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The study demonstrates that anincompatibility between a surface temperature climatology and a given oceanmodel, into which the climatology is assimilated via Haney restoration, cancause model ocean climate drift and interdecadal oscillations when the ocean isswitched to a weaker restoration. This is made using an idealized Atlantic Oceanmodel driven by thermal and wind forcing only. Initially, the temperatureclimatology is forcefully assimilated into the model, and an implied heat fluxfield is diagnosed. During this stage any incompatibility is suppressed. Therestoring boundary condition is then switched to a new forcing consisting of apart of the diagnosed flux and a part of the restoring forcing in such a waythat at the moment of the switching the heat flux is identical to that prior tothe switching. Under this new forcing condition, the incompatibility becomesmanifest, causing changes in convection patterns, and producing drift andinterdecadal oscillations. The mechanisms are described

Effects of convection instability due to incompatibility between ocean dynamics and surface forcings