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  • 1
    Publication Date: 2024-05-29
    Description: Media inform the public, thereby influencing societal debates and political decisions. Despite climate change’s importance, drivers of media attention to climate change remain differently understood. Here we assess how different sociopolitical and extreme weather events affect climate change media coverage, both immediately and in the weeks following the event. To this end, we construct a data set of over 90,000 climate change articles published in nine major German newspapers over the past three decades and apply fixed effects panel regressions to control for confounders. We find that United Nations Climate Change Conferences affect coverage most strongly and most persistently. Climate protests incite climate coverage that extends well beyond the reporting on the event itself, whereas many articles on weather extremes do not mention climate change. The influence of all events has risen over time, increasing the media prominence of climate change.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 2
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    Chichester, [England] : Wiley
    Call number: 9781444328479 (e-book)
    Type of Medium: 12
    Pages: 1 Online-Ressource (XIII, 768 Seiten) , Illustrationen
    Edition: Second edition
    ISBN: 9781444328479 (e-book) , 978-1-4443-2847-9
    Language: English
    Note: Contents Contents Preface Acknowledgements Part 1: Making Sediment Introduction Clastic sediment as a chemical and physical breakdown product 1.1 Introduction: clastic sediments—'accidents' of weathering 1.2 Silicate minerals and chemical weathering 1.3 Solute flux: rates and mechanisms of silicate chemical weathering 1.4 Physical weathering 1.5 Soils as valves and filters for the natural landscape 1.6 Links between soil age, chemical weathering and weathered-rock removal 1.7 Provenance: siliciclastic sediment-sourcing Further reading 2 Carbonate, siliceous, iron-rich and evaporite sediments 2.1 Marine vs. freshwater chemical composition and fluxes 2.2 The calcium carbonate system in the oceans 2.3 Ooid carbonate grains 2.4 Carbonate grains from marine plants and animals 2.5 Carbonate muds, oozes and chalks 2.6 Other carbonate grains of biological origins 2.7 Organic productivity, sea-level and atmospheric controls of biogenic CaCO3 deposition rates 2.8 CaCO3 dissolution in the deep ocean and the oceanic CaCO3 compensation mechanism 2.9 The carbonate system on land 2.10 Evaporite salts and their inorganic precipitation as sediment 2.11 Silica and pelagic plankton 2.12 Iron minerals and biomineralizers 2.13 Desert varnish 2.14 Phosphates 2.15 Primary microbial-induced sediments: algal mats and stromatolites Further reading 3 Sediment grain properties 3.1 General 3.2 Grain size 3.3 Grain-size distributions 3.4 Grain shape and form 3.5 Bulk properties of grain aggregates Further reading Part 2: Moving Fluid Introduction 4 Fluid basics 4.1 Material properties of fluids 4.2 Fluid kinematics 4.3 Fluid continuity with constant density 4.4 Fluid dynamics 4.5 Energy, mechanical work and power Further reading 5 Types of fluid motion 5.1 Osborne Reynolds and flow types 5.2 The distribution of velocity in viscous flows: the boundary layer 5.3 Turbulent flows 5.4 The structure of turbulent shear flows 5.5 Shear flow instabilities, flow separation and secondary currents 5.6 Subcritical and supercritical flows: the Froude number and hydraulic jumps 5.7 Stratified flow generally 5.8 Water waves 5.9 Tidal flow—long-period waves Further reading Part 3: Transporting Sediment Introduction 6 Sediment in fluid and fluid flow—general 6.1 Fall of grains through stationary fluids 6.2 Natural flows carrying particulate material are complex 6.3 Fluids as transporting machines 6.4 Initiation of grain motion 6.5 Paths of grain motion 6.6 Categories of transported sediment 6.7 Some contrasts between wind and water flows 6.8 Cohesive sediment transport and erosion 6.9 A warning: nonequilibrium effects dominate natural sediment transport systems 6.10 Steady state, deposition or erosion: the sediment continuity equation and competence vs. capacity Further reading 7 Bedforms and sedimentary structures in flows and under waves 7.1 Trinity of interaction: turbulent flow, sediment transport and bedform development 7.2 Water-flow bedforms 7.3 Bedform phase diagrams for water flows 7.4 Water flow erosional bedforms on cohesive beds 7.5 Water wave bedforms 7.6 Combined flows: wave-current ripples and hummocky cross-stratification 7.7 Bedforms and structures formed by atmospheric flows Further reading 8 Sediment gravity flows and their deposits 8.1 Introduction 8.2 Granular flows 8.3 Debris flows 8.4 Turbidity flows 8.5 Turbidite evidence for downslope transformation from turbidity to debris flows Further reading 9 Liquefaction, fluidization and sliding sediment deformation 9.1 Liquefaction 9.2 Sedimentary structures formed by and during liquefaction 9.3 Submarine landslides, growth faults and slumps 9.4 Desiccation and synaeresis shrinkage structures Further reading Part 4: Major External Controls on Sedimentation and Sedimentary Environments Introduction 10 Major external controls on sedimentation 10.1 Climate 10.2 Global climates: a summary 10.3 Sea-level changes 10.4 Tectonics 10.5 Sediment yield, denudation rate and the sedimentary record Further reading Part 5: Continental Sedimentary Environments Introduction 11 Rivers 11.1 Introduction 11.2 River networks, hydrographs,patterns and long profiles 11.3 Channel form 11.4 Channel sediment transport processes, bedforms and internal structures 11.5 The floodplain 11.6 Channel belts, alluvial ridges and avulsion 11.7 River channel changes, adjustable variables and equilibrium 11.8 Alluvial architecture: product of complex responses 11.9 Alluvial architecture: scale, controls and time Further reading 12 Subaerial Fans: Alluvial and Colluvial 12.1 Introduction 12.2 Controls on the size (area) and gradient of fans 12.3 Physical processes on alluvial fans 12.4 Debris-flow-dominated alluvial fans 12.5 Stream-flow-dominated alluvial fans 12.6 Recognition of ancient alluvial fans and talus cones Further reading 13 Aeolian Sediments in Low-Latitude Deserts 13.1 Introduction 13.2 Aeolian system state 13.3 Physical processes and erg formation 13.4 Erg margins and interbedform areas 13.5 Erg and draa evolution and sedimentary architecture 13.6 Erg construction, stasis and destruction: climate and sea-level controls 13.7 Ancient desert facies Further reading 14 Lakes 14.1 Introduction 14.2 Lake stratification 14.3 Clastic input by rivers and the effect of turbidity currents 14.4 Wind-forced physical processes 14.5 Temperate lake chemical processes and cycles 14.6 Saline lake chemical processes and cycles 14.7 Biological processes and cycles 14.8 Modern temperate lakes and their sedimentary facies 14.9 Lakes in the East African rifts 14.10 Lake Baikal 14.11 The succession of facies as lakes evolve 14.12 Ancient lake facies Further reading 15 Ice 15.1 Introduction 15.2 Physical processes of ice flow 15.3 Glacier flow, basal lubrication and surges 15.4 Sediment transport, erosion and deposition by flowing ice 15.5 Glacigenic sediment: nomenclature and classification 15.6 Quaternary and modern glacial environments and facies 15.7 Ice-produced glacigenic erosion and depositional facies on land and in the periglacial realm 15.8 Glaciofluvial processes on land at and within the ice-front 15.9 Glacimarine environments 15.10 Glacilacustrine environments 15.11 Glacial facies in the pre-Quaternary geological record: case of Cenozoic Antarctica Further reading Part 6: Marine Sedimentary Environments Introduction 16. Estuaries 16.1 Introduction 16.2 Estuarine dynamics 16.3 Modern estuarine morphology and sedimentary environments 16.4 Estuaries and sequence stratigraphy Further reading 17. River and Fan Deltas 17.1 Introduction to river deltas 17.2 Basic physical processes and sedimentation at the river delta front 17.3 Mass movements and slope failure on the subaqueous delta 17.4 Organic deposition in river deltas 17.5 River delta case histories 17.6 River deltas and sea-level change 17.7 Ancient river delta deposits 17.8 Fan deltas Further reading 18. Linear Siliciclastic Shorelines 18.1 Introduction 18.2 Beach processes and sedimentation 18.3 Barrier-inlet-spit systems and their deposits 18.4 Tidal flats, salt marsh and chenier ridges 18.5 Ancient clastic shoreline facies Further reading 19 Siliciclastic Shelves 19.1 Introduction: shelf sinks and lowstand bypass 19.2 Shelf water dynamics 19.3 Holocene highstand shelf sediments: general 19.4 Tide-dominated, low river input, highstand shelves 19.5 Tide-dominated, high river input, highstand shelves 19.6 Weather-dominated highstand shelves Further reading 20 Calcium-carbonate-evaporite Shorelines, Shelves and Basins 20.1 Introduction: calcium carbonate 'nurseries' and their consequences 20.2 Arid carbonate tidal flats, lagoons and evaporite sabkhas 20.3 Humid carbonate tidal flats and marshes 20.4 Lagoons and bays 20.5 Tidal delta and margin-spillover carbonate tidal sands 20.6 Open-shelf carbonate ramps 20.7 Platform margin reefs and carbonate build-ups 20.8 Platform margin slopes and basins 20.9 Carbonate sediments, cycles and sea-level change 20.10 Displacement and destruction of carbonate environments: silicicl
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  • 3
    Publication Date: 2024-02-21
    Description: As network infrastructures with 10 Gb/s bandwidth and beyond have become pervasive and as cost advantages of large commodity-machine clusters continue to increase, research and industry strive to exploit the available processing performance for large-scale database processing tasks. In this work we look at the use of high-speed networks for distributed join processing. We propose Data Roundabout as alight weight transport layer that uses Remote Direct Memory Access (RDMA) to gain access to the throughput opportunities in modern networks. The essence of Data Roundabout is a ring shaped network in which each host stores one portion of a large database instance. We leverage the available bandwidth to (continuously) pump data through the high-speed network. Based on Data Roundabout, we demonstrate cyclo-join, which exploits the cycling flow of data to execute distributed joins. The study uses different join algorithms (hash join and sort-merge join) to expose the pitfalls and the advantages of each algorithm in the data cycling arena. The experiments show the potential of a large distributed main-memory cache glued together with RDMA into a novel distributed database architecture.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 4
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    In:  ACM Transactions on Database Systems
    Publication Date: 2024-02-21
    Description: A grand challenge of distributed query processing is to devise a self-organizing architecture which exploits all hardware resources optimally to manage the database hot set, minimize query response time, and maximize throughput without single point global coordination. The Data Cyclotron architecture [Goncalves and Kersten 2010] addresses this challenge using turbulent data movement through a storage ring built from distributed main memory and capitalizing on the functionality offered by modern remote-DMA network facilities. Queries assigned to individual nodes interact with the storage ring by picking up data fragments, which are continuously flowing around, that is, the hot set. The storage ring is steered by the Level Of Interest (LOI) attached to each data fragment, which represents the cumulative query interest as it passes around the ring multiple times. A fragment with LOI below a given threshold, inversely proportional to the ring load, is pulled out to free up resources. This threshold is dynamically adjusted in a fully distributed manner based on ring characteristics and locally observed query behavior. It optimizes resource utilization by keeping the average data access latency low. The approach is illustrated using an extensive and validated simulation study. The results underpin the fragment hot set management robustness in turbulent workload scenarios. A fully functional prototype of the proposed architecture has been implemented using modest extensions to MonetDB and runs within a multirack cluster equipped with Infiniband. Extensive experimentation using both microbenchmarks and high-volume workloads based on TPC-H demonstrates its feasibility. The Data Cyclotron architecture and experiments open a new vista for modern distributed database architectures with a plethora of new research challenges.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 5
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    In:  ACM Transactions on Database Systems
    Publication Date: 2024-02-21
    Description: Automatic recycling of intermediate results to improve both query response time and throughput is a grand challenge for state-of-the-art databases. Tuples are loaded and streamed through a tuple-at-a-time processing pipeline, avoiding materialization of intermediates as much as possible. This limits the opportunities for reuse of overlapping computations to DBA-defined materialized views and function/result cache tuning. In contrast, the operator-at-a-time execution paradigm produces fully materialized results in each step of the query plan. To avoid resource contention, these intermediates are evicted as soon as possible. In this article we study an architecture that harvests the byproducts of the operator-at-a-time paradigm in a column-store system using a lightweight mechanism, the recycler. The key challenge then becomes the selection of the policies to admit intermediates to the resource pool, to determine their retention period, and devise the eviction strategy when facing resource limitations. The proposed recycling architecture has been implemented in an open-source system. An experimental analysis against the TPC-H ad-hoc decision support benchmark and a complex, real-world application (SkyServer) demonstrates its effectiveness in terms of self-organizing behavior and its significant performance gains. The results indicate the potentials of recycling intermediates and charts a route for further development of database kernels.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 6
    Monograph available for loan
    Monograph available for loan
    Cambridge, Mass. : Belknap Press
    Call number: RIFS 23.95556
    Type of Medium: Monograph available for loan
    Pages: XVI, 622 Seiten , Ill.
