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  • English  (73)
  • Wissenschaftspark Albert Einstein  (70)
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  • Naturkundemuseum Potsdam
  • SB Ludwigsfelde
  • Bibliothek des Konservatismus
  • Lehrbuch  (73)
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  • 1
    UID:
    almafu_BV010983272
    Format: XIV, 468 S. : graph. Darst. , 1 Diskette (9 cm)
    ISBN: 0-387-94518-0
    Note: Bd. 1 u.d.T.: Economic and financial modeling with Mathematica. - Systemvoraussetzungen: files can be read on DOS/Windows, Macintosh, NeXT, and UNIX computers; Mathematica 2.2 or later is recommended for maximum use of the diskette files
    Language: English
    Subjects: Computer Science , Economics
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    Keywords: Ökonometrisches Modell ; Mathematica ; Finanzplanungsmodell ; Mathematica ; Aufsatzsammlung ; Aufsatzsammlung ; Aufsatzsammlung ; Lehrbuch
    Author information: Varian, Hal R. 1947-
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  • 2
    Book
    Book
    New York :American Inst. of Physics,
    UID:
    almahu_BV005587615
    Format: XXXIX, 520 S. : , Ill., graph. Darst., Kt.
    ISBN: 0-88318-712-4 , 0-88318-711-6 , 978-0-88318-712-8
    Content: "A superb reference." Physics Today "Will become a classic text in climate research. " Physics World "Valuable to anyone who studies, models, or uses the climate of the earth." Walter Robinson, Bulletin of the American Meteorological Society "Informative and authoritative on a remarkably wide range of topics." Nature Are we entering a period of global warming? Is weather predictable? Physics of Climate offers you an in-depth description of atmospheric circulation and how environmental phenomena worldwide interact in a single, unified system. This integrated approach unites all the key features of the climate system--oceans, atmosphere, and cryosphere--to explain the structure and behavior of climate over time. Ideal for students and professionals in meteorology, oceanography, geophysics, and physics.
    Note: Hier auch später erschienene, unveränderte Nachdrucke
    Language: English
    Subjects: Physics , Geography
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    Keywords: Atmosphäre ; Klimatologie ; Physik ; Dynamische Meteorologie ; Klima ; Lehrbuch
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  • 3
    Book
    Book
    New York :Cambridge University Press,
    UID:
    almafu_BV045246046
    Format: xxxii, 302 Seiten : , Diagramme.
    ISBN: 978-1-108-41987-1 , 978-1-108-41987-1
    Content: "Global climate change is a topic of continuously growing interest. As more international treaties come into force, media coverage has increased and many universities are now starting to conduct courses specifically on climate change laws and policies. This textbook provides a survey of the international law on climate change, explaining how significant international agreements have sought to promote compliance with general norms of international law.Benoit Mayer provides an account of the rules agreed upon through lengthy negotiations under the United Nations Framework Convention on Climate Change (UNFCCC) and multiple other forums on mitigation, geoengineering, adaptation, loss and damage and international support.The International Law on Climate Change is suitable for undergraduate and graduate students studying climate, environmental or international law. It is supported by a suite of online resources featuring regularly updated lists of complementary materials and weblinks, and annually updated briefs for specific chapters"...
    Content: "Climate change is one of the greatest concerns of our time. For more than a quarter century, efforts have been made to mobilize international law as a tool to tackle climate change. Through the outcomes of protracted international negotiations and extensive doctrinal research, a new field of study has gradually emerged in international law. The international law on climate change is a system of State obligations to tackle climate change. It seeks to protect not only the sovereign rights of every State, but also the effective enjoyment of human rights, the interests of future generations and humankind as a whole, as well as other forms of life on Earth. The task is formidable: an attempt at altering the way we are changing our world. Some of the most complex negotiations ever undertaken have only touched the surface of the problem. The challenges are daunting, but the stakes are high and failure is not an option. It is hardly an overstatement that the fate of humankind depends on the international law on climate change"...
    Language: English
    Subjects: Law
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    Keywords: Klimaänderung ; Migration ; Gesetzgebung ; Klimaschutz ; Internationales Umweltrecht ; Lehrbuch
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  • 4
    Book
    Book
    Chichester [u.a.] :Wiley,
    UID:
    almahu_BV021730040
    Format: X, 280 S. : , graph. Darst., Kt. , 1 CD-ROM (12 cm)
    ISBN: 0-470-86172-X , 0-470-86173-8 , 978-0-470-86172-1 , 978-0-470-86173-8
    Content: The weather can be a cause of disruption, despair and even danger everywhere around the world at one time or another. Even when benign it is a source of constant fascination. Applied Atmospheric Dynamics connects this interest with the theoretic underpinnings of fluid dynamics; linking real physical events as diverse as Hurricane Katrina and the strong katabatic winds of Antarctica, with quantitative conceptual models of atmospheric behaviour. Assuming only basic calculus the book provides a physical basis for understanding atmospheric motions around the globe as well as detailing the advances that have led to a greater understanding of weather and climate. The accompanying supplementary cd-rom features colour graphics, maps, databases, animations, project materials, as well as weather data tips.
    Note: Includes bibliographical references and index
    Language: English
    Subjects: Geography
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    Keywords: Allgemeine atmosphärische Zirkulation ; Lehrbuch
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  • 5
    UID:
    almafu_BV043509141
    Format: x, 231 Seiten : , Illustrationen, Diagramme, Karte.
