Articles | Volume 11, issue 6
https://doi.org/10.5194/gmd-11-2009-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-11-2009-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Model description paper
| 
04 Jun 2018
Model description paper |
| 04 Jun 2018
Soil Methanotrophy Model (MeMo v1.0): a process-based model to quantify global uptake of atmospheric methane by soil
Fabiola Murguia-Flores
CORRESPONDING AUTHOR
School of Geographical Sciences, University of Bristol, Bristol, BS8
1SS, UK
Sandra Arndt
School of Geographical Sciences, University of Bristol, Bristol, BS8
1SS, UK
current address: Department of Geosciences, Environment and Society, Université
Libre de Bruxelles, Brussels, Belgium
Anita L. Ganesan
School of Geographical Sciences, University of Bristol, Bristol, BS8
1SS, UK
Guillermo Murray-Tortarolo
Catedra CONACyT comisionado al Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autonoma de Mexico, Morelia, Mexico
Edward R. C. Hornibrook
School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ,
UK
current address: Earth, Environmental and Geographic Sciences, The University of
British Columbia, Okanagan Campus, Kelowna, BC, V1V 1V7, Canada
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- Country-level methane emissions and their sectoral trends during 2009–2020 estimated by high-resolution inversion of GOSAT and surface observations R. Janardanan et al. 10.1088/1748-9326/ad2436
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- Modelling alternative harvest effects on soil CO2 and CH4 fluxes from peatland forests X. Li et al. 10.1016/j.scitotenv.2024.175257
- Does forest management affect the magnitude and direction of the afforestation effect on soil methane fluxes? A meta-analysis G. Gatica et al. 10.1016/j.foreco.2022.120009
- Consumption of atmospheric methane by soil in a lowland broadleaf mixed forest J. DUŠEK et al. 10.17221/183/2018-PSE
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- Soil organic carbon is a key determinant of CH4 sink in global forest soils J. Lee et al. 10.1038/s41467-023-38905-8
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- The Global Methane Budget 2000–2017 M. Saunois et al. 10.5194/essd-12-1561-2020
- The impact of spatially varying wetland source signatures on the atmospheric variability ofδD-CH4 A. Stell et al. 10.1098/rsta.2020.0442
- Attribution of the accelerating increase in atmospheric methane during 2010–2018 by inverse analysis of GOSAT observations Y. Zhang et al. 10.5194/acp-21-3643-2021
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- Stimulated or Inhibited Response of Methane Flux to Nitrogen Addition Depends on Nitrogen Levels R. Chang et al. 10.1029/2021JG006600
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- The paradox of assessing greenhouse gases from soils for nature-based solutions R. Vargas & V. Le 10.5194/bg-20-15-2023
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- East Asian methane emissions inferred from high-resolution inversions of GOSAT and TROPOMI observations: a comparative and evaluative analysis R. Liang et al. 10.5194/acp-23-8039-2023
- Inverse modeling of 2010–2022 satellite observations shows that inundation of the wet tropics drove the 2020–2022 methane surge Z. Qu et al. 10.1073/pnas.2402730121
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- On Upscaling of Soil Microbial Processes and Biogeochemical Fluxes From Aggregates to Landscapes A. Ebrahimi & D. Or 10.1029/2017JG004347
- ESA CCI Soil Moisture for improved Earth system understanding: State-of-the art and future directions W. Dorigo et al. 10.1016/j.rse.2017.07.001
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Short summary
Soil bacteria known as methanotrophs are the only biological sink for atmospheric methane (CH4). Their activity depends on climatic and edaphic conditions, thus varies spatially and temporarily. Based on this, we developed a model (MeMo v1.0) to assess the global CH4 consumption by soils. The global CH4 uptake was 33.5 Tg CH4 yr-1 for 1990–2009, with an increasing trend of 0.1 Tg CH4 yr-2. The regional analysis proved that warm and semiarid regions represent the most efficient CH4 sink.
Soil bacteria known as methanotrophs are the only biological sink for atmospheric methane (CH4)....