    Edition: 1st paperback ed.
    ISBN: 9780674292130
    Uniform Title: Chute du ciel
    Language: English
    Branch Library: RIFS Library
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  • 7
    Monograph available for loan
    Monograph available for loan
    London : Routledge
    Call number: RIFS 23.95609
    Type of Medium: Monograph available for loan
    Pages: xii, 163 Seiten , Illustrationen, Diagramme
    ISBN: 041556722X , 9780415567237 , 9780415567220
    Language: English
    Branch Library: RIFS Library
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  • 8
    Monograph available for loan
    Monograph available for loan
    Edinburgh : Edinburgh University Press
    Call number: RIFS 23.95612
    Type of Medium: Monograph available for loan
    Pages: vii, 256 Seiten
    Edition: Second edition
    ISBN: 9780748691135
    Language: English
    Branch Library: RIFS Library
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  • 9
    Monograph available for loan
    Monograph available for loan
    Cambridge, Mass. [u.a.] : MIT Press
    Call number: RIFS 23.95560
    Type of Medium: Monograph available for loan
    Pages: XIX, 279 S. , Ill. , 23 cm
    ISBN: 0262515857 , 0262015447 , 9780262515856 , 9780262015448
    Language: English
    Branch Library: RIFS Library
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  • 10
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Routledge
    Call number: RIFS 23.95542
    Type of Medium: Monograph available for loan
    Pages: XIV, 203 S. , graph. Darst., Kt. , 24 cm
    Edition: 1. publ.
    ISBN: 0415477506 , 0415477514 , 9780415477505 , 9780415477512
    Language: English
    Branch Library: RIFS Library
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  • 11
    Call number: RIFS 23.95498
    Description / Table of Contents: The essays in this volume address the displacement of natural and cultural heritage caused by disasters, whether they be dramatic natural impacts or terrible events unleashed by humankind, including holocaust and genocide. Disasters can be natural or human-made, rapid or slow, great or small, yet the impact is effectively the same; nature, people and cultural heritage are displaced or lost. Yet while heritage and place are at risk from disasters, in time,sites of suffering are sometimes reframed as sites of memory; through this different lens these "difficult" places become heritage sites that attract tourists. Ranging widely chronologically and geographically, the contributors explore the impact of disasters, trauma and suffering on heritage and sense of place, in both theory and practice.
    Type of Medium: Monograph available for loan
    Pages: xx, 337 pages , Illustrationen
    Edition: Paperback ed.
    ISBN: 9781843839637 , 9781783274307
    Series Statement: Heritage matters
    Language: English
    Branch Library: RIFS Library
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  • 12
    Call number: 9783034803960 (e-book)
    Type of Medium: 12
    Pages: 1 Online-Ressource (XI, 220 Seiten) , Illustrationen
    ISBN: 9783034803960 (e-book) , 978-3-0348-0396-0
    Language: English
    Note: Contents 1 High elevation treelines 1.1 The task 1.2 Previous works 2 Definitions and conventions 2.1 The life form ‘tree’ 2.2 Lines and transitions 2.3 Limitation, stress and disturbance 2.4 Altitude-related and other environmental drivers 2.5 Treeline nomenclature 3 Treeline patterns 3.1 Treeline taxa 3.2 The summit syndrome and other treeline depressions 3.3 Mass elevation effect 3.4 Treeline elevation 3.5 Time matters 3.6 Forest structure near treeline 4 Treeline climate 4.1 Specific aspects of treeline climatology 4.2 Criteria to define temperature regimes at treeline 4.3 Treeline temperatures in different bioclimatic regions 4.3.1 Subarctic and boreal zone (45–68° N) 4.3.2 Cool temperate zone (45–47° N, 44° S) 4.3.3 Warm temperate zone (28–42° N, 36° S) 4.3.4 Subtropical zone (19° S, 19° N) 4.3.5 Equatorial tropics (6° N to 3° S) 4.3.6 Mediterranean ‘treelines’ (38–42° N) 4.3.7 The Nothofagus and Metrosideros case 4.3.8 Treeline temperatures across bioclimatic zones 4.4 Seedbed and branch temperatures 4.5 Whole forest temperatures 5 Global mountain statistics based on treeline elevation 5.1 Mountain geostatistics 5.2 Elevational belts 5.3 Global treeline ecotones 6 Structure and stature of treeline trees 6.1 Foliage properties 6.2 Wood properties 6.3 Bark properties 6.4 Root traits 6.5 Tree stature 6.6 Dry matter allocation in treeline trees 7 Growth and development 7.1 Tree growth near the treeline 7.1.1 In situ growth of seedlings 7.1.2 In situ growth of saplings and adult trees 7.2 Xylogenesis at the treeline 7.2.1 In situ cambial activity 7.2.2 Apical growth dynamics 7.3 Root growth 7.4 Phenology at the treeline 8 Evolutionary adjustments to life at the treeline 8.1 Phylogenetic selection 8.2 Genotypic responses of growth and development 8.3 Genotypic responses of physiological traits 9 Reproduction, early life stages and tree demography 9.1 Amount and quality of seeds at high elevation 9.2 Germination, seedling and sapling stage 9.3 Tree demography at the treeline 10 Freezing and other forms of stress 10.1 Stress at the treeline in a fitness context 10.2 Mechanisms and principles of freezing resistance 10.3 Freezing resistance in treeline trees 10.4 Other forms of stress at the treeline 10.4.1 Freeze-thaw cycles and hydraulic failure 10.4.2 Winter desiccation 11 Water, nutrient and carbon relations 11.1 Tree water relations during the growing season 11.2 Nutrient relations 11.3 Carbon relations 12 Treeline formation - currently, in the past and in the future 12.1 Causes of current treelines 12.2 Treelines in the recent past 12.3 Treelines in the distant past (Holocene) 12.4 Treelines in the future References Subject Index Taxonomic Index
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  • 13
    Call number: AWI G6-23-95368
    Type of Medium: Monograph available for loan
    Pages: XIX, 1004 Seiten , Illustrationen
    ISBN: 9780891189602 , 978-0-891-18960-2 , 0891189602
    ISSN: 2163-5804 , 1047-4986
    Series Statement: Soil Science Society of America book series 10
    Language: English
    Note: Contents Foreword Preface Contributors Chapter 1 Issues of Sampling Design in Wetlands / Monica Rivas Casado, Ron Corstanje, Pat Bellamy, and Ben Marchant DESIGN-BASED SAMPLING APPROACHES MODEL-BASED SAMPLING APPROACHES Chapter 2 Soil and Sediment Sampling of Inundated Environments / Todd Z. Osborne and R.D. DeLaune SAMPLING IN INUNDATED ENVIRONMENTS: SAMPLING PLAN AND GENERAL CONSIDERATIONS SAMPLING METHODS FOR INUNDATION DEPTHS LESS THAN 1.5 METERS SAMPLING METHODS FOR INUNDATION DEPTHS GREATER THAN 1.5 METERS SPECIAL CONDITIONS OR CONSIDERATIONS Chapter 3 Physicochemical Characterization of Wetland Soils / K.R. Reddy, M.W. Clark, R.D. DeLaune, and M. Kongchum SOIL SAMPLING PHYSICOCHEMICAL PROPERTIES CONCLUSIONS Chapter 4 Soil Pore Water Sampling Methods / M.M. Fisher and K.R. Reddy TECHNIQUES FOR SAMPLING SOIL PORE WATER SAMPLE HANDLING CONSIDERATIONS SAMPLING PORE WATER GASES SUMMARY Chapter 5 Reduction–Oxidation Potential and Oxygen / J. Patrick Megonigal and Martin Rabenhorst REDOX POTENTIAL THEORY OXYGEN MEASUREMENT WITH DIFFUSION CHAMBERS REDOX MEASUREMENT Chapter 6 Determination of Dissolved Oxygen, Hydrogen Sulfide, Iron(II), and Manganese(II) in Wetland Pore Waters / George W. Luther III and Andrew S. Madison EXPERIMENTAL PRINCIPLES OF ELECTRODE FABRICATION EXPERIMENTAL PRINCIPLES OF WORKING ELECTRODE CALIBRATIONS PROCEDURES FOR MICROPROFILING SUMMARY Chapter 7 Soil Redox Potential and pH Controllers / Kewei Yu and Jörg Rinklebe REDOX POTENTIAL AND pH CONTROL MODIFICATIONS AN AUTOMATED BIOGEOCHEMICAL MICROCOSM SYSTEM APPLICATIONS Chapter 8 Morphological Methods to Characterize Hydric Soils / M.J. Vepraskas EQUIPMENT METHODS AND TECHNIQUES FOR DESCRIBING HYDRIC SOILS FIELD TEST TO ASSESS SOIL MATERIAL TYPE IDENTIFYING HYDRIC SOIL FIELD INDICATORS Chapter 9 Emergent Macrophyte Biomass Production / Christopher Craft SAMPLING CONSIDERATIONS INDIRECT METHODS DIRECT METHODS EMERGING METHODS Chapter 10 Photosynthetic Measurements in Wetlands / S.R. Pezeshki OXYGEN EXCHANGE MEASUREMENT TECHNIQUE CARBON ISOTOPE TECHNIQUE MICROMETEOROLOGICAL TECHNIQUE CHLOROPHYLL FLUORESCENCE METHOD PHOTOSYNTHETIC MEASUREMENTS USING CHAMBERS SUMMARY Chapter 11 Gas Transport and Exchange through Wetland Plant Aerenchyma / Brian K. Sorrell and Hans Brix GENERAL PRINCIPLES EXPERIMENTAL PRINCIPLES LABORATORY AND GLASSHOUSE CHAMBERS MODELING APPROACHES Chapter 12 A Primer on Sampling Plant Communities in Wetlands / Curtis J. Richardson and Ryan S. King OVERVIEW OF SAMPLING PLANT POPULATIONS AND COMMUNITIES SAMPLE SIZE PLANT SAMPLING APPROACHES RAPID ASSESSMENT APPROACHES TO ESTIMATE PLANT ABUNDANCE AND COVER PERCENTAGE PLANT SAMPLING METHODS AND CALCULATION PROCEDURES ANALYSIS OF DATA COMPARISON OF PLANT COMMUNITIES SUGGESTIONS FOR DEVELOPING A PLANT SAMPLING PROGRAM APPENDIX Chapter 13 Plant Productivity—Bottomland Hardwood Forests / William H. Conner and Julia A. Cherry ABOVEGROUND PRODUCTIVITY BELOWGROUND PRODUCTIVITY Chapter 14 Current Methods to Evaluate Net Primary Production and Carbon Budgets in Mangrove Forests / Victor H. Rivera-Monroy, Edward Castañeda-Moya, Jordan G. Barr, Vic Engel, Jose D. Fuentes, Tiffany G. Troxler, Robert R. Twilley, Steven Bouillon, Thomas J. Smith III, and Thomas L. O’Halloran CURRENT METHODS TO ESTIMATE NET PRIMARY PRODUCTIVITY COMPARING MANGROVE NET PRIMARY PRODUCTION ESTIMATES TO WHOLE-FOREST CARBON FLUX MEASUREMENTS SUMMARY AND FUTURE RESEARCH DIRECTIONS APPENDIX Chapter 15 Characterization of Wetland Soil Organic Matter / Robert L. Cook and Thomas S. Bianchi SAMPLE TREATMENT AND PROCESSING SPECTROSCOPIC CHARACTERIZATION BULK ELEMENTAL AND CHEMICAL BIOMARKER ANALYSES SUMMARY Chapter 16 Dissolved Organic Matter / Robert G. Qualls EQUIPMENT AND INSTRUMENTATION MATERIALS AND REAGENTS SAMPLE PREPARATION PROCEDURES CONCLUSIONS Chapter 17 Soil Microbial Biomass and Phospholipid Fatty Acids / Jörg Rinklebe and Uwe Langer THE SUBSTRATE-INDUCED RESPIRATION METHOD PHOSPHOLIPID FATTY ACIDS ESTIMATES OF MICROBIAL BIOMASS SUMMARY Chapter 18 Molecular Genetic Analysis of Wetland Soils / Hee-Sung Bae and Andrew V. Ogram DNA EXTRACTION QUANTITATIVE POLYMERASE CHAIN REACTION POLYMERASE CHAIN REACTION BASED MOLECULAR CLONING Chapter 19 Enzyme Activities / Hojeong Kang, Seon-Young Kim, and Chris Freeman EQUIPMENT AND INSTRUMENTATION MATERIALS AND REAGENTS SAMPLE PREPARATION PROCEDURE CALCULATION SUMMARY Chapter 20 Organic Matter Mineralization and Decomposition / Scott D. Bridgham and Rongzhong Ye LITTER DECOMPOSITION DECOMPOSITION OF STANDARD SUBSTRATES SOIL HETEROTROPHIC RESPIRATION PHOTODEGRADATION Chapter 21 Methanogenesis and Methane Oxidation in Wetland Soils / Kanika S. Inglett, Jeffery P. Chanton, and Patrick W. Inglett EXPERIMENTAL METHANE MEASUREMENTS ISOTOPIC MEASUREMENTS OF METHANE Chapter 22 Greenhouse Gas Emission by Static Chamber and Eddy Flux Methods / Kewei Yu, April Hiscox, and R.D. DeLaune STATIC CHAMBER MEASUREMENT EDDY COVARIANCE MEASUREMENT SUMMARY Chapter 23 Characterization of Organic Nitrogen in