Oceanic and atmospheric methane cycling in the cGENIE Earth system model – release v0.9.14

• Published in: Geoscientific Model Development 2020-11, Vol.13 (11), p.5687-5706
• Main Authors: Reinhard, Christopher T, Olson, Stephanie L, Kirtland Turner, Sandra, Pälike, Cecily, Kanzaki, Yoshiki, Ridgwell, Andy
• Format: Article
• Language: English
• Subjects: Anaerobic microorganisms; Analysis; Atmosphere; Atmospheric boundary layer; Atmospheric chemistry; Atmospheric methane; Biogeochemical cycle; Biogeochemical cycles; Biogeochemistry; Biosphere; Carbon; Carbon cycle; Climate; Cycles; Earth; Extrasolar planets; Flexibility; Gas hydrates; General circulation models; Humidity; Hydrates; Hydrogen; Mathematical models; Metabolism; Methane; Methanogenesis; Microorganisms; Numerical models; Ocean circulation; Oceans; Oxidation; Oxygen; Photochemistry; Physics; Physiological aspects; Simulation; Sulfur; Sulphur; Terrestrial environments; Terrestrial planets; Time dependence; Wetlands
• ISSN: 1991-9603; 1991-959X; 1991-962X; 1991-9603; 1991-962X
• DOI: 10.5194/gmd-13-5687-2020

The methane (CH4) cycle is a key component of the Earth system that links planetary climate, biological metabolism, and the global biogeochemical cycles of carbon, oxygen, sulfur, and hydrogen. However, currently lacking is a numerical model capable of simulating a diversity of environments in the ocean, where CH4 can be produced and destroyed, and with the flexibility to be able to explore not only relatively recent perturbations to Earth's CH4 cycle but also to probe CH4 cycling and associated climate impacts under the very low-O2 conditions characteristic of most of Earth's history and likely widespread on other Earth-like planets. Here, we present a refinement and expansion of the ocean–atmosphere CH4 cycle in the intermediate-complexity Earth system model cGENIE, including parameterized atmospheric O2–O3–CH4 photochemistry and schemes for microbial methanogenesis, aerobic methanotrophy, and anaerobic oxidation of methane (AOM). We describe the model framework, compare model parameterizations against modern observations, and illustrate the flexibility of the model through a series of example simulations. Though we make no attempt to rigorously tune default model parameters, we find that simulated atmospheric CH4 levels and marine dissolved CH4 distributions are generally in good agreement with empirical constraints for the modern and recent Earth. Finally, we illustrate the model's utility in understanding the time-dependent behavior of the CH4 cycle resulting from transient carbon injection into the atmosphere, and we present model ensembles that examine the effects of atmospheric pO2, oceanic dissolved SO42-, and the thermodynamics of microbial metabolism on steady-state atmospheric CH4 abundance. Future model developments will address the sources and sinks of CH4 associated with the terrestrial biosphere and marine CH4 gas hydrates, both of which will be essential for comprehensive treatment of Earth's CH4 cycle during geologically recent time periods.