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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing :
    Keywords: Geomorphology. ; Geology. ; Physical geography. ; Geography. ; Environment. ; Geomorphology. ; Geology. ; Earth System Sciences. ; Regional Geography. ; Environmental Sciences.
    Description / Table of Contents: Geomorphological landscapes of Eastern Canada: general overview -- Case studies, with at least one outstanding example from each of the major physiographic regions -- Geomorphological landscapes as heritage.
    Abstract: This is the only book to focus on the geomorphological landscapes of eastern Canada and provides a companion volume to “Landscapes and Landforms of Western Canada” (2017). There are a number of unique characteristics of eastern Canada’s landscapes, notably its magnificent coastlines, the extraordinary variety and extent of wetlands, the huge Great Lakes-St. Lawrence basin, the high incidence of meteorite craters , the spectacular Niagara Falls, urban karst in Montreal and Ottawa, youthful, glaciated karst in Ontario, Newfoundland, Quebec and Nova Scotia, the ubiquitous permafrost terrain of Nunavut, Labrador and northern Quebec and the magnificent arctic fjords and glaciers. Looking at coastlines, the tidal extremes of the Bay of Fundy are world renowned; the structural complexity of the island of Newfoundland is less well known, but produces an astounding variety of coastlines in close succession; the arctic fjordlands of Baffin and Ellesmere islands and the extravagant raised beaches of Hudson Bay bear comparison with the classic fjords of Norway and the Baltic Sea raised beaches. As for wetlands there are distinctive Arctic, Subarctic, Boreal, Eastern Temperate and Atlantic wetlands and their extent is second only to those of Russia. In the Hudson and James bay regions between 75-100% of the terrestrial surface is comprised of wetlands. One of North America’s largest river basins, the Great Lakes-St. Lawrence basin, has its source in Minnesota, straddles the USA-Canada border and debouches into Quebec as the St. Lawrence River and evolves through its estuary into the Gulf of St. Lawrence, a journey of almost 5,000 km. As far as meteorite craters are concerned, 10% of the world’s total are located in eastern Canada, including some of the largest and most complex. They are preserved preferentially in the ancient Shield terrain of Quebec. Finally, the three million km² of permafrost controlled relief in eastern Canada serves as a reminder of the vulnerability of eastern Canada’s landscapes to climate change. Effects of warming are expressed through thawing of the permafrost, disruption of transportation corridors and urban construction problems, ever-present geomorphic hazards.
    Type of Medium: Online Resource
    Pages: XVI, 596 p. 411 illus., 387 illus. in color. , online resource.
    Edition: 1st ed. 2020.
    ISBN: 9783030351373
    Series Statement: World Geomorphological Landscapes,
    DDC: 551.41
    Language: English
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  • 2
    Monograph available for loan
    Monograph available for loan
    Chichester [u.a.] : Wiley
    Call number: M 01.0425
    Type of Medium: Monograph available for loan
    Pages: xii, 322 S.
    ISBN: 0471895903
    Series Statement: Publication / International Association of Geomorphologists 9
    Classification:
    Applied Geology
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Vancouver : University of British Columbia Press
    Call number: AWI G3-23-95320
    Description / Table of Contents: This collection of papers by internationally known scientists in the field of geocryology was originally presented as a series of lectures at the University of British Columbia in 1980-81 in honour of J. Ross MacKay. Together they illustrate the central dilemma in a science where fieldwork must be undertaken in the harsh periglacial environment and where, consequently, it is difficult to test theory rigorously. The papers provide a valuable overview of the current status of international research in a wide area of the field - permafrost, patterned ground, and cold climate phenomena and processes. The treatment varies from anecdotal, historical, and descriptive to mathematical. The studies on soil freezing, ice formation and thaw are relatively sophisticated treatments that are physically sound, theoretically based, and quantitatively precise, as are the computational methods and the extension of results to engineering site evaluations given in other contributions. The regional accounts of geocryological and nival phenomena, on the other hand, remain entirely empirical and, for the most part, qualitative. This critical mismatch of understanding between microscale and regional scale is emphasized in the review of the status of periglacial studies. Ross MacKay's most valuable contribution to science has been his consistent demonstration of how to occupy the middle ground by applying simple physical concepts to explain variations in the landscape.
