Earth News This Week

Showing posts with label Climate Change. Show all posts
Showing posts with label Climate Change. Show all posts

Wednesday, February 6, 2008

Geoforchungszentrum's 16 critical climate change effects

Potential Anthropogenic Tipping Elements in the Earth System

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© Schellnhuber 2007


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1 Arctic Sea Ice Loss

As sea ice melts in a warming climate, it exposes a dark ocean surface, which absorbs more solar radiation and thus amplifies the warming. Over the last 30 years the area covered by sea ice has decreased significantly. This is also bad news for many species, like seals or polar bears, which depend on that ice for hunting and breeding. Time Frame: ~ 100 yr.

2 Melting of Greenland Ice Sheet

Greenland’s ice sheet is melting due to the extraordinary warming of the Arctic region. Recent observations sug- gest an accelerated destabilization also due to melt-water lubrication effects. The complete collapse of the Greenland ice sheet would cause a global sea level rise of 7 m. Time Frame: Unknown due to highly non-linear processes. Current estimates: 300–1000 yr.

3 Methane Escape from Thawing Permafrost Regions and Continental Shelves

Huge amounts of methane, which is a highly potent greenhouse gas, could be released by global warming. On the one hand, terrestric methane will emanate from thawing permafrost areas in Siberia and Northern America. On the other hand, ‘methane ice’ assembled by natural processes over millions of years off many coasts might be activated by changing ocean temperatures and currents. Time Frame: ~ 1000 yr.

4 Boreal Forest Dieback

Northern boreal forests account for almost one third of the global forest inventory. They are declining in a warming climate because of enhanced disturbance stress through fires, pests, and storms. At the same time, their regenerative capabilities are diminished by temperature and water stress as well as direct human interference (logging, fragmentation, etc.). The dieback would trigger massive release of carbon dioxide, which in turn enhances climate change as well as significant losses in biodiversity. Time Frame: ~ 50–100 yr.

5 Suppression of Atlantic Deep Water Formation

The warm Atlantic surface ocean current is responsible for the benign climate in Northwestern Europe. This gre- at ‘conveyor belt’ is ultimately driven by cold and dense water sinking to the bottom of the North Atlantic off the coasts of Greenland and Labrador. A warming climate leads to an increased freshwater flow into the ocean, thus decreasing the water’s density and slowing down the deep water formation. Time frame: ~ 100–500 yr.

6 Climatic Change-Induced Ozone Hole over Northern Europe

Particularly Northern Europe could face a climate change-induced ozone hole. Global warming at the bottom of atmospheric strata implies cooling in the stratospheric “roof”. This cooling induces ice cloud formation which in turn provides a catalyst for ozone destruction. Time Frame: ~ 10–1000 yr.

7 Darkening of the Tibetan Plateau

As the snow cover of the Tibetan territory melts due to global warming, the exposed dark rock surface will amplify regional warming through increased absorption of solar radiation. As a side effect, the freshwater supply for many Asian countries, which depend on glacier melt water, will be reduced. Moreover, it is possible that the darkening of the Tibetan plateau could affect the Indian monsoon system. Time Frame: ~ 50–100 yr.

8 Disruption of Indian Monsoon

Up to 90% of India’s precipitation is provided by the regular summer monsoon. Carbon dioxide as well as aerosols play a key role in this highly variable system. Air pollution, land-cover change and greenhouse gas emissions could bring about a roller-coaster succession of intensified and weakened monsoons in South Asia causing extreme droughts and floods. Time Frame: 30–100 yr.

9 Re-Greening of the Sahara and Sealing of Dust Sources

Vegetation could re-appear due to higher precipitation in the Sahel region, but this greening of the Sahara may be overridden by intensive land-use, especially grazing. If the re-greening happened, it could seal major sources of dust that is blown across the Atlantic and fertilizes South American ecosystems. Time Frame: ~ 50 yr.

10 West African Monsoon Shift

The West African monsoon is affected both by heavy deforestation in coastal areas and increasing sea-surface temperatures. The future of this monsoon system is still uncertain. Global warming may bring about a doubling of dry years in the Sahel by the end of the century or a complete monsoon collapse, both of which would have profound large-scale impacts. Time Frame: ~ 50–100 yr.

