The Copenhagen Diagnosis

O.K. First some gallows humor, a re-telling of an old medico joke.

Scientists have some good news and some bad news.

“I could listen to some good news. What is it?”

It is the End of Life on the Planet as we know it.

“That’s the good news. So what could be the bad news?”

We have been telling you that for 15 years.

Now on to a re-post of “Copenhagen Diagnosis Released, Detailing Accelerating Indicators of Climate Change In Last Three Years” that Jack Rosebro originally posted to Green Car Congress, 25 November 2009.

Note: The images and captions are from the post, the Easter eggs and their snarky captions are compliments of After Gutenberg. Zemanta added some links.

A team of 26 climate scientists from Australia, Austria, Canada, France, Germany, Switzerland, the United Kingdom, and the United States have published the “Copenhagen Diagnosis”, an interim synthesis report on developments in climate change science from mid-2006 to the present day. The report points out that many key harbingers of climate change “are occurring at the high end or even beyond the expectations of only a few years ago.””

Although the report is not an official Intergovernmental Panel on Climate Change (IPCC) document, many of its authors have served as lead authors of IPCC Assessment Reports in the past, and most of them have authored or co-authored seminal papers on climate change.

The rationale [for the report] is two-fold,” the authors explain. “First, this report serves as an interim evaluation of the evolving science midway through an IPCC cycle: IPCC’s AR5 (Fifth Assessment Report) is not due for completion until 2013.” The most recent peer-reviewed papers evaluated by the authors of the Fourth Assessment Report (AR4) were published in mid-2006. Work published after then will be evaluated by the IPCC during the AR5 authoring cycle, which is just getting underway.

Second, and most important, the report serves as a handbook of science updates that supplements the IPCC AR4 in time for Copenhagen in December 2009, and any national or international climate change policy negotiations that follow.” In this sense, the report models itself on the efforts of Working Group 1 in the IPCC’s Assessment Reports, presenting no new data on climate change, but instead gathering and synthesizing existing scientific literature, and noting trends that have been confirmed by multiple sources.

Recent and significant climate change findings cited in Copenhagen Diagnosis include: [emissions, surface temperatures, atmospheric changes, cryospheric changes, oceanic changes, tipping points.]

Fossil Fuel Emissions Over Time
“Global carbon dioxide emissions from fossil fuel combustion, 1980-2010, as compared to baseline scenarios used by the IPCC to project business as usual emissions.”

Emissions. Global carbon dioxide emissions from fossil fuels in 2008 were nearly 40% higher in 2008 than in 1990. This is roughly equal to the most severe emissions scenario yet considered by the IPCC, even though that scenario (A1, Fossil Intensive) was originally calculated as a reference baseline, absent any efforts towards emission reduction such as the Kyoto Protocol.

Concurrent with increased greenhouse gas (GHG) levels—now deemed higher than at any point in time in the last 800,000 years—the ability of natural oceanic and terrestrial carbon sinks to absorb CO2 from the Earth’s atmosphere appears to be deteriorating, having likely decreased by at least 5% in the past half century, although inter-annual variability is large.

The degradation of natural carbon sinks amplifies the effects of climate change, producing the same net effect on atmospheric concentrations of GHGs as increases in greenhouse gas emissions. Some specific carbon sinks, such as the Southern Ocean, appear to be slowing their carbon uptake much more rapidly than the global average, and some natural GHG sinks may be undergoing processes which will transform them into carbon emitters.

Following a decade of relative stability, for example, the atmospheric concentration of methane (CH4), a potent greenhouse gas, began to rise inexplicably in 2007. Although deteriorating permafrost has been observed in Russia, Sweden, and Tibet, the precise source of the increase has not yet been identified.

As permafrost melts and the depth of its active layer deepens, organic material begins to decay. If the surface is covered with water, methane-producing bacteria break down the organic matter. Such bacteria cannot, however, survive in the presence of oxygen; if thawed soils are exposed to air, carbon dioxide-producing bacteria participate in the decay process. Both events amplify the effects of warming temperatures by releasing greenhouse gases. The likely magnitude of such a positive feedback, which is considered to be a potential tipping element, is unknown.

