Ashley Dubnick

Total Page:16

File Type:pdf, Size:1020Kb

Ashley Dubnick Hydrological Controls on the Biogeochemistry of Polar Glacier Ice and its Meltwater by Ashley Dubnick A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Earth and Atmospheric Sciences University of Alberta © Ashley Dubnick, 2018 Abstract Ice masses in the Antarctic, Greenland, and Canadian Arctic cover approximately 10% of the Earth’s surface, contain approximately 70% of the Earth’s freshwater, and are the top contributors to eustatic sea level rise. In recent years, these polar glacier systems have experienced significant increases in mass loss and melt rates, and the quantity of melt in these regions is expected to increase further under a warming climate. Existing research indicates that the physical, chemical, and microbial characteristics of these ice masses and the meltwater they produce are often distinct from those of other natural water sources. Their characteristics also show high temporal and spatial variability that may result from the combined presence of distinct and variable biogeochemical environments, particularly on the glacier surface and near the bed, and the strong variations in hydrological dynamics that often occur in glacial systems. This study examines glacier ice and meltwater from the Antarctic, Greenland, and Canadian Arctic to (1) investigate the variability in microbial assemblages and nutrient species/concentrations in the various biogeochemical environments that exist within and between polar glacier systems, and (2) evaluate how glacier hydrology influences the development and export of microbes and nutrients from these systems. Results of this study indicate that distinct biogeochemical environments exist in glacial systems, that they can function as sources and/or sinks for specific nutrients and microbes, and that the nutrients and microbes exported in glacial meltwater can vary according to the meltwater sources, flow paths, and residence times within the glacial system. Consequently, the biogeochemical characteristics of glacier ice and meltwater can differ between glaciers with different features, thermal regimes and/or hydrological systems, can change over the course of the melt season as the hydrological system within a glacier evolves, and can show different seasonal patterns for specific microbiological and nutrient parameters. ii Preface A version of Chapter 2 has been published [Dubnick et al., 2017b]. I was responsible for field measurements and sample collection, data analysis and manuscript composition. J. Wadham and J. Orwin collaborated on the study design and field work and all authors (J. Wadham, M. Tranter, M. Sharp, J. Orwin, J. Barker, E. Bagshaw and S. Fitzsimons) contributed to manuscript edits. A version of Chapter 3 has also been published [Dubnick et al., 2017a]. I was responsible for study design, data collection and analyses and manuscript composition. J. Hawkings and A. Beaton collaborated on the study design, hydrology/chemistry fieldwork, and chemical analyses and S. Kazemi completed DNA extractions and contributed to microbial data analyses. S. Kazemi, M. Sharp, J. Wadham, J. Hawkings, A. Beaton, and B. Lanoil contributed to manuscript edits. Hydrology and chemistry field data were also published elsewhere [Hawkings et al., 2016]. Chapter 4 is unpublished work. I completed the study design, field work, sample processing, data analyses and manuscript composition. B. Danielson assisted with field work and sampling and A. Saidi-Mehrabad completed DNA extractions. M. Sharp, M. Bhatia and J. Barker contributed to manuscript edits. iii Table of Contents Abstract .............................................................................................................................. ii Preface ............................................................................................................................... iii Table of Contents ............................................................................................................. iv List of Tables .................................................................................................................. viii List of Figures ................................................................................................................... ix Chapter 1: Introduction ....................................................................................................1 1.1 Motivation ........................................................................................................... 1 1.2 Objectives and thesis outline .............................................................................. 3 1.3 Scientific background ......................................................................................... 4 Chapter 2: Trickle or treat: the dynamics of nutrient export from polar glaciers ....12 2.1 Abstract ............................................................................................................. 12 2.2 Introduction ....................................................................................................... 13 2.3 Methods............................................................................................................. 16 2.3.1 Study site ....................................................................................................... 16 2.3.2 Data collection .............................................................................................. 17 2.3.2.1 Discharge monitoring ............................................................................. 17 2.3.2.2 Meteorological monitoring ..................................................................... 18 2.3.2.3 Sampling................................................................................................. 