I'm trying to run 1x and 4x CO2 experiments with CESM 1.1.1 at 0.9x1.25_gx1v6 resolution, but they both have a dramatic cooling in the first ~10-20 years. I've attached a timeseries of the global mean surface temperature with 1xCO2 in blue and 4xCO2 in red. I've also attached some net radiative flux variables. You'll notice the TOA net solar flux is different, but this seems to mostly be due to an increase in sea ice in the 1x CO2 simulation. The downwelling solar flux is identical in both runs.I'm guessing that my custom compset might be causing the problem, but I have no idea how. My custom compset file looks like this:I've also been thinking that this could just be because my initial conditions are from a different model configuration that runs warmer. However, when I look at the January sea-ice fraction, the sea-ice extends down to ~45N in the Pacific, which is pretty unrealistic.I also heard that it might be better to start as a hybrid using one of the "b40" runs as the intial condition, found here:https://svn-ccsm-inputdata.cgd.ucar.edu/trunk/inputdata/ccsm4_init/Someone also suggested it could be related to the use of 30 levels instead of 26?Any other ideas to explain this would be a huge help.
Thanks,
Walter
Thanks,
Walter