It is now estimated that if global emission rates could immediately be stabilized at present-day levels, just twenty more years of business-as-usual emissions would give a 25% probability of warming exceeding 2 °C above pre-industrial levels, even if society could achieve zero emissions after 2030.

To stabilize climate, a decarbonized global society-with near-zero emissions of CO2 and other long-lived greenhouse gases-would now have to be reached well within this century in any case. Many of the most up-to-date emissions reduction scenarios require a decline to zero carbon or carbon negative levels by 2050 to limit warming to no more than 2 ºC.

Trend Analysis of Rising Global Surface Temperatures
Source: NASA’s Goddard Institute for Space Science (GISS)

Annual variability and averaged linear trend of global surface temperatures, 1980-2008.

Surface temperatures. Recent global temperatures demonstrate human-induced warming: temperatures have increased at a rate of 0.19 °C per decade for the past quarter century, in close alignment with modeled predictions based on projected greenhouse gas increases. In addition to a warming limit of 2 ºC, many scientists consider an increase of 0.20 ºC per decade to be a “rate of warming” limit beyond which many ecosystems will experience a reduced ability to adapt.

Although natural, short-term fluctuations are occurring as expected—for example, temperatures were higher in 1998, the record year for temperatures so far, than in 2008—“there is no indication in the data of a slowdown or pause in the human-caused climatic warming trend” that underlies annual or decadal variability.

For example, a La Niña climate pattern was active in 2008. Such a pattern can normally can be expected to reduce average global surface temperatures. At the same time, solar output was at its lowest level of the satellite era, which would normally be expected to create another temporary cooling influence. Absent any anthropogenic warming, these two factors would typically be expected to make 2008 temperatures among the coolest since record-keeping began. However, 2008 was the ninth warmest year on record. “This underpins the strong greenhouse warming that has occurred in the atmosphere over the past century,” write the authors.

Global Temperature Change, Human and Solar Influences
Anthropogenic and solar variability influences on global temperature changes, 1980-2009, and (projected) 2009-2030.

Atmosphere. Worldwide air temperature, humidity and rainfall trend patterns now “exhibit a distinct fingerprint that cannot be explained by phenomena apart from increased atmospheric greenhouse gas concentrations”. Atmospheric temperatures have maintained a strong warming trend since the 1970s (~0.6 °C), consistent with expectations of greenhouse induced warming. Each year of the present decade—2001 through 2008—has been among the top ten warmest years since instrumental records began.

“The 2007 IPCC Assessment… states clearly that without substantial global reductions of greenhouse gas emissions we can likely expect a world of increasing droughts, floods and species loss, of rising seas and displaced human populations. However, even since the 2007 IPCC Assessment the evidence for dangerous, long-term and potentially irreversible climate change has strengthened.”

—Met Office, UK, 24 November 2009

This week, the UK’s Met (Meteorological) Office projected that unless an exceptionally cold spell occurs within the next month, global 2009 temperatures will be higher than 2008, making 2009 one of the five warmest years since records began around 150 years ago. 2010 will bring with it the influence of El Niño ocean currents, and the Met office estimates a 50% chance that next year will see record average global temperatures.

Arctic sea-ice area, Modeled vs. Observed
“Mean modeled Arctic sea-ice area, range of modeled Arctic sea-ice, and observed Arctic sea-ice area, in millions of square kilometers”

Cryosphere. A wide array of satellite-based as well as direct ice measurements “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”; and the contribution of the cryosphere—the portions of the Earth’s surface where water is frozen’to global sea-level has increased from 0.8 millimeters per year in the 1990s to 1.2 millimeters per year today. Many non-polar glaciers are critical sources of drinking water and hydropower.

In particular, summer-time melting of Arctic sea-ice has accelerated in a manner that no climate model had predicted, with the area of sea-ice melt during 2007, 2008, and 2009 was about 40% greater than the average prediction from IPCC AR4 climate models.