    ISBN: 978-0-691-15761-0
    Content: "Sustainability is a global imperative and a scientific challenge like no other. This concise guide provides students and practitioners with a strategic framework for linking knowledge with action in the pursuit of sustainable development, and serves as an invaluable companion to more narrowly focused courses dealing with sustainability in particular sectors such as energy, food, water, and housing, or in particular regions of the world. Written by leading experts, Pursuing Sustainability shows how more inclusive and interdisciplinary approaches and systems perspectives can help you achieve your sustainability objectives. It stresses the need for understanding how capital assets are linked to sustainability goals through the complex adaptive dynamics of social-environmental systems, how committed people can use governance processes to alter those dynamics, and how successful interventions can be shaped through collaborations among researchers and practitioners on the ground. The ideal textbook for undergraduate and graduate students and an invaluable resource for anyone working in this fast-growing field, Pursuing Sustainability also features case studies, a glossary, and suggestions for further reading. Provides a strategic framework for linking knowledge with action Draws on the latest cutting-edge science and practices. Serves as the ideal companion text to more narrowly focused courses. Utilizes interdisciplinary approaches and systems perspectives. Illustrates concepts with a core set of case studies used throughout the book. Written by world authorities on sustainability. An online illustration package is available to professors"...
    Language: English
    Subjects: Economics , Geography , General works
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    Keywords: Nachhaltigkeit ; Umweltpolitik ; Umweltökonomie ; Nachhaltigkeit ; Ressourcenökonomie ; Nachhaltigkeit ; Lehrbuch ; Glossar enthalten ; Lehrmittel
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  • 6
    Online Resource
    Online Resource
    London : Macmillan International, Red Globe Press
    UID:
    b3kat_BV046997191
    Format: 1 Online-Ressource (xvii, 268 Seiten) , Diagramme
    ISBN: 9781352007527
    Content: This short textbook provides an introduction to queer theory, exploring its key genealogies and terms as well as its application across various academic disciplines and to contemporary life more generally.The authors engage with a wide range of developments in queer theory thinking including discussions of identity politics, transgender theory, intersectionality, post-colonial theory, Indigenous studies, disability studies, affect theory, and more. In offering an updated reflection on the present tensions that queer theory must negotiate, as well as its unfolding future(s), Queer Theory Now is an ideal resource for anyone starting out on their queer theory journey; for students who want to get a grasp of the basic concepts, for teachers looking for a textbook for their queer theory course, or for scholars who want a quick go-to resource for key queer theory ideas and terms
    Additional Edition: Erscheint auch als Druck-Ausgabe, Hardcover ISBN 978-1-352-00784-8
    Additional Edition: Erscheint auch als Druck-Ausgabe, Paperback ISBN 978-1-352-00751-0
    Language: English
    Subjects: Comparative Studies. Non-European Languages/Literatures , Sociology
    RVK:
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    Keywords: Queer-Theorie ; Lehrbuch ; Lehrbuch
    Author information: McCann, Hannah
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  • 7
    UID:
    kobvindex_GFZ122189
    Format: xiii, 210 Seiten , Illustrationen
    Edition: [Final report]
    ISBN: 9780309301831 , 0-309-30183-1
    Content: Once ice-bound, difficult to access, and largely ignored by the rest of the world, the Arctic is now front and center in the midst of many important questions facing the world today. Our daily weather, what we eat, and coastal flooding are all interconnected with the future of the Arctic. The year 2012 was an astounding year for Arctic change. The summer sea ice volume smashed previous records, losing approximately 75 percent of its value since 1980 and half of its areal coverage. Multiple records were also broken when 97 percent of Greenland's surface experienced melt conditions in 2012, the largest melt extent in the satellite era. Receding ice caps in Arctic Canada are now exposing land surfaces that have been continuously ice covered for more than 40,000 years. What happens in the Arctic has far-reaching implications around the world. Loss of snow and ice exacerbates climate change and is the largest contributor to expected global sea level rise during the next century. Ten percent of the world's fish catches comes from Arctic and sub-Arctic waters. The U.S. Geological Survey estimated that up to 13 percent of the world's remaining oil reserves are in the Arctic. The geologic history of the Arctic may hold vital clues about massive volcanic eruptions and the consequent release of massive amount of coal fly ash that is thought to have caused mass extinctions in the distant past. How will these changes affect the rest of Earth? What research should we invest in to best understand this previously hidden land, manage impacts of change on Arctic communities, and cooperate with researchers from other nations? The Arctic in the Anthropocene reviews research questions previously identified by Arctic researchers, and then highlights the new questions that have emerged in the wake of and expectation of further rapid Arctic change, as well as new capabilities to address them. This report is meant to guide future directions in U.S. Arctic research so that research is targeted on critical scientific and societal questions and conducted as effectively as possible. The Arctic in the Anthropocene identifies both a disciplinary and a cross-cutting research strategy for the next 10 to 20 years, and evaluates infrastructure needs and collaboration opportunities. The climate, biology, and society in the Arctic are changing in rapid, complex, and interactive ways. Understanding the Arctic system has never been more critical; thus, Arctic research has never been more important. This report will be a resource for institutions, funders, policy makers, and students. Written in an engaging style, The Arctic in the Anthropocene paints a picture of one of the last unknown places on this planet, and communicates the excitement and importance of the discoveries and challenges that lie ahead.
