Published on April 7, 2008
Meeting the Climate-Change Challenge: Meeting the Climate-Change Challenge John P. Holdren Director, The Woods Hole Research Center Teresa & John Heinz Professor of Environmental Policy, Harvard University President, American Association for the Advancement of Science SES Distinguished Scientist Seminar Marine Biological Laboratory Woods Hole 3 November 2006 In this talk I will argue that…: In this talk I will argue that… Climate change is coming at us faster, with larger impacts and bigger risks, than even most climate scientists expected as recently as a few years ago. The stated goal of the UNFCCC – avoiding dangerous anthropogenic interference in the climate – is in fact unattainable, because today we are already experiencing dangerous anthropogenic interference. The real question now is whether we can still avoid catastrophic anthro-pogenic interference in climate. There is no guarantee that catastrophe can be avoided even we start taking serious evasive action immediately; but if we wait even one more decade before starting, the chance of avoiding catastrophe will get very much smaller. And I will talk about what, specifically, we need to do. What climate change means: What climate change means Climate consists of averages & extremes of hot & cold wet & dry snowpack & snowmelt winds & storm tracks ocean currents & upwellings and the patterns of these in space and time. Small changes in global-average surface T entail large & consequential changes in climatic patterns. Difference between an ice age & an interglacial is ~5°C. The stakes in climate change: The stakes in climate change Climate governs, so climate change alters, productivity of farms, forests, & fisheries prevalence of oppressive heat &humidity geography of disease damages from storms, floods, droughts, wildfires property losses from sea-level rise expenditures on engineered environments distribution & abundance of species What is the evidence that climate is now changing in unusual & threatening ways?: What is the evidence that climate is now changing in unusual & threatening ways? We know -- from thermometer records in the atmosphere and the oceans, and from ice cores, bore holes, tree rings, corals, pollens, sediments, and more -- that Earth’s climate is now changing at a pace far outside the range of expected natural variation, and in the opposite direction from what the known, natural, cyclic influences on climate would otherwise be causing at this time. We should be cooling, but we are warming up: by ~0.8 C in Tavg in the last 125 years, more over the continents, several times that over the continents at high latitudes. On a worldwide average, the 12 warmest years of the last 125 have all occurred since 1990, 20 of the 21 warmest since 1980. The last 50 years appear to have been the warmest half century in 6000 years. Is current climate change unusual?: Is current climate change unusual? National Research Council, 2006 1000 years of “proxy” surface temperatures, 100+ from thermometers Slide7: Upward trend continues; 2005 was a new record; we’re at 0.8°C above 1880-1900 average; 0.5°C since 1970. J. Hansen et al., PNAS 103: 14288-293 (26 Sept 2006) Green bars show 95% confidence intervals Thermometers: global T has risen 0.8°C in 125 yrs °C Slide8: Temperature increases are nonuniform: higher mid-continent, highest of all in far North. (These are observations, not modeling results.) J. Hansen et al., PNAS 103: 14288-293 (26 Sept 2006) 2001-2005 mean ∆Tavg above 1951-80 base, °C Slide9: Hadley Centre, 2003 Surface, balloon, & satellite temperatures agree Further evidence of changing climate: Further evidence of changing climate As expected in a warming world, observations over recent decades also show… Evaporation & rainfall are increasing; Coastal glaciers are retreating; Mountain glaciers are disappearing; Permafrost is thawing; Sea ice is shrinking; Greenland is melting; Sea level is rising; Species are moving. Evaporation & precipitation are increasing: Evaporation & precipitation are increasing NCDC, 2000 Effect is not uniform; most places getting wetter, some getting drier. Slide12: Muir Glacier, Alaska, 1941-2004 NSIDC/WDC for Glaciology, Boulder, compiler. 