11 Dieback of Amazon Rainforest

A large fraction of precipitation in the Amazon basin is recycled evaporation water. The reduction of regional rainfall in a warming climate, intimately connected to El Niño/Southern Oscillation, as well as forest fragmentation due to human activity could bring the forest cover to a critical threshold. Amazon dieback would have profound influence on the global climate and at the same time result in a huge loss of biodiversity. Time Frame: ~ 50–100 yr.

12 Change in Southern Pacific Climate Oscillation

Although uncertainties are large, some climate models predict an increased frequency and/or intensity of El Niño conditions in the Southern Pacific. The impacts of such a change in the oceanic oscillation patterns would be felt around the globe, especially in the form of droughts in South-East Asia and many other regions. Time Frame: Rapid changes possible in 10-100 yr.

13 Disruption of Marine Carbon Pump

This “pump” acts as a sink for both natural and anthropogenic excess CO2. There is a risk of a decline of this sink caused by increased ocean acidification and stratification owing to rising atmospheric CO2 levels. The acidification impedes floating and fixed organisms, such as plankton algae and corals, to build their skeletons, which bind carbon. Time Frame: unknown.

14 Suppression of Antarctic Deep Water Formation and Nutrients Upwelling

Similar to the North Atlantic, convection of water masses in the Southern ocean can be suppressed by freshwater inflow from melting ice. If there is a critical threshold, it has not been assessed so far. The resulting decline of nutrients would reduce krill, which marks the basis of the marine food chain. Time Frame: ~ 100 yr?

15 Collapse of the West Antarctic Ice Sheet

Although assumed to be not as vulnerable as the Green- land Ice Sheet, a collapse of the West Antarctic Ice Sheet could be initiated within this century. Warming oceans result in melting of offshore ice shelves, which currently impede the out-flow of the continental ice masses be- hind. Furthermore, the warm water could be undercutting the ice sheet and yield further separation from the bedrock, thus accelerating the decay. The complete ice sheet collapse would raise the global sea level by 4-5 m. Time frame: ~ 300–1000 yr.

16 Antarctic Ozone Hole

Already strongly perturbed by humanity’s emissions of chlorofluorocarbons in the past, the protective ozone layer is believed to be regenerating after these chemicals have been banned. Yet strong interactions between stratospheric ozone depletion and global warming may widen the ozone hole over the Antarctic once again. Time Frame: ~ 10–100 yr.



by Margret Boysen — last modified Tue, 17.07.2007 15:36

Thursday, October 25, 2007

Kyoto protocol: A Dodo?

Time to ditch Kyoto

Nature 449, 973-975 (25 October 2007) | doi:10.1038/449973a; Published online 24 October 2007

Gwyn Prins1 & Steve Rayner2

  1. Gwyn Prins is at the London School of Economics Mackinder Centre for the Study of Long Wave Events, London WC2A 2AE, UK.
  2. Steve Rayner is at the James Martin Institute for Science and Civilization, University of Oxford, Oxford OX1 1HP, UK.
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Climate policy after 2012, when the Kyoto treaty expires, needs a radical rethink. More of the same won't do, argue Gwyn Prins and Steve Rayner.

Time to ditch Kyoto

B. MELLOR

The Kyoto Protocol is a symbolically important expression of governments' concern about climate change. But as an instrument for achieving emissions reductions, it has failed1. It has produced no demonstrable reductions in emissions or even in anticipated emissions growth. And it pays no more than token attention to the needs of societies to adapt to existing climate change. The impending United Nations Climate Change Conference being held in Bali in December — to decide international policy after 2012 — needs to radically rethink climate policy.

Kyoto's supporters often blame non-signatory governments, especially the United States and Australia, for its woes. But the Kyoto Protocol was always the wrong tool for the nature of the job. Kyoto was constructed by quickly borrowing from past treaty regimes dealing with stratospheric ozone depletion, acid rain from sulphur emissions and nuclear weapons. Drawing on these plausible but partial analogies, Kyoto's architects assumed that climate change would be best attacked directly through global emissions controls, treating tonnes of carbon dioxide like stockpiles of nuclear weapons to be reduced via mutually verifiable targets and timetables. Unfortunately, this borrowing simply failed to accommodate the complexity of the climate-change issue2.

