Temporal and Spatial Variations in the Long-Term Fluctuations of Wildlife Populations in Greenland
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Eske Brun Og Det Moderne Grønlands Tilblivelse 1932 – 64
Eske Brun og det moderne Grønlands tilblivelse 1932 – 64 Ph.d.-afhandling af Jens Heinrich, juni 2010 Hovedvejleder dr. phil., lektor Thorkild Kjærgaard, Ilisimatusarfik Bivejleder ph.d. Søren Forchhammer I tilknytning til Ilisimatusarfik/Grønlands Univesitet KVUG (Kommissionen for Videnskabelige Undersøgelser i Grønland) Forside foto – Eske Brun, ca. 1940 © Nunatta Katersugaasivia/Grønlands Nationalmuseum Johan Carl Brun Gotfred Hansen (1711-75) læge (1765-1835) Stamtræ vinhandler Kilde DBL Constantin Brun (Brun og Hansen, (1746-1836) storkøbmand Nb. - ikke alle er inkluderet) Andreas Nicolai Hansen (1798-1873) Carl Frederik Balthazar Brun Ida de Bombelles f. Brun grosserer (1784-1869) godsejer, kammerherre (1792-1857) kunstner Petrus Friederich (Fritz) Constantin Alexander Brun Carl A. A. F. J. Brun Alfred Peter Hansen Octavius Hansen James Gustav Hansen Brun (1813-1888) amtmand (1814-1893) (1824-1898) (1829-1893) (1838-1903) (1843-1912) biavler, landmand generalmajor ingeniør politiker, grosserer, politiker, etatsråd sagfører Oscar Brun Axel Brun Erik Brun Constantin Brun Charles Brun Rigmor Hansen Ingeborg Hansen (1851-1921) (1870-1958) (1867-1915) (1860-1945) (1866-1919) (1875-1948) (1873-1949) landmand, politiker læge læge diplomat amtmand, politiker Carl Brun (1897-1958) Eske Brun diplomat (1904-1987) Departementschef Gift i 1937 med Ingrid f. Winkel (1911-) Tre børn; Johan (1938-), Christian (1940-) og Ida (1942- ) Eske Brun og det moderne Grønlands tilblivelse 1932-1964 Indholdsfortegnelse Forord ................................................................................................................................................ -
Sheep Farming As “An Arduous Livelihood”
University of Alberta Cultivating Place, Livelihood, and the Future: An Ethnography of Dwelling and Climate in Western Greenland by Naotaka Hayashi A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Anthropology ©Naotaka Hayashi Spring 2013 Edmonton, Alberta Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission. Abstract In order to investigate how Inuit Greenlanders in western Greenland are experiencing, responding to, and thinking about recent allegedly human-induced climate change, this dissertation ethnographically examines the lives of Greenlanders as well as Norse and Danes in the course of past historical natural climate cycles. My emphasis is on human endeavours to cultivate a future in the face of difficulties caused by climatic and environmental transformation. I recognize locals’ initiatives to carve out a future in the promotion of sheep farming and tree-planting in southern Greenland and in adaptation processes of northern Greenlandic hunters to the ever-shifting environment. -
Information About Greenland
INFORMATION ABOUT GREENLAND Temperatures Because the air in Greenland is very dry and does not have as much humidity as air on the European continent, the temperatures are perceived differently. –10 degrees Celsius will feel equivalent to +10-12 degrees on the continent. Aurora Borealis – Northern lights Aurora Borealis is exhibited all year round, and can be observed in dark and clear night skies. Aurora Borealis is a fascinating phenomenon that arises from electrical discharges made by the sun, which interact with the magnetic conditions and the atmosphere above the polar region. Purple, red, white, yellow and green lights are either seen moving across the sky as a waving curtain, or they are seen as radiating from a single point in the sky. Remember that in the summer the sun is up all day and night or at least it doesn’t get dark enough to be able to see the Northern lights. Midnight sun North of the Polar Circle the midnight sun rules from May to July, inspiring new ways of living - because how morning is defined when the sun never sets? South of the Polar Circle and in other summer periods the nights are bright but without the sun exactly shining. This is also a spectacular experience. Time zone The Greenlandic time zone is –4 hours CET. When it is midday in Greenland, it is 16.00 hours in Copenhagen, Frankfurt and Paris, 15.00 hours in London and 10.00 hours in New York. All time indications in programme are local times. By departure from Copenhagen at 9.15AM you arrive in Greenland 9.55AM (depending of air craft). -