2002, updated 2006. Online glacier photograph database. Boulder, CO: National Snow and Ice Data Center. August 1941 August 2004 Coastal glaciers are retreating Slide13: Courtesy Lonnie Thompson Mountain glaciers are disappearing Slide14: Permafrost melts when T ≥ 0°C ACIA 2004 Permafrost is thawing Average annual ground temperature, Fairbanks, AK °C Slide15: NASA photograph Extent of Arctic summer ice in 1979 (top satellite image) and in 2003 (lower satellite image). North Polar ice cap is sea ice -- it’s floating and so does not change sea level when it melts. But the reduced reflectivity when the ice is replaced by water amplifies the warming effect of greenhouse gases. Sea ice is shrinking Greenland is melting: Greenland is melting ACIA, 2004 Summer surface melting on Greenland, 1979-2002 Slide17: Greenland melting (continued) 2005 broke the 2002 record Slide18: 1993-2003 ≈ 35 mm = 3.5 mm/yr; compare 1910-1990 = 1.5±0.5 mm/yr. Sea-level is rising mm ACIA, 2004 Slide19: Species are moving So, global climate is changing…: So, global climate is changing… in the direction of average warming, accompanied by many phenomena consistent with this, and at pace that is unusual in the recent historical record. But we know climate has sometimes changed quite abruptly in the past from natural causes. Is it really humans who are responsible for what is happening now? Or is it nature? What is the evidence? How much is human-caused?: How much is human-caused? NATURAL INFLUENCES ON GLOBAL CLIMATE variations in the energy output of the Sun variations in the Earth’s orbit and tilt continental drift changes in atmospheric composition from volcanoes, biological activity, weathering of rocks “internal” dynamics of ice-ocean-land-atmosphere system HUMAN INFLUENCES ON GLOBAL CLIMATE rising concentration of “greenhouse gases” (GHG) from deforestation, agricultural practices, fossil-fuel burning rising concentration of particulate matter from agricultural burning, cultivation, fossil-fuel burning, alteration of Earth’s surface reflectivity by deforestation, desertification increased high cloudiness from aircraft contrails Slide22: 400,000 years of greenhouse-gas & temperature history based on bubbles trapped in Antarctic ice Time scale expanded for last 150 years (right side of diagram) CO2 & CH4 are far above range of natural variation in current geologic era. Last time CO2 >300 ppm was 25 Myr BP in Eocene. Hansen,Clim.Change 68, 2005 The strengths of the natural and human influences can be measured or estimated, and then compared.: The strengths of the natural and human influences can be measured or estimated, and then compared. • The measure used in the climate-science community for quantifying and comparing natural & human influences is the change they cause in the flow of radiant energy in the atmosphere. This measure is called radiative forcing or just forcing. Its units are watts per square meter (W/m2), averaged over the globe and over the year, defined as positive when the effect is in the direction of warming Earth’s surface. • The best estimates of the forcings from all the influences on global climate in the 250 years since the beginning of the Industrial Revolution indicate that the biggest effect has been from the rising concentrations of greenhouse gases in this period. Slide24: Effective climate forcings 1750-2000 Correlating various lines of evidence has reduced uncertainties Units are watts per square meter alteration in global-average atmospheric radiation flow WARMING COOLING Slide25: The main cause of the CO2 build-up in the last 250 years has been emissions from fossil fuels & deforestation Fossil-fuel contribution is confirmed by reduced C-14 content. Fossil fuels provide 80% of civilization’s energy today. The “Fingerprint” of GHG on Global Climate: The “Fingerprint” of GHG on Global Climate Observations warming of near-surface ocean exactly accounts for energy imbalance caused by GHG & particles decreased day-night temperature differences larger T increases in winter than summer Match with theory & models Magnitudes and geographic & temporal patterns of changes match what theory & models say should result from the observed changes in GHG, taking into account effects of observed changes in anthropogenic & volcanic particulates + best estimates of changes in solar output. This pattern match is a “fingerprint” unique to GHG. If something else were driving current climatic change, fingerprint would be different. Slide27: Hansen et al., SCIENCE 308:1425-31 (2005) Measured increase in ocean heat storage matches what models predict to result from the energy inflow-outflow imbalance arising from the currently estimated forcings. Slide28: Source: Hansen et al., Earth's energy imbalance: Confirmation and implications. Science 308, 1431, 2005. (A) Forcings used to drive climate simu- lations. (B) Simulated and observed surface temperature change. The smoking gun: The smoking gun Essentially all of the observed climate-change phenomena are consistent with the predictions of climate science for GHG-induced warming. No alternative “culprit” identified so far – no potential cause of climate change other than greenhouse gases – yields this “fingerprint” match. A credible skeptic would need to explain both what the alternative cause of the observed changes is and how it could be that