Wetlands / C.M. VanZomeren, H. Knicker, W.T. Cooper, and K.R. Reddy CHEMICAL FRACTIONATION OF SOIL ORGANIC NITROGEN CHLOROFORM FUMIGATION METHOD NUCLEAR RESONANCE SPECTROSCOPY MASS SPECTROMETRY OF ORGANIC NITROGEN CONCLUSIONS Chapter 24 Measurements of Nitrogen Mineralization Potential in Wetland Soils / Eric D. Roy and John R. White POTENTIALLY MINERALIZABLE NITROGEN SUBSTRATE-INDUCED NITROGEN MINERALIZATION LIMITATIONS SUMMARY Chapter 25 Wind Tunnel Method for Measurement of Ammonia Volatilization / M.E. Poach, K.S. Ro, and P.G. Hunt EQUIPMENT AND INSTRUMENTATION MATERIALS AND REAGENTS SAMPLE PREPARATION PROCEDURE SAMPLE ANALYSIS CALCULATION STATISTICAL ANALYSIS QUALITY ASSURANCE SUMMARY Chapter 26 Ammonium Oxidation in Wetland Soils / K.S. Inglett, A.V. Ogram, and K.R. Reddy AEROBIC AMMONIUM OXIDATION (NITRIFICATION) ANAEROBIC AMMONIUM OXIDATION (ANAMMOX) METHODS FOR ASSESSING AEROBIC AMMONIUM OXIDATION (NITRIFICATION) METHODS FOR ASSESSING ANAEROBIC AMMONIUM OXIDATION (ANAMMOX) POTENTIAL MOLECULAR METHODS FOR ASSESSING AMMONIUM OXDIATION IN WETLAND SOILS SUMMARY Chapter 27 Denitrification Measurement Using Membrane Inlet Mass Spectrometry / Patrick W. Inglett, Todd M. Kana, and Soonmo An GENERAL PRINCIPLES EXPERIMENTAL PRINCIPLES ISOTOPE PAIRING BY THE MIMS METHOD SUMMARY Chapter 28 Nitrate Reduction, Denitrification, and Dissimilatory Nitrate Reduction to Ammonium in Wetland Sediments / Amy J. Burgin, Stephen K. Hamilton, Wayne S. Gardner, and Mark J. McCarthy EQUIPMENT AND INSTRUMENTATION MATERIALS AND REAGENTS PROCEDURES SAMPLE PREPARATION CALCULATIONS Chapter 29 System-Level Denitrification Measurement Based on Dissolved Gas Equilibration Theory and Membrane Inlet Mass Spectrometry / Andrew Laursen and Patrick W. Inglett GENERAL THEORY EXPERIMENTAL PRINCIPLES CALCULATIONS DISCUSSION AND LIMITATIONS SUMMARY Chapter 30 Biogeochemical Nitrogen Cycling in Wetland Ecosystems: Nitrogen-15 Isotope Techniques / Dries Huygens, Mark Trimmer, Tobias Rütting, Christoph Müller, Catherine M. Heppell, Katrina Lansdown, and Pascal Boeckx EXPERIMENTAL STUDY SETUPS ISOTOPE PAIRING AND REVISED ISOTOPE PAIRING TECHNIQUES ISOTOPE DILUTION AND TRACING TECHNIQUES Chapter 31 Biological Dinitrogen Fixation / Patrick W. Inglett ACETYLENE REDUCTION DINITROGEN-15 INCORPORATION SUMMARY Chapter 32 Methods for Soil Phosphorus Characterization and Analysis of Wetland Soils / Curtis J. Richardson and K.R. Reddy TERMINOLOGY, OPERATIONAL DEFINITIONS, AND COMPARISON OF PHOSPHORUS FORMS SAMPLE PREPARATION AND STORAGE SOIL PHOSPHORUS ANALYSIS PHOSPHORUS AVAILABILITY INDICES ANION EXCHANGE RESIN AND IRON OXIDE PAPER SOIL INORGANIC PHOSPHORUS FORMS GENERAL COMMENTS Chapter 33 Phosphorus Characterization in Wetland Soils by Solution Phosphorus-31 Nuclear Magnetic Resonance Spectroscopy / Alexander W. Cheesman, James Rocca, and Benjamin L. Turner BRIEF OVERVIEW OF THE PRINCIPLES APPLICATION TO WETLAND SOILS Chapter 34 Phosphorus Sorption and Desorption
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  • 14
    Call number: 4/M 23.95439
    In: Frontiers in earth sciences
    Description / Table of Contents: This book will constitute the proceedings of the ILP Workshop held in Abu Dhabi in December 2009. It will include a reprint of the 11 papers published in the December 2010 issue of the AJGS, together with 11 other original papers.
    Type of Medium: Monograph available for loan
    Pages: xx, 474 Seiten , Illustrationen, Karten
    ISBN: 9783642292781 , 978-3-642-29278-1
    ISSN: 1863-4621
    Series Statement: Frontiers in earth sciences
    Language: English
    Note: Contents Part I The Emirati Foreland and Foothills 1 Structural and stratigraphic evolution of Abu Dhabi in the context of Arabia / Ken W. Glennie 2 Architecture of the Oman–UAE ophiolite: evidence for a multi-phase magmatic history / K. M. Goodenough, M. T. Styles, D. Schofield, R. J. Thomas, Q. C. Crowley, R. M. Lilly, J. McKervey, D. Stephenson and J. N. Carney 3 New constrains on the thickness of the Semail ophiolite in the Northern Emirates / Charles Naville, Martine Ancel, Paul Andriessen, Patrice Ricarte and François Roure 4 The Jurassic–Cretaceous depositional and tectonic evolution of the southernwestern margin of the Neotethys Ocean, Northern Oman and United Arab Emirates / Emrys R. Phillips, Colin N. Waters and Richard A. Ellison 5 Forced folding of the neoautochthonous Late Cretaceous–Early Tertiary sequence at the western end of the Hatta Zone, Northern Oman Mountains / Mohammed Warrak 6 Seismic stratigraphy and subsidence history of the United Arab Emirates (UAE) rifted margin and overlying foreland basins / M. Y. Ali, A. B. Watts and M. P. Searle 7 Depth seismic imaging using reflection and first arrival traveltime tomography: Application to a deep profile across the Northern Emirates Foothills / Anne Jardin, Karine Broto and Timothée Perdrizet 8 Forward kinematic modelling of a regional transect in the Northern Emirates using geological and apatite fission track age constraints on paleo-burial history / Mihai Tarapoanca, Paul Andriessen, Karine Broto, Louis Chérel, Nadine Ellouz-Zimmermann, Jean-Luc Faure, Anne Jardin, Charles Naville and François Roure 9 Paleo-fluids characterisation and fluid flow modelling along a regional transect in Northern United Arab Emirates (UAE) / Jean-Paul Callot, Liesbeth Breesch, Nicole Guilhaumou, François Roure, Rudy Swennen and Nadège Vilasi 10 Diagenesis of the Khuff Formation (Permian–Triassic), northern United Arab Emirates / Simone Fontana, Fadi H. Nader, Sadoon Morad, Andrea Ceriani and Ihsan S. Al-Aasm Part II The Zagros and Makran tectonic wedges 11 Evidence for mantle exhumation along the Arabian margin in the Zagros (Kermanshah area, Iran) / Jean-Christophe Wrobel-Daveau, Jean-Claude Ringenbach, Saeid Tavakoli, Geoffrey M. H. Ruiz, Pierre Masse and Dominique Frizon de Lamotte 12 Structural style of the Makran Tertiary accretionary complex in SE-Iran / J.-P. Burg, A. Dolati, D. Bernoulli and J. Smit 13 Preliminary fault analysis and paleostress evolution in the Makran Fold-and-Thrust Belt in Iran / A. Dolati and J.-P Burg Part III Seismic hazards in Saudi Arabia and adjacent Parts of the Arabian Plate 14 Improvement of seismicity parameters in the Arabian Shield and Platform Using earthquake location and magnitude calibration / A. M. Al-Amri and A. J. Rodgers 15 Seismotectonics and seismogenic source zones of the Arabian Platform / Abdullah M. Al-Amri 16 Seismic zones regionalization and hazard assessment of SW Arabian Shield and Southern Red Sea Region / M. A. Al-Malki and A. M. Al-Amri Part IV Yemen margins and the Gulf of Aden 17 The Cryogenian Arc formation and successive High-K calc-alkaline plutons of Socotra Island (Yemen) / Y. Denèle, S. Leroy, E. Pelleter, R. Pik, J-Y Talbot and K. Khanbarri 18 Sedimentary basins of Yemen: their tectonic development and lithostratigraphic cover / Mustafa Abdullatif As-Saruri, Rasoul Sorkhabi and Rasheed Baraba 19 Paleostress analysis of the volcanic margins of Yemen / Khaled Khanbari and Philippe Huchon 20 From rifting to oceanic spreading in the Gulf of Aden: A synthesis / Sylvie Leroy, Philippe Razin, Julia Autin, François Bache, Elia d’Acremont, Louise Watremez, Jérémy Robinet, Céline Baurion, Yoann Denèle, Nicolas Bellahsen, Francis Lucazeau, Frédérique Rolandone, Stéphane Rouzo, Josep Serra Kiel, Cécile Robin, François Guillocheau, Christel Tiberi, Clémence Basuyau, Marie-Odile Beslier, Cynthia Ebinger, Graham Stuart, Abdulhakim Ahmed, Khaled Khanbari, Ismaël Al-Ganad, Philippe de Clarens, Patrick Unternehr, Khalfan Al-Toubi and Ali Al-Lazki 21 Upper mantle anisotropy of Southeast Arabia passive margin [Gulf of Aden Northern conjugate margin], Oman / Ali Al-Lazki, Cindy Ebinger, Michael Kendall, George Helffrich, Sylvie Leroy, Christel Tiberi, Graham Stuart and Khalfan Al-Toobi Part V Geodynamic Modelling 22 Samovar: a thermomechanical code for modeling of geodynamic processes in the lithosphere—application to basin evolution / Yuriy Elesin, Taras Gerya, Irina M. Artemieva and Hans Thybo Biographies Index
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  • 15
    Monograph available for loan
    Monograph available for loan
    Sankt-Peterburg : Sankt-Peterburgskij Gosudarstvennyj Universitet
    Call number: AWI Bio-13-0030
    Description / Table of Contents: Atlas contains photographic images of 91 plant species and pollen which are found in Lena River Delta as well as information about current conditions of their growth. This is a major advantage of this atlas as compared to other publications of this kind. All information is presented in Russian and English. All materials were collected in framework of the Russian-German expeditions "Lena-2009", "Lena-2010", "Lena-2011" and "Lena-2012". Photographs illustrate the general view of the plant, inflorescence and pollen grains in different positions and from high to low focus. Plants are grouped into families, where each family has its own color. Atlas is addressed not only to specialists in palynology, but to all who are interested in the flora and vegetation of the Arctic region, including students of geographical, biological and environmental fields.
    Type of Medium: Monograph available for loan
    Pages: 111 Seiten , Illustrationen
    ISBN: 9785439100361
    Language: Russian , English
    Note: Contents: Introduction. - Apiaceae. - Asteraceae. - Betulaceae. - Boraginaceae. - Brassicaceae. - Campanulaceae. - Caryophyllaceae. - Crassulaceae. - Cyperaceae. - Diapensiaceae. - Ericaceae. - Fabaceae. - Gentianaceae. - Hippuriadaceae. - Juncaceae. - Lentibulariaceae. - Liliaceae. - Onagraceae. - Papaveraceae. - Parnassiaceae. - Pinaceae. - Plumbaginaceae. - Poaceae. - Polemoniaceae. - Polygonaceae. - Portulacaceae. - Primulaceae. - Pyrolaceae. - Ranunculaceae. - Rosaceae. - Salicaceae. - Saxifragaceae. - Scrophulariaceae. - Valerianaceae. - Index of plants by family. - Alphabetical index of plants. , In englischer und russischer Sprache. , Teilw. in kyrillischer Schrift
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  • 16
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge University Press
    Call number: AWI A4-11-0035
    Description / Table of Contents: The polar regions have experienced some remarkable environmental changes in recent decades, such as the Antarctic ozone hole, the loss of large amounts of sea ice from the Arctic Ocean and major warming on the Antarctic Peninsula. The polar regions are also predicted to warm more than any other region on Earth over the next century if greenhouse gas concentrations continue to rise. Yet trying to separate natural climate variability from anthropogenic forcing still presents many problems. This book presents a thorough review of how the polar climates have changed over the last million years and sets recent changes within a long term perspective, as determined from ice and ocean sediment cores. The approach taken is highly cross-disciplinary and the close links between the atmosphere, ocean and ice at high latitudes are stressed. The volume will be invaluable for researchers and advanced students in polar science, climatology, global change, meteorology, oceanography and glaciology.
