Report from the Field Workshop on Studies of Tidewater Glaciers
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Canadian Arctic 1987
Canadian Arctic 1987 TED WHALLEY Ellesmere Island has, at Cape Columbia, the northern-most land in the world, at latitude about 83.1°. It is a very mountainous island, particularly on the north west and the east sides, and its mountains almost reach the north coast - the northern-most mountains in the world. It was from here that most of the attempts to reach the North Pole have started, including that of Peary - reputedly, but perhaps not actually, the first man to reach the Pole. Nowadays, tourist flights to the Pole by Twin Otter from Resolute Bay are common, but are somewhat expensive. The topography of Ellesmere is dominated by several large and small ice-caps which almost bury the mountains, and only the Agassiz Ice-Cap, which is immediately west of Kane Basin, has a name. On the north-west side there are two large and unnamed ice-caps, the larger of which straddles 82°N and the smaller straddles 8I.5°N. There is also a large unnamed ice-cap immediately west of Smith Sound, a smaller one on the south-east tip of Ellesmere Island, and another north of the settlement of Grise Fiord on the south coast. The north coast of Ellesmere was the home of great ice shelves, but, at about the turn of the century, the ice shelves started to break off and float away as so-called 'ice islands' that circulated for many decades around the arctic ocean, and still do. They have often been used as natural platforms for scientific expeditions. Perhaps nine-tenths of the original ice shelves have floated away. -
Short Title Changes in Surface Height, 1957-1967, Of
SHORT TITLE CHANGES IN SURFACE HEIGHT, 1957-1967, OF THE GILMAN GLACIER Keith Charles Arnold, Facu1ty of Graduate Studies, Interdiscip1inary G1acio1ogy, for degree of Master of Science ABSTRACT Keith Charles Arnold Determination of Changes of Surface Height, 1957 to 1967, of the Gi1man Glacier, Northern Ellesmere Island, Canada. Facu1ty of Graduate Studies Interdiscip1inary G1acio10gy Master of Science SUMMARY In 1967, 29 points on the Gi1man Glacier origina11y 10cated in 1957 were repositioned with a mean error of 0.36 m. Their height were redetermined with a mean error of 0.25 m. Refraction coefficients ranged from 0.047 to 0.558, with a mean of 0.162. A profile in the accumulation area showed 1itt1e change. Down glacier from a seismic profile near the average position of the equi1ibrium 1ine, 1957 to 1967, the average height 10ss was 2.4 m. From May 1958 to May 1967 the glacier advanced 25.4 m. A volume 10ss ca1cu1ated from height 10ss and glacier advance was 165 x 106 m3 , compared with 140 x 106 m3 ca1cu1ated from mass balance data, part1y estimated for missing years, and glacier f10w through the seismic profile. This area had a negative mass balance of 91 cm ice/yr; 69 cm ice/yr wou1d balance the vertical component of f10w, keeping the surface unchanged. DETERMINATION OF CHANGES OF SURFACE HEIGHT, 1957-1967, OF THE GILMAN GLACIER, NORTHERN ELLESMERE ISLAND, CANADA K. C. Arnold A thesis submitted in accordance with the regu1ations for the degree of Master of Science at McGi11 University. 1968 1 ® K.C. Arnold 1969 TABLE OF CONTENTS -
The Distant Early Warning (DEW) Line: a Bibliography and Documentary Resource List
The Distant Early Warning (DEW) Line: A Bibliography and Documentary Resource List Prepared for the Arctic Institute of North America By: P. Whitney Lackenbauer, Ph.D. Matthew J. Farish, Ph.D. Jennifer Arthur-Lackenbauer, M.Sc. October 2005 © 2005 The Arctic Institute of North America ISBN 1-894788-01-X The DEW Line: Bibliography and Documentary Resource List 1 TABLE OF CONTENTS 1.0 PREFACE 2 2.0 BACKGROUND DOCUMENTS 3 2.1 Exchange of Notes (May 5, 1955) Between Canada and the United States Of America Governing the Establishment of a Distant Early Warning System in Canadian Territory.......................................................................................................... 3 2.2 The DEW Line Story in Brief (Western Electric Corporation, c.1960) ……………… 9 2.3 List of DEW Line Sites ……………………………………….…………………….... 