18 2.3.3 Laboratory analyses ...................................................................................... 19 2.3.4 Data processing and statistical analyses ....................................................... 20 2.4 Results ............................................................................................................... 21 2.4.1 Hydrology and major ions ............................................................................ 21 iv 2.4.2 Dissolved inorganic nitrogen ........................................................................ 22 2.4.3 Dissolved inorganic phosphorus ................................................................... 23 2.4.4 Dissolved organic matter .............................................................................. 24 2.5 Discussion ......................................................................................................... 26 2.5.1 Nutrient sources and sinks along the flow path ............................................ 26 2.5.1.1 Supraglacial environments ..................................................................... 26 2.5.1.2 Ice-marginal environments ..................................................................... 27 2.5.1.3 Proglacial environments ......................................................................... 30 2.5.2 Trickle or Treat: hydrologically controlled nutrient dynamics ..................... 30 2.6 Conclusions ....................................................................................................... 35 2.7 Acknowledgements ........................................................................................... 36 Chapter 3: Hydrological controls on glacially exported microbial assemblages .......45 3.1 Abstract ............................................................................................................. 45 3.2 Introduction ....................................................................................................... 46 3.3 Methods............................................................................................................. 49 3.3.1 Field site ........................................................................................................ 49 3.3.2 Sample collection and processing ................................................................. 49 3.3.3 Chemical indices ........................................................................................... 51 3.3.4 Analytical procedures ................................................................................... 53 3.3.5 DNA sequence processing and statistical analyses ....................................... 55 3.4 Results ............................................................................................................... 57 3.4.1 Hydrology/hydrochemistry ........................................................................... 57 3.4.2 Microbiology................................................................................................. 58 v 3.5 Discussion ......................................................................................................... 60 3.5.1 Hydrological regime ..................................................................................... 60 3.5.2 First-order control on exported microbial assemblages: subglacial drainage 62 3.5.3 Second-order control on exported microbial assemblages: source water and subglacial residence time .............................................................................. 63 3.6 Conclusions ....................................................................................................... 64 3.7 Acknowledgements ..........................................................................................
Recommended publications
  • Pleistocene Geology of Eastern South Dakota
    Pleistocene Geology of Eastern South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 262 Pleistocene Geology of Eastern South Dakota By RICHARD FOSTER FLINT GEOLOGICAL SURVEY PROFESSIONAL PAPER 262 Prepared as part of the program of the Department of the Interior *Jfor the development-L of*J the Missouri River basin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1955 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $3 (paper cover) CONTENTS Page Page Abstract_ _ _____-_-_________________--_--____---__ 1 Pre- Wisconsin nonglacial deposits, ______________ 41 Scope and purpose of study._________________________ 2 Stratigraphic sequence in Nebraska and Iowa_ 42 Field work and acknowledgments._______-_____-_----_ 3 Stream deposits. _____________________ 42 Earlier studies____________________________________ 4 Loess sheets _ _ ______________________ 43 Geography.________________________________________ 5 Weathering profiles. __________________ 44 Topography and drainage______________________ 5 Stream deposits in South Dakota ___________ 45 Minnesota River-Red River lowland. _________ 5 Sand and gravel- _____________________ 45 Coteau des Prairies.________________________ 6 Distribution and thickness. ________ 45 Surface expression._____________________ 6 Physical character. _______________ 45 General geology._______________________ 7 Description by localities ___________ 46 Subdivisions. ________-___--_-_-_-______ 9 Conditions of deposition ___________ 50 James River lowland.__________-__-___-_--__ 9 Age and correlation_______________ 51 General features._________-____--_-__-__ 9 Clayey silt. __________________________ 52 Lake Dakota plain____________________ 10 Loveland loess in South Dakota. ___________ 52 James River highlands...-------.-.---.- 11 Weathering profiles and buried soils. ________ 53 Coteau du Missouri..___________--_-_-__-___ 12 Synthesis of pre- Wisconsin stratigraphy.
