If You Choose to Sail Upon the Seas of Banking, Build Your Bank As You Would Your Boat, with the Strength to Sail Safely Through Any Storm.”
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Strengthening Protected Area System of the Komi Republic to Conserve Virgin Forest Biodiversity in the Pechora Headwaters Region
Strengthening Protected Area System of the Komi Republic to Conserve Virgin Forest Biodiversity in the Pechora Headwaters Region PIMS 2496, Atlas Award 00048772, Atlas Project No: 00059042 Terminal Evaluation, Volume I November 2014 Russian Federation GEF SO1: Catalysing the Sustainability of Protected Areas SP3: Strengthened National Terrestrial Protected Area Networks Russian Federation, Ministry of Natural Resources Komi Republic, Ministry of Natural Resources United National Development Program Stuart Williams KOMI REPUBLIC PAS PROJECT - TE Acknowledgements The mission to the Komi Republic was well organised and smoothly executed. For this, I would like to thank everyone involved starting with Irina Bredneva and Elena Bazhenova of the UNDP-CO for making all the travel arrangements so smooth and easy, and making me welcome in Moscow. In the Komi Republic, the project team ensured that I met the right stakeholders, showed me the results of the project efforts in remote and beautiful areas of the republic, and accompanying me. Special thanks are due to Alexander Popov (the National Project Director) and Vasily Ponomarev (the Project Manager) for the connections, arrangements, for accompanying me and for many fruitful discussions. Other team members who accompanied the mission included Svetlana Zagirova, Andrei Melnichuk and Anastasiya Tentyukova. I am also grateful to all the other stakeholders who gave freely of their time and answered my questions patiently (please see Annex III for a list of all the people met over the course of the mission to the Komi Republic). I am also particularly grateful for the tireless efforts of Alexander Oshis, my interpreter over the course of the mission even when he was not well, for the clear and accurate interpretation. -
Arctic Expedition12° 16° 20° 24° 28° 32° Spitsbergen U Svalbard Archipelago 80° 80°
distinguished travel for more than 35 years Voyage UNDER THE Midnight Sun Arctic Expedition12° 16° 20° 24° 28° 32° Spitsbergen u Svalbard Archipelago 80° 80° 80° Raudfjorden Nordaustlandet Woodfjorden Smeerenburg Monaco Glacier The Arctic’s 79° 79° 79° Kongsfjorden Svalbard King’s Glacier Archipelago Ny-Ålesund Spitsbergen Longyearbyen Canada 78° 78° 78° i Greenland tic C rcle rc Sea Camp Millar A U.S. North Pole Russia Bellsund Calypsobyen Svalbard Archipelago Norway Copenhagen Burgerbukta 77° 77° 77° Cruise Itinerary Denmark Air Routing Samarin Glacier Hornsund Barents Sea June 20 to 30, 2022 4° 8° Spitsbergen12° u Samarin16° Glacier20° u Calypsobyen24° 76° 28° 32° 36° 76° Voyage across the Arctic Circle on this unique 11-day Monaco Glacier u Smeerenburg u Ny-Ålesund itinerary featuring a seven-night cruise round trip Copenhagen 1 Depart the U.S. or Canada aboard the Five-Star Le Boréal. Visit during the most 2 Arrive in Copenhagen, Denmark enchanting season, when the region is bathed in the magical 3 Copenhagen/Fly to Longyearbyen, Spitsbergen, light of the Midnight Sun. Cruise the shores of secluded Norway’s Svalbard Archipelago/Embark Le Boréal 4 Hornsund for Burgerbukta/Samarin Glacier Spitsbergen—the jewel of Norway’s rarely visited Svalbard 5 Bellsund for Calypsobyen/Camp Millar archipelago enjoy expert-led Zodiac excursions through 6 Cruising the Arctic Ice Pack sandstone mountain ranges, verdant tundra and awe-inspiring 7 MåkeØyane/Woodfjorden/Monaco Glacier ice formations. See glaciers calve in luminous blues and search 8 Raudfjorden for Smeerenburg for Arctic wildlife, including the “King of the Arctic,” the 9 Ny-Ålesund/Kongsfjorden for King’s Glacier polar bear, whales, walruses and Svalbard reindeer. -
