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  • Wissenschaftspark Albert Einstein  (23)
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  • 1
    UID:
    almafu_BV046716218
    Umfang: 267 Seiten : , Illustration.
    ISBN: 978-3-428-15953-6
    Serie: Beihefte zu "Der Staat" Heft 24
    Inhalt: Der herausragende Rang Ernst-Wolfgang Böckenförde als Denker des Staates, als Rechtswissenschaftler und auch als Bundesverfassungsrichter wird in Deutschland wenig bestritten. Weniger bekannt ist, dass er auch über Deutschland hinaus als einflussreicher Gelehrter gelten kann. Über achtzig seiner Aufsätze und zwei seiner Bücher sind in zahlreiche Sprachen übersetzt worden. Die hier versammelten Autorinnen und Autoren sind allesamt durch Übersetzungen und Interpretationen mit seinem Werk in besonderer Weise vertraut. In zwölf Beiträgen wird gezeigt, wie Böckenförde jenseits von Deutschland verstanden und verständlich gemacht wird, wann, unter welchen Bedingungen und zu welchen Anlässen er in den jeweiligen wissenschaftlichen und auch politischen, kulturellen oder religiösen Diskursen Italiens, Polens, Frankreichs, Koreas, Japans und in der spanisch- und portugiesischsprachigen Welt Südamerikas »zum Argument« gemacht wird.
    Inhalt: Dabei wird auch deutlich, wie unterschiedlich übersetzte Rechtskonzepte in lokale Rechtsdiskurse integriert und in ihrer Bedeutung an den jeweiligen Kontext angepasst werden. Bei aller Diversität der Rezeption wird indes überall wahrgenommen, dass das Denken Böckenfördes eine besonders originelle und ergiebige Verknu¨pfung zwischen der deutschen Staatslehre und dem politischen Liberalismus darstellt. / »The Reception of Ernst-Wolfgang Böckenförde's Oeuvre in International Comparative Perspective« --
    Inhalt: Ernst-Wolfgang Böckenförde is a much-discussed scholar also beyond German-speaking lands. The articles in this collection analyze the reception of his work in the academic as well as political, cultural, and religious discourses of Italy, Poland, Korea, Japan, and in the Spanish and Portuguese-speaking world of South America. They show when, how, and in what context Böckenförde's writings are invoked to buttress or challenge a particular argument. The contributors are all particularly familiar with his work, having translated and/or interpreted it in the various languages
    Weitere Ausg.: Erscheint auch als Online-Ausgabe ISBN 978-3-428-55953-4
    Sprache: Deutsch
    Fachgebiete: Rechtswissenschaft
    RVK:
    RVK:
    Schlagwort(e): 1930-2019 Böckenförde, Ernst-Wolfgang ; Rezeption ; Internationaler Vergleich ; Staatsrecht ; Konferenzschrift ; Konferenzschrift ; Konferenzschrift ; Festschrift ; Konferenzschrift ; Hochschulschrift ; Konferenzschrift ; Bibliografie ; Fotografie
    Mehr zum Autor: Stein, Tine 1965-
    Mehr zum Autor: Künkler, Mirjam 1977-
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  • 2
    Buch
    Buch
    London u.a. :Belhaven,
    UID:
    almafu_BV001304624
    Umfang: XIV, 173 S.
    Ausgabe: 1. publ.
    ISBN: 1-85293-048-9
    Anmerkung: Zugl.: Oslo, Univ., Diss., 1986
    Sprache: Englisch
    Fachgebiete: Wirtschaftswissenschaften
    RVK:
    Schlagwort(e): Internationaler Umweltschutz ; Umweltpolitik ; Umweltschutz ; Hochschulschrift ; Hochschulschrift
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  • 3
    Buch
    Buch
    London [u.a.] : Earthscan
    UID:
    gbv_635267608
    Umfang: XII, 264 S. , graph. Darst., Kt.
    Ausgabe: 1. publ.
    ISBN: 9781844078264
    Inhalt: Introduction -- Criteria-based definitions of scientific terms -- Comparisons between generations -- Objections to theories of generational justice -- What to sustain? : capital or well being as an axiological goal -- How much to sustain? : the demands of justice in the intergenerational context -- Conclusion
    Anmerkung: Includes bibliographical references and index , Teilw. zugl.: Düsseldorf, Univ., Diss.
    Weitere Ausg.: Erscheint auch als Online-Ausgabe Tremmel, Jörg, 1970 - A theory of intergenerational justice London [u.a.] : Earthscan, 2009 ISBN 9781844078264
    Sprache: Englisch
    Schlagwort(e): Generationengerechtigkeit ; Hochschulschrift
    Mehr zum Autor: Tremmel, Jörg 1970-
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  • 4
    UID:
    gbv_1817785389
    Umfang: xi, 121 Seiten , Diagramme, Illustrationen
    Inhalt: The deciduous needle tree larch (Larix Mill.) covers more than 80% of the Asian boreal forests. Only a few Larix species constitute the vast forests and these species differ markedly in their ecological traits, most importantly in their ability to grow on and stabilize underlying permafrost. The pronounced dominance of the summergreen larches makes the Asian boreal forests unique, as the rest of the northern hemisphere boreal forests is almost exclusively dominated by evergreen needle-leaf forests. Global warming is impacting the whole world but is especially pronounced in the arctic and boreal regions. Although adapted to extreme climatic conditions, larch forests are sensitive to varying climatic conditions. By their sheer size, changes in Asian larch forests as range shifts or changes in species composition and the resulting vegetation-climate feedbacks are of global relevance. It is however still uncertain if larch forests will persist under the ongoing warming climate or if they will be replaced by evergreen forests. [...]
