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Baffin Bay Sea Ice Extent and Synoptic Moisture Transport Drive Water Vapor
Atmos. Chem. Phys., 20, 13929–13955, 2020 https://doi.org/10.5194/acp-20-13929-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Baffin Bay sea ice extent and synoptic moisture transport drive water vapor isotope (δ18O, δ2H, and deuterium excess) variability in coastal northwest Greenland Pete D. Akers1, Ben G. Kopec2, Kyle S. Mattingly3, Eric S. Klein4, Douglas Causey2, and Jeffrey M. Welker2,5,6 1Institut des Géosciences et l’Environnement, CNRS, 38400 Saint Martin d’Hères, France 2Department of Biological Sciences, University of Alaska Anchorage, 99508 Anchorage, AK, USA 3Institute of Earth, Ocean, and Atmospheric Sciences, Rutgers University, 08854 Piscataway, NJ, USA 4Department of Geological Sciences, University of Alaska Anchorage, 99508 Anchorage, AK, USA 5Ecology and Genetics Research Unit, University of Oulu, 90014 Oulu, Finland 6University of the Arctic (UArctic), c/o University of Lapland, 96101 Rovaniemi, Finland Correspondence: Pete D. Akers ([email protected]) Received: 9 April 2020 – Discussion started: 18 May 2020 Revised: 23 August 2020 – Accepted: 11 September 2020 – Published: 19 November 2020 Abstract. At Thule Air Base on the coast of Baffin Bay breeze development, that radically alter the nature of rela- (76.51◦ N, 68.74◦ W), we continuously measured water va- tionships between isotopes and many meteorological vari- por isotopes (δ18O, δ2H) at a high frequency (1 s−1) from ables in summer. On synoptic timescales, enhanced southerly August 2017 through August 2019. Our resulting record, flow promoted by negative NAO conditions produces higher including derived deuterium excess (dxs) values, allows an δ18O and δ2H values and lower dxs values. -
Geology of Greenland Bulletin 185, 67-93
Sedimentary basins concealed by Acknowledgements volcanic rocks The map sheet was compiled by J.C. Escher (onshore) In two areas, one off East Greenland between latitudes and T.C.R. Pulvertaft (offshore), with final compilation 72° and 75°N and the other between 68° and 73°N off and legend design by J.C. Escher (see also map sheet West Greenland, there are extensive Tertiary volcanic legend). In addition to the authors’ contributions to the rocks which are known in places to overlie thick sedi- text (see Preface), drafts for parts of various sections mentary successions. It is difficult on the basis of exist- were provided by: L. Melchior Larsen (Gardar in South ing seismic data to learn much about these underlying Greenland, Tertiary volcanism of East and West Green- sediments, but extrapolation from neighbouring onshore land); G. Dam (Cretaceous–Tertiary sediments of cen- areas suggests that oil source rocks are present. tral West Greenland); M. Larsen (Cretaceous–Tertiary Seismic data acquired west of Disko in 1995 have sediments in southern East Greenland); J.C. Escher (map revealed an extensive direct hydrocarbon indicator in of dykes); S. Funder (Quaternary geology); N. Reeh the form of a ‘bright spot’ with a strong AVO (Amplitute (glaciology); B. Thomassen (mineral deposits); F.G. Versus Offset) anomaly, which occurs in the sediments Christiansen (petroleum potential). Valuable comments above the basalts in this area. If hydrocarbons are indeed and suggestions from other colleagues at the Survey are present here, they could either have been generated gratefully acknowledged. below the basalts and have migrated through the frac- Finally, the bulletin benefitted from thorough reviews tured lavas into their present position (Skaarup & by John Korstgård and Hans P. -
Sir John Franklin and the Arctic
