Effects of Climate Change on Arctic Ecosystems
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Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra
Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473. -
Cold Season Emissions Dominate the Arctic Tundra Methane Budget
Cold season emissions dominate the Arctic tundra methane budget Donatella Zonaa,b,1,2, Beniamino Giolic,2, Róisín Commaned, Jakob Lindaasd, Steven C. Wofsyd, Charles E. Millere, Steven J. Dinardoe, Sigrid Dengelf, Colm Sweeneyg,h, Anna Kariong, Rachel Y.-W. Changd,i, John M. Hendersonj, Patrick C. Murphya, Jordan P. Goodricha, Virginie Moreauxa, Anna Liljedahlk,l, Jennifer D. Wattsm, John S. Kimballm, David A. Lipsona, and Walter C. Oechela,n aDepartment of Biology, San Diego State University, San Diego, CA 92182; bDepartment of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, United Kingdom; cInstitute of Biometeorology, National Research Council, Firenze, 50145, Italy; dSchool of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138; eJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109-8099; fDepartment of Physics, University of Helsinki, FI-00014 Helsinki, Finland; gCooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80304; hEarth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO 80305; iDepartment of Physics and Atmospheric Science, Dalhousie University, Halifax, Nova Scotia, Canada B3H 4R2; jAtmospheric and Environmental Research, Inc., Lexington, MA 02421; kWater and Environmental Research Center, University of Alaska Fairbanks, Fairbanks, AK 99775-7340; lInternational Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK 99775-7340; mNumerical Terradynamic Simulation -
AAR Chapter 2
Go back to opening screen 9 Chapter 2 Physical/Geographical Characteristics of the Arctic –––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––– Contents 2.2.1. Climate boundaries 2.1. Introduction . 9 On the basis of temperature, the Arctic is defined as the area 2.2. Definitions of the Arctic region . 9 2.2.1. Climate boundaries . 9 north of the 10°C July isotherm, i.e., north of the region 2.2.2. Vegetation boundaries . 9 which has a mean July temperature of 10°C (Figure 2·1) 2.2.3. Marine boundary . 10 (Linell and Tedrow 1981, Stonehouse 1989, Woo and Gre- 2.2.4. Geographical coverage of the AMAP assessment . 10 gor 1992). This isotherm encloses the Arctic Ocean, Green- 2.3. Climate and meteorology . 10 2.3.1. Climate . 10 land, Svalbard, most of Iceland and the northern coasts and 2.3.2. Atmospheric circulation . 11 islands of Russia, Canada and Alaska (Stonehouse 1989, 2.3.3. Meteorological conditions . 11 European Climate Support Network and National Meteoro- 2.3.3.1. Air temperature . 11 2.3.3.2. Ocean temperature . 12 logical Services 1995). In the Atlantic Ocean west of Nor- 2.3.3.3. Precipitation . 12 way, the heat transport of the North Atlantic Current (Gulf 2.3.3.4. Cloud cover . 13 Stream extension) deflects this isotherm northward so that 2.3.3.5. Fog . 13 2.3.3.6. Wind . 13 only the northernmost parts of Scandinavia are included. 2.4. Physical/geographical description of the terrestrial Arctic 13 Cold water and air from the Arctic Ocean Basin in turn 2.4.1. -
Spring 2016 ᐅᐱᕐᖔᖅ Nunavut Arctic College Media Spring 2016 ᓄᓇᕗᑦ ᓯᓚᑦᑐᖅᓴᕐᕕᖕᒥ ᑐᓴᖃᑦᑕᐅᑎᓕᕆᔩᑦ Spring 2016