    Anmerkung: Dissertation Universität Potsdam 2022
    Weitere Ausg.: Erscheint auch als Online-Ausgabe Schulte, Luise Dynamics of Larix (Mill.) species in Siberia during the last 50,000 years inferred from sedimentary ancient DNA Potsdam, 2022
    Sprache: Englisch
    Schlagwort(e): Hochschulschrift ; Hochschulschrift ; Hochschulschrift
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  • 5
    UID:
    kobvindex_GFZ168757734X
    Umfang: viii, 270 Seiten , Illustrationen, Diagramme , 21 cm
    ISSN: 04533267
    Serie: Veröffentlichungen des Institutes für Bodenmechanik und Felsmechanik am Karlsruher Institut für Technologie (KIT) Heft 186
    Anmerkung: Dissertation, Karlsruher Institut für Technologie (KIT), 2019 , 1 Introduction 1.1 Practical relevance of the subject 1.2 Motivation and aims of research presented in this thesis 1.3 Outline 1.4 Notation 2 Constitutive description 2.1 Elasticity 2.2 Hypoelasticity 2.3 Transverse isotropic (hypo)elasticity 2.4 Dilatancy 2.4.1 From direct shear to general conditions 2.4.2 Overview of expressions describing the state dependent Dilatancy of cohesionless soils 2.4.3 State-dependent Dilatancy for monotonic loading described by Li & Dafalias [1] 2.4.4 State-dependent Dilatancy described by Grandas & Triantafyllidis [2] 2.4.5 Basic postulates for cohesive soils 24 2.4.6 How to evaluate the Dilatancy from undrained triaxial tests on cohesive soils 2.4.7 Revision and reformulation of Taylors' rule [3] to account for the behaviour of cohesive soils 3 Experimental observations on cohesive soils 3.1 Parametric study on Kaolin 3.1.1 Inherent anisotropy 3.1.2 Dilatancy 3.2 Parametric study on Lower Rhine Clay (LRC) 3.2.1 Stress amplitude 3.2.2 Loading frequency 3.2.3 Overconsolidation ratio 3.2.4 Issues 3.2.5 Dilatancy 4 Comparison between different viscous model families 4.1 Charateristic isotachs and overconsolidation ratio 4.2 Creep rate 4.3 Development of constitutive equations 4.3.1 Nonstationary Flow Surface model (NSFS) 4.3.2 Overstress Viscoplastic model (OVP) 4.3.3 Visco-plastic model with Norton's power law (NVP) 4.3.4 Visco-hypoplastic model (VHP) 4.4 Adjustment to a unique reference isotach 4.5 Material parameters 4.6 Numerical implementation 4.7 Element Test Simulations 4.7.1 Isotropic compression with constant strain rate 4.7.2 Creep test 4.7.3 Stress relaxation test 4.7.4 Response envelopes 4.7.5 Undrained creep rupture 4.7.6 Simulation of experiments under oedometric loading 4.8 Final remarks 5 Anisotropic Visco ISA - (AVISA) model 5.1 ISA plasticity 5.1.1 Mechanical model 5.2 Mechanical model formulation under fully mobilized states 5.2.1 Elastic stiffness tensor E 5.2.2 Incorporation of inherent anisotropy and fabric effects 5.2.3 Characteristic surfaces and void ratios 5.2.4 Flow rule m 5.2.5 Overconsolidation ratio OCR 5.2.6 Degree of nonlinearity Y 5.3 Numerical implementation 5.4 Calibration of material parameters 5.4.1 Parameters for the small strain stiffness (IS) 5.4.2 Parameters for the transversal hypoelasticity 5.4.3 Parameters for the critical state and the loading surface 5.4.4 The parameter used to -quantify the creep rate of the material viz. the time-dependent effects 5.5 Simulations of tests under monotonic loading 5.5.1 Soft and/or normally consolidated clays 5.5.2 Stiff and/or ovcrconsolidated clays 5.5.3 Time-dependent behaviour of clays 5.5.4 Directional response 5.5.5 Limitations of the model 5.6 Simulations of tests under cyclic loading 5.6.1 Low plasticity clay - Kaolin 5.6.2 High plasticity clay - Lower Rhine Clay 6 Constitutive anamnesis model for clays 6.1 Historiotropic flow surface 6.1.1 Evolution of back stress tensor σB 6.2 Mechanical model formulation 6.2.1 Elastic stiffness tensor E 6.2.2 Incorporation of inherent anisotropy and fabric effects 6.2.3 Characteristic surfaces and void ratios 6.2.4 Incorporation of Dilatancy in a general hypoplastic model 6.2.5 Overconsolidation ratio OCR 6.2.6 Degree of nonlinearity Y 6.2.7 Flow rule m 6.2.8 Time dependency and critical void ratio 6.2.9 Uniqueness and Attainability of the critical state 6.2.10 Earth pressure coefficient K0 6.3 Inspection: Does the one dimensional version of the model satisfy the special cases? 6.3.1 Using isotropic elasticity (α = 1) 6.3.2 Using transversal isotropic elasticity 6.4 Numerical implementation 6.5 Calibration of material parameters 6.5.1 Parameters for the transversal hypoelasticity 6.5.2 Parameters for the historiotropic surface 6.5.3 Parameters for the critical, loading and dilatancy surface 6.5.4 The parameter used to quantify the creep rate of the material viz. the time-dependent effects 6.6 Simulations of tests under monotonia and cyclic loading 6.6.1 Kaolin 6.6.2 Lower Rhine Clay 6.7 Modified shape of the historiotropic surface 6.8 Final remarks 7 Application to BVP 7.1 Soil improvement by prior loading 7.2 Simulation of the bearing capacity of a shallow foundation 7.2.1 Monotonic loading 7.2.2 Cyclic loading 7.3 Consolidation of Kaolin under alternating cyclic loading 7.3.1 Filter disks in end plates (triaxial test) 7.3.2 Central porous stone in end plates (triaxial test) 7.4 Tunnel settlement of Metro Line No. 4 in Shanghai 7.5 Final remarks 8 Summary and Outlook - Zusammenfassung und Ausblick 8.1 Summary 8.2 Outlook 8.3 Zusammenfassung 8.4 Ausblick Appendix A Required derivatives Appendix B Programming the creep rupture condition for the VHP model Appendix C Mathematica script for the calibration of ei0 Appendix D Summary of constitutive relations of the reference and of AVISA model Appendix E Approximation of the mean pressure p with time t Bibliography
