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Climate Change Science: A Modern Synthesis

Volume 1 - The Physical Climate

Gebonden Engels 2013 2013e druk 9789400757561
Verwachte levertijd ongeveer 9 werkdagen

Samenvatting

An introduction to the principles of climate change science with an emphasis on the empirical evidence for climate change and a warming world. Additional readings are given at the end of each chapter. A list of "Things to Know" opens each chapter. Chapters are arranged so that the student is first introduced to the scientific method(s), examples of the use of the scientific method from other sciences drawn from the history of science with an emphasis on climate science. Climate science is treated in each chapter based on the premise of global warming. Chapter treatments on the atmosphere. biosphere, geosphere, hydrosphere, and anthroposphere and their inter-relationships are given.

Specificaties

ISBN13:9789400757561
Taal:Engels
Bindwijze:gebonden
Aantal pagina's:564
Uitgever:Springer Netherlands
Druk:2013

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<p>CONTENTS<br>INTRODUCTION<br>1.1 Introduction to Global Warming<br>1.2 Greenhouse Effect<br>1.3 Climate Sensitivity<br>1.4 Average Global Temperature from 1880 to 2009<br>1.5 Carbon Dioxide<br>1.6 Global Warming, Climate, and Weather<br>1.6.1 Arctic Sea Ice Extent 1979-2005<br>1.6.2 Impacts of Global Warming<br>1.7 Timescales, Positive Feedbacks, and Tipping Points<br>1.8 Energy and Climate Policy<br>1.8.1 Energy Choices<br>1.9 Forcings and Feedbacks<br>1.9.1 Earth’s Albedo<br>1.9.2 Irradiance<br>1.10 Energy Budget<br>1.11 Affected Weather<br>1.12 Hockey Stick Controversy<br>Additional Reading<br>PART I – SCIENTIFIC PRINCIPLES AND THE SCIENTIFIC METHOD<br>2 – SCIENTIFIC PRINCIPLES<br>Abstract<br>Key Words</p><p>Things to Know<br>Introduction<br>2.1 Internet Searches<br>2.2 The Warming Earth: Heat and the Principles of Thermodynamics<br>2.2.1 The Zeroth Law of Thermodynamics<br>2.2.2 The First Law of Thermodynamics<br>2.2.3 The Second Law of Thermodynamics<br>2.2.4 The Third Law of Thermodynamics<br>2.3 Climate Scientists<br>2.3.1 Scientific Laws and Climate Scientists<br>2.4 Scientific Jargon<br>2.5 Communication between Scientists and the Public<br>2.6 The Concept of Time<br>2.7 From Hothouse to Icehouse<br>2.8 Earth’s Energy Imbalance<br>2.9 An Introduction to Science<br>2.9.1 Reasons to Study Science<br>2.9.2 The Philosophy of Science<br>2.9.3 Early History of Science<br>2.9.4 Aristotle (384-322 BC)<br>2.10 Early Scientists<br>2.10.1 Pliny the Elder (23 AD – 79 AD) <br>2.10.2 Claudius Ptolemy (c. AD 90 – c. AD 168)<br>2.10.3 Nicolaus Copernicus (1473 – 1543)<br>2.10.4 Galileo Galilei (1564 – 1642) <br>2.10.5 Francis Bacon (1561 – 1626)<br>2.10.6 Johannes Kepler and Tycho Brahe<br>2.10.7 Isaac Newton <br>2.11 Empiricism<br>2.12 Inductive Logic<br>2.13 Multiple Working Hypotheses<br>2.14 Deductive Logic<br/>2.15 Models and Simulations<br>2.16 The Nature of Science<br>2.17 The Science of Nature<br>2.18 Chaos Theory<br>2.19 Scientific Notation<br>Additional Reading<br>3 - THE SCIENTIFIC METHOD AND ITS