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In this report we set forth a simulation method for long-term simulations ofNorESM, the Norwegian Earth System Model. In this the sediment is repeatedlydecoupled and coupled to the ocean model (BLOM/iHAMOCC), a process called burstcoupling. Through this, the ocean (seawater and sediment) is brought into anapproximate steady state. We show that just the model has to run at least 50000yr to get in an approximate steady state. With burst coupling this can be donein a computationally reasonable time (wall time in the order of one week). Themethod can be used to generate the sediment over hundreds of thousands ofyears, so it is useful not only for present-day simulations but also forpaleo-climatological studies.

Long-term climate simulation in NorESM: burst-coupling the sediment in the BLOM/iHAMOCC ocean module