    In: Veröffentlichungen des Institutes für Bodenmechanik und Felsmechanik am Karlsruher Institut für Technologie (KIT), Heft 186
    Weitere Ausg.: eng
    Sprache: Englisch
    Schlagwort(e): Hochschulschrift
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  • 6
    UID:
    kobvindex_GFZ20190403143535
    Umfang: xvii, 103 Seiten , Illustrationen
    Inhalt: In ice-rich permafrost regions, changes in the permafrost thermal regime cause surface disturbances. These changes are amplified by the increase in air temperatures recorded in the Arctic in the past decades. Thermokarst is a process that leads to surface subsidence and formation of characteristic landforms following thawing of ice-rich permafrost or melting of massive ice. Thermokarst is widespread on hillslopes and the number of associated landforms is increasing in the Arctic. Through this process large amounts of material are eroded and transported to the sea or accumulate along hillslopes. While hillslope thermokarst modifies terrestrial and aquatic ecosystems, there is limited understanding of its environmental impact at a regional scale. In this thesis we quantify the environmental impacts of hillslope thermokarst on the valley and nearshore ecosystems along the Yukon Coast, Canada. Using supervised machine learning, we identified geomorphic factors that favour the development of coastal retrogressive thaw slump (RTS), one of the most dynamic hillslope thermokarst landform. Coastal geomorphology and ground ice type and content play a major role in RTS occurrence. Using aerial photographs and satellite imagery, we traced the evolution of RTSs between 1952 and 2011. During this time, the number and areal coverage of RTSs increased by 73%. RTSs eroded and partly released to the nearshore zone organic carbon contained in millions of cubic meters of material. Our results show that 56% of the RTSs identified along the coast in 2011 have eroded 16.6 × 10^6 m3 of material; a large part (45%) was transported alongshore due to coastal processes. Moreover, we show that RTSs are a major contributor to the carbon budget in the nearshore ecosystem: 17% of the coastal RTSs identified in 2011 contributed annually up to 0.6% of the organic carbon released by coastal retreat along the Yukon Coast. To assess the impact of hillslope thermokarst on the terrestrial ecosystem, we measured the spatial distribution of soil organic carbon (SOC) and total nitrogen (TN) along hillslopes in three Arctic valleys. We highlight the high spatial variability in the distribution of SOC and TN in the valleys. This distribution is caused by complex soil processes occurring along the hillslopes. Hillslope thermokarst impacts the degradation of organic matter and affects the storage of SOC and TN.
    Anmerkung: Dissertation, Universität Potsdam, 2018 , Contents Acknowledgements Abstract (English/Deutsch/Français) List of figures List of tables 1 Introduction 1.1 Scientic background 1.1.1 The Arctic coast, permafrost and climate change 1.1.2 Organic carbon in permafrost soils 1.1.3 Hillslope thermokarst processes 1.2 Aims 1.3 Study region 1.4 Methods 1.4.1 Mapping 1.4.2 Spline interpolation and volumes estimations 1.4.3 Fieldwork 1.4.4 Geochemical analyses 1.4.5 Statistical analyses 1.5 Thesis outline 1.6 Authors’ contributions 2 Synthesis 2.1 Retrogressive thaw slumps are widely spread in ice-rich permafrost areas 2.2 Retrogressive thaw slumps contribute signicantly to the nearshore or-ganic carbon 2.3 Thermokarst impacts the distribution of soil organic carbon along hill-slopes 2.4 Outlook . 3 Terrain Controls on the Occurrence of Coastal RTSs 3.1 Abstract 3.2 Introduction 3.3 Study area 3.4 Methods 3.4.1 Mapping of retrogressive thaw slumps and landform classication 3.4.2 Environmental variables 3.4.3 Univariate regression trees 3.5 Results 3.5.1 Characteristics of retrogressive thaw slumps 3.5.2 Density and areal coverage of retrogressive thaw slumps 3.6 Discussion 3.6.1 Characteristics and distribution of retrogressive thaw slumps 3.6.2 Terrain factors explaining retrogressive thaw slump occurrence 3.6.3 Coastal Processes 3.7 Conclusion 4 RTSs release sediments and organic carbon into the Arctic Ocean 4.1 Abstract 4.2 Introduction 4.3 Study Area 4.4 Methods 4.4.1 Evolution of retrogressive thaw slumps 4.4.2 Volume Estimations 4.4.3 Estimates of soil and dissolved organic carbon values 4.5 