USE<br>Abstract<br>Keywords<br>Things to Know<br>The Scientific Method<br>3.1 A Linearized Approach to the Scientific Method<br>3.2 Data Collection – Experimentation, Measurement, Observation <br>3.3 Ideas, Persistence, Documentation, Testing, Reproducibility, Publication<br>3.4 Hypotheses<br>3.5 Theories <br>3.6 Newton’s Laws of Motion <br>3.7 The Peer-Review Process<br>3.8 Use of the Scientific Method<br>3.8.1 James Hutton and Uniformitarianism<br>3.8.2 Charles Darwin and the Origin of Species<br>3.8.3 James Watson and Francis Crick – the Structure of DNA<br>3.8.4 Harry Hess and Plate Tectonic Theory<br>3.8.5 Plate Tectonic Theory<br>3.8.6 Wallace Broecker and the First Use of the Term Global Warming<br>3.9 Use of the Scientific Method in Climate Change Science<br>3.9.1 Joseph Fourier and the Greenhouse Effect<br>3.9.2 John Tyndall and Thermal Radiation<br>3.9.3 Svante Arrhenius and Carbon Dioxide<br>3.9.4 T. C. Chamberlin and the Ice Ages<br>3.9.5 Guy Stewart Callendar and Rising Temperatures<br>3.9.6 Gilbert Plass and Doubling of Carbon Dioxide<br>3.9.7 Hans Suess and Carbon-14 in Carbon Dioxide<br>3.9.8 Roger Revelle and Ocean Chemistry <br>3.9.9 Charles David Keeling and CO2<br>3.9.10 Syukuro (“Suki”) Manabe and Climate Modeling<br>3.9.11 James Hansen and Temperature Analysis<br>3.9.12 William Ruddiman and Paleoclimate<br>3.9.13 Gavin Schmidt and GISS<br>3.9.14 Stefan Rahmstorf, Sea Level and Temperature Rise<br>Additional Reading<br>PART II – OVERVIEW OF CLIMATE CHANGE SCIENCE<br>4 – EARTH’S ENERGY BUDGET<br>Abstract<br>Keywords<br>Things to Know<br>Introduction<br>4.1 Weather and Climate<br>4.2 Solar and Heat Energy<br>4.3 Earth’s Radiation Laws<br/>4.4 Earth’s Energy Imbalance<br>Additional Reading<br>5 – CLIMATE CHANGE TRENDS<br>Abstract<br>Keywords<br>Things to Know<br>5. Climate Change Trends<br>5.1 Rising Temperatures<br>5.1.1 Temperature Scales<br>5.1.2 Temperatures Shown by Graphs<br>5.1.3 Rising Land and Sea Temperatures<br>5.1.4 Tropospheric Warming and Stratospheric Cooling<br>5.2 Sources of Uncertainty with Temperature Data<br>5.3 Climate Construction from Instrumental Data<br>5.4 Measurement of Temperature<br>5.5.1 Global Temperature from Meteorological Stations<br>5.5 The Berkeley Earth Surface Temperature (BEST) Study<br>5.6 Land Temperatures from Boreholes<br>5.7 Rising Sea Temperatures<br>5.7.1 Relative Distribution of Sea-Surface Temperatures (SSTs)<br>5.7.2 Ocean Heat Content<br>5.8 Melting Ice<br>5.8.1 Permafrost, Methane, and Clathrates<br>5.8.2 Methane Clathrates<br>5.9 Rising Sea Level<br>5.10 Migration of Plants and Animals<br>5.11 Species Extinctions<br>5.12 Human Health Effects of Rising Temperatures<br>5.13 Attribution<br>5.14 Greenhouse Gases <br>5.15 Human Fingerprints on Global Warming<br>5.16.1 Earth’s Cooling Upper Atmosphere<br>5.16.2 Rising Tropopause <br>5.16.3 Less Heat Escaping to Space<br>5.16.4 Nights Warming Faster than Days<br>5.16.5 Winter Warming Faster than Summer<br>5.16.6 More Fossil Fuel Carbon in Coral <br>5.16.7 Shrinking Upper Atmosphere<br>5.16.8 Less Oxygen in the Atmosphere <br>5.16.9 More Fossil Fuel Carbon in the Atmosphere <br>5.16.10 More Heat Returning to