    Note: MAB0014.001: AWI P5-14-0057 , Contents: SUMMARY. - 1 INTRODUCTION. - Study Context and Charge to the Committee. - Study Approach and Methodology. - Report Organization. - 2 RATIONALE FOR CONTINUED ARCTIC RESEARCH. - 3 EMERGING QUESTIONS. - Evolving Arctic. - Will Arctic communities have greater or lesser influence on their futures?. - Will the land be wetter or drier, and what are the associated implications for surface water, energy balances, and ecosystems?. - How much of the variability of the Arctic system is linked to ocean circulation?. - What are the impacts of extreme events in the new ice-reduced system?. - How will primary productivity change with decreasing sea ice and snow cover?. - How will species distributions and associated ecosystem structure change with the evolving cryosphere?. - Hidden Arctic. - What surprises are hidden within and beneath the ice?. - What is being irretrievably lost as the Arctic changes?. - Why does winter matter?. - What can "break or brake" glaciers and ice sheets?. - How unusual is the current Arctic warmth?. - What is the role of the Arctic in abrupt change?. - What has been the Cenozoic evolution of the Arctic Ocean Basin?. - Connected Arctic. - How will rapid Arctic warming change the jet stream and affect weather patterns in lower latitudes?. - What is the potential for a trajectory of irreversible loss of Arctic land ice, and how will its impact vary regionally?. - How will climate change affect exchanges between the Arctic Ocean andsubpolar basins?. - How will Arctic change affect the long-range transport and persistence of biota?. - How will changing societal connections between the Arctic and the rest of the world affect Arctic communities?. - Managed Arctic. - How will decreasing populations in rural villages and increasing urbanization affect Arctic peoples and societies?. - Will local, regional, and international relations in the Arctic move toward cooperation or conflict?. - How can 21st-century development in the Arctic occur without compromising the environment or indigenous cultures while still benefiting global and Arctic inhabitants?. - How can we prepare forecasts and scenarios to meet emerging management needs?. - What benefits and risks are presented by geoengineering and other large-scale technological interventions to prevent or reduce climate change and associated impacts in the Arctic?. - Undetermined Arctic. - Priority Setting. - 4 MEETING THE CHALLENGES. - Enhancing Cooperation. - Interagency. - International. - Interdisciplinary. - Intersectoral. - Cooperation through Social Media. - Sustaining Long-Term Observations. - Rationale for Long-Term Observations. - Coordinating Long-Term Observation Efforts. - Managing and Sharing Information. - Preserving the Legacy of Research through Data Preservation and Dissemination. - Creating a Culture of Data Preservation and Sharing. - Infrastructure to Ensure Data Flows from Observation to Users, Stakeholders, and Archives. - Data Visualization and Analysis. - Maintaining and Building Operational Capacity. - Mobile Platforms. - Fixed Platforms and Systems. - Remote Sensing. - Sensors. - Power and Communication. - Models in Prediction, Projection, and Re-Analyses. - Partnerships with Industry. - Growing Human Capacity. - Community Engagement. - Investing in Research. - Comprehensive Systems and Synthesis Research. - Non-Steady-State Research. - Social Sciences and Human Capacity. - Stakeholder-Initiated Research. - International Funding Cooperation. - Long-Term Observations. - 5 BUILDING KNOWLEDGE AND SOLVING PROBLEMS. - REFERENCES. - APPENDIXES. - A Acronyms and Abbreviations. - B Speaker and Interviewee Acknowledgments. - C Summary of Questionnaire Responses. - D Biographical Sketches of Committee Members.
    Language: English
    Keywords: Lehrbuch
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  • 8
    UID:
    kobvindex_GFZ1728654289
    Format: 528 Seiten , Illustrationen, Diagramme , 26 cm x 16.5 cm
    Edition: 5th revised edition
    ISBN: 9783866305328 , 386630532X
    Series Statement: European coatings library
    Uniform Title: Das Rheologie-Handbuch 〈engl〉