SIR JOHN FRANKLIN AND THE ARCTIC REGIONS: SHOWING THE PROGRESS OF BRITISH ENTERPRISE FOR THE DISCOVERY OF THE NORTH WEST PASSAGE DURING THE NINE~EENTH CENTURY: WITH MORE DETAILED NOTICES OF THE RECENT EXPEDITIONS IN SEARCH OF THE MISSING VESSELS UNDER CAPT. SIR JOHN FRANKLIN WINTER QUARTERS IN THE A.ROTIO REGIONS. SIR JOHN FRANKLIN AND THE ARCTIC REGIONS: SHOWING FOR THE DISCOVERY OF THE NORTH-WEST PASSAGE DURING THE NINETEENTH CENTURY: WITH MORE DETAILED NOTICES OF THE RECENT EXPEDITIONS IN SEARCH OF THE MISSING VESSELS UNDER CAPT. SIR JOHN FRANKLIN. BY P. L. SIMMONDS, HONORARY AND CORRESPONDING JIIEl\lBER OF THE LITERARY AND HISTORICAL SOCIETIES OF QUEBEC, NEW YORK, LOUISIANA, ETC, AND MANY YEARS EDITOR OF THE COLONIAL MAGAZINE, ETC, ETC, " :Miserable they Who here entangled in the gathering ice, Take their last look of the descending sun While full of death and fierce with tenfold frost, The long long night, incumbent o•er their heads, Falls horrible." Cowl'ER, LONDON: GEORGE ROUTLEDGE & CO., SOHO SQUARE. MDCCCLI. TO CAPT. SIR W. E. PARRY, R.N., LL.D., F.R.S., &c. CAPT. SIR JAMES C. ROSS, R.N., D.C.L., F.R.S. CAPT. SIR GEORGE BACK, R.N., F.R.S. DR. SIR J. RICHARDSON, R.N., C.B., F.R.S. AND THE OTHER BRAVE ARCTIC NAVIGATORS AND TRAVELLERS WHOSE ARDUOUS EXPLORING SERVICES ARE HEREIN RECORDED, T H I S V O L U M E I S, IN ADMIRATION OF THEIR GALLANTRY, HF.ROIC ENDURANCE, A.ND PERSEVERANCE OVER OBSTACLES OF NO ORDINARY CHARACTER, RESPECTFULLY DEDICATED, BY THEIR VERY OBEDIENT HUMBLE SERVANT, THE AUTHOR. -
Place Names Working in Greenland
Methodology in collecting geographical names in Greenland Lisathe Møller • Specialized consultant at Oqaasileriffik, the Greenland Language Secretariat. • Secretary for the Geographical Names Authority, and Project Manager for collecting information about existing names and reporting to the Place Names Authority. Overview of my presentation/ Saqqummiussassama tulleriinneri • Place Names Authority Act in Greenland • Geographical naming methods in Greenland • Geographical names collection in Greenland Law on Greenland Geographical Names Authority • The Goverment set up the Greenland Geographical Names Authority in order to ensure the registration of, and authoritative advice and information on the naming of the geographical names. • The Greenland Geographical Names Authority’s objectives are: • to collect, register and authorize geographical names in Greenland, excluding local road and places inside municipal borders. • The Greenland Geographical Names Authority consists of 5 members, appointed by the Minister. • The Greenland Geographical Names Authority's competence cannot be wholly or partly transferred to the other. Geographical naming methods in Greenland • There are two main different methods of naming places in Greenland – Greenlanders naming of places and foreigners naming of places are different. Geographical naming methods in Greenland Greenlanders often named places according to their characteristics which resembles something. For example The island name is Uummannaq which means resemble a heart. Geographical naming methods in Greenland Greenlanders often named places according to its function • Nasittarfik is called that because sealers used to use the site as a lookout place. Nasittarfik means a lookout point. • The headland is called Pituffik. Because hunters used to catch a whale from a beach on site, and tethered the whale on a stone. -
Greenland Last Ice Area
