Methane

Methane (CH₄) is a powerful short-lived greenhouse gas with a lifetime in the atmosphere of just over 12 years¹. Since the 1700s, the concentration of CH₄ in the atmosphere has risen from about 700 to 1850 parts per billion (ppb). Despite being present in the atmosphere at very low concentrations, CH₄ exerts a strong influence on global temperature because it is highly effective at absorbing infrared radiation. Most of the warming from CH₄ occurs within 50 years of its emission; however, some lingers beyond 100 years. Current estimates are that global anthropogenic CH₄ emissions have contributed about 40 percent (~40%) of the total warming the world has experienced since the industrial revolution².

Sources of methane

Global anthropogenic CH₄ emissions (i.e. those caused by human activity) come primarily from three major sources: agriculture (~40%); oil, gas, and coal (~30%); and waste (~20%)¹. In the agricultural sector, livestock are the dominant source³.

Key Points

• Worldwide methane emissions from ruminant animals have made a substantial contribution to current global warming.
• New Zealand’s ruminant animals’ methane emissions make a substantial contribution to total New Zealand greenhouse gases emissions and the global warming that our emissions have contributed to so far.
• Methane is a short-lived gas; because of this, its emissions don’t have to be reduced to zero to meet the temperature goals of the Paris Agreement. This is in contrast to the long-lived gas carbon dioxide, which has to be reduced to zero.
• Setting national methane emissions reduction targets involves balancing social, economic, environmental and equity issues that science can only partly inform.

Estimates of the CH₄ currently produced globally by livestock are in the range of 90 to 120 million tonnes CH₄ per annum^4,5,6. This is 30 percent of total anthropogenic CH₄ emissions. Livestock have been responsible for around 14 percent of the warming experienced by the Earth since the Nineteenth Century⁷. Enteric CH₄ emissions, those arising from the digestion of feed, comprise approximately 90 per cent of all livestock-derived emissions, with cattle (77 percent) being the dominant source globally⁴.

Worldwide by 2030, CH₄ emissions are forecast to be 12 percent above current emissions⁶.

In New Zealand, CH₄ emissions from agriculture livestock have risen from 1.1 million tonnes in 1990 to 1.16 million tonnes in 2016⁷. Dairy cattle emissions currently comprise 50 percent of New Zealand’s agricultural CH₄ emissions. Methane emissions from New Zealand’s agricultural sector peaked in 2006 and current forecasts are that they will remain relatively unchanged until at least 2030⁸.

Breakdown in the atmosphere

Methane has a short life in the atmosphere, principally because of chemical reactions with hydroxyl radicles (OH) in the troposphere (between the Earth’s surface and the stratosphere). These reactions break down CH₄ into water (H₂O) and carbon dioxide (CO₂)². Given that enteric CH₄ arising from the digestion of plant material removes CO₂ from the atmosphere by photosynthesis, it is easy to think it's simply a case of CO₂ in and CO₂ out, and hence completely neutral with respect to global warming.

This is incorrect, because for a short time some of the CO₂ removed from the atmosphere by photosynthesis is present in the atmosphere as CH₄. This absorbs more infrared radiation than the CO₂ from which it was originally derived (see reference source⁹ for a more detailed discussion).

How does methane compare with other greenhouse gases?

The three main anthropogenic greenhouse gases (GHG) are CO₂, CH₄ and nitrous oxide (N₂O). These differ in their longevity in the atmosphere and in their absorption of infrared radiation. International treaties designed to encourage the reduction of anthropogenic GHG, for example the United Framework Convention on Climate Change (UNFCCC), refer to GHG collectively. This raises the question: how should individual GHG be compared with each other?

To answer this question, scientists have devised systems that allow all GHG to be expressed using common units. The most common of these systems is called Global Warming Potentials (GWP) in which CO₂ is given a value of one and other gases are compared with CO₂ based on their longevity in the atmosphere and their ability to absorb infrared radiation¹⁰.

In international reporting to the UNFCCC, GHG are compared over a 100-year timeframe: CH₄ currently has a value of 25 and N₂O a value of 298. Using these values, GHG can be reported in a common currency known as carbon dioxide equivalents (CO₂-e). Figure 1 explains graphically how CH₄ warms the atmosphere relative to CO₂. Basically, one tonne of CH₄ creates the same average warming as 25 tonnes of CO₂ over a 100-year period (i.e. the area under the curves are equal).

Figure 1 also shows that the GWP gives a good representation of the average warming over a given period of time relative to CO₂. However, it hides the fact that the time course of warming caused by CH₄ is very different to that of CO₂. Methane has a short life in the atmosphere and a much higher level of warming initially, but one that disappears relatively quickly. Carbon dioxide has less of an immediate impact but, because it decays much more slowly, the warming continues at a similar level for hundreds of years.