16 3.0 ARCHIVAL COLLECTIONS 23 3.1 Rt. Hon. John George Diefenbaker Centre ……………………………………….…... 23 3.2 Library and Archives Canada …………………………………….…………………... 26 3.3 Department of National Defence, Directorate of History and Heritage ………………. 46 3.4 NWT Archives Council, Prince of Wales Northern Heritage Centre ……………….... 63 3.5 Yukon Territorial Archives, Whitehorse, YT ………………………………………… 79 3.6 Hudson Bay Company Archives ……………………………………………………... 88 3.7 Archives in the United States ……………………………………………………….… 89 4.0 PUBLISHED SOURCES 90 4.1 The Globe and Mail …………………………………………………………………………… 90 4.2 The Financial Post ………………………………………………………………………….…. 99 4.3 Other Print Media …………………………………………………………………..… 99 4.4 Contemporary Journal Articles ……………………………………………………..… 100 4.5 Government Publications …………………………………………………………….. 101 4.6 Corporate Histories ………………………………………………………………...... 103 4.7 Professional Journal Articles ………………………………………………………..… 104 4.8 Books ………………………………………………………………………………..… 106 4.9 Scholarly and Popular Articles ………………………………………………….……. 113 4.10 Environmental Issues and Cleanup: Technical Reports and Articles …………….…. 117 5.0 OTHER SOURCES 120 5.1 Theses and Dissertations ……………………………………………………………... -
Fluctuations of Tidewater Glaciers in Hornsund Fjord (Southern Svalbard) Since the Beginning of the 20Th Century
Title: Fluctuations of tidewater glaciers in Hornsund Fjord (Southern Svalbard) since the beginning of the 20th century Author: Małgorzata Błaszczyk, Jacek A. Jania, Leszek Kolondra Citation style: Błaszczyk Małgorzata, Jania Jacek A., Kolondra Leszek. (2013). Fluctuations of tidewater glaciers in Hornsund Fjord (Southern Svalbard) since the beginning of the 20th century. “Polish Polar Research” (vol. 34, no. 4 (2013), s. 327-352), doi 10.2478/popore-2013-0024 vol. 34, no. 4, pp. 327–352, 2013 doi: 10.2478/popore−2013−0024 Fluctuations of tidewater glaciers in Hornsund Fjord (Southern Svalbard) since the beginning of the 20th century Małgorzata BŁASZCZYK, Jacek A. JANIA and Leszek KOLONDRA Wydział Nauk o Ziemi, Uniwersytet Śląski, ul. Będzińska 60, 41−200 Sosnowiec, Poland <[email protected]> <[email protected]> <[email protected]> Abstract: Significant retreat of glaciers terminating in Hornsund Fjord (Southern Spits− bergen, Svalbard) has been observed during the 20th century and in the first decade of the 21st century. The objective of this paper is to present, as complete as possible, a record of front positions changes of 14 tidewater glaciers during this period and to distinguish the main factors influencing their fluctuations. Results are based on a GIS analysis of archival maps, field measurements, and aerial and satellite images. Accuracy was based on an as− sessment of seasonal fluctuations of a glacier’s ice cliff position with respect to its mini− mum length in winter (November–December) and its maximum advance position in June or July. Morphometric features and the environmental setting of each glacier are also pre− sented. -
Nunavut, a Creation Story. the Inuit Movement in Canada's Newest Territory
Syracuse University SURFACE Dissertations - ALL SURFACE August 2019 Nunavut, A Creation Story. The Inuit Movement in Canada's Newest Territory Holly Ann Dobbins Syracuse University Follow this and additional works at: https://surface.syr.edu/etd Part of the Social and Behavioral Sciences Commons Recommended Citation Dobbins, Holly Ann, "Nunavut, A Creation Story. The Inuit Movement in Canada's Newest Territory" (2019). Dissertations - ALL. 1097. https://surface.syr.edu/etd/1097 This Dissertation is brought to you for free and open access by the SURFACE at SURFACE. It has been accepted for inclusion in Dissertations - ALL by an authorized administrator of SURFACE. For more information, please contact [email protected]. Abstract This is a qualitative study of the 30-year land claim negotiation process (1963-1993) through which the Inuit of Nunavut transformed themselves from being a marginalized population with few recognized rights in Canada to becoming the overwhelmingly dominant voice in a territorial government, with strong rights over their own lands and waters. In this study I view this negotiation process and all of the activities that supported it as part of a larger Inuit Movement and argue that it meets the criteria for a social movement. This study bridges several social sciences disciplines, including newly emerging areas of study in social movements, conflict resolution, and Indigenous studies, and offers important lessons about the conditions for a successful mobilization for Indigenous rights in other states. In this research I examine the extent to which Inuit values and worldviews directly informed movement emergence and continuity, leadership development and, to some extent, negotiation strategies. -
