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New option for a uniform thermal forcing anomaly
ISMIP6 ocean forcing is usually applied as a 2D field of thermal forcing. In experiments to date, thermal forcing anomalies for future warming have been 2D fields derived from climate models. This commit adds a simple option to add a uniform thermal forcing anomaly everywhere. The anomaly is added to the background thermal forcing field. To apply this option, the user sets thermal_forcing_anomaly to a nonzero value (in deg C) in the [parameters] section of the config file. Optionally, the forcing can be phased in linearly by setting the parameter thermal_forcing_anomaly_timescale to a nonzero value in the config file. For example, a timescale of 100 years means that after 50 years, only half the full anomaly is applied. In the config file, the user should also set the starting time (in years) for applying the anomaly, if different from 0. For example, if the anomaly is applied starting in year 1950, set thermal_forcing_anomaly_tstart = 1950. (Assuming that the starting time for the anomaly is equal to the time in the input file does not work for restart runs, since the model tstart variable is then read from the restart time slice, not the initial input file.) I tested the new option in 550-year experiments with anomalies of 1 C and 2 C, to identify the regions most sensitive to a given increase in thermal forcing.
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