GHGs are NOT having the effects that all current scientific understanding says they should have. (No skeptic has done either thing.) Serious impacts are already occurring: Serious impacts are already occurring Frequency of major floods, droughts, heat waves, & wildfires is up all over the world…as predicted by theory & models. Evidence is persuasive that increasing frequency of powerful tropical storms is also being driven by global climate change. Heat stress from ocean warming is impacting coral reefs worldwide, exacerbated by increasing acidity from CO2 uptake. Moist tropical forests are drying out & burning. World Health Organization estimates direct health impacts of climate change already amount to ≥150,000 premature deaths/yr in 2000. Slide31: There’s a consistent 50-year upward trend in every region except Oceania, where the 1990s were a bit below the 1980s. Floods by continent & decade from 1950 Slide32: The trend has been upward everywhere. Wildfires by continent & decade from 1950 Slide33: Westerling et al., SCIENCE, 18 August 2006 Correlation of wildfire increases with temperature is clear Slide34: Running, Science, 18 August 2006 This works in part through soil moisture Slide35: Tropical Cyclone Power Dissipation Index (PDI) has increased substantially over past 50 years along with tropical sea surface temperatures Source: Kerry Emanuel, MIT, http://wind.mit.edu/~emanuel/anthro2.htm. SST anomaly (deg C) with arbitrary vertical offset. PDI scaled by constant. Slide36: GFDL CM2.1 Historical Forcing Runs Using 5 “Random” Initial Conditions Deg C Year Source: Knutson et al. (2005) J. of Climate, accepted for publication. Long-term warming of the “Main Development Region” is consistent with climate model historical simulations that include greenhouse gas forcing… Slide37: McWilliams et al., ECOLOGY, 86, 2055, 2005 Bleaching of coral reefs has been increasing with sea surface temperature (SST) all over the world. These results are from the Caribbean. The Amazon is drying & burning under the influence of deforestation & climate-change-induced drought: The Amazon is drying & burning under the influence of deforestation & climate-change-induced drought Nepstad et al., Forest Ecology & Management 154, 2001 Slide39: WHO estimates climate change already causing ≥150,000 premature deaths/yr in 2000 Slide40: IPCC 2001scenarios to 2100 ---------------- Where are we headed? The next 100 years compared to the last 1000 Projections of global average surface temperature show we’re heading for a climatic state far outside the range of variation of the last 1000 years. Indeed, we’re on our way to making the world hotter in the 21st century than it’s been in the last million years. Slide41: Note that continental warming far exceeds the global average. Mid-21st century warming under BAU Impacts of BAU climate change : Impacts of BAU climate change Consequences expected with high likelihood include… reduced agricultural productivity in many regions at ∆Tavg ≈ 2-3°C; nearly everywhere at ∆Tavg > 3°C; increasing devastation from droughts, heat waves, wildfires, powerful storms, and floods; accelerating loss of biodiversity from its two greatest reservoirs: tropical forests and coral reefs expanded geographic ranges of malaria, cholera, dengue fever, and other diseases whose vectors or pathogens are temperature- or moisture-dependent; significant property losses from slowly rising sea level (~1.5 feet per century) as a result of thermal expansion of sea water. Slide43: Easterling and Apps, 2005 Crop yields in tropics start dropping at ∆T ≥ 1-1.5°C Slide44: Easterling and Apps, 2005 Temperate-zone crop yields start dropping at ∆T ≥ 1-2°C Slide45: Drought in the Sahel gets worse in a warming world Isaac Held, NOAA GFDL, 3-06 Slide46: Extreme heat waves in Europe are already 2X more frequent due to global warming, with much more to come Black lines are observed temps, smoothed & unsmoothed; red, blue, & green lines are Hadley Centre simulations w natural & anthropogenic forcing; yellow is natural only. Asterisk and inset show 2003 heat wave that killed 35,000. Stott et al., Nature 432: 610-613 (2004) Slide47: Projected differences 1990s to 2090s by UK model show large warming, drying, carbon loss in Amazon Cox et al., Theor. Appl. Climatol. 