    [Show full text]
  • Navigating Troubled Waters a History of Commercial Fishing in Glacier Bay, Alaska
    National Park Service U.S. Department of the Interior Glacier Bay National Park and Preserve Navigating Troubled Waters A History of Commercial Fishing in Glacier Bay, Alaska Author: James Mackovjak National Park Service U.S. Department of the Interior Glacier Bay National Park and Preserve “If people want both to preserve the sea and extract the full benefit from it, they must now moderate their demands and structure them. They must put aside ideas of the sea’s immensity and power, and instead take stewardship of the ocean, with all the privileges and responsibilities that implies.” —The Economist, 1998 Navigating Troubled Waters: Part 1: A History of Commercial Fishing in Glacier Bay, Alaska Part 2: Hoonah’s “Million Dollar Fleet” U.S. Department of the Interior National Park Service Glacier Bay National Park and Preserve Gustavus, Alaska Author: James Mackovjak 2010 Front cover: Duke Rothwell’s Dungeness crab vessel Adeline in Bartlett Cove, ca. 1970 (courtesy Charles V. Yanda) Back cover: Detail, Bartlett Cove waters, ca. 1970 (courtesy Charles V. Yanda) Dedication This book is dedicated to Bob Howe, who was superintendent of Glacier Bay National Monument from 1966 until 1975 and a great friend of the author. Bob’s enthusiasm for Glacier Bay and Alaska were an inspiration to all who had the good fortune to know him. Part 1: A History of Commercial Fishing in Glacier Bay, Alaska Table of Contents List of Tables vi Preface vii Foreword ix Author’s Note xi Stylistic Notes and Other Details xii Chapter 1: Early Fishing and Fish Processing in Glacier Bay 1 Physical Setting 1 Native Fishing 1 The Coming of Industrial Fishing: Sockeye Salmon Attract Salters and Cannerymen to Glacier Bay 4 Unnamed Saltery at Bartlett Cove 4 Bartlett Bay Packing Co.
    [Show full text]
  • Glacial Geomorphological Mapping a Review of Approaches And
    Earth-Science Reviews 185 (2018) 806–846 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Glacial geomorphological mapping: A review of approaches and frameworks for best practice T ⁎ Benjamin M.P. Chandlera, , Harold Lovellb, Clare M. Bostonb, Sven Lukasc, Iestyn D. Barrd, Ívar Örn Benediktssone, Douglas I. Bennf, Chris D. Clarkg, Christopher M. Darvillh, David J.A. Evansi, Marek W. Ewertowskij, David Loiblk, Martin Margoldl, Jan-Christoph Ottom, David H. Robertsi, Chris R. Stokesi, Robert D. Storrarn, Arjen P. Stroeveno,p a School of Geography, Queen Mary University of London, Mile End Road, London E1 4NS, UK b Department of Geography, University of Portsmouth, Portsmouth, UK c Department of Geology, Lund University, Lund, Sweden d School of Science and the Environment, Manchester Metropolitan University, Manchester, UK e Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland f Department of Geography and Sustainable Development, University of St Andrews, St Andrews, UK g Department of Geography, University of Sheffield, Sheffield, UK h Geography, School of Environment, Education and Development, University of Manchester, Manchester, UK i Department of Geography, Durham University, Durham, UK j Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Poznań, Poland k Department of Geography, Humboldt University of Berlin, Berlin, Germany l Department of Physical Geography and Geoecology, Charles University, Prague, Czech Republic m Department
    [Show full text]
  • The Mcmurdo Dry Valleys: a Landscape on the Threshold of Change
    Geomorphology 225 (2014) 25–35 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph The McMurdo Dry Valleys: A landscape on the threshold of change Andrew G. Fountain a,⁎, Joseph S. Levy b, Michael N. Gooseff c,DavidVanHornd a Department of Geology, Portland State University, Portland, OR 97201, USA b Institute for Geophysics, University of Texas, Austin, TX 78758, USA c Dept. of Civil & Environmental Engineering, Pennsylvania State University, University Park, PA 16802, USA d Department of Biology, University of New Mexico, Albuquerque, NM 87131, USA article info abstract Article history: Field observations of coastal and lowland regions in the McMurdo Dry Valleys suggest they are on the threshold Received 26 March 2013 of rapid topographic change, in contrast to the high elevation upland landscape that represents some of the low- Received in revised form 19 March 2014 est rates of surface change on Earth. A number of landscapes have undergone dramatic and unprecedented land- Accepted 27 March 2014 scape changes over the past decade including, the Wright Lower Glacier (Wright Valley) — ablated several tens of Available online 18 April 2014 meters, the Garwood River (Garwood Valley) has incised N3 m into massive ice permafrost, smaller streams in Taylor Valley (Crescent, Lawson, and Lost Seal Streams) have experienced extensive down-cutting and/or bank Keywords: N Permafrost undercutting, and Canada Glacier (Taylor Valley) has formed sheer, 4 meter deep canyons. The commonality Glaciers between all these landscape changes appears to be sediment on ice acting as a catalyst for melting, including Climate change ice-cement permafrost thaw.