Earth <br>5.16.11 Pattern of Ocean Warming <br>5.16 Components of the Climate Change Process<br>5.17 Other Effects of Global Warming<br>5.18 Forcings and Feedbacks in the Climate System<br>5.18.1 Forcings<br>5.18.2 Positive and Negative Forcing and their Effects<br>5.18.3 Feedbacks<br>5.19 Climate Sensitivity<br>Additional Reading<br>6 – EARTH’S SURFACE TEMPERATURE<br>Abstract<br>Keywords<br/>Things to Know<br>6. Introduction<br>6.1 Tipping Points<br>6.2 Temperature Records<br>6.3 Data Reduction<br>6.4 Data Analysis<br>6.5 Climate Data Analysis Tools (CDAT)<br>6.6 Data Reporting<br>6.7 Average Land Temperatures<br>6.8 History of the Development of the Global Average Temperature<br>6.9 Current Analysis Method<br>6.10 Temperature Anomalies<br>6.11 History of Temperature Recordings<br>6.12 Sea Surface Temperatures (SSTs)<br>6.13 Projections of Future Temperatures<br>6.14 The IPCC Special Report on Emission Scenarios (SRES), 2007<br>Additional Reading<br>7 – CLIMATE CHANGE SCIENCE AS EARTH SCIENCE<br>Abstract<br>Keywords<br>Things to Know<br> Introduction<br>7.1 Climate Science as Earth Science<br>7.2 The Faint Young Sun Paradox<br>7.3 The Gaia Hypothesis<br>7.4 Introduction to Life Science<br>7.5 Introduction to the Atmosphere<br>7.6 Open System Science<br>7.7 Uniformitarianism and Climate Change Science<br>7.8 Recent Climate Data and Future Projections<br>7.9 Components of the Climate Change System<br>7.10 Good Science, Bad Science, and Non-Science<br>7.11 Examples of Good Science<br>7.12 Examples of Bad Science  <br>7.13 Examples of Non-Science<br>7.14 Ethics in Science<br>7.15 The Concept of Scale in Earth and Climate Change Science<br>7.16 Map Scales<br>7.17 Fractals<br>7.18 Graph Scales<br>7.19 Time Scales<br>7.20 Earth Scales<br>7.21 Planetary Scales<br>7.22 Cosmic Scales<br>Additional Reading<br>PART III – EARTH’S ATMOSPHERE<br>8 – INTRODUCTION TO EARTH’S ATMOSPHERE<br>Abstract<br>Keywords<br>Things to Know<br> Introduction<br>8.1 The Atmosphere<br>8.2 Composition of the Atmosphere<br>8.2.1 Carbon Dioxide<br>8.2.2 Methane (CH4)<br>8.2.3 Nitrous Oxide (N20)<br>8.2.4 Ozone (O3)<br>8.2.5 Chlorofluorocarbons (CFCs)<br>8.2.6 Other Trace Gases<br>8.2.7 Aerosols<br>8.3 Lapse Rate<br>8.4 Vertical Structure of the Atmosphere<br/>8.5 Atmospheric Circulation<br>Additional Reading</p><p>9 – CARBON DIOXIDE, OTHER GREENHOUSE GASES, AND THE CARBON CYCLE<br>Abstract<br>Keywords<br>Things to Know<br> Introduction<br>9.1 Carbon Dioxide (CO2)<br>9.1.1 The Keeling Curve<br>9.2 The Carbon Cycle<br>9.3 Carbon Dioxide and the Carbon Cycle<br>9.4 Sources and Sinks of Carbon Dioxide<br>9.4.1 Sources of Atmospheric Carbon Dioxide<br>9.4.2 Oxidation – Reduction of Carbon<br>9.4.3 Sinks of Atmospheric Carbon Dioxide<br>9.4.4 Carbon Cycle Disequilibrium9.4.5 Restoring Carbon Cycle Equilibrium<br>9.5 Methane (CH4)<br>9.5.1 Sources and Sinks of Atmospheric Methane<br>9.6 Nitrous Oxide<br>9.6.1 Sources and Sinks of Atmospheric Nitrous Oxide<br>9.6.2 Increases in Atmospheric Nitrous Oxide Concentration<br>9.7 Halocarbons<br>9.7.1 Sources and Sinks of Halocarbons<br>9.7.2 Increases in Atmospheric Halocarbons Concentration<br>9.8 Ozone<br>9.9 