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  • 2000-2004  (2,485)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Tulsa, Okla. : PennWell
    Call number: PIK P 124-08-0025
    Type of Medium: Monograph available for loan
    Pages: x, 283 p. : ill. : 24 cm
    ISBN: 0878147896
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  • 2
    Monograph available for loan
    Monograph available for loan
    London ; Sterling : Earthscan
    Call number: PIK B 160-03-0117
    Type of Medium: Monograph available for loan
    Pages: 358 p. + CD
    Edition: 1. ed.
    ISBN: 1853839477
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  • 3
    Call number: PIK N 456-03-0125 ; AWI G5-04-0014
    In: International geophysics series, Volume 80
    Type of Medium: Monograph available for loan
    Pages: XXIX, 354 Seiten , Illustrationen
    ISBN: 0126173311 , 0-12-617331-1
    Series Statement: International geophysics series 80
    Language: English
    Note: Contents Prologue Acknowledgments List of Symbols PART I Foundations 1 INTRODUCTION: The Basic Challenge 1.1 The Climate System 1.2 Some Basic Observations 1.3 External Forcing 1.3.1 Astronomical Forcing 1.3.2 Tectonic Forcing 1.4 The Ice-Age Problem 2 TECHNIQUES FOR CLIMATE RECONSTRUCTION 2.1 Historical Methods 2.1.1 Direct Quantitative Measurements 2.1.2 Descriptive Accounts of General Environmental Conditions 2.2 Surficial Biogeologic Proxy Evidence 2.2.1 Annually Layered Life Forms 2.2.2 Surface Geomorphic Evidence 2.3 Conventional Nonisotopic Stratigraphic Analyses of Sedimentary Rock and Ice 2.3.1 Physical Indicators 2.3.2 Paleobiological Indicators (Fossil Faunal Types and Abundances) 2.4 Isotopic Methods 2.4.1 Oxygen Isotopes 2.4.2 Deuterium and Beryllium in Ice Cores 2.4.3 Stable Carbon Isotopes 2.4.4 Strontium and Osmium Isotopes 2.5 Nonisotopic Geochemical Methods 2.5.1 Cadmium Analysis 2.5.2 Greenhouse Gas Analysis of Trapped Air in Ice Cores 2.5.3 Chemical and Biological Constituents and Dust Layers in Ice Cores 2.6 Dating the Proxy Evidence (Geochronometry) 3 A SURVEY OF GLOBAL PALEOCLIMATIC VARIATIONS 3.1 The Phanerozoic Eon (Past 600 My) 3.2 The Cenozoic Era (Past 65 My) 3.3 The Plio-Pleistocene (Past 5 My) 3.4 Variations during the Last Ice Age: IRD Events 3.5 The Last Glacial Maximum (20 ka) 3.6 Postglacial Changes: The Past 20 ky 3.7 The Past 100 Years 3.8 The Generalized Spectrum of Climatic Variance 3.9 A Qualitative Discussion of Causes 4 GENERAL THEORETICAL CONSIDERATIONS 4.1 The Fundamental Equations 4.2 Time Averaging and Stochastic Forcing 4.3 Response Times and Equilibrium 4.4 Spatial Averaging 4.5 Climatic-Mean Mass and Energy Balance Equations 4.5.1 The Water Mass Balance 4.5.2 Energy Balance 5 SPECIAL THEORETICAL CONSIDERATIONS FOR PALEOCLIMATE: Structuring a Dynamical Approach 5.1 A Basic Problem: Noncalculable Levels of Energy and Mass Flow 5.2 An Overall Strategy 5.3 Notational Simplifications for Resolving Total Climate Variability 5.4 A Structured Dynamical Approach 5.5 The External Forcing Function, F 5.5.1 Astronomical/Cosmic Forcing 5.5.2 Tectonic Forcing 6 BASIC CONCEPTS OF DYNAMICAL SYSTEMS ANALYSIS: Prototypical Climatic Applications 6.1 Local (or Internal) Stability 6.2 The Generic Cubic Nonlinearity 6.3 Structural (or External) Stability: Elements of Bifurcation Theory 6.4 Multivariable Systems 6.4.1 The Two-Variable Phase Plane 6.5 A Prototype Two-Variable Model 6.5.1 Sensitivity of Equilibria to Changes in Parameters: Prediction of the Second Kind 6.5.2 Structural Stability 6.6 The Prototype Two-Variable System as a Stochastic-Dynamical