Auyuittuq National Park of Canada Spring 2005

Total Page:16

File Type:pdf, Size:1020Kb

Auyuittuq National Park of Canada Spring 2005 Auyuittuq National Park of Canada Spring 2005 Location Auyuittuq Auyuittuq National Park lies on the northeastern Vegetation Activities shore of Baffin Island, Nunavut, almost entirely National Park of Canada within the Arctic Circle. It was established in There are no trees in Auyuittuq. Plant-life Visitors can obtain the service of an outfitter to Pronounced “Ow-you-eet-took” 1976. Auyuittuq means "the land that does not consists of shrub willows, heather, sedge take them the final stretch from Pangnirtung to melt" and is at the northern extreme of the grasses, lichens, mosses, and a short season Pangnirtung Pass. Access to the park is either by Canadian Shield, on the island's Cumberland of colourful wildflowers. They thrive under outfitters' boat or snowmobile, or hiking, or cross- Peninsula.The park protects a representative the moist and sunny conditions of summer. country skiing. Once in the park, visitors are Climate sample of the Northern Davis Natural Region, Arctic willow is the tallest tundra species. virtually on their own, carrying all their needs with and includes 19 089 km2 of mountains, fjords, and Other plants include the Arctic poppy, them. Most people come to hike the Pass' trail, The park's polar marine climate causes long, glaciers. Pangnirtung is the closest community cotton grass, and broad-leaved willow herb. which has three designated campsites, though cold winters, and short, cool summers. Snow to the park, and is accessible by airline from Most plants grow in clumps which helps to random camping is permitted. Broughton Island exists year-round, though precipitation is only Iqaluit. The park can also be reached via preserve warmth, and many grow in and Pangnirtung have hotels and lodges. A few about 200 mm annually. Average temperature tussocks. These are essentially a mound of fixed-roof emergency shelters are located in the ooBroughton Island, but is inaccessible to hikers highs are -23 C in January and 10 C in July. during ice break-up in July and August. built-up root systems that continue to park. Mountain climbers come from all over the Weather patterns are extreme and Auyuittuq is a vast, unspoiled increase each year. world to scale Auyuittuq’s peaks. Cumberland unpredictable, and strong breezes usually arctic wilderness. Auyuittuq is located in the Sound offers excellent fishing for Arctic char. blow along the fjords. A few brief weeks of Arctic Cordillera Ecozone. Wilderness trekkers must register with the park endless daylight in the summer are countered office, and a "no trace" camping ethic is strongly by a similar period of endless night during the encouraged. Even campfires are not permitted. middle of winter. Any garbage or other refuse, including organic Wildlife waste, remains undecomposed for decades and can diminish a later visitor's park experience. The animal life of Auyuittuq National Park is a small but hardy assemblage of 12 Geology mammal species, and about 40 types of Home birds. Land mammals include lemmings, The park's rugged mountain tundra is rich Bay Arctic hares, Arctic fox, polar bears, and D ie a with glaciers, fjords, and is dominated by d v ro y is caribou. In the adjacent seas there are B a B a y the massive Penny Ice Cap. This area of B S populations of Beluga whales, narwhal, a t o ra k i solid ice is over 300 m thick and covers O t walrus, and Ringed, Bearded, and Harp 2 some 5 100 km . It is a remnant of the huge seals. Bird species include snow geese, ice sheets that once covered much of North Eider ducks, and shorebirds such as America. The Penny Highland mountains, PE Broughton NN Island glaucous gulls. One can also observe Y composed of typical Shield granite, reach I ptarmigan, snowy owls, gyrfalcons, ravens, Greenshield C Lake E heights of over 2 000 m. Along the coast, C and the occasional finches and sparrows. A P narrow fjords with high (up to 900 m), steep Glacier/Icefield Sea life is generally more plentiful than that walls show where glaciers have created found on land. Most of the animals are For more information, contact: The Superintendent valley floors below sea level. N distinctly adapted to their arctic Auyuittuq National Park Nunavut Field Unit ARCTIC CIRCLE environment, possessing thick coats of fur or down feathers, insulating layers of P.O. Box 353 Pangnirtung, Nunavut Cumberland Sound blubber, and short ears to help conserve X0A 0R0 Pangnirtung 0 44 000 m essential body heat. Telephone: (867) 473-8828 © Parks Canada Fax: (867) 473-8612 Website: www.pc.gc.ca/auyuittuq Auyuittuq National Park of Canada Spring 2005 Location Auyuittuq Auyuittuq National Park lies on the northeastern Vegetation Activities shore of Baffin Island, Nunavut, almost entirely National Park of Canada within the Arctic Circle. It was established in There are no trees in Auyuittuq. Plant-life Visitors can obtain the service of an outfitter to Pronounced “Ow-you-eet-took” 1976. Auyuittuq means "the land that does not consists of shrub willows, heather, sedge take them the final stretch from Pangnirtung to melt" and is at the northern extreme of the grasses, lichens, mosses, and a short season Pangnirtung Pass. Access to the park is either by Canadian Shield, on the island's Cumberland of colourful wildflowers. They thrive under outfitters' boat or snowmobile, or hiking, or cross- Peninsula.The park protects a representative the moist and sunny conditions of summer. country skiing. Once in the park, visitors are Climate sample of the Northern Davis Natural Region, Arctic willow is the tallest tundra species. virtually on their own, carrying all their needs with and includes 19 089 km2 of mountains, fjords, and Other plants include the Arctic poppy, them. Most people come to hike the Pass' trail, The park's polar marine climate causes long, glaciers. Pangnirtung is the closest community cotton grass, and broad-leaved willow herb. which has three designated campsites, though cold winters, and short, cool summers. Snow to the park, and is accessible by airline from Most plants grow in clumps which helps to random camping is permitted. Broughton Island exists year-round, though precipitation is only Iqaluit. The park can also be reached via preserve warmth, and many grow in and Pangnirtung have hotels and lodges. A few about 200 mm annually. Average temperature tussocks. These are essentially a mound of fixed-roof emergency shelters are located in the ooBroughton Island, but is inaccessible to hikers highs are -23 C in January and 10 C in July. during ice break-up in July and August. built-up root systems that continue to park. Mountain climbers come from all over the Weather patterns are extreme and Auyuittuq is a vast, unspoiled increase each year. world to scale Auyuittuq’s peaks. Cumberland unpredictable, and strong breezes usually arctic wilderness. Auyuittuq is located in the Sound offers excellent fishing for Arctic char. blow along the fjords. A few brief weeks of Arctic Cordillera Ecozone. Wilderness trekkers must register with the park endless daylight in the summer are countered office, and a "no trace" camping ethic is strongly by a similar period of endless night during the encouraged. Even campfires are not permitted. middle of winter. Any garbage or other refuse, including organic Wildlife waste, remains undecomposed for decades and can diminish a later visitor's park experience. The animal life of Auyuittuq National Park is a small but hardy assemblage of 12 Geology mammal species, and about 40 types of Home birds. Land mammals include lemmings, The park's rugged mountain tundra is rich Bay Arctic hares, Arctic fox, polar bears, and D ie a with glaciers, fjords, and is dominated by d v ro y is caribou. In the adjacent seas there are B a B a y the massive Penny Ice Cap. This area of B S populations of Beluga whales, narwhal, a t o ra k i solid ice is over 300 m thick and covers O t walrus, and Ringed, Bearded, and Harp 2 some 5 100 km . It is a remnant of the huge seals. Bird species include snow geese, ice sheets that once covered much of North Eider ducks, and shorebirds such as America. The Penny Highland mountains, PE Broughton NN Island glaucous gulls. One can also observe Y composed of typical Shield granite, reach I ptarmigan, snowy owls, gyrfalcons, ravens, Greenshield C Lake E heights of over 2 000 m. Along the coast, C and the occasional finches and sparrows. A P narrow fjords with high (up to 900 m), steep Glacier/Icefield Sea life is generally more plentiful than that walls show where glaciers have created found on land. Most of the animals are For more information, contact: The Superintendent valley floors below sea level. N distinctly adapted to their arctic Auyuittuq National Park Nunavut Field Unit ARCTIC CIRCLE environment, possessing thick coats of fur or down feathers, insulating layers of P.O. Box 353 Pangnirtung, Nunavut Cumberland Sound blubber, and short ears to help conserve X0A 0R0 Pangnirtung 0 44 000 m essential body heat. Telephone: (867) 473-8828 © Parks Canada Fax: (867) 473-8612 Website: www.pc.gc.ca/auyuittuq.
