Very Strong Atmospheric Methane Growth in the 4 Years 2014–2017: Implications for the Paris Agreement
Royal Holloway University of London · Victoria University of Wellington · +17 more institutions
Abstract
Abstract Atmospheric methane grew very rapidly in 2014 (12.7 ± 0.5 ppb/year), 2015 (10.1 ± 0.7 ppb/year), 2016 (7.0 ± 0.7 ppb/year), and 2017 (7.7 ± 0.7 ppb/year), at rates not observed since the 1980s. The increase in the methane burden began in 2007, with the mean global mole fraction in remote surface background air rising from about 1,775 ppb in 2006 to 1,850 ppb in 2017. Simultaneously the 13 C/ 12 C isotopic ratio (expressed as δ 13 C CH4 ) has shifted, now trending negative for more than a decade. The causes of methane's recent mole fraction increase are therefore either a change in the relative proportions (and totals) of emissions from biogenic and thermogenic and pyrogenic sources, especially in the…
Citation impact
- FWCI
- 55.74
- Percentile
- 100%
- References
- 128
Authors
23- EGEuan G. NisbetCorresponding
Royal Holloway University of London
- MMMartin ManningCorresponding
Victoria University of Wellington
- EJE. J. DlugokenckyCorresponding
National Oceanic and Atmospheric Administration, NOAA Earth System Research Laboratory
- RFRebecca Fisher
Royal Holloway University of London
- DLDavid Lowry
Royal Holloway University of London
Topics & keywords
- Methane
- Atmospheric methane
- Environmental science
- Sink (geography)
- Subtropics
- Methane emissions
- Atmospheric sciences
- Greenhouse gas
- Climate action
Funding
- SRSight Research UKAwards: NE/I013342/1, NE/N016122/1, NE/R017638/1, NE/I02934X/1, NE/F006160/1, NE/S003657/1, NE/I014683/1, NE/P019641/1, NE/M001768/1, NE/K006045/1, NE/N018001/1, NE/N014375/1, NE/N015584/1, NE/K00221X/1, NE/N018028/1, NE/R01809X/1, NE/I028874/1, NE/N016211/1, ncas10014, NE/N015835/1, bas0100032, NE/S00159X/1, NE/M005836/1, NE/I029161/1, NE/N016238/1
- UHUniversität Heidelberg
- NFNorges Forskningsråd
- NONational Oceanic and Atmospheric Administration
- NENatural Environment Research CouncilAwards: NE/I02934X/1, bas0100032, NE/N015584/1, NE/I014683/1, NE/P019641/1, NE/I028874/1, NE/M005836/1, NE/N015835/1, NE/R01809X/1, NE/S00159X/1, NE/K00221X/1, NE/N016238/1, NE/P019641/1, NE/I029161/1, NE/N016122/1, NE/N018028/1, NE/I014683/1, NE/R017638/1, NE/S003657/1, NE/M001768/1, NE/N014375/1, NE/F006160/1, NE/I013342/1, NE/S00159X/1, NE/N016238/1, NE/I028874/1, NE/M001768/1, NE/N018001/1, NE/N016211/1, ncas10014, NE/K006045/1, NE/K006045/1
- RHRoyal Holloway, University of London