Results 4.5.1 Evolution of retrogressive thaw slumps between 1952 and 2011 4.5.2 Eroded material and estimated amount of mobilized SOC and DOC 4.6 Discussion 4.6.1 Increase in slump activity 4.6.2 Eroded material from retrogressive thaw slumps and organic car-bon uxes 4.6.3 Impact of retrogressive thaw slumps on the coastal ecosystem 4.7 Conclusion 5 Snapshot of carbon and nitrogen distribution in Arctic valleys 5.1 Abstract 5.2 Introduction 5.3 Study Area 5.4 Methods 5.4.1 Spatial analyses 5.4.2 Sampling Scheme 5.4.3 Geochemical analyses 5.4.4 Environmental variables and statistical analyses 5.5 Results 5.5.1 Geomorphology of the valleys 5.5.2 Spatial distribution of carbon and nitrogen 5.5.3 Correlations between soil characteristics and geochemical variables 5.6 Discussion 5.6.1 Variability in soil and geochemical properties in Arctic valleys 5.6.2 Hillslope Processes 5.7 Conclusion 6 Eidessttatliche Erklärung A Appendix A.1 Chapter 3 A.2 Chapter 4 A.3 Chapter 5 Bibliography
    Sprache: Englisch
    Schlagwort(e): Hochschulschrift
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  • 7
    UID:
    kobvindex_GFZBV014315979
    Umfang: 1 Band (verschiedene Seitenzählungen) , Illustrationen
    ISSN: 1400-3813
    Serie: Earth Sciences Centre, Göteborg University : A 77
    Anmerkung: Enthält 5 Zeitschriftenaufsätze , Dissertation, Göteborgs Universitet, 2002 , Table of Contents: Introduction Methods Summary of Papers Paper I Paper II Paper III Paper IV Paper V Conclusions and discussion Acknowledgements References Appendices Paper I: Late Quaternary stratigraphy of western Yamal Peninsula, Russia : new constraints on the configuration of the Eurasian ice sheet / Forman, S. L., Ingólfson, Ó., Gataullin, V., Manley, W. F., Lokrantz, H. Paper II: Late Quaternary stratigraphy, glacial limits and paleoenvironments of the Maresale area, western Yamal Peninsula, Russia / Forman, S. L., Ingólfson, Ó., Gataullin, V., Manley, W. F., Lokrantz, H. Paper III: Late Quaternary stratigraphy, Radiocarbon Chronology, and Glacial History at Cape Shpindler, Southern Kara Sea, Arctic Russia / Manley, W. F., Lokrantz, H., Gataullin, V., Ingólfson, Ó., Andersson, T. Paper IV: Glaciotectonised Quaternary sediments at Cape Shpindler, Yugorski Peninsula, Arctic Russia : implications of glacial history, ice movements and Kara Sea Ice Sheet configuration / Lokrantz, H., Ingólfson, Ó. and Forman, S. L. Paper V: Origin of a massive ground ice body on Yugorski Peninsula, Arctic Russia : buried glacier ice or intrasedimental segregation ice? / Lokrantz, H. and Ingólfson, Ó.
    Sprache: Englisch
    Schlagwort(e): Hochschulschrift
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  • 8
    Buch
    Buch
    Hannover : Fachrichtung Geodäsie und Geoinformatik, Univ. Hannover
    Dazugehörige Titel
    UID:
    kobvindex_GFZ176793534X
    Umfang: 155 Seiten , Illustrationen, Diagramme
    ISBN: 978-3-7696-5279-6 , 9783769652796
    ISSN: 0174-1454
    Serie: Wissenschaftliche Arbeiten der Fachrichtung Geodäsie und Geoinformatik der Leibniz Universität Hannover Nr. 369
    Anmerkung: Auch veröffentlicht in: Deutsche Geodätische Kommission bei der Bayerischen Akademie der Wissenschaften, Reihe C, Nr. 867, München 2021, ISBN 978-3-7696-5279-6 , Dissertation, Gottfried Wilhelm Leibniz Universität Hannover, 2021 , Contents 1. Introduction 1.1. Motivation 1.2. Main Contributions 1.3. Thesis Outline 2. Basics 2.1. Feature based Image Matching 2.1.1. Overview: What is Feature based Image Matching? 2.1.2. Desired Properties for Detected Features and Descriptors 2.1.3. Scale-Invariant Feature Detection 2.1.4. Feature Affine Shape Estimation 2.1.5. Feature Orientation Assignment 2.1.6. Feature Description 2.1.7. Descriptor Matching 2.2. Convolutional Neural Network (CNN) 2.2.1. Architecture of CNN 2.2.2. Training of CNN 2.3. Siamese Convolutional Neural Network 3. Related Work 3.1. Local Feature Detection 3.1.1. Translation and Rotation Invariant Features 3.1.2. Scale Invariant Features 3.1.3. Detectors based on a Comparison of Grey Values or Saliency 3.1.4. Detectors based on Machine Learning 3.2. Feature Orientation and Affine Shape Estimation 3.2.1. Orientation Assignment 3.2.2. Affine Shape Estimation 3.3. Local Feature Description 3.3.1. Hand Crafted Descriptors 3.3.2. Machine Learning based Descriptors 3.4. An Application: Orientation of Oblique Aerial Images 3.5. Discussion 3.5.1. Orientation Assignment and Affine Shape Estimation 3.5.2. Descriptor Learning 3.5.3. An Aerial Photogrammetric Benchmark 3.5.4. Ability to Transfer Learned Modules 4. Deep Learning Feature Representation 4.1. Overview of the Methodology 4.2. Descriptor Learning using Active Weak Match Finder - WeMNet 4.2.1. Descriptor Learning Architecture 4.2.2. Generation of Training Pairs 4.2.3. Loss Function 4.2.4. Weak Match Branch 4.3. Self Supervised Feature Affine Shape Learning - MoNet 4.3.1. Affine Transformation Decomposition 4.3.2. Self Supervised Affine Shape Estimation Module 4.4. Self