    Note: Contents 1. Introduction 1.1 Rheology, rheometry and viscoelasticity 1.2 Deformation and flow behavior 1.3 References 2 Flow behavior and viscosity 2.1 Introduction 2.2 Definition of terms 2.2.1 Shear stress 2.2.2 Shear rate 2.2.3 Viscosity 2.3 Shear load-dependent flow behavior 2.3.1 Ideal-viscous flow behavior 2.4 Types of flow illustrated by the Two-Plates model 2.5 References 3 Rotational tests 3.1 Introduction 3.2 Basic principles 3.2.1Test modes-controlled shear rate (CSR) and controlled shear stress (CSS), raw data and rheological parameters 3.3 Flow curves and viscosity functions 3.3.1 Description of the test 3.3.2 Shear-thinning flow behavior 3.3.3 Shear-thickening flow behavior 3.3.4 Yield point 3.3.5 Overview: flow curves and viscosity functions 3.3.6 Fitting functions for flow and viscosity curves 3.3.7 The effects of rheology additives in water-based dispersions 3.4 Time-dependent flow behavior and viscosity function 3.4.1 Test description 3.4.2 Time-dependent flow behavior of samples showing no hardening 3.4.3 Time-dependent flow behavior of samples showing hardening 3.5 Temperature-dependent flow behavior and viscosity function 3.5.1 Test description 3.5.2 Temperature-dependent flow behavior of samples showing no hardening 3.5.3 Temperature-dependent flow behavior of samples showing hardening 3.5.4 Fitting functions for curves of the temperature-dependent viscosity 3.6 Pressure-dependent flow behavior and viscosity function 3.7 References 4 Elastic behavior and shear modulus 4.1 Introduction 4.2 Definition of terms 4.2.1 Deformation and strain 4.2.2 Shear modulus 4.3 Shear load-dependent deformation behavior 4.3.1 Ideal-elastic deformation behavior 4.4 Yield point determination using the shear stress/deformation diagram 4.5 References 5 Viscoelastic behavior 5.1 Introduction 5.2 Basic principles 5.2.1 Viscoelastic liquids according to Maxwell 5.2.2 Viscoelastic solids according to Kelvin/Voigt 5.3 Normal stresses 5.4 References 6 Creep tests 6.1 Introduction 6.2 Basic principles 6.2.1 Description of the test 6.2.2 Ideal-elastic behavior 6.2.3 Ideal-viscous behavior 6.2.4 Viscoelastic behavior 6.3 Analysis 6.3.1 Behavior of the molecules 6.3.2 The Burgers model 6.3.3 Curve discussion 6.3.4 Definition of terms 6.3.5 Data conversion 6.3.6 Determination of the molar mass distribution 6.4 Determination of the yield point via creep tests 6.5 References 7 Relaxation tests 7.1 Introduction 7.2 Basic principles 7.2.1 Description of the test 7.2.2 Ideal-elastic behavior 7.2.3I deal-viscous behavior 7.2.4 Viscoelastic behavior 7.3 Analysis 7.3.1 Behavior of the molecules 7.3.2 Curve discussion 7.3.3 Definition of terms 7.3.4 Data conversion 7.3.5 Determination of the molar mass distribution 7.4 References 8 Oscillatory tests 8.1 Introduction 8.2 Basic principles 8.2.1 Ideal-elastic behavior 8.2.2 Ideal-viscous behavior 8.2.3 Viscoelastic behavior 8.2.4 Definition of terms 8.2.5 The test modes controlled shear strain and controlled shear stress, raw data and rheological parameters 8.3 Amplitude sweeps 8.3.1 Description of the test 8.3.3 Limiting value of the LVE range 8.3.4 Determination of the yield point and the flow point by amplitude sweeps 8.3.5 Frequency-dependence of amplitude sweeps 8.3.6 SAGS and LAOS tests, and Lissajous diagrams 8.4 Frequency sweeps 8.4.1 Description of the test 8.4.2 Behavior of uncrosslinked polymers (solutions and melts) 8.4.3 Behavior of crosslinked polymers5 8.4.4 Behavior of dispersions and gels 8.4.5 Comparison of superstructures using frequency sweeps 8.4.6 Multiwave test 8.4.7 Data conversion 8.5 Time-dependent behavior at constant dynamic-mechanical and isothermal conditions 8.5.1 Description of the test 8.5.2 Time-dependent behavior ofs amples showing no hardening 8.5.3 Time-dependent behavior of samples showing hardening 8.6 Temperature-dependent behavior at constant dynamic mechanical conditions 8.6.1 Description of the test 8.6.2 Temperature-dependent behavior of samples showing no hardening 8.6.3 Temperature-dependent behavior of samples showing hardening 8.6.4 Thermoanalysis (TA) 8.7 Time/temperature shift 8.7.1 Temperature shift factor according to the WLF method 8.8 The Cox/Merz relation 8.9 Combined rotational and oscillatory tests 8.9.1 Presetting rotation and oscillation in series 8.9.2 Superposition of oscillation and rotation 8.10 References 9 Complex behavior, surfactant systems 9.1 Surfactant systems 9.1.1 Surfactant structures and micelles 9.1.2 Emulsions 9.1.3 Mixtures of surfactants and polymers, polymers containing surfactant components 9.1.4 Applications of surfactant systems 9.2 Rheological behavior of surfactant systems 9.2.1 Typical shear behavior 9.2.2 Shear-induced effects, shear-banding and "rheochaos" 9.3 References 10 Measuring systems 10.1 Introduction 10.2 Concentric cylinder measuring systems (CCMS) 10.2.1 Cylinder measuring systems in general 10.2.2 Narrow-gap concentric cylinder measuring systems according to ISO3219 10.2.3 Double-gap measuring systems (DCMS) 10.2.4 High-shear cylinder measuring systems (HSMS) 10.3 Cone-and-plate measuring systems (CPMS) 10.3.1 Geometry 10.3.2 Calculations 10.3.3 Conversion between raw data and rheological parameters 10.3.4 Flow instabilities and secondary flow effects in CP systems 10.3.5 Cone truncation and gap setting 10.3.6 Maximum particle size 10.3.7 Filling of the cone-and-plate measuring system 10.3.8 Advantages and disadvantages of cone-and-plate measuring systems 10.4 Parallel-plate measuring systems (PPMS) 10.4.1 Geometry 10.4.2 Calculations 10.4.3 