The following applies to analyses show in figures 02, 03, 04, 05, 06, 08, 13, 14, 16, 17, 18, 19, 20, 21, A1 and A2 and the creation of the section shown in figure 11. Variables from different experiments are named as follows : OJ ORCA025-JRA OJST ORCA025-JRA-strong OJO ORCA025-JRA-OMIP OJO2nd ORCA025-JRA-OMIP-2nd VC VIKING20X-CORE VJS VIKING20X-JRA-short VJL VIKING20X-JRA-long VJO VIKING20X-JRA-OMIP IJL INALT20-JRA-long CDFTOOLS are used to compute - AMOC fields in depth coordinates (cdfmoc) and density coordinates, here sigma2 (cdfmocsig) $CDFTOOLS/cdfmoc -v $IN_V -decomp -t $IN_T -u $IN_U -o $OUT $CDFTOOLS/cdfamocsig -v $IN_V -t $IN_T -r 2000 -isodep -o $OUT For AMOC calculations on the nest grid, a routine, only taking into account for the Atlantic subbasin is used (cdfamoc - included here) $CDFTOOLS/cdfamoc -v $IN_V -decomp -t $IN_T -u $IN_U -o $OUT - detrended SSH fields (cdfzeromean) The global mean SSH at each timestep is subtracted from the SSH-field to exclude the model-related drift prior to SSH-variance calculations; on the nest grid, the global mean SSH from the host grid is used for detrending: $CDFTOOLS/cdfglobalmean -f $IN -v sossheig -p T -zeromean -o $GLOBAL_MEAN_HOST -oz $ZOUT -surf $CDFTOOLS/cdfzeromean -f $IN -v sossheig -p T -zeromean -readmean $GLOBAL_MEAN_HOST -o $OUT -oz $ZOUT -surf (both routines, cdfglobalmean and cdfzeromean, included here) - non-zonal or non-meridional sections defined in text file "SECTION" (cdf_xtrax_brokenline) $CDFTOOLS/cdf_xtrac_brokenline -t $IN_T -u $IN_U -v $IN_V -f SECTION -vecrot -b $BAT -o $OUT SECTION are DS, FBC, sec53N, NBCsection_obs and additionally including adjustments necessary for the coarser ORCA025 grid, sec53N_O025 and NBCsection_obs_O025 - densities (cdfsig0) $CDFTOOLS/cdfsig0 -t $IN_T -o $OUT - EKE (cdfeke_KIEL - routine included here - based on CDFTOOLS-version 3.0) $CDFTOOLS/cdfeke_KIEL $IN_U $IN_V $IN_T -o $OU - fresh water content (cdffwc) $CDFTOOLS/cdffwc -s $IN_T -bv ARCTIC,SPG -o $OUT -ssh ferret is used to derive further quanities: - SSH variance based on 5-day averaged date using expression @var - transport integrations based on sigma0 criteria - time-filtering is applied by using the Hanning filter expression @shn (23 months for interannual, 119 months for pentadal) - linear trends are derived using regresst.jnl