GWPs are the most commonly used method for comparing different GHG but they’re not the only method. GWPs have also been criticised as being an inappropriate metric when considering how CH₄ should be treated relative to CO₂ under ambitious GHG mitigation, and when considering the impact of cumulative emissions year-on-year¹¹.

Does New Zealand have a specific methane reduction target?

Under the 2015 Paris Agreement, 196 countries pledged to reduce GHG emissions with an aim of restricting global temperature rise to well below two degrees Celsius (2^oC) and pursue efforts to keep the warming as low as 1.5^oC. Parties to the Paris Agreement have submitted plans for reducing emissions up to the year 2030 – so-called Nationally Determined Contributions (NDC). New Zealand in its NDC has committed to reducing CO₂-e GHG emissions to 30 percent below 2005 levels by 2030.

Parties to the agreement are expected to strengthen their reduction commitment over time. New Zealand has not set a specific target for individual gases within its emissions reductions. However, since CH₄ from agriculture comprises more than 40 percent of all CO₂-e emissions, there is likely to be pressure on the livestock sector to reduce CH₄ emissions. In the longer term, the current government is working on a Zero Carbon Bill. In its consultation phase, that bill outlined options that could result in differential targets for the three principal GHGs out to 2050.

These options included a target to reduce CO₂ to ‘net zero’ by 2050 (emissions minus removals of CO₂ stored in things like trees). They also included a reduction in all gases to net zero (using the same approach) by 2050, and a differential treatment of the short-lived gas (CH₄) and the long-lived gases (CO₂ and N₂O). This latter option calls for ‘stabilising’ CH₄ at some level, with the other gases reduced to net zero.

Why should methane be treated differently to carbon dioxide and nitrous oxide?

The 2018 report⁷, commissioned by the Parliamentary Commissioner for the Environment (PCE), lays out in detail the scientific basis for treating CH₄ differently to CO₂ when it comes to GHG mitigation. The following brief summary draws on this report.

As methane lives for only a short time in the atmosphere, stabilising or reducing emissions below their current levels would see the concentration in the atmosphere level off within a few decades. This in turn means that, eventually, no additional warming will occur in excess of that caused already by existing emissions, but this levelling off in warming will take some time.

Figure 1 shows that although CH₄ lasts for around 12 years in the atmosphere, the warming from an individual emission pulse continues for more than 100 years after the gas has disappeared from the atmosphere. So stabilising emissions at current levels still results in increased warming for several centuries (albeit at a declining rate).

In contrast, CO₂ can remain in the atmosphere for thousands of years, so the removal of previous emissions will not offset current emissions in the same way that CH₄ does. Each CO₂ unit emitted increases the concentration in the atmosphere. If CO₂ emissions are stabilised, the concentration in the atmosphere will continue to increase as the removal of past emissions will not balance the addition of emissions. Hence, temperatures will keep rising. The only way for CO₂ concentration in the atmosphere to stabilise, and hence make no further increased contribution to warming, is for the net emissions of CO₂ to be zero.

The different behaviour of CO₂ and CH₄ in the atmosphere leads to two very clear conclusions. First, for the world to stay within the below-2^oC temperature limit, CO₂ emissions need to be reduced to zero as quickly as possible. Second, CH₄ emissions don’t have to be reduced to zero but the less CH₄ is emitted, the less the Earth will warm overall. The more CH₄ is reduced below current levels, the more feasible it is for the world stay well below the 2^oC limit (see Figure 1).

So is there an unambiguous methane reduction target for New Zealand?

Setting national targets for GHG reduction has to consider more than science. Science tells us that to meet the Paris Agreement temperature limit of well below 2^oC, CH₄ does not have to go to zero. However, the lower future emissions go, the less New Zealand will contribute to climate change. Science alone doesn’t tell us what a national reduction target should be, or the rate at which the target should be reached. Setting targets involves far wider consideration of social, economic, environmental and equity issues (both within New Zealand and between New Zealand and the rest of the world). These involve judgements and trade-offs that science can only partially inform.

The recent PCE report⁹ estimated that if New Zealand reduced its CH₄ emissions by 10 to 22 percent below 2016 levels by 2050 (the range reflects differing assumptions around atmospheric feedback processes and emissions from other countries), then our CH₄ emissions would contribute no further to global warming than they already are. This implies that if emissions could be reduced by more than 10 to 22 percent below 2016 levels, we would contribute to ‘cooling’ the planet, relative to the warming caused up to 2016.*

Press coverage has generally interpreted the 10 to 22 percent as an appropriate national target for New Zealand, a notion that the author of the report went to considerable effort to refute. Interpreting 10 to 22 percent as an appropriate target implicitly assumes that ‘not adding any further to warming’ is an appropriate way to frame a national target for CH₄ and, further, that 2016 is the correct reference year.