Conversion between raw data and rheological parameters 10.4.4 Flow instabilities and secondary flow effects in a PP system 10.4.5 Recommendations for gap setting 10.4.6 Automatic gap setting and automatic gap control using the normal force control option 10.4.7 Determination of the temperature gradient in the sample 10.4.8 Advantages and disadvantages of parallel-plate measuring systems 10.5 Mooney/Ewart measuring systems (MEMS) 10.6 Relative measuring systems 10.6.1 Measuring systems with sandblasted, profiled or serrated surfaces 10.6.2 Spindles in the form of disks, pins, and spheres 10.6.3 Krebs spindles 10.6.4 Paste spindles and rotors showing pins and vanes 10.6.5 Ball measuring systems (motion along a circular path) 10.6.6 Further relative measuring systems 10.7 Measuring systems for solid torsion bars 10.7.1 Bars showing a rectangular cross section 10.7.2 Bars showing a circular cross section 10.7.3 Composite materials 10.8 Special measuring devices 10.8.1 Special measuring conditions which influence rheology 10.8.2 Rheo-optical measuring devices 10.8.3 Other special measuring devices 10.8.4 Other kinds of testings besides shear tests 10.9 References 11 Instruments 11.1 Introduction 11.2 Short overview: methods for testing viscosity and elasticity 11.2.1 Very simple determinations 11.2.2 Flow on a horizontal plane 11.2.3 Spreading or slump on a horizontal plane after lifting a container 11.2.4 Flow on an inclined plane 11.2.5 Flow on a vertical plane or over a special tool 11.2.6 Flow in a channel, trough or bowl 11.2.7 Flow cups and other pressureless capillary viscometers 11.2.8 Devices showing rising, sinking, falling and rolling elements 11.2.9 Penetrometers, consistometers and texture analyzers 11.2.10 Pressurized cylinder and capillary devices 11.2.11 Simple rotational viscometer tests 11.2.12 Devices with vibrating oroscillating elements 11.2.13 Rotational and oscillatory curemeters (for rubber testing) 11.2.14 Tension testers 11.2.15 Compression testers 11.2.16 Linear shear testers 11.2.17 Bending or flexure testers 11.2.18 Torsion testers 11.3 Flow cups 11.3.1 ISO cups 11.3.2 Other types of flow cups 11.4 Capillary viscometers 11.4.1 Glas scapillary viscometers 11.4.2 Pressurized capillary viscometers 11.5 Falling-ball viscometers 11.6 Stabinger viscometer 11.7 Rotational and oscillatory rheometers 11.7.1 Rheometer set ups 11.7.2 Controll oops 11.7.3 Devices to measure to
    Language: English
    Keywords: Lehrbuch
    Author information: Mezger, Thomas G. 1954-
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  • 9
    UID:
    kobvindex_GFZ1041332971
    Format: 1 Online-Ressource (XVI, 723 Seiten) , Illustrationen
    Edition: corrected publication 2019
    Edition: Online edition Springer eBook Collection. Biomedical and Life Sciences
    ISBN: 9783319773155 , 978-3-319-77315-5
    Content: Intended as a text for upper-division undergraduates, graduate students and as a potential reference, this broad-scoped resource is extensive in its educational appeal by providing a new concept-based organization with end-of-chapter literature references, self-quizzes, and illustration interpretation. The concept-based, pedagogical approach, in contrast to the classic discipline-based approach, was specifically chosen to make the teaching and learning of plant anatomy more accessible for students. In addition, for instructors whose backgrounds may not primarily be plant anatomy, the features noted above are designed to provide sufficient reference material for organization and class presentation. This text is unique in the extensive use of over 1150 high-resolution color micrographs, color diagrams and scanning electron micrographs. Another feature is frequent side-boxes that highlight the relationship of plant anatomy to specialized investigations in plant molecular biology, classical investigations, functional activities, and research in forestry, environmental studies and genetics, as well as other fields. Each of the 19 richly-illustrated chapters has an abstract, a list of keywords, an introduction, a text body consisting of 10 to 20 concept-based sections, and a list of references and additional readings. At the end of each chapter, the instructor and student will find a section-by-section concept review, concept connections, concept assessment (10 multiple-choice questions), and concept applications. Answers to the assessment material are found in an appendix. An index and a glossary with over 700 defined terms complete the volume
