibouti Djibouti rince Bhutan Thimphu Dominica Roseau Honduras Tegucig alpa Bolivia Sucre Dominican Republic Santo -
CBD Third National Report
CONTENTS A. REPORTING PARTY ............................................................................................................... 3 Information on the preparation of the report ....................................................................... 3 B. PRIORITY SETTING, TARGETS AND OBSTACLES ....................................................................... 4 Priority Setting ................................................................................................................ 6 Challenges and Obstacles to Implementation ...................................................................... 7 2010 Target .................................................................................................................... 9 Global Strategy for Plant Conservation (GSPC) ...................................................................37 Ecosystem Approach .......................................................................................................54 C. ARTICLES OF THE CONVENTION ...........................................................................................56 Article 5 – Cooperation ....................................................................................................56 Article 6 - General measures for conservation and sustainable use ........................................58 Biodiversity and Climate Change .................................................................................60 Article 7 - Identification and monitoring .............................................................................61 -
Chapter 24. the BAY of BISCAY: the ENCOUNTERING of the OCEAN and the SHELF (18B,E)
Chapter 24. THE BAY OF BISCAY: THE ENCOUNTERING OF THE OCEAN AND THE SHELF (18b,E) ALICIA LAVIN, LUIS VALDES, FRANCISCO SANCHEZ, PABLO ABAUNZA Instituto Español de Oceanografía (IEO) ANDRE FOREST, JEAN BOUCHER, PASCAL LAZURE, ANNE-MARIE JEGOU Institut Français de Recherche pour l’Exploitation de la MER (IFREMER) Contents 1. Introduction 2. Geography of the Bay of Biscay 3. Hydrography 4. Biology of the Pelagic Ecosystem 5. Biology of Fishes and Main Fisheries 6. Changes and risks to the Bay of Biscay Marine Ecosystem 7. Concluding remarks Bibliography 1. Introduction The Bay of Biscay is an arm of the Atlantic Ocean, indenting the coast of W Europe from NW France (Offshore of Brittany) to NW Spain (Galicia). Tradition- ally the southern limit is considered to be Cape Ortegal in NW Spain, but in this contribution we follow the criterion of other authors (i.e. Sánchez and Olaso, 2004) that extends the southern limit up to Cape Finisterre, at 43∞ N latitude, in order to get a more consistent analysis of oceanographic, geomorphological and biological characteristics observed in the bay. The Bay of Biscay forms a fairly regular curve, broken on the French coast by the estuaries of the rivers (i.e. Loire and Gironde). The southeastern shore is straight and sandy whereas the Spanish coast is rugged and its northwest part is characterized by many large V-shaped coastal inlets (rias) (Evans and Prego, 2003). The area has been identified as a unit since Roman times, when it was called Sinus Aquitanicus, Sinus Cantabricus or Cantaber Oceanus. The coast has been inhabited since prehistoric times and nowadays the region supports an important population (Valdés and Lavín, 2002) with various noteworthy commercial and fishing ports (i.e. -
May 2016, Volume 5, Issue No
SharingHåfa the Håfa AdaiAdai Spirit with EverydayOur Visitors and Each Other May 2016, Volume 5, Issue No. 3 HÅFA ADAI PLEDGE CEREMONY LIVING THE HÅFA ADAI PLEDGE Creative indeed Fresh New Local Restaurant Three Squares Guam joins the Håfa Adai Pledge familia Håfa Adai Pledge signing ceremony held at Three Squares Restaurant Guam in Tamuning on Wednesday, April 20. Standing L-R: Rose Q. Cunlie, Guam Visitors Bureau, Director of Finance and Administration; Telo T. Taitague, Guam Visitors Bureau, Vice President; Marie Nededog Guerrero, Three Squares by B&G Pacific, LLC, Owner and CEO; Frank Guerrero, Three Squares by B&G Pacific, LLC, Representative; Nate Denight, Guam Visitors Bureau, President and Chief Executive Ocer and Pilar Laguana, Guam Visitors Bureau, Director of Global Marketing. Michelle Pier, owner and CEO of Creative Indeed. An independent artist and entrepreneur born on the island of Guam, Michelle Pier is known for her mesmerizing original acrylic paintings that incorporates GUAMPEDIA: Johnny Sablan the beauty of Guam. Pier has exhibited and sold hundreds of paintings locally and internationally. She is also known for establishing many of the local craft Keeping Chamorro culture through music fairs, festivals and other community events such as the Annual Luna Festival and Annual Holiday Craft Fair. It is through these events that inspires creativity among hundreds of local individuals, businesses and organizations. In Pier’s eorts, she has helped the local people to reconnect with their creativity and encourage them to create unique careers. It is also through these events that help connect local entrepreneurs and the community and to interact to promote “buy local”. -
Names of Sub-Areas and Divisions of FAO Fishing Areas 27 and 37 NORTH-EAST ATLANTIC