Supervised Orientation Assignment Module - MGNet 4.5. Full Affine Estimation Network - Full-AfFNet 4.5.1. Full Affine Network 4.5.2. Training Loss 4.5.3. Data Augmentation 4.6. Inference based on the Trained Networks 4.7. Discussion 4.7.1. Descriptor Learning 4.7.2. Affine Shape Estimation 4.7.3. Orientation Assignment Learning 4.7.4. The Inference Pipeline 5. Experiments and Results 5.1. Datasets 5.1.1. Datasets for Training 5.1.2. Datasets for Testing 5.2. Evaluation and Analysis Criteria 5.2.1. Task A: Patch based Image Matching 5.2.2. Task B: Descriptor Distance Analysis 5.2.3. Task C: Feature based Image Matching 5.2.4. Task D: Image Orientation 5.2.5. Summary of Tasks and Involved Datasets 5.3. Descriptor Learning and Patch Based Image Matching 5.3.1. Parameter Study for WeMNet 5.3.2. Comparison to Related Work 5.4. Descriptor Distance Analysis 5.4.1. Translation 5.4.2. Rotation 5.4.3. Affine Shape Transformation 5.5. Image Matching Analysis 5.5.1. Parameter Study for Affine Shape Learning 5.5.2. Image Matching for Rotation Dataset 5.5.3. Image Matching for Hpatches Affine Dataset 5.6. Image Orientation 5.6.1. Determination of Image Orientation 5.6.2. Experiment Setup Details 5.6.3. Orientation Result of Different Blocks 5.6.4. Matching Quality Analysis 6. Discussion 6.1. Descriptor Learning and Patch Based Image Matching 6.1.1. Parameter Study 6.1.2. Comparison to Related Works 6.2. Descriptor Distance Analysis 6.2.1. Translation 6.2.2. Rotation 6.2.3. Affine Shape Transformation 6.3. Feature based Image Matching 6.3.1. Parameter Study 6.3.2. Rotation Set 6.3.3. Affine Set 6.4. Image Orientation 7. Conclusion and Outlook Bibliography A. Affine Shape Adaptation Theory A.l. transformation of affine Gaussian scale-space A.2. Local affine distortion measurement A.3. More affine transformation
    In: Wissenschaftliche Arbeiten der Fachrichtung Geodäsie und Geoinformatik der Leibniz Universität Hannover
    Sprache: Englisch
    Schlagwort(e): Hochschulschrift
    Mehr zum Autor: Chen, Lin 1987-
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  • 9
    UID:
    kobvindex_GFZ1030123993
    Umfang: xxi, 197 Seiten , Illustrationen, Diagramme
    Inhalt: Earth's climate varies continuously across space and time, but humankind has witnessed only a small snapshot of its entire history, and instrumentally documented it for a mere 200 years. Our knowledge of past climate changes is therefore almost exclusively based on indirect proxy data, i.e. on indicators which are sensitive to changes in climatic variables and stored in environmental archives. Extracting the data from these archives allows retrieval of the information from earlier times. Obtaining accurate proxy information is a key means to test model predictions of the past climate, and only after such validation can the models be used to reliably forecast future changes in our warming world. The polar ice sheets of Greenland and Antarctica are one major climate archive, which record information about local air temperatures by means of the isotopic composition of the water molecules embedded in the ice. However, this temperature proxy is, as any indirect climate data, not a perfect recorder of past climatic variations. Apart from local air temperatures, a multitude of other processes affect the mean and variability of the isotopic data, which hinders their direct interpretation in terms of climate variations. This applies especially to regions with little annual accumulation of snow, such as the Antarctic Plateau. While these areas in principle allow for the extraction of isotope records reaching far back in time, a strong corruption of the temperature signal originally encoded in the isotopic data of the snow is expected. This dissertation uses observational isotope data from Antarctica, focussing especially on the East Antarctic low-accumulation area around the Kohnen Station ice-core drilling site, together with statistical and physical methods, to improve our understanding of the spatial and temporal isotope variability across different scales, and thus to enhance the applicability of the proxy for estimating past temperature variability. The presented results lead to a quantitative explanation of the local-scale (1–500 m) spatial variability in the form of a statistical noise model, and reveal the main source of the temporal variability to be the mixture of a climatic seasonal cycle in temperature and the effect of diffusional smoothing acting on temporally uncorrelated noise. These findings put significant limits on the representativity of single isotope records in terms of local air temperature, and impact the interpretation of apparent cyclicalities in the records. Furthermore, to extend the analyses to larger scales, the timescale-dependency of observed Holocene isotope variability is studied. This offers a deeper understanding of the nature of the variations, and is crucial for unravelling the embedded true temperature variability over a wide range of timescales.