Kyoto has failed in several ways, not just in its lack of success in slowing global warming, but also because it has stifled discussion of alternative policy approaches that could both combat climate change and adapt to its unavoidable consequences. As Kyoto became a litmus test of political correctness, those who were concerned about climate change, but sceptical of the top-down approach adopted by the protocol were sternly admonished that "Kyoto is the only game in town". We are anxious that the same mistake is not repeated in the current round of negotiations.

The Kyoto Protocol was always the wrong tool for the nature of the job.

Already, in the post-Kyoto discussions, we are witnessing that well-documented human response to failure, especially where political or emotional capital is involved, which is to insist on more of what is not working: in this case more stringent targets and timetables, involving more countries. The next round of negotiations needs to open up new approaches, not to close them down as Kyoto did.

Economic theory recognizes the futility of throwing good money after bad. In politics, however, sunk costs are often seen as political capital or as an investment of reputation and status. So we acknowledge that those advocating the Kyoto regime will be reluctant to embrace alternatives because it means admitting that their chosen climate policy has and will continue to fail. But the rational thing to do in the face of a bad investment is to cut your losses and try something different.

No silver bullet

Influenced by three major policy initiatives of the 1980s, the Kyoto strategy is elegant but misguided. Ozone depletion, acid rain and nuclear arms control are difficult problems, but compared to climate change they are relatively simple. Ozone depletion could be prevented by controlling a small suite of artificial gases, for which technical substitutes could be found. Acid rain was mainly caused by a single activity in a single industrial sector (power generation) and nuclear arms reductions were achieved by governments agreeing to a timetable for mutually verifiable reductions in warheads. None of this applies to global warming.

The rational thing to do in the face of a bad investment is to cut your losses and try something different.

In practice, Kyoto depends on the top-down creation of a global market in carbon dioxide by allowing countries to buy and sell their agreed allowances of emissions. But there is little sign of a stable global carbon price emerging in the next 5–10 years. Even if such a price were to be established, it is likely to be modest — sufficient only to stimulate efficiency gains3. Without a significant increase in publicly funded research and development (R&D) for clean energy technology and changes to innovation policies, there will be considerable delay before innovation catches up with this modest price signal.

On present trends, for another 20 years, the world will continue installing carbon-intensive infrastructure, such as coal power plants, with a 50-year lifetime. If climate change is as serious a threat to planetary well-being as we have long believed it to be, it is time to interrupt this cycle.

Climate change is not amenable to an elegant solution because it is not a discrete problem. It is better understood as a symptom of a particular development path and its globally interlaced supply-system of fossil energy. Together they form a complex nexus of mutually reinforcing, intertwined patterns of human behaviour, physical materials and the resulting technology. It is impossible to change such complex systems in desired ways by focusing on just one thing.

Social scientists understand how path-dependent systems arise4; but no one has yet determined how to deliberately unlock them. When change does occur it is usually initiated by quite unexpected factors. When single-shot solutions such as Kyoto are attempted, they often produce quite unintended, often negative consequences. The many loopholes that have enabled profiteers to make money from the Clean Development Mechanism, without materially affecting emissions, are examples5. Therefore, there can be no silver bullet — in this case the top-down creation of a global carbon market — to bring about the desired end.

Time to ditch Kyoto

L. LOMBARDI/ZUMA PRESS/NEWSCOM

Climate villains? Protesters have called for the United States and Australia to ratify the Kyoto Protocol.

But could there be silver buckshot? Could we assemble a portfolio of approaches that would move us in the right direction, even though we cannot predict which specific ones might stimulate the necessary fundamental change? If so, what would such a portfolio look like? We believe that a radical rethink of climate policy should possess at least five central elements.

Focus mitigation efforts on the big emitters

The notion that emissions mitigation is a global commons problem, requiring consensus among more than 170 countries, lies at the heart of the Kyoto approach. Engaging all of the world's governments has the ring of idealistic symmetry (matching global threat with universal response), but the more parties there are to any negotiation, the lower the common denominator for agreement — as has been the case under Kyoto.

The G8+5 Climate Change Dialogue, established in 2006 to convene the leaders of the top 13 polluters, was a belated recognition of the error of involving too many parties, each with dramatically different stakes and agendas. In September, the United States convened the top 16 polluters. Such initiatives are summarily dismissed by Kyoto's true believers, who see them as diversions rather than necessary first steps. However, these approaches begin to recognize the reality that fewer than 20 countries are responsible for about 80% of the world's emissions. In the early stages of emissions mitigation policy, the other 150 countries only get in the way.