Spring 2016 ᐅᐱᕐᖔᖅ Nunavut Arctic College Media Spring 2016 ᓄᓇᕗᑦ ᓯᓚᑦᑐᖅᓴᕐᕕᖕᒥ ᑐᓴᖃᑦᑕᐅᑎᓕᕆᔩᑦ Spring 2016 LOOK UP! • AARLURIT ! • ᐋᕐᓗᕆᑦ! FRONTLIST Nunavut Arctic College has been publishing for almost three decades. Our press predates the political creation of Nunavut, but not the historical reality of a distinct Inuit land. We have been around for some time, yet we are new on the landscape of Canadian publishing. Most people across Canada (and the world) are not familiar with our books. There is a good reason for this. Our books were purposefully published to serve students, Willem Rasing teachers, and community members in the Eastern Arctic. These works were not intended for wide distribution, enviable sales, or awards; they exist as urgent, at times rough-hewn manifestations of intimate and collaborative efforts to archive the ISBN: 978-1-897568-40-8 knowledge and history of unique generations. The narrators in our pages are often $27.95 Inuit who weathered the bewildering movement from the land to static settlements in May 2016 the mid-20th century, and those who entered residential schools. 6” x 9” | 312 pages Notwithstanding our territorial obligation to date, our work has benefitted from the Trade paperback engagement and initiative of outsiders. Alongside Inuit Elders, leaders, educators, English students, and translators, a perusal of our books reveals the thoughtful participation of southern and international writers, editors, and scholars. These encounters blur the binaries of Inuit and Qallunaaq (southerner) ways of knowing, doing, and telling. They Cultural studies; Native studies; History arouse the tension, possibility, and limitation in the fusion of Western written custom and Inuit oral tradition. -
Circumpolar Arctic Vegetation Classification
Phytocoenologia Research Paper Published online December 2017 Open Access Article Circumpolar Arctic Vegetation Classification Donald A. Walker*, Fred J.A. Daniëls, Nadezhda V. Matveyeva, Jozef Šibík, Marilyn D. Walker, Amy L. Breen, Lisa A. Druckenmiller, Martha K. Raynolds, Helga Bültmann, Stephan Hennekens, Marcel Buchhorn, Howard E. Epstein, Ksenia Ermokhina, Anna M. Fosaa, Starri Hei∂marsson, Birgit Heim, Ingibjörg S. Jónsdóttir, Natalia Koroleva, Esther Lévesque, William H. MacKenzie, Greg H.R. Henry, Lennart Nilsen, Robert Peet, Volodya Razzhivin, Stephen S. Talbot, Mikhail Telyatnikov, Dietbert Thannheiser, Patrick J. Webber & Lisa M. Wirth Abstract Aims: An Arctic Vegetation Classification (AVC) is needed to address issues related to rapid Arctic-wide changes to climate, land-use, and biodiversity. Location: The 7.1 million km2 Arctic tundra biome. Approach and conclusions: The purpose, scope and conceptual framework for an Arctic Vegetation Archive (AVA) and Classification (AVC) were developed during numerous workshops starting in 1992. The AVA and AVC are modeled after the European vegetation archive (EVA) and classification (EVC). The AVA will use Turboveg for data management. The AVC will use a Braun-Blanquet (Br.-Bl.) classification approach. There are approxi- mately 31,000 Arctic plots that could be included in the AVA. An Alaska AVA (AVA-AK, 24 datasets, 3026 plots) is a prototype for archives in other parts of the Arctic. The plan is to eventually merge data from other regions of the Arctic into a single Turboveg v3 database. We present the pros and cons of using the Br.-Bl. clas- sification approach compared to the EcoVeg (US) and Biogeoclimatic Ecological Classification (Canada) ap- proaches. -
Arctic Climate Feedbacks: Global Implications
for a living planet ARCTIC CLIMATE FEEDBACKS: GLOBAL IMPLICATIONS ARCTIC CLIMATE FEEDBACKS: GLOBAL IMPLICATIONS Martin Sommerkorn & Susan Joy Hassol, editors With contributions from: Mark C. Serreze & Julienne Stroeve Cecilie Mauritzen Anny Cazenave & Eric Rignot Nicholas R. Bates Josep G. Canadell & Michael R. Raupach Natalia Shakhova & Igor Semiletov CONTENTS Executive Summary 5 Overview 6 Arctic Climate Change 8 Key Findings of this Assessment 11 1. Atmospheric Circulation Feedbacks 17 2. Ocean Circulation Feedbacks 28 3. Ice Sheets and Sea-level Rise Feedbacks 39 4. Marine Carbon Cycle Feedbacks 54 5. Land Carbon Cycle Feedbacks 69 6. Methane Hydrate Feedbacks 81 Author Team 93 EXECUTIVE SUMMARY VER THE PAST FEW DECADES, the Arctic has warmed at about twice the rate of the rest of the globe. Human-induced climate change has Oaffected