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. |
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Page 13
... Younger Dryas cold interval and the very rapid termination of the last glaciation (adapted from Jacob- son et al. 2000) precipitation that are consistently recorded in environ- mental archives occur on shorter timescales, ranging from ...
... Younger Dryas cold interval and the very rapid termination of the last glaciation (adapted from Jacob- son et al. 2000) precipitation that are consistently recorded in environ- mental archives occur on shorter timescales, ranging from ...
Page 15
... Younger Dryas cold event some 11 600 years ago . In this record the event is manifested as a warming estimated to be as much as 15 ° C , accompanied by a doubling in annual pre- cipitation volume , that occurred in less than a decade ...
... Younger Dryas cold event some 11 600 years ago . In this record the event is manifested as a warming estimated to be as much as 15 ° C , accompanied by a doubling in annual pre- cipitation volume , that occurred in less than a decade ...
Page 17
... Younger Dryas and the timing of the Antarctic Cold Reversal and the atmos- pheric CO2 increase with respect to the Younger Dryas event, as deduced from the CH isotopic 4 synchronisation, records of the the GRIP, Byrd and Vostok ice ...
... Younger Dryas and the timing of the Antarctic Cold Reversal and the atmos- pheric CO2 increase with respect to the Younger Dryas event, as deduced from the CH isotopic 4 synchronisation, records of the the GRIP, Byrd and Vostok ice ...
Page 54
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Page 66
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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