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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Minorities-Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (415 pages)
    Edition: 1st ed.
    ISBN: 9783642693113
    Series Statement: Dahlem Workshop Report ; v.27
    DDC: 305.8
    Language: English
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Barrier island ecology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (407 pages)
    Edition: 1st ed.
    ISBN: 9783319680866
    DDC: 910
    Language: English
    Note: Intro -- Dedication -- Preface -- Motivation -- An Overview of Barrier Dynamics -- Scope of the Volume: An Overview of Chapters -- Observation-Focused Contributions -- Modeling-Focused Contributions -- State of the Science and Future Directions -- Contents -- Contributors -- Part I: Observations and Conceptual Models of Barrier Response to Changing Climate -- Runaway Barrier Island Transgression Concept: Global Case Studies -- 1 Introduction -- 2 Methodology -- 3 Background -- 3.1 Marsh Deterioration Processes and Existing Modeling Results -- 3.2 Effects of Sea-level Rise on Hydrodynamics and Sediment Transport -- 3.3 Barrier/Tidal Inlet Response to Various Forcings: Basic Relationships -- 4 Case Studies -- 4.1 Nauset Spit-New Inlet, Cape Cod, Massachusetts -- 4.2 Ocean City Inlet-Assateague Island, Maryland -- 4.3 Virginia Barriers -- 4.4 Barataria Barriers, Louisiana -- 4.5 Chandeleur Islands and Isle Dernieres, Louisiana -- 4.5.1 The Chandeleur Islands -- 4.5.2 The Isles Dernieres -- 4.6 Copper River Barriers, Alaska -- 4.7 East Friesian Islands, Germany -- 5 Runaway Transgression Model -- 5.1 Presentation of Concept and Stages -- 5.1.1 Stable Barrier -- 5.1.2 Disintegrating Barrier -- 5.2 Final Disposition of Barrier Sand -- 6 Summary and Conclusions -- References -- Drowned Barriers as Archives of Coastal-­Response to Sea-Level Rise -- 1 Introduction -- 2 Barrier Coastal-Response to Transgression -- 3 Synthesis of Drowned Barriers -- 4 Characteristics of Drowned Barriers -- 5 Patterns of Drowned Barrier Distribution and Behaviour -- 5.1 Distribution of Drowned Barriers in Space and Time -- 5.2 Barrier Formation -- 5.3 Barrier Retreat Through Overstepping -- 5.4 Barrier Preservation -- 6 Relative Significance of Controls on Barrier Overstepping -- 6.1 Relative Sea-Level Rise -- 6.2 Sediment Supply -- 6.3 Topography/Antecedence. , 7 Prerequisites for Barrier Retreat Through Overstepping -- 8 Conclusions -- References -- Barrier Island and Estuary Co-evolution in Response to Holocene Climate and Sea-­Level Change: Pamlico Sound and the Outer Banks Barrier Islands, North Carolina, USA -- 1 Introduction -- 2 Study Area -- 2.1 Modern Setting -- 2.2 Antecedent Topography -- 3 Evolution in Response to Climate and Sea-Level Change -- 3.1 Early Holocene to ca 4000 Cal Year BP -- 3.1.1 Coastal Evolution -- 3.2 ca 4000-3500 Cal Year BP -- 3.2.1 Coastal Evolution -- 3.3 ca 3500-1200 Cal Year BP (750 CE-Common Era) -- 3.3.1 Coastal Evolution -- 3.4 The Medieval Climate Anomaly (ca 1200 Cal Year BP to ca 800 Cal Year BP -- 750-1150 CE) -- 3.4.1 Coastal Evolution -- 3.5 The Little Ice Age (ca 500 Cal Year BP) to Present -- 3.5.1 Coastal Evolution -- 4 Summary -- References -- Abrupt Increase in Washover Deposition Along a Transgressive Barrier Island During the Late Nineteenth Century Acceleration in Sea-Level Rise -- 1 Introduction -- 2 Study Area and Background -- 3 Methods -- 3.1 Coring -- 3.2 Radiocarbon Dating -- 3.3 Washover Measurements -- 4 Results and Interpretations -- 4.1 Depositional Environments and Lithologic Facies -- 4.1.1 Beach Facies -- 4.1.2 Dune Facies -- 4.1.3 Saltmarsh Facies -- 4.1.4 Washover Facies -- 4.1.5 Facies A -- 4.1.6 Facies B -- 4.2 Stratigraphy -- 5 Discussion -- 6 Conclusions -- References -- Follets Island: A Case of Unprecedented Change and Transition from Rollover to Subaqueous Shoals -- 1 Introduction -- 2 Study Area -- 3 Methodology -- 4 Results -- 4.1 Lithofacies -- 4.2 Stratigraphy -- 4.3 Sand Budget and Flux Analysis -- 4.3.1 Sand Overwash Estimate -- 4.3.2 Drowning Time Estimate -- 4.3.3 Modern Versus Long-Term Overwash Flux -- 4.3.4 Back-Barrier Accommodation -- 5 Discussion -- 6 Conclusions -- References. , Role of the Foredune in Controlling Barrier Island Response to Sea Level Rise -- 1 Introduction -- 2 Controls on Dune Height -- 2.1 Role of the Geologic Framework -- 3 Beach-Dune Interaction -- 3.1 Sediment Supply from the Nearshore -- 3.2 Transport Potential -- 3.3 Vegetation -- 4 Foredune Erosion and Recovery -- 4.1 Dune Recovery at Santa Rosa Island -- 4.2 Storm Frequency and Sequencing -- 4.3 Alongshore Variability and Lateral Erosion -- 5 Anthropogenic Impact to Dune Recovery -- 6 Summary -- References -- Part II: Mechanisms of Barrier Response to Changing Climate -- Geometric Constraints on Long-Term Barrier Migration: From Simple to Surprising -- 1 Introduction -- 2 Background -- 2.1 Cross-shore Shoreface-Barrier Profile -- 2.2 Landward Profile Translation and Sediment Excavation -- 2.3 Response to Sea-Level Rise: Qualitative Concept -- 3 Simplest Migration Scenario: Generalized Bruun Rule for Barriers, and Long-Term Consequences -- 3.1 Assumptions -- 3.2 Generalized Bruun Rule for Barriers -- 3.3 Long-Term Consequences -- 4 The Effect of Shoreface Composition on Barrier Response to RSLR -- 5 The Effect of Sediment Losses (or Gains) on Barrier Response to RSLR -- 6 The Effect of Back-Barrier Deposition, Deposit Thickness, and Composition -- 6.1 Coupling Between Back-Barrier Deposition and Barrier Migration Trajectory -- 6.2 Negative Feedback -- 6.3 Positive Feedback -- 6.4 Timescalesof Migration-Trajectory Adjustments -- 7 Toward the Real World: Numerical Modeling -- 8 Discussion -- 9 Conclusions -- References -- Shoreface Controls on Barrier Evolution and Shoreline Change -- 1 Introduction -- 2 Shoreface-Accommodation Controls on Barrier Form and Dimensions -- 3 Shoreface Dynamics: The Missing Link -- 3.1 Sediment-Transport Processes -- 3.2 Geological Evidence -- 3.3 Knowledge Gaps -- 4 Lower Shoreface Change and Barrier Evolution. , 4.1 Framework for Investigating Shoreface Morphologic-­Response Timescales -- 4.2 Exploring Shoreface Response to Sea-Level Change -- 4.3 Implications for Barrier Response to Climate Change -- 5 Conclusions -- 5.1 Shoreface-Related Accommodation Constraints on Barrier Form and Volume -- 5.2 Challenges in Forecasting Barrier Evolution: Lagged Shoreface Response -- References -- Morphodynamics of Barrier Response to Sea-­Level Rise -- 1 Introduction -- 2 Dynamic Processes Affecting Barriers -- 2.1 Shoreface Evolution -- 2.2 Overwash -- 2.3 Alongshore Sediment Transport -- 3 Morphokinematics Versus Morphodynamics of Barrier Response to Sea-Level Rise -- 4 A Simplified Morphodynamic Model of Barrier Evolution -- 5 Morphodynamic Barrier Response to Sea-Level Rise -- 5.1 Modes of Barrier Response -- 5.2 Controls on Barrier Response -- 5.3 Threshold Response to Back-Barrier Geometry -- 6 Alongshore Coupling -- 7 Discussion -- 8 Conclusions -- References -- The Role of Ecomorphodynamic Feedbacks and Landscape Couplings in Influencing the Response of Barriers to Changing Climate -- 1 Introduction -- 2 Vegetation Control of Dune Morphology -- 2.1 Maximum Potential Dune Height -- 2.2 Hummockiness -- 2.3 Number, Spacing, and Size of Multiple Dunes -- 3 Factors Controlling Dune and Barrier State Across Scales -- 4 Couplings Between Barriers and Back-Barrier Marshes -- 4.1 Effect of Back-Barrier Marshes on Barrier Migration Rate -- 4.2 Effect of Barrier Dynamics on Back-Barrier Marshes -- 4.3 Effects of Overwash on Marshes: Experimental Results -- 5 Summary and Implications -- References -- The Role of Vegetation in Determining Dune Morphology, Exposure to Sea-Level Rise, and Storm-Induced Coastal Hazards: A U.S. Pacific Northwest Perspective -- 1 Introduction -- 2 Study Area Description -- 3 U.S. Pacific Northwest Beach and Foredune Morphometrics. , 4 Relative Importance of Sand Supply and Beach Grasses to Dune Geomorphology -- 4.1 Species-Specific Feedbacks -- 4.2 Retrospective Analysis -- 5 Implications to Coastal Protection Services -- 6 Implications for Enhancing Beach-Dune Interaction Models -- 7 Synthesis and Conclusions -- References -- Barrier Islands as Coupled Human-Landscape Systems -- 1 Introduction -- 2 Beach Nourishment and Coupled Coastal Dynamics -- 2.1 Modelling the Coupled Economic-Physical System -- 2.2 Developed Coastlines and Common-Pool Resources -- 3 Inundation and Abandonment: An Attractor Disappears -- 3.1 Modeling the Decision to Abandon: Physical Forcing -- 3.2 Modeling the Decision to Abandon: Policy Forcing -- 3.3 Modeling the Decision to Abandon: Psychological Forcing -- 4 Boom, Bust, Repeat: An Attractor Emerges -- 5 Conclusions -- References -- Index.