System: Effects of Random Forcing 6.6.1 The Stochastic Amplitude 6.6.2 Structural Stochastic Stability 6.7 More Than Two-Variable Systems: Deterministic Chaos PART II Physics of the Separate Domains 7 MODELING THE ATMOSPHERE AND SURFACE STATE AS FAST-RESPONSE COMPONENTS 7.1 The General Circulation Model 7.2 Lower Resolution Models: Statistical-Dynamical Models and the Energy Balance Model 7.2.1 A Zonal-Average SDM 7.2.2 Axially Asymmetric SDMs 7.2.3 The Complete Time-Average State 7.3 Thermodynamic Models 7.3.1 Radiative-Convective Models 7.3.2 Vertically Averaged Models (the EBM) 7.4 The Basic Energy Balance Model 7.5 Equilibria and Dynamical Properties of the Zero-Dimensional (Global Average) EBM 7.6 Stochastic Resonance 7.7 The One-Dimensional (Latitude-Dependent) EBM 7.8 Transitivity Properties of the Atmospheric and Surface Climatic State: Inferences from a GCM 7.9 Closure Relationships Based on GCM Sensitivity Experiments 7.9.1 Surface Temperature Sensitivity 7.10 Formal Feedback Analysis of the Fast-Response Equilibrium State 7.11 Paleoclimatic Simulations 8 THE SLOW-RESPONSE "CONTROL" VARIABLES: An Overview 8.1 The Ice Sheets 8.1.1 Key Variables 8.1.2 Observations 8.2 Greenhouse Gases: Carbon Dioxide 8.3 The Thermohaline Ocean State 8.4 A Three-Dimensional Phase-Space Trajectory 9 GLOBAL DYNAMICS OF THE ICE SHEETS 9.1 Basic Equations and Boundary Conditions 9.2 A Scale Analysis 9.3 The Vertically Integrated Ice-Sheet Model 9.4 The Surface Mass Balance 9.5 Basal Temperature and Melting 9.6 Deformable Basal Regolith 9.7 Ice Streams and Ice Shelves 9.8 Bedrock Depression 9.9 Sea Level Change and the Ice Sheets: The Depression-Calving Hypothesis 9.10 Paleoclimatic Applications of the Vertically Integrated Model 9.11 A Global Dynamical Equation for Ice Mass 10 DYNAMICS OF ATMOSPHERIC CO2 10.1 The Air-Sea Flux, Q↑ 10.1.1 Qualitative Analysis of the Factors Affecting Q↑ 10.1.2 Mathematical Formulation of the Ocean Carbon Balance 10.1.3 A Parameterization for Q↑ 10.2 Terrestrial Organic Carbon Exchange, W↑G 10.2.1 Sea Level Change Effects 10.2.2 Thermal Effects 10.2.3 Ice Cover Effects 10.2.4 Long-Term Terrestrial Organic Burial, W↓G 10.2.5 The Global Mass Balance of Organic Carbon 10.3 Outgassing Processes, V↑ 10.4 Rock Weathering Downdraw, W↓ 10.5 A Global Dynamical Equation for Atmospheric CO2 10.6 Modeling the Tectonically Forced CO2 Variations, µˆ : Long-Term Rock Processes 10.6.1 The Long-Term Oceanic Carbon Balance 10.6.2 The GEOCARB Model 10.7 Overview of the Full Global Carbon Cycle 11 SIMPLIFIED DYNAMICS OF THE THERMOHALINE OCEAN STATE 11.1 General Equations 11.1.1 Boundary Conditions 11.2 A Prototype Four-Box Ocean Model 11.3 The Wind-Driven, Local-Convective, and Baroclinic Eddy Circulations 11.3.1 The Wind-Driven Circulation: Gyres and Upwelling 11.3.2 Local Convective Overturnings and Baroclinic Eddy Circulations 11.4 The Two-Box Thermohaline Circulation Model: Possible Bimodality of the Ocean State 11.4.1 The Two-Box System 11.4.2 A Simple Model of the TH Circulation 11.4.3 Meridional Fluxes 11.4.4 Dynamical Analysis of the Two-Box Model 11.5 Integral Equations for the Deep Ocean State 11.5.1 The Deep Ocean Temperature 11.5.2 The Deep Ocean Salinity 11.6 Global Dynamical Equations for the Thermohaline State: θ and Sφ PART III Unified Dynamical Theory 12 THE COUPLED FAST- AND SLOW-RESPONSE VARIABLES AS A GLOBAL DYNAMICAL SYSTEM: Outline of a Theory of Paleoclimatic Variation 12.1 The Unified Model: A Paleoclimate Dynamics Model 12.2 Feedback-Loop Representation 12.3 Elimination of the Fast-Response Variables: The Center