Recommended publications
  • Origin, Burial and Preservation of Late Pleistocene-Age Glacier Ice in Arctic
    Origin, burial and preservation of late Pleistocene-age glacier ice in Arctic permafrost (Bylot Island, NU, Canada) Stephanie Coulombe1 2 3, Daniel Fortier 2 3 5, Denis Lacelle4, Mikhail Kanevskiy5, Yuri Shur5 6 1Polar Knowledge Canada, Cambridge Bay, X0B 0C0, Canada 5 2Department of Geography, Université de Montréal, Montréal, H2V 2B8, Canada 3Centre for Northern Studies, Université Laval, Quebec City, G1V 0A6, Canada 4Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, K1N 6N5, Canada 5Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5910, USA 6Department of Civil and Environmental Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5960, USA 10 Correspondence to: Stephanie Coulombe ([email protected]) Over the past decades, observations of buried glacier ice exposed in coastal bluffs and headwalls of retrogressive thaw slumps of the Arctic indicate that considerable amounts of late Pleistocene glacier ice survived the deglaciation and are still preserved in permafrost. In exposures, relict glacier ice and intrasedimental ice often coexist and look alike but their genesis is strikingly different. This paper aims to present a detailed description and infer the origin of a massive ice body preserved in the permafrost 15 of Bylot Island (Nunavut). The massive ice exposure and core samples were described according to the cryostratigraphic approach, combining the analysis of permafrost cryofacies and cryostructures, ice crystallography, stable O-H isotopes and cation contents. The ice was clear to whitish in appearance with large crystals (cm) and small gas inclusions (mm) at crystal intersections, similar to observations of englacial ice facies commonly found on contemporary glaciers and ice sheets.
    [Show full text]
  • Baffin Island: Field Research and High Arctic Adventure, 1961-1967
    University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2016-02 Baffin Island: Field Research and High Arctic Adventure, 1961-1967 Ives, Jack D. University of Calgary Press Ives, J.D. "Baffin Island: Field Research and High Arctic Adventure, 1961-1967." Canadian history and environment series; no. 18. University of Calgary Press, Calgary, Alberta, 2016. http://hdl.handle.net/1880/51093 book http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca BAFFIN ISLAND: Field Research and High Arctic Adventure, 1961–1967 by Jack D. Ives ISBN 978-1-55238-830-3 THIS BOOK IS AN OPEN ACCESS E-BOOK. It is an electronic version of a book that can be purchased in physical form through any bookseller or on-line retailer, or from our distributors. Please support this open access publication by requesting that your university purchase a print copy of this book, or by purchasing a copy yourself. If you have any questions, please contact us at [email protected] Cover Art: The artwork on the cover of this book is not open access and falls under traditional copyright provisions; it cannot be reproduced in any way without written permission of the artists and their agents. The cover can be displayed as a complete cover image for the purposes of publicizing this work, but the artwork cannot be extracted from the context of the cover of this specific work without breaching the artist’s copyright.