Choosing ‘not adding any further to warming’ as the benchmark by which to set a methane reduction target makes the tacit assumption that the warming caused to date is the acceptable level for New Zealand (i.e. that we have some sort of property right to the warming we have already caused) and that not causing any more warming fulfils our contribution to meeting the goals of the Paris Agreement. This is certainly not an issue that can be decided by science.

The choice of reference year is also problematic. The Paris Agreement doesn’t set GHG emission targets relative to a reference year. It simply seeks to limit warming relative to the pre-industrial levels (loosely, since the mid-Nineteenth Century¹²). It’s then up to each country to set emission targets they think will be consistent with that overall goal.

New Zealand’s commitment under the Kyoto Protocol was not to increase GHG emissions above 1990 levels on average over the 2008 to 2012 period. For 2013 to 2020, New Zealand voluntarily agreed to reduce emissions to five percent below 1990 levels. Under the Paris Agreement, the emissions reduction target is 30 percent below 2005 levels. Science can inform the consequences of using a particular reference year but it doesn’t tell us the appropriate reference year to choose. So, science can’t provide a definitive CH₄ reduction target for New Zealand. However, science can help ensure that any target takes into account CH₄'s short-lived life in our atmosphere, alongside social, economic, environmental and equity issues. Any methane target needs to be regularly reviewed to ensure it takes account of changing circumstances.

* ‘Cooling’ here refers to causing less warming than that caused relative to a reference point, e.g. a particular reference year. All emissions of methane will cause the earth to be warmer than if they had not been emitted. With a shortlived gas like methane, reductions in emissions against a fixed reference point can result in the absolute contribution to warming going down, compared with that reference point. Current methane emissions still warm the atmosphere, but not as much as previous emissions did. This is not the case for a long-lived gas like carbon dioxide.

References

1. Ciais P., C. Sabine, G. Bala et al. 2013. Carbon and Other Biogeochemical Cycles. In: Stocker T. F., D. Qin, G. K. Plattner et al. (eds). Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA. Pages 465-570.
2. Myhre, G., D. Shindell, F. M. Bréon et al. Chapter 8: Anthropogenic and Natural Radiative Forcing. In: Stocker T. F., D. Qin, G. K. Plattner et al. (eds). Climate Change 2013: The Scientific Basis. Cambridge University Press, Cambridge, UK, and New York, USA.
3. Smith P., M. Bustamante, H. Ahammad, H. Clark, H. Dong, E. A. Elsiddig, H. Haberl, R. Harper, J. House, M. Jafari, O. Masera, C. Mbow, N. H. Ravindranath, C.W. Rice, C. Robledo Abad, A. Romanovskaya, F. Sperling, and F. Tubiello. 2014. Agriculture, Forestry and Other Land Use (AFOLU). In: Climate Change 2014. Mitigation of Climate Change. Contribution of Working Group III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Edenhofer, O., R. Pichs-Madruga, Y. Sokona, E. Farahani, S. Kadner, K. Seyboth, A. Adler, I. Baum, S. Brunner, P. Eickemeier, B. Kriemann, J. Savolainen, S. Schlömer, C. von Stechow, T. Zwickel and J. C. Minx (eds)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.
4. Gerber, P. J., H. Steinfeld, B. Henderson, A. Mottet, C. Opio, J. DIjkman, A. Falcucci, and G. Tempio. 2013. Tackling climate change through livestock: a global assessment of emissions and mitigation opportunities. Food and Agriculture Organization of the United Nations (FAO).
5. Wolf, J., G. R. Asrar, and T. O. West. 2017. Revised methane emissions factors and spatially distributed annual carbon fluxes for global livestock. Carbon Balance and Management, 12, 16.
6. FAO. 2016. Food and Agriculture Organization of the United Nations Statistics Division. Faostat. http://www.fao.org/faostat/en/#data
7. Ministry for the Environment. 2018. http://www.mfe.govt.nz/sites/default/files/ media/Climate%20Change/National%20GHG%20Inventory%20Report%20 1990-2016 final.pdf
8. Ministry for the Environment. 2017. www.mfe.govt.nz/publications/climatechange/ new-zealands-third-biennial-report-under-united-nations-framework
9. Parliamentary Commissioner for the Environment. 2018. A note on New Zealand’s methane emissions from livestock, August 2018.
10. Climate Change 1995. The Science of Climate Change: Summary for Policymakers and Technical Summary of the Working Group I Report. Page 22.
11. Allen M. R., K. P. Shine, J. S. Fuglestvedt et al. 2018. A solution to the misrepresentations of CO₂-equivalent emissions of short-lived climate pollutants under ambitious mitigation. Climate and Atmospheric Science advances online: DOI: 10.1038/s41612-018-0026-8.
12. Reisinger A., and H. Clark. 2017. How much do direct livestock emissions actually contribute to global warming? Global Change Biology. 00:1–13. https://doi.org/10.1111/gcb.13975

This article was originally published in Technical Series December 2018