    [Show full text]
  • Glacier and Permafrost Effects As Related to Climate Change
    Chapter 9 Natural Hazards in Forests: Glacier and Permafrost Effects as Related to Climate Change Wilfried Haeberli1 and C.R. Burn2 1Department of Geography, University of Zurich, Switzerland 2Department of Geography and Environmental Studies, Carleton University, Ottawa, Canada Atmospheric warming is predicted to be greater in polar regions than at lower latitudes and more pronounced at high altitudes than in lowlands. In polar regions, air and ground warming may lead to a more northerly exten- sion of the boreal forest, as growing seasons lengthen and become warmer. Near-surface permafrost degradation will probably accompany such an evolution in environmental conditions. In some cases slope movement may be catastrophic, but in most instances the settlement is expected to be slow, and the water released by melting ground ice will evaporate. Subpolar forests in permafrost regions are primarily used for firewood and rough lumber, but not construction-grade materials. This is unlikely to change because long- term ground instability, relatively cold soil temperatures, depletion of nutrients in the active layer, and restriction of root systems to the active layer all limit tree growth. Extensive forest fires, usually initiated by lightning after a week or two of hot weather, also deplete timber stocks. There have been suggestions that wildfire may increase following climate warming. Meltwater runoff from glaciated and perennially frozen areas represents only a small portion of the annual water supply, but strongly influences stream flow in lowlands during the warm/dry season. The disappearance of perennial ice above and below the earth surface influences the seasonality of discharge by reducing meltwater production in the warm season and by increasing the permeability of frozen/thawing materials.
    [Show full text]
  • Last Glacial Ice Sheet Dynamics Offshore NE Greenland – a Case Study from Store Koldewey Trough
    Last Glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough Ingrid L. Olsen1, Tom Arne Rydningen1, Matthias Forwick1, Jan Sverre Laberg1, Katrine Husum2 1Department of Geosciences, UiT The Arctic University of Norway, Box 6050 Langnes, NO-9037 Tromsø, Norway 2Norwegian Polar Institute, Box 6606 Langnes, NO-9296 Tromsø, Norway Correspondence to: Ingrid L. Olsen ([email protected]) Abstract The presence of a grounded Greenland Ice Sheet on the northeastern part of the Greenland continental shelf during the Last Glacial Maximum is supported by new swath bathymetry and high-resolution seismic data, supplemented with multi-proxy analyses of sediment gravity cores from Store Koldewey Trough. Subglacial till fills the trough, 5 with an overlying drape of maximum 2.5 m thick glacier-proximal and glacier-distal sediment. The presence of mega-scale glacial lineations and a grounding zone wedge in the outer part of the trough, comprising subglacial till, provides evidence of the expansion of fast-flowing, grounded ice, probably originating from the area presently covered with the Storstrømmen ice stream and thereby previously flowing across Store Koldewey Island and Germania Land. Grounding zone wedges and recessional moraines provide evidence that multiple halts and/or 10 readvances interrupted the deglaciation. The formation of the grounding zone wedges is estimated to be at least 130 years, whilst distances between the recessional moraines indicate that the grounding line locally retreated between 80 to 400 meters/year during the deglaciation, assuming that the moraines formed annually. The complex geomorphology in Store Koldewey Trough is attributed to the trough shallowing and narrowing towards the coast.