Determination Report
DETERMINATION REPORT CLIMATE CHANGE GLOBAL SERVICES (CCGS) Determination Report on JI Project “Evaporation System Modernization at OJSC “Ilim Group” Branch in Koryazhma” RUSSIAN FEDERATION BUREAU VERITAS CERTIFICATION REPORT NO. RUSSIA /0023/2009, REV . 01 Report Template Revision 4, 28/09/2007 BUREAU VERITAS CERTIFICATION Report No: RUSSIA/0023-1/2009 rev. 01 DETERMINATION REPORT Date of first issue: Organizational unit: 18/05/2009 Bureau Veritas Certification Holding SAS Client: Client ref.: CCGS Ltd. Mr. Dmitry Potashev Summary: Bureau Veritas Certification has made the determination of the project “Evapor ation System modernization at OJSC “Ilim Group” Branch in Koryazhma”, on the basis of UNFCCC criteria for the JI, as well as criteria given to provide for consistent project operations, monitoring and reporting. UNFCCC criteria refer to Article 6 of the Kyoto Protocol, the JI guidelines and the subsequent decisions by the JI Supervisory Committee, as well as the host country criteria. The determination is carried out under Track 1 as per Glossary of JI terms, in line with paragraph 23 of the JI guidelines. The determination scope is defined as an independent and objective review of the project design document, the project’s baseline, monitoring plan and other relevant documents, and consists of the following three phases: i) desk review of the project design document and particularly the baseline and monitoring plan; ii) follow-up interviews with project stakeholders; iii) resolution of outstanding issues and the issuance of the final determination report and opinion. The overall determination, from Contract Review to Determination Report & Opinion, was conducted using Bureau Veritas Certification internal procedures. -
Market Risk Index 120 Amundsen Sea 90 60 30 0 30 60 90 120
COUNTRY RISK MAP 2010 150 120 90 60 30 0 30 60 90 120 150 180 ARCTIC OCEAN FRANZ JOSEF ARCTIC OCEAN LAND SEVERNAYA ARCTIC OCEAN ZEMLYA Ellesmere Island QUEEN ELIZABETH Longyearbyen NEW SIBERIAN ISLANDS Svalbard NOVAYA Kara Sea ISLANDS Greenland Sea ZEMLYA Laptev Sea Banks (NORWAY) Barents Sea Island Greenland East Siberian Sea Beaufort Sea Ban Wrangel (DENMARK) Island Victoria Bay Island Ban Jan Mayen Norwegian Chukchi (NORWAY) Island Sea Sea Arctic Circle (66°33') Arctic Circle (66°33') NORWAY Great Nuuk ICELAND White Sea U. S. Bear Lake (Godthåb) SWEDEN Provideniya Davis Denmark Strait Reykjavík Faroe Islands FINLAND Lake Strait (DEN.) Gulf R U S S I A Tórshavn of Ladoga Lake Great Bothnia Onega Slave Lake Hudson Oslo Helsinki 60 60 Bay Stockholm Tallinn Gulf of Alaska Rockall EST. Labrador (U.K.) Baltic Bering Sea Riga S North Sea LAT. Sea DENMARK Moscow Sea Copenhagen LITH. Lake RUSSIA Sea of C A N A D A UNITED Vilnius Baikal S Minsk N D Dublin Isle of KINGDOM S Okhotsk LA Man IS (U.K.) BELARUS T IA N Lake IRELAND Amsterdam Berlin Warsaw U.S. LE U Winnipeg Kamchatskiy A NETH. Astana Sakhalin A Island of L D S London Brussels POLAND E U T A N GERMANY Prague Kyiv I A N I S L Newfoundland Celtic BELGIUM LUX. Sea Guernsey (U.K.) Luxembourg CZECH REP. U K R A I N E Jersey (U.K.) SLOVAKIA Gulf of Paris Vienna Bratislava S K A Z A K H S T A N Ulaanbaatar KURIL Lake St. -