the Arctic earlier than expected. As a result, climate change is already destabilising important arctic systems including sea ice, the Greenland Ice Sheet, mountain glaciers, and aspects of the arctic carbon cycle including altering patterns of frozen soils and vegetation and increasing “Human-induced methane release from soils, lakes, and climate change has wetlands. The impact of these changes on the affected the Arctic Arctic’s physical systems, earlier than expected.” “There is emerging evidence biological and growing concern that systems, and human inhabitants is large and projected to grow arctic climate feedbacks throughout this century and beyond. affecting the global climate In addition to the regional consequences of arctic system are beginning climate change are its global impacts. Acting as the to accelerate warming Northern Hemisphere’s refrigerator, a frozen Arctic plays a central role in regulating Earth’s climate signifi cantly beyond system. -
Letter from the President
Issue 49 - Spring / Summer 2018 Photo credits: NARFU Letter from the President Secretariat’s Corner Dear IASSA Members! Letter from the President . ……….. .1 This June marked a year since ICASS IX took place in Umea, Swe- Council’s letter . .2 den. ICASS IX was an existing event that brought together 800 IASSA Priorities Progress. .. .3 scholars and community members. We are in the process of devel- IASSA in the Arctic Council. .5 oping plans for ICASS X in Arkhangelsk, Russia that will take place in June of 2020. We are in the very beginning of this journey, and Features the co-conveners and the Council are very much looking for you in- IASC Medal: Oran Young …….. .8 put, suggestions and recommendations in respect to general organi- Arctic Horizons……….. 10 zation, themes, side events or other ideas. Please share them with National Inuit Strategy on me at your convenience. Research…..….……………………….11 Arctic Science Agreement . 12 IASSA is continuing to advance its priorities (see next page). At ICASS IX we proposed the new IASSA platform From Growth to Workshop Invitation . …... 15 Prominence that includes nine priorities, which will be instru- mental in bringing the IASSA to the next level of success. In Coun- Upcoming Conferences. ... 16 cil’s effort to move from ideas to action we established internal task forces that will be charged with developing implementation recom- Recent Conferences & Work- mendations, suggestions and plans. The Council will also be solicit- shops………………………………… .17 ing and analyzing the input from IASSA membership. We will strive to finalize plans and mechanisms for each approved priority in 2019. -
The Alaska Vegetation Classification
The Alaska Vegetation Forest Service Pacific Northwest Research Station General Technical Classification Report PNW-GTR-286 July 1992 L.A. Viereck, CT. Dyrness, A.R. Batten, and K.J. Wenzlick Authors L.A. VIERECK is a principal plant ecologist, C.T. DYRNESS was a research soil scientist (now retired), and K.J. WENZLICK was a secretary (currently is an editorial assistant, Research information Services, Portland, Oregon 97208), ‘Institute of Northern Forestry, 308 Tanana Drive, Fairbanks, Alaska 99775-5500; and A.R. BATTEN is research associate at University of Alaska Museum, Fairbanks, Alaska 99775-l200. Abstract Viereck, L.A.; Dyrness, C.T.; Batten, A.R.; Wenzlick, K.J. 1992. The Alaska vegetation classification. Gen. Tech. Rep. PNW-GTR-286. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 278 p. The Alaska vegetation classification presented here is a comprehensive, statewide system that has been under development since 1976. The classification is based, as much as possible, on the characteristics of the vegetation itself and is designed to categorize existing vegetation, not potential vegetation. A hierarchical system with five levels of resolution is used for classifying Alaska vegetation. The system, an agglomerative one, starts with 888 known Alaska plant communities, which are listed and referenced. At the broadest level of resolution, the system contains three formations-forest, scrub, and herbaceous vegetation. In addition to the classification, this report contains a key to levels I, II, and III; complete descriptions of all level IV units; and a glossary of terms used. Keywords: Vegetation, classification, Alaska, tundra, boreal forest, coastal forest, plant communities. -
