Last year global methane reached a new historic high, marking the second highest year‐over‐year jump recorded over the last 20 years. More importantly, the jump in 2018 extended an unanticipated multi‐year resurgence of growth in global methane levels that has generated enormous concern in the science community. Scientists report that the new and unexpected methane math threatens to eliminate the anticipated gains of the Paris Climate Agreement, an agreement built upon models that assumed stable methane.[3]

The “why” behind this resurgence is hotly debated and not well understood. That said, most experts in the field suspect that all traditional sources (natural and anthropogenic) are contributing at least in small part to the surge, and that the biggest contributor might be wetlands responding to climate change (though there is some dissent on this point).[4]

Interestingly, the answer to the question about which emissions source is driving the methane surge is very different from the answer to the question about which emission source is best targeted in order to address the surge. It is extremely challenging to control how wetlands respond to climate change (assuming that is the driver).

Thus, there is wide agreement among experts that, regardless of the drivers behind the surge, reducing emissions from fossil‐fuel production and distribution, primarily through ending leaks and venting, is one of the few options available to control global methane levels and that this option is the most practical one. In addition, scientists report that there are narrow opportunities to address agricultural emissions, e.g. changes in the diet of livestock can reduce the production of methane without affecting production.

Globally anthropogenic methane emissions account for roughly 48% of total methane emissions, and in turn fossil‐fuel methane emissions account for roughly 34% of total anthropogenic emissions.[5]
In the United States, the natural gas and petroleum system is the largest source of methane emissions.[6] The most recent analysis suggests that U.S. methane emissions from oil and gas activity have increased over the last 10 years at 3.4% per year,[7] about 40% over the decade.[8]

Methane is a short‐lived but super‐potent greenhouse gas and is the second most important contributor to anthropogenic global warming after CO2, accounting for one‐quarter of the anthropogenic radiative imbalance (the human forcing of warming) since the pre‐industrial era.[9]

Prior to the industrial era global methane levels were low and relatively stable for the last 800,000 years, ranging from 300 – 800 ppb. With the advent of agriculture and then fossil fuel operations, methane levels skyrocketed to more than 1,800 ppb.

Starting in 1990s, the growth in global methane levels began to slow down, and global methane became relatively stable over the period of 2000 – 2006. A resurgence of global methane was not anticipated and came as a surprise.[10]Crucially, methane levels were considered stable in the pathway models prepared for the Paris Climate Agreement.[11]

Nevertheless, global methane levels resumed rapid growth starting in 2007. Growth accelerated further starting in 2014 and extending through 2017.[12]This exceptional growth continued in 2018.[13] NOAA recently announced that the rate of methane increase accelerated over the past five years, jumping 50 percent over the growth rate observed 2007 – 2013.[14] The sustained growth of the last five years was last observed in the 1980s when the Soviet Union’s gas industry was developing very rapidly.[15]

At first the durability of this emerging trend was questioned and years of rapid growth were seen as anomalies.[16] However, the period of resumed growth in global methane levels now stands at 12 years (2007 – 2018) compared to the 7‐year period of stable methane levels (2000 – 2006). And preliminary data from 2018 indicates that the trend of extraordinarily high growth now stands at 5 years.

In this light the era of stable global methane levels is increasingly seen as the anomaly, and growth in global methane seen as the resumption of a long‐standing pattern.[17] This emerging consensus was highlighted in two recent high‐profile papers published in 2019 representing the consensus views of a large array of experts in the field.[18]

The threat posed by this resumption in methane growth is significant. A group of 23 scientists recently reported  

Thus even if anthropogenic CO2 emissions are successfully constrained to a RCP2.6-like pathway, the unexpected and sustained current rise in methane may so greatly overwhelm all progress from the other reduction efforts that the Paris Agreement will fail.”[19]

While the resumption of growth in global methane is now well documented, the drivers are less well understood and hotly debated. Present global environmental monitoring networks only provide sparse information about methane concentrations, making it challenging and complex to distinguish between the myriad individual sources of methane from the fossil fuel industries, and dispersed sources like wetlands and agriculture. Gaps in monitoring also make it impossible to rule out a decrease in the efficacy of natural mechanisms that sweep methane from the atmosphere (aka “sinks”).

Potential drivers in the category of increased emissions include emissions from intensive agricultural practices, emissions from oil and gas operations, and increased emissions from wetlands responding to global warming. [This last potential driver is particularly worrisome as it implies the engagement of a global warming feedback loop.] A number of studies have assigned and evaluated the role of each of these drivers, with different studies assigning greater weight to different drivers; all are generally considered to play at least a minor role.[20]

While the size of the role of fossil‐fuel production and distribution in driving the recent growth of global methane is hotly debated, it is well documented that fossil‐fuel production is one of the major drivers in sustaining industrial era methane levels.[21] As a result, reducing fossil‐fuel methane emissions would have a significant impact in addressing the methane surge. The lifetime of methane is relatively short (∼11 years), and the elevated global methane levels of the industrial era only occur as a result of large anthropogenic emissions. Finally, fossil‐fuel production and distribution is certainly one of the major sources of anthropogenic emissions.

Fossil‐fuel methane emissions are also the most easily addressed source of emissions. The International Energy Agency estimates industry can reduce its worldwide emissions by 75 percent — and that up to two‐thirds of those reductions (40 – 50% of total emissions) can be realized at zero net cost.[22]

In addition, there are particular opportunities to address emissions from agriculture.[23] Turner et al., 2019, note that changes in the diet of livestock could reduce the production of methane in dairy cattle without reducing milk production.