    Anmerkung: Kumulative Dissertation , Dissertation Universität Potsdam 2018 , Contents: 1 General introduction. - 1.1 Challenges of isotope-based temperature reconstructions. - 1.2 Thesis overview. - 1.3 Author contributions. - 2 Theoretical background. - 2.1 The isotopic composition of firn and ice. - 2.1.1 Fractionation of water isotopologues. - 2.1.2 Relationship with temperature. - 2.1.3 Measuring of the isotopic composition. - 2.2 Processes within the firn column. - 2.2.1 The firn column of polar ice sheets. - 2.2.2 The density of firn. - 2.2.3 The temperature profile of firn. - 2.2.4 Vapour diffusion in firn. - 2.3 Internal climate variability. - 3 Regional climate signal vs.local noise: a two-dimensional view of water isotopes. - 3.1 Introduction. - 3.2 Data and methods. - 3.3 Results. - 3.3.1 Trench isotope records. - 3.3.2 Single-profile representativity. - 3.3.3 Mean trench profiles. - 3.3.4 Spatial correlation structure. - 3.3.5 Statistical noise model. - 3.4 Discussion. - 3.4.1 Local noise vs. regional climate signal. - 3.4.2 Representativity of isotope signals. - 3.4.3 Implications. - 3.5 Conclusions. - 3.6 Appendix A: Derivation of noise model. - 3.6.1 Definitions. - 3.6.2 Derivation of model correlations. - 3.6.3 Estimation of parameters. - 3.7 Appendix B: Noise level after diffusion. - 4 Constraints on post-depositional isotope modifications in east antarctic firn. - 4.1 Introduction. - 4.2 Data and methods. - 4.2.1 Sampling and measurements. - 4.2.2 Trench depth scale. - 4.2.3 Spatial variability of trench profiles. - 4.2.4 Quantification of downward advection, densification and diffusion. - 4.2.5 Statistical tests. - 4.3 Results. - 4.3.1 Comparison of T15 and T13 isotope data. - 4.3.2 Expected isotope profile changes. - 4.3.3 Temporal vs. spatial variability. - 4.4 Discussion. - 4.4.1 Densification, diffusion and stratigraphic noise. - 4.4.2 Additional post-depositional modifications. - 4.5 Conclusions. - 5 On the similarity and apparent cycles of isotope variations. - 5.1 Introduction. - 5.2 Data and Methods. - 5.2.1 Data. - 5.2.2 Spectral analysis. - 5.2.3 Rice’s formula. - 5.2.4 Cycle length and amplitude estimation. - 5.2.5 Model for vertical isotope profiles. - 5.3 Results. - 5.3.1 Spectral analysis of isotope profiles. - 5.3.2 Theoretical and observed cycle length. - 5.3.3 Illustrative examples. - 5.3.4 Depth dependency of cycle length. - 5.3.5 Simulated vs. observed isotope variations. - 5.4 Discussion and summary. - 5.5 Conclusions. - 5.6 Appendix A: Input sensitivity. - 5.7 Appendix B: Additional results. - 5.8 Appendix C: Spectral significance testing. - 6 Timescale-dependency of antarctic isotope variations. - 6.1 Introduction. - 6.2 Data and methods. - 6.2.1 DML and WAIS isotope records. - 6.2.2 Spectral model. - 6.2.3 Timescale-dependent signal-to-noise ratio. - 6.2.4 Effects of diffusion and time uncertainty. - 6.2.5 Present-day temperature decorrelation. - 6.3 Results. - 6.3.1 Illustration of model approach. - 6.3.2 DML and WAIS isotope variability. - 6.4 Discussion. - 6.4.1 Interpretation of noise spectra. - 6.4.2 Interpretation of signal spectra. - 6.4.3 Signal-to-noise ratios. - 6.4.4 Differences between DML and WAIS. - 6.5 Conclusions. - 7 Declining temperature variability from LGM to holocene. - 8 General discussion and conclusions. - 8.1 Short-scale spatial and temporal isotope variability. - 8.1.1 Local spatial variability. - 8.1.2 Seasonal to interannual variability. - 8.1.3 Spatial vs. temporal variability. - 8.2 Extension to longer scales. - 8.2.1 Spatial vs. temporal variability on interannual timescales. - 8.2.2 Holocene and longer timescales. - 8.3 Concluding remarks and outlook. - Bibliography. - A Methods to: declining temperature variability from lgm to holocene. - A.1 Temperature proxy data. - A.2 Model-based temperature and variability change. - A.3 Temperature recalibration of proxy records. - A.3.1 Recalibration of ice-core records. - A.3.2 Recalibration of marine records. - A.4 Variance and variance ratio estimation. - A.5 Noise correction. - A.5.1 Testing effect of noise correction. - A.6 Effect of ecological adaption and bioturbation. - A.7 Effect of proxy sampling locations. - B Layering of surface snow and firn: noise or seasonal signal?. - B.1 Introduction. - B.2 Materials and methods. - B.2.1 Firn-core density profiles. - B.2.2 Trench density profiles. - B.2.3 Dielectric profiling and density estimates. - B.2.4 Comparison of DEP and CT density. - B.2.5 Ion measurements. - B.3 Results. - B.3.1 2-D trench density data. - B.3.2 Spatial correlation structure. - B.3.3 Comparison of mean density, isotope and impurity profiles. - B.3.4 Spectral analysis of vertical density data. - B.4 Discussion. - B.4.1 Spatial variability. - B.4.2 Representativeness of single profiles. - B.4.3 Seasonal cycle in snow density. - B.4.4 Density layering in firn and impurities. - B.5 Conclusions. - Acknowledgements - Danksagung.