    Type of Medium: Monograph available for loan
    Pages: xii, 434 Seiten , Illustrationen
    Edition: First published
    ISBN: 9780521850100 , 978-0-521-85010-0
    Language: English
    Note: Contents: Preface. - 1. Introduction. - 1.1 The environment of the polar regions. - 1.2 The role of the polar regions in the global climate system. - 1.3 Possible implications of high latitude climate change. - 2. Polar climate data and models. - 2.1 Introduction. - 2.2 Instrumental observations. - 2.3 Meteorological analysis fields. - 2.4 Remotely sensed data. - 2.5 Proxy climate data. - 2.6 Models. - 3. The high latitude climates and mechanisms of change. - 3.1 Introduction. - 3.2 Factors influencing the broadscale climated of the polar regions. - 3.3 Processes of the high latitude climates. - 3.4 The mechanisms of high latitude climate change. - 3.5 Atmospheric circulation. - 3.6 Temperature. - 3.7 Cloud and precipitation. - 3.8 Sea ice. - 3.9 The ocean circulation. - 3.10 Concluding remarks. - 4. The last million years. - 4.1 Introduction. - 4.2 The Arctic. - 4.3 The Antarctic. - 4.4 Linking high latitude climate change in the two hemispheres. - 5. The Holocene. - 5.1 Introduction. - 5.2 Forcing of the climate system during the Holocene. - 5.3 Atmospheric circulation. - 5.4 Temperature. - 5.5 The ocean circulation. - 5.6 Sea ice and sea surface temperatures. - 5.7 Atmospheric gases and aerosols. - 5.8 The cryosphere, precipitation and sea level. - 5.9 Concluding remarks. - 6. The instrumental period. - 6.1 Introduction. - 6.2 The main meteorological elements. - 6.3 Changes in the atmospheric circulation. - 6.4 The ocean environment. - 6.5 Sea ice. - 6.6. Snow cover. - 6.7 Permafrost. - 6.8 Atmospheric gases and aerosols. - 6.9 Terrestrial ice and sea level. - 6.10 Attribution of recent changes. - 6.11 Concluding remarks. - 7. Predictions for the next 100 years. - 7.1 Introduction. - 7.2 Possible future greenhouse gas emission scenarios and the IPCC models. - 7.3 Changes in the atmospheric circulation and the modes of climate variability. - 7.4 The main meteorological elements. - 7.5 The ocean circulation and water masses. - 7.6 Sea ice. - 7.7 Seasonal snow cover and the terrestrial environment. - 7.8 Permafrost. - 7.9 Atmospheric gases and aerosols. - 7.10 Terrestrial ice, the ice shelves and sea level. - 7.11 Concluding remarks. - 8. Summary and future research needs. - 8.1 Introduction. - 8.2 Gaining improved understanding of past climate change. - 8.3 Modelling the high latitude climate system. - 8.4 Data required. - 8.5 Concluding remarks. - References. - Index.
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  • 17
    Publication Date: 2023-07-18
    Language: English
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  • 18
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    Springer
    Publication Date: 2023-07-18
    Description: ‘Transgovernance: Advancing Sustainability Governance’ analyses what implications recent and ongoing changes in the relations between politics, science and media – together characterized as the emergence of a knowledge democracy – may have for governance for sustainable development, on global and other levels of societal decision making, and vice versa: How can the discussion on sustainable development contribute to a knowledge democracy? How can concepts such as second modernity, reflexivity, configuration theory, (meta)governance theory and cultural theory contribute to a ‘transgovernance’ approach which goes beyond mainstream sustainability governance? This volume presents contributions from various angles: international relations, governance and metagovernance theory, (environmental) economics and innovation science. It offers challenging insights regarding institutions and transformation processes, and into the paradigms behind contemporary sustainability governance. This book gives the sustainability governance debate a new context. It transforms classical questions into new options for societal decision making and identifies starting points and strategies aimed at effective governance of transitions to sustainability.
    Language: English
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  • 19
    Publication Date: 2023-07-18
    Description: The concept of boundary work has been put forward as an analytical approach towards the study of interactions between science and policy. While the concept has been useful as a case-study approach, there are several weaknesses and constraints when using the concept in a more systemic analysis of the interactions between knowledge production and sustainable development decision-making at the international level, such as its inability to capture the diversity of institutions involved in such boundary work. Another inability involves a lack of conceptualisation of the impacts of the specific conditions of intergovernmental decision-making, such as rules for representation and the mode of negotiation. This chapter suggests complementing the concept of boundary work with a configuration approach based on a two-dimensional conceptualisation of the boundary space in international decision-making that allows the positioning of institutions with regard to their degree of politicisation and their position in terms of national and regional representation. Such an approach could be a useful guide in the further conceptualisation and application of the boundary concept.
    Language: English
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  • 20
    Publication Date: 2023-07-18
    Description: Hydrothermal carbonization (HTC) is an aqueous-phase route to produce carbon materials using biomass or biomass-derived precursors. In this paper, a comprehensive physicochemical and textural characterization of HTC materials obtained using four different precursors, namely, xylose, glucose, sucrose, and starch, is presented. The development of porosity in the prepared HTC materials as a function of thermal treatment (under an inert atmosphere) was specifically monitored using N2 and CO2 sorption analysis. The events taking place during the thermal treatment process were studied by a combined thermogravimetric/infrared (TGA-IR) measurement. Interestingly, these inexpensive biomass-derived carbon materials show good selectivity for CO2 adsorption over N2 (CO2/N2 selectivity of 20 at 273 K, 1 bar and 1:1 gas composition). Furthermore, the elemental composition, morphologies, degree of structural order, surface charge, and functional groups are also investigated.
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  • 21
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    In:  Soils of Urban, Industrial, Traffic, Mining and Military Areas. SUITMA 7. Abstracts
    Publication Date: 2023-07-18
    Description: The recognition of soils and their functions by the public and, in particular, the planning community isgenerally poor. However, conversion of soils to urban uses is occurring at an unprecedented rate dueto an increasing share of the population living in urban areas and changing lifestyles. Urban planners,developers and planning agencies allocate urban lands to varying uses but land use decisions aregenerally not based on soil information as urban growth is managed predominantly for economicdevelopment. However, urban areas must also deal with challenges such as demographic change,urban densification, climate change and infrastructure provision. Thus, managing urban sustainabilityhas to include ecological aside economic, cultural, and political dimensions. Urban developmentneeds to be managed to minimize negative impacts and maximize environmental quality. Policydecisions towards maximizing short-term economic benefits must be balanced by decisions towardssustainable use and management of urban soils as urban land use has long-term consequences. Therecognition of soils by the planning community can particularly be improved by highlighting the valueof urban soil functions for the well-being of urban dwellers. This approach was recommended at thedialogue session ’Urbanization: Challenges to Soil Management‘ during the first Global Soil Week2012 in Berlin, Germany. Further suggestions how to raise the awareness about urban soils and howto deal with challenges regarding their management will be presented.
    Language: English
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  • 22
    Publication Date: 2023-07-18
    Language: English
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  • 23
    Publication Date: 2023-07-18
    Description: Temporal and spatial patterns in eastern North Atlantic sea-surface temperatures (SST) were reconstructed for marine isotope stage (MIS) 11c using a submeridional transect of five sediment cores. The SST reconstructions are based on planktic foraminiferal abundances and alkenone indices, and are supported by benthic and planktic stable isotope measurements, as well as by ice-rafted debris content in polar and middle latitudes. Additionally, the larger-scale dynamics of the precipitation regime over northern Africa and the western Mediterranean region was evaluated from iron concentrations in marine sediments off NW Africa and planktic δ 13C in combination with analysis of planktic foraminiferal abundances down to the species level in the Mediterranean Sea. Compared to the modern situation, it is revealed that during entire MIS 11c sensu stricto (ss), i.e., between 420 and 398ka according to our age models, a cold SST anomaly in the Nordic seas co-existed with a warm SST anomaly in the middle latitudes and the subtropics, resulting in steeper meridional SST gradients than during the Holocene. Such a SST pattern correlates well with a prevalence of a negative mode of the modern North Atlantic Oscillation. We suggest that our scenario might partly explain the longer duration of wet conditions in the northern Africa during MIS 11c compared to the Holocene.
    Language: English
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  • 24
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    In:  The Roads From Rio: Lessons Learned from Twenty Years of Multilateral Environmental Negotiations
    Publication Date: 2023-07-18
    Language: English
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  • 25
    Publication Date: 2023-07-18
    Description: The dynamics of the 18O(3P) + 32O2 isotope exchange reaction were studied using crossed atomic and molecular beams at collision energies (Ecoll) of 5.7 and 7.3 kcal/mol, and experimental results were compared with quantum statistical (QS) and quasi-classical trajectory (QCT) calculations on the O3(X1A’) potential energy surface (PES) of Babikov et al. [D. Babikov, B. K. Kendrick, R. B. Walker, R. T. Pack, P. Fleurat-Lesard, and R. Schinke, J. Chem. Phys.118, 6298 (2003)]. In both QS and QCT calculations, agreement with experiment was markedly improved by performing calculations with the experimental distribution of collision energies instead of fixed at the average collision energy. At both collision energies, the scattering displayed a forward bias, with a smaller bias at the lower Ecoll. Comparisons with the QS calculations suggest that 34O2 is produced with a non-statistical rovibrational distribution that is hotter than predicted, and the discrepancy is larger at the lower Ecoll. If this underprediction of rovibrational excitation by the QS method is not due to PES errors and/or to non-adiabatic effects not included in the calculations, then this collision energy dependence is opposite to what might be expected based on collision complex lifetime arguments and opposite to that measured for the forward bias. While the QCT calculations captured the experimental product vibrational energy distribution better than the QS method, the QCT results underpredicted rotationally excited products, overpredicted forward-bias and predicted a trend in the strength of forward-bias with collision energy opposite to that measured, indicating that it does not completely capture the dynamic behavior measured in the experiment. Thus, these results further underscore the need for improvement in theoretical treatments of dynamics on the O3(X1A’) PES and perhaps of the PES itself in order to better understand and predict non-statistical effects in this reaction and in the formation of ozone (in which the intermediate O3 * complex is collisionally stabilized by a third body). The scattering data presented here at two different collision energies provide important benchmarks to guide these improvements.
    Language: English
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  • 26
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    In:  Recarbonization of the biosphere : ecosystems and the global carbon cycle
    Publication Date: 2023-07-18
    Language: English
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  • 27
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    In:  The Asahi Shimbun AJW, January 27, 2013
    Publication Date: 2023-07-18
    Language: English
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  • 28
    Publication Date: 2023-07-18
    Description: Institutions for biodiversity governance are located at the interface of human and ecological systems. The analysis of such institutions is challenged due to addressing a multitude of complex interactions between these two systems occurring at different natural scales and levels of human organization. Due to this complexity, empirical analysis of biodiversity management often leads to context-specific explanations, providing little scope for comparative work or the development of more generalised, theory-based accounts. We aim at reducing complexity in understanding human-biodiversity relations, making cases comparable across sites, and propose that, in order to address complexity, we need a method of abstraction that leads to the development of a more structured analysis, based on selection of explanatory factors according to cconceptual models as well as empirical significance. We suggest that the stylisation of typical "resource use-perspectives" - the combination of typical transactions that are inextricably linked by the interest of the actor - can be a useful method for realizing appropriate model selection. In this paper, we provide an account of how use-perspectives can be developed and to what kind of analysis they can contribute, using the example of agrobiodiversity in grain as seed, food, or genetic material.