Mozambique Zambia South Africa Zimbabwe Tanzania
UNITED NATIONS MOZAMBIQUE Geospatial 30°E 35°E 40°E L a k UNITED REPUBLIC OF 10°S e 10°S Chinsali M a l a w TANZANIA Palma i Mocimboa da Praia R ovuma Mueda ^! Lua Mecula pu la ZAMBIA L a Quissanga k e NIASSA N Metangula y CABO DELGADO a Chiconono DEM. REP. OF s a Ancuabe Pemba THE CONGO Lichinga Montepuez Marrupa Chipata MALAWI Maúa Lilongwe Namuno Namapa a ^! gw n Mandimba Memba a io u Vila úr L L Mecubúri Nacala Kabwe Gamito Cuamba Vila Ribáué MecontaMonapo Mossuril Fingoè FurancungoCoutinho ^! Nampula 15°S Vila ^! 15°S Lago de NAMPULA TETE Junqueiro ^! Lusaka ZumboCahora Bassa Murrupula Mogincual K Nametil o afu ezi Namarrói Erego e b Mágoè Tete GiléL am i Z Moatize Milange g Angoche Lugela o Z n l a h m a bez e i ZAMBEZIA Vila n azoe Changara da Moma n M a Lake Chemba Morrumbala Maganja Bindura Guro h Kariba Pebane C Namacurra e Chinhoyi Harare Vila Quelimane u ^! Fontes iq Marondera Mopeia Marromeu b am Inhaminga Velha oz P M úngu Chinde Be ni n è SOFALA t of ManicaChimoio o o o o o o o o o o o o o o o gh ZIMBABWE o Bi Mutare Sussundenga Dondo Gweru Masvingo Beira I NDI A N Bulawayo Chibabava 20°S 20°S Espungabera Nova OCE A N Mambone Gwanda MANICA e Sav Inhassôro Vilanculos Chicualacuala Mabote Mapai INHAMBANE Lim Massinga p o p GAZA o Morrumbene Homoíne Massingir Panda ^! National capital SOUTH Inhambane Administrative capital Polokwane Guijá Inharrime Town, village o Chibuto Major airport Magude MaciaManjacazeQuissico International boundary AFRICA Administrative boundary MAPUTO Xai-Xai 25°S Nelspruit Main road 25°S Moamba Manhiça Railway Pretoria MatolaMaputo ^! ^! 0 100 200km Mbabane^!Namaacha Boane 0 50 100mi !\ Bela Johannesburg Lobamba Vista ESWATINI Map No. -
11010329.Pdf
THE RISE, CONSOLIDATION AND DISINTEGRATION OF DLAMINI POWER IN SWAZILAND BETWEEN 1820 AND 1889. A study in the relationship of foreign affairs to internal political development. Philip Lewis Bonner. ProQuest Number: 11010329 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 11010329 Published by ProQuest LLC(2018). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106- 1346 ABSTRACT The Swazi kingdom grew out of the pressures associated with competition for trade and for the rich resources of Shiselweni. While centred on this area it acquired some of its characteristic features - notably a regimental system, and the dominance of a Dlamini aristocracy. Around 1815 the Swazi came under pressure from the South, and were forced to colonise the land lying north of the Lusutfu. Here they remained for some years a nation under arms, as they plundered local peoples, and were themselves swept about by the currents of the Mfecane. In time a more settled administration emerged, as the aristocracy spread out from the royal centres at Ezulwini, and this process accelerated under Mswati as he subdued recalcitrant chiefdoms, and restructured the regiments. -
Shadwick, E. H., Et Al. Seasonal Variability of the Inorganic Carbon
