For the ATMOS part of the project, a correction system was implemented in the Max-Planck
Institute Earth System Model in its low resolution version (MPI-ESM-LR), that was successfully
used in the Kiel
For the MODINI part, the MPI-ESM-LR was initialised for decadal retrospective forecasts
(hindcasts in the following) using windstress anomalies from reanalysis. This work was
published as part of an
Sensitivity experiments to investigate the role of local sea surface temperature pattern changes in shaping climate change in the North Atlantic sector. For details see Hand et al. (2018) ( https://doi.org/10.1007/s00382-018-4151-1 )