Manifold 12.4 Sources of Instability: The Dissipative Rate Constants 12.5 Formal Separation into Tectonic Equilibrium and Departure Equations 13 FORCED EVOLUTION OF THE TECTONIC-MEAN CLIMATIC STATE 13.1 Effects of Changing Solar Luminosity and Rotation Rate 13.1.1 Solar Luminosity (S) 13.1.2 Rotation Rate (Ω) 13.2 General Effects of Changing Land-Ocean Distribution and Topography (h) 13.3 Effects of Long-Term Variations of Volcanic and Cosmic Dust and Bolides 13.4 Multimillion-Year Evolution of CO2 13.4.1 The GEOCARB Solution 13.4.2 First-Order Response of Global Ice Mass and Deep Ocean Temperature to Tectonic CO2 Variations 13.5 Possible Role of Salinity-Driven Instability of the Tectonic-Mean State 13.6 Snapshot Atmospheric and Surficial Equilibrium Responses to Prescribed y-Fields Using GCMs 14 THE LATE CENOZOIC ICE-AGE DEPARTURES: An Overview of Previous Ideas and Models 14.1 General Review: Forced vs. Free Models 14.1.1 Models in Which Earth-Orbital Forcing Is Necessary 14.1.2 Instability-Driven (Auto-oscillatory) Models 14.1.3 Hierarchical Classification in Terms of Increasing Physical Complexity 14.2 Forced Ice-Line Models (Box 1, Fig. 14-1) 14.3 Ice-Sheet Inertia Models 14.3.1 The Simplest Forms (Box 2) 14.3.2 More Physically Based Ice-Sheet Models: First Applications 14.3.3 Direct Bedrock Effects (Box 3) 14.3.4 Bedrock-Calving Effects (Box 4) 14.3.5 Basal Meltwater and Sliding (Box 5) 14.3.6 Ice Streams and Ice Shelf Effects 14.3.7 Continental Ice-Sheet Movement (Box 6) 14.3.8 Three-Dimensional (λ, φ, hI) Ice-Sheet Models 14.4 The Need for Enhancement of the Coupled Ice-Sheet/Atmospheric Climate Models 14.5 Ice-Sheet Variables Coupled with Additional Slow-Response Variables 14.5.1 Regolith Mass, mr (Box 7) 14.5.2 The Deep Ocean Te
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  • 4
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Routledge
    Call number: AWI A3-02-0037
    Description / Table of Contents: Synoptic and dynamic climatology provides the first comprehensive account of the dynamical behaviour and mechanisms of the global climate system and its components, together with a modern survey of synoptic-scale weather systems in the tropics and extratropics, and of the methods and applications of synoptic climate classification. It is unrivalled in the scope and detail of its contents. The work is thoroughly up to date, with extensive reference sections by chapter. It is illustrated with plates and nearly 300 figures. Part 1 provides an introduction to the global climate system and the space-time scales of weather and climate processes, followed by a chapter on climate data and their analysis. Part 2 describes and explains the characteristics of the general circulation of the global atmosphere, planetary waves and blocking behavior, and the nature and causes of global teleconnection patterns. Part 3 discusses synoptic weather systems in the extratropics and tropics, and satellite-based climatologies of synoptic features. It also describes the methods and applications of synoptic climatology and summarizes current climatic research and its directions. The book is intended for advanced students in climatology and environmental and atmospheric sciences, as well as for professionals in the field of climate dynamics and variability. It presents both established findings about global climate and unresolved issues. Its comprehensive reference lists provide an invaluable guide to further study.
    Type of Medium: Monograph available for loan
    Pages: XV, 620 S., [2] Bl. : Ill., graph. Darst., Kt.
    Edition: 1. publ.