In this context the 23 authors of Nisbet et al wrote:  

We may not be able to influence the factors driving the new rise in methane, especially if it is a climate change feedback, but by monitoring, quantifying and reducing the very large anthropogenic inputs, especially from the gas, coal and cattle industries, and perhaps by direct removal, we may be able to cut the total methane burden to be compliant with the Paris goals.”

First published by Climate Code Red, 5 May 2019

Citations 

Dean et al. (2018): Methane Feedbacks to the Global Climate System in a Warmer World. Reviews of Geophysics. January 2018. https://doi.org/10.1002/2017RG000559

Howarth (2019): Is Shale Gas a Major Driver of Recent Increase in Global Atmospheric Methane?, Biogeosciences Discuss., https://doi.org/10.5194/bg-2019 – 131, in review, 2019.

Jacobson et al. (2018): Chapter 8: Observations of atmospheric carbon dioxide and methane. In Second State of the Carbon Cycle Report (SOCCR2): A Sustained Assessment Report [Cavallaro, N., G.

Shrestha, R. Birdsey, M. A. Mayes, R. G. Najjar, S. C. Reed, P. Romero‐Lankao, and Z. Zhu (eds.)]. U.S. Global Change Research Program, Washington, DC, USA, pp. 337 – 364, https://doi.org/10.7930/SOCCR2.2018.Ch8.

Lan et al. (2019): Long‐Term Measurements Show Little Evidence for Large Increases in Total U.S. Methane Emissions Over the Past Decade. Geophysical Research Letters. April 2019. https://doi.org/10.1029/2018GL081731

Lyon and Schwietzke (2019) Does new NOAA study really show that methane emissions have been overestimated? No. Energy Exchange. EDF. May 2019

Maasakkers et al. (2019): Global distribution of methane emissions, emission trends, and OH concentrations and trends inferred from an inversion of GOSAT satellite data for 2010 – 2015. Atmospheric Chemistry and Physics. January

NOAA AGGI 2019. Rising Emissions Drive Greenhouse Gas Index Increase. NOAA Research News. 21 May 2019 https://research.noaa.gov/article/ArtMID/587/ArticleID/2455/RISING-EMISSIONS-DRIVE-GREENHOUSE-GAS-INDEX-INCREASE

Nisbet et al. (2019): Very Strong Atmospheric Methane Growth in the 4 Years 2014 – 2017: Implications for the Paris Agreement. Global Biogeochemical Cycles. March 2019. https://doi.org/10.1029/2018GB006009

Shindell et al. (2017): The social cost of methane: theory and applications. Faraday Discussions. January 2017 DOI10.1039/c7fd00009j

Turner, Frankenberg, and Kort (2019): Interpreting contemporary trends in atmospheric methane. Proceedings of the National Academy of Sciences. 19 February 2019.

Underwood (2019): Rising Methane Emissions Could Derail the Paris Agreement. EOS. 19 April 2019. https://eos.org/research-spotlights/rising-methane-emissions-could-derail-the-paris-agreement

Worden et al. (2017): Reduced biomass burning emissions reconcile conflicting estimates of the post‐2006 atmospheric methane budget. Nature Communications. December 2017. https://doi.org/10.1038/s41467-017 – 02246‐0

Notes 

[1] NOAA Earth System Research Laboratory Global Monitoring Division. https://esrl.noaa.gov/gmd/ccgg/trends_ch4/
[2] Nisbet et al., 2019. Turner, Frankenberg, and Kort, 2019.
[3] Nisbet et al., 2019; Underwood, 2019.
[4] Jacobson et al., 2018. Nisbet et al, 2019. Turner, Frankenberg, and Kort, 2019.
[5] Dean et al., 2018.
[6] https://www.epa.gov/ghgemissions/overview-greenhouse-gases
[7] Lan et al. 2019.
[8] Lyon and Schwietzke (2019)
[9] Turner, Frankenberg, and Kort, 2019.
[10] Nisbet et al., 2019. Turner, Frankenberg, and Kort, 2019. Underwood, 2019.
[11] Nisbet et al., 2019
[12] Nisbet et al., 2019. Turner, Frankenberg, and Kort, 2019. Underwood, 2019.
[13] NOAA Earth System Research Laboratory Global Monitoring Division. https://esrl.noaa.gov/gmd/ccgg/trends_ch4/
[14] NOAA AGGI, 2019
[15] Nisbet et al, 2019
[16] Turner, Frankenberg, and Kort, 2019
[17] Turner et al., 2019
[18] Nisbet et al., 2019. Turner, Frankenberg, and Kort, 2019. Underwood, 2019.
[19] Nisbet et al., 2019
[20] Nisbet et al., 2019. Turner, Frankenberg, and Kort, 2019. Massakkers et al., 2019. Worden et al., 2017. Howarth et al., 2019. Jacobson et al., 2018. Lan et al., 2019.
[21] Dean et al., 2018. Nisbet et al., 2019.
[22] International Energy Agency, 2017. World Energy Outlook 2017. IEA Publications, Paris. https://www.iea.org/newsroom/news/2017/october/commentary-the-environmental-case-for-natural-gas.html
[23] Shindell et al., 2017