" ; :contributor_url = "https://orcid.org/0000-0002-2747-8456" ; :realm = "ocean seaIce" ; :source = "NEMO/releases/release-3.6 revision r6721" ; :source_type = "VIKING20X.L46-KKG36107B details here: https://git.geomar.de/NEMO/EXP/VIKING20X.L46-KKG36107B" ; :acknowledgment = "The ocean model simulation was performed at the North German Supercomputing Alliance (HLRN). We thank the NEMO system team for support" ; :summary = "VIKING20X aims at hindcast simulations of Atlantic Ocean circulation variability on monthly to multi-decadal timescales and with a spatial resolution sufficient to capture mesoscale processes well into subarctic latitudes. VIKING20X is an expanded and updated version of the original VIKING20 model configuration, now covering the Atlantic from the Nordic Seas towards the southern tip of Africa with a 1/20 degree grid, nested into a global ocean-sea-ice model at 1/4 degree resolution. The applied atmospheric forcing JRA55-do (with -do- for -driving the ocean-) builds on the Japanese reanalysis product JRA-55 with improvements through the implementation of satellite and several other reanalysis products. All atmospheric forcing fields are available on a 1/2 degree horizontal grid at 3-hourly temporal resolution covering the period 1958 to 2019. JRA55-do will be continuously extended into the present at least until 2023. Along with the atmospheric fields, JRA55-do also provides an interannually varying daily river runoff field at 1/4 degree horizontal resolution, which includes freshwater fluxes from ice sheets. For Greenland, this even includes the enhanced observed melting of the past decades." ; :name = "VIKING20X.L46-KKG36107B_1d_19800101_19800131_grid_T.nc" ; :title = "VIKING20X-JRA-short: daily to multi-decadal ocean dynamics under JRA55-do atmospheric forcing" ; :history = "Fri Jul 28 11:23:21 2023: ncatted -O -a name,global,m,c,VIKING20X.L46-KKG36107B_1d_19800101_19800131_grid_T.nc -a title,global,m,c,VIKING20X-JRA-short: daily to multi-decadal ocean dynamics under JRA55-do atmospheric forcing -a cdm_data_type,global,m,c,grid -a pi,global,m,c,Klaus Getzlaff -a
-a pi_url,global,m,c,https://orcid.org/0000-0002-0347-7838 -a institution_id,global,m,c,https://ror.org/02h2x0161 -a institution,global,m,c,GEOMAR Helmholtz Centre for Ocean Research -a research_devision,global,m,c,Ocean Circulation and Climate Dynamics -a research_unit,global,m,c,Ocean Dynamics -a creator_name,global,m,c,Klaus Getzlaff -a
-a creator_url,global,m,c,https://orcid.org/0000-0002-0347-7838 -a project,global,m,c,RACE, iAtlantic -a references,global,m,c,Biastoch, A., Schwarzkopf, F. U., Getzlaff, K., Rühs, S., Martin, T., Scheinert, M., Schulzki, T., Handmann, P., Hummels, R., and Böning, C. W.: Regional imprints of changes in the Atlantic Meridional Overturning Circulation in the eddy-rich ocean model VIKING20X, Ocean Sci., 17, 1177-1211, https://doi.org/10.5194/os-17-1177-2021, 2021. -a metadata_link,global,m,c,https://www.wdc-climate.de/ui/entry?acronym=VIKING20XJRAshort -a keywords,global,m,c,OCEAN GENERAL CIRCULATION MODELS/(OGCM), REGIONAL OCEAN MODELS, ATMOSPHERIC/OCEAN INDICATORS, ATLANTIC OCEAN, WATER TEMPERATURE, THERMOHALINE CIRCULATION, OCEAN TEMPERATURE, OCEAN SALINITY, OCEAN OVERTURNING, OCEAN MIXED LAYER, OCEAN CURRENTS, OCEAN UPWELLING -a keywords_vocabulary,global,m,c,GCMD:GCMD Keywords -a license,global,m,c,CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/deed.en) -a date_created,global,m,c,2019-09-02 -a date_modified,global,m,c,2023-07-28 -a contributor_name,global,m,c,Franziska Schwarzkopf -a
