Articles | Volume 14, issue 6
Geosci. Model Dev., 14, 3603–3631, 2021
Geosci. Model Dev., 14, 3603–3631, 2021

Model description paper 15 Jun 2021

Model description paper | 15 Jun 2021

Model of Early Diagenesis in the Upper Sediment with Adaptable complexity – MEDUSA (v. 2): a time-dependent biogeochemical sediment module for Earth system models, process analysis and teaching

Guy Munhoven


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Guy Munhoven on behalf of the Authors (21 Apr 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (28 Apr 2021) by Sandra Arndt
Short summary
Sea-floor sediments play an important role in biogeochemical cycling of elements (e.g. carbon, silicon, nutrients) in the ocean. Realistic sediment modules are, however, not yet commonly used in global ocean biogeochemical models. Here we present MEDUSA, a model of the processes taking place in the surface sea-floor sediments which control the interaction between the sediments and the ocean. MEDUSA can be configured to meet the exact needs of any given ocean biogeochemical model.