Afvikling Af Grønlands Kolonistatus 1945-54
Afvikling af Grønlands kolonistatus 1945-54 En historisk udredning DANSK INSTITUT FOR INTERNATIONALE STUDIER 2007 © København 2007 Dansk Institut for Internationale Studier Strandgade 56 1401 København K Danmark Tlf.:+4532698787 Fax: +4532698700 E-mail: [email protected] Web: www.diis.dk ISBN Printudgave (denne udgave) 978-87-7605-186-0 Bogudgave 978-87-7605-187-7 Denne printudgave er ikke i handelen Teksten kan downloades gratis fra www.diis.dk (fra 18. januar 2007) Bogudgaven kan købes i boghandelen fra ca. 1. marts 2007 Indhold Indledning ̗7 2. Grønland og Danmark før 1945ʳ Θʳ10 Indledning ʳΘʳ10 Grønland som dansk koloniʳΘʳ10 Grønland mellem Nordamerika og Europa: 2. verdenskrigʳΘʳ16 2. verdenskrig som et vendepunkt ʳΘʳ23 3. Grønlandsspørgsmålet mellem suverænitet, selvbestemmelse og afhængighedΘ26 Indledning ʳΘʳ26 Suverænitet ʳΘʳ28 National selvbestemmelsesret ʳΘʳ34 Afhængighedsfaktorer: sikkerhedspolitik og økonomi ʳΘʳ39 Afslutning ʳΘʳ51 4. Den internationale sammenhæng: afkoloniseringsprocessen i FN ʳΘʳ53 Indledning ʳΘʳ53 Normative rammer ʳΘʳ54 Organisatoriske rammer ʳΘʳ61 Afslutning ̗68 5. Folkerettens udvikling vedrørende afkolonisering og selvbestemmelse ʳΘʳ69 Generelt om folkerettens udvikling – særligt om betingelserne for sædvanedannelse ʳΘ70 Om kolonial selvbestemmelse, staters territoriale integritet og mindretalsrettigheder ʳΘ72 Etableringen af kolonial selvbestemmelse som folkeretlig norm ʳΘʳ74 Kravene til gennemførelse af kolonial selvbestemmelse (omkring 1953-54) ʳΘʳ82 Vurdering af processen omkring Grønlands integration i Danmark 1953-54 ʳΘʳ88 Sammenfatning ʳΘʳ93 Kort konklusion ʳΘʳ96 6. Ny grønlandspolitik på vej: Danske og grønlandske initiativer 1945-50 ʳΘʳ97 Indledning ʳΘʳ97 Grønlandsspørgsmålet vokser frem ʳΘʳ98 Hedtoft i offensiven ʳΘʳ107 Den nye Grønlandspolitik sættes på skinner ʳΘʳ119 Afslutning ʳΘʳ127 7. Grønlandsspørgsmålet i FN 1945-50 ʳΘʳ129 De danske myndigheder og rapporteringsforpligtelsen til FN ʳΘʳ129 FN-samlingen 1946 ʳΘʳ132 FN-samlingen 1947ʳʳΘʳ136 FN-samlingen 1948 ʳΘʳ139 Møderne i 4. -
Geological Survey of Denmark and Greenland Bulletin 14, 78
Bulletin 14: GSB191-Indhold 04/12/07 14:36 Side 1 GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 14 · 2007 Quaternary glaciation history and glaciology of Jakobshavn Isbræ and the Disko Bugt region, West Greenland: a review Anker Weidick and Ole Bennike GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Bulletin 14: GSB191-Indhold 04/12/07 14:36 Side 2 Geological Survey of Denmark and Greenland Bulletin 14 Keywords Jakobshavn Isbræ, Disko Bugt, Greenland, Quaternary, Holocene, glaciology, ice streams, H.J. Rink. Cover Mosaic of satellite images showing the Greenland ice sheet to the east (right), Jakobshavn Isbræ, the icefjord Kangia and the eastern part of Disko Bugt. The position of the Jakobshavn Isbræ ice front is from 27 June 2004; the ice front has receded dramatically since 2001 (see Figs 13, 45) although the rate of recession has decreased in the last few years. The image is based on Landsat and ASTER images. Landsat data are from the Landsat-7 satellite. The ASTER satellite data are distributed by the Land Processes Distribution Active Archive Center (LP DAAC), located at the U.S. Geological Survey Center for Earth Resources Observation and Science (http://LPDAAC.usgs.gov). Frontispiece: facing page Reproduction of part of H.J. Rink’s map of the Disko Bugt region, published in 1853. The southernmost ice stream is Jakobshavn Isbræ, which drains into the icefjord Kangia; the width of the map illustrated corresponds to c. 290 km. Chief editor of this series: Adam A. Garde Scientific editor of this volume: Jon R. Ineson Editorial secretaries: Jane Holst and Esben W. -