    [Show full text]
  • EXPERIENCES 2021 Table of Contents
    NUNAVUT EXPERIENCES 2021 Table of Contents Arts & Culture Alianait Arts Festival Qaggiavuut! Toonik Tyme Festival Uasau Soap Nunavut Development Corporation Nunatta Sunakkutaangit Museum Malikkaat Carvings Nunavut Aqsarniit Hotel And Conference Centre Adventure Arctic Bay Adventures Adventure Canada Arctic Kingdom Bathurst Inlet Lodge Black Feather Eagle-Eye Tours The Great Canadian Travel Group Igloo Tourism & Outfitting Hakongak Outfitting Inukpak Outfitting North Winds Expeditions Parks Canada Arctic Wilderness Guiding and Outfitting Tikippugut Kool Runnings Quark Expeditions Nunavut Brewing Company Kivalliq Wildlife Adventures Inc. Illu B&B Eyos Expeditions Baffin Safari About Nunavut Airlines Canadian North Calm Air Travel Agents Far Horizons Anderson Vacations Top of the World Travel p uit O erat In ed Iᓇᓄᕗᑦ *denotes an n u q u ju Inuit operated nn tau ut Aula company About Nunavut Nunavut “Our Land” 2021 marks the 22nd anniversary of Nunavut becoming Canada’s newest territory. The word “Nunavut” means “Our Land” in Inuktut, the language of the Inuit, who represent 85 per cent of Nunavut’s resident’s. The creation of Nunavut as Canada’s third territory had its origins in a desire by Inuit got more say in their future. The first formal presentation of the idea – The Nunavut Proposal – was made to Ottawa in 1976. More than two decades later, in February 1999, Nunavut’s first 19 Members of the Legislative Assembly (MLAs) were elected to a five year term. Shortly after, those MLAs chose one of their own, lawyer Paul Okalik, to be the first Premier. The resulting government is a public one; all may vote - Inuit and non-Inuit, but the outcomes reflect Inuit values.
    [Show full text]
  • Across Borders, for the Future: Torngat Mountains Caribou Herd Inuit
    ACROSS BORDERS, FOR THE FUTURE: Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study Prepared for the Nunatsiavut Government and Makivik Corporation, Parks Canada, and the Torngat Wildlife and Plants Co-Management Board - June 2014 This report may be cited as: Wilson KS, MW Basterfeld, C Furgal, T Sheldon, E Allen, the Communities of Nain and Kangiqsualujjuaq, and the Co-operative Management Board for the Torngat Mountains National Park. (2014). Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study. Final Report to the Nunatsiavut Government, Makivik Corporation, Parks Canada, and the Torngat Wildlife and Plants Co-Management Board. Nain, NL. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise (except brief passages for purposes of review) without the prior permission of the authors. Inuit Knowledge is intellectual property. All Inuit Knowledge is protected by international intellectual property rights of Indigenous peoples. As such, participants of the Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study reserve the right to use and make public parts of their Inuit Knowledge as they deem appropriate. Use of Inuit Knowledge by any party other than hunters and Elders of Nunavik and Nunatsiavut does not infer comprehensive understanding of the knowledge, nor does it infer implicit support for activities or projects in which this knowledge is used in print, visual, electronic, or other media. Cover photo provided by and used with permission from Rodd Laing. All other photos provided by the lead author.
    [Show full text]
  • Cryosat-2 Delivers Monthly and Inter-Annual Surface Elevation Change for Arctic Ice Caps
    The Cryosphere, 9, 1895–1913, 2015 www.the-cryosphere.net/9/1895/2015/ doi:10.5194/tc-9-1895-2015 © Author(s) 2015. CC Attribution 3.0 License. CryoSat-2 delivers monthly and inter-annual surface elevation change for Arctic ice caps L. Gray1, D. Burgess2, L. Copland1, M. N. Demuth2, T. Dunse3, K. Langley3, and T. V. Schuler3 1Department of Geography, University of Ottawa, Ottawa, K1N 6N5, Canada 2Natural Resources Canada, Ottawa, Canada 3Department of Geosciences, University of Oslo, Oslo, Norway Correspondence to: L. Gray ([email protected]) Received: 29 April 2015 – Published in The Cryosphere Discuss.: 26 May 2015 Revised: 15 August 2015 – Accepted: 3 September 2015 – Published: 25 September 2015 Abstract. We show that the CryoSat-2 radar altimeter can 1 Introduction provide useful estimates of surface elevation change on a variety of Arctic ice caps, on both monthly and yearly Recent evidence suggests that mass losses from ice caps and timescales. Changing conditions, however, can lead to a glaciers will contribute significantly to sea level rise in the varying bias between the elevation estimated from the radar coming decades (Meier et al., 2007; Gardner et al., 2013; altimeter and the physical surface due to changes in the ratio Vaughan et al., 2013). However, techniques to measure the of subsurface to surface backscatter. Under melting condi- changes of smaller ice caps are very limited: Satellite tech- tions the radar returns are predominantly from the surface so niques, such as repeat gravimetry from GRACE (Gravity Re- that if surface melt is extensive across the ice cap estimates covery and Climate Experiment), favour the large Greenland of summer elevation loss can be made with the frequent or Antarctic Ice Sheets, while ground and airborne exper- coverage provided by CryoSat-2.