Ice shelves, which connect continental ice sheets to the ocean, are also in flux, with the Antarctic Peninsula seeing 7 major collapses over the past 20 years. Shelf weakening has also been observed in the Bellingshausen and Amundsen seas, indicating a more widespread influence of atmospheric and oceanic warming than previously thought. The collapse of ice shelves often contributes to an accelerated destabilization of ice sheets to which the ice shelves were once attached.

Oceans. Upwards of 80% of the warming created by the emission of manmade greenhouse gases are now stored in the world’s oceans. Satellite data shows recent global average sea level rise (3.4 mm per year over the past 15 years) to be approximately 80% higher than past IPCC predictions. This acceleration is consistent with a doubling in contribution from melting of glaciers, ice caps, and the Greenland and West Antarctic ice sheets.

By 2100, global sea level is likely to rise at least twice as much as the Working Group 1 of the IPCC AR4 had projected just two years ago. If emissions continue to rise unabated, sea level rise may well exceed 1 meter, with an estimated upper limit of around 2 meters sea level rise, by 2100. The relative inertia of oceanic mass ensures that sea levels will continue to rise worldwide for centuries after global temperatures have been stabilized. Several meters of sea level rise must be expected over the next few centuries, regardless of any emissions reductions that may occur during that time.

Ocean acidification and de-oxygenation, both of which are amplified by warming, are also contributing to a decline in the ability of large swaths of the oceans to support marine life. The increase in heat content of the upper ocean between 1963 and 2003 is estimated to be approximately 50% higher than previously estimated, a calculation that is consistent with observed sea level rise during the same period of time.

Resilience. Recent studies suggest that the disruptive effects of climate change may be greater than anticipated at just 2 ºC of warming, and one aspect of climate change that has been particularly difficult to estimate is the ability of a given ecosystem to recover from, or adapt to, a given change in equilibrium.

More than a dozen vulnerable tipping elements in the climate system (e.g. continental ice-sheets, Amazon rainforest, West African monsoon, thermohaline ocean circulation cycle) could be pushed towards abrupt and/or irreversible change if warming continues along a business-as-usual trajectory throughout this century. Here, the authors invoke the precautionary principle: waiting for higher levels of scientific certainty could mean that “some tipping points will be crossed before they are recognized.”

At a press conference announcing the release of the report, co-author Richard Somerville of the Scripps Institution of Oceanography in La Jolla, California acknowledged the difficulty of reconciling scientifically documented trends with political goals and media chatter:

There’s an urgency to this that is not political or ideological, but scientific. There are, for example, no liberal or conservative theories of, for example, ocean circulation. There is simply a theory of ocean circulation… A Galileo comes along one every hundred years or so [to successfully challenge science], but most people who think they are Galileo are wrong.

—Richard Somerville

GCC Resources

  • I. Allison, N. L. Bindoff, R.A. Bindoff, R.A. Bindschadler, P.M. Cox, N. de Noblet, M.H. England, J.E. Francis, N. Gruber, A.M. Haywood, D.J. Karoly, G. Kaser, C. Le Quéré, T.M. Lenton, M.E. Mann, B.I. McNeil, A.J. Pitman, S. Rahmstorf, E. Rignot, H.J. Schellnhuber, S.H. Schneider, S.C. Sherwood, R.C.J. Somerville, K.Steffen, E.J. Steig, M. Visbeck, and A.J. Weaver: The Copenhagen Diagnosis, 2009: Updating The World On The Latest Climate Science. 24 November 2009: The University of New South Wales Climate Change Research Centre (CCRC), Sydney

  • Met Office: Climate Science Statement, 24 November 2009

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7 Comments

  1. jcwinnie
    Posted 2009-11-27 at 10:17 am | Permalink

    Although the main point is the same, i.e., You know that really, really bad news? Well, it wasn’t as bad as it really is., still Ben Jervey provides a somewhat different read of the report.

    montage
    26 climate scientists deliver the really bad news.

    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 2oC. Even with zero emissions after 2030. Every year of delayed action increase the chances of exceeding 2oC 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 2oC 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.