Other Trace Gases<br>9.10 Atmospheric Residence Time of Greenhouse Gases<br>Additional Reading<br>10 - EARTH’S ALBEDO, RADIATIVE FORCING AND CLIMATE CHANGE<br>Abstract<br>Keywords<br>Things to Know<br> Introduction<br>10.1 Earth’s Albedo<br>10.1.1 Solid Earth Albedo<br>10.1.2 Ocean Albedo<br>10.1.3 Glacial Ice Albedo<br>10.1.4 Water Vapor<br>10.1.5 Cloud Albedo<br>10.1.6 Deforestation and Albedo<br>10.2 Radiative Forcing<br>10.2.1 Factors Affecting Greenhouse Radiative Forcing<br>10.3 Global Warming Potentials (GWPs)<br>10.4 Calculation of Greenhouse Gas Radiative Forcing<br>10.5 Radiative Forcing of Ozone<br>10.5.1 Stratospheric Ozone<br>10.5.2 Tropospheric Ozone<br>10.6 Aerosols<br>10.6.1 Sources and Sinks of Aerosols<br>10.6.2 Radiative Forcing by Aerosols<br>10.7 Direct Radiative Forcing<br>10.8 Indirect Radiative Forcing<br>10.9 Total Anthropogenic Radiative Forcing: Greenhouse Gases and Aerosols<br>10.10 Observed Climate Variations<br/>10.11 Clouds and their Impacts on Climate Change<br>10.11.1 High-Level Clouds<br>10.11.2 Mid-Level Clouds<br>10.11.3 Low-Level Clouds<br>10.12 Orographic Rainfall<br>Additional Reading<br>11 – ATMOSPHERIC CIRCULATION AND CLIMATE<br>Abstract<br>Keywords<br>Things to Know<br> Introduction<br>11.1 Atmospheric Circulation<br>11.2 Insolation<br>11.3 Air Flow Patterns<br>11.4 Climate Change Effects on Atmospheric Circulations<br>11.5 Extreme Weather Events<br>11.5.1 Washington, D.C. Metro<br>11.5.2 Binghamton, N.Y. <br>11.5.3 Allentown, PA. <br>11.5.4 Harrisburg, PA <br>11.5.5 Dayton, Ohio <br>11.5.6 Colorado Springs, Colo. <br>11.5.7 Tucson, Arizona. <br>11.6 Record Heat <br>11.6.1 Houston, Texas <br>11.6.2 Dallas, Texas <br>11.6.3 Phoenix, Arizona <br>11.6.4 Corpus Christi, Texas. <br>11.7 Record Cold <br>11.7.1 International Falls, Minn. <br>11.8 Record River Flooding <br>11.9 Tropical Storm Lee's Tornadoes <br>11.10 Other Meteorological Events<br>Additional Reading<br>PART IV - THE WORLD OCEAN AND CLIMATE<br>12 – THE WORLD OCEAN<br>Abstract<br>Keywords<br>Things to Know<br> Introduction<br>12.1 The World Ocean<br>12.2 Ocean Salinity<br>12.3 Ocean Topography<br>12.4 The World Ocean and Carbon Dioxide<br>12.5 Ocean Acidification<br>12.6 Oceanic Circulation<br>12.6.1 Thermohaline Circulation <br>Additional Reading<br>13 – OCEAN HEAT CONTENT AND RISING SEA LEVEL <br>Abstract<br>Keywords<br>Things to Know<br> Introduction<br>13.1 Global Warming and Sea Level Rise<br>13.2 Arctic Oscillation (AO) and Arctic Sea Ice<br>13.3 Atlantic Multidecadal Oscillation (AMO)<br>13.4 Pacific Decadal Oscillation (PDO)<br>13.5 Future Potential Sea Level Rise<br>13.6 Ocean Heat Content<br>13.7 El Niño – La Niña (or ENSO)<br>Additional Reading<br>PART V – EARTH’S CRYOSPHERE AND RECENT CLIMATE HISTORY<br>14 – GLACIERS AND THE LATEST ICE AGEAbstractKeywords<br>Things to Know<br>14. Introduction<br>14.1 Greenland Ice Sheet<br>14.2 Antarctica<br>14.3 Mountain Glaciers<br>14.4 Ice Cores<br>14.5 Stable Isotope Analysis<br>14.6 Ice Cores and Proxies<br>14.6.1 Dating Ice Cores<br>14.6.2 Mountain Glacier Ice Cores<br>14.7 The Ice Age<br>14.7.1 History<br>14.7.2 Climate Forcing by Orbital