Climate and composition impacts of a net-zero anthropogenic methane future using an emissions-driven chemistry-climate model
Authors: Staniaszek Zosia , Griffiths Paul T. , Folberth Gerd A. , O'Connor Fiona M. , Archibald Alexander T. 
Published: March 2021

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&lt;p&gt;Methane&amp;#160;(CH&lt;sub&gt;4&lt;/sub&gt;),&amp;#160;the second most important greenhouse gas in terms of radiative forcing,&amp;#160;is on the rise;&amp;#160;but&amp;#160;there are extensive&amp;#160;opportunities for mitigation with existing technologies.&amp;#160;Anthropogenic emissions account for around 60% of the global methane source,&amp;#160;and the&amp;#160;recent atmospheric methane growth rate puts us on a trajectory comparable to the most extreme future methane scenarios in the sixth Coupled Model Intercomparison Project (CMIP6).&amp;#160;&lt;/p&gt;
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&lt;p&gt;We use&amp;#160;a&amp;#160;new&amp;#160;methane emissions-driven configuration of the&amp;#160;UK Earth System Model&amp;#160;(UKESM1)&amp;#160;to explore the role of anthropogenic methane in the earth system.&amp;#160;The full methane cycle is represented, including surface deposition, chemistry&amp;#160;and interactive wetland emissions.&amp;#160;As a baseline scenario we used Shared Socioeconomic Pathway 3-7.0 (SSP3-7.0) &amp;#8211; the highest methane emissions scenario in CMIP6.&amp;#160;In an idealised&amp;#160;experiment,&amp;#160;all anthropogenic methane emissions were instantaneously&amp;#160;stopped&amp;#160;from 2015&amp;#160;onwards&amp;#160;in a coupled atmosphere-ocean&amp;#160;simulation&amp;#160;running&amp;#160;from 2015-2050, to make a&amp;#160;net-zero&amp;#160;anthropogenic methane emissions scenario.&amp;#160;&amp;#160;&lt;/p&gt;
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&lt;p&gt;Within a decade,&amp;#160;significant changes&amp;#160;can be seen in&amp;#160;atmospheric&amp;#160;composition and climate, compared to&amp;#160;SSP3-7.0.&amp;#160;The atmospheric methane burden declines&amp;#160;to below&amp;#160;pre-industrial levels within 12 years, and by&amp;#160;the&amp;#160;late 2030s reaches a constant&amp;#160;level&amp;#160;around&amp;#160;44% below&amp;#160;that of the&amp;#160;present day (2015).&amp;#160;The tropospheric ozone burden and surface mean ozone concentrations decreased by 12% and 15% respectively by 2050 &amp;#8211; key in terms of limiting global warming as well as improving air quality and human health.&amp;#160;&lt;/p&gt;
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&lt;p&gt;By 2050 the net-zero anthropogenic methane scenario results in a global mean surface temperature (GMST) 1&amp;#730;C lower than the baseline, a significant value in the context of climate goals such as the Paris Agreement. Through decomposition of the radiation budget, the change in climate can be directly attributed to the reduction in methane and indirectly to the resulting changes in ozone, clouds and ozone precursors such as CO. In addition, the changes in climate result in impacts on the interactive wetland emissions via changes in temperature and wetland extent, highlighting the coupled nature of methane in the earth system.&amp;#160;&lt;/p&gt;
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&lt;p&gt;Cessation of anthropogenic methane emissions has profound impacts on near-term warming and on tropospheric ozone, but ultimately cannot single-handedly&amp;#160;achieve the&amp;#160;necessary reductions&amp;#160;for meeting&amp;#160;Paris goals.&amp;#160;&lt;/p&gt;
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