Allow genuine emissions markets to evolve from the bottom up

Theoretically, the simplest way to establish a price signal would be through a carbon tax. However, past experience with Britain's fuel price escalator (1993–99) and US President Bill Clinton's attempt to introduce a modest 4.3-cent-per-gallon hike in gasoline tax, shows there are serious political obstacles to establishing a level of tax sufficiently high to encourage energy efficiency, let alone to stimulate serious investments in innovation.

An alternative price-based approach to market failure is cap-and-trade. But to work, such schemes must be built — like all genuine markets — from the bottom up. The cap shapes the market by signalling the social goal as simply as possibly: in this case, reduction of anthropogenic impact on the environment. The market does the rest. But, in trying to introduce, from the top down, a global market in all greenhouse gases and all sources and sinks, the Kyoto approach tries to do too much, too soon, especially in the absence of binding legal frameworks to enforce contracts among parties who are not bound by other strong ties.

There is no precedent for imposing a global trading system from above. First, lessons need to be learned from regional experiments with trading. The European Union Emission Trading Scheme confined itself to trading only in carbon, but then made the fatal error of allowing governments unrestricted powers to allocate allowances instead of auctioning a limited supply, leading to a collapse in the price. The Chicago Climate Exchange is successfully trading a basket of gases, but participation is voluntary. Eventually, different trading systems could evolve and link up as sensible standard practices emerge, giving rise to a global market. But in the final analysis, cap-and-trade cannot deliver the escape velocity required to get investment in technological innovation into orbit, in time. That calls for something else.

Put public investment in energy R&D on a wartime footing

We stare at stark divergences of trends. On the one hand, the International Energy Agency predicts a doubling of global energy demand from present levels in the next 25 years. On the other, since 1980 there has been a worldwide reduction of 40% in government budgets for energy R&D6. Without huge investment in R&D, the technologies upon which a viable emissions reduction strategy depends will not be available in time to disrupt a new cycle of carbon-intensive infrastructure.

So investment in energy R&D should be placed on a wartime footing. This is a cause that embraces the political spectrum, including Kyoto supporters. In 1992 former US Vice-President Al Gore called for a 'strategic environment initiative' as part of his vision for a 'global Marshall Plan'. The conservative American Enterprise Institute in Washington DC also supports primary research on sustainable new energy technologies. In 2006, Lord Rees, the president of Britain's Royal Society suggested that major public investment in R&D should be kick-started by a global investment in energy technologies research on the scale of the Manhattan Project7.

It seems reasonable to expect the world's leading economies and emitters to devote as much money to this challenge as they currently spend on military research — in the case of the United States, about $80 billion per year. Such investment would provide a more promising foundation for decarbonization of the global energy system than the current approach.

Increase spending on adaptation

For the best part of a decade, discussion of adaptation was regarded by most participants in climate policy-making as tantamount to betrayal8. Even though it was widely recognized by the end of the 1980s that the existing stock of atmospheric greenhouse gases was likely to lead to some inevitable warming, the policy community suppressed discussion of adaptation out of fear that it would blunt the arguments for greenhouse-gas mitigation.

Today, although the taboo on discussing adaptation is lifting, the allocation of effort remains skewed. The (unmet) commitment of international resources to the multilateral Adaptation Fund under the United Nations Climate Change Convention is $1.5 billion, derived in part from a tax on the Clean Development Mechanism. Funds for mitigation, however, come from many sources and total at least $19 billion. We believe that global adaptation efforts need to be funded at comparable scales to those we advocate for investment in technology R&D.

Time to ditch Kyoto

T. YAMANAKA/AFP/GETTY

J. SUTTON-HIBBERT/ZUMA PRESS/NEWSCOM

The treaty negotiated at Kyoto in 1997 has been ratified by 172 nations. Has it made a difference?

Many climate activists seem to assume that slowing greenhouse-gas emissions has logical and ethical priority over adapting to climate impacts. But the ethical issues cut both ways. Current emissions reductions will mainly benefit future generations, whereas the momentum already in the climate system drives the near-term. Faced with imminent warming, adaptation has a faster response time, a closer coupling with innovation and incentive structures, and thereby confers more protection more quickly to more people. It is not clear to us that the interests of millions of people in poorer countries who depend on marginal ecosystems are best served by an exclusive preoccupation with mitigation. Indeed, such a narrow focus is likely to be a fatal error. Mitigation and adaptation must go hand in hand.