    Sprache: Englisch
    Schlagwort(e): Hochschulschrift
    Mehr zum Autor: Laepple, Thomas
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  • 10
    Buch
    Buch
    Hannover : Fachrichtung Geodäsie und Geoinformatik der Leibniz-Universität Hannover
    Dazugehörige Titel
    UID:
    kobvindex_GFZ1890123749
    Umfang: 207 Seiten , Illustrationen, Diagramme , 30 cm
    ISSN: 01741454
    Serie: Wissenschaftliche Arbeiten der Fachrichtung Geodäsie und Geoinformatik der Leibniz Universität Hannover Nr. 396
    Inhalt: With increasing urbanization, a well-functioning transport infrastructure that takes into account the needs of the society is becoming more and more important. In particular, a high proportion of motorized traffic can cause far-reaching problems that affect large parts of the urban population, such as traffic congestion or increased air pollution. To counteract this trend, an optimized distribution of traffic flows could improve the situation from a societal perspective. Since most routing decisions are made based on digital maps before the journey starts, clear and intuitive visualization is crucial for conveying the cartographic information to the traveler. While most existing services typically provide the most efficient routing options in terms of travel time, newer approaches attempt to guide drivers to societally favorable routes. These take into account societally relevant factors, which are referred to as scenarios in this thesis, and include environmental issues such as traffic congestion or air pollution. However, since such a societally favorable route is not necessarily efficient for the individual traveler, it is important to convince the traveler to choose a seemingly less efficient route. For this purpose, an automatic method for visualizing route maps is developed, which calculates societally favorable routes, and communicates them visually to the end user in such a way that the user would prefer to use them. For this communication, different visual variables of cartography are used, whose usage is adapted to the different scenarios and controlled by scenario-specific thresholds. Based on the goal of dynamic distribution of traffic flows, the proposed method recommends routes that are not necessarily the shortest or fastest, but rather those that seek to avoid unfavorable or hazardous paths or areas. The proposed design variants of route maps use a large variety of symbolization techniques; including classic visual variables of cartography such as color, size or pattern, but also more abstract methods that use cartographic generalization techniques.
    Inhalt: Mit zunehmender Verstädterung gewinnt eine gut funktionierende Verkehrsinfrastruktur, die den Bedürfnissen der Gesellschaft Rechnung trägt, immer mehr an Bedeutung. Insbesondere ein hoher Anteil an motorisiertem Verkehr kann weitreichende Probleme verursachen, die große Teile der Stadtbevölkerung betreffen, wie z.B. Verkehrsstaus oder erhöhte Luftverschmutzung. Um dieser Entwicklung entgegenzuwirken, könnte eine optimierte Verteilung der Verkehrsströme die Situation für die Gemeinschaft verbessern. Da die meisten Routing-Entscheidungen vor Reiseantritt auf der Grundlage digitaler Karten getroffen werden, ist eine klare und intuitive Visualisierung entscheidend für die Vermittlung kartografischer Informationen an den Reisenden. Während die meisten bestehenden Dienste in der Regel die effizientesten Routing-Optionen im Hinblick auf die Reisezeit bieten, versuchen neuere Ansätze, die Fahrer auf gesellschaftlich vorteilhafte Routen zu leiten. Diese berücksichtigen gesellschaftlich relevante Faktoren, die in dieser Arbeit als Szenarien bezeichnet werden. Darunter fallen Umweltprobleme wie Verkehrsstaus oder Luftverschmutzung. Da eine solche gesellschaftlich vorteilhafte Route für den einzelnen Reisenden jedoch nicht zwangsläufig effizient ist, ist es wichtig, den Reisenden davon zu überzeugen, eine scheinbar weniger effiziente Route zu wählen. Dazu wird im Rahmen der Arbeit ein automatisches Verfahren zur Visualisierung von Routenkarten entwickelt, welches gesellschaftlich vorteilhafte Routen berechnet und diese so visuell dem Endnutzer kommuniziert, dass dieser sie bevorzugt nutzen möchte. Für diese Kommunikation kommen verschiedene visuelle Variablen der Kartographie zum Einsatz, deren Verwendung auf die verschiedenen Szenarien angepasst sind und über Szenario-spezifische Schwellwerte gesteuert werden. Basierend auf dem Ziel einer dynamischen Verteilung der Verkehrsströme empfiehlt die vorgeschlagene Methode Routen, die nicht unbedingt die kürzesten oder schnellsten sind, sondern vielmehr solche Routen, die ungünstige oder gefährliche Wege oder Bereiche zu vermeiden versuchen. Die vorgeschlagenen Designvarianten von Routenkarten nutzen eine Vielzahl von Symbolisierungstechniken; darunter klassische, visuelle Variablen der Kartographie wie Farbe, Größe oder Muster, aber auch abstraktere Methoden, die kartographische Generalisierungstechniken verwenden.