78: 137-156 (2004) Slide48: Acidification of the ocean from CO2 uptake: history and “business as usual” projection Red line is global annual average; blue lines show ocean-to-ocean & seasonal variation. Ocean pH has already fallen by 0.1 pH unit. Projected additional changes are likely to have large impacts on corals and other ocean organisms that make skeletons/ shells from calcium carbonate. Additional possible outcomes: Additional possible outcomes Other possible outcomes for which evidence is growing include… drastic changes in ocean circulation patterns, with large impacts on regional climates and on fisheries; rapid increases in sea level (2-4 meters per century?) from melting, slumping, disintegration of Greenland & Antarctic ice sheets; accelerated emissions of CO2 and CH4 from warming northern soil & melting permafrost, sharply increasing the pace of expected impacts and the possibilities for unexpected ones. Atlantic “conveyor” behavior: Atlantic “conveyor” behavior NATURE, 12-01-05 Theory & models predict that global warming will slow the con-veyor. Recent measurements suggest north-ward heat transport by the conveyor may already have slowed by 25% Greenland, Antarctica, & future sea level: Greenland, Antarctica, & future sea level Recent observations of accelerating ice loss from Greenland & instability in West Antarctic Sheet, plus paleoclimate evidence, indicate rapid sea level rise from warming is possible. All the ice on Greenland ≈ 7 m increase in sea level; ice in West Antarctic Ice Sheet ≈ 5 m. Rates at which this ice could become sea water are still highly uncertain, but 12 m in 350-500 years is possible (~3 m per century); some think even faster is possible (Hansen 2005). East Antarctic Ice Sheet could add another 60 m, presumably only over many centuries…but recent surprises indicate science uncertain here. Slide52: From a presentation by Richard B. Alley, U of Pennsylvania (with permission) +7 m +12 m +70 m GIS = Greenland Ice Sheet WAIS = West Antarctic Ice Sheet EAIS = East Antarctic Ice Sheet The choices: The choices Facing these dangers, we have 3 options: Mitigation, meaning measures to reduce the pace & magnitude of the changes in global climate being caused by human activities. Adaptation, meaning measures to reduce the adverse impacts on human well-being resulting from the changes in climate that do occur. Suffering the adverse impacts that are not avoided by either mitigation or adaptation. The choices (concluded): The choices (concluded) Mitigation and adaptation are both essential. Human-caused climate change is already occurring. Adaptation efforts are already taking place and must be expanded. But adaptation becomes costlier and less effective as the magnitude of climate changes grows. The greater the amount of mitigation that can be achieved at affordable cost, the smaller the burdens placed on adaptation and the smaller the suffering. The remainder of this tutorial focuses mainly on mitigation: the size of the need, the available approaches, and the policy levers and prospects. Mitigation by managing forests & soils: Mitigation by managing forests & soils Reduce emissions of CO2 from deforestation in the tropics. “Avoided deforestation” depends on figuring out how owners of forest land – individuals, firms, countries – can be paid not to deforest, reflecting the value to society of keeping the forests intact. Accelerate reforestation and afforestation in regions where this is practicable. Improve management of agricultural soils to increase carbon storage. The last two could take up ~20% of atmospheric CO2 buildup expected in 21st century under “business as usual”. Mitigation by reducing emissions of CH4 & soot: Mitigation by reducing emissions of CH4 & soot Anthropogenic methane (CH4) comes 30% from energy systems, 30% from livestock, 25% from agriculture, 15% from landfills & waste treatment. Technical means exist for reducing all of these. Methane’s relatively short atmospheric lifetime means emissions reductions translate quickly into reduced concentrations, thus reduced forcing. Soot comes from 2-stroke & diesel engines as well as from traditional uses of biomass fuels, agricultural burning, and forest fires. The engine and biomass fuels emissions are amenable to sharp reduction by technical means. The very short atmospheric lifetime of soot (days to weeks) means emissions reductions translate quickly into reduced forcing. Mitigation by geo-engineering: Mitigation by geo-engineering Increasing surface reflectivity to cool the Earth Humans have done this inadvertently by deforestation, desertification, but more is undesirable. Reflectivity of man-made surfaces (buildings, roads) can be increased, but global impact is limited by small fraction of land surface used for these purposes (~2%). Large-scale alteration of reflectivity of oceans would be expected to have undesired climatological & ecological side effects. Increasing the atmosphere’s reflectivity by injecting reflecting particles into the stratosphere might be affordable (& reversible), but would be likely to deplete stratospheric ozone. Placing reflecting materials or mirrors in Earth orbit (or at the Lagrangian equilibration point between the Sun and the Earth) would be staggeringly expensive. Mitigation