At a time when the evidence is stronger than ever that human activity is the primary cause for global climate change, Ruddiman's breakthrough text returns in a thoroughly updated new edition. It offers a clear, engaging, objective portrait of the current state of climate science, including compelling recent findings on anthropogenic global warming and important advances in understanding past climates.
At a time when the evidence is stronger than ever that human activity is the primary cause for global climate change, Ruddiman's breakthrough text returns in a thoroughly updated new edition. It offers a clear, engaging, objective portrait of the current state of climate science, including compelling recent findings on anthropogenic global warming and important advances in understanding past climates.Hinweis: Dieser Artikel kann nur an eine deutsche Lieferadresse ausgeliefert werden.
From the contents: PART I: FRAMEWORK OF CLIMATE SCIENCE - Overview of Climate Science - Climatic Archives, Data and Models - PART II: TECTONIC-SCALE CLIMATE CHANGE - CO2 and Long-Term Climate - Plate Tectonics and Long-Term Climate - Greenhouse Earth - From Greenhouse to Icehouse: The Last 50 Million Years - PART III: ORBITAL-SCALE CLIMATE CHANGE - Astronomical Control of Solar Radiation - Insolation Control of Monsoons - Insolation Control of Ice Sheets - Orbital-Scale Changes in CO2 and Methane - Orbital-Scale Interactions, Feedback, and Unsolved Problems - PART IV: DEGLACIAL AND MILLENNIAL CLIMATE CHANGE - The Last Glacial Maximum - Climate During and Since the Last Deglaciation - Millennial Oscillations of Climate - PART V: HISTORICAL AND FUTURE CLIMATE CHANGE - Humans and Pre-Industrial Climate - Climate Change During the Last 1000 Years - Climate Change Since 1850 - Causes of the Warming of the Last 125 Years - Future Climate Change
From the contents: PART I: FRAMEWORK OF CLIMATE SCIENCE - Overview of Climate Science - Climatic Archives, Data and Models - PART II: TECTONIC-SCALE CLIMATE CHANGE - CO2 and Long-Term Climate - Plate Tectonics and Long-Term Climate - Greenhouse Earth - From Greenhouse to Icehouse: The Last 50 Million Years - PART III: ORBITAL-SCALE CLIMATE CHANGE - Astronomical Control of Solar Radiation - Insolation Control of Monsoons - Insolation Control of Ice Sheets - Orbital-Scale Changes in CO2 and Methane - Orbital-Scale Interactions, Feedback, and Unsolved Problems - PART IV: DEGLACIAL AND MILLENNIAL CLIMATE CHANGE - The Last Glacial Maximum - Climate During and Since the Last Deglaciation - Millennial Oscillations of Climate - PART V: HISTORICAL AND FUTURE CLIMATE CHANGE - Humans and Pre-Industrial Climate - Climate Change During the Last 1000 Years - Climate Change Since 1850 - Causes of the Warming of the Last 125 Years - Future Climate Change
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