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PLANETARY BOUNDARIES the urgent need for societal transformations
PLANETARY BOUNDARIES the urgent need for societal transformations MODERATOR: Andrew Revkin dotEarth, New York Times Sybil Seitzinger International Geosphere-Biosphere Programme Deborah Rogers International Human Dimensions Programme on Global Environmental Change Gisbert Glaser Senior Policy Advisor International Council for Science
Planetary and societal risksWhy we need planetary stewardship Professor Sybil Seitzinger Executive Director International Geosphere-Biosphere Programme
Antarctic ice core Modern humans appear in Africa Carbon dioxide Methane Carbon dioxide Temperature Methane Loulergue, L.,et al Orbittal and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 2008. Lüthi, D. et al High-resolution carbon dioxide concentration record 650,000-800,000 years before present Nature, 2008.
Antarctic ice core Beyond natural boundaries Methane Carbon dioxide Loulergue, L.,et al Orbittal and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 2008. Lüthi, D. et al High-resolution carbon dioxide concentration record 650,000-800,000 years before present Nature, 2008.
Source: GRIP ice core data (Greenland) And S. Oppenheimer, ”Out of Eden”, 2004 Human Development andGlacial-Interglacial Cycling Source: GRIP icecore data (Greenland) and S. Oppenheimer, ”Out of Eden”, 2004
IGBP Climate-change index Global carbon dioxide Arctic sea-ice minimum Global surface temperature Global sea level
IGBP Climate-change index
The Great Acceleration – a planet under pressure
Population US Bureau of the Census (2000) International database IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Total real GDP Nordhaus (1997) The economics of new goods. University of Chicago Press IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Foreign direct investment World Bank (2002) data and statistics IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Damming of rivers World Commission on Dams (2000) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Water use Shiklomanov (1990) Global Water Resources IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Fertiliser consumption International Fertilizer Industry Association (2002) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Urban population The State of the World’s Cities (2001) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Paper consumption Pulp and paper international (1993) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Motor vehicles Global environmental outlook (2000) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Telephones Canning (2001) A database of world infrastructure stocks, 1950-95 World Bank IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
International tourism World Tourism Organization (2001) Tourism industry trends IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Shrimp farm production IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Domesticated land IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Planetary response
Atmospheric CO2 concentration Etheridge et al. Geophys Res 101: 4115-4128 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Atmospheric N2O concentration Machida et al Geophys Res Lett 22:2921-2925 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Atmospheric CH4 concentration Blunier et al J Geophy Res 20: 2219-2222 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Northern hemisphere average surface temperature Mann et al Geophys Res Lett 26(6): 759-762 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Ozone depletion IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Tropical rainforest and woodland loss  IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Natural climatic disasters  IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Fisheries exploitation IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Coastal zone nitrogen flux IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Biodiversity loss IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
Great acceleration IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
“Our foot is stuck on the accelerator and we are heading towards an abyss.”     Ban Ki-Moon
A resilient Earth System
Reduced resilience – our precarious predicament
Where are the thresholds in the Earth system? Photograph by Annie Griffiths Belt National Geographic, February 2008 – © National Geographic Society, All rights reserved.
Ozone Depletion Climate Change Atmospheric Aerosol Loading Nitrogen Ocean  Acidification Phosphorus  Rate of Biodiversity Loss Global  FreshwaterUse Land System Change Chemical  Pollution  Rockström et al. 2009
2011 Global Risks ReportWorld Economic Forum “The world is in no position to face major, new shocks.”
Planetary stewardship- a safe operating space for humanity
Planetary Stewardship 2020 2040 2050 2030
New knowledge toward solutionsLondon, 26-29 March 2012
Planetary and societal risksWhy we need planetary stewardship Professor Sybil Seitzinger Executive Director International Geosphere-Biosphere Programme www.igbp.net Sybil.seitzinger@igbp.kva.se

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Planetary Boundaries: The Urgent Need for Societal Transformations