Variations<br>14.7.3 Eccentricity<br>14.7.4 Obliquity<br>14.7.5 Precession<br>14.8 Milankovitch Cycles and Ice Ages<br>14.9 Solar Variations<br>14.10 Questions not Explained by Milankovitch Cycles<br>Additional Reading<br>15 – PERMAFROST AND METHANE <br>Abstract<br>Keywords<br>Things to Know<br>15. Introduction<br>15.1 Distribution<br>15.2 Origin of Permafrost<br>15.3 Methane Chemistry<br>15.4 Future Projections for Permafrost and Methane<br>15.5 Methane Gun Hypothesis<br>Additional Reading<br>PART VI - LAND AND ITS CLIMATES</p><p>16 CONTINENTS AND MOUNTAIN RANGES<br>Abstract<br>Keywords<br>Things to Know<br>16. Introduction<br>16.1 Continental Drift <br>16.2 Harry Hess and Sea-Floor Spreading<br>16.3 Plate Tectonics<br>16.3.1 Types of Plate Boundaries<br>16.4 Continental Mountain Ranges<br>16.5 Islands<br>Additional Reading<br>17 – CLIMATE CLASSIFICATIONS<br>Abstract<br>Key Words<br>Things to Know<br> An Introduction to Climate Classification <br>17.1 Air Masses<br>17.2 Modern Climate Classification <br>17.2.1 The Bergeron Climate Classification<br>17.3 The Köppen-Geiger Classification<br>17.3.1 Group A Climates<br>17.3.2 Group B Climates<br>17.3.3 Group C Climates<br>17.3.4 Group D Climates<br>17.3.5 Group E Climates<br>17.4 The Thornthwaite Climate Classification<br>Additional Reading<br>PART VII - CLIMATE MODELS<br>18 – TYPES OF MODELS<br>Abstract<br>Key Words<br>Things to Know<br> Introduction<br>18.1 Climate Models<br>18.1.1 Simplifying the Climate System<br/>18.1.2 Boundary Conditions<br>18.1.3 Climate Modeling Centers<br>18.2 Types of Climate Models<br>18.2.1 Box Models<br>18.2.2 Energy Balance Models<br>18.2.3 Radiative-Convective Models<br>18.2.4 Statistical-Dynamical Models<br>18.2.5 General Circulation Models <br>18.3 Confidence and Validation<br>Additional Reading<br>PART VIII – CLIMATES OF THE PAST (PALEOCLIMATOLOGY)</p><p><br>19 – ANCIENT CLIMATES AND PROXIES<br>Abstract<br>Keywords<br>Things to Know<br> Introduction<br>19.1 Historical Records<br>19.2 Ice Cores<br>19.3 Stable Isotope Analysis<br>19.4 Ice Cores and Proxies<br>19.5 Dating Ice Cores<br>19.6 Dendroclimatology<br>19.7 Ocean Sediments<br>19.8 Paleoclimate Reconstruction from Biogenic Material<br>19.9 Paleoclimate Reconstruction from Terrigenous Material<br>19.10 Terrestrial Sediments<br>19.11 Periglacial Features<br>19.12 Glacial Fluctuations<br>19.13 Lake-Level Fluctuations<br>19.13.1 Russia’s Lake El’gygytgyn (Lake E)<br>19.14 Pollen Analysis<br>19.15 Sedimentary Rocks<br>Additional Reading<br>20 – CLIMATES OF THE RECENT PAST<br>Abstract<br>Key Words<br>Things to Know<br>Introduction<br>20.1 Holocene Climates<br>20.2 Younger Dryas Cooling<br>20.3 Mid-Holocene Thermal Maximum<br>20.4 Late Holocene Neoglaciation<br>20.5 Little Ice Age<br>20.6 Medieval Warm Period<br>20.7 Holocene Climate Forcing Mechanisms<br>20.8 Coupled Internally-Externally Driven Climate Change<br>20.9 Contemporary Climate Change<br>Additional Reading<br>21 - PLEISTOCENE GLACIATIONS<br>Abstract<br>Keywords<br>Things to Know<br>21. Pleistocene Glaciations<br>21.1 Glacials and Interglacials<br>21.2 Causes of Glacial Advances and Retreats<br>21.3 Paleocene-Eocene Thermal