    [Show full text]
  • Institute of Arctic and Alpine Research
    Institute of Arctic and Alpine Research 2001–2002 Biennial Report Institute of Arctic and Alpine Research University of Colorado 450 UCB Boulder, Colorado 80309-0450 Tel 303/492-6287 Fax 303/492-6388 www.instaar.colorado.edu RL-1 1560 30th Street Boulder, CO 80303 Mountain Research Station 818 County Road 116 Nederland, Colorado 80466 Tel 303/492-8842 Fax 303/492-8841 (Director: William B. Bowman) www.colorado.edu/mrs/ INSTAAR Council Carol B. Lynch, Vice Chancellor for Research and Dean of the Graduate School Todd Gleason, Dean, College of Arts and Sciences Robert Davis, Dean, College of Engineering Charles Stern, Chair/Professor, Department of Geological Sciences Kenneth Foote, Chair/Professor, Department of Geography Russell Monson, Chair/Professor, Environmental, Population and Organismic Biology Hon-Yim Ko, Chair/Professor, Department of Civil, Environmental, and Architectural Engineering James P. Syvitski, Director/Professor, INSTAAR/Department of Geological Sciences INSTAAR Scientific Advisory Committee Richard Alley, Professor, Department of Geosciences, Pennsylvania State University William Fitzhugh, Department of Anthropology, National Museum of Natural History, Smithsonian Institution Hugh French, Professor, Departments of Geography and Earth Sciences, University of Ottawa Peter Groffman, Institute of Ecosystem Studies, Millbrook, NY Steve Hargreaves, CEO, ERIC Companies, Englewood, CO Robert Howarth, Program in Biogeochemistry and Environmental Change, Cornell University Tim Killeen, Director, National Center for Atmospheric
    [Show full text]
  • Surface Energy Balance and Melt Thresholds Over 11 Years at Taylor Glacier, Antarctica Matthew J
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, F04014, doi:10.1029/2008JF001029, 2008 Click Here for Full Article Surface energy balance and melt thresholds over 11 years at Taylor Glacier, Antarctica Matthew J. Hoffman,1 Andrew G. Fountain,2 and Glen E. Liston3 Received 7 April 2008; revised 14 August 2008; accepted 3 October 2008; published 17 December 2008. [1] In the McMurdo Dry Valleys, Victoria Land, Antarctica, melting of glacial ice is the primary source of water to streams, lakes, and associated ecosystems. To understand geochemical fluxes and ecological responses to past and future climates requires a physically based energy balance model. We applied a one-dimensional model to one site on Taylor Glacier using 11 years of daily meteorological data and seasonal ablation measurements. Inclusion of transmission of solar radiation into the ice was necessary to accurately model summer ablation and ice temperatures. Results showed good correspondence between calculated and measured ablation and ice temperatures over the 11 years. Ablation (18 cm aÀ1) was dominated by sublimation with very few occurrences of melt (42 days during 11 years). Results also indicated that above freezing air temperatures did not necessarily result in melt and, in turn, melt occurred during subfreezing air temperatures under some conditions. For air temperatures near freezing, low wind speed was critically important for melt initiation. According to the model, subsurface melt, away from rocks and sediment in the ice, occurred three times more frequently than surface melt; occurs no deeper than 50 cm below the glacier surface; and was small, never exceeding 8% by mass. The magnitude of subsurface melting and the energy balance indicate that Taylor Glacier ice is intermediate in optical properties between snow and blue ice.
    [Show full text]
  • Ecology of Aquatic Insects in Monsoonal Temperate Glacier Streams of Southeast Tibet: A
    Ecology of aquatic insects in monsoonal temperate glacier streams of Southeast Tibet: A departure from the conceptual model DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Heather L. Fair, B.S., M.B.A., M.S. Graduate Program in Environmental Science The Ohio State University 2017 Dissertation Committee: Professor Roman P. Lanno, Advisor Professor Richard H. Moore Emeritus Professor David L. Denlinger Emeritus Professor Donald Dean Copyrighted by Heather L. Fair-Wu 2017 Abstract The cryosphere is shrinking as a result of climate change. Mountain glaciers, a key component of the cryosphere, serve as headwaters to glacier meltwater streams which support communities of stenothermic organisms. The Tibetan plateau is known as “the Third Pole” for its high number of glaciers, yet very few scientific papers have been published on aquatic invertebrate ecology of glacier-fed streams in the region. On the edges of the Tibetan Plateau in Southeast Tibet’s Hengduan mountains, monsoonal temperate glaciers extend well below the treeline as valley glaciers, and are perhaps the most endangered cryosphere-dominated streams in the world due to their low latitudes and altitudes, which makes them sensitive to atmospheric temperature changes. The glaciated headwaters of the Mekong and Yangtze Rivers comprise a small fraction of the annual river discharge, yet at a local scale provide glacial meltwater that supports endemic and potentially rare species. Water temperature and channel stability differ between seasons due to the torrential flow from glacial meltwater during the summer melt season.
