EGU26-18139, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-18139
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Friday, 08 May, 10:45–12:30 (CEST), Display time Friday, 08 May, 08:30–12:30
 
Hall X5, X5.120
Interactive Simulation of Methane and Hydrogen Soil Deposition Using the Newly Implemented BIODEP Submodel of the ECHAM5/MESSy Atmospheric Chemistry Model (EMAC) v2.55
Anna Martin1, Klaus Klingmüller1, Benedikt Steil1, Sergey Gromov1, Yu-Ri Lee2, Dong Yeong Chang2, Nic Surawski4, Jos Lelieveld1,5, Sujong Jeong3, and Andrea Pozzer1,5
Anna Martin et al.
  • 1Max-Planck-Insitit for Chemistry, Atmospehric Chemistry, Germany (a.martin@mpic.de)
  • 2Environmental Planning Institute, Seoul National University, Seoul, 08826, Republic of Korea
  • 3Department of Environmental Management, Graduate School of Environmental Studies, Seoul National University, Seoul, 08826, Republic of Korea
  • 4Centre for Green Technology, University of Technology Sydney, Gadigal Country, Ultimo NSW 2007, Australia
  • 5The Cyprus Institute, Climate and Atmosphere Research Center, Nicosia, 1645, Cyprus
Methane (CH₄) and molecular hydrogen (H₂) are key components of atmospheric composition with important implications for climate processes. Methane acts as a strong greenhouse gas, whereas hydrogen affects climate indirectly by modifying the atmosphere’s oxidative capacity. The primary atmospheric removal pathway for methane is its reaction with hydroxyl radicals, while hydrogen is mainly removed through microbial consumption in soils. In addition to atmospheric oxidation, roughly 6% of global methane emissions are taken up by soils, making this pathway a meaningful contributor to the overall methane budget. The efficiency of soil uptake depends on a range of environmental and soil-related factors, including soil texture, temperature, moisture content, and -for methane- nitrogen availability. Accurately representing these controls requires an integrated description of atmospheric conditions alongside land surface characteristics and soil hydrological processes.
In this work, we present BIODEP, a newly developed biogenic deposition module implemented within the Modular Earth Submodel System (MESSy). BIODEP is coupled to the ECHAM5/MESSy atmospheric chemistry model (EMAC) and the JSBACH land surface and vegetation model, which includes a detailed five-layer soil hydrology scheme. The performance of the model including the newly implemented BIODEP submodel is evaluated by comparing simulated methane and hydrogen atmospheric mixing ratios with measurements from more than 50 stations of the NOAA GML Carbon Cycle Cooperative Global Air Sampling Network covering the period 2009–2019. In addition, the column-averaged methane mixing ratio is compared with observations from the Greenhouse Gases Observing Satellite (GOSAT). For present-day conditions, the model captures observed spatial distributions and seasonal variability of soil uptake fluxes.
By explicitly connecting soil characteristics with meteorological drivers and atmospheric composition, BIODEP enhances EMAC’s capability to represent trace gas dynamics across a range of climate conditions. This development advances the understanding of soil–atmosphere exchange mechanisms and provides a robust modeling framework for assessing future methane and hydrogen cycles, which is essential for climate mitigation strategies and the planning of a sustainable hydrogen economy.

How to cite: Martin, A., Klingmüller, K., Steil, B., Gromov, S., Lee, Y.-R., Chang, D. Y., Surawski, N., Lelieveld, J., Jeong, S., and Pozzer, A.: Interactive Simulation of Methane and Hydrogen Soil Deposition Using the Newly Implemented BIODEP Submodel of the ECHAM5/MESSy Atmospheric Chemistry Model (EMAC) v2.55, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-18139, https://doi.org/10.5194/egusphere-egu26-18139, 2026.