by reducing CO2 emissions from energy systems: Mitigation by reducing CO2 emissions from energy systems The emissions arise from a 4-fold product… C = P x GDP / P x E / GDP x C / E where C = carbon content of emitted CO2 (kilograms), and the four contributing factors are P = population, persons GDP / P = economic activity per person, $/pers E / GDP = energy intensity of economic activity, GJ/$ C / E = carbon intensity of energy supply, kg/GJ For example, in the year 2000, the world figures were… 6.1x109 pers x $7400/pers x 0.01 GJ/$ x 14 kgC/GJ = 6.4x1012 kgC = 6.4 billion tonnes C What happens to these factors on the “business as usual” path?: What happens to these factors on the “business as usual” path? 2000 2050 2100 ------- ------- ------- Population, billions 6.1 9 10 Economy, trillion 2000$ 45 150 480 Energy, exajoules 450 900 1800 Fossil C in CO2, gigatons 6.4 14 21 Corresponds to 2.4%/yr avg growth of real GDP, 1.0%/yr decline in energy intensity of GDP, 0.2%/yr decline in C intensity of energy supply. Where’s the leverage for reductions in these?: Where’s the leverage for reductions in these? POPULATION Lower is better for lots of reasons: 8 billion people in 2100 is preferable by far to 10 billion. Reduced growth can be achieved by measures that are attractive in their own right (e.g., education, opportunity, health care, reproductive rights for women). GDP PER PERSON This is not a lever that most people want to use, because higher is generally accepted to be better. But we’re not getting rich as fast as we think if GDP growth comes at the expense of the environmental underpinnings of well-being. Internalizing environmental costs of economic growth (including those of climate change) may slow that growth a bit...but not much. Some lifestyle changes in industrialized countries could increase quality of life even though they reduced GDP. Leverage against CO2 emissions (continued): Leverage against CO2 emissions (continued) ENERGY INTENSITY OF GDP Getting more GDP out of less energy – i.e. increasing energy efficiency – has been a long-term trend. It could be accelerated. It entails more efficient cars, trucks, planes, buildings, appliances, manufacturing processes. This opportunity offers the largest, cheapest, fastest leverage on carbon emissions. CARBON INTENSITY OF ENERGY SUPPY This ratio too has been falling, but more slowly than energy intensity of GDP. Reducing it entails changing… the mix of fossil & non-fossil energy sources (most importantly more renewables and/or nuclear) and/or the characteristics of fossil-fuel technologies (most importantly with carbon capture & sequestration). Reducing E/GDP: Transportation: Reducing E/GDP: Transportation Oil used as transport fuel ≈ 25% of global CO2 from fossil-fuel combustion Growth in these uses can be reduced by… increasing the efficiency of cars, trucks, buses, trains, aircraft increasing the load factors of these (e.g., passengers per vehicle per trip) mode switching (e.g., cars buses, trucks trains) urban & economic planning that affects living & production patterns so as to reduce commuting and freight transport Reducing E/GDP: Buildings: Reducing E/GDP: Buildings Heating, cooling , refrigeration, lighting, office equipment ≈ 33% of global CO2 from fossil-fuel combustion. Energy used for these purposes can be reduced by… improvements in building envelopes (wall & roof insulation, high-performance windows) improved building orientation, shading, passive energy storage; increased efficiency of heating & cooling (improved furnaces, air conditioners, ground-water heat pumps) increased efficiency of lighting, refrigerators, computers, other appliances Reducing E/GDP: Industry: Reducing E/GDP: Industry Industrial energy use ≈ 40% of global CO2 from fossil-fuel combustion. Biggest users include oil refining, plastics, fertilizers, iron & steel, aluminum, cement, pulp & paper. Energy used for these purposes can be reduced by… improved efficiency of electric motors & individual industrial processes increased use of on-site combined heat & power (CHP) increased recycling of energy-intensive materials shift in composition of industrial activity from materials-intensive to knowledge- and information-intensive goods & services Slide66: 1.2 1.1 1.0 0.9 0.8 0.7 0.6 0.5 0.4 Carbon Intensity of World Primary Energy, 1900-2050 Carbon Intensity (tC/toe) Source: National Academy of Engineering, 1997 1900 1920 1940 1960 1980 2000 Carbon Intensity of: Wood = 1.25 Coal = 1.08 Oil = 0.84 Gas = 0.64 2020 2040 2050 C/E: History and BAU projections C/E: Will running out of fossil fuel take care of it?: C/E: Will running out of fossil fuel take care of it? Combustion of conventional fossil fuels yields about 15 million tonnes C in CO2 per EJ of natural gas 20 million tonnes