Euan Nisbet

Greenhouse gases -  they’re natural. They keep us warm – they add about 33^oC to the Earth’s natural surface temperature of -18^oC. That should give us a nice comfortable planet averaging about 15^oC on its gentle oceans and fertile continents. But then humans came along. We burned trees, and then coal, then oil and gas. We emitted  lots of Carbon dioxide. It wasn’t just CO₂.  We pushed up methane, CH₄ even more when we pumped gas in leaky pipes to warm our houses and make power, and we made gassy waste dumps and sewers. We kept lots of ruminant animals like cows and sheep. So we’ve been warming the planet.

Royal Holloway’s greenhouse gas lab studies all the greenhouse gases – but especially methane, which is arguably the most interesting and the easiest to bring under control as it is only in the air for roughly a decade before it is destroyed by natural reactions.

We led the UK Natural Environment Research Council’s Project MOYA - The Global Methane budget, a consortium of 14 institutions including universities and also the British Antarctic Survey and the Centre for Ecology and Hydrology, looking at methane all over the world but especially in tropical Africa (Upper Congo basin) and Amazonia. We also maintain long-term measurement in the high Arctic (Spitsbergen) and the equatorial Atlantic (Ascension).

Here in London, we have one of the world’s longest urban records of greenhouse gases and we are mapping leaks and cows and landfills all over the UK with our mobile laboratory.  It’s not just methane  – we measure CO₂, CO, N₂O and H₂ (did you know hydrogen is an indirect greenhouse gas and affects air pollution?) as well as methane: all part of the gasbusters’ job.

References

• Nicklas, RW, Puchtel, IS, Ash, RD, Piccoli, PM, Hanski, E, Nisbet, E, Waterton, P, Pearson, DG & Anbar, AD 2019, 'Secular mantle oxidation across the Archean-Proterozoic boundary: Evidence from V partitioning in komatiites and picrites', Geochimica et Cosmochimica Acta, vol. 250, pp. 49-75. https://doi.org/10.1016/j.gca.2019.01.037
• Yang, J, Junium, CK, Grassineau, NV, Nisbet, EG, Izon, G, Mettam, C, Martin, A & Zerkle, AL 2019, 'Ammonium availability in the Late Archaean nitrogen cycle', Nature Geoscience, vol. 12, pp. 553-557. https://doi.org/10.1038/s41561-019-0371-1
• Nisbet, E, Dlugokencky, EJ & Bousquet, P 2014, 'Methane on the rise – again', Science, vol. 343, no. 6170, pp. 493-495. https://doi.org/10.1126/science.1247828
• Nisbet, EG, Manning, MR, Dlugokencky, EJ, Fisher, RE, Lowry, D, Michel, SE, Myhre, CL, Platt, SM, Allen, G, Bousquet, P, Brownlow, R, Cain, M, France, JL, Hermansen, O, Hossaini, R, Jones, AE, Levin, I, Manning, AC, Myhre, G, Pyle, JA, Vaughn, BH, Warwick, NJ & White, JWC 2019, 'Very Strong Atmospheric Methane Growth in the 4 Years 2014–2017: Implications for the Paris Agreement', Global Biogeochemical Cycles, vol. 33, no. 3, pp. 318-342. https://doi.org/10.1029/2018GB006009
• Nisbet, E, Dlugokencky, EJ, Manning, MR, Lowry, D, Fisher, R, France, J, Michel, SE, Miller, JB, White, JWC, Vaughn, B, Bousquet, P, Pyle, JA, Warwick, N, Cain, M, Brownlow, R, Zazzeri, G, Lanoiselle, M, Manning, AC, Gloor, E, Worthy, DEJ, Brunke, EG, Labuschagne, C, Wolff, EW & Ganesan, AL 2016, 'Rising atmospheric methane: 2007–2014 growth and isotopic shift', Global Biogeochemical Cycles, vol. 30, no. 9, pp. 1356-1370. https://doi.org/10.1002/2016GB005406