Call for Resources: Teaching Climate Law

I administer the Climate Law Teaching Resources site for the IUCN’s Academy of Environmental Law: http://www.iucnael.org/en/online-resources/climate-law-teaching-resources. The site includes syllabi and climate negotiation simulations for use in the classroom.

If you have pertinent materials you are willing to share with the teaching community, please send them to me and I will have them posed promptly on the site. Thanks, wil

Climate Change: The Long-Term View

nclimate2923-f2In a new study published in the journal Nature Climate Change, Clark, et al. suggest that our policy orientation in terms of mitigation and adaptation responses to climate change should be expanded to assess the past 20,000 years and the next 10,000 years, well beyond the IPCC’s focus on the 21st and 22nd Century. The authors contend that this temporal horizon, “on a geological timescale,” provides a more realistic assessment of the ultimate impacts of anthropogenic emissions, as well as the compelling need to substantially accelerate our commitment to reducing emissions.

The study utilized several different scenarios for temperatures and sea-level change over the course of 10,000 years, as well as referencing of our best understanding of climate change over the past 20,00 years. The study’s projections are based on a suite of four future emissions scenarios with carbon releases between 1,280 and 5,120 PgC, with current the current cumulative human carbon emissions already approaching the low-end scenario.

The researchers argue that projections of climatic change over the next 10,000 years is justified by the inertia of the climatic system. As a consequence, “60-70% of the maximum surface temperature anomaly and nearly 100% of the sea-level rise from any given emission scenario remains after 10,000 years, and that the ultimate return to pre-industrial CO2 concentrations will not occur for hundreds of thousands of years.”

Among the conclusions of the study:

  • Projected temperature increases of 2.0-7.5°C over the course of this century will exceed those during even the warmest levels reached in the Holocene, “producing a climate state not previously experienced by human civilizations.” Moreover, temperatures will remain elevated above Holocene levels for more than 10,000 years;
  • Even the lowest emissions scenario in the study, 1,280 PgC, results in sea level rise associated with the Greenland ice sheet of 4 meters over 10,000 years. Higher scenarios result in an ice-free Greenland over the course of 2500-6000 years, which could result in approximately 7 meters of sea level rise;
  • The lowest emissions scenario yields as much as 24 meters of global mean sea level rise over 10,000 years associated with melting of Antarctic ice sheets;
  • An equilibrium climate sensitivity of 3.5°C, consistent with IPCC AR5 scenarios, could yield sea level rise of 25-52 meters within the next 10,000 years, reaching 2-4 meters per century, “values that are unprecedented in more than 8,000 years.
  • The only method to avoid a further commitment to sea level rise above the current projections of 1.7 meters “is to achieve net-zero emissions;”
    • There are 122 countries with at least 10% of current population weighted area that will be directly affected by coastal submergence and 25 coastal megacities will have at least 50% of their population-weighted area impacted
  • The authors draw several policy implications from this long-term assessment of climatic impacts:
    • On millennial timescales, the use of conventional discounting approaches ensure that “future climate impacts … would be valued at zero, irrespective of the levels of certainty and magnitude.” This poses profound questions in terms of considerations of intergenerational equity and our obligations to future generations;
    • There is a compelling need for global energy policies that result in net-zero or net-negative carbon dioxide emissions; “a marginal reduction in emissions is insufficient to prevent future damages.” Such technologies would need to be kept in place for tens of thousands of years “without fail.” It also suggests radical changes in terms of financial incentives, a need to accelerate research and development of technologies to transform energy systems and infrastructure, and a focus on global equity considerations.”

 

Among the class discussion questions that might be posed are the following:

 

  1. Is it pertinent for us to consider the potential impacts of climate change on a timescale of 10,000 years? Does it make more sense to formulate policies to protect the current and immediate successor generations?
  2. If, as the article suggests, the current rate of discounting future losses is inappropriate for climatic impacts, what alternative system should we employ?
  3. What are the most viable “negative emissions” technologies that might be available, and are there any risks in their utilization that should be weighed against their benefits of reducing atmospheric concentrations of carbon dioxide?

NOAA Annual Greenhouse Gas Index

aggi_2008_medThe U.S. National Oceanic & Atmospheric Administration publishes an Annual Greenhouse Gas Index (AGGI), “a measure of the warming influence of long-lived trace gases and how that influence is changing each year.” Thus, AGGI is an index that measures climate forcing associated with long-lived greenhouse gases. The Index would be an excellent resource for instructors who involve their students in climate negotiations exercises, as well as a potent reminder of how the promise of Paris is confronted by the practical reality of trends in radiative forcing and atmospheric concentrations of greenhouse gases.