  2. jcwinnie
    Posted 2009-11-28 at 11:18 am | Permalink

    The oceans play a key role in regulating climate, absorbing more than a quarter of the carbon dioxide that humans put into the air. Now, the first year-by-year accounting of this mechanism during the industrial era suggests the oceans are struggling to keep up with rising emissions — a finding with potentially wide implications for future climate.

    Oceans’ uptake of man-made carbon may be slowing

  3. jcwinnie
    Posted 2009-11-30 at 6:41 pm | Permalink

    “It is almost certainly the case,” says Joe, “that the planet has warmed up more this decade than NASA says, and especially more than the UK’s Hadley Center says.” Professor Romm and other climate scientists are most concerned about the Arctic Ocean, since it is “the place on Earth that has been warming fastest.”

    Recent Climate Progress articles on the topic:

  4. jcwinnie
    Posted 2009-12-13 at 9:23 am | Permalink

    In June, dozens of Academies of Science, including ours and China’s, issued a joint statement on ocean acidification, warned “Marine food supplies are likely to be reduced with significant implications for food production and security in regions dependent on fish protein, and human health and wellbeing” and “Ocean acidification is irreversible on timescales of at least tens of thousands of years.” They conclude:

    Ocean acidification is a direct consequence of increasing atmospheric CO2 concentrations. To avoid substantial damage to ocean ecosystems, deep and rapid reductions of global CO2 emissions by at least 50% by 2050, and much more thereafter are needed.

    We, the academies of science working through the InterAcademy Panel on International Issues (IAP), call on world leaders to:

    • Acknowledge that ocean acidification is a direct and real consequence of increasing atmospheric CO2 concentrations, is already having an effect at current concentrations, and is likely to cause grave harm to important marine ecosystems as CO2 concentrations reach 450 ppm and above;

    • Recognise that reducing the build up of CO2 in the atmosphere is the only practicable solution to mitigating ocean acidification;

    • Within the context of the UNFCCC negotiations in the run up to Copenhagen 2009, recognise the direct threats posed by increasing atmospheric CO2 emissions to the oceans and therefore society, and take action to mitigate this threat;

    • Implement action to reduce global CO2 emissions by at least 50% of 1990 levels by 2050 and continue to reduce them thereafter.

    If we want to save life in the oceans — and save ourselves, since we depend on that life — the time to start slashing carbon dioxide emissions is now.

    For a recent story on ocean acidification, see “New climate change signal: oceans turning acidic.”

    The Sounds of Science

  5. jcwinnie
    Posted 2009-12-14 at 9:39 am | Permalink

    HuffPo contributor Wendy Gordon interrupts her day dream of a tropical vacation to remind us that rising CO2 levels means “a less hospitable environment for many forms of sea life.”

    Learn more by watching Acid Test: The Movie.

    P.S. “And if you are planning a seaside vacation, you can help protect coral reefs by avoiding use of sun tan lotions that harm reefs (those that contain chemical UV barriers such as benzophenone and cinnamate and also parabens). These trigger viral infections in coral that can kill them.”

  6. jcwinnie
    Posted 2009-12-14 at 10:33 am | Permalink

    The Times has learned that negotiators from developed countries are planning to use the idea of a review to justify failing to agree the 25-40 per cent cut in the 1990 level of emissions by 2020, recommended by the IPCC.

    Even the most ambitious provisional offers made by all the countries amount to a reduction of only 18 per cent.

    Tony Blair, the former Prime Minister, said leaders would be unable to deliver a deal in line with what the IPCC had recommended.

    In an interview yesterday with The Times in Copenhagen, he said: “It would be a big mistake if we failed to get an agreement because we didn’t meet the highest expectations people have.

    “Get the agreement, get it under way, and then understand you will inevitably have to change and adjust as you proceed.

    “If you actually manage to cut emissions by 18 per cent by 2020, you would have made a very, very big change in the way economies work,” he said, before adding: “Don’t let the best be the enemy of the good.”

    A joint report by Mr Blair’s office and the Climate Group, an environmental body backed by some of the world’s biggest companies, including BP, HSBC and Google, said that, even if all the provisional offers were delivered, emissions of CO2 in 2020 would still be 5 billion tonnes higher than the atmosphere could safely accommodate.