kn Greenland Last Ice Area Potentials for hydrocarbon and mineral resources activities Mette Frost, WWF-DK Copenhagen, September 2014 Report Greenland Last Ice Area. Potentials for hydrocarbon and mineral resources activities. The report is written by Mette Frost, WWF Verdensnaturfonden. Published by WWF Verdensnaturfonden, Svanevej 12, 2400 København NV. Denmark. Phone +45 3536 3635 – E-mail: [email protected] WWF Global Arctic Programme, 275 Slater Street, Ottawa, Ontario, K1P 5L4. Canada. Phone: +1 613 232 2535 Project The report has been developed under the Last Ice Area project, a joint project between WWF Canada, WWF Denmark and WWF Global Arctic Programme. Other WWF reports on Greenland – Last Ice Area Greenland Last Ice Area. Scoping study: socioeconomic and socio-cultural use of the Greenland LIA. By Pelle Tejsner, consultant and PhD. and Mette Frost, WWF-DK. November 2012. Seals in Greenland – an important component of culture and economy. By Eva Garde, WWF-DK. November 2013. Front page photo: Yellow house in Kullorsuaq, Qaasuitsup Kommunia, Greenland. July 2012. Mette Frost, WWF Verdensnaturfonden. The report can be downloaded from www.wwf.dk [1] CONTENTS Last Ice Area Introduction 4 Last Ice Area / Sikuusarfiit Nunngutaat 5 Last Ice Area/ Den Sidste Is 6 Summary 7 Eqikkaaneq 12 Sammenfatning 18 1. Introduction – scenarios for resources development within the Greenland LIA 23 1.1 Last Ice Area 23 1.2 Geology of the Greenland LIA 25 1.3 Climate change 30 2. Mining in a historical setting 32 2.1 Experiences with mining in Greenland 32 2.2 Resources development to the benefit of society 48 3. -
Upper-Air Temperatures Around Greenland: 1964–2005 Jason E
GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L12706, doi:10.1029/2006GL025723, 2006 Click Here for Full Article Upper-air temperatures around Greenland: 1964–2005 Jason E. Box1,2 and Ariel E. Cohen2 Received 15 January 2006; revised 2 March 2006; accepted 4 May 2006; published 28 June 2006. [1] A 42-year collection of 12h balloon soundings from recent decade, which spans a time of record-setting six sites surrounding Greenland reveal distinct patterns of global and regional temperatures [World Meteorological tropospheric and stratospheric temperature variability. Organization, 2005]. Seasonal mean upper-air temperatures exhibit statistically [4] In this study, we check data temporal homogeneity, significant correlations with surface air temperature records. and then determine the extent that surface air temperature Over the full 1964–2005 record, patterns of statistically variability is linked with upper air temperature variability. significant tropospheric warming and stratospheric cooling Using statistical regression, we measure temporal tempera- are evident. Overall, the magnitude of warming decreases ture trends and statistical significance around Greenland at with height, becoming cooling in the mid-stratosphere. fixed levels throughout the troposphere and stratosphere. During the recent 12-year period (1994–2005) lacking We discuss potential causes of the observed variability. major volcanic forcing, statistically significant warming (+2.5 K to +5 K) is evident throughout the troposphere at all 2. Data and Methods sites, with seasonal changes in the +3 K to +9 K range near the surface at 1000 hPa. The recent (1994–2005) [5] The primary data set used in this study comes from tropospheric warming has dominated the 1964–2005 operational weather balloon soundings, that is, radiosondes, lower troposphere temperature change, despite 1964–1982 made 12-hourly since at least 1964. -
Arctic Report Card 2017
Arctic Report Card 2017 Arctic Report Card 2017 Arctic shows no sign of returning to reliably frozen region of recent past decades 2017 Headlines 2017 Headlines Video Executive Summary Contacts Arctic shows no sign of returning to reliably frozen Vital Signs region of recent past decades Surface Air Temperature Despite relatively cool summer temperatures, Terrestrial Snow Cover observations in 2017 continue to indicate that the Greenland Ice Sheet Arctic environmental system has reached a 'new Sea Ice normal', characterized by long-term losses in the Sea Surface Temperature extent and thickness of the sea ice