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  • 29
    Publication Date: 2023-07-18
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  • 30
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    In:  Recarbonization of the biosphere : ecosystems and the global carbon cycle
    Publication Date: 2023-07-18
    Language: English
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  • 31
    Publication Date: 2023-07-18
    Description: Abstract. It has been claimed for more than a century that atmospheric new particle formation is primarily influenced by the presence of sulfuric acid. However, the activation process of sulfuric acid related clusters into detectable particles is still an unresolved topic. In this study we focus on the PARADE campaign measurements conducted during August/September 2011 at Mt Kleiner Feldberg in central Germany. During this campaign a set of radicals, organic and inorganic compounds and oxidants and aerosol properties were measured or calculated. We compared a range of organic and inorganic nucleation theories, evaluating their ability to simulate measured particle formation rates at 3 nm in diameter (J3) for a variety of different conditions. Nucleation mechanisms involving only sulfuric acid tentatively captured the observed noon-time daily maximum in J3, but displayed an increasing difference to J3 measurements during the rest of the diurnal cycle. Including large organic radicals, i.e. organic peroxy radicals (RO2) deriving from monoterpenes and their oxidation products, in the nucleation mechanism improved the correlation between observed and simulated J3. This supports a recently proposed empirical relationship for new particle formation that has been used in global models. However, the best match between theory and measurements for the site of interest was found for an activation process based on large organic peroxy radicals and stabilised Criegee intermediates (sCI). This novel laboratory-derived algorithm simulated the daily pattern and intensity of J3 observed in the ambient data. In this algorithm organic derived radicals are involved in activation and growth and link the formation rate of smallest aerosol particles with OH during daytime and NO3 during night-time. Because the RO2 lifetime is controlled by HO2 and NO we conclude that peroxy radicals and NO seem to play an important role for ambient radical chemistry not only with respect to oxidation capacity but also for the activation process of new particle formation. This is supposed to have significant impact of atmospheric radical species on aerosol chemistry and should be taken into account when studying the impact of new particles in climate feedback cycles.
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  • 32
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    In:  Recarbonization of the biosphere : ecosystems and the global carbon cycle
    Publication Date: 2023-07-18
    Language: English
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  • 33
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    In:  Journal of plant nutrition and soil science
    Publication Date: 2023-07-18
    Language: English
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  • 34
    Publication Date: 2023-07-18
    Description: Variations in the poleward-directed Atlantic heat transfer was investigated over the past 135ka with special emphasis on the last and present interglacial climate development (Eemian and Holocene). Both interglacials exhibited very similar climatic oscillations during each preceding glacial terminations (deglacial TI and TII). Like TI, also TII has pronounced cold-warm-cold changes akin to events such as H1, Blling/Allerd, and the Younger Dryas. But unlike TI, the cold events in TII were associated with intermittent southerly invasions of an Atlantic faunal component which underscores quite a different water mass evolution in the Nordic Seas. Within the Eemian interglaciation proper, peak warming intervals were antiphased between the Nordic Seas and North Atlantic. Moreover, inferred temperatures for the Nordic Seas were generally colder in the Eemian than in the Holocene, and vice versa for the North Atlantic. A reduced intensity of Atlantic Ocean heat transfer to the Arctic therefore characterized the Eemian, requiring a reassessment of the actual role of the ocean-atmosphere system behind interglacial, but also, glacial climate changes.
    Language: English
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  • 35
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    In:  IASS Fact Sheet
    Publication Date: 2023-07-18
    Description: The use of fossil hydrocarbons in the energy and transport sectors is a major source of greenhouse gas emissions. It also ties our society to ever dwindling reserves. Synthetic fuels could play a crucial role in establishing a carbon neutral energy supply.
    Language: English
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  • 36
    Publication Date: 2023-07-18
    Description: The energy demand of the world is foreseen to be increased due to the improvements on the living standard of the developing countries and the development of the global economy. The increase in sustainability of the energy supply must be considered as a must to avoid spoiling natural resources for the next human generations and more dramatic effects such as the so-called global atmospheric warming. The utilization of CO2-free energy sources, as in the case of renewables, is one of the most promising ways to attain such objectives. Nevertheless, the massive energy production with such energy sources are far from being practically feasible in the short-medium term and an innovative solution should be put into practice for the CO2-free exploitation of the huge fossil fuel resources already available. This general assumption is also applicable to any energy carrier such as Hydrogen or electricity. In this case, an analysis is done of the Hydrogen production processes and the discussion of the need to develop a CO2-free production scheme like methane cracking is shown.
    Language: English
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  • 37
    Publication Date: 2023-07-18
    Description: Large point sources such as major population centers (MPCs) emit pollutants which can be deposited nearby or transported over long distances before deposition. We have used tracer simulations of aerosols emitted from MPCs worldwide to assess the fractions which are deposited at various distances away from their source location. Considering only source location, prevailing meteorology, and the aerosol size and solubility, we show that fine aerosol particles have a high potential to pollute remote regions. About half of the emitted mass of aerosol tracers with an ambient diameter ≤1.0 μm is typically deposited in regions more than 1000 km away from the source. Furthermore, using the Köppen-Geiger climate classification to categorize the sources into various climate classes we find substantial differences in the deposition potential between these classes. Tracers originating in arid regions show the largest remote deposition potentials, with values more than doubled compared to the smallest potentials from tracers in tropical regions. Seasonal changes in atmospheric conditions lead to variations in the remote deposition potentials. On average the remote deposition potentials in summer correspond to about 70-80% of the values in winter, with a large spread among the climate classes. For tracers from tropical regions the summer remote deposition values are only about 31% of the winter values, while they are about 95% for tracers from arid regions.
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  • 38
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    In:  IASS Blog, 17.11.2014
    Publication Date: 2023-07-18
    Description: In the basement, in an alcove that's almost a small room, stands a small wood stove. If it weren't on a pedestal, it would barely be a metre high; but even so it's small, almost cute. The wood from which it's made appears to be untreated; its whiteness is rustic, quaint, innocent. It takes a minute to realise what's wrong. A 'wood stove' should be a stove for burning wood - not one made of wood. It should make combustion possible without itself being combustible.
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  • 39
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    In:  Transgovernance: advancing sustainability governance
    Publication Date: 2023-07-18
    Description: Sustainable development is all over the place. The concept is broad and vague. The vagueness of the concept has a Janus face. It has been called a unifying concept because its vagueness breeds a consensus that might be utilised later on. Vagueness is an asset if it triggers action. On the other hand, if sustainable development is everything, maybe it is nothing… Although – or maybe because – the concept is vague, it has overwhelming appeal on political agendas, programmes and dialogues. The precautionary principle is the nucleus of a powerful moral imperative. The multidimensional nature of the concept, covering ecological, economic and social aspects of change relates to our needs for integration. Sustainable development as a concept bears a persuasive character. Actors of all kinds may contribute to it, citizens, enterprises, NGOs, governments et cetera. Thinking about the governance of sustainable development leads us to the recognition of a multi-level, multi-scale, multi-disciplinary character of the problematique. Moreover, the term development refers to change, to transitions and transformations. Governance of sustainable development therefore has to cope with complex dynamics. This chapter deals with the specific consequences of sustainability governance inside knowledge democracies. The concept of knowledge democracy sheds new light on the emerging relationships between politics, media and science. It shows how the emergence of participatory democracy besides representative democracy, the revolutionary rise of social media besides corporate media, the emergence of transdisciplinary trajectories besides classical disciplinary science lead to explosions of complex interactions. We will digress upon the variety of possible future variants of knowledge democracies, quiet and turbulent ones, in relation to the quest for sustainable development. Our main conclusion will be that strategies for sustainability may vary with the types of knowledge democracies around.
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  • 40
    Publication Date: 2023-07-18
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  • 41
    Publication Date: 2023-07-18
    Description: In this study we compare the response of four state-of-the-art Earth system models to climate engineering under scenario G1 of two model intercomparison projects: GeoMIP (Geoengineering Model Intercomparison Project) and IMPLICC (EU project "Implications and risks of engineering solar radiation to limit climate change"). In G1, the radiative forcing from an instantaneous quadrupling of the CO 2 concentration, starting from the preindustrial level, is balanced by a reduction of the solar constant. Model responses to the two counteracting forcings in G1 are compared to the preindustrial climate in terms of global means and regional patterns and their robustness. While the global mean surface air temperature in G1 remains almost unchanged compared to the control simulation, the meridional temperature gradient is reduced in all models. Another robust response is the global reduction of precipitation with strong effects in particular over North and South America and northern Eurasia. In comparison to the climate response to a quadrupling of CO 2 alone, the temperature responses are small in experiment G1. Precipitation responses are, however, in many regions of comparable magnitude but globally of opposite sign.
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  • 42
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    In:  Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
    Publication Date: 2023-07-18
    Description: We examine the claim that in governance for solar climate engineering research, and especially field tests, there is no need for external governance beyond existing mechanisms such as peer review and environmental impact assessments that aim to assess technically defined risks to the physical environment. By drawing on the historical debate on recombinant DNA research, we show that defining risks is not a technical question but a complex process of narrative formation. Governance emerges from within, and as a response to, narratives of what is at stake in a debate. In applying this finding to the case of climate engineering, we find that the emerging narrative differs starkly from the narrative that gave meaning to rDNA technology during its formative period, with important implications for governance. While the narrative of rDNA technology was closed down to narrowly focus on technical risks, that of climate engineering continues to open up and includes social, political and ethical issues. This suggests that, in order to be legitimate, governance must take into account this broad perception of what constitutes the relevant issues and risks of climate engineering, requiring governance that goes beyond existing mechanisms that focus on technical risks. Even small-scale field tests with negligible impacts on the physical environment warrant additional governance as they raise broader concerns that go beyond the immediate impacts of individual experiments.
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  • 43
    Publication Date: 2023-07-18
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  • 44
    Publication Date: 2023-07-18
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  • 45
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    In:  IASS Blog, 01.12.2014
    Publication Date: 2023-07-18
    Description: It is often claimed that a higher ratio of natural gas to coal in our energy mix can mitigate current carbon dioxide emissions and serve as a 'bridge' to future renewable-based scenarios. This is because the carbon footprint of energy produced through the combustion of methane is about half that of energy produced from coal.
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  • 46
    Publication Date: 2023-07-18
    Description: The Indo-Gangetic Plain (IGP) region is one of the most densely populated regions in the World, but ground-based observations of air pollutants are highly limited in this region. Here, surface ozone observations made during March 2009-June 2011 at a semi-urban site (Pantnagar; 29.0°N, 79.5°E, 231m amsl) in the IGP region are presented. Ozone mixing ratios show a daytime photochemical buildup with ozone levels sometimes as high as 100 ppbv. Seasonal variation in 24-h average ozone shows a distinct spring maximum (39.3±18.9 ppbv in May) while daytime (1130-1630h) average ozone shows an additional peak during autumn (48.7±13.8 ppbv in November). The daytime, but not daily average, observed ozone seasonality is in agreement with the space-borne observations of OMI tropospheric column NO2, TES CO (681hPa), surface ozone observations at a nearby high altitude site (Nainital) in the central Himalayas and to an extent with results from a global chemistry transport model (MATCH-MPIC). It is suggested that spring and autumn ozone maximum are mainly due to photochemistry, involving local pollutants and small-scale dynamical processes. Biomass burning activity over the northern Indian region could act as an additional source of ozone precursors during spring. The seasonal ozone photochemical buildup is estimated to be 32-41 ppbv during spring and autumn and 9-14 ppbv during August-September. A correlation analysis between ozone levels at Pantnagar and Nainital along with the mixing depth data suggests that emissions and photochemical processes in the IGP region influence the air quality of pristine Himalayan region, particularly during midday hours of spring. The evening rate of change (8.5 ppbv hr-1) is higher than the morning rate of change, which is dissimilar to those at other urban or rural sites. Ozone seasonality over the IGP region is different than that over southern India. Results from the MATCH-MPIC model capture observed ozone seasonality but overestimate ozone levels. Model simulated daytime ratios of H2O2/HNO3 are higher and suggesting that this region is in a NOx-limited regime. A chemical box model (NACR Master Mechanism) is used to further corroborate this using a set of sensitivity simulations, and to estimate the integrated net ozone production in a day (72.9 ppbv) at this site.
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  • 47
    Publication Date: 2023-07-18
    Description: In this study the sensitivity of the model performance of the chemistry transport model (CTM) LOTOS-EUROS to the description of the temporal variability of emissions was investigated. Currently the temporal release of anthropogenic emissions is described by European average diurnal, weekly and seasonal time profiles per sector. These default time profiles largely neglect the variation of emission strength with activity patterns, region, species, emission process and meteorology. The three sources dealt with in this study are combustion in energy and transformation industries (SNAP1), nonindustrial combustion (SNAP2) and road transport (SNAP7). First of all, the impact of neglecting the temporal emission profiles for these SNAP categories on simulated concentrations was explored. In a second step, we constructed more detailed emission time profiles for the three categories and quantified their impact on the model performance both separately as well as combined. The performance in comparison to observations for Germany was quantified for the pollutants NO2, SO2 and PM10 and compared to a simulation using the default LOTOS-EUROS emission time profiles. The LOTOS-EUROS simulations were performed for the year 2006 with a temporal resolution of 1 h and a horizontal resolution of approximately 25 × 25km2. In general the largest impact on the model performance was found when neglecting the default time profiles for the three categories. The daily average correlation coefficient for instance decreased by 0.04 (NO2), 0.11 (SO2) and 0.01 (PM10) at German urban background stations compared to the default simulation. A systematic increase in the correlation coefficient is found when using the new time profiles. The size of the increase depends on the source category, component and station. Using national profiles for road transport showed important improvements in the explained variability over the weekdays as well as the diurnal cycle for NO2. The largest impact of the SNAP1 and 2 profiles were found for SO2. When using all new time profiles simultaneously in one simulation, the daily average correlation coefficient increased by 0.05 (NO2), 0.07 (SO2) and 0.03 (PM10) at urban background stations in Germany. This exercise showed that to improve the performance of a CTM, a better representation of the distribution of anthropogenic emission in time is recommendable. This can be done by developing a dynamical emission model that takes into account regional specific factors and meteorology.