    Note: Contents I Plants as Unique Organisms; History and Tools of Plant Anatomy 1 The Nature of Plants 1.1 Plants Have Multiple Pigments with Multiple Functions 1.2 Plants Use Water, and the Properties of Water, in Unique Ways 1.3 Plants Use Anabolic Metabolism to Manufacture Every Molecule Needed for Growth and Produce Virtually No Waste 1.4 Cell Walls Are Nonliving Matrices Outside the Plant Cell Membrane that House and/or Perform a Variety of Functions 1.5 The Plant Life Cycle Alternates Between a Haploid Gametophyte Stage and a Diploid Sporophyte Stage 1.6 Meristematic Activity Continues Throughout the Life of a Plant 1.7 Fruits Disperse Seeds Through Space: Dormancy Disperses Seeds Through Time 1.8 Earth’s History Is Divided into Four Major Time Periods 1.8.1 The Precambrian: 4550 to 542 mya 1.8.2 The Paleozoic Era: 542 to 251 mya 1.8.3 The Mesozoic Era: 251–66 mya 1.8.4 The Cenozoic Era: 66 mya to Present 1.9 Life on Earth Has Experienced Five Mass Extinctions: A Sixth Is in Progress 1.10 Many Plants and Animals Have Coevolved 1.11 The Plant Body Consists of Four Organs 1.11.1 Roots 1.11.2 Stems 1.11.3 Leaves 1.11.4 Flowers and Fruit 1.12 Plant Organs Are Initially Made of Three Tissues 1.13 “Plant” Can Be Broadly Defined 1.14 Bryophytes Lack Vasculature and Produce Spores 1.15 Ferns and Fern Allies Are Seedless Tracheophytes 1.16 Gymnosperms Are Seed-Producing Tracheophytes that Lack Flowers and Fruit 1.17 Monocots and Eudicots Are the Two Largest Groups of Angiosperms 1.18 Understanding Plant Structure Requires a Sense of Scale 1.19 “Primary” and “Secondary” Are Important Concepts in Plant Anatomy 1.19.1 Primary Versus Secondary Growth and Meristems 1.19.2 Primary Versus Secondary Xylem and Phloem 1.19.3 Primary Versus Secondary Cell Walls 1.20 Chapter Review References and Additional Readings 2 Microscopy and Imaging 2.1 Robert Hooke, 1635–1703, Described a Cell as the Basic Unit of Life by Studying the Bark of the Cork Oak Tree, Quercus suber 2.2 Antoni Van Leeuwenhoek, 1632–1723, Was the First Scientist to Observe Microorganisms 2.3 Nehemiah Grew, 1641–1712, Was the Father of Plant Anatomy 2.4 Robert Brown, 1773–1858, Discovered the Nucleus of the Cell by Studying Orchid Petals 2.5 Katherine Esau, 1898–1997, Advanced the Field of Plant Anatomy with Her Influential Textbooks 2.6 Light Microscopy: The Most Useful Tool of the Plant Anatomist 2.7 The Compound Light Microscope Uses Multiple Lenses to Form and Capture Images 2.8 The Resolving Power of a Lens Places Limits on Resolution and Magnification 2.9 The Confocal Microscope Allows for Sharper Detail, Computer Control, and 3-D Imaging with a Modified Compound Microscope 2.10 Electron Microscopy Allows a View into the World of Cellular Ultrastructure 2.11 The Transmission Electron Microscope Reveals Internal Cellular Detail 2.12 The Scanning Electron Microscope Resolves Surface Detail 2.13 Different Microscopies Produce Different Images of the Same Specimen 2.14 Chapter Review References and Additional Readings II Cellular Plant Anatomy 3 Plant Cell Structure and Ultrastructure 3.1 Plant Cells Are Complex Structures 3.2 Plant Cells Synthesize an External Wall and Contain a Variety of Internal Compartments 3.3 Cells and Cell Organelles Are Typically Bound by Lipid Bilayer Membranes 3.4 Vacuoles Play a Role in Water and Ion Balance 3.5 Plastids Are a Diverse Family of Anabolic Organelles 3.5.1 Proplastid 3.5.2 Etioplast 3.5.3 Elaioplast 3.5.4 Amyloplast 3.5.5 Chromoplast 3.5.6 Gerontoplast 3.5.7 Chloroplast 3.5.8 Chloroplast Functions 3.5.9 The Dimorphic Chloroplasts of C 4 Photosynthesis 3.5.10 Guard Cell Chloroplasts 3.5.11 Sun Versus Shade Chloroplasts 3.6 All Plastids Are Developmentally Related 3.7 Mitochondria Synthesize ATP and Small Carbon Skeletons 3.8 Microbodies Are the Site of Specific Biochemical Pathways 3.9 The Endoplasmic Reticulum Synthesizes Proteins and Some Lipids 3.10 The Golgi Apparatus Processes and Packages Polysaccharides and Proteins for Secretion 3.11 The Nucleus Houses the Cell’s Genetic Material and Participates in Ribosome Synthesis 3.12 The Cytoskeleton Organizes the Cell and Helps Traffic Organelles 3.13 Chapter Review References and Additional Readings 4 Mitosis and Meristems 4.1 The Plant Cell Cycle Includes Interphase, Mitosis, and Cytokinesis 4.2 A Pre-prophase Microtubule Band Precedes Mitosis and Defines the Plane of Cell Division 4.3 Mitosis May Be Divided into Distinct, but Continuous, Stages 4.4 Cytokinesis Begins with Initiation of the Cell Plate and Grows by the Deposition of Callose 4.5 Microtubules Play a Critical Role in Mitosis and Cytokinesis 4.6 Apical Meristems Are the Sites of Primary Growth 4.7 The Shoot Apical Meristem Is the Site of Lateral Organ Initiation 4.8 Axillary Buds Arise De Novo in the Developing Leaf Axis 4.9 Tunica-Corpus Organization Describes Shoot Apical Meristem Growth in Many Eudicots 4.10 Gymnosperms Do Not Possess a Tunica-Corpus 4.11 The Root Apical Meristem Provides the Primary Growth of Roots 4.12 Lateral Roots Originate from Inside the Pericycle, Not from the Root Apical Meristem 4.13 Intercalary Meristems Contribute to Stem and Leaf Growth in Monocots 4.14 Many Lower Vascular Plants