    ISBN: 0415031168
    Note: Contents: List of plates. - Preface. - Acknowledgments. - PART 1 The climate system and its study. - 1 Introduction. - 1.1 The global climate system. - 1.2 Time and space scales of weather and climate processes. - 1.3 Dynamic and synoptic climatology. - 1.4 The structure of the book. - 2 Climate data and their analysis. - 2.1 Synoptic meteorological data. - 2.2 Remotely sensed data. - 2.3 Climate variables and their statistical description. - 2.4 Analytical tools for spatial data. - 2.5 Time series. - 2.6 Empirical orthogonal function analysis, clustering, and classification. - Appendix 2.1 Eulerian and Lagrangian methods. - PART 2 Dynamic climatology. - 3 Global climate and the general circulation. - 3.1 Planetary controls. - 3.2 Basic controls of the atmospheric circulation and its maintenance. - 3.3 Circulation cells. - 3.4 The Earth's geography. - 3.5 Climate system feedbacks. - 3.6 General circulation models. - 3.7 The global circulation-description. - 3.8 Centers of action. - 3.9 Global climatic features. - 3.10 Air masses. - Appendix 3.1 Potential vorticity. - 4 Large-scale circulation and climatic characteristics. - 4.1 Time-averaged circulation. - 4.2 Jetstreams. - 4.3 Planetary waves. - 4.4 Zonal index. - 4.5 Zonal and blocking flow modes. - 4.6 Blocking mechanisms.- 4.7 Low-frequency circulation variability and persistence. - 4.8 Intraseasonal oscillations. - Appendix 4.1 Spectral harmonic functions. - Appendix 4.2 Eliassen-Palm flux. - Appendix 4.3 Normal modes. - 5 Global teleconnections. - 5.1 Pressure oscillations and teleconnection patterns. - 5.2 The Southern Oscillation and El Niño. - 5.3 ENSO mechanisms. - 5.4 Teleconnections with ENSO. - 5.5 Extratropical teleconnection patterns. - 5.6 North Atlantic Oscillation. - 5.7 North Pacific Oscillation. - 5.8 Zonally symmetric oscillations. - 5.9 The southern hemisphere. - 5.10 Tropical-extratropical teleconnections. - 5.11 Teleconnections and synoptic-scale activity. - 5.12 Time-scale aspects of teleconnections. - 5.13 Interannual to interdecadal oscillations. - Appendix 5.1 Partitioning between equatorially symmetric and antisymmetric components. - PART 3 Synoptic climatology. - 6 Synoptic systems. - 6.1 Early studies of extra tropical systems. - 6.2 Climatology of cyclones and anticyclone. - 6.3 Development of cyclones. - 6.4 Storm tracks. - 6.5 Satellite-based climatologies of synoptic features. - 6.6 Synoptic-scale systems in the tropics. - Appendix 6.1 The Q-vector formulation. - 7 Synoptic climatology and its applications / Roger G. Barry and Allen H. Perry. - 7.1 Synoptic pattern classification. - 7.2 Subjective typing procedures. - 7.3 Objective typing procedures. - 7.4 Principal catalogs and their uses. - 7.5 Regional applications. - 7.6 Analogs. - 7.7 Seasonal structure. - 7.8 Climatic trends. - 7.9 Environmental applications. - 8 Retrospect and prospect. - Further reading. - Index.
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  • 5
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Routledge
    Call number: AWI A5-18-91525
    Type of Medium: Monograph available for loan
    Pages: XVI, 421 S. , Ill., graph. Darst., Kt. , 25cm
    Edition: 8. ed.