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  • 48
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    In:  IASS Blog, 18.12.2014
    Publication Date: 2023-07-18
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  • 49
    Publication Date: 2023-07-18
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  • 50
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    In:  Recarbonization of the biosphere : ecosystems and the global carbon cycle
    Publication Date: 2023-07-18
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  • 51
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    In:  Recarbonization of the biosphere : ecosystems and the global carbon cycle
    Publication Date: 2023-07-18
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  • 52
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    In:  IASS Blog, 20.11.2014
    Publication Date: 2023-07-18
    Description: This December, the 20th United Nations Framework Convention on Climate Change (UNFCCC) Conference of the Parties (COP) will be held in Lima, Peru. There climate change negotiations will focus on reducing emissions of carbon dioxide, the long-lived greenhouse gas primarily responsible for anthropogenic climate change. However, on the short-term, air pollutants that also have an influence on climate, known as short-lived climate forcing pollutants (SLCPs) should also be addressed.
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  • 53
    Publication Date: 2023-07-18
    Description: Global-scale solar geoengineering is the deliberate modification of the climate system to offset some amount of anthropogenic climate change by reducing the amount of incident solar radiation at the surface. These changes to the planetary energy budget result in differential regional climate effects. For the first time, we quantitatively evaluate the potential for regional disparities in a multi-model context using results from a model experiment that offsets the forcing from a quadrupling of CO2 via reduction in solar irradiance. We evaluate temperature and precipitation changes in 22 geographic regions spanning most of Earthʼs continental area. Moderate amounts of solar reduction (up to 85% of the amount that returns global mean temperatures to preindustrial levels) result in regional temperature values that are closer to preindustrial levels than an un-geoengineered, high CO2 world for all regions and all models. However, in all but one model, there is at least one region for which no amount of solar reduction can restore precipitation toward its preindustrial value. For most metrics considering simultaneous changes in both variables, temperature and precipitation values in all regions are closer to the preindustrial climate for a moderate amount of solar reduction than for no solar reduction.
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  • 54
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    In:  IISD: SDG Knowledge Hub; Commentary
    Publication Date: 2023-07-18
    Description: STORY HIGHLIGHTSA little bit more than a year ago, delegates of the UN Conference on Sustainable Development (UNCSD or Rio+20) agreed that they would “strive to achieve a land-degradation-neutral world in the context of sustainable development.”
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  • 55
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    In:  Recarbonization of the biosphere : ecosystems and the global carbon cycle
    Publication Date: 2023-07-18
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  • 56
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    In:  The International Relations and Security Network
    Publication Date: 2023-07-18
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  • 57
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    In:  GAIA - Ecological Perspectives for Science and Society
    Publication Date: 2023-07-18
    Description: Solar radiation management(SRM), a subset of approaches to climate engineering, aims to manipulate the global climate on a large scale. It includes techniques like spraying sulfate aerosols into the stratosphere or brightening marine clouds to reflect more sunlight back into space. In an attempt to examine the socio-political context of SRM, research frequently starts from model projections of physi cal changes in the environment. But assessing socio-political matters is complex, and while model projections may help, experiences from research on CO2-induced climate change reveal many blind spots and some unique challenges.
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  • 58
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    In:  Soils of Urban, Industrial, Traffic, Mining and Military Areas. SUITMA 7. Abstracts
    Publication Date: 2023-07-18
    Description: The urban ecosystem and its ecosystem services (ESs) are managed for the wellbeing of urbandwellers. Thus, sustainable urban development depends on ESs aside economic, cultural and politicaldimensions. Soils play a central role in the urban ecosystem as they fulfill various functions andprovide several ESs. In urban areas, they are usually built to perform specific functions and providespecific ESs, e.g., (i) supporting buildings, roads and infrastructure; (ii) waste adsorption; (iii)supporting biomass production for green infrastructure and urban agriculture; (iv) filter, buffer andtransformation of contaminants; (v) regulating air and water quality; (vi) supporting nutrient cycling.In urban areas, some soils may be strongly modified by human activities, which changes theircomposition and functions, and, therefore, their ability to provide ESs. Urban soils and, moregenerally, SUITMAs (soils in urban, industrial, traffic, mining and military areas) may fulfill individuallya smaller number of ESs, smaller than those of natural soils outside of urban areas. Secondary andincidental ESs, if not disservices, may also be performed by SUITMAs.In this paper, we attempt to rank SUITMAs, according to the ESs they provide. Focus is made onthe nature of services, their importance and the number of services provided by each soil type. Workis also assigned to assess the extent to which urban soils can be deliberately altered to enhance ESs.After the tentative classification of soils, two examples will be given, i) sealed soil deemed tocomplete only few functions and provide specific services, and ii) soils of green-roofs designed toprovide a wide range of ESs, including particularly the control of the quality of air and water, thetemperature control, and the moderation of biodiversity loss.In conclusion, focus is to turn the attention towards the recognition of SUITMAs and theirmanagement as basis for the sustainable development of the urban ecosystem.
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  • 59
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    In:  Journal of the American Chemical Society
    Publication Date: 2023-07-18
    Description: A generalized synthesis of high-quality,mesoporous zeolite (e.g., MFI-type) nanocrystals ispresented, based on a biomass-derived, monolithic Ndopedcarbonaceous template. As an example, ZSM-5single crystals with desirable large-diameter (12−16 nm)intracrystalline mesopores are synthesized. The platformprovides scope to optimize template dimensions andchemistry for the synthesis of a range of micro-/mesoporous crystalline zeolites in a cost-effective andhighly flexible manner.
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  • 60
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    In:  SGI - Sustainable Governance Indicators News
    Publication Date: 2023-07-18
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  • 61
    Publication Date: 2023-07-18
    Description: This study presents results from systematic time-resolved experiments regarding the guest molecule geometry. The in situ observations of formation and dissociation processes of multicomponent hydrates were performed by means of Raman spectroscopy and a newly designed experimental setup including powder X-ray diffraction (PXRD) whose capabilities will be presented here in more detail. Both experimental setups allow investigating hydrate kinetics as a function of pressure, temperature, and feed gas composition. The unique feature of both setups is the continuous gas flow providing a constant composition of the gas phase during the whole experiment. This is crucial for the formation of mixed hydrates formed from feed gas mixtures that contain one or more components in low concentrations. The formation of structure II hydrates including C 3H 8, iso-C 4H 10, n-C 4H 10, or neo-C 5H 12 besides CH 4 was analysed according to a multi-step model. For the initial phase it turned out that hydrates grown from the gas mixture containing 2% n-C 4H 10 and 98% CH 4 have the highest formation rate at defined p, T conditions in comparison to other hydrates formed from gas mixtures containing about 2 vol% of the above mentioned hydrocarbons besides CH 4. But the reaction mechanisms for each hydrate system emerged to be different. Furthermore, Raman and time-resolved PXRD experiments were performed to study the formation of structure H hydrates with a low-concentrated large hydrocarbon guest molecule. In case of a gas mixture containing 1% iso-C 5H 12 and 99% CH 4 the formation of a simple structure I CH 4 hydrate was observed at first. Later on, structure H CH 4 + iso-C 5H 12 hydrate was formed resulting in a coexistence of both structures.
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  • 62
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    Institute for Advanced Sustainability Studies (IASS)
    In:  IASS Dissertation
    Publication Date: 2023-07-18
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  • 63
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    In:  Recarbonization of the biosphere : ecosystems and the global carbon cycle
    Publication Date: 2023-07-18
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  • 64
    Publication Date: 2023-07-18
    Description: Carbon dioxide is a harmful greenhouse gas. But it is also the basic ingredient of countless chemical products. In recent years, research on the sequestration and practical use of carbon dioxide has yielded a number of important initial breakthroughs.
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  • 65
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    In:  Financial Crises, Sovereign Risk and the Role of Institutions
    Publication Date: 2023-07-18
    Description: The concerns about tax haven activity shown by leading nations originate not only from a sense of injustice caused by the fact that tax havens allow multi-billion dollar firms such as Google, Starbucks and Apple to pay only a few pennies in taxes but the notion that tax haven activity fuels international financial instability through various avenues. This contribution evaluates the risk of financial collapse or liquidity crisis to tax havens in general. It shows that tax havens are more exposed to the risk of a financial collapse than non-tax havens and that this risk positively depends on the amount of profits shifted to them. We find that the risk of a tax haven collapse is positively related to the corporate tax rate and MNCs are willing to make more daring investments in tax havens the higher corporate tax rates. However, MNCs take the risk of losing their investments due to a financial collapse into account and hence invest only a fraction of their profits in tax havens.
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  • 66
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    In:  WeltRisikoBericht 2014: Schwerpunkt: Risikoraum Stadt
    Publication Date: 2023-07-18
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  • 67
    Publication Date: 2023-07-18
    Description: The impact of the megacities of the world on global tropospheric ozone, and conversely, the extent to which megacities are influenced by emissions of ozone precursors from outside of the megacities is examined under the four alternative RCP ("Representative Concentration Pathway") emissions scenarios. Despite accounting for about 6% of present-day anthropogenic emissions of ozone precursor species, the contribution of emissions from megacities to global tropospheric ozone is calculated to be 0.84%. By 2100 this contribution falls to between 0.18% and 0.62% depending on the scenario, with the lower value being for the most-polluting of the four future emissions scenarios due to stringent controls on ozone precursor emissions from highly populated areas combined with a stronger tropospheric background ozone field. The higher end of this range is from the least-polluting of the four emissions scenarios, due to lower background tropospheric ozone combined with the use of a simpler downscaling methodology in the construction of the scenario, which results in higher emissions from megacities. Although the absolute impact of megacities on global ozone is small, an important result of this study is that under all future scenarios, future air quality in megacities is expected to be less influenced by local emissions within the cities, but instead more influenced by emission sources outside of the cities, with mixing ratios of background ozone projected to play an increasing role in megacity air quality throughout the 21st century. Assumptions made when downscaling the emissions scenarios onto the grids used in such modelling studies can have a large influence on these results; future generations of emissions scenarios should include spatially explicit representations or urban development suitable for air quality studies using global chemical transport models.
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    Publication Date: 2023-07-18
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    In:  Transgovernance: advancing sustainability governance
    Publication Date: 2023-07-18
    Description: In the 20 years since the United Nations summit on sustainable development in Rio de Janeiro in 1992, the world has become more diverse, turbulent, fast and multi-polar. Tensions between old and new forms of politics, science and media, representing the emergence of what has been framed as the knowledge democracy, have brought about new challenges for sustainability governance. However, the existing governance frameworks seem to deny this social complexity and uncertainty. They also favour centralised negotiations and institutions, view governments as exclusive decision makers, and imply hegemony of Western economic, political and cultural principles. This is also reflected in the language of sustainability governance: it is centralist and is referring to monolithic concepts (the economy, the climate, the Earth System) rather than embracing diversity and complexity. This chapter sheds light on the problematic relations between cultural diversity, sustainable development and governance. These three concepts share a normative character, which is always a good predictor of trouble if interaction takes place. It is argued that the implementation deficit of sustainable development can be traced back to three problems: a neglect of the opportunities which cultural diversity offers, an implicit preference for central top-down political solutions, and an underestimation of the ‘wickedness’ of many sustainability challenges. It is concluded that sustainability governance should be more culturally sensitive, reflexive and dynamic. This requires institutions, instruments, processes, and actor involvement based on compatibility of values and traditions rather than on commonality or integration. It also calls for situationally effective combinations of ideas from hierarchical, network and market governance. This implies an approach beyond traditional forms of governance, towards a culturally sensitive metagovernance for sustainable development, beyond disciplinary scientific research, beyond states and other existing institutional borders, beyond existing ways to measure progress, beyond linear forms of innovation, and beyond cultural integration or assimilation, towards looking for compatibility. Governance for sustainable transformations requires what we have framed in this volume as transgovernance.