    This would mean that global temperature would rise more than 2C above pre-industrial levels, with the result that large parts of the world would become uninhabitable.

    The joint report, published yesterday, proposed a review of targets in 2015 to allow “scaling up of ambition”.

    Countries are unlikely to improve on their provisional offers over the next five days, because the US has made clear it will not be raising its own relatively weak provisional target for cutting emissions.

    President Obama has offered to cut US emissions by 4 per cent on 1990 levels by 2020, subject to approval by the US Congress. The EU has committed to a 20 per cent cut over the same time scale, but said it would raise this to 30 per cent if other countries made comparable efforts.

    Mr Blair discussed Mr Obama’s offer last week with Todd Stern, the US chief climate negotiator, and agreed that the focus should be on accelerating US emissions cuts in the decade after 2020 rather than before.

    Mr Blair said that, while the scientific evidence of man-made global warming was very strong, it was much less clear how quickly temperatures would rise.

    “When you come to very precise dates, percentages and so on [. . .] then the figures are somewhat more fudgeable.

    “The important thing is to give a clear direction out of this conference. Don’t fixate on the precise percentage,” he said.

    A source close to Britain’s negotiating team said Britain would continue to press publicly for a deal in line with the IPCC’s recommendation, but acknowledged that the targets emerging from the summit would need to be reconsidered at a later date.

    Bernarditas Muller, lead negotiator for the G77 and China group of developing countries, said putting off the most difficult decisions on emissions cuts would be a betrayal of commitments made by rich countries under the UN Climate Convention.

    “Developing countries have the most to lose if we do not agree a just and ambitious outcome in Copenhagen. We are simply asking developed countries, ‘Don’t shirk your responsibilities. Just do what you have already agreed to do under the Climate Convention’.”

    Smaller developing countries were excluded yesterday from a meeting in Copenhagen of environment ministers from about 40 countries.

    Ed Miliband, the Energy and Climate Change Secretary, said after the meeting: “We’re now getting close to midnight in this negotiation and we need to act like it.

    “That means more urgency to solve problems, not just identify them, more willingness to shift from entrenched positions and more ambitious commitments.”

    The Prince of Wales will address the summit tomorrow and Gordon Brown will meet other leaders in Copenhagen on Wednesday.

    About 120 Prime Ministers and Presidents will attend the final day of the summit on Friday.

    Copenhagen stalls decision on catastrophic climate change for six years

  7. jcwinnie
    Posted 2009-12-15 at 6:03 pm | Permalink

    Writing for Reuters, Sunanda Creagh tells us that it is bad news for the clownfish, of Finding Nemo fame. “Nemo is more lost than ever, thanks to climate change.”

    Ocean acidification caused by global warming is destroying the sense of smell and navigational abilities of the little orange clownfish of Finding Nemo fame, pushing the species closer to extinction, a new report has found.

    The report, launched on Monday by the International Union for Conservation of Nature on the sidelines of global climate talks in Copenhagen, named 10 species that will be hardest hit by global warming.

    Among the 10 was the clownfish, which uses its sense of smell to find its way to its host anemone.

    “Ocean acidification and rising temperatures are of course destroying the coral reefs but, on top of that, they are affecting their olfactory senses,” the report’s co-author, Wendy Foden told reporters.

    “They are literally unable to find their way home.”

    The 10 species named in the report were: beluga whale, clownfish, leatherback turtle, emperor penguin, quiver tree, ringed seal, salmon, staghorn coral, arctic fox and koala.

    Higher temperatures cause more of the eggs laid by giant leatherback turtles to develop as females, Foden said.

    “It’s leading to extremely skewed sex ratios developing,” she said.

    Koalas are finding it harder than ever to get enough to eat because warmer conditions have made their staple, eucalyptus leaves, less nutritious, she said.

    “Species can adapt but the conditions need to change sufficiently slowly,” said Foden. “If our governments commit to strong and timely targets, if this meeting is successful here, we can slow the pace of climate change and give these species a chance to survive.”

    The full report can be found at http://cmsdata.iucn.org/downloads/species_and_climate_change.pdf

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