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 52
Page v
... greenhouse gases , reactive gases , aerosol particles - is now significantly different from what it was a century ago . The Earth's biota is now experiencing the sixth great extinction event , but the first caused by another species ...
... greenhouse gases , reactive gases , aerosol particles - is now significantly different from what it was a century ago . The Earth's biota is now experiencing the sixth great extinction event , but the first caused by another species ...
Page x
... Greenhouse Accounting, Research School of Biological Sciences, The Australian National University, Canberra Folke, Carl Center for Transdisciplinary Environmental Studies (CTM) and Department of Systems Ecology, Stockholm University ...
... Greenhouse Accounting, Research School of Biological Sciences, The Australian National University, Canberra Folke, Carl Center for Transdisciplinary Environmental Studies (CTM) and Department of Systems Ecology, Stockholm University ...
Page xi
... Greenhouse Accounting, Research School of Biological Sciences, The Australian National University, Canberra Scholes, R. J. Council for Scientific and Industrial Research, South Africa Serneels, Suzanne University of Louvain, Belgium ...
... Greenhouse Accounting, Research School of Biological Sciences, The Australian National University, Canberra Scholes, R. J. Council for Scientific and Industrial Research, South Africa Serneels, Suzanne University of Louvain, Belgium ...
Page 1
... greenhouse gases (Fig. 1.1). The heat-absorbing property of these gases and the empiri- cal demonstration that their changing atmospheric concentrations been closely linked to climate change over the last 400 000 years combine to pose ...
... greenhouse gases (Fig. 1.1). The heat-absorbing property of these gases and the empiri- cal demonstration that their changing atmospheric concentrations been closely linked to climate change over the last 400 000 years combine to pose ...
Page 4
... greenhouse gas concentrations and climate change even during the intervals of rapid warming at each glacial termination . Although the phasing and likely lags are still not precisely determined for each glacial- interglacial transition ...
... greenhouse gas concentrations and climate change even during the intervals of rapid warming at each glacial termination . Although the phasing and likely lags are still not precisely determined for each glacial- interglacial transition ...
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