Review of Greenland Avtivities 2001
GEOLOGY OF GREENLAND SURVEY BULLETIN 191 • 2002 Review of Greenland activities 2001 GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF THE ENVIRONMENT GEUS GSB191-Indhold 13/12/02 11:28 Side 1 GEOLOGY OF GREENLAND SURVEY BULLETIN 191 • 2002 Review of Greenland activities 2001 Edited by A.K. Higgins, Karsten Secher and Martin Sønderholm GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF THE ENVIRONMENT GSB191-Indhold 13/12/02 11:28 Side 2 Geology of Greenland Survey Bulletin 191 Keywords Geological mapping, Greenland activities 2001, limnology, marine geophysics, mineral resources, palynology, petroleum geology, sedimentology, sequence stratigraphy, stratigraphy. Cover A major landslide was reported from the southern shore of the Nuussuaq peninsula in November 2000 (see Pedersen et al., page 73). During the follow-up field studies, periodic minor rock falls created dust clouds that prompted the local population to designate the area as the ‘smoking mountains’. Highest summits are 1900 m above the fjord. View to the east from a vantage point on the island of Disko. Photo: Stig A. Schack Pedersen. Frontispiece: facing page Outcrop of the contact zone of a 20 m wide kimberlitic dyke south-west of Kangerlussuaq airport, southern West Greenland. This dyke is one of the largest known kimberlite dykes in the world. The locality is marked J on Fig. 2 in Jensen et al. (page 58). Photo: Sven Monrad Jensen. Chief editor of this series: Peter R. Dawes Scientific editors: A.K. Higgins, Karsten Secher and Martin Sønderholm Technical editing: Esben W. Glendal Illustrations: Annabeth Andersen, Lis Duegaard, Jette Halskov and Stefan Sølberg Lay-out and graphic production: Carsten E. -
Review of Greenland Activities 1998 Li131999 183 I Ll B S D L G F L G
R i f G l d i i i 1998 GEOLOGY OF GREENLAND SURVEY BULLETIN 183 • 1999 Review of Greenland activities 1998 G l f G l d S B ll i 183 1999 GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF ENVIRONMENT AND ENERGY GEUS GEOLOGY OF GREENLAND SURVEY BULLETIN 183 • 1999 Review of Greenland activities 1998 Edited by A. K. Higgins and W.Stuart Watt GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF ENVIRONMENT AND ENERGY Geology of Greenland Survey Bulletin 183 Keywords Airborne geophysics, climatic research, geological mapping, Greenland activities 1998, limnology, resource studies, petroleum geol- ogy, publications review. Cover The area around the head of Søndre Strømfjord has been known for some time to contain saline lakes. The salinity in these closed- basin lakes has resulted from evaporation during the Holocene and as a result the sediments can be used as climate archives. The sediments in some of these lakes are laminated and it is easier to take cores when the lakes are frozen (see Anderson et al. this vol- ume). The photograph shows returning from Store Saltsø, one of the saline lakes in the area, after a day’s coring. The fossil shore- lines around the lake are highlighted by the snow in the background. Photo: N.J. Anderson. Frontispiece: facing page The Apparsuit promontory south-east of Upernavik seen from the deck of M/S Sila during the 1998 reconnaissance for mineral occur- rences in North-West Greenland (see Thomassen et al. p. 39). The promontory, 540 m high, is composed of exfoliated granite belong- ing to the 1.86 Ga Prøven igneous complex and hosts an important bird cliff, as can be seen from the coloration. -
(National Legislation) © DOALOS/OLA
