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A model of the Earth's Dole effect

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Amplification of global warming through pH dependence of DMS production simulated with a fully coupled Earth system model

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Amplification of global warming through pH-dependence of DMS-production simulated with a fully coupled Earth system model

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Climate and carbon cycle changes from 1850 to 2100 in MPI-ESM simulations for the Coupled Model Intercomparison Project phase 5

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Developments in the MPI-M Earth System Model version 1.2 (MPI-ESM 1.2) and its response to increasing CO2

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Global ocean biogeochemistry model HAMOCC: Model architecture and performance as component of the MPI‐Earth system model in different CMIP5 experimental realizations

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Global warming amplified by reduced sulphur fluxes as a result of ocean acidification

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Impact of land-sea organic matter fluxes on the ocean biogeochemistry during the Last Deglaciation

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Incorporating a prognostic representation of marine nitrogen fixers into the global ocean biogeochemical model HAMOCC

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Incorporating the stable carbon isotope 13C in the ocean biogeochemical component of the Max Planck Institute Earth System Model

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Incorporating the stable carbon isotope ¹³C in the ocean biogeochemical component of the Max Planck Institute Earth System Model

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Light absorption by marine cyanobacteria affects tropical climate mean state and variability

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Light absorption by marine cyanobacteria affects tropical climate mean state and variability

Microstructure and composition of marine aggregates as co-determinants for vertical particulate organic carbon transfer in the global ocean

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Microstructure and composition of marine aggregates as co-determinants for vertical particulate organic carbon transfer in the global ocean

Ocean carbon cycle during the last deglaciation in the Max Planck Institute Earth System Model

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Oceanic CO2 outgassing triggered by terrestrial organic carbon fluxes during deglacial flooding

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Sensitivity of a coupled climate-carbon cycle model to large volcanic eruptions during the last millennium

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Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2

Testing global ocean carbon cycle models using measurements of atmospheric O2 and CO2 concentration

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The climate of a retrograde rotating Earth

The global ocean biogeochemistry model HAMOCC: Model architecture and performance as component of the MPI-earth system model in different CMIP5 experimental realizations

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Variations of ocean biogeochemistry in a transient deglacial simulation with MPI-ESM

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