Articles | Volume 26, issue 13
https://doi.org/10.5194/acp-26-9509-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-26-9509-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A multi-model approach to constrain the atmospheric hydrogen budget
Srinath Krishnan
CORRESPONDING AUTHOR
CICERO Center for International Climate Research, Oslo, Norway
Ragnhild Bieltvedt Skeie
CICERO Center for International Climate Research, Oslo, Norway
Øivind Hodnebrog
CICERO Center for International Climate Research, Oslo, Norway
Gunnar Myhre
CICERO Center for International Climate Research, Oslo, Norway
Maria Sand
CICERO Center for International Climate Research, Oslo, Norway
Marit Sandstad
CICERO Center for International Climate Research, Oslo, Norway
Hannah Bryant
School of Geosciences, University of Edinburgh, Edinburgh, UK
Didier A. Hauglustaine
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France
Fabien Paulot
Geophysical Fluid Dynamics Laboratory, National Oceanic & Atmospheric Administration, Princeton, NJ, USA
Michael Prather
Earth System Science Department, University of California Irvine, Irvine, CA, USA
David Stevenson
School of Geosciences, University of Edinburgh, Edinburgh, UK
Data sets
CESM2-WACCM data for A multi-model approach to constrain the atmospheric hydrogen budget Øivind Hodnebrog https://doi.org/10.11582/2025.98qdasg2
Model code and software
ciceroOslo/simpleH2: v1.0.1 (v1.0.1) R. B. Skeie et al. https://doi.org/10.5281/zenodo.20643957
Short summary
Hydrogen (H2) is an indirect greenhouse gas that can affect climate through chemical reactions in the atmosphere. To better understand this impact, it is important to constrain the sources and sinks of hydrogen. Using a suite of three-dimensional and one-dimensional models, we find that atmospheric production of hydrogen is 37–60 Tg/yr and that the geological source of H2 is much smaller than suggested. More field and isotopic measurements are needed to improve these estimates.
Hydrogen (H2) is an indirect greenhouse gas that can affect climate through chemical reactions...
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