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Planetary Boundaries: Introduction. Kevin Noone Swedish Secretariat for Environmental Earth System Sciences Department of Applied Environmental Sciences & Stockholm Resilience Centre, Stockholm University. Eighth International Seminar on Climate System and Climate Change
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Planetary Boundaries:Introduction Kevin Noone Swedish Secretariat for Environmental Earth System Sciences Department of Applied Environmental Sciences & Stockholm Resilience Centre, Stockholm University Eighth International Seminar on Climate System and Climate Change 18-29 July 2011, Beijing, China
Where will we go in this lecture? • Background: limits to growth, tipping points • Our new epoch – the Anthropocene • Planetary Boundaries • It’s all connected
Main points • We humans can cause the global environment to move into a state with which we have no historical experience • We have identified a number of non-negotiable natural boundaries that we should not exceed • Development and wellbeing can be created if these boundaries are respected
The Limits to Growth – D. Meadows et al. (1972) • Looked at five variables: population, per capita industrial output, food per capita, pollution, non-renewable resources • Used very primitive computing resources • Exponential reserve index:
World3 D. H. Meadows, et al. “Limits to Growth”, 1972
World3 D. H. Meadows, et al. “Limits to Growth”, 1972
Limits to Growth – revisited in 2008 Turner, G. M. (2008), Global Environmental Change, 18(3), 397-411.
Tipping points J. Schellnhuber, in Steffen, et al., Challenges of a Changing Earth, 2002
Tipping elements Ramanathan & Feng, 2008: PNAS, 105 (38), 14,245-14,250.
Our species’ history First migration of fully modern humans out of Africa Beginning of agriculture Aborigines arrive in Australia Migrations of fully modern humans from South Asia to Europe Great European civilisations: Greek, Roman Source: GRIP ice core data (Greenland) and S. Oppenheimer, ”Out of Eden”, 2004
390 A look farther back in time CO2 (ppmv) Years before present Lüthi, D., et al.. 2008. EPICA Dome C Ice Core 800KYr Carbon Dioxide Data. IGBP PAGES/World Data Center for Paleoclimatology Data Contribution Series # 2008-055
Some perspective Source: CEOS Handbook
Changes in the nitrogen cycle 1890 1990 Galloway & Cowling, Ambio 31 (2), 2002
Global agricultural land use Source: Foley et al., Science, 2005, Ramankutty & Foley, 1999
Global agricultural land use Source: Foley et al., Science, 2005, Ramankutty & Foley, 1999
We can be seen from space http://visibleearth.nasa.gov
Temperature projections IPCC AR4 WG I, 2007
The steamy summer of 2003 Casualties Economic effects www.grid.unep.ch/product/publication/download/ew_heat_wave.en.pdf
Unusual or normal? Temperature Anomaly (°C) Source: Stott et al. Nature 432, 610-614, 2004
“Extreme” weather UK Wroclaw, Poland, 1997 http://noahsark.isac.cnr.it/
Flooding in the UK 4-year event 12-year event 30-year event Source: Allen & Kabat, EuroScience Open Forum, 2004
Surprise: arctic sea ice Updated from Stroeve, et al., 2007. Geophys. Res. Lett., 34: L09501.
Where are we headed? Fossil Fuel CO2 Emissions (Pg C yr-1) Raupach et al. 2007, PNAS, updated; Le Quéré et al. 2009, Nature Geoscience
Planetary Boundaries New Scientist 27 Feb 2010 Scientific American April 2010 Rockström, et al., Nature, 2009
Planetary Boundaries: Authors Johan Rockström, Will Steffen, Kevin Noone, Åsa Persson, F. Stuart Chapin, III, Eric F. Lambin, Timothy M. Lenton, Marten Scheffer, Carl Folke, John Schellnhuber, Björn Nykvist, Cynthia A. de Wit, Terry Hughes, Sander van der Leeuw, Henning Rodhe, Sverker Sörlin, Peter K. Snyder, Robert Costanza, Uno Svedin, Malin Falkenmark, Louise Karlberg, Robert W. Corell, Victoria J. Fabry, James Hansen, Diana Liverman, Katherine Richardson, Paul Crutzen, Jonathan A. Foley
Some properties of PBs • Associated with a large-scale change in how planetary systems function (often a threshold or “tipping point”); these are non-negotiable • Have some “control” variable • Include normative aspects of defining preferred states - holocene stability
Some properties of PBs • Operate on time scales over which ethics and political action are relevant • A “safe operating space” can be created within the boundaries
Boundary Safe operating space Zone of uncertainty Planetary Boundaries
Climate 350 ppm CO2 +1 W/m2 Ocean acidification Aragonite saturation ratio > 2.75 Chemical pollution Not yet quantified Aerosol loading Not yet quantified Ozone depletion 276 DU Nitrogen & Phosphorus loading 35 MT N/yr 11 MT P/yr Biodiversity loss 10 E/MSY Freshwater use 4000 km3/yr Land use 15% Rockström, et al., Nature, 2009
Boundary choice: Major ice sheets – or not? Source: Zachos, J., et al. (2001), Science, 292, 686.
Climate Change Ozone depletion ? Phosphorus flow Latest data Atmospheric aerosol load ? ? 90-00 ? Nitrogen flow Ocean acidity 70-80 ? 50-60 Biodiversity loss Freshwater consumption ? Pre- Ind. Chemical pollution Agricultural land use
Consequences and solutions J. Foley, Scientific American, April 2010
Amazonian land use change 1975 http://visibleearth.nasa.gov/ Rondonia (central Amazon basin)
Amazonian land use change 1986 http://visibleearth.nasa.gov/ Rondonia (central Amazon basin)
Amazonian land use change 1992 http://visibleearth.nasa.gov/ Rondonia (central Amazon basin)
Amazonian land use change 2001 http://visibleearth.nasa.gov/ Rondonia (central Amazon basin)
It’s all connected Rockström, et al., Nature, 2009
... and how they work after Snyder, et al., Climate Dynamics 23, 279-302, 2004;
Anthropogenic CO2 in the oceans Source: Sabine, et al., Science 305, 367-371, 2004
Changing ocean pH pCO2 = 280 ppmv 1870 2000- 2009 pCO2 = 375 ppmv Source: Guinotte, et al., Coral Reefs 22, 551-558, 2003
Changing ocean pH pCO2 = 415 ppmv 2020- 2029 2040- 2049 pCO2 = 465 ppmv Source: Guinotte, et al., Coral Reefs 22, 551-558, 2003