    Type of Medium: Monograph available for loan
    Pages: XVI, 213 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 0774802049 , 0-7748-0204-9
    Language: English , French , Russian
    Note: CONTENTS List of Figures and Illustrations List of Tables Preface Acknowledgements Notation 1. On the Scientific Method of J. Ross Mackay / W.H. MATHEWS 2. Experimental Observations of Periglacial Processes in the Arctic / ALFRED JAHN 3. Extreme Rainfall and Rapid Snowmelt as Causes of Mass Movements in High Latitude Mountains / ANDERS RAPP 4. Estimation of Avalanche Runout Distances in New Zealand/ B.B. FITZHARRIS 5. The Ice Factor in Frozen Ground / L.W. GOLD 6. Models of Soil Freezing / M.W. SMITH 7. A Step Function Model of Ice Segregation / S.I. OUTCALT 8. Recent Observations on the Deformation of Ice and Ice-Rich Permafrost / N.R. MORGENSTERN 9. Distribution of Recently Active Ice and Soil Wedges in the U.S.S.R. / N.N. ROMANOVSKIJ 10.Periglacial Problems / A.L. WASHBURN Notes on Contributors Author Citation Index Index , Abstracts in englischer, französischer und russischer Sprache
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Malden, Mass. [u.a.] : Blackwell
    Call number: AWI G3-23-95310
    Type of Medium: Monograph available for loan
    Pages: XVIII, 261 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 140512976X , 1-4051-2976-X , 978-1-4051-2976-3
    Series Statement: Environmental systems and global change series 1
    Language: English
    Note: Contents Preface 1 The evidence for cryospheric change 1.1 Introduction 1.2 The geomorphic and hydrologic effects of cryospheric change 1.3 Sub-arctic and alpine hydrology 1.4 Glacier loss and mountain permafrost 1.5 Permafrost 1.6 The carbon balance of the cryosphere 1.7 River and lake ice break-up and freeze-up 1.8 Ocean circulation 1.9 The mass balance of the polar ice sheets 1.10 Sea level 1.11 Importance of sea ice. 1.12 Ecological impacts 1.13 Socio-economic effects 1.14 Conclusions (Text word count-including figure captions and tables but excluding references- 9,015) 2 The monitoring of cryospheric change 2.1 Introduction 2.2 In situ measurements 2.2.1 Land surface air temperature 2.2.2 Terrestrial snow and snow on sea ice 2.2.3 Sea ice 2.2.4 Ice sheets and alpine glaciers 2.2.5 Permafrost and seasonally frozen ground 2.2.6 River runoff 2.2.7 River and lake ice freeze-up and break-up 2.3 Conclusions 3 Processes of cryospheric change 3.1 Introduction 3.2 Snow and ice as energy regulators 3.2.1 The energetics of the snow surface 3.2.2 The energetics of the snowpack 3.2.3 The energetics of glaciers 3.2.4 The energetics of sea ice and various terrain types 3.2.5 Permafrost 3.3 Snow and ice reservoir functions 3.3.1 Mass budget for snow 3.3.2 Mass balance for glacier ice 3.3.3 The mass balance of an ice sheet 3.3.4 Mass balance of sea ice 3.4 Snowfall 3.4.1 Interception by vegetation 3.4.2 Snow accumulation 3.4.3 Snow cover structure 3.5 Snow avalanches 3.6 Snow melt, runoff and streamflow generation 3.7 Snow chemistry 3.8 Snow ecology 3.9 Glacier melt 3.10 Formation of an ice cover 3.11 River and lake ice 3.12 Sediment budgets 4 Patterns of the contemporary cryosphere at local to global scales 4.1 Introduction 4.2 Remote sensing observations 4.3 Land and sea surface temperature 4.3.1 Terrestrial snow and snow on sea ice 4.3.2 Sea ice 4.3.3 Ice sheets & glaciers: estimation of volume 4.3.4 Ice sheets & glaciers: mass balance components 4.3.5 Permafrost 4.3.6 River runoff 4.3.7 River and lake ice freeze-up/break-up 4.4 Numerical Models 4.5 Conclusions: validation, coordinated projects and climate data records 5 The evidence for past cryospheric changes 5.1 Introduction 5.2 The uniqueness of the Quaternary Period 5.3. Initiation of glacial ages 5.4 Reconstructing extent of glacial environments 5.5 Extreme events 5.6 Ice sheet modelling 5.6.1 The Antarctic Ice Sheet 5.6.2 Greenland 5.6.3 North America: Innuitian, Laurentide and Cordilleran ice sheets 5.6.4 British Isles, Scandinavian and Barents ice sheets 5.6.5 The Patagonian and New Zealand ice caps 5.7 Non-glacial Quaternary environments 5.7.1 Late Quaternary permafrost in North America and Europe 5.7.2 Treeline variations 5.7.3 Climatic snowline 5.7.4 Glacier fluctuations 5.7.5 Paraglaciation 6 The transience of the cryosphere and transitional landscapes 6.1 Introduction 6.1.1 The landscape as palimpsest 6.2 Glacial landscapes: macro scale 6.2.1 Cirque landscapes 6.2.2 Fjord and strandflat landscapes 6.3 Periglacial landscapes: macro-scale 6.4 Paraglacial landscapes: macro-scale 6.5 Glacial landscapes: medium-scale 6.5.1 The transition from glacial to fluvial dominance 6.6 Proglacial landscapes: medium-scale 6.6.1 Glacifluvial landforms 6.6.2 The Channeled Scablands 6.6.3 Sub-glacial channels 6.6.4 Sub-glacial, ice-marginal and supraglacial sediment-landform associations 6.7 Periglacial landscapes: medium scale 6.7.1 The transition