Limnol. Oceanogr., 56(1), 2011, 303–322 E 2011, by the American Society of Limnology and Oceanography, Inc. doi:10.4319/lo.2011.56.1.0303 Seasonal variability of the inorganic carbon system in the Amundsen Gulf region of the southeastern Beaufort Sea E. H. Shadwick,a,* H. Thomas,a M. Chierici,b B. Else,c A. Fransson,d C. Michel,e L. A. Miller,f A. Mucci,g A. Niemi,e T. N. Papakyriakou,c and J.-E´ . Tremblayh a Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada bDepartment of Chemistry, University of Gothenburg, Go¨teborg, Sweden c Center for Earth Observation Science, University of Manitoba, Winnipeg, Manitoba, Canada dDepartment of Earth Sciences, University of Gothenburg, Go¨teborg, Sweden e Freshwater Institute, Fisheries and Oceans Canada, Winnipeg, Manitoba, Canada f Institute of Ocean Sciences, Fisheries and Oceans Canada, Sidney, British Columbia, Canada g Department of Earth and Planetary Sciences, McGill University, Montreal, Que´bec, Canada hDepartment de Biologie, Universite´ Laval, Que´bec, Que´bec, Canada Abstract During a year-round occupation of Amundsen Gulf in the Canadian Arctic Archipelago dissolved inorganic and organic carbon (DIC, DOC), total alkalinity (TA), partial pressure of CO2 (pCO2) and related parameters were measured over a full annual cycle. A two-box model was used to identify and assess physical, biological, and chemical processes responsible for the seasonal variability of DIC, DOC, TA, and pCO2. Surface waters were undersaturated with respect to atmospheric CO2 throughout the year and constituted a net sink of 22 21 1.2 mol C m yr , with ice coverage and ice formation limiting the CO2 uptake during winter. -
Marine Mammals and Sea Turtles of the Mediterranean and Black Seas
Marine mammals and sea turtles of the Mediterranean and Black Seas MEDITERRANEAN AND BLACK SEA BASINS Main seas, straits and gulfs in the Mediterranean and Black Sea basins, together with locations mentioned in the text for the distribution of marine mammals and sea turtles Ukraine Russia SEA OF AZOV Kerch Strait Crimea Romania Georgia Slovenia France Croatia BLACK SEA Bosnia & Herzegovina Bulgaria Monaco Bosphorus LIGURIAN SEA Montenegro Strait Pelagos Sanctuary Gulf of Italy Lion ADRIATIC SEA Albania Corsica Drini Bay Spain Dardanelles Strait Greece BALEARIC SEA Turkey Sardinia Algerian- TYRRHENIAN SEA AEGEAN SEA Balearic Islands Provençal IONIAN SEA Syria Basin Strait of Sicily Cyprus Strait of Sicily Gibraltar ALBORAN SEA Hellenic Trench Lebanon Tunisia Malta LEVANTINE SEA Israel Algeria West Morocco Bank Tunisian Plateau/Gulf of SirteMEDITERRANEAN SEA Gaza Strip Jordan Suez Canal Egypt Gulf of Sirte Libya RED SEA Marine mammals and sea turtles of the Mediterranean and Black Seas Compiled by María del Mar Otero and Michela Conigliaro The designation of geographical entities in this book, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN. Published by Compiled by María del Mar Otero IUCN Centre for Mediterranean Cooperation, Spain © IUCN, Gland, Switzerland, and Malaga, Spain Michela Conigliaro IUCN Centre for Mediterranean Cooperation, Spain Copyright © 2012 International Union for Conservation of Nature and Natural Resources With the support of Catherine Numa IUCN Centre for Mediterranean Cooperation, Spain Annabelle Cuttelod IUCN Species Programme, United Kingdom Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the sources are fully acknowledged. -
World Cruise - 2022 Use the Down Arrow from a Form Field