    [Show full text]
  • Nitrogen and Sulphur Biogeochemistry in a High Arctic Glacial Watershed: an Investigation with Isotopic Tracers and Solute Chemistry
    Nitrogen and Sulphur biogeochemistry in a High Arctic glacial watershed: an investigation with isotopic tracers and solute chemistry Arif Husain Ansari Department of Geography The University of Sheffield June 2012 Thesis submitted for the degree of Doctor of Philosophy Table of Contents Nitrogen and Sulphur biogeochemistry in a High Arctic glacial watershed: an investigation with isotopic tracers and solute chemistry ................................................................................... i Acknowledgements ....................................................................................................................................... 2 CHAPATER 1: INTRODUCTION .............................................................................................................. 3 1.1 Significance of this study ...................................................................................................... 3 1.2 Aim of the study .................................................................................................................... 4 1.3 Thesis outline ........................................................................................................................ 6 CHAPTER 2: NITROGEN AND SULPHUR BIOGEOCHEMICAL CYCLING IN HIGH ARCTIC: A REVIEW ....................................................................................................................................................... 7 2.1 Nitrogen Biogeochemistry ...................................................................................................
    [Show full text]
  • An Inventory-Driven Rock Glacier Status Model (Intact Vs
    Geomorphology 350 (2020) 106887 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph An inventory-driven rock glacier status model (intact vs. relict) for South Tyrol, Eastern Italian Alps a,b a c a b Christian Kofler , Stefan Steger , Volkmar Mair , Marc Zebisch , Francesco Comiti , a,d Stefan Schneiderbauer a Institute for Earth Observation, Eurac Research, 39100 Bozen/Bolzano, Italy b Faculty of Science and Technology, Free University of Bozen-Bolzano, 39100 Bozen/Bolzano, Italy c Office for Geology and Building Materials Testing, 39053 Kardaun/Cardano, Italy d UNU-EHS, GLOMOS Programme, 39100 Bozen/Bolzano, Italy a r t i c l e i n f o a b s t r a c t Article history: Ice presence in rock glaciers is a topic that is likely to gain importance in the future due to the expected Received 4 April 2019 decrease in water supply from glaciers and the increase of mass movements originating in periglacial Received in revised form 16 August 2019 areas. This makes it important to have at ones disposal inventories with complete information on the state Accepted 24 September 2019 of rock glaciers. This study presents a method to overcome incomplete information on the status of rock Available online 28 October 2019 glaciers (i.e. intact vs. relict) recorded in regional scale inventories. The proposed data-driven modelling framework can be used to estimate the likelihood that rock glaciers contain frozen material. Potential Keywords: predictor variables related to topography, environmental controls or the rock glacier appearance were Machine learning derived from a digital terrain model (DTM), satellite data and gathered from existing data sets.
    [Show full text]
  • Glacial Geomorphological Mapping
    1 Glacial geomorphological mapping: 2 a review of approaches and frameworks for best practice 3 4 Benjamin M.P. Chandler1 *, Harold Lovell2, Clare M. Boston2, Sven Lukas3, Iestyn D. Barr4, 5 Ívar Örn Benediktsson5, Douglas I. Benn6, Chris D. Clark7, Christopher M. Darvill8, 6 David J.A. Evans9, Marek W. Ewertowski10, David Loibl11, Martin Margold12, Jan-Christoph Otto13, 7 David H. Roberts9, Chris R. Stokes9, Robert D. Storrar14, Arjen P. Stroeven15, 16 8 9 1 School of Geography, Queen Mary University of London, Mile End Road, London, E1 4NS, UK 10 2 Department of Geography, University of Portsmouth, Portsmouth, UK 11 3 Department of Geology, Lund University, Lund, Sweden 12 4 School of Science and the Environment, Manchester Metropolitan University, Manchester, UK 13 5 Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland 14 6 Department of Geography and Sustainable Development, University of St Andrews, St Andrews, UK 15 7 Department of Geography, University of Sheffield, Sheffield, UK 16 8 Geography, School of Environment, Education and Development, University of Manchester, Manchester, UK 17 9 Department of Geography, Durham University, Durham, UK 18 10 Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Poznań, Poland 19 11 Department of Geography, Humboldt University of Berlin, Berlin, Germany 20 12 Department of Physical Geography and Geoecology, Charles University, Prague, Czech Republic 21 13 Department of Geography and Geology, University of Salzburg, Salzburg, Austria 22 14 Department of the Natural and Built Environment, Sheffield Hallam University, Sheffield, UK 23 15 Geomorphology & Glaciology, Department of Physical Geography, Stockholm University, Stockholm, Sweden 24 16 Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden 25 26 *Corresponding author.
    [Show full text]