  • 1. PLANETARY BOUNDARIES the urgent need for societal transformations
  • 2. PLANETARY BOUNDARIES the urgent need for societal transformations MODERATOR: Andrew Revkin dotEarth, New York Times Sybil Seitzinger International Geosphere-Biosphere Programme Deborah Rogers International Human Dimensions Programme on Global Environmental Change Gisbert Glaser Senior Policy Advisor International Council for Science
  • 3. Planetary and societal risksWhy we need planetary stewardship Professor Sybil Seitzinger Executive Director International Geosphere-Biosphere Programme
  • 4.
  • 5. Antarctic ice core Modern humans appear in Africa Carbon dioxide Methane Carbon dioxide Temperature Methane Loulergue, L.,et al Orbittal and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 2008. Lüthi, D. et al High-resolution carbon dioxide concentration record 650,000-800,000 years before present Nature, 2008.
  • 6. Antarctic ice core Beyond natural boundaries Methane Carbon dioxide Loulergue, L.,et al Orbittal and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 2008. Lüthi, D. et al High-resolution carbon dioxide concentration record 650,000-800,000 years before present Nature, 2008.
  • 7. Source: GRIP ice core data (Greenland) And S. Oppenheimer, ”Out of Eden”, 2004 Human Development andGlacial-Interglacial Cycling Source: GRIP icecore data (Greenland) and S. Oppenheimer, ”Out of Eden”, 2004
  • 8. IGBP Climate-change index Global carbon dioxide Arctic sea-ice minimum Global surface temperature Global sea level
  • 10. The Great Acceleration – a planet under pressure
  • 11. Population US Bureau of the Census (2000) International database IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 12. Total real GDP Nordhaus (1997) The economics of new goods. University of Chicago Press IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 13. Foreign direct investment World Bank (2002) data and statistics IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 14. Damming of rivers World Commission on Dams (2000) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 15. Water use Shiklomanov (1990) Global Water Resources IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 16. Fertiliser consumption International Fertilizer Industry Association (2002) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 17. Urban population The State of the World’s Cities (2001) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 18. Paper consumption Pulp and paper international (1993) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 19. Motor vehicles Global environmental outlook (2000) IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 20. Telephones Canning (2001) A database of world infrastructure stocks, 1950-95 World Bank IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 21. International tourism World Tourism Organization (2001) Tourism industry trends IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 22. Shrimp farm production IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 23. Domesticated land IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 25. Atmospheric CO2 concentration Etheridge et al. Geophys Res 101: 4115-4128 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 26. Atmospheric N2O concentration Machida et al Geophys Res Lett 22:2921-2925 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 27. Atmospheric CH4 concentration Blunier et al J Geophy Res 20: 2219-2222 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 28. Northern hemisphere average surface temperature Mann et al Geophys Res Lett 26(6): 759-762 IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 29. Ozone depletion IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 30. Tropical rainforest and woodland loss IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 31. Natural climatic disasters IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 32. Fisheries exploitation IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 33. Coastal zone nitrogen flux IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 34. Biodiversity loss IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 35. Great acceleration IGBP synthesis: Global Change and the Earth System, Steffen et al 2004
  • 36. “Our foot is stuck on the accelerator and we are heading towards an abyss.” Ban Ki-Moon
  • 38. Reduced resilience – our precarious predicament
  • 39. Where are the thresholds in the Earth system? Photograph by Annie Griffiths Belt National Geographic, February 2008 – © National Geographic Society, All rights reserved.
  • 40. Ozone Depletion Climate Change Atmospheric Aerosol Loading Nitrogen Ocean Acidification Phosphorus Rate of Biodiversity Loss Global FreshwaterUse Land System Change Chemical Pollution Rockström et al. 2009
  • 41. 2011 Global Risks ReportWorld Economic Forum “The world is in no position to face major, new shocks.”
  • 42. Planetary stewardship- a safe operating space for humanity
  • 43. Planetary Stewardship 2020 2040 2050 2030
  • 44. New knowledge toward solutionsLondon, 26-29 March 2012
  • 45. Planetary and societal risksWhy we need planetary stewardship Professor Sybil Seitzinger Executive Director International Geosphere-Biosphere Programme www.igbp.net Sybil.seitzinger@igbp.kva.se

Notes de l'éditeur

  1. To note:London 7-10 MayPlanetary meeting focusing on solutions2500 leading global-change thinkersInfluence 2012 Earth Summit: Rio +20INTEGRATION of many research and policy communities is key. We want the best global change thinkers to attendPlanet Under Pressure: new knowledge, new solutions
  2. This great acceleration really started in the 50s
  3. To note:London 7-10 MayPlanetary meeting focusing on solutions2500 leading global-change thinkersInfluence 2012 Earth Summit: Rio +20INTEGRATION of many research and policy communities is key. We want the best global change thinkers to attendPlanet Under Pressure: new knowledge, new solutions
  4. The biophysical responses of the Earth System show many of the same features as the Great Acceleration in the human enterprise.The hockeystick pattern applies all key indicators that form the basis for human well being and environmental health.
  5. Nitrous oxide makes up an extremely small amount of the atmosphere - it is less than one-thousandth as abundant as carbon dioxide. However, it is 200 to 300 times more effective in trapping heat than carbon dioxide.Nitrogen is removed from the atmosphere by plants and converted into forms such as ammonia, which can then be used by the plants. This is called nitrogen fixation. At the same time, micro-organisms remove nitrogen from the soil and put it back into the atmosphere - denitrification - and this process produces nitrous oxide. Nitrous oxide also enters the atmosphere from the ocean.Nitrous oxide has one of the longest atmosphere lifetimes of the greenhouse gases, lasting for up to 150 years.Burning fossil fuels and wood is one source of the increase in atmospheric nitrous oxide, however the main contributor is believed to be the widespread use of nitrogen-base fertilisers. Sewage treatment plants may also be a major source of this gas.Since the Industrial Revolution, the level of nitrous oxide in the atmosphere has increased by 16%.
  6. Beyond climate