The Dynamics and Mass Budget of Arctic Glaciers Extended Abstracts
The Dynamics and Mass Budget of Arctic Glaciers Extended abstracts Workshop and GLACIODYN (IPY) meeting, 15 - 18 January 2007, Pontresina (Switzerland) IASCIASC WorkingWorking groupgroup onon ArcticArctic GlaciologyGlaciology Institute for Marine and Atmospheric Research Utrecht Utrecht University, The Netherlands The Dynamics and Mass Budget of Arctic Glaciers Extended abstracts Workshop and GLACIODYN (IPY) Meeting, 15 - 18 January 2007, Pontresina (Switzerland) IASC Working Group on Arctic Glaciology Organized by J. Oerlemans and C.H. Tijm-Reijmer Institute for Marine and Atmospheric Research Utrecht Utrecht University, The Netherlands 1 2 CONTENTS Preface..............................................................................................7 Johannes Oerlemans Program ............................................................................................9 List of participants.........................................................................13 Abstracts ........................................................................................17 20th Century evolution and modelling of Hoffellsjökull, Southeast Iceland .........................................................................................18 Gufinna Aalgeirsdóttir, H. Björnsson, F. Pálsson and S.P. Sigursson The surface energy balance of Storbreen....................................20 Liss M. Andreassen, M.R. van den Broeke, J. Oerlemans Topographic controls on the spatial variability of glacier surface energy balance ............................................................................23 -
Non Illegal Chimera.Pdf
DECAMERON NON-ILLEGAL CHIMERA’S DECAMERON PACKET 1. This planet contains an extended corona of about 50,000 km that contains elemental hydrogen. The proposed MUSE mission will study this planet’s atmosphere. This is the smaller of two planets proposed to contain a layer of superionic water. The mantle of this planet may feature an ocean of liquid diamond with floating "diamond-bergs." This planet’s magnetotail is (*) twisted into a corkscrew shape. This planet’s rings are named for greek letters and it was originally called George's Star by its discoverer William Herschel. Moons of this planet are named for characters in works of Shakespeare and Alexander Pope, such as Miranda, Oberon and Titania. For 10 points, name this blue "ice giant" known for its extreme axial tilt, the seventh planet from the sun. ANSWER: Uranus <Calin, Science - Earth/Space> 2. This character hears the sayings of Solomon such as "a good name is better than a precious ointment" from his father. In a novel, after receiving a diamond and a red purse, Julie Herbault receives a letter from an alias named after this character. This character creates a stirrup for a horse for a society that buries a couple once one of them dies. It’s not Odysseus, but this character escapes from and blinds a man-eating giant. This character tells a similarly named (*) porter his story after the porter asks God why this character is so rich. In The Count of Monte Cristo, this character’s name is adopted by Edmund Dantes, and in another work, this character sees a valley of diamonds after tying his turban to the leg of a roc. -
HAULING OUT: International Trade and Management of Walrus