C in CO2 per EJ of petroleum 25 million tonnes C in CO2 per EJ of coal 1 tonne of C makes 3.67 tonnes of CO2 Remaining ultimately recoverable resources would yield 200+ billion tonnes of C in CO2 from natural gas 300+ billion tonnes of C in CO2 from petroleum 4,000 billion tonnes of C in CO2 from coal Current C content of the atmosphere (380 ppmv) = 800 billion tonnes C in CO2, an increase of about 215 billion tonnes C since 1750. About half of added CO2 now stays in atmosphere; if this remains so, adding 700 billion more tonnes of C in CO2 will get us to 2X 1750 concentration. There is more than enough conventional fossil fuel to double, even triple & quadruple, the pre-industrial atmospheric concentration of carbon dioxide. Reducing C/E going forward: Reducing C/E going forward HERE THE POSSIBILITIES ARE… Increasing the efficiency of conversion of fossil-fuels to end-use energy forms (most importantly electricity) Potential is limited because conversion efficiencies are constrained by thermodynamics and already high. Switching from high C/E to low C/E fossil fuels (coal to oil & natural gas, oil to natural gas) Potential is limited because oil & gas are much less abundant than coal (unless unconventional gas resources become practical) CO2 capture & sequestration (CCS) when fossil-fuels are converted or burned Switching from fossil to non-fossil primary energy sources (renewables & geothermal, nuclear) What’s a suitable target for CO2 reductions?: What’s a suitable target for CO2 reductions? The climate-policy aim negotiated in the process of formulating the UN Framework Convention on Climate Change was… “stabilization of greenhouse gas concentrations in the atmosphere at a level that would prevent dangerous anthropogenic interference with the climate system”. There was no formal consensus at that time about what level is “dangerous” in this sense. Suitable CO2 target? (continued): Suitable CO2 target? (continued) There is still no formal consensus. But it’s increasingly clear that the current level of anthropogenic interference is dangerous: Significant impacts in terms of floods, droughts, wildfires, species, melting ice already evident at ~0.8°C above pre-industrial Tavg. Current GHG concentrations commit us to ~0.6°C more. Suitable CO2 target? (continued): Suitable CO2 target? (continued) It is now entirely plausible that… ∆Tavg ~ 1.5°C will mean the end of coral reefs & polar bears ∆Tavg ~ 2°C will mean catastrophic melting of Greenland & Antarctic ice, with commitment to multi-meter rises in sea level ∆Tavg ~ 2.5°C will sharply reduce global crop yields Thus stopping at 2x pre-industrial CO2 (550 ppmv, corresponding to ~3°C), once thought a reason-able target by many) may not be good enough. Many analysts & groups now conclude that prudence requires aiming not to exceed 2°C. Slide72: The path to avoid ∆Tavg >2°C (gold) requires much earlier, more drastic action than path to avoid >3°C (green). BAU ( 6°C+) (~3°C) (~2°C) Future BAU emissions path compared to paths for stabilizing CO2 concentration to limit ∆Taverage Thought experiment: How much carbon-free energy needed to stabilize CO2 at 550 ppmv?: Thought experiment: How much carbon-free energy needed to stabilize CO2 at 550 ppmv? Carbon-free energy in 2000 (from renewables and nuclear energy) ≈ 100 exajoules/year. (Fossil fuels ≈ 350 EJ/yr) With BAU economic growth, the future need for C-free energy (renewables, nuclear, & advanced fossil with CO2 sequestration) depends on rate of improvement of energy efficiency as follows: C-free energy (exajoules) in 2050 2100 ------ ------- E/GDP falls 1%/yr (BAU) 600 1500 E/GDP falls 1.5%/yr 350 800 E/GCP falls 2.0%/yr 180 350 Stabilizing at 450-500 ppmv would be possible if emissions were flat for ~50 years, then declined. : 0 Historical emissions Reduced carbon intensity of the baseline economy Emissions proportional to economic growth 2055 2005 1955 14 7 1.9 28 21 Currently projected path Stabilization Triangle Flat path Virtual Triangle GtC/yr Stabilizing at 450-500 ppmv would be possible if emissions were flat for ~50 years, then declined. The virtual triangle results more from structural shifts in the economy (toward services) and less from the carbon-saving activity required to fill the stabilization triangle. The green “stabilization triangle” represents the emissions that should & could be avoided by new policies (a depiction due to Socolow & Pacala). Slide75: Energy Efficiency Decarbonized Electricity Fuel Displacement by Low-Carbon Electricity Forests & Soils Decarbonized Fuels Stabilization Triangle 2004 2054 7 GtC/y 14 GtC/y The triangle can be filled by a portfolio of 7 wedges Methane Management Each wedge accounts for 1 GtC/yr in 2055 2005 2005 This particular set of wedges is only illustra-tive, not prescriptive. 