Among the findings of the latest assessment:

  1. Carbon dioxide concentrations creased by an average of 1.76 ppm per year from 1979-2015. However, the trend has accelerated in recent years, averaging about 1.5 ppm per year in the 1980s and 1990s, 2.0 ppm per year during the last decade. Moreover, atmospheric carbon dioxide increased 3 ppm in the past year, for only the second time since 1979.
    1. Increases in carbon dioxide concentrations in the atmosphere has resulted in a whopping 50% increase in its direct warming influence on climate since 1990
  2. While methane concentrations remained constant in the atmosphere from  1999-2006 (after declining from 1983-1999), they have been increasing since 2007, due to factors such as increasing temperatures in the Arctic in 2007, increased precipitation in the tropics in 2007 and 2007; this trend accelerated between 2014-2015. Nitrous oxides concentrations have also accelerated in recent years.
  3. Radiative forcing from chloroflourocabons is in decline, primarily due to the Montreal Protocol on Substances that Deplete the Ozone Layer. The importance of this regime, designed to address threats to the ozone layer, in terms of climate change are clear: without the treaty, climate forcing would have been 0.3 watt m-2 greater, or approximately half of the increase in radiative forcing attributable to carbon dioxide since 1990;
  4. Radiative forcing of long-lived, well-mixed greenhouse gases increased 37% from 1990 (the Kyoto baseline year)  to 2015, with carbon dioxide accounting for nearly 80% of this increase;
  5. Increases in greenhouse gas concentrations over the past 60 years have accounted for approximately 75% of the total increase in the Index in the past 260 years.

Among the questions for class discussion that this study’s findings might generate are:

  • What impacts might purported fugitive methane releases associated with fracking be having on concentrations of atmospheric methane?
  • What might the implications be of positive feedback mechanisms that might release substantial amounts of methane from ocean-based methane clathrates?
  • Why are concentrations of carbon dioxide accelerating in recent years despite efforts at the national and international level to arrest greenhouse gas emissions?

Biofuels and Food Production

biofuelsMost of the scenarios in the IPCC’s Fifth Assessment Report that set out pathways to avoid temperature increases above 2C rely on large-scale use of so-called “negative emissions technologies,” with the lion’s share coming from the use of Bioenergy and Carbon Capture and Sequestration (BECCS) options. However, there is increasing concern that BECCS could have serious negative ramifications for food security for some of the world’s most vulnerable populations. A recent study by Tim Searchinger et al., analyzing results from a suite of models assessing changes in land use, crop production and food consumption associated with the production of biofuels, suggests that these concerns are valid, and may have serious ramifications for the use of BECCS in the future.

Among the findings of the study were the following:

  1. Approximately 25-50% of net calories associated with diversion of corn or wheat to ethanol are not replaced through planting of other crops, but rather is taken out of food and feed consumption. Failure to replace crops reduces greenhouse gas emissions from land use change and direct emissions of carbon dioxide by people and livestock;
  2. Most analysis of the greenhouse gas emissions implications of biofuel production assume that the emissions associated with fermenting and burning ethanol is offset by carbon absorption by growth of crops diverted to ethanol production. However, this accounting methodology is faulty, because carbon absorbed by crops that would be grown anyway doesn’t constitute a valid offset, because it’s not linked to biofuel production and is not additional.
    1. The only valid form of crop growth offsets would be either from growth of additional crops to replace those diverted to biofuels production, or increases on crop yields on existing croplands;
    2. Moreover, converting forests or grasslands to produce additional food crops would also release carbon, “reducing or negating the net offset from producing more crops;”
  3. One study suggests that approximately 20% of calories diverted by biofuel production are not replaced. “Food reductions result not from a tailored tax on overconsumption or high-carbon foods but from broad global increases in crop prices.”

Among the class discussion questions that might be pertinent to this article are the following:

  • What would the food implications be of a large-scale commitment to BECCS?
  • What are the prospects to avoid food security issues outlined in this study by techniques such as increasing crop yields or using alternative bioenergy feedstocks, such as algae or cellulosic sources?;
  • If trade-offs are indeed inevitable in terms of food production and greenhouse gas emissions, how should the world community make decisions under such conditions?

Addressing “Loss and Damage” Under the Paris Agreement

I have recently published an online commentary on Article 8 of the Paris Agreement on The Conversation site, which addresses the issue of “loss and damage.” I think that loss and damage is an excellent issue to discuss with students because untitledit provides a device to discuss many “meta issues,” including the potential role of State responsibility and liability for climate damages, the role of climate justice, and the effectiveness of risk-pooling mechanisms, such as insurance.

