I have a couple of questions about using CMIP6 anomaly forcing. I have switched from the default (CMIP5 era?) anomaly forcing to the CMIP6 forcing referenced in the documentation, e.g. /glade/p/cesmdata/cseg/inputdata/atm/datm7/anomaly_forcing/CMIP6-SSP1-2.6/. These files don't seem to have a dedicated domain file but work with the default domain file (/glade/p/cesmdata/cseg/inputdata/atm/datm7/anomaly_forcing/domain.permafrostRCN). However, there are no U or V wind files for any SSP. Should I omit wind when using CMIP6 anomaly forcing or is there another version of these files that includes wind files?
Second, according to the anomaly files the CMIP6 anomaly forcing uses 2000-2014 as a reference, while the older default files use 2001-2013. Is is important to match the climate cycling (DATM_CLMNCEP_YR_START & DATM_CLMNCEP_YR_END) with these years exactly or is safe to use a subset of these years? I can't tell whether underlying historical climatology is being used in a detrended form to only provide the variance properties or if the anomaly is calculated against specific years of raw data. If the latter changing the years for the cycling would introduce a bia.
As a side note I had to convert the CMIP6 anomaly files to netCDF5 to get simulations to run, which is part of why I wonder if I don't have the latest version.
Second, according to the anomaly files the CMIP6 anomaly forcing uses 2000-2014 as a reference, while the older default files use 2001-2013. Is is important to match the climate cycling (DATM_CLMNCEP_YR_START & DATM_CLMNCEP_YR_END) with these years exactly or is safe to use a subset of these years? I can't tell whether underlying historical climatology is being used in a detrended form to only provide the variance properties or if the anomaly is calculated against specific years of raw data. If the latter changing the years for the cycling would introduce a bia.
As a side note I had to convert the CMIP6 anomaly files to netCDF5 to get simulations to run, which is part of why I wonder if I don't have the latest version.