FN Archimer Export Format PT J TI FOCI-MOPS v1-integration of marine biogeochemistry within the Flexible Ocean and Climate Infrastructure version 1 (FOCI 1) Earth system model BT AF CHIEN, Chia-Te DURGADOO, Jonathan V. EHLERT, Dana FRENGER, Ivy KELLER, David P. KOEVE, Wolfgang KRIEST, Iris LANDOLFI, Angela PATARA, Lavinia WAHL, Sebastian OSCHLIES, Andreas AS 1:1;2:1,2;3:1;4:1;5:1;6:1;7:1;8:1,3;9:1;10:1;11:1,2; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:; C1 GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Düsternbrooker Weg 20, 24105 Kiel, Germany Kiel University, 24118 Kiel, Germany ISMAR-CNR, via Fosso del Cavaliere 100, 0133 Rome, Italy C2 IFM GEOMAR, GERMANY UNIV KIEL, GERMANY CNR ISMAR, ITALY IN DOAJ IF 5.1 TC 6 UR https://archimer.ifremer.fr/doc/00788/90000/95574.pdf https://archimer.ifremer.fr/doc/00788/90000/95575.pdf https://archimer.ifremer.fr/doc/00788/90000/95576.pdf https://archimer.ifremer.fr/doc/00788/90000/95577.pdf LA English DT Article CR BIOSOPE OISO - OCÉAN INDIEN SERVICE D'OBSERVATION BO L'Atalante AB The consideration of marine biogeochemistry is essential for simulating the carbon cycle in an Earth system model. Here we present the implementation and evaluation of a marine biogeochemical model, the Model of Oceanic Pelagic Stoichiometry (MOPS) in the Flexible Ocean and Climate Infrastructure (FOCI) climate model. FOCI-MOPS enables the simulation of marine biological processes, i.e. the marine carbon, nitrogen, and oxygen cycles with prescribed or prognostic atmospheric CO2 concentration. A series of experiments covering the historical period (1850-2014) were performed following the DECK (Diagnostic, Evaluation and Characterization of Klima) and CMIP6 (Coupled Model Intercomparison Project 6) protocols. Overall, modelled biogeochemical tracer distributions and fluxes, transient evolution in surface air temperature, air-sea CO2 fluxes, and changes in ocean carbon and heat contents are in good agreement with observations. Modelled inorganic and organic tracer distributions are quantitatively evaluated by statistically derived metrics. Results of the FOCI-MOPS model, including sea surface temperature, surface pH, oxygen (100-600 m), nitrate (0-100 m), and primary production, are within the range of other CMIP6 model results. Overall, the evaluation of FOCI-MOPS indicates its suitability for Earth climate system simulations. PY 2022 PD AUG SO Geoscientific Model Development SN 1991-959X PU Copernicus Gesellschaft Mbh VL 15 IS 15 UT 000834839600001 BP 5987 EP 6024 DI 10.5194/gmd-15-5987-2022 ID 90000 ER EF