    ISBN: 0415271711 (pbk.) , 0415271703
    Language: English
    Note: Contents: Preface to the eighth edition. - Acknowledgements. - 1 INTRODUCTION AND HISTORY OF METEOROLOGY AND CLIMATOLOGY. - A The atmosphere. - B Solar energy. - C Global circulation. - D Climatology. - E Mid-latitude disturbances. - F Tropical weather. - G Palaeoclimates. - H The global climate system. - 2 ATMOSPHERIC COMPOSITION, MASS AND STRUCTURE. - A Composition of the atmosphere. - 1 Primary gases. - 2 Greenhouse gases. - 3 Reactive gas species. - 4 Aerosols. - 5 Variations with height. - 6 Variations with latitude and season. - 7 Variations with time. - B Mass of the atmosphere. - 1 Total pressure. - 2 Vapour pressure C The layering of the atmosphere. - 1 Troposphere. - 2 Stratosphere. - 3 Mesosphere. - 4 Thermosphere. - 5 Exosphere and magnetosphere. - 3 SOLAR RADIATION AND THE GLOBAL ENERGY BUDGET. - A Solar radiation. - 1 Solar output. - 2 Distance from the sun. - 3 Altitude of the sun. - 4 Length of day. - B Surface receipt of solar radiation and its effects. - 1 Energy transfer within the earth-atmosphere system. - 2 Effect of the atmosphere. - 3 Effect of cloud cover. - 4 Effect of latitude. - 5 Effect ofland and sea. - 6 Effect of elevation and aspect. - 7 Variation of free-air temperature with height. - C Terrestrial infra-red radiation and the greenhouse effect. - D Heat budget of the earth. - E Atmospheric energy and horizontal heat transport. - 1 The horizontal transport of heat. - 2 Spatial pattern of the heat budget components. - 4 ATMOSPHERIC MOISTURE BUDGET. - A The global hydrological cycle. - B Humidity. - 1 Moisture content. - 2 Moisture transport. - C Evaporation. - D Condensation. - E Precipitation characteristics and measurement. - 1 Forms of precipitation. - 2 Precipitation characteristics. - a Rainfall intensity. - b Areal extent of a rainstorm. - c Frequency of rainstorms. - 3 The world pattern of precipitation. - 4 Regional variations in the altitudinal maximum of precipitation. - 5 Drought. - 5 ATMOSPHERIC INSTABILITY, CLOUD FORMATION AND PRECIPITATION PROCESSES. - A Adiabatic temperature changes. - B Condensation level. - C Air stability and instability. - D Cloud formation. - 1 Condensation nuclei. - 2 Cloud types. - 3 Global cloud cover. - E Formation of precipitation. - 1 Bergeron-Findeisen theory. - 2 Coalescence theories. - 3 Solid precipitation. - F Precipitation types. - 1 'Convective type' precipitation. - 2 'Cyclonic type' precipitation. - 3 Orographic precipitation. - G Thunderstorms. - 1 Development. - 2 Cloud electrification and lightning. - 6 ATMOSPHERIC MOTION: PRINCIPLES. - A Laws of horizontal motion. - 1 The pressure-gradient force. - 2 The earth's rotational deflective (Coriolis) force. - 3 The geostrophic wind. - 4 The centripetal acceleration. - 5 Frictional forces and the planetary boundary layer. - B Divergence, vertical motion and vorticity. - 1 Divergence. - 2 Vertical motion. - 3 Vorticity. - C Local winds. - 1 Mountain and valley winds. - 2 Land and sea breezes. - 3 Winds due to topographic barriers. - 7 PLANETARY-SCALE MOTIONS IN THE ATMOSPHERE AND OCEAN. - A Variation of pressure and wind velocity with height. - 1 The vertical variation of pressure systems. - 2 Mean upper-air patterns. - 3 Upper wind conditions. - 4 Surface pressure conditions. - B The global wind belts. - 1 The trade winds. - 2 The equatorial westerlies. - 3 The mid-latitude (Ferrel) westerlies. - 4 The polar easterlies. - C The general circulation. - 1 Circulations in the vertical and horizontal planes. - 2 Variations in the circulation of the northern hemisphere. - a Zonal index variations. - b North Atlantic Oscillation. - D Ocean structure and circulation. - 1 Above the thermocline. - a Vertical. - b Horizontal. - 2 Deep ocean water interactions. - a Upwelling. - b Deep ocean circulation. - 3 The oceans and atmospheric regulation. - 8 NUMERICAL MODELS OF THE GENERAL CIRCULATION, CLIMATE AND WEATHER PREDICTION / T. N. Chase and R. G. Barry. - A Fundamentals of the GCM. - B Model simulations. - 1 GCMs. - 2 Simpler models. - 3 Regional models. - C Data sources for forecasting. - D Numerical weather prediction. - 1 Short- and medium-range forecasting. - 2 'Nowcasting'. - 3 Long-range outlooks. - 9 MID-LATITUDE SYNOPTIC AND MESOSCALE SYSTEMS. - A The airmass concept. - B Nature of the source area. - 1 Cold airmasses. - 2 Warm airmasses. - C Airmass modification. - 1 Mechanisms of modification. - a Thermodynamic changes. - b Dynamic changes. - 2 The results of modification: secondary airmasses. - a Cold air. - b Warm