from periglacial to fluvial dominance 6.8 Paraglacial landscapes: medium-scale 6.9 Glacial landscapes: local-scale 6.9.1 Primary glacigenic deposits 6.9.2 Small scale erosional forms 6.10 Proglacial landscapes: local-scale 6.11 Periglacial landscapes: local scale 6.13 Paraglacial landscapes: local-scale 6.13 Landscape resistance, collapse and recovery 6.14 Transitional landscapes at Quaternary, Holocene and Anthropocene timescales 7 Cryospheric change and vulnerability at Quaternary, Holocene and Anthropocene time scales 7.1 Introduction 7.2 Panarchy 7.2.1 Panarchy, sustainability and transformability 7.2.2 Collapse and the vulnerability of socio-economic systems 7.3 Changing ice cover and biomes since the Last Glacial Maximum 7.3.1 The Last Glacial Maximum 7.3.2 The Holocene Optimum 7.4 The first explorers in North America 7.5 Implications of cryospheric change/collapse 7.5.1 Snow quantity 7.5.2 Snow quality 7.5.3 River and lake ice 7.5.4 Permafrost 7.5.5 Glaciers 7.5.6 River basins 7.5.7 Sea ice 7.5.8 Ice sheets 7.5.9 Sea level change 7.5.10 Carbon sequestration 7.5.11 Vegetation 7.5.12 Polar bears 7.5.13 Human health 7.5.14 Persistent organic pollutants 7.5.15 Socio-cultural conditions and health status 7.5.16 Livelihoods and socio-economic conditions 7.5.17 Governance 7.6 Concluding thoughts References Index
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 337 (1989), S. 452-454 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Happ and others4"6 have shown that specific sediment yield presently increases downstream in the south-eastern United States, which they explained in terms of remobilization of sedi-ment eroded from uplands during the first two centuries of European agrarian settlement. Schumm7 has asserted that ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 91-92 (1982), S. 93-109 
    ISSN: 1573-5117
    Keywords: land use ; sediment yield ; water quality ; sediment quality
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Attempts to establish land use effects on sediment yield and water quality require consideration of (1) background biogeochemical cycling, (2) quantitative land use mapping, (3) selection of appropriate transport and attenuation models and (4) assessment of critical or threshold amounts, and types of land use change. Progress in each of these problem areas is considered.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 91-92 (1982), S. 93-109 
    ISSN: 1573-5117
    Keywords: land use ; sediment yield ; water quality ; sediment quality
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Attempts to establish land use effects on sediment yield and water quality require consideration of (1) background biogeochemical cycling, (2) quantitative land use mapping, (3) selection of appropriate transport and attenuation models and (4) assessment of critical or threshold amounts, and types of land use change. Progress in each of these problem areas is considered.
    Type of Medium: Electronic Resource
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  • 8
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    Unknown
    In:  Geological Society Special Publication 320: 71-84.
    Publication Date: 2009-07-27
    Description: The terms proglacial and periglacial are well-understood descriptors of contemporary and past environments, but the paraglacial concept is more controversial and has prompted vigorous debate. Definitions are reviewed and the paraglacial concept is considered critically. It is argued that the term paraglacial' defined as non-glacial processes conditioned by glaciation' describes landscapes that are adjusted neither to Last Glacial Maximum nor to contemporary geomorphic processes. Where a landscape is paraglacial it can be characterized in terms of rate of change and trajectory of that change. It cannot be defined in relation to glaciers (as in proglacial) or by cold-climate processes (as in periglacial). Almost all paraglacial landforms and all paraglacial landscapes are transient and transitional. An interesting challenge of paraglacial landscapes is then to determine their rates of change; how far they have advanced along the trajectory from glacial to non-glacial; and how to recognize empirically the temporal and spatial relationships between proglacial, periglacial, paraglacial and fluvial landscapes. Implications of this approach to paraglacial landscapes are discussed in relation to historical and dynamic geomorphology.
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  • 9
    Publication Date: 1982-07-01
    Print ISSN: 0018-8158
    Electronic ISSN: 1573-5117
    Topics: Biology
    Published by Springer
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  • 10
    Publication Date: 2001-01-01
    Print ISSN: 1001-6538
    Electronic ISSN: 1861-9541
    Topics: Natural Sciences in General
    Published by Springer
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