Page 1 Order No. 191 of 27 May 1963 on the Delimitation of the Territorial Sea of Greenland Article 1 (1) The territorial waters of Greenland shall consist of the internal waters and the territorial sea. (2) The territorial sea shall comprise those areas of the sea which to landward are bounded by the lines specified in article 2 and to seaward by lines drawn in such a manner that the distance from every point on these lines to the nearest point on the inner boundary line is three nautical miles (5,556 metres). (3) The internal waters shall comprise those water areas, such as harbours, harbour entrances, roadsteads, bays, fiords, sounds, belts and other waters, which are situated inside the lines specified in article 2. Article 2 The lines which, in accordance with article 1, are taken as a basis for the delimitation of the territorial sea and the inland waters shall consist of the coastline (low-water mark at mean spring-tide) or of straight lines between the following points: No. 1 - Sea Chart No. 1100 Position Designation 1 59° 44.7' N 43° 53.6' W Southernmost island south of Cape Farvel (Umánarssuaq) thence a straight line to 2 59° 44.8' N 44° 10.9' W Nunat thence a straight line to 3 59° 50.8'N 44° 59.3' W Small island directly south of Kulusuk thence a straight line to 4 59° 58.6' N 45° 21.9' W Naujat thence a straight line to 5 60° 16.0' N 45° 38.0' W Ikardluk thence a straight line to 6 60° 26.1' N 45° 58.0' W Tukingasek (Tukingassoq) thence a straight line to 7 60° 37.3' N 46° 43.4' W Island SSW of Angissit thence a straight line -
Greenland, Kingdom of Denmark
Journal of Global Change Data & Discovery. 2019, 3(1): 83-88 ©2019 GCdataPR DOI:10.3974/geodp.2019.01.12 Global Change Research Data Publishing & Repository www.geodoi.ac.cn Global Change Data Encyclopedia Greenland, Kingdom of Denmark Liu, C.1* Zhang, Y. H.1 Shen, Y.1 Chen, L. J.2 1. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2. National Geomatics Center of China, Beijing 100830, China Keywords: Greenland; Kingdom of Denmark; islands; Nansen; data encyclopedia The Greenland of Kingdom of Denmark[1] is geo-located at 594442N–833946N, 731513W–112011W. It is in the northeast of North America, between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. The Greenland is the world’s larg- est island, and three-quarters of Greenland is covered by the ice-snow (Figure 1). The main island is the Greenland, its area is 2,112,448.97 km2 and its coastline is 49,200.82 km[2]. Besides the mainland of Greeland, there are 27,388 small islands, isles and independent rocks of Greeland with area bigger than 24 m2. The main islands include the following islands (Table 1): DiskoIsland, Arve-prinsensEjland, UbekendtEjland, Itilleq, IleDeFrance, Nunarssit, Tingmiarmit, Ikeq, Agpat, Qutdlikorssuit/Qu llikorsuit Island, Kekertarmiut, Karasuk, Ikamiuk, Sermitsiak, Iluiteq, Maniitsoq, Kangeq, Uvtorsiutit, Simiutak, Kulusuk, Aluk-tunordleq, SanerataTime, Kitak, Kigataq, Savissivik, DiskofjordQeqertaq, Milait, Sujunikajik, Figure 1 Map of Greenland in .kmz data Aumat, Nanortalik, Kullorsuaq, Tukingassoq, format (Google Earth image) Aasiaat, Uummannaq, Agto, Maligissat, Timerdlit, Angissorssuaq, Kitsigsut, Received: 26-02-2019; Accepted: 15-03-2019; Published: 25-03-2019 Foundation: Ministry of Science and Technology of the P. -
Sustainable Regions - Sustainable Local Communities NORDREGIO Contributions to ICASS VIII: Northern Sustainabilities Congress
Sustainable Regions - Sustainable Local Communities NORDREGIO Contributions to ICASS VIII: Northern Sustainabilities Congress Ryan Weber & Rasmus Ole Rasmussen (Eds) NORDREGIO WORKING PAPER 2014:2 Contents Foreword ..................................................................................... 3 1 Introduction to the Arctic Co-operation Project Sustainable Regions - Sustainable Local communities .................................................... 6 2 Arctic Local Communities and the Competence Building in Relation to Large Mining Projects - Case Sodankylä, Finland ........................ 11 3 Connections between global production networks and local production systems in the High North ........................................... 14 4 Impacts of cross-border cooperation on the socio-economic development of Kiruna and Narvik ................................................ 14 5 Inclusion of Sami tourism in destination development ............... 18 6 Narsaq: A Community Challenged by Municipal Restructuring and Uranium Mining in South Greenland .............................................. 22 7 Mapping virtual mobilities in the Arctic - Examples from North America and Northern Sweden ..................................................... 31 8 Multi-Functionality as Scenarios for Land Use Development in the Arctic ........................................................................................ 36 9 Monitoring demographic changes in light of administrative restructuring – the case of Kujalleq Municipality in Greenland ......... -
