Data for: Revisiting the modelled cloud radiative feedback on ENSO — the source of model uncertainty

These experiments are used to identify the origins of bias in the cloud radiative feedback on ENSO, including the SW feedback, vertical cloud cover anomalies, and cloud cover anomalies different levels. The results were equivalent to 10-member ensemble runs. We conducted four main sets of experiments, which started with the same ocean initial state (CESM_sst and MPI_sst), with four El Niño events (mpi El Niño, cesm El Niño,moderate El Niño and mega El Niño) we superimposed.