Dear All,
I am wondering about a strange jump in T2m over oceans at the beginning of 2017. From 2017 onward, T2M from CAMS is nearly equal to T2m from ERA5, but before 2017 they differ by up t several degrees:
Over land there is no such jump. I suppose that the SST used as the lower boundary condition has been changed, being different from that used in ERA5 before 2017.
More important than the source of the difference are the possible implication. Is the CAMS reanalysis compatible with ERA5 before 2017? Can I combine data from both reanalyses?
Best regards,
Andreas Sterl