HAULING OUT: International Trade and Management of Walrus Tanya Shadbolt, Tom Arnbom, & Ernest W. T. Cooper A TRAFFIC REPORT HaulingOut_REPORT_FINAL.indd 1 2014-05-13 6:21 PM © 2014 World Wildlife Fund. All rights reserved. ISBN: 978-0-9693730-9-4 All material appearing in this publication is copyrighted and may be reproduced with permission. Any reproduction, in full or in part, of this publication must credit TRAFFIC. The views of the authors expressed in this publication do not necessarily reflect those of TRAFFIC, World Wildlife Fund (WWF), or the International Union for Conservation of Nature (IUCN). The designation of geographical entities in this publication and the presentation of the material do not imply the expression of any opinion whatsoever on the part of WWF, TRAFFIC, or 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 TRAFFIC symbol copyright and Registered Trademark ownership are held by WWF. TRAFFIC is a strategic alliance of WWF and IUCN. Suggested citation: Shadbolt, T., Arnbom, T. and Cooper, E.W.T. (2014). Hauling Out: International Trade and Management of Walrus. TRAFFIC and WWF-Canada. Vancouver, B.C. Cover photo: Pacific walrus (Odobenus rosmarus divergens) males hauled out at Round Island, Alaska, United States © Kevin Schafer/WWF-Canon HaulingOut_REPORT_FINAL.indd 2 2014-05-13 6:21 PM TABLE OF CONTENTS Table of Contents i Acknowledgements v Executive Summary 1 1 Introduction 9 1.1 Purpose of the report -
Ward Hunt Island and Vicinity1
18 (3): 236-261 (2011) Extreme ecosystems and geosystems in the Canadian High Arctic: Ward Hunt Island and vicinity1 Warwick F. VINCENT2, Centre d’études nordiques and Département de biologie, Université Laval, Québec, Québec, Canada, [email protected] Daniel FORTIER, Centre d’études nordiques and Département de géographie, Université de Montréal, Montréal, Québec, Canada. Esther LÉVESQUE, Noémie BOULANGER-LAPOINTE & Benoît TREMBLAY, Centre d’études nordiques and Département de chimie-biologie, Université du Québec à Trois-Rivières, Trois-Rivières, Québec, Canada. Denis SARRAZIN, Centre d’études nordiques, Université Laval, Québec, Québec, Canada. Dermot ANTONIADES, Sección Limnología, Facultad de Ciencias, Universidad de la Republica, Montevideo, Uruguay. Derek R. MUELLER, Department of Geography and Environmental Studies, Carleton University, Ottawa, Ontario, Canada. Abstract: Global circulation models predict that the strongest and most rapid effects of global warming will take place at the highest latitudes of the Northern Hemisphere. Consistent with this prediction, the Ward Hunt Island region at the northern terrestrial limit of Arctic Canada is experiencing the onset of major environmental changes. This article provides a synthesis of research including new observations on the diverse geosystems/ecosystems of this coastal region of northern Ellesmere Island that extends to latitude 83.11° N (Cape Aldrich). The climate is extreme, with an average annual air temperature of –17.2 °C, similar to Antarctic regions such as the McMurdo Dry Valleys. The region is geologically distinct (the Pearya Terrane) and contains steep mountainous terrain intersected by deep fiords and fluvial valleys. Numerous glaciers flow into the valleys, fiords, and bays, and thick multi-year sea ice and ice shelves occur along the coast. -
Qikiqtani Inuit Association 2010
QTC Interview and Testimony Summaries Qikiqtani Inuit Association 2010 NOTICE TO READER This document was submitted 20 October 2010 at the Board Meeting of the Qikiqtani Inuit Association. Qikiqtani Inuit Association P.O. Box 1340 Iqaluit, NU X0A 0H0 Phone: (867) 975-8400 Fax: (867) 979-3238 The preparation of this document was completed under the direction of: Madeleine Redfern Executive Director, Qikiqtani Truth Commission P.O. Box 1340 Iqaluit, NU X0A 0H0 Tel: (867) 975-8426 Fax: (867) 979-1217 Email: [email protected] Table of Contents: Introduction ................................................................................................................................................... 1 Contents .................................................................................................................................................... 1 QIA interviews .......................................................................................................................................... 1 QTC interviews ......................................................................................................................................... 1 Photos ........................................................................................................................................................ 2 Arctic Bay ................................................................................................................................................. 3 Qikiqtani Inuit Association .................................................................................................................. -