    [Show full text]
  • Auyuittuq, Hiking Expedition
    Auyuittuq, Hiking Expedition Program Descriptive & Day-by-day: Auyuittuq National Park Majestic towers, carved in bedrock by glaciers, shooting straight for the sun: such scenery is what Auyuittuq National Park has to offer. It is, without a doubt, one of the most awe-inspiring places on Earth. Set in the middle of the Penny Ice Cap, bisected from North to South by the Akshayuk pass, an immense valley opens inland. After a two-day hike surrounded by severe-looking, barren plateaus, we will set up base camp. From there, you will go on a day hike to one of the most spectacular lookouts of the park, Mount Thor. On your way, you will have an opportunity to see impressive rock formations dating back to the last ice age, moraines, boulder fields, and much more. During this five-day hike, you will tread over terrain ranging from arid gravel to humid, fertile tundra, with sharp peaks and a huge glacier in the backdrop. Memories like these are unlikely to fade away. The hiking trip To hike Auyuittuq Park you will need to be able to walk with a 16 to 20 kg (35-45 lb) back pack for a distance of 8 to 18 km (5 to 12 mi) per day (4 to 8 hours a day). Trail is not technical and do not present an altitude challenge, be ready to have, at moment to cross glacier river (water high to your knees). Days will be spent in the great outdoor while nights will be spent in tent. You should be prepared to live outside for the entire trip and have minimal camping experience Kekerten Island and Pangnirtung After leaving Auyuittuq Park, an Inuit guide will take you on a boat ride to the remarkable Kekerten Island.
    [Show full text]
  • Caribou (Barren-Ground Population) Rangifer Tarandus
    COSEWIC Assessment and Status Report on the Caribou Rangifer tarandus Barren-ground population in Canada THREATENED 2016 COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC. 2016. COSEWIC assessment and status report on the Caribou Rangifer tarandus, Barren-ground population, in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. xiii + 123 pp. (http://www.registrelep-sararegistry.gc.ca/default.asp?lang=en&n=24F7211B-1). Production note: COSEWIC would like to acknowledge Anne Gunn, Kim Poole, and Don Russell for writing the status report on Caribou (Rangifer tarandus), Barren-ground population, in Canada, prepared under contract with Environment Canada. This report was overseen and edited by Justina Ray, Co-chair of the COSEWIC Terrestrial Mammals Specialist Subcommittee, with the support of the members of the Terrestrial Mammals Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment and Climate Change Canada Ottawa, ON K1A 0H3 Tel.: 819-938-4125 Fax: 819-938-3984 E-mail: [email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur le Caribou (Rangifer tarandus), population de la toundra, au Canada. Cover illustration/photo: Caribou — Photo by A. Gunn. Her Majesty the Queen in Right of Canada, 2016. Catalogue No. CW69-14/746-2017E-PDF ISBN 978-0-660-07782-6 COSEWIC Assessment Summary Assessment Summary – November 2016 Common name Caribou - Barren-ground population Scientific name Rangifer tarandus Status Threatened Reason for designation Members of this population give birth on the open arctic tundra, and most subpopulations (herds) winter in vast subarctic forests.