Incidentally, The Conversation site has a lot of interesting energy and climate commentary by academics. Because it’s designed to be accessible to wider audiences, much of the content might be particularly appropriate for undergraduate students.

Updated Compendium on the Paris Agreement

untitledThis site’s Compendium on the Paris Agreement, which seeks to bring together key online resources on the agreement, has been expanded recently to more than 130 links. The Compendium is available at: http://teachingclimatelaw.org/wp-admin/post.php?post=2993&action=edit

Any suggestions for additional resources are greatly appreciated, and can be submitted to the Compendium’s creator, Wil Burns, at: jiwlp@berkeley.edu.

“Tough Love” on the Path to 2C?

In a new article (subscription only, but link here will take you to a pre-edited version on Professor Anderson’s home page) published in the journal Nature Geoscience, Kevin Anderson of Tyndall Centre for Climate Change Research at the University of Manchester, argues that many of the recent scenarios for limiting temperatures to 2C or below are far too insouciant about the challenges ahead. Anderson contends that such “up-beat — and largely uncontested — headlines . . . are deliveClimate_Feedback_logo_sred through unrealistically early peaks in global emissions, or through the large-scale rollout of speculative technologies intended to remove CO2 from the atmosphere …”

By contrast, Anderson contends that the carbon budgets consistent with a 2C scenario requires “profound and immediate changes to the consumption and production of energy.” Among Anderson’s conclusions:

  1. The IPCC’s 1000 Gt cumulative carbon budget (for having a 66% chance or better of avoiding passing the 2C threshold) requires cessation of all carbon emissions from energy systems by 2050, five decades earlier than projected by the IPCC in its 5th Synthesis Report;
  2. Of 400 IPCC scenarios that have 50% chance or more of keeping temperatures below 2C, a whopping 344 require large-scale deployment of so-called negative emissions technologies (poster’s note: these include technologies such as Direct Air Capture and Bioenergy and Carbon Capture and Sequestration);
  3. Limiting emissions to 1000 GtCO2, with energy production alone chewing up 140 GtCO2 of this budget from 2011 to 2014 alone (overall a fifth of the budget has been emitted in four years), “suggests a profoundly more challenging timeframe and rate of mitigation than that typically asserted by many within the scientific community;”
    1. To avoid exceeding the remaining 650 GtCO2 in the budget would require ratcheting up emissions reduction rates to 10% annually by 2025, continuing this rate to virtual elimination of carbon dioxide by 2050. This would most likely exclude the use of fossil fuels in the post-2050 period, even with deployment of carbon capture and storage, unless its life cycle carbon emissions could be reduced by an order of magnitude;
  4. Given the need to avoid further imperiling the welfare of the global poor, developing countries should need to reduce carbon intensity by approximately 13% annually, higher still for the wealthiest developed countries.

Anderson’s piece could be an excellent reading for a module on long-term responses to climate change and what it will mean to reach the overarching objectives of the Paris Agreement. Among the questions that would be ripe for class discussion:

  1. What would be the policy implications of seeking to meet the more ambitious objective under Paris of limiting temperature increases to 1.5C above pre-industrial levels?;
  2. Anderson portrays negative emissions options as “speculative” or a deus ex machina; do you agree? Assuming that negative technologies can help to remove carbon from the atmosphere, are there any downsides to this approach?;
  3. What are some of the measures that could be taken to effectuate the radical transformation of the world’s economy that could meet the objective of limiting temperatures to 2C?

Likelihood of an Anthropogenic Fingerprint for Record Warming

280_newsPage-280One of the ongoing debates in climate science, and by extension, climate policy making, is the role of anthropogenic greenhouse gas emissions in historically unprecedented increases in temperature over the past few decades. A recent study by Michael Mann, et al. in the journal Scientific Reports seeks to

A New Tool for Teaching the Ultimate Wicked Problem

wicked problem cartoonWicked public policy problems have generated calls for better interdisciplinary collaboration for decades. No one discipline can effectively tackle them. Climate change is perhaps the ultimate wicked problem; the high profile that the COP21 meetings in Paris received will no doubt re-invigorate calls to break down disciplinary silos in the interests of mitigating dangerous climate change. But that won’t make silo-busting any easier; neither academic structures nor the complexity of the problem facilitate it.

But what if browser-based search engines like Google were not the only easy way to dig into climate change? What if we could access the collective knowledge of thousands of experts representing all of the disciplines that form the grist for individual, organizational, and societal climate change decision-making? This would be no mean feat. Anyone thinking seriously about geoengineering, for example, ideally would bring to the conversation an understanding of risk and risk management, economics and cost-benefit analysis, ethics and philosophy, atmospheric sciences and the functioning of complex systems, and societal decision-making and governance.