cover, the extent Arctic Ocean Primary Productivity and duration of the winter snow cover and the mass of ice in the Greenland Ice Sheet and Arctic glaciers, Tundra Greenness and warming sea surface and permafrost Other Indicators temperatures. Terrestrial Permafrost Groundfish Fisheries in the Highlights Eastern Bering Sea Wildland Fire in High Latitudes • The average surface air temperature for the year ending September 2017 is the 2nd warmest since 1900; however, cooler spring and summer temperatures contributed to a rebound in snow cover in the Eurasian Arctic, slower summer sea ice loss, Frostbites and below-average melt extent for the Greenland ice sheet. Paleoceanographic Perspectives • The sea ice cover continues to be relatively young and thin with older, thicker ice comprising only 21% of the ice cover in on Arctic Ocean Change 2017 compared to 45% in 1985. Collecting Environmental • In August 2017, sea surface temperatures in the Barents and Chukchi seas were up to 4° C warmer than average, Intelligence in the New Arctic contributing to a delay in the autumn freeze-up in these regions. -
State of the Climate in 2009
STATE OF THE CLIMATE IN 2009 D.S. Arndt, M.O. Baringer and M.R. Johnson, Eds. Associate Eds. L.V. Alexander, H.J. Diamond, R.L. Fogt, J.M. Levy, J. Richter-Menge, P.W. Thorne, L.A. Vincent, A.B. Watkins and K.M. Willett (a) Yearly mean sea surface temperature anomalies (SSTA) in 2009 and (b) SSTA differences between 2009 and 2008. Anomalies are defi ned as departures from the 1971-2000 climatology. Refer to Chapter 3, Figure 3.1 for a more detailed description. Special Supplement to the Bulletin of the American Meteorological Society Vol. 91, No. 7, July 2010 Unauthenticated | Downloaded 10/10/21 06:29 AM UTC STATE OF THE CLIMATE IN 2009 Unauthenticated | Downloaded 10/10/21 06:29 AM UTC HOW TO CITE THIS DOCUMENT Citing the complete report: Arndt, D. S., M. O. Baringer, and M. R. Johnson, Eds., 2010: State of the Climate in 2009. Bull. Amer. Meteor. Soc., 91 (7), S1–S224. Citing a chapter (example): Diamond, H. J., Ed., 2010: The tropics [in “State of the Climate in 2009”]. Bull. Amer. Meteor. Soc., 91 (7), S79–S106. Citing a section (example): Halpert, M., G. D. Bell, and M. L’Heureux, 2010: ENSO and the Tropical Pacific [in “State of the Climate in 2009”]. Bull. Amer. Meteor. Soc., 91 (7), S79–S82. Unauthenticated | Downloaded 10/10/21 06:29 AM UTC E DITOR & AUTHOR AffILIATIONS (alphabetical by name) EDITORS Attaher, Samar M., Agricultural Research Center, MALR, Alexander, Lisa V., Climate Change Research Centre, Universi- Cairo, Egypt ty of New South Wales, Sydney, New South Wales, Australia Baez, Julian, DMH-DINAC / CTA-UCA, Asunción, -
Issn 1198-6727
ISSN 1198-6727 FISHERIES CATCH RECONSTRUCTIONS: ISLANDS, PART IV Fisheries Centre Research Reports 2014 Volume 22 Number 2 ISSN 1198-6727 Fisheries Centre Research Reports 2014 VOLUME 22 NUMBER 2 FISHERIES CATCH RECONSTRUCTIONS: ISLANDS, PART IV Fisheries Centre, University of British Columbia, Canada Edited by Kyrstn Zylich, Dirk Zeller, Melanie Ang and Daniel Pauly Fisheries Centre Research Reports 22(2) 157 pages © published 2014 by The Fisheries Centre, University of British Columbia 2202 Main Mall Vancouver, B.C., Canada, V6T 1Z4 ISSN 1198-6727 Fisheries Centre Research Reports 22(2) 2014 Edited by Kyrstn Zylich, Dirk Zeller, Melanie Ang and Daniel Pauly CONTENT Preface i Reconstruction of total marine fisheries catches for Anguilla (1950 - 2010) 1 Robin Ramdeen, Kyrstn Zylich, and Dirk Zeller Reconstruction of total marine fisheries catches for the British Virgin Islands (1950 - 2010) 9 Robin Ramdeen, Sarah Harper, Kyrstn Zylich, and Dirk Zeller Reconstruction of domestic fisheries catches in the Chagos Archipelago: 1950 - 2010 17 Dirk Zeller and Daniel Pauly Reconstruction of total marine fisheries catches for Cuba (1950 - 2010) 25 Andrea Au, Kyrstn Zylich, and Dirk Zeller Reconstruction of total marine fisheries catches for Dominica (1950 - 2010) 33 Robin Ramdeen, Sarah Harper, and Dirk Zeller Reconstruction of total marine fisheries catches for the Dominican Republic (1950 - 2010) 43 Liesbeth van der Meer, Robin Ramdeen, Kyrstn Zylich, and Dirk Zeller The catch of living marine resources around Greenland from 1950 t0 2010 55 -