De Økonomiske Forhold I De Grønlandske Kommuner
ARBEJDSNOTAT NR. 16 DE OKONOMISKE FORHOLD I DE GRONLANDSKE KOM- MUNER VED HJEMMESTYRETS INDFORELSE D:!, DANMARKS STATISTIK . Kobenhavn 1985 7 JUNI 1985 DAN' 'TATISTIK buv ¡ KET F O R O R D Publikationen beskriver ferst forholdene i de gran- landske kommuner generelt pá baggrund af en rmkke vigtige indikatorer for den befolkningsmmssige og okonomiske ud- vikling, og derefter folger en beskrivelse af forholdene i de enkelte kommuner. Publikationen supplerer Statistiske Undersogelser nr. 40 1984 "Indkomst- og erhvervsforholdene i Granland ved Hjemmestyrets indforelse" med regionale oplysninger. Publikationen er udarbejdet af fuldmmgtig, cand. polit. Lise Lyck. Danmarks Statistik, januar 1985 5 I N D H O L D Side KAPITEL I KOMMUNEINDDELINGEN 7 KAPITEL II FORHOLDENE I DE GRONLANDSKE KOMMUNER BELYST UD FRA FORSKELLIGE BEFOLKNINGS- MÆSSIGE OG OKONOMISKE INDIKATORER .... 11 KAPITEL III TABELMATERIALE TIL BELYSNING AF DE BE- FOLKNINGSMÆSSIGE OG OKONOMISKE FORHOLD I DE ENKELTE KOMMUNER 19 KAPITEL IV DE BEFOLKNINGSMÆSSIGE OG OKONOMISKE FORHOLD I DE ENKELTE KOMMUNER 25 IV.01 Nanortalik/Nanortalik 25 IV.02 Julianeháb/Qagortoq 30 IV.03 Narssaq/Narsaq 34 IV.04 Ivigtut/Ivittuut 38 IV.05 Frederiksháb/Paamiut 42 IV.06 Godtháb/Nuuk 46 IV.07 Sukkertoppen/Maniitsoq 50 IV.08 Holsteinsborg/Sisimiut 54 IV.09 Kangatsiaq/Kangaatsiaq 58 IV.10 Egedesminde/Aasiaat 62 IV.11 Christiansháb/Qasigiannguit 66 IV.12 Jakobshavn/Ilulissat 70 IV.14 Godhavn/Qeqertarsuaq 74 IV.15 Umanak/Uummannaq 78 IV.16 Upernavik/Upernavik 82 IV.17 Thule/Qaanaaq 86 IV.18 Angmagssalik/Tasiilaq 90 IV.19 Scoresbysund/Ittoggortoormiit 94 IV.20 Hele Grenland 99 LITTERATURFORTEGNELSE 105 7 KAPITEL I KOMMUNEINDDELINGEN Grenland er opdelt i 18 kommuner samt nogle omráder uden for den kommunale inddeling, som omfatter baserne i Sdr. -
The Ministry of Immigration and Integration's Overview of Travel Docu-Ments, Visa Conditions and Border Crossing Points
The Ministry of Immigration and Integration's overview of travel docu- ments, visa conditions and border crossing points The Ministry of Immigration and Integration hereby provides an overview of foreign nationals who are exempt from passport requirements under section 1(5) of Executive Order No. 330 of 24 April 2018 on Aliens’ Access to Denmark (Aliens Order), an overview of foreign nationals who are ex- empt from the visa requirement under section 2 of Executive Order No. 376 of 20 March 2015 on Aliens' Access to Denmark on the basis of a Visa (Visa Order), as well as an overview of approved border crossing points under section 11(16) of the Aliens Order.1 I. Exempt from any form of travel identity document 1. Finnish, Icelandic, Norwegian and Swedish nationals who enter Denmark directly from and exit directly to Finland, Iceland, Norway or Sweden. 2. Young persons of less than 18 years who are not nationals of Finland, Iceland, Norway or Sweden but have their permanent residence in one of the mentioned countries when travelling in a group with Nordic young per- sons in connection with school excursions, sports events and similar cir- cumstances of no more than one month's duration, and when the entry with the group and the exit with the group takes place directly from and to Finland, Iceland, Norway or Sweden, respectively. 1 The overview of approved border crossing points in the Faroe Islands and Greenland, see para. VII, 3-6, of the overview, is published according to section 38(3) of Decree No. 182 of 22 March 2001 on the entry into force for the Faroe Islands of the Aliens Act and accord- ing to section 38(3) of Decree No.