2055 Slide76: There are more than 7 wedges to choose from: Here are 15 candidates. Policy options for promoting mitigation: Policy options for promoting mitigation Measures to affect choices among available technologies analysis of and education about the options correction of perverse incentives lowering bureaucratic barriers financing for targeted options performance & portfolio standards subsidies for targeted options emission cap & trade programs taxes on carbon or energy Measures to improve mix of available technologies improving capabilities for RD&D encouraging RD&D with tax policy & other policies funding the conduct of RD&D promoting niche & pre-commercial deployment international transfer of resulting technologies These are listed in order of increasing intrusiveness & political difficulty. But combinations that don’t include one of the last two are almost certain to be insufficient. Policy options embraced to date: Policy options embraced to date The Kyoto Protocol a landmark as a negotiated global commitment to move forward to address the problem but limited in time frame, magnitude of required reductions, and participation The EU carbon trading system implemented starting in January 2005, embracing 12,000 installations accounting for almost half of EU carbon emissions C trading price reached $100/tC, but has recently fallen amid loss of confidence about monitoring, cheating Non-federal jurisdictions in the United States USA has not ratified Kyoto; federal climate policy consists only of research, incentives, and modest “voluntary” targets. But 28 states have climate-action plans, 21 have renewable portfolio standards, 234 cities have embraced Kyoto targets, many major corporations are acting. US Senate endorsed mandatory, national GHG restraints in 6/05. Corporate Commitments and Results: Corporate Commitments and Results 10% reduction 10% reduction $650 million saved 69% reduction $2 billion saved 65% reduction $791 million saved 25% reduction 9% reduction 6% reduction 10% reduction “It’s made us more competitive” 25% reduction $100 million saved 13% reduction Absolute cap 35% reduction $200 million saved 19% reduction 37% reduction 17% reduction 5% reduction 72% reduction 1% reduction $1.5 billion clean tech R&D Sense of the Senate Resolution, 6-22-05: Sense of the Senate Resolution, 6-22-05 It is the sense of the Senate that Congress should enact a comprehensive and effective national program of mandatory, market-based limits and incentives on emissions of green-house gases that slow, stop, and reverse the growth of such emissions at a rate and in a manner that-- (1) will not significantly harm the United States economy; and (2) will encourage comparable action by other nations that are major trading partners and key contributors to global emissions. Policy recommendations (my own): Policy recommendations (my own) Pursue a new global framework for mitigation and adaptation in the post-Kyoto period It must include mandatory, economy-wide reductions in GHG emissions below BAU everywhere, and it needs to be equitable, achievable, and adequate to the magnitude of the challenge. Pursue “win-win” technical and policy measures Pursue most vigorously those measures that address economic, social, and non-climate environmental goals as well as climate. Increase investments in energy-technology innovation A tripling to quadrupling of government investments is warranted worldwide, along with increased incentives for innovation in the private sector. Expand international cooperation on energy-technology innovation Cooperation is needed to reduce costs & spread benefits in implementing climate-friendly technologies in the interest of the whole world. A few references…: A few references… Intergovernmental Panel on Climate Change, Climate Change 2001: Synthesis Report – Summary for Policymakers, IPCC, 2001 http://www.ipcc.ch/pub/un/syreng/spm.pdf National Academy of Sciences, Climate Change Science: An Analysis of Some Key Questions, National Academy Press, 2001 http://books.nap.edu/html/climatechange/climatechange.pdf U.S. Global Change Research Program, Climate Change Impacts on the United States, USGCRP, 2001 http://www.usgcrp.gov/usgcrp/Library/nationalassessment/ National Commission on Energy Policy, Ending the Energy Stalemate: A Bipartisan Strategy to Meet America’s Energy Challenges, December 2004 http:www.energycommission.org International Climate Change Taskforce, Meeting the Climate Challenge, January 2005. http://www.tai.org.au/Publications_Files/Papers&Sub_Files/Meeting%20the%20Climate%20Challenge%20FV.pdf The Arctic Council, Arctic Climate Impact Assessment, Arctic Council, 2005. http://www.acia.uaf.edu James Hansen, “A slippery slope”, Climatic Change, vol. 68, February 2005, pp 269-279.