Kitaa Kujataa Avanersuaq Tunu Kitaa
Oodaap Qeqertaa (Oodaaq(Oodaaq Island) Ø) KapCape Morris Morris Jesup Jesup D AN L Nansen Land N IAD ATN rd LS Fjio I Freuchen PEARY LAND ce NR den IAH Land pen Ukioq kaajallallugu / Year-round nde TC Ukioq kaajallallugu / Hele året I IES STATION NORD RC UkiupUkiup ilaannaa ilaannaa / Kun / Seasonal visse perioder Tartupaluk HN (Hans Ø)Island) I RC SP N Wa Mylius-Erichsen IN UkioqUkioq kaajallallugu kaajallallugu / Hele / Year-round året shington Land WR Land OP UkiupUkiup ilaannaa ilaannaa / Kun / Seasonal visse perioder Da RN ugaard -Jense ND CO n Land LA R NS K E n Sermersuaq S rde UllersuaqUllersuaq (Humbolt(Humbolt Gletscher) Glacier) S fjo U rds (Cape(Kap Alexander) Alexander) M lvfje S gha Ingleeld Land RA Nio D Siorapaluk U KN Kitsissut (Carey Islands)Øer) QAANAAQ Moriusaq AVANERSUAQ Ille de France Pitufk Thule (Thule Air Base) LL AAU U G Germania LandDANMARKSHAVN CapeKap York York G E E K Savissivik K O O C C H B Q H i C A ( m Dronning M K O u F Y Margrethe II e s A F l s S Land Shannon v S e I i T N l T l r e i a B B r ZACKENBERG AU s Kullorsuaq a YG u DANEBORG y a ) Clavering Ø T q Nuussuaq Clavering Island Innarsuit Tasiusaq Ymer ØIsland UPERNAVIK Aappilattoq TraillTraill Island Ø Kangersuatsiaq Upernavik Kujalleq Summit MESTERSVIG (3.238 m) Sigguup Nunaa Stauning (Svartenhuk) AlperAlps Nuugaatsiaq Illorsuit Jameson Land Ukkusissat Niaqornat Nerlerit Inaat Qaarsut Saatut (Constable Pynt)Point) Kangertittivaq UUMMANNAQNuussuaq Ikerasak TUNU ITTOQQORTOORMIIT QEQERTARSUAQQEQERTARSUAQ (Disko (Disko Island) Ø) AVANNAA EastØstgrønland -
Hjemmestyrets Bekendtgørelse Nr. 4 Af 22. Januar 2009 Om Valg Til Fælles Bygdebestyrelser I April 2009
Hjemmestyrets bekendtgørelse nr. 4 af 22. januar 2009 om valg til fælles bygdebestyrelser i april 2009. Historisk § 1. I medfør af § 8 i Landstingslov nr. 14 af 19. november 2007 om strukturreformen af den kommunale sektor og efter høring af kommunernevælges det anførte antal bygdebestyrelsesmedlemmer til fælles bygdebestyrelser i følgende valgkredse: Kommune Kujalleq Valgkreds Antal Valgkredsen omfatter Aappilattoq, Narsaq 3 Aappilattoq Kujalleq, Tasiusaq Ikerasassuaq (vejrstation) Narsaq Kujalleq (Narsarmijit) Tasiusaq Nuugaarsuk Saputit Saputit Tasia Alluitsup Paa, 3 Alluitsup Paa Ammassivik Akuliaruseq Alluitsoq Ammassivik Qorlortorsuaq Qallimiut Eqalugaarsuit, Saarloq, 3 Eqalugaarsuit Qassimiut Saarloq Qassimiut Isortoq Narsarsuaq, 3 Narsarsuaq Qassiarsuk, Igaliku, Upernaviarsuk Vatnaverfi Eqaluit Eqaluit Akia Illorsuit Kangerluarsorujuk Kangerluarsorujuup Qinngua Qanisartuut Qaqortukulooq Saqqaa Tasilikulooq Qassiarsuk Arnannguit Inneruulalik Issormiut Kangerlua Kiattuut Nunataaq Qinngua Qinngua Kangilleq Qorlortoq Qorlortup Itinnera Sillisit Tasiusaq Igaliku Atarnaatsoq Igaliku Kujalleq Iterlak Timerliit Uummannartuuaraq Kommuneqarfik Sermersooq Valgkreds Antal Valgkredsen omfatter Kulusuk, Tiniteqilaaq, 5 Kulusuk Isortoq Tiniteqilaaq Isortoq Kuummiut, Sermiligaaq 5 Kuummiut Sermiligaaq Kapisillit, 3 Kapisillit Qeqertarsuatsiaat Qeqertarsuatsiaat Arsuk 3 Arsuk Qeqqata Kommunia Valgkreds Antal Valgkredsen omfatter Itilleq, Sarfannguit 5 Itilleq Sarfannguit Atammik, Napasoq 5 Atammik Napasoq Kangaamiut 3 Kangaamiut Kangerlussuaq 3 -
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.