Have a Single Initial Cell in the Shoot and Root Apical Meristems 4.15 Lateral Meristems Are the Site of Secondary Growth in Eudicots 4.16 Chapter Review References and Additional Readings 5 Cell Walls 5.1 Transparent Plant Cell Walls Contain Cellulose and Are Synthesized to the Exterior of the Protoplast 5.2 Primary Cell Walls Are a Structural Matrix of Cellulose and Several Other Components 5.3 Plasmodesmata Connect Adjacent Cells Via Holes in the Primary Cell Wall 5.4 Secondary Cell Walls Are Rigid, Thick, and Lignified 5.5 Pits Are Holes in the Secondary Cell Wall 5.6 Transfer Cells Have Elaborated Primary Cell Walls for High Rates of Transport 5.7 Chapter Review References and Additional Readings 6 Parenchyma, Collenchyma, and Sclerenchyma 6.1 Parenchyma Cells Are the Most Common Plant Cell Type 6.2 Parenchyma Cells May Exhibit Totipotency 6.3 Collenchyma Cells Are Used for Support and Are the Least Common Cell Type 6.4 Birefringence Is a Common Phenomenon in Collenchyma Walls 6.5 Sclerenchyma Cells Provide Support, Protection, and Long-Distance Water Transport 6.6 Fibers Impart Support and Protection 6.7 Sclereids Are Reduced Sclerenchyma Cells That Occur Singly or in Clumps 6.8 Xylem Vessel Elements Are Water-Conducting Sclerenchyma 6.9 Chapter Review References and Additional Readings III Vascular Tissues 7 Xylem 7.1 Xylem Is a Complex Tissue Containing Multiple Cell Types, Each with a Specific Structure and Function 7.2 The Primary Functions of Xylem Are Water Conduction, Mineral Transport, and Support 7.3 Tracheids Are Imperforate Tracheary Elements and the Sole Water Conductors in Gymnosperms 7.4 Angiosperm Tracheids, Fiber Tracheids, and Libriform Fibers Represent a Continuum of Imperforate Tracheary Element Design and Function 7.5 Vessel Elements Are Perforate Cells and the Main Water Conductors in Angiosperms 7.6 Vessel Element Side Walls Are Patterned for Strength and Water Movement 7.7 Most Vessel Elements End in a Perforation Plate and Are Connected to Another Vessel Element 7.8 Xylem Parenchyma Are Living Cells Involved in Xylem Metabolism and Protection 7.9 Chapter Review References and Additional Readings 8 Phloem 8.1 Phloem Is a Complex Tissue Containing Multiple Cell Types, Each with a Specific Structure and Function 8.2 Phloem’s Main Function Is Photosynthate Translocation 8.3 Sieve Tube Elements Are Living Cells Responsible for Translocation 8.4 Companion Cells Support the Sieve Tube Element and Are Involved in Phloem Loading and Unloading in Angiosperms 8.5 Phloem Parenchyma Cells Are Involved in Radial Translocation, Xylem/Phloem Coordination, and Storage 8.6 Phloem Fibers Protect the Delicate Sieve Tubes 8.7 Secondary Phloem Typically Only Functions for One Growing Season 8.8 Gymnosperm Phloem Is Simpler Than An
    Language: English
    Keywords: Electronic books ; Lehrbuch
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    kobvindex_GFZ166673425X
    Format: 1 Online-Ressource (xxiii, 346 Seiten) , Illustrationen, Diagramme, Karten (überwiegend farbig)
    Edition: Tthird edition
    ISBN: 9783030104665 , 978-3-030-10466-5
    Content: It is not so long ago (a mere 17,000 years – a blink in geologic time) that vast areas of the Northern Hemisphere were covered with ice sheets up to two miles thick, lowering the oceans by more than 120 m. By 11,000 years ago, most of the ice was gone. Evidence from polar ice cores and ocean sediments show that Ice Ages were persistent and recurrent over the past 800,000 years. The data suggests that Ice Ages were the normal state, and were temporarily interrupted by interglacial warm periods about nine times during this period. Quasi-periodic variations in the Earth cause the solar input to high northern latitudes to vary with time over thousands of years. The widely accepted Milankovitch theory implies that the interglacial warm periods are associated with high solar input to high northern latitudes. However, many periods of high solar input to high northern latitudes occur during Ice Ages while the ice sheets remain. The data also indicates that Ice Ages will persist regardless of solar input to high northern latitudes, until several conditions are met that are necessary to generate a termination of an Ice Age. An Ice Age will not terminate until it has been maturing for many tens of thousands of years leading to a reduction of the atmospheric CO2 concentration to less than 200 ppm. At that point, CO2 starvation coupled with lower temperatures will cause desertification of marginal regions, leading to the generation of large quantities of dust. High winds transfer this dust to the ice sheets greatly increasing their solar absorptivity, and at the next up-lobe in the solar input to high northern latitudes, solar power melts the ice sheets over about a 6,000-year interval. A warm interglacial period follows, during which dust levels drop remarkably. Slowly but surely, ice begins accumulating again at high northern latitudes and an incipient new Ice Age begins. This third edition presents data and models to support this theory