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    In:  energy post, 16.06.2014
    Publication Date: 2023-07-18
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  • 71
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    In:  Transatlantic Perspectives, 02.05.2013
    Publication Date: 2023-07-18
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  • 72
    Publication Date: 2023-07-18
    Description: Klaus Töpfer, Executive Director of the Institute for Advanced Sustainability Studies (IASS) in Potsdam, former UN Under-Secretary-General and Executive Director of the UN Environment Programme as well as Minister for the Environment in Germany, turned 75 in 2013. His outstanding achievements inspired us to assemble this volume. Klaus Töpfer has been at the forefront of sustainability efforts for several decades, with a long track record of turning vision into reality, and a firm conviction that knowledge can be a crucial building block for transitions towards sustainability. Our world is shaped, more than ever before, by human activities. The scope of technology, to systemically alter nature in ways impossible for previous generations to comprehend, requests and requires a new relationship with »planet Earth.« Such a relationship may speak, in the end, not just of profit and loss but also of a new meaning of wealth, including a sense of ethics, stewardship, and responsibility. For the time being, it seems paramount to face these new challenges, striving for new ways of understanding and, subsequently, new modes of response.
    Description: Ernst Th. Rietschel - Foreword page 9Achim Steiner – Foreword page 11Falk Schmidt, Nick Nuttall - Sustainable, Transformative, Democratic: Klaus Töpfer’s Contributions for Transitions Towards Sustainability page 13Paul J. Crutzen - The Anthropocene: When Humankind Overrides Nature page 21Maheswar Rupakheti and Mark Lawrence - From Buddha Air to Dirty Air to Clean Air: The ABCs of South Asia page 29Veerabhadran Ramanathan - The Two Worlds We Inhabit: The Top Four Billion (T4B) and the Bottom Three Billion (B3B) page 41Hans Joachim Schellnhuber - Climate Change, the Monarch Butterfly, and Intergenerational Contracting page 51Reinhard F. Hüttl - Caring for the ‘Skin of the Earth’—Soils as a Critical Component of Global Development page 61Joachim von Braun - Guiding Urban–Rural Linkages Toward Sustainable Development page 75Ernst Ulrich von Weizsäcker - Klaus Töpfer at 75 page 97Mario Tobias - Translating Knowledge into Action: How Do Innovative Technologies Enable Sustainability? page 103Matthias Kleiner, Caroline A. Lodemann - Science in Democracy—Knowledge Exchange in an Informed Society page 111Carlo Rubbia - Innovative Scientific and Technological Developments for a Coherent Energy Policy page 123Laurence Tubiana, Andreas Rüdinger, Thomas Spencer - Evolution of the Energy Transition in Germany, France, and Europe: A Process in the Making page 127Pekka Haavisto - Global Contract for Sustainability page 141Klaus Milke and Christoph Bals - Acting–Negotiations–Alliances: The ‘Energiewende’ in Germany and its Relevance to the Great Transformation and a Global Contract page 147Karsten Sach - IRENA – A Story of Conviction, Perseverance, and Transformation page 159Manfred Konukiewitz - International Climate Finance for Developing Countries: The Green Climate Fund aims for Transformative Ambition page 173Uwe Schneidewind and Mandy Singer-Brodowski - Enabling the Great Transformation: Transdisciplinarity as Individual and Institutional Challenge page 189Günther Bachmann - Steam Engines, Renewable Energies & Co. page 201Volker Hauff - Governance: The Deficit on the Way to Sustainability page 221WAN Gang - Professor Klaus Töpfer: Promoter of Scientific Cooperation page 233Fengting Li, Jiang Wu, Dahe Jiang,Dong Li, and Sun Jie - Professor Klaus Töpfer: Leading the Way to a Sustainable Future page 237Juan Mayr Maldonado - Klaus Töpfer: A Visionary Leader, Charismatic, and Humanist page 243Massoumeh Ebtekar - Klaus Töpfer: A Pioneer for the Environmental Dimension of Dialogue among Civilizations page 253James Gustave Speth - New Economy Transformation: The Eight-fold Way page 257Timothy E. Wirth - Klaus Töpfer at 75: Remarks of the Honoroble Timothy E. Wirth page 263Ralf Fücks - End or Beginning? page 271Angelika Zahrnt - On the Recapturing of Alternatives page 275Claus Leggewie - Transnational Citizenship. Ideals and European Citizenship: Legal and Cultural Dimensions page 285Ulrich Beck - Transformations of the Social and Political: Beyond Methodological Nationalism page 297Authors page 309
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  • 73
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    In:  Carbon Sequestration in Urban Ecosystems
    Publication Date: 2023-07-18
    Language: English
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  • 74
    Publication Date: 2023-07-18
    Description: Highly porous N-doped carbon materials with apparent surface areas in the 1300-2400 m2 g-1 range and pore volumes up to 1.2 cm 3 g-1 have been synthesized from hydrothermal carbons obtained from mixtures of algae and glucose. The porosity of these materials is made up of uniform micropores, most of them having sizes 〈1 nm. Moreover, they have N contents in the 1.1-4.7 wt% range, and the heteroatom is mainly a pyridone-type structure. These microporous carbons present unprecedented large CO2 capture capacities, up to 7.4 mmol g-1 (1 bar, 0 °C). The importance of the pore size on the CO2 capture capacity of microporous carbon materials is clearly demonstrated. Indeed, a good correlation between the CO2 capture capacity at sub-atmospheric pressure and the volume of narrow micropores is observed. The results suggest that pyridinic-N, pyridonic/pyrrolic-N and quaternary-N do not contribute significantly to the CO2 adsorption capacity, owing probably to their low basicity in comparison with amines. These findings will help the design of high-performance CO2 capture sorbents.
    Language: English
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  • 75
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    In:  Transgovernance: advancing sustainability governance
    Publication Date: 2023-07-18
    Description: It seems intuitive to identify boundaries of an earth system which is increasingly threatened by human activities. Being aware of and hence studying boundaries may be necessary for effective governance of sustainable development. Can the planetary boundaries function as useful ‘warning signs’ in this respect? The answer presented in the article is: yes; but. It is argued that these boundaries cannot be described exclusively by scientific knowledge-claims. They have to be identified by science-society or transdisciplinary deliberations. The discussion of governance challenges related to the concept concludes with two main recommendations: to better institutionalise integrative transdisciplinary assessment processes along the lines of the interconnected nature of the planetary boundaries, and to foster cross-sectoral linkages in order to institutionalise more integrative and yet context sensitive governance arrangements. These insights are briefly confronted with options for institutional reform in the context of the Rio + 20 process. If humankind will not manage a transition towards sustainability, its ‘safe operating space’ continues shrinking. Governance arrangements for such ‘systems at risk’ may then be, first, more ‘forceful’ and, second, may run counter to our understanding of ‘open societies’. It is not very realistic that the world is prepared to achieve the first, and it is not desirable to get the effects of the latter. Scholars and practitioners of sustainability may find this a convincing argument to act now.
    Language: English
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  • 76
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    In:  X. Conference “Policies Against Hunger”
    Publication Date: 2023-07-18
    Language: English
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  • 77
    Publication Date: 2023-07-18
    Description: New multiproxy marine data of the Eemian interglacial (MIS5e) from the Norwegian Sea manifest a cold event with near-glacial surface ocean summer temperatures (3-4 °C). This mid-Eemian cooling divided the otherwise relatively warm interglacial climate and was associated with widespread expansions of winter sea-ice and polar water masses due to changes in atmospheric circulation and ocean stability. While the data also verify a late rather than early last interglacial warm peak, which is in general disharmony with northern hemisphere insolation maximum and the regional climatic progression of the early Holocene, the cold event itself was likely instrumental for delaying the last interglacial climate development in the Polar North when compared with regions farther south. Such a 'climatic decoupling' of the Polar region may bear profound implications for the employment of Eemian conditions to help evaluate the present and future state of the Arctic cryosphere during a warming interglacial.
    Language: English
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  • 78
    Publication Date: 2023-07-18
    Description: Possible feedback effects between aeolian dust, climate and ice sheets are studied for the first time with an Earth system model of intermediate complexity over the late Pleistocene period. Correlations between climate and dust deposition records suggest that aeolian dust potentially plays an important role for the evolution of glacial cycles. Here climatic effects from the dust direct radiative forcing (DRF) caused by absorption and scattering of solar radiation are investigated. Key elements controlling the dust DRF are the atmospheric dust distribution and the absorption-scattering efficiency of dust aerosols. Effective physical parameters in the description of these elements are varied within uncertainty ranges known from available data and detailed model studies. Although the parameters can be reasonably constrained, the simulated dust DRF spans a~wide uncertainty range related to the strong nonlinearity of the Earth system. In our simulations, the dust DRF is highly localized. Medium-range parameters result in negative DRF of several watts per square metre in regions close to major dust sources and negligible values elsewhere. In the case of high absorption efficiency, the local dust DRF can reach positive values and the global mean DRF can be insignificantly small. In the case of low absorption efficiency, the dust DRF can produce a significant global cooling in glacial periods, which leads to a doubling of the maximum glacial ice volume relative to the case with small dust DRF. DRF-induced temperature and precipitation changes can either be attenuated or amplified through a feedback loop involving the dust cycle. The sensitivity experiments suggest that depending on dust optical parameters, dust DRF has the potential to either damp or reinforce glacial–interglacial climate changes.
    Language: English
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  • 79
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    In:  Transgovernance: advancing sustainability governance
    Publication Date: 2023-07-18
    Description: Truth is always concrete, as are emergencies. If truth and reliability of good decisions is what, in general, nourishes change and the readiness of people to trust in transformation, emergency response should be at the heart of this. Responding to emergency situations is about immediate decisions and action. If carried out incorrectly or badly performed, it not only fails in substance, but is likely to destroy and delegitimise any further attempts to transform constraints and contingencies which have caused the emergency situation in the first place. Neither the recent debates on international environmental governance nor those focusing on the multilateral governance framework for sustainable development, emphasise the issue of emergency response. This reluctance is most likely due to the fact that dealing with emergency control is still regarded as a strictly national task. This article believes that this approach is inadequate. It argues that the character of emergencies is changing. Whereas conventional emergencies are mostly local, it is clear that limited and calculable nuclear accidents and the adverse effects of climate change, demonstrate that the modern generation of emergencies has the potential to surpass geographic limits, national borders and to be long term. Therefore, this article argues that emergency control may have an important role in clustering change processes and transition efforts, at least under certain conditions and whilst framed by the concept of transgovernance.
    Language: English
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  • 80
    Publication Date: 2023-07-18
    Description: Emissions of greenhouse gases and air pollutants from megacities impact the climate. The long-lived greenhouse gases CO 2, CH 4 and N 2O as well as climate-active pollutants such as NO x, VOC and particulate matter (PM) are all emitted from megacities. NO x and VOC contribute to tropospheric ozone formation and affect the lifetime of long-lived greenhouse gases. Anthropogenic aerosols include sulphate, black carbon (BC) and particulate organic matter (POM). Aerosols impact climate directly (absorption, backscattering) and also have indirect (cloud) effects. We assess the climate impact of megacity emissions with the Met Office Hadley Centre Earth System Model HadGEM2 applying an "annihilation" scenario in which the emissions at megacities are entirely removed. Generally, the contribution of megacities to global pollutant emissions is on the order of 2-5% of the total global annual anthropogenic base emission flux. The impact of megacity climate-active pollutants is assessed via an annual mean top-of-atmosphere direct radiative forcing (AMTOA-DRF) from long-lived GHG as well as ozone, methane and aerosols. In this simulations the long-lived component (CO 2, CH 4 and N 2O) contributes a positive TOA-DRF of +120.0, +28.4 and +3.3mWm -2, respectively, under present-day conditions. Climate-active pollutants (NO x, VOC) contribute an AMTOA-DRF of +5.7±0.02mWm -2 from an increase in the ozone burden -1.9±0.04mWm -2, -6.1±0.21mWm -2 from the aerosol AMTOA-DRF in the short-wave spectrum and +1.5±0.01mWm -2 from aerosol in the long-wave spectrum. The combined AMTOA-DRF from all climate-active pollutants is slightly negative at -0.8±0.24mWm -2 and the total AMTOA-DRF amounts to +150.9±0.24mWm -2. Under future conditions (2050s) the total AMTOA-DRF from long-lived GHG is found to profoundly increase to +322.6mWm -2 while the total AMTOA-DRF from climate-active pollutants turns positive and decreases slightly to +0.5±0.09mWm -2 yielding a combined AMTOA-DRF of +323.1±0.09mWm -2 in the future. It is apparent that under the given emission scenarios the radiative forcing from long-lived GHG, particularly CO 2, by far dominates the impact of megacities on climate.
    Language: English
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  • 81
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    In:  Transgovernance: advancing sustainability governance
    Publication Date: 2023-07-18
    Description: In this chapter, the Summary and Recommendations are included of the first report of the TransGov project of IASS, Potsdam, authored by Roeland J. in ’t Veld. For this report the contributions to this volume were used as source of inspiration.
