Unmask temporal trade-offs in climate policy debates
ABSTRACT: Global warming potentials (GWPs) have become an essential element of climate policy and are built into legal structures that regulate greenhouse gas emissions. This is in spite of a well-known shortcoming: GWP hides trade-offs between short- and long-term policy objectives inside a single time scale of 100 or 20 years (1). The most common form, GWP100, focuses on the climate impact of a pulse emission over 100 years, diluting near-term effects and misleadingly implying that short-lived climate pollutants exert forcings in the long-term, long after they are removed from the atmosphere (2). Meanwhile, GWP20 ignores climate effects after 20 years. We propose that these time scales be ubiquitously reported as an inseparable pair, much like systolic-diastolic blood pressure and city-highway vehicle fuel economy, to make the climate effect of using one or the other time scale explicit. Policy-makers often treat a GWP as a value-neutral measure, but the time-scale choice is central to achieving specific objectives (2–4). Read the RESEARCH BRIEF below.
Scientists and policymakers use measurements like global warming potential to compare how varying greenhouse gases, like carbon dioxide and methane, contribute to climate change.
Yet, despite its widespread use, global warming potential fails to provide an accurate look at how greenhouse gases affect the environment in the short and long-term, according to a team of researchers from Princeton University, the Environmental Defense Fund and Harvard University.
The researchers argue in the May 5 issue of Science that because global warming potential calculates the warming effects of greenhouse gases over 100 years, they discount the effects of any greenhouse gas that disappears from the atmosphere after a decade or two. This masks the trade-offs between short- and long-term policies at the heart of today’s political and ethical debates.
What is needed, the researchers conclude, is a standardized approach that recognizes both commonly utilized timescales — 20 and 100 years — as a ubiquitous pair. This two-valued approach would provide clarity to climate change policy analyses, which often result in misleading debates about policy trade-offs.
“Different gases have widely different lifetimes in the atmosphere after emission and affect the climate in different ways over widely different timescales,” said co-author Michael Oppenheimer, the Albert G. Milbank Professor of Geosciences and International Affairs, Woodrow Wilson School of Public and International Affairs and the Department of Geosciences at Princeton University. “The paired approach creates a more comprehensive picture of the nature of climate change and the effects of various policies to stem its consequences.”
While most reports reference only one of these metrics — most measure the effects over 100 years — a standardized approach including both should become the norm to avoid skewing results. For example, recent studies show anti-shale gas advocacy groups base arguments around the 20-year time horizon, while the pro-shale gas community emphasizes the 100-year timescale, but both metrics are needed to truly understand the short- and long-term impacts shale gas has on the environment.
The researchers liken the 20- and 100-year timescales to city-highway vehicle fuel efficiency data. Car dealerships boast about miles per gallon for both highway and city, providing buyers with an analysis relevant to different roadways. The dual-number system also enables buyers to calculate an average.
Another example is how blood pressure is measured with two numbers, systolic and diastolic. The first number (systolic) measures the pressure in your blood vessels as the heart beats. The second number (diastolic) calculates the pressure in your blood vessels when your heart rests between beats. Together, the numbers reveal whether a person has an average blood pressure, like 120 over 80, or is at risk of pre-hypertension or high blood pressure.
While the researchers advocate using both 20- and 100-year time scales (rather than one or the other), they do not advocate for a change in time horizons. Both the 20- and 100-year time scales are now the default in climate change policy, and shifting to new time horizons would likely be met with much resistance.
“It is imperative that both the near- and long-term climate impacts of policies be transparent to a decisionmaker,” said lead author Ilissa B. Ocko, climate scientist at the Environmental Defense Fund. “We are not saying that one timescale is more important than the other, just that the decisionmaker must be fully informed of climate impacts on all timescales.”
The widespread adoption of this improved combined measure would require communication and coordination between key scientific journals and scientific societies. Groups dealing with climate change groups —the Intergovernmental Panel on Climate Change, U.S. Environmental Protection Agency, the U.N. Environmental Programme and the United Nations Framework Convention on Climate Change — would also need to adopt the new measure in their reports.
The proposal was written by lead authors Ilissa B. Ocko, Steven P. Hamburg and Nathaniel O. Keohane from the Environmental Defense Fund. Co-authors include, from Princeton University, Michael Oppenheimer, the Albert G. Milbank Professor of Geosciences and International Affairs, Woodrow Wilson School of Public and International Affairs and the Department of Geosciences; and Stephen W. Pacala, the Frederick D. Petrie Professor in Ecology and Evolutionary Biology, Department of Ecology and Evolutionary Biology. Additional authors include David W. Keith, Joseph D. Roy-Mayhew and Daniel P. Schrag from Harvard University.
The paper, “Unmask temporal trade-offs in climate policy debates,” was published online May 5 in Science. The work was partially funded by the Robertson Foundation, the Kravis Scientific Research Fund and the High Meadows Foundation.