This document contains both information and form fields. To read information, World Cruise - 2022 use the Down Arrow from a form field. 20 world JAN 5, 2022 JAN 19, 2022 JAN 19, 2022 JAN 5, 2022 111 days 111 days 97 days 88 days 22 cruise roundtrip from roundtrip from Los Angeles to Ft. Lauderdale Ft. Lauderdale Los Angeles Ft. Lauderdale to Rome Florence/Pisa (Livorno) Genoa Rome (Civitavecchia) Catania Monte Carlo (Sicily) MONACO ITALY Naples Marseille Mykonos FRANCE GREECE Kusadasi PORTUGAL Atlantic Barcelona Heraklion Ocean SPAIN (Crete) Los Angeles Lisbon TURKEY UNITED Bermuda Ceuta Jerusalem/Bethlehem STATES (West End) (Spanish Morocco) Seville (Ashdod) ine (Cadiz) ISRAEL Athens e JORDAN Dubai Agadir (Piraeus) Aqaba Pacific MEXICO Madeira UNITED ARAB Ocean MOROCCO l Dat L (Funchal) Malta EMIRATES Ft. Lauderdale CANARY (Valletta) Suez Abu ISLANDS Canal Honolulu Huatulco Dhabi ne inn Puerto Santa Cruz Lanzarote OMAN a a Hawaii r o Hilo Vallarta NICARAGUA (Arrecife) de Tenerife Salãlah t t Kuala Lumpur I San Juan del Sur Cartagena (Port Kelang) Costa Rica COLOMBIA Sri Lanka PANAMA (Puntarenas) Equator (Colombo) Singapore Equator Panama Canal MALAYSIA INDONESIA Bali SAMOA (Benoa) AMERICAN Apia SAMOA Pago Pago AUSTRALIA South Pacific South Indian Ocean Atlantic Ocean Ocean Perth Auckland (Fremantle) Adelaide Sydney New Plymouth Burnie Picton Departure Ports Tasmania Christchurch More Ashore (Lyttelton) Overnight Fiordland NEW National Park ZEALAND up to continentscontinents (North America, South America, 111 51 Australia, Europe, Africa -
Information to Users
INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely afreet reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back of the book. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. University Microfilms International A Beil & Howell Information Company 300 North Zeeb Road. Ann Arbor. Ml 48106-1346 USA 313/761-4700 800/521-0600 Order Number 0211125 A need to know: The role of Air Force reconnaissance in war planning, 1045-1953 Farquhar, John Thomas, Ph.D. The Ohio State University, 1991 Copyright ©1001 by Farquhar, John Thomas. -
Trace Elements and Stable Isotope Diagrams of Late Pleistocene Ice Wedges of Batagaika Yedoma, Central Yakutia
Trace elements and stable isotope diagrams of Late Pleistocene ice wedges of Batagaika yedoma, Central Yakutia Yu.K.Vasil'chuk1 J.Yu.Vasil'chuk1 N. A. Budantseva1 A.C. Vasil'chuk1 1Department of Geography, Lomonosov Moscow State University, Moscow, Russia, e-mail: [email protected] Abstract The subject of the study is the yedoma ice complex, which locates in the Batagaika depression, Sakha Republic, Russia. The oxygen and hydrogen stable isotope composition, and the content of the dissolved forms of minor and major elements were studied for the first time in ice-wedges of Batagaika depression, which makes the novelty of the study. The isotope composition of the two most saline ice-wedges located in the upper and lower parts of the Batagay depression indicates that they were formed in a close temperature range, the average winter temperature was close to –34/–35 °C, and the average January air temperature was –51/ –53 °C. The ice-wedge with the lowest content of all the trace elements was formed in more severe conditions, the average winter air temperature was close to -36 °C, and the average January air temperature was –54/–55 °C. Keywords: permafrost; ice wedge; oxygen isotope; hydrogen isotope; trace elements; East Siberia, Late Pleistocene The subject of the study is the yedoma, which is found lacustrine or taberal deposits, which are form horizontal in the Batagaika depression (67°34'49" N, 134°46'19" E), wedge 150-200 meters long and intruding into the located 10 km southeast of Batagai settlement (about 17 yedoma deposits and overlaying it. -
Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (marked ‘cp’).