Cultural Heritage Resources Report & Inventory
Phase I: NTI IIBA for Cultural Heritage Resources Conservation Areas Report and Inventory Appedices Cultural Heritage Area: Queen Maud Gulf and Interpretative Migratory Bird Sanctuary Materials Study Prepared for Nunavut Tunngavik Inc. 1 May 2011 This report is part of a set of studies and a database produced for Nunavut Tunngavik Inc. as part of the project: NTI IIBA for Conservation Areas, Cultural Resources Inventory and Interpretative Materials Study Inquiries concerning this project and the report should be addressed to: David Kunuk Director of Implementation Nunavut Tunngavik Inc. 3rd Floor, Igluvut Bldg. P.O. Box 638 Iqaluit, Nunavut X0A 0H0 E: [email protected] T: (867) 975‐4900 Project Manager, Consulting Team: Julie Harris Contentworks Inc. 137 Second Avenue, Suite 1 Ottawa, ON K1S 2H4 Tel: (613) 730‐4059 Email: [email protected] Report Authors: Philip Goldring, Consultant: Historian and Heritage/Place Names Specialist (primary author) Julie Harris, Contentworks Inc.: Heritage Specialist and Historian Nicole Brandon, Consultant: Archaeologist Note on Place Names: The current official names of places are used here except in direct quotations from historical documents. Throughout the document Umingmaktok, for example, refers to the settlement previously known as Bay Chimo. Names of places that do not have official names will appear as they are found in the source documents. Contents Section 1: Introduction ................................................................................................................... -
Vegetation Type Dominates the Spatial Variability in CH4 Emissions Across Multiple Arctic Tundra Landscapes
Ecosystems (2016) 19: 1116–1132 DOI: 10.1007/s10021-016-9991-0 Ó 2016 The Author(s). This article is published with open access at Springerlink.com Vegetation Type Dominates the Spatial Variability in CH4 Emissions Across Multiple Arctic Tundra Landscapes Scott J. Davidson,1,2* Victoria L. Sloan,2 Gareth K. Phoenix,1 Robert Wagner,2 James P. Fisher,1 Walter C. Oechel,2,3 and Donatella Zona1,2 1Department of Animal and Plant Sciences, University of Sheffield, Western Bank, Sheffield, South Yorkshire S10 2TN, UK; 2Global Change Research Group and Department of Biology, San Diego State University, San Diego, California 92182, USA; 3Department of Environment, Earth and Ecosystems, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK ABSTRACT Methane (CH4) emissions from Arctic tundra are to identify drivers of CH4 flux, and to examine an important feedback to global climate. Cur- relationships between gross primary productivity rently, modelling and predicting CH4 fluxes at (GPP), dissolved organic carbon (DOC) and CH4 broader scales are limited by the challenge of fluxes. We found that a highly simplified vegeta- upscaling plot-scale measurements in spatially tion classification consisting of just three vegeta- heterogeneous landscapes, and by uncertainties tion types (wet sedge, tussock sedge and other) regarding key controls of CH4 emissions. In this explained 54% of the variation in CH4 fluxes study, CH4 and CO2 fluxes were measured to- across the entire transect, performing almost as gether with a range of environmental variables well as a more complex model including water and detailed vegetation analysis at four sites table, sedge height and soil moisture (explaining spanning 300 km latitude from Barrow to Ivotuk 58% of the variation in CH4 fluxes). -