    Anmerkung: Dissertation, Gottfried Wilhelm Leibniz Universität Hannover, 2024 , 1 Introduction 1.1 Motivation and problem statemen 1.2 Research objectives and key hypotheses 1.3 Structure of the thesis 2 Theoretical background 2.1 Visual communication with maps 2.2 Route choice factors 2.3 Cartographic symbolization 2.3.1 Visual variables 2.3.1.1 Levels of organization of visual variables 2.3.1.2 ‘Original visual variables’ as proposed by Bertin 2.3.1.3 Visual variable additions 2.3.1.4 Experimental visual variables 2.3.1.5 Conjunctions of visual variables 2.3.1.6 Dynamic visual variables 2.3.2 Cartographic design tools 2.3.3 Visual metaphor 2.3.4 Cartographic generalization and map abstraction 2.3.4.1 Insights from cognitive mapping research 2.3.4.2 Elementary processes of cartographic generalization 2.3.4.3 Cartographic generalization algorithms 2.4 Nudging 2.5 Maps and emotions 2.5.1 Classifying emotions 2.5.2 Instruments for measuring emotions 2.6 Map-related usability testing 2.6.1 Types of user study designs 2.6.2 Statistical analysis of user survey results 2.6.2.1 Descriptive statistics 2.6.2.2 Basic statistical tests and models 2.6.2.3 Sophisticated statistical models for non-parametric data 2.6.2.4 Statistical significance 2.6.2.5 Main effect and post-hoc tests 2.6.2.6 Effect sizes 2.6.2.7 Inter-rater reliability 2.6.2.8 Software for statistical analysis 3 Related work 3.1 Visual route communication using visual variables 3.2 Cartographic generalization for route map communication 3.3 Map-based visualization of environmental hazards 3.4 The role of emotions in map-based communication 3.5 Research gap addressed in this thesis 4 Framework and data preprocessing 4.1 Research framework 4.2 Scenarios 4.2.1 Traffic 4.2.2 Air quality 4.3 Routing 4.3.1 Data basis for route calculation 4.3.2 Calculation of favorable routes 4.3.3 Routing results 5 Visualization concepts for designing ‘social’ route maps 5.1 Map symbols 5.2 Data-based calculation of graphical differences in symbolization 5.3 Visually modified geometry 5.3.1 Line distortion and simplification 5.3.1.1 Line distortion 5.3.1.2 Line simplification 5.3.1.3 Combined approach 5.3.1.4 Topological issues and further adaptions 5.3.2 Length distortion using PUSH 5.3.3 Application to discrete areas: Geometric deformation of risk zones 5.4 Examples of route map design variants 5.4.1 Design variants for symbolizing route favorability 5.4.2 Application of the methodology to discrete objects 6 Usability evaluation of proposed route map design variants 6.1 User study 1: Subjective usability – Attractiveness, intuitiveness and suitability of design variants 6.1.1 Sub-hypotheses 6.1.2 Study design 6.1.3 Participants 6.1.4 Results – Intuitiveness and suitability 6.1.5 Results – Attractiveness 6.1.6 Discussion and conclusion – User study 1 6.2 User study 2: Objective usability – Effectiveness of line objects for influencing route choice in the traffic scenario 6.2.1 Common design specifications in user study 2 and user study 3 6.2.2 Sub-hypotheses 6.2.3 Route maps 6.2.4 Design variants 6.2.5 Calculation of graphical differences among design variants and modification intensities 6.2.6 Study design 6.2.7 Participants 6.2.8 Results – User study 2 6.2.8.1 Influencing route choice 6.2.8.2 Decision time 6.2.8.3 Route characteristics 6.2.8.4 Map use habits 6.2.9 Discussion – User study 2 6.2.9.1 Effectiveness for influencing route choice behavior 6.2.9.2 The role of time during decision making 6.2.9.3 Relations between route choice and route characteristics 6.2.9.4 Transferability of the findings to real world applications 6.2.10 Conclusion – User study 2 6.2.11 Modification of line objects using dynamic visual variables 6.3 User study 3: Objective usability – The impact of visual communication and emotions on route choice decision making using modification of line and area objects 6.3.1 Sub-hypotheses 6.3.2 Route maps 6.3.3 Design variants 6.3.3.1 Line modifications 6.3.3.2 Area modifications 6.3.3.3 Line + area modifications 6.3.4 Study design 6.3.5 Participants 6.3.6 Results – User study 3 6.3.6.1 H1: Shift towards choosing the societally favorable route 6.3.6.2 H2: Scenario-dependent willingness to adapt route choice behavior 6.3.6.3 H3: Scenario-dependent effectiveness of symbolization dimensions 6.3.6.4 H4: Influence of combining multiple visual variables in one representation 6.3.6.5 H5: Emotional responses to map symbols 6.3.6.6 H6: Effect of emotions on route choice decision making 6.3.6.7 Helpfulness of map visualizations 6.3.6.8 Route choice strategies 6.3.6.9 Text-based sentiment analysis 6.3.6.10 Suitability of visualizations 6.3.6.11 Further factors influencing route choice 6.3.7 Discussion – User study 3 6.3.7.1 Influence of different design variants on route choice 6.3.7.2 The effect of emotions on route choice 6.3.7.3 Limitations of the study design 6.3.7.4 Outlook 6.3.8 Conclusion – User study 3 7 Interactive web-based visualization of route maps 7.1 Application architecture 7.2 User interface and functionalities 7.3 User assessment to usability of the application 7.4 Usability test – Results 7.5 Limitations and future adaptions 8 Implications of the findings 8.1 Agreement with key hypotheses 8.2 Assessment regarding successful design variants for influencing route choice towards a societally favorable route 8.3 Limitations and challenges 8.4 Suggestions for future research 8.5 Summary and contribution of the dissertation Appendix Bibliography Curriculum vitae Acknowledgments
    In: Wissenschaftliche Arbeiten der Fachrichtung Geodäsie und Geoinformatik der Leibniz Universität Hannover, Nr. 396
    Weitere Ausg.: eng
    Sprache: Englisch
    Schlagwort(e): Hochschulschrift
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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