By Carl E. Seashore
A brown textile coated e-book with numerous diagrams
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A close view of the numerical equipment used to resolve huge matrix eigenvalue difficulties that come up in a number of engineering and medical purposes. The emphasis is at the tougher nonsymmetric difficulties, yet a lot of the real fabric for symmetric difficulties can also be coated. The textual content features a sturdy theoretical part, and likewise describes many of the very important options built lately including a couple of computing device courses.
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S. S. in Physics from the University of Massachusetts. Mr. Silver currently teaches science in New Jersey. CONTENTS AT A GLANCE CHAPTER 1 Global Perspective—Thinking about the Earth PART ONE WHAT WE KNOW AND HOW WE KNOW IT CHAPTER 2 Taking the Earth’s Temperature CHAPTER 3 Signs of Global Warming PART TWO WHY CLIMATE CHANGES CHAPTER 4 The Earth’s Thermostat—Keeping the Earth Warm CHAPTER 5 Greenhouse Chemistry CHAPTER 6 Origin and Impact of Greenhouse Gases PART THREE WHAT WE CAN EXPECT AND WHAT WE CAN DO CHAPTER 7 Consequences of Global Warming CHAPTER 8 Resetting the Earth’s Thermostat—Solutions Final Exam APPENDIX A Glossary APPENDIX B Milestones in the History of Climate Change APPENDIX C Satellites That Monitor Weather and Climate APPENDIX D Units of Measurement Applied to Climate Change APPENDIX E Selected Resources APPENDIX F Summary of Key Climate Variables APPENDIX G Lingering Doubts and Concerns APPENDIX H Answers to Chapter Review Questions APPENDIX I Answers to Final Exam Index CONTENTS Acknowledgments CHAPTER 1 Global Perspective—Thinking about the Earth PART ONE WHAT WE KNOW AND HOW WE KNOW IT CHAPTER 2 Taking the Earth’s Temperature Global Temperature Measurement—The Basics How Is the Earth’s Temperature Changing?
Table 2-2 Layers of the Earth’s Atmosphere Figure 2-15 Satellites in orbit measure the earth’s temperature using instruments that collect long-wavelength light energy. ) One of the main advantages of satellites is that they monitor almost the entire earth each day, providing the largest statistical database and the greatest resolution of variation from one place on the earth to another. Satellites measure the total heat radiated from the earth, which has a direct bearing on the earth’s temperature.
The warming trend for the last 25 years is more than double that of the past century (Figure 2-4). Figure 2-4 Earth with a fever. How much should we be concerned with a temperature rise of less than 1°C? The last ice age was, on average, only about 5°C (9°F) colder than present-day global averages. The last time the global average temperature was about 5°C (9°F) warmer than today, sea levels were 4–6 m (13–20 ft) higher than present levels. THE PAST 13 CENTURIES Since the cave men did not have thermometers thousands of years ago, scientists today have to rely on indirect methods to determine what the earth’s climate once was.
Elementary Experiments in Psychology by Carl E. Seashore