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  • 3
    Online Resource
    Online Resource
    Berlin, Heidelberg : Springer Berlin Heidelberg
    Keywords: Geometry, algebraic ; Mathematics ; Algebraic geometry. ; Algebra. ; Algebraic Geometry ; Mathematics ; Körper ; Ordnung ; Spektrum
    Description / Table of Contents: This book is of interest to students as well as experts in the area of real algebraic geometry, quadratic forms, orderings, valuations, lattice ordered groups and rings, and in model theory. The original motivation comes from orderings on fields and commutative rings. This is explained as is the important application to minimal generation of semi-algebraic sets. Many results in the new theory of abstract real spectra (also called spaces of signs) appear here for the first time. The reader needs elementary knowledge of commutative rings, ordered fields and real closed fields and valuations
    Type of Medium: Online Resource
    Pages: Online-Ressource (VI, 198 p, online resource)
    ISBN: 9783540699965 , 9783540617297
    Series Statement: Lecture Notes in Mathematics 1636
    RVK:
    Language: English
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  • 4
    Online Resource
    Online Resource
    Cham : Springer
    Keywords: Geography ; Climate change ; Coasts ; Physical geography ; Geomorphology ; Environmental management
    Description / Table of Contents: This book presents chapters, written by leading coastal scientists, which collectively depict the current understanding of the processes that shape barrier islands and barrier spits, with an emphasis on the response of these landforms to changing conditions. A majority of the world’s population lives along the coast at the dynamic intersection between terrestrial and marine ecosystems and landscapes. As narrow, low-lying landforms, barriers are especially vulnerable to changes in sea level, storminess, the geographic distribution of grass species, and the rate of sand supply-some barriers will undergo rapid changes in state (e.g., from landward migrating to disintegrating), on human time scales. Attempts by humans to prevent change can hasten the loss of these landforms, threatening their continued existence as well as the recreational, financial and ecosystem service benefits they provide. Understanding the processes and interactions that drive landscape response to climate change and human actions is essential to adaptation. As managers and governments struggle to plan for the future along low-lying coasts worldwide, and scientists conduct research that provides useful guidance, this volume offers a much-needed compilation for these groups, as well as a window into the science of barrier dynamics for anyone who is generally interested in the impacts of a changing world on coastal environments
    Type of Medium: Online Resource
    Pages: Online-Ressource (XXIII, 395 p. 140 illus., 123 illus. in color, online resource)
    ISBN: 9783319680866
    Series Statement: SpringerLink
    Language: English
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  • 5
    Book
    Book
    Vancouver : Douglas & McIntyre
    Keywords: Newman, Murray A
    Type of Medium: Book
    Pages: ix, 262 p., [48] p. of plates , ill. (some col.) , 25 cm
    ISBN: 1550541250
    DDC: 597/.0074/71133
    Language: English
    Note: Includes index
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  • 6
    Publication Date: 2021-04-29
    Description: Dryland slopes, fluvial fans and terraces are recognized as highly sensitive process-response systems and important geoarchives for the reconstruction of palaeoclimatic driven landscape development in Southern Africa. The aim of this study is to study a dryland drainage system with a clearly limited regional catchment area, whose drainage and sedimentation behavior is unaffected by distant meteorological events or changes in climatic outside the region. Our results highlight for the first time the widespread occurrence of fluvial and lacustrine sediments in the Naukluft Mts. foreland as part of the Great Escarpment and their potential as Late Quaternary geoarchives. The region’s special interest and overarching value lies (i) in the bounded catchments of both the lacustrine BüllsPort Playa and