    [Show full text]
  • A Descriptiol\ of the PENNY ICE CAP. ITS Accuml: LATION and ABLATION
    342 JOURNAL OF GLACIOLOGY STUDIES IN GLACIER PHYSICS ON THE PENNY ICE CAP, BAFFIN ISLAND, I953 INTRODUCTION Studies in glacier physics formed a major part of the work of the Baffin Island Expedition, 1953, the second expedition of the Arctic Institute of North America to Baffin. This work will be reported in a series of articles in this journal: the first (Part I) appears below; further parts will follow in due course. It was decided to visit the Penny Ice Cap of the Cumberland Peninsula as a sequel to our work on the Barnes Tee Cap in 1950, since it is the only other large area of glaciation in Baffin Island and because our knowledge of the glaciation of the eastern Canadian Arctic is still very limited. From a study of the aerial photographs taken by the Roya l Canadian Air Force in 1948 and the map, together with a consideration of the general resources of the expedition, it was planned to land a glacio-meteorological camp (Camp AI) by means of a Norseman aircraft on a high dome of the ice cap and another camp in the region of the firn line of onc of the more accessible glaciers (now called Highway Glacier) flowing into the head of the Pangnirtung Pass (see Figs. I and 3, pp. 343 and 347). Here there are two lakes, which were considered to be suitable for spring and autumn aircraft landings and for a base camp. From the two glacier camps it was planned to assess the particular regimen of the glaciation and to couple with this studies of some more general problems in glacier physics.
    [Show full text]
  • Ice Velocity Changes on Penny Ice Cap, Baffin Island, Since the 1950S
    Journal of Glaciology (2017), Page 1 of 15 doi: 10.1017/jog.2017.40 © The Author(s) 2017. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Ice velocity changes on Penny Ice Cap, Baffin Island, since the 1950s NICOLE SCHAFFER,1,2 LUKE COPLAND,1 CHRISTIAN ZDANOWICZ3 1Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, Ontario K1N 6N5, Canada 2Natural Resources Canada, Geological Survey of Canada, 601 Booth St., Ottawa, Ontario K1A 0E8, Canada 3Department of Earth Sciences, Uppsala University, Uppsala 75236, Sweden Correspondence: Nicole Schaffer <[email protected]> ABSTRACT. Predicting the velocity response of glaciers to increased surface melt is a major topic of ongoing research with significant implications for accurate sea-level rise forecasting. In this study we use optical and radar satellite imagery as well as comparisons with historical ground measurements to produce a multi-decadal record of ice velocity variations on Penny Ice Cap, Baffin Island. Over the period 1985–2011, the six largest outlet glaciers on the ice cap decelerated by an average rate of − − 21 m a 1 over the 26 year period (0.81 m a 2), or 12% per decade. The change was not monotonic, however, as most glaciers accelerated until the 1990s, then decelerated. A comparison of recent imagery with historical velocity measurements on Highway Glacier, on the southern part of Penny Ice − Cap, shows that this glacier decelerated by 71% between 1953 and 2009–11, from 57 to 17 m a 1.
    [Show full text]
  • Poster Presentations
    Poster Presentations Poster Presenting Author Title Number Air quality monitoring in communities of the Canadian arctic during the high shipping Aliabadi, Amir Abbas 73 season with a focus on local and marine pollution Allard, Michel 376 Permafrost International conference advertisment Vertical structure and environmental forcing of phytoplankton communities in the Beaufort Ardyna, Mathieu 139 Sea: Validation and application of novel satellite-derived phytoplankton indicators Spatial and Temporal Variability of Leaf Area Index and NDVI in a Sub-Arctic Tundra Arruda, Sean 279 Environment ASA 377 ASA Interactive Outreach Poster Occurrence and characteristics of Arctic Skate, Amblyraja hyperborea (Collette 1879) Atchison, Sheila 122 (Rajidae), in the Canadian Beaufort Use and analysis of community and industry observations of adverse marine and weather Atkinson, David E 76 states in the Western