Global Change and the Earth System: A Planet Under PressureThe interactions between environmental change and human societies have a long, complex history spanning many millennia, but these have changed fundamentally in the last century. Human activities are now so pervasive and profound that they are altering the Earth in ways which threaten the very life support system upon which humans depend. This book describes what is known about the Earth System and the impact of changes caused by humans. It considers the consequences of these changes with respect to the stability of the Earth System and the well-being of humankind; as well as exploring future paths towards Earth System science in support of global sustainability. |
From inside the book
Results 1-5 of 87
Page vii
... Processes 2.3.2 Biogeochemical Processes 2.3.3 The Role of Biodiversity 2.4 New Insights into Spatial Variability of the Earth System 2.4.1 Spatial Patterns of Land Cover 2.4.2 Spatial Patterns of Carbon Sources and Sinks 2.4.3 Trace ...
... Processes 2.3.2 Biogeochemical Processes 2.3.3 The Role of Biodiversity 2.4 New Insights into Spatial Variability of the Earth System 2.4.1 Spatial Patterns of Land Cover 2.4.2 Spatial Patterns of Carbon Sources and Sinks 2.4.3 Trace ...
Page 1
... processes and components, both bi- otic and abiotic, upon which the human species depends. This book describes what is known about the Earth Sys- tem and the nature of the human-driven changes im- pacting it. It also considers the ...
... processes and components, both bi- otic and abiotic, upon which the human species depends. This book describes what is known about the Earth Sys- tem and the nature of the human-driven changes im- pacting it. It also considers the ...
Page 2
... processes. Classical analytical science in which individual variables are isolated and their separate effects deter- mined individually cannot cope with the challenges posed by Earth System science. This is often most clearly seen where ...
... processes. Classical analytical science in which individual variables are isolated and their separate effects deter- mined individually cannot cope with the challenges posed by Earth System science. This is often most clearly seen where ...
Page 3
... processes in the past set contem- porary observational snapshots in a time continuum ; and · ▫ enhanced computing power makes possible not only essential data assimilation , but increasingly sophis- ticated models that improve ...
... processes in the past set contem- porary observational snapshots in a time continuum ; and · ▫ enhanced computing power makes possible not only essential data assimilation , but increasingly sophis- ticated models that improve ...
Page 7
... processes which contribute to climate comprise the climate system , and they are closely connected to biogeo- chemical cycles . However , there are some important differences between climate change and global change : · ▫ Many ...
... processes which contribute to climate comprise the climate system , and they are closely connected to biogeo- chemical cycles . However , there are some important differences between climate change and global change : · ▫ Many ...
Contents
1 | |
6 | |
Harvard University USA The University of Newcastle | 60 |
Claussen Martin | 75 |
How Humans are Changing the Earth System | 81 |
3 | 109 |
Magnitudes Rates and Significance of Human Changes | 131 |
4 | 142 |
Department of Geosciences Harvey Nick | 166 |
5 | 203 |
NASA Headquarters Washington DC USA Potsdam Institute for Climate Impact Research | 234 |
Dalhousie University Canada Scholes R | 251 |
References | 299 |
Mitra A | 305 |
Acknowledgements | 307 |
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Common terms and phrases
aerosol aerosol particles Africa agricultural anthropogenic areas Asia atmos atmospheric CO2 Berlin Heidelberg biodiversity Biogeochem Cy biological biomass biosphere Cambridge carbon cycle century chemical climate change climate system CO₂ coastal zone complex concentration decades deforestation dynamics Earth System functioning ecosys ecosystems effects emissions ENSO environment environmental estimated example extinction feedbacks fertilisation flux forcing forest fossil fuel Gaia Geophys Res glacial Greenland growth Heidelberg New York Holocene human activities human-driven hydrological hydrological cycle ice core IGBP IGBP Global Change impacts important increase influence interactions IPCC land-cover Lovelock marine natural nitrogen North Atlantic nutrients ocean organic ozone past patterns perturbation photosynthesis phytoplankton plant population processes production radiative forcing record regions responses river role scale Science sediment significant simulations soil solar species surface temperature terrestrial ecosystems Tg N yr–1 thermohaline circulation tion transport trends tropical tropospheric variability vegetation warming Younger Dryas