Names of Sub-areas and Divisions of FAO fishing areas 27 and 37 NORTH-EAST ATLANTIC Subarea I Barents Sea Subarea II Norwegian Sea, Spitzbergen, and Bear Island Division II a Norwegian Sea Division II b Spitzbergen and Bear Island Subarea III Skagerrak, Kattegat, Sound, Belt Sea, and Baltic Sea; the Sound and Belt together known also as the Transition Area Division III a Skagerrak and Kattegat Division III b,c Sound and Belt Sea or Transition Area Division III b (23) Sound Division III c (22) Belt Sea Division III d (24-32) Baltic Sea Subarea IV North Sea Division IV a Northern North Sea Division IV b Central North Sea Division IV c Southern North Sea Subarea V Iceland and Faroes Grounds Division V a Iceland Grounds Division V b Faroes Grounds Subarea VI Rockall, Northwest Coast of Scotland and North Ireland, the Northwest Coast of Scotland and North Ireland also known as the West of Scotland Division VI a Northwest Coast of Scotland and North Ireland or West of Scotland Division VI b Rockall Subarea VII Irish Sea, West of Ireland, Porcupine Bank, Eastern and Western English Channel, Bristol Channel, Celtic Sea North and South, and Southwest of Ireland - East and West Division VII a Irish Sea Division VII b West of Ireland Division VII c Porcupine Bank Division VII d Eastern English Channel Division VII e Western English Channel Division VII f Bristol Channel Division VII g Celtic Sea North Division VII h Celtic Sea South Division VII j South-West of Ireland - East Division VII k South-West of Ireland - West Subarea VIII Bay of Biscay -
195 the Gulf of Guinea
THE GULF OF GUINEA: THE NEW DANGER ZONE Africa Report N°195 – 12 December 2012 Translation from French TABLE OF CONTENTS EXECUTIVE SUMMARY AND RECOMMENDATIONS ................................................. i I. INTRODUCTION ............................................................................................................. 1 II. A STRATEGIC REGION IN THE GRIP OF INSECURITY ...................................... 2 A. RENEWED STRATEGIC INTEREST IN NATURAL RESOURCES .......................................................... 2 B. A CONTEXT FAVOURABLE TO MARITIME CRIME ......................................................................... 3 C. WEAK MARITIME POLICIES .......................................................................................................... 4 III. NIGERIA: EPICENTRE OF VIOLENCE AT SEA ...................................................... 6 A. POOR GOVERNANCE AND MARITIME CRIME ................................................................................ 6 1. A leaky oil sector ......................................................................................................................... 6 2. The rise in economic crime .......................................................................................................... 7 3. State capacity hampered by corruption ........................................................................................ 8 4. The Niger Delta ........................................................................................................................... -
4 European Policy and Energy Interests – Challenges from the Gulf of Guinea ␣
CHAPTER I OIL POLICY IN THE GULF OF GUINEA 4 European Policy and Energy Interests – Challenges from the Gulf of Guinea ␣ By Lutz Neumann 1. Introduction ␣ The Gulf of Guinea has great oil and gas potential. While predictions on Africa should be made with some care, analysts and representatives of the oil industry appear to agree that the region belongs to those areas where production will rapidly increase in the coming years and decades. Output figures of the chief oil- producing countries, Nigeria and Angola, are expected to double or triple within the next decade and thus will cause certain dynamics on the shaping of trade movements (see table 1). Table 1: Projected Oil Production of Gulf of Guinea 2005-2030 (in b/d) 2005 2010 2015 2030 Nigeria 2,719,000 3,042,000 3,729,000 4,422,000 Angola 1,098,000 2,026,000 2,549,000 3,288,000 Equatorial-Guinea 313,000 466,000 653,000 724,000 Congo (Brazzaville) 285,000 300,000 314,000 327,000 Gabon 303,000 291,000 279,000 269,000 Côte d’Ivoire 43,000 71,000 83,000 94,000 Cameroun 84,000 72,000 66,000 61,000 Congo (Kinshasa) 30,000 33,000 30,000 25,000 Ghana 11,000 16,000 20,000 23,000 Total Africa 9,936,000 12,059,000 13,975,000 16,242,000 Source: EIA, U.S. Department of Energy.␣ FRIEDRICH-EBERT-STIFTUNG 59 OIL POLICY IN THE GULF OF GUINEA CHAPTER I The African countries along the Atlantic coast represent a growing supplier region. -
Influence of the Gulf of Guinea Coastal and Equatorial Upwellings on the Precipitations Along Its Northern Coasts During the Boreal Summer Period
Asian Journal of Applied Sciences 4 (3): 271-285, 2011 ISSN 1996-3343 I DOI: 10.3923/ajaps.2011.271.285 © 2011 Knowledgia Review, Malaysia Influence of the Gulf of Guinea Coastal and Equatorial Upwellings on the Precipitations along its Northern Coasts during the Boreal Summer Period 'K.E. Ali, 'K.Y. Kouadio, 'E.-P. Zahiri, 'A. Aman, 'A.P. Assamoi and 2B. Bourles 'LAPAMF, Universite de Cocody-Abidjan BP 231 Abidjan, Cote d'Ivoire 2IRD/LEGOS-CRHOB, Representation !RD, 08 BP 841 Cotonou, Republique du Benin Corresponding Author: Angora Aman, Universite de Cocody-Abidjan 22 BP 582 Abidjan 22, LAPA-MF, UFR-SSMT, Cote d'Ivoire Tel: (225) 07 82 77 52 Fax: (225) 22 44 14 07 ABSTRACT The Gulf of Guinea (GG) is an area where a seasonal upwelling takes place, along the equator and its northern coasts between Benin and Cote d'Ivoire. The coastal upwelling has a real impact on the local yet documented biological resources. However, climatic impact studies of this seasonal upwelling are paradoxically very rare and disseminated and this impact is still little known, especially on the potential part played by the upwelling onset on the regional precipitation in early boreal summer. This study shows that coastal precipitations of the July-September period are correlated by both the coastal and equatorial sea-surface temperatures (SSTS). This correlation results in a decrease or a rise of rainfall when the SSTs are abnormally cold or warm respectively. The coastal areas that are more subject to coastal and equatorial SSTs influence are located around the Cape Three Points, where the coastal upwelling exhibits the maximum of amplitude.