While no one can be an expert in everything, what if we could easily explore and learn from work being done across all climate-relevant disciplines? What opportunities would this open up for teaching about a problem as wicked as climate change? How much better prepared could law and policy decision-makers be to tackle climate change?

After more than 25 years in the climate change field, in 2010 Laura Kosloff and I began to use specialized TheBrain® software to build a climate knowledge solution with the lofty goal of helping users find “actionable knowledge” to support climate change thinking and decision-making. The open-access Climate Web contains far more information than any individual is likely to ever want to know; there just is no one-size-fits-all “actionable knowledge” when it comes to climate change. While we have only scratched the surface of the Climate Web’s potential, we are encouraged by user feedback including “having the Climate Web available is like having 100 experts in climate science, risk, communications and corporate strategy at the decision-making table with you.” That’s exactly the kind of inter-disciplinary perspective we’re trying to promote. You can see it in action in this recent Climate Web webinar recording.

The Climate Web and Teaching Climate Change

The core idea of TheBrain® software we use in the Climate Web derives from the concept of “mind maps.” Mind maps tap the organizational power of visualizing relationships of information. Their two-dimensional nature limits their capacity, however. TheBrain® software takes such visualization to a new level. It is uniquely suitable to linking together information from the wide range of disciplines relevant to understanding and responding to climate change. The Climate Web incorporates more than 11,000 reports, books, and journal articles. It is home to hundreds of PowerPoint presentations, infographics, and videos. More than 15,000 URLs point to news stories and web pages external to the Climate Web. More items are added practically every day.

The Climate Web curates, organizes, and links climate change information and ideas. With more than 500 topic headings and 750 index terms, the Climate Web pulls together published sources, news stories, multimedia materials, Q&A, discussion points, and commonly voiced arguments. This multi-subject and multi-resource organization facilitates cross-discipline exploration, and offers a knowledge solution that supports individualized learning and interdisciplinary thinking. Instead of presenting a single point of view or advocating a particular policy or technology outcome, the Climate Web curates arguments and ideas from hundreds of experts and thought-leaders across numerous disciplines. It creates a learning environment that encourages users to look at climate change through alternative disciplinary lenses.

A key feature of the Climate Web is that critical visuals, ideas, and other information can be extracted from included sources and then linked throughout the Climate Web. That makes it possible, for example, to collect in one place what dozens of reports might have to say about a specific issue. It also makes it easy for users to find their way to documents and resources of which they are not aware, but that might include “actionable knowledge” they need. Consider this example: Alan Rowson’s 2013 report, A New Agenda on Climate Change, was one of the most insightful pieces of climate analysis that year. But in three years, we have found only four people who had previously heard of the report. In exploring the Climate Web, you will likely find A New Agenda on Climate Change and many other resources that might influence your climate change thinking.

In the bullets below, we briefly lay out how the Climate Web can support efforts to bring more interdisciplinary and individualized learning into the climate classroom.

The Climate Web and Curriculum Development

In developing a climate curriculum, the Climate Web can point you to wide-ranging resources for any climate change topic, as well as to people and organizations working on those topics.The Climate Web makes it possible to put together a more diverse class curriculum than we’re accustomed to seeing. One example is the Climate Web’s exploration of “Big Climate Questions”:

  • Are Climate Risks Much More Immediate Than We Realize?
  • Can We Overcome Communication Barriers to Addressing Climate Change?
  • Is Economic Cost-Benefit Analysis the Right Frame for Inter-Generational Decisions?
  • Will a Low-Carbon Transition Come Too Late to Avoid Dangerous Climate Change?
  • Will a Successful Climate Social Movement Get Organized?
  • Is Business Friend or Foe When it Comes to Addressing Climate Change?
  • Will Adaptation (as Opposed to Mitigation) be Chosen as the Path of Least Resistance?

These may seem like straightforward questions. But they’re not. How policy and business decision-makers think about these questions will direct national and global policy, life-and-death business decisions, and the disposition of trillions of investment dollars. The Climate Web allows students to explore these questions, access differing points of view, and hopefully challenge their own pre-existing assumptions.

