Countdown to Copenhagen

President Obama will be going to next month's international climate change meeting in Copenhagen--and Shareable.net will be there, too, with regular dispatches from contributor Chris Carlsson

In the meantime, you might zip over to Good magazine and read their useful series of pieces on the lead-up to Copenhagen. As Ben Jervey reports, this week a group of 26 climatologists released The Copenhagen Diagnosis: Updating the World on the Latest Climate Science “to synthesize the most policy-relevant climate science.” Key findings, as summarized by Jervey:

  • Surging greenhouse gas emissions: Global carbon dioxide emissions from fossil fuels in 2008 were nearly 40 percent higher than those in 1990. Even if global emission rates are stabilized at present-day levels, just 20 more years of emissions would give a 25 percent probability that warming exceeds 2 degrees Celsius. Even with zero emissions after 2030. Every year of delayed action increase the chances of exceeding 2 degrees of warming.
  • Recent global temperatures demonstrate human-based warming: Over the past 25 years, temperatures have increased at a rate of 0.190C per decade, in every good agreement with predictions based on greenhouse gas increases. Even over the past ten years, despite a decrease in solar forcing, the trend continues to be one of warming. Natural, short-term fluctuations are occurring as usual but there have been no significant changes in the underlying warming trend.
  • Acceleration of melting of ice-sheets, glaciers and ice-caps: A wide array of satellite and ice measurements now demonstrate beyond doubt that both the Greenland and Antarctic ice-sheets are losing mass at an increasing rate. Melting of glaciers and ice-caps in other parts of the world has also accelerated since 1990.
  • Rapid Arctic sea-ice decline: Summer-time melting of Arctic sea-ice has accelerated far beyond the expectations of climate models. This area of sea-ice melt during 2007-2009 was about 40 percent greater than the average prediction from IPCC AR4 climate models.
  • Current sea-level rise underestimates: Satellites show great global average sea-level rise (3.4 mm/yr over the past 15 years) to be 80 percent above past IPCC predictions. This acceleration in sea-level rise is consistent with a doubling in contribution from melting of glaciers, ice caps and the Greenland and West-Antarctic ice-sheets.
  • Sea-level prediction revised: By 2100, global sea-level is likely to rise at least twice as much as projected by Working Group 1 of the IPCC AR4, for unmitigated emissions it may well exceed 1 meter. The upper limit has been estimated as 2 meters sea-level rise by 2100. Sea-level will continue to rise for centuries after global temperature have been stabilized and several meters of sea level rise must be expected over the next few centuries.
  • Delay in action risks irreversible damage: Several vulnerable elements in the climate system (e.g. continental ice-sheets. Amazon rainforest, West African monsoon and others) could be pushed towards abrupt or irreversible change if warming continues in a business-as-usual way throughout this century. The risk of transgressing critical thresholds (“tipping points”) increase strongly with ongoing climate change. Thus waiting for higher levels of scientific certainty could mean that some tipping points will be crossed before they are recognized.
  • The turning point must come soon: If global warming is to be limited to a maximum of 2 degrees Celsius above pre-industrial values, global emissions need to peak between 2015 and 2020 and then decline rapidly. To stabilize climate, a decarbonized global society—with near-zero emissions of CO2 and other long-lived greenhouse gases—need to be reached well within this century. More specifically, the average annual per-capita emissions will have to shrink to well under 1 metric ton CO2 by 2050. This is 80 to 90 percent below the per-capita emissions in developed nations in 2000.

For an argument for the importance of sharing to countering climate change, see the Shareable.net Q&A with Robin Chase.

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