Maximum<br>21.4 Initial Eocene Thermal Maximum (IETM)<br>21.5 The Cooling Begins<br>21.6 Formation of the Isthmus of Panama and the Freezing of the Arctic<br/>21.7 Other Influences and Possible Causes of Ice Ages<br>21.8 Maximum Extent and Characteristics of Continental Glaciers<br>21.8.1 The North American Ice Line<br>21.8.2 Europe and Asia’s Continental Glaciation<br>21.8.3 Southern Hemisphere Glaciation<br>Additional Reading<br>PART IX - FUTURE CLIMATES AND MITIGATION<br>22 - PROJECTIONS OF FUTURE CLIMATES<br>Abstract<br>Key Words<br>Things to Know<br>Introduction<br>22.1 Hotter - Global Warming<br>22.2 Flatter – The Digital Age<br>22.3 More Crowded – Population Increase<br>22.3.1 Population and Demographics<br>22.4 IPCC Projections of Future Climate Change <br>22.5 Politics and Global Warming<br>22.5.1 Politicians and Their Views <br>22.5.2 Ronald Reagan<br>22.5.3 Richard Nixon<br>22.5.4 Barak Obama<br>Additional Reading<br>PART X – SKEPTICS AND DENIERS OF GLOBAL WARMING<br>23 - UNDERSTANDING CLIMATE DENIAL<br>Abstract   <br>Keywords<br>Things to Know<br>Introduction<br>23.1 Basis for the Scientific Consensus on Climate Change<br>23.2 Characteristics of Denial<br>23.2.1 Fake Experts<br>23.2.2 Cherry Picking<br>23.2.3 Logical Fallacies<br>23.2.4 Impossible Expectations<br>23.2.5 Conspiracy Theories<br>23.2.6 Denial Characteristics at a Psychological Level<br>23.3 Drivers of Climate Denial<br>23.3.1 Conservative Ideology<br>23.3.2 Conservative Think Tanks<br>23.3.3 Mainstream Media’s Balance-as-Bias<br>23.3.4 Government<br>23.3.5 Corporate Vested Interests<br>23.3.6 Internet<br>23.4 Responding to Climate Denial<br>23.4.1 Familiarity Backfire Effect<br>23.4.2 Overkill Backfire Effect<br>23.4.3 Worldview Backfire Effect<br>23.4.4 Alternative Explanation<br>23.4.5 Summary<br>Additional Reading<br>PART XI - SPECIFIC DECLARATIONS AGAINST CLIMATE SCIENCE AND CLIMATE SCIENTISTS<br>24 - REBUTTALS TO CLIMATE MYTHS<br>Abstract   <br>Keywords<br>Things to Know<br> Introduction<br>24.1 Fake Experts<br/>24.1.1 A Petition of Tens of Thousands of Non-Experts<br>24.1.2 A Contrarian Take on Climate Sensitivity<br>24.2 Cherry Picking<br>24.2.1 Warming at Over Two Hiroshima Bombs per Second<br>24.2.2 Hockey Stick versus Hockey Team<br>24.2.3 Sun and Climate Moving in Opposite Directions<br>24.2.4 Human Emissions Upsetting the Natural Balance<br>22.3 Logical Fallacies<br>24.3.1 What does past climate change tell us?<br>24.3.2 CO2 Lag – The Chicken and Egg Dilemma<br>24.3.3 What Were Scientists Predicting in the 1970s?<br>24.3.4 How a Trace Gas has such a Significant Effect<br>24.4 Impossible Expectations<br>24.4.1 What Lessons do we learn from Past Model Predictions?<br>24.4.2 Science is never settled<br>24.4.3 Uncertainty is Not Our Friend<br>24.5 Conspiracy Theories<br>24.5.1 Nine Climategate Investigations Across Two Countries<br>24.5.2 Confusing ‘Mike’s Trick’ with ‘Hide the Decline’<br>24.5.3 Tracking down Trenberth’s ‘Missing Heat’<br>Additional Reading <br>ABBREVIATIONS<br>GLOSSARY<br>APPENDICES<br>INDEX</p><p>

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        Climate Change Science: A Modern Synthesis