The Climate Web and Classroom Discussion

The Climate Web pulls together news stories and other materials for current topics in climate change, encouraging in-depth classroom discussion. Two recent topics are:

The Climate Web and Student Research and Learning

  • The Climate Web organizes topical resources in ways that make it easy for a user to explore. The Climate Engineering Deep Dive, for example—one of more than 50 Climate Web Deep Dives—integrates about 300 resources. But just as importantly, users can easily jump to topics including inter-generational decision-making, risk management, decision-making under uncertainty, climate ethics, and other topics relevant to discussions of climate engineering.
  • While the Climate Web organizes a vast amount of information, it does not seek to provide easy answers. Its structure requires thinking and user involvement. This provides exactly the kind of process that contributes to student learning and knowledge retention.

The Climate Web and Course Support  

  • Course materials can provide hyperlinks into the Climate Web, facilitating student access to exactly the information desired.
  • The Climate Spotlight Tool allows a window into the Climate Web from any website to be customized to the needs of a particular class, pointing to reading and research materials specific to the class.
  • The Climate Web can be used in the classroom to explore topics outside a professor’s specific discipline. The one-day Scenario Planning course built into the Climate Web, for example, can facilitate exploration of climate change risk scenarios; this is a key topic for corporate and policy risk managers.

We undertook to build the Climate Web with the goal of helping users find “actionable knowledge” to support climate change thinking and decision-making. We believe it can help prepare students for the intensely inter-disciplinary nature of the climate change problem. We invite you to explore it for yourself. We have found from experience that the software interface is not immediately intuitive to everyone, but the learning curve is only 10-15 minutes. We have also found that the webinar referenced above (available here with full length Q&A and here in shortened form), is a big help in communicating the structure and functioning of the Climate Web.

We would be interested to hear about your experience with the Climate Web. This will help us as we continue to work with the Climate Web to help tame the wicked problem of climate change.

 

Dr. Mark C. Trexler (mark@climatographer.com)

Laura H. Kosloff, J.D. (laura@climatographer.com)

The Climatographers

503-913-0025

Soil Carbon Sequestration and Biochar Technologies

The recognition that most IPCC scenarios for to avoid exceeding the 2°C “guardrail” require large-scale deployment of negative emissions technologies (NETs) has led to extensive recent discussion of the potential effectiveness and risks associated with a range of option. However, as the authors of a new study published in theBiochar journal Global Change Biology conclude, most studies to date have focused on bioenergy with carbon capture and sequestration (BECCS), direct air capture, enhanced weathering of minerals, and afforestation and reforestation. This study, by Pete Smith at the University of Aberdeen, expands the scope of inquiry to two other NETs options: 1. soil carbon sequestration (SCS), through methods such as alternation of agricultural practices, including no-till or low-till with residue management, organic amendment and fire management; and 2. Biochar, which is production of charcoal as soil amendment via the process of pyrolysis which can, inter alia, sequester carbon. Biochar, at least, is often included under the rubric of “climate geoengineering” options, in the subcategory of carbon dioxide removal (CDR) approaches.

Among the study’s findings:

  1. SCS at global scale could sequester from 0.4-0.7GtCeq. yr-1, with technical potential of 1.37GtCeq. yr-1, at a cost of ~$70-370 per ton of Ceq. Biochar could effectuate sequestration of ~1 GtCeq yr-1, with a maximum potential of 1.8 GtCeq yr-1
  2. By contrast, BECCS might be able to sequester 3.3 GtCeq yr-1 by 2100, and direct air capture a comparable amount. However, the potential of SCS and biochar are higher than either enhanced weathering and comparable to afforestation and deforestation;
  3. About 20% of the mitigation to be derived from SCS could occur at negative cost, and 80% between $0-40 tCeq. Biochar costs range from -$581-1560 billion;
  4. In terms of water requirements, SCS and biochar are virtually zero, while direct air capture has medium to high water demands, and BECCS creating “a very large water footprint;”
  5. In terms of energy requirements, SCS has a negligible energy impact, and biochar can actually produce energy during the pyrolysis process; by contrast, both direct air capture and enhancing mineral weathering have significant energy requirements;
  6. One significant issue in terms of both SCS and biochar is “sink saturation,” i.e. decreased carbon sequestration potential as soils approach a new, higher equilibrium level. This can occur after 10-100 years for SCS, and is also an issue for biochar. This has implications for deployment of these technologies, as most scenarios for use of NETs envision primary importance in the second half of this century, meaning that deployment of some approaches in the next few years might have little impact later this century.

Overall, the author of the study concludes that SCS and biochar should be given serious consideration in integrated assessment models given their advantages over some other NET approaches.

Among the classroom questions that this study might generate:

  1. How do we determine the optimal mix of R&D funding for NETs?
  2. What should be the most important criteria for determining if we proceed with research on individual NETs options?
  3. What kind of governance architecture should be established for NETs research and development and/or deployment?