    Note: Contents 1 History and Description of Ice Ages 1.1 Discovery of Ice Ages 1.2 Description of Ice Sheets 1.3 Vegetation During LGM 1.3.1 LGM Climate 1.3.2 Global Flora 1.3.3 Ice Age Forests 1.4 Vegetation and Dust Generation During the LGM 1.4.1 Introduction: Effect of Low CO2 on Plants 1.4.2 C3 and C4 Flora Differences 1.4.3 Effects of Low CO2 on Tree Lines 1.4.4 Source of the LGM Dust 2 Variability of the Earth’s Climate 2.1 Factors that Influence Global Climate 2.2 Stable Extremes of the Earth’s Climate 2.3 Ice Ages in the Recent Geological Past 3 Ice Core Methodology 3.1 History of Ice Core Research 3.2 Dating Ice Core Data 3.2.1 Introduction 3.2.2 Age Markers 3.2.3 Counting Layers Visually 3.2.4 Layers Determined by Measurement 3.2.5 Ice Flow Modeling 3.2.6 Other Dating Methods 3.2.7 Synchronization of Dating of Ice Cores from Greenland and Antarctica 3.2.8 GISP2 Experience 3.2.9 Tuning 3.2.10 Flimsy Logic 3.3 Processing Ice Core Data 3.3.1 Temperature Estimates from Ice Cores 3.3.2 Temperature Estimates from Borehole Models 3.3.3 Climate Variations 3.3.4 Trapped Gases 4 Ice Core Data 4.1 Greenland Ice Core Historical Temperatures 4.2 Antarctica Ice Core Historical Temperatures 4.2.1 Vostok and EPICA Data 4.2.2 Homogeneity of Antarctic Ice Cores 4.3 North-South Synchrony 4.3.1 Direct Comparison of Greenland and Antarctica Ice Core Records 4.3.2 Sudden Changes 4.3.3 Interpretation of Sudden Change in Terms of Ocean Circulation 4.3.4 Seasonal Variability of Precipitation 4.4 Data from High-Elevation Ice Cores 4.5 Carbon Dioxide 4.5.1 Measurements 4.5.2 Explanations 4.6 Dust in Ice Cores 5 Ocean Sediment Data 5.1 Introduction 5.2 Chronology 5.3 Universality of Ocean Sediment Data 5.4 Summary of Ocean Sediment Ice Volume Data 5.5 Comparison of Ocean Sediment Data with Polar Ice Core Data 5.6 Historical Sea Surface Temperatures 5.7 Ice-Rafted Debris 6 Other Data Sources 6.1 Devil’s Hole 6.1.1 Devil’s Hole Data 6.1.2 Comparison of Devil’s Hole Data with Ocean Sediment Data 6.1.3 Devil’s Hole: Global or Regional Data? 6.1.4 Comparison of Devil’s Hole Data with Vostok Data 6.1.5 The Continuing Controversy 6.2 Speleothems in Caves 6.3 Magnetism in Rocks and Loess 6.3.1 Magnetism in Loess 6.3.2 Rock Magnetism in Lake Sediments 6.4 Pollen Records 6.5 Physical Indicators 6.5.1 Ice Sheet Moraines 6.5.2 Coral Terraces 6.5.3 Mountain Glaciers 6.6 Red Sea Sediments 7 Overview of the Various Models for Ice Ages 7.1 Introduction 7.2 Variability of the Sun 7.3 Astronomical Theory 7.4 Volcanism 7.5 Greenhouse Gases 7.6 Role of the Oceans 7.6.1 Glacial-Interglacial Cycles: The Consensus View 7.6.2 Sudden Climate Change - The Consensus View 7.6.3 Wunsch’s Objections 7.7 Models Based on Clouds 7.7.1 Extraterrestrial Dust Accretion 7.7.2 Clouds Induced by Cosmic Rays 7.7.3 Ocean–Atmosphere Model 7.8 Models Based on the Southern Hemisphere 8 Variability of the Earth’s Orbit: Astronomical Theory 8.1 Introduction 8.2 Variability of the Earth’s Orbit 8.2.1 Variability Within the Orbital Plane 8.2.2 Variability of the Orbital Plane 8.3 Calculation of Solar Intensities 8.4 Importance of Each Orbital Parameter 8.5 Historical Solar Irradiance at Higher Latitudes 8.6 Connection Between Solar Variability and Glaciation/Deglaciation Cycles According to Astronomical Theory 8.6.1 Models for Ice Volume 8.6.2 Review of the Imbries’ Model 8.6.3 Memory Model 8.6.4 Modification of Paillard Model 8.7 Models Based on Eccentricity or Obliquity 8.7.1 A Model Based on Eccentricity 8.7.2 The Middle-Pleistocene Transition (MPT) 9 Comparison of Astronomical Theory with Data 9.1 Ice Volume Versus Solar Input 9.2 Spectral Analysis 9.2.1 Introduction 9.2.2 Spectral Analysis of Solar and Paleoclimate Data 10 Interglacials 11 Terminations of Ice Ages 11.1 Abstract 11.2 Background 11.3 Terminations 11.4 North or South (or Both)? 11.5 Models Based on CO 2 and the Southern Hemisphere 11.6 Climate Models for Terminations of Ice Ages 11.7 Model Based on Solar Amplitudes 11.8 Dust as the Driver for Terminations 11.8.1 Introduction 11.8.2 Antarctic Dust Data 11.8.3 Correlation of Ice Core Dust Data with Terminations 11.8.4 Dust Levels on the Ice Sheets 11.8.5 Optical Properties of Surface Deposited Dust 11.8.6 Source of the Dust 11.8.7 Ice Sheet Margins 11.9 Model Based on Solar Thresholds 11.10 The Milankovitch Model Versus the Most Likely Model 11.10.1 Criteria for a Theory 11.10.2 The “Milankovitch” Model 11.10.3 The Most Likely Model 11.10.4 Unanswered Questions 12 Status of Our Understanding References Index
    Language: English
    Subjects: Earth Sciences , Geography
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