air. - 3 The age of the airmass. - D Frontogenesis. - 1 Frontal waves. - 2 The frontal-wave depression. - E Frontal characteristics. - 1 The warm front. - 2 The cold front. - 3 The occlusion. - 4 Frontal-wave families. - F Zones of wave development and frontogenesis. - G Surface/upper-air relationships and the formation of frontal cyclones. - H Non-frontal depressions. - 1 The lee cyclone. - 2 The thermal low. - 3 Polar air depressions. - 4 The cold low. - I Mesoscale convective systems. - 10 WEATHER AND CLIMATE IN MIDDLE AND HIGH LATITUDES. - A Europe. - 1 Pressure and wind conditions. - 2 Oceanicity and continentality. - 3 British airflow patterns and their climatic characteristics. - 4 Singularities and natural seasons. - 5 Synoptic anomalies. - 6 Topographic effects. - B North America. - 1 Pressure systems. - 2 The temperate west coast and Cordillera. - 3 Interior and eastern North America. - a Continental and oceanic influences. - b Warm and cold spells. - c Precipitation and the moisture balance. - C The subtropical margins. - 1 The semi-arid southwestern United States. - 2 The interior southeastern United States. - 3 The Mediterranean. - 4 North Africa. - 5 Australasia. - D High latitudes. - 1 The southern westerlies. - 2 The sub-Arctic. - 3 The polar regions. - a The Arctic. - b Antarctica. - 11 TROPICAL WEATHER AND CLIMATE. - A The intertropical convergence. - B Tropical disturbances. - 1 Wave disturbances. - 2 Cyclones. - a Hurricanes and typhoons. - b Other tropical disturbances. - 3 Tropical cloud clusters. - C The Asian monsoon. - 1 Winter. - 2 Spring. - 3 Early summer. - 4 Summer. - 5 Autumn. - D East Asian and Australian summer monsoons. - E Central and southern Africa. - 1 The African monsoon. - 2 Southern Africa. - F Amazonia. - G El Niño-Southern Oscillation (ENSO) events. - 1 The Pacific Ocean. - 2 Teleconnections. - H Other sources of climatic variations in the tropics. - 1 Cool ocean currents. - 2 Topographic effects. - 3 Diurnal variations. - I Forecasting tropical weather. - 1 Short- and extended-range forecasts. - 2 Long-range forecasts. - 12 BOUNDARY LAYER CLIMATES. - A Surface energy budgets. - B Non-vegetated natural surfaces. - 1 Rock and sand. - 2 Water. - 3 Snow and ice C Vegetated surfaces. - 1 Short green crops. - 2 Forests. - a Modification of energy transfers. - b Modification of airflow. - c Modification of the humidity environment. - d Modification of the thermal environment. - D Urban surfaces. - 1 Modification of atmospheric composition. - a Aerosols. - b Gases. - c Pollution distribution and impacts. - 2 Modification of the heat budget. - a Atmospheric composition. - b Urban surfaces. - c Human heat production. - d Heat islands. - 3 Modification of surface characteristics. - a Airflow. - b Moisture. - 4 Tropical urban climates. - 13 CLIMATE CHANGE. - A General considerations. - B Climate forcings and feedbacks. - 1 External forcing. - 2 Short-term forcing and feedback. - C The climatic record. - 1 The geological record. - 2 Late glacial and post-glacial conditions. - 3 The past 1000 years. - D Possible causes of recent climatic change. - 1 Circulation changes. - 2 Energy budgets. - 3 Anthropogenic factors. - E Model s
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  • 6
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Routledge
    Call number: PIK N 071-18-91872
    Type of Medium: Monograph available for loan
    Pages: XXIII, 216 Seiten
    ISBN: 0415302765 , 9780415302760
    Series Statement: Routledge research in environmental politics 5
    Language: English
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  • 7
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Mycobacterium tuberculosis, which causes tuberculosis, is the greatest single infectious cause of mortality worldwide, killing roughly two million people annually. Estimates indicate that one-third of the world population is infected with latent M. tuberculosis. The synergy between ...
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  • 8
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Fifty million new infections with Mycobacterium tuberculosis occur annually, claiming 2–3 million lives from tuberculosis worldwide. Despite the apparent lack of significant genetic heterogeneity between strains of M. tuberculosis, there is mounting evidence that considerable ...
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  • 9
  • 10
    Publication Date: 2004-09-01
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Published by Springer Nature
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