Southern Arctic
ECOLOGICAL REGIONS OF THE NORTHWEST TERRITORIES Southern Arctic Ecosystem Classification Group Department of Environment and Natural Resources Government of the Northwest Territories 2012 ECOLOGICAL REGIONS OF THE NORTHWEST TERRITORIES SOUTHERN ARCTIC This report may be cited as: Ecosystem Classification Group. 2012. Ecological Regions of the Northwest Territories – Southern Arctic. Department of Environment and Natural Resources, Government of the Northwest Territories, Yellowknife, NT, Canada. x + 170 pp. + insert map. Library and Archives Canada Cataloguing in Publication Northwest Territories. Ecosystem Classification Group Ecological regions of the Northwest Territories, southern Arctic / Ecosystem Classification Group. ISBN 978-0-7708-0199-1 1. Ecological regions--Northwest Territories. 2. Biotic communities--Arctic regions. 3. Tundra ecology--Northwest Territories. 4. Taiga ecology--Northwest Territories. I. Northwest Territories. Dept. of Environment and Natural Resources II. Title. QH106.2 N55 N67 2012 577.3'7097193 C2012-980098-8 Web Site: http://www.enr.gov.nt.ca For more information contact: Department of Environment and Natural Resources P.O. Box 1320 Yellowknife, NT X1A 2L9 Phone: (867) 920-8064 Fax: (867) 873-0293 About the cover: The small digital images in the inset boxes are enlarged with captions on pages 28 (Tundra Plains Low Arctic (north) Ecoregion) and 82 (Tundra Shield Low Arctic (south) Ecoregion). Aerial images: Dave Downing. Main cover image, ground images and plant images: Bob Decker, Government of the Northwest Territories. Document images: Except where otherwise credited, aerial images in the document were taken by Dave Downing and ground-level images were taken by Bob Decker, Government of the Northwest Territories. Members of the Ecosystem Classification Group Dave Downing Ecologist, Onoway, Alberta. -
Rapid Ecosystem Change at the Southern Limit of the Canadian Arctic, Torngat Mountains National Park
remote sensing Article Rapid Ecosystem Change at the Southern Limit of the Canadian Arctic, Torngat Mountains National Park Emma L. Davis 1,*, Andrew J. Trant 1, Robert G. Way 2, Luise Hermanutz 3 and Darroch Whitaker 4 1 School of Environment, Resources and Sustainability, University of Waterloo, 200 University Avenue West, Waterloo, ON N2L 3G1, Canada; [email protected] 2 Northern Environmental Geoscience Laboratory, Department of Geography and Planning, Queen’s University, Kingston, ON K7L 3N6, Canada; [email protected] 3 Department of Biology, Memorial University, St. John’s, NL A1B 3X9, Canada; [email protected] 4 Western Newfoundland and Labrador Field Unit, Parks Canada, Rocky Harbour, NL A0K 4N0, Canada; [email protected] * Correspondence: [email protected] or [email protected] Abstract: Northern protected areas guard against habitat and species loss but are themselves highly vulnerable to environmental change due to their fixed spatial boundaries. In the low Arctic, Torngat Mountains National Park (TMNP) of Canada, widespread greening has recently occurred alongside warming temperatures and regional declines in caribou. Little is known, however, about how biophysical controls mediate plant responses to climate warming, and available observational data are limited in temporal and spatial scope. In this study, we investigated the drivers of land cover change for the 9700 km2 extent of the park using satellite remote sensing and geostatistical modelling. Random forest classification was used to hindcast and simulate land cover change for four different land cover types from 1985 to 2019 with topographic and surface reflectance imagery (Landsat Citation: Davis, E.L.; Trant, A.J.; Way, archive).