Variations in global methane sources and sinks during 1910–2010

• Published in: Atmospheric Chemistry and Physics
• Main Authors: A. Ghosh, P. K. Patra, K. Ishijima, T. Umezawa, A. Ito, D. M. Etheridge, S. Sugawara, K. Kawamura, J. B. Miller, E. J. Dlugokencky, P. B. Krummel, P. J. Fraser, L. P. Steele, R. L. Langenfelds, C. M. Trudinger, J. W. C. White, B. Vaughn, T. Saeki, S. Aoki, T. Nakazawa
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2015
• Subjects: Physics; QC1-999; Chemistry; QD1-999; Arctic; Antarctic; Antarc*
• Online Access: https://doi.org/10.5194/acp-15-2595-2015; https://doaj.org/article/162480c7e17a46f295daf7693abee4f8

Atmospheric methane (CH 4 ) increased from ~900 ppb (parts per billion, or nanomoles per mole of dry air) in 1900 to ~1800 ppb in 2010 at a rate unprecedented in any observational records. However, the contributions of the various methane sources and sinks to the CH 4 increase are poorly understood. Here we use initial emissions from bottom-up inventories for anthropogenic sources, emissions from wetlands and rice paddies simulated by a~terrestrial biogeochemical model, and an atmospheric general circulation model (AGCM)-based chemistry-transport model (i.e. ACTM) to simulate atmospheric CH 4 concentrations for 1910–2010. The ACTM simulations are compared with the CH 4 concentration records reconstructed from Antarctic and Arctic ice cores and firn air samples, and from direct measurements since the 1980s at multiple sites around the globe. The differences between ACTM simulations and observed CH 4 concentrations are minimized to optimize the global total emissions using a mass balance calculation. During 1910–2010, the global total CH 4 emission doubled from ~290 to ~580 Tg yr −1 . Compared to optimized emission, the bottom-up emission data set underestimates the rate of change of global total CH 4 emissions by ~30% during the high growth period of 1940–1990, while it overestimates by ~380% during the low growth period of 1990–2010. Further, using the CH 4 stable carbon isotopic data (δ 13 C), we attribute the emission increase during 1940–1990 primarily to enhancement of biomass burning. The total lifetime of CH 4 shortened from 9.4 yr during 1910–1919 to 9 yr during 2000–2009 by the combined effect of the increasing abundance of atomic chlorine radicals (Cl) and increases in average air temperature. We show that changes of CH 4 loss rate due to increased tropospheric air temperature and CH 4 loss due to Cl in the stratosphere are important sources of uncertainty to more accurately estimate the global CH 4 budget from δ 13 C observations.