    Language: English
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  • 82
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    In:  IASS Blog, 23.12.2014
    Publication Date: 2023-07-18
    Description: Berlin may not be the Netherlands, but there is definitely a fair amount of bicycling infrastructure throughout the city. And if you're biking in Berlin you're not alone on the road with only cars for company either. The debate about which cities are the best for biking aside, I enjoy biking, and this summer I biked home from work at least once a week. For me, this meant a journey of roughly 30 km and just under two hours depending on traffic, traffic lights, and how much energy I had at the end of the work day.
    Language: English
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  • 83
    Publication Date: 2023-07-18
    Description: STORY HIGHLIGHTSManaging soils in a sustainable way is essential in the fight against hunger.This is particularly true with regard to the poorest people in the world, as their survival often hinges on the soils that are most severely degraded.But arable land is very limited.
    Language: English
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  • 84
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    In:  Recarbonization of the biosphere : ecosystems and the global carbon cycle
    Publication Date: 2023-07-18
    Language: English
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  • 85
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    In:  Transgovernance: advancing sustainability governance
    Publication Date: 2023-07-18
    Description: The chapter argues for a lecture of the notion of development as strongly linked to the uneven distribution of material and non-material sources of power among groups. It thus analyses the rise of a public environmentalist awareness in the late twentieth century as a challenge to the capitalist pattern of production and consumption. Finally, the chapter aims to shed some light on the process of mainstreaming these claims by subsuming them within the western model of societal transformation, under the new, catchy label of sustainable development. Pressing for institutional solutions to environmental depletion has meant to further spread the sustainability goal worldwide. On the other hand, it has also implied a kind of betrayal of the truly transformative instances of many social movements and local communities, which were seeking for a revolutionary, rather than reformative, path to societal change.
    Language: English
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  • 86
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    In:  Transgovernance: advancing sustainability governance
    Publication Date: 2023-07-18
    Description: In the late 1960s a debate about the long-term feasibility and desirability of economic growth as a one-size-fits-all economic policy emerged. It was argued that economic growth was one of the underlying causes of ecological and social problems faced by humanity. The issue remained strongly disputed until the inception of the Sustainable Development discourse by which the debate was politically settled. Nevertheless, given that many ecological and social problems remain unsolved and some have become even more severe, there are renewed calls for the abandoning of the economic growth commitment, particularly in already affluent countries. This chapter summarises the growth debate hitherto and examines two alternatives, the steady-state economy proposed by Herman Daly and economic de-growth proposed by Serge Latouche. In spite of recent disputes between the Anglo-Saxon steady-state school and the emerging continental de-growth school, it is argued, consistent with recent contributions on the issue, that steady-state and de-growth are not mutually exclusive but inevitably complements. The steady-state has the advantage of comprehensive theoretical elaboration, while de-growth has the advantage of an attractive political slogan which has re-opened the debate on the issue. Latouche is also a social thinker who gives a voice to the critiques of economic growth contained in the notion of development from outside Europe and the United States. The steady-state economy, and de-growth are held by some analysts to be beyond what is politically feasible. Although this argument is valid, it fails to recognise that past desirable societal changes were made possible through reflexive societal processes conducive to collective action and institutional change. It is concluded that the debate must ultimately rest in the physical quantities that a given economy needs for the ‘good life’ in the long run, how to decide on these quantities, how to achieve them, and how to maintain an approximate global steady-state. Finally, some recommendations for further research along with some reflections on the potential role of scholars are provided.
    Language: English
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  • 87
    Publication Date: 2023-06-21
    Language: English
    Type: info:eu-repo/semantics/report
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  • 88
    Publication Date: 2023-06-21
    Language: English
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  • 89
    Publication Date: 2023-06-21
    Language: English
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  • 90
    Publication Date: 2023-06-21
    Language: English
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  • 91
    Call number: M 23.95223
    Type of Medium: Monograph available for loan
    Pages: 406 Seiten
    Edition: softcover reprint of the original 1st ed. 1974
    ISBN: 978-94-010-2216-3
    Series Statement: Astrophysics and Space Science Library, A Series of Books on the Recent Developments of Space Science and of General Geophysics and Astrophysics Published in Connection with the Journal Space Science Reviews 44
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 92
    Publication Date: 2023-06-16
    Description: The Aegean is the most seismically active and tectonically complex region in Europe. Damaging earthquakes have occurred here throughout recorded history, often resulting in considerable loss of life. The Monte Carlo method of probabilistic seismic hazard analysis (PSHA) is used to determine the level of ground motion likely to be exceeded in a given time period. Multiple random simulations of seismicity are generated to calculate, directly, the ground motion for a given site. Within the seismic hazard analysis we explore the impact of different seismic source models, incorporating both uniform zones and distributed seismicity. A new, simplified, seismic source model, derived from seismotectonic interpretation, is presented for the Aegean region. This is combined into the epistemic uncertainty analysis alongside existing source models for the region, and models derived by a K-means cluster analysis approach. Seismic source models derived using the K-means approach offer a degree of objectivity and reproducibility into the otherwise subjective approach of delineating seismic sources using expert judgment. Similar review and analysis is undertaken for the selection of peak ground acceleration (PGA) attenuation models, incorporating into the epistemic analysis Greek-specific models, European models and a Next Generation Attenuation model. Hazard maps for PGA on a “rock” site with a 10% probability of being exceeded in 50 years are produced and different source and attenuation models are compared. These indicate that Greek-specific attenuation models, with their smaller aleatory variability terms, produce lower PGA hazard, whilst recent European models and Next Generation Attenuation (NGA) model produce similar results. The Monte Carlo method is extended further to assimilate epistemic uncertainty into the hazard calculation, thus integrating across several appropriate source and PGA attenuation models. Site condition and fault-type are also integrated into the hazard mapping calculations. These hazard maps are in general agreement with previous maps for the Aegean, recognising the highest hazard in the Ionian Islands, Gulf of Corinth and Hellenic Arc. Peak Ground Accelerations for some sites in these regions reach as high as 500–600 cm s−2 using European/NGA attenuation models, and 400–500 cm s−2 using Greek attenuation models.
    Language: English
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  • 93
    Publication Date: 2023-06-16
    Description: Pakistan and the western Himalaya is a region of high seismic activity located at the triple junction between the Arabian, Eurasian and Indian plates. Four devastating earthquakes have resulted in significant numbers of fatalities in Pakistan and the surrounding region in the past century (Quetta, 1935; Makran, 1945; Pattan, 1974 and the recent 2005 Kashmir earthquake). It is therefore necessary to develop an understanding of the spatial distribution of seismicity and the potential seismogenic sources across the region. This forms an important basis for the calculation of seismic hazard; a crucial input in seismic design codes needed to begin to effectively mitigate the high earthquake risk in Pakistan. The development of seismogenic source zones for seismic hazard analysis is driven by both geological and seismotectonic inputs. Despite the many developments in seismic hazard in recent decades, the manner in which seismotectonic information feeds the definition of the seismic source can, in many parts of the world including Pakistan and the surrounding regions, remain a subjective process driven primarily by expert judgment. Whilst much research is ongoing to map and characterise active faults in Pakistan, knowledge of the seismogenic properties of the active faults is still incomplete in much of the region. Consequently, seismicity, both historical and instrumental, remains a primary guide to the seismogenic sources of Pakistan. This study utilises a cluster analysis approach for the purposes of identifying spatial differences in seismicity, which can be utilised to form a basis for delineating seismogenic source regions. An effort is made to examine seismicity partitioning for Pakistan with respect to earthquake database, seismic cluster analysis and seismic partitions in a seismic hazard context. A magnitude homogenous earthquake catalogue has been compiled using various available earthquake data. The earthquake catalogue covers a time span from 1930 to 2007 and an area from 23.00° to 39.00°N and 59.00° to 80.00°E. A threshold magnitude of 5.2 is considered for K-means cluster analysis. The current study uses the traditional metrics of cluster quality, in addition to a seismic hazard contextual metric to attempt to constrain the preferred number of clusters found in the data. The spatial distribution of earthquakes from the catalogue was used to define the seismic clusters for Pakistan, which can be used further in the process of defining seismogenic sources and corresponding earthquake recurrence models for estimates of seismic hazard and risk in Pakistan. Consideration of the different approaches to cluster validation in a seismic hazard context suggests that Pakistan may be divided into K = 19 seismic clusters, including some portions of the neighbouring countries of Afghanistan, Tajikistan and India.
    Language: English
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  • 94
    Publication Date: 2023-06-16
    Description: In any probabilistic seismic-hazard model, the earthquake activity that cannot be associated with well-characterized fault structures is taken into account as seismicity distributed over a geographical region. Ground-motion prediction equations (GMPEs) are generally based on predictor variables describing the spatial extension of a rupture. The approach taken to model rupture finiteness can therefore bias the estimation of seismic hazard. We study the effect of rupture finiteness in modeling distributed seismicity using the OpenQuake (OQ) engine, the open-source software for seismic hazard and risk assessment promoted by the Global Earthquake Model initiative. For a simple test case we show how the inclusion of rupture finiteness, with respect to the point-rupture approximation, leads to a significant increase in the probabilities of exceedance for a given level of motion. We then compare the OQ engine with the calculation software developed by the U.S. Geological Survey-National Seismic Hazard Mapping Project. By considering a gridded seismicity model for California, we show how different approaches for modeling finite ruptures affect seismic-hazard estimates. We show how sensitivity to rupture finiteness depends not only on the spatial distribution of activity rates but also on the GMPE model. Considering two sites in Los Angeles and San Francisco, we show that for a return period of 475 years, the percent difference in the associated ground-motion levels when using point and finite ruptures ranges from 19% to 46%; for a return period of 2475 years the difference ranges from 29% to 58%.
    Language: English
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  • 95
    Publication Date: 2023-06-16
    Language: English
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  • 96
    Monograph available for loan
    Monograph available for loan
    New York : Penguin
    Call number: PIK 23-95148
    Description / Table of Contents: "Since it was first published in 1981 Getting to Yes has become a central book in the Business Canon: the key text on the psychology of negotiation. Its message of "principled negotiations"--finding acceptable compromise by determining which needs are fixed and which are flexible for negotiating parties--has influenced generations of businesspeople, lawyers, educators and anyone who has sought to achieve a win-win situation in arriving at an agreement. It has sold over 8 million copies worldwide in 30 languages, and since it was first published by Penguin in 1991 (a reissue of the original addition with Bruce Patton as additional coauthor) has sold over 2.5 million copies--which places it as the #10 bestselling title overall in Penguin Books, and #3 bestselling nonfiction title overall. We have recently relicensed the rights to Getting to Yes, and will be doing a new revised edition--a 30th anniversary of the original publication and 20th of the Penguin edition. The authors will be bringing the book up to date with new material and a assessment of the legacy and achievement of Getting to Yes after three decades"--
    Type of Medium: Monograph available for loan
    Pages: XXIX, 204 S. , graph. Darst. , 20 cm
    Edition: 3. ed., updated and rev.
    ISBN: 9780143118756
    Language: English
    Location: A 18 - must be ordered
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  • 97
    Monograph available for loan
    Monograph available for loan
    London : Penguin
    Call number: PIK 23-95110
    Type of Medium: Monograph available for loan
    Pages: XXIX, 696 S. , Ill., Kt. , 20 cm
    ISBN: 9780141027821
    Language: English
    Branch Library: PIK Library
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  • 98
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    GFZ Data Services
    Publication Date: 2023-03-16
    Description: Abstract
    Description: The EMEC earthquake catalogue is an extension in time and space of the CENEC catalogue (Grünthal et al., 2009, http://doi.org/10.1007/s10950-008-9144-9). It consists of some 45,000 entries in Europe and the Mediterranean area and extends to the west to encompass the North Atlantic Ridge. The criteria are Mw ≥ 3.5 for events with latitude ≥ 44°N and Mw ≥ 4.0 for events with latitude 〈 44°N, in the time period 1000-2006. Data within the catalogue area can be obtained as ASCII-file through the EMEC Earthquake Catalogue Web Service. This webservice also enables the creation of seismicity maps according to user's specifications. In addition, a list of earthquakes in the time period 300-999 for Mw ≥ 6.0 in the catalogue area with latitude ≤ 40°N and longitude ≥ 10°E is given and a list of fake events in the time period 1000-1799.
    Keywords: EMEC ; Earthquake catalogue ; European Mediterranean region ; Unified moment magnitude
    Language: English
    Type: Dataset , Dataset
    Format: 1 Files
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  • 99
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    IUGG Secretariat, KIT Karlsruhe Institute of Technology
    In:  IUGG Annual Report
    Publication Date: 2023-03-01
    Language: English
    Type: info:eu-repo/semantics/report
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  • 100
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    IUGG Secretariat, KIT Karlsruhe Institute of Technology
    In:  IUGG Annual Report
    Publication Date: 2023-03-01
    Language: English
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