Renewed growth of atmospheric methane

By M. Rigby, R. Prinn, P. Fraser, P. Simmonds, R. Langenfelds, J. Huang, D. Cunnold, L. Steele, P. Krummel, R. Weiss and 6 more. 2008

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History of chemically and radiatively important atmospheric gases from the Advanced Global Atmospheric Gases Experiment (AGAGE) (2018, methodology): “Analysis of these observations shows that global average OH levels vary from year to year only occasionally significantly, but exhibit no significant long-term trend (Prinn et al., 2001, 2005; Rigby et al., 2008, 2013, 2017, latter updated in Fig.”
The impacts of climate change and human activities on biogeochemical cycles on the Qinghai‐Tibetan Plateau (2013, background): “Such processes are irreversible in the short term without large-scale human intervention, and would release a large amount of carbon, particularly if they are accompanied by permafrost thawing (Rigby et al., 2008).”
Global wetland contribution to 2000–2012 atmospheric methane growth rate dynamics (2017, background): “…latitudinal variability (Nisbet et al 2014), and several explanations have been proposed, including a reduction in the OH sink capacity for CH 4 (Rigby et al 2008), increases in Arctic and tropical wet-land emissions (Dlugokencky et al 2009), increased fossil fuel activities related to…”