Work the problem at appropriate scales

Climate change is a multi-level governance problem. Some commentators recognized early on that it is not just, or even primarily, a matter for negotiation among nation states9. However, national governments have been slow to recognize this. Global responses to climate policy can learn from the US system of federalism that encourages small-scale policy experiments at the state or local-government levels as well as with the philanthropic and private sectors. When state or local policies succeed, such experiments can be implemented at the federal level, and often with the enthusiastic support of national politicians.

David Victor at the Council on Foreign Relations and his colleagues have proposed exactly this approach to climate policy, suggesting that a "global federalism of climate policy" is emerging from the rubble of the Kyoto Protocol. Rather than the top-down universalism embodied in Kyoto, countries would choose policies that suit their particular circumstances. Ironically, this 'policies and measures' approach was being pursued before the emergence of the Kyoto regime10. However, it has been largely neglected in the post-Kyoto process. Although a bottom-up approach may seem painfully slow and sprawling, it may be the only way to build credible institutions that markets endorse. The agenda for the Bali conference should focus on this and on the scale-up of energy R&D rather than on drafting a 'bigger and better' version of Kyoto.

The silver buckshot approach

Sometimes the best line of attack is not head-on. Indirect measures can deliver much more: these range from informational instruments, such as labelling of consumer products; market instruments, such as emissions trading; and market stimuli, such as procurement programmes for clean technologies; to a few command-and-control mechanisms, such as technology standards11. The benefit of this approach is that it focuses on what governments, firms and households actually do to reduce their emissions, in contrast to the directive target setting that has characterized international discussions since the late 1980s.

Because no one can know beforehand the exact consequences of any portfolio of policy measures, with a bottom-up approach, governments would focus on navigation, on maintaining course and momentum towards the goal of fundamental technological change, rather than on compliance with precise targets for emissions reductions. The flexibility of this inelegant approach would allow early mitigation efforts to serve as policy experiments from which lessons could be learned about what works, when and where12. Thus cooperation, competition and control could all be brought to bear on the problem.

Does the Kyoto bandwagon have too much political momentum? We hope not. It will take courage for a policy community that has invested much in boosting Kyoto to radically rethink climate policy and adopt a bottom-up 'social learning' approach. But finding a face-saving way to do so is imperative. Not least, this is because today there is strong public support for climate action; but continued policy failure 'spun' as a story of success could lead to public withdrawal of trust and consent for action, whatever form it takes.

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References

  1. Victor, D. The Collapse of the Kyoto Protocol and the Struggle to Slow Global Warming (Princeton Univ. Press, New Jersey, 2001).
  2. Prins, G. & Rayner, S. The Wrong Trousers. Radically Rethinking Climate Policy Joint Working Paper (James Martin Inst./Mackinder Centre, in the press).
  3. British Petroleum Statistical Review of World Energy June 2007; http://www.bp.com/statisticalreview
  4. Arthur, W. B. Econ. J. 99, 116–131 (1989). | Article |
  5. Wara, M. Nature 445, 595–596 (2007). | Article | PubMed | ChemPort |
  6. Rayner, S. The International Challenge of Climate Change: UK Leadership in the G8 and EU, Memorandum to the Environmental Audit Committee, House of Commons (24 November 2004).
  7. Rees, M. Science 313, 591 (2006). | Article | PubMed | ChemPort |
  8. Pielke, R. A., Prins, G., Rayner, S. & Sarewitz, D. Nature 445, 597–598 (2007). | Article | PubMed | ChemPort |
  9. Rayner, S. & Malone, E. L. Ten Suggestions for Policy Makers in Human Choice and Climate Change: An International Assessment, Vol. 4, What Have We Learned? (eds Rayner, S. & Malone, E.) 109–138 (Battelle Press, Columbus, Ohio, 1998).
  10. Victor, D. G., House, J. C. & Joy, S. Science 311, 336 (2006). | PubMed | ChemPort |
  11. US Department of Energy A Compendium of Options for Government Policy to Encourage Private Sector Responses to Potential Climate Change. Report to the Congress of the United States (1989).
  12. Verweij, M. et al. Public Administration 84, 817–843 (2006).