the ephemeral rivers Tsauchab and Tsondab within the South African Great Escarpment and (ii) in the rivers’ endorheic character and dead ends within the Namib Sand Sea to the West. All these lacustrine and fluvial systems first and foremost exclude supra-regional influences within the flow regime. Uniquely, the key palaeoclimatic question of periodical shifts of the rainfall zones during Holocene and Late Glacial times can be studied in both these catchments. This study also combines new data from the semi-desert environment of the Naukluft Mts. with data from the terminus sites Sossusvlei and Tsondabvlei within the Namib dunes. From our interpretation of the desert flash flood series, the drainage history from pre-LGM times within MIS 3 up to modern times is represented in our data. The Late Termination I was the period with the highest flow rates post MIS3, raising the Urikos Terrace. This must have been caused by strong monsoonal rainfall events from summer TTT, giving rise to extreme flash floods. Little Ice Age sediments have filled the entire thalweg, with the exception of remnant Holocene to MIS 3 terraces to the sides and provide a unique framework for ecological conditions.
    Type: info:eu-repo/semantics/article
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  • 7
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    In:  Petroleum Geology: North-West Europe and Global Perspectives - Proceedings of the 6th Petroleum Geology Conference
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/bookPart
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  • 8
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
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  • 9
    Publication Date: 2021-08-11
    Description: Permafrost region subsurface organic carbon (OC) pools are a major component of the terrestrial carbon cycle and vulnerable to a warming climate. Thermokarst lagoons are an important transition stage with complex depositional histories during which permafrost and lacustrine carbon pools are transformed along eroding Arctic coasts. The effects of temperature and salinity changes during thermokarst lake to lagoon transitions on thaw history and lagoon deposits are understudied. We analyzed two 30-m-long sediment cores from two thermokarst lagoons on the Bykovsky Peninsula, Northeast Siberia, using sedimentological, geochronological, hydrochemical, and biogeochemical techniques. Using remote sensing we distinguished between a semi-closed and a nearly closed lagoon. We (1) characterized the depositional history, (2) studied the impact of marine inundation on ice-bearing permafrost and taliks, and (3) quantified the OC pools for different stages of thermokarst lagoons. Fluvial and former Yedoma deposits were found at depth between 30 and 8.5 m, while lake and lagoon deposits formed the upper layers. The electrical conductivity of the pore water indicated hypersaline conditions for the semi-closed lagoon (max: 108 mS/cm), while fresh to brackish conditions were observed beneath a 5 m-thick surface saline layer at the nearly closed lagoon. The deposits had a mean OC content of 15 ± 2 kg/m3, with higher values in the semi-closed lagoon. Based on the cores we estimated a total OC pool of 5.7 Mt-C for the first 30 m of sediment below five mapped lagoons on the Bykovsky Peninsula. Our results suggest that paleo river branches shaped the middle Pleistocene landscape followed by late Pleistocene Yedoma permafrost accumulation and early Holocene lake development. Afterward, lake drainage, marine flooding, and bedfast ice formation caused the saline enrichment of pore water, which led to cryotic talik development. We find that the OC-pool of Arctic lagoons may comprise a substantial inventory of partially thawed and partially refrozen OC, which is available for microbial degradation processes at the Arctic terrestrial-marine interface. Climate change in the Arctic leading to sea level rise, permafrost thaw, coastal erosion, and sea ice loss may increase the rate of thermokarst lagoon formation and thus increase the importance of lagoons as biogeochemical processors of former permafrost OC.
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 10
    Publication Date: 2020-02-12
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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