Canadian Arctic: A MEOPAR Project Atlaskina, Ksenia 346 Characterization of the northern snow albedo with satellite observations A permafrost temperature regime simulator as a learning tool for secondary school Inuit Aubé-Michaud, Sarah 29 students Awan, Malik 12 Wolverine: a traditional resource in Nunavut Bagnall, Ben 26 Spatial variability of hazard risk to infrastructure, Arviat, Nunavut Using a media scan to reveal disparities in the coverage of and conversation on issues of Baikie, Gail 38 importance to local women regarding the muskrat falls hydro-electric development in Labrador Balasubramaniam, Ann 62 Beyond Data Analysis: Learning to framing
    [Show full text]
  • Importance of Auyuittuq National Park
    Auyuittuq NATIONAL PARK OF CANADA Draft Management Plan January 2009 i Cover Photograph(s): (To be Added in Final Version of this Management Plan) National Library of Canada cataloguing in publication data: Parks Canada. Nunavut Field Unit. Auyuittuq National Park of Canada: Management Plan / Parks Canada. Issued also in French under title: Parc national du Canada Auyuittuq, plan directeur. Issued also in Inuktitut under title: ᐊᐅᔪᐃᑦᑐᖅ ᒥᕐᖑᐃᓯᕐᕕᓕᕆᔨᒃᑯᑦ ᑲᓇᑕᒥ ᐊᐅᓚᓯᓂᕐᒧᑦ ᐊᑐᖅᑕᐅᔪᒃᓴᖅ 1. Auyuittuq National Park (Nunavut)‐‐Management. 2. National parks and reserves‐‐Canada‐‐Management. 3. National parks and reserves‐‐Nunavut‐‐ Management. I. Parks Canada. Western and Northern Service Centre II. Title. FC XXXXXX 200X XXX.XXXXXXXXX C200X‐XXXXXX‐X © Her Majesty the Queen in the Right of Canada, represented by the Chief Executive Officer of Parks Canada, 200X. Paper: ISBN: XXXXXXXX Catalogue No.: XXXXXXXXX PDF: ISBN XXXXXXXXXXX Catalogue No.: XXXXXXXXXXXX Cette publication est aussi disponible en français. wktg5 wcomZoxaymuJ6 wktgotbsix3g6. i Minister’s Foreword (to be included when the Management Plan has been approved) QIA President’s Foreword (to be included when the Management Plan has been approved) NWMB Letter (to be included when the Management Plan has been approved) Recommendation Statement (to be included when the Management Plan has been approved) i Acknowledgements The preparation of this plan involved many people. The input of this diverse group of individuals has resulted in a plan that will guide the management of the park for many years.
    [Show full text]
  • National Park System: a Screening Level Assessment
    Environment Canada Parks Canada Environnement Canada Parcs Canada Edited by: Daniel Scott Adaptation & Impacts Research Group, Environment Canada and Roger Suffling School of Planning, University of Waterloo May 2000 Climate change and Canada’s national park system: A screening level assessment Le Changement climatique et le réseau des parcs nationaux du Canada : une évaluation préliminaire This report was prepared for Parks Canada, Department of Canadian Heritage by the Adaptation & Impacts Research Group, Environment Canada and the Faculty of Environmental Studies, University of Waterloo. The views expressed in the report are those of the study team and do not necessarily represent the opinions of Parks Canada or Environment Canada. Catalogue No.: En56-155/2000E ISBN: 0-662-28976-5 This publication is available in PDF format through the Adaptation and Impacts Research Group, Environment Canada web site < www1.tor.ec.gc.ca/airg > and available in Canada from the following Environment Canada office: Inquiry Centre 351 St. Joseph Boulevard Hull, Quebec K1A 0H3 Telephone: (819) 997-2800 or 1-800-668-6767 Fax: (819) 953-2225 Email: [email protected] i Climate change and Canada’s national park system: A screening level assessment Le Changement climatique et le réseau des parcs nationaux du Canada : une évaluation préliminaire Project Leads and Editors: Dr. Daniel Scott1 and Dr. Roger Suffling2 1 Adaptation and Impacts Research Group, Environment Canada c/o the Faculty of Environmental Studies, University of Waterloo Waterloo, Ontario N2L 3G1 519-888-4567 ext. 5497 [email protected] 2 School of Planning Faculty of Environmental Studies, University of Waterloo Waterloo, Ontario N2L 3G1 Research Team: Derek Armitage - Ph.D.
    [Show full text]