Melting Characteristics of Snow Cover on Tidewater Glaciers in Hornsund Fjord, Svalbard
water Article Melting Characteristics of Snow Cover on Tidewater Glaciers in Hornsund Fjord, Svalbard Michał Laska 1,* ID , Barbara Barzycka 1 and Bartłomiej Luks 2 ID 1 Faculty of Earth Sciences, University of Silesia in Katowice, B˛edzi´nska60, 41-200 Sosnowiec, Poland; [email protected] 2 Institute of Geophysics, Polish Academy of Sciences, Ksi˛eciaJanusza 64, 01-452 Warsaw, Poland; [email protected] * Correspondence: [email protected]; Tel.: +48-32-36-89-896 Received: 16 August 2017; Accepted: 16 October 2017; Published: 19 October 2017 Abstract: In recent years, the Svalbard area, especially its southern section, has been characterised by an exceptionally thin snow cover, which has a significant impact of the annual mass balance of glaciers. The objective of this study was to determine melting processes of the snow cover deposited on 11 glaciers that terminate into Hornsund Fjord during the melting period of 2014. The study included analyses of snow pits and snow cores, meteorological data collected from automatic weather stations and Polish Polar Station Hornsund, and supervised classification of six Landsat 8 images for assessing the progress of snow cover melting. The calculated Snow-Covered Area (SCA) varied from 98% at the beginning of the melting season to 43% at the end of August. The melting vertical gradient on Hansbreen was −0.34 m 100 m−1, leading to surface melting of −1.4 cm water equivalent (w.e.) day−1 in the ablation zone (c. 200 m a.s.l. (above sea level)) and −0.7 cm w.e. day−1 in the accumulation zone (c. -
Bathymetry and Geographical Regionalization of Brepollen (Hornsund, Spitsbergen) Based on Bathymetric Profiles Interpolations
vol. 34, no. 1, pp. 1–22, 2013 doi: 10.2478/popore−2013−0001 Bathymetry and geographical regionalization of Brepollen (Hornsund, Spitsbergen) based on bathymetric profiles interpolations Mateusz MOSKALIK1, Piotr GRABOWIECKI1, Jarosław TĘGOWSKI2 and Monika ŻULICHOWSKA3 1 Instytut Geofizyki, Polska Akademia Nauk, ul. Księcia Janusza 64, 01−452 Warszawa, Poland <[email protected]> <[email protected]> 2 Wydział Oceanografii i Geografii, Uniwersytet Gdański, Al. M. Piłsudskiego 46, 81−378 Gdynia, Poland <[email protected]> 3 Wydział Biologii i Nauk o Ziemi, Uniwersytet Jagielloński, ul. Gronostajowa 7, 30−387 Kraków, Poland <[email protected]> Abstract: Determination of High Arctic regions bathymetry is strictly dependent from weather and ice mass quantity. Due to safety, it is often necessary to use a small boat to study fjords area, especially close to glaciers with unknown bathymetry. This precludes the use of modern multi−beam echosounders, and so traditional single−beam echosounders have been used for bathymetry profiling. Adequate interpolation techniques were determined for the most probable morphological formations in−between bathymetric profiles. Choosing the most accurate interpolation method allows for the determination of geographical regionalisation of submarine elevations of the Brepollen area (inner part of Hornsund, Spitsbergen). It has also been found that bathymetric interpolations should be performed on averaged grid values, rather than individual records. The Ordinary Kriging Method was identified as the most adequate for interpolations and was compared with multi beam scan− ning, which was possible to make due to a previously modelled single beam interpolation map. In total, eight geographical units were separated in Brepollen, based on the bathy− metry, slope and aspect maps.