-a contributor_url,global,m,c,https://orcid.org/0000-0002-2747-8456 -a realm,global,m,c,ocean seaIce -a source,global,m,c,NEMO/releases/release-3.6 revision r6721 -a source_type,global,m,c,VIKING20X.L46-KKG36107B details here: https://git.geomar.de/NEMO/EXP/VIKING20X.L46-KKG36107B -a acknowledgment,global,m,c,The ocean model simulation was performed at the North German Supercomputing Alliance (HLRN). We thank the NEMO system team for support -a summary,global,m,c,VIKING20X aims at hindcast simulations of Atlantic Ocean circulation variability on monthly to multi-decadal timescales and with a spatial resolution sufficient to capture mesoscale processes well into subarctic latitudes. VIKING20X is an expanded and updated version of the original VIKING20 model configuration, now covering the Atlantic from the Nordic Seas towards the southern tip of Africa with a 1/20 degree grid, nested into a global ocean-sea-ice model at 1/4 degree resolution. The applied atmospheric forcing JRA55-do (with -do- for -driving the ocean-) builds on the Japanese reanalysis product JRA-55 with improvements through the implementation of satellite and several other reanalysis products. All atmospheric forcing fields are available on a 1/2 degree horizontal grid at 3-hourly temporal resolution covering the period 1958 to 2019. JRA55-do will be continuously extended into the present at least until 2023. Along with the atmospheric fields, JRA55-do also provides an interannually varying daily river runoff field at 1/4 degree horizontal resolution, which includes freshwater fluxes from ice sheets. For Greenland, this even includes the enhanced observed melting of the past decades. /scratch/usr/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/WDCC/./grid_T/host/VIKING20X.L46-KKG36107B_1d_19800101_19800131_grid_T.nc\n", "Wed Jul 26 17:38:54 2023: ncrcat -O -F -7 -L 1 -d time_counter,1,31 VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T.nc /scratch/usr/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/WDCC/grid_T/host/VIKING20X.L46-KKG36107B_1d_19800101_19800131_grid_T.nc\n", "Tue Sep 3 12:28:06 2019: ncrcat -O -F -d time_counter,1,186 /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800101-19800119.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800120-19800207.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800208-19800226.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800227-19800316.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800317-19800404.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800405-19800423.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800424-19800512.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800513-19800531.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800601-19800619.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800620-19800708.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T.nc\n", "Tue Sep 3 05:40:18 2019: ncrcat /gfs1/work/shkifmkg/TDIR/STORE_VIKING20X.L46-KKG36107B_190903053230/tmp_re-chunk_1567481581467878220/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800101-19800119_1_1_100_100_l00001.nc /gfs1/work/shkifmkg/TDIR/STORE_VIKING20X.L46-KKG36107B_190903053230/tmp_re-chunk_1567481581467878220/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800101-19800119_1_1_100_100_l00002.nc 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/gfs1/work/shkifmkg/TDIR/STORE_VIKING20X.L46-KKG36107B_190903053230/tmp_re-chunk_1567481581467878220/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800101-19800119_1_1_100_100_l00018.nc /gfs1/work/shkifmkg/TDIR/STORE_VIKING20X.L46-KKG36107B_190903053230/tmp_re-chunk_1567481581467878220/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800101-19800119_1_1_100_100_l00019.nc /gfs1/work/shkifmkg/SDIR/VIKING20X.L46/VIKING20X.L46-KKG36107B-S/1d/grid_T_19800101_19800704/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800101-19800119.nc\n", "Tue Sep 3 05:33:01 2019: ncks -a -d time_counter,0,0,1 -7 -L 1 --cnk_dmn time,1 --cnk_dmn time_counter,1 --cnk_dmn z,1 --cnk_dmn depthu,1 --cnk_dmn depthv,1 --cnk_dmn depthw,1 --cnk_dmn deptht,1 --cnk_dmn x,100 --cnk_dmn y,100 VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800101-19800119.nc /gfs1/work/shkifmkg/TDIR/STORE_VIKING20X.L46-KKG36107B_190903053230/tmp_re-chunk_1567481581467878220/VIKING20X.L46-KKG36107B_1d_19800101_19800704_grid_T_19800101-19800119_1_1_100_100_l00001.nc" ; }