Campaign facets:
model_version: origin/maint-1.2 (v1 Cryosphere campaign branch) more info needed?
campaign: Cryosphere
Science_driver
20190306.A_WCYCL1850-DIB-ISMF_CMIP6.ne30_oECv3wLI.edison
experiment:: Within global, coupled ESM simulations, improve our understanding for (1) how global and regional climate factors control Antarctic sub-ice shelf melt rates and (2) how realistic, explicitly resolve sub-ice shelf melt rates impact regional and global climate. ** draft statement **
20190923.GMPAS-IAF.T62_oEC60to30v3wLI.cori-knl
Low-resolution, data-atmosphere (CORE-IAF forcing), active ocean and ice control run with standard (data) runoff forcing for S. Ocean freshwater fluxes
20190225.GMPAS-DIB-IAF-ISMF.T62_oEC60to30v3wLI.cori-knl
Low-resolution, data-atmosphere (CORE-IAF forcing) with CORE S. Ocean freshwater flux fields replaced by data iceberg (DIB) climatology and explicitly resolved ice shelf melt fluxes (ISMF)
20190430.A_WCYCL1850-DIB-ISMF_CMIP6.ne30_oECv3wLI.control.cori-knl
experiment:
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Low-resolution, fully coupled, control run with standard runoff treatment for S. Ocean freshwater fluxes (i.e., based on snowcapping)
20190306.A_WCYCL1850-DIB-ISMF_CMIP6.ne30_oECv3wLI.
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experiment:
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edison
Low-resolution, fully coupled, with data iceberg (DIB) climatology and explicitly resolved ice shelf melt fluxes (ISMF) replacing snowcapping-based fluxes
20190819.GMPAS-DIB-IAF-ISMF.T62_oEC60to30v3wLI.cori-knl
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experiment:
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.testNewGM
same as 20190225.GMPAS-DIB-IAF-ISMF.T62_oEC60to30v3wLI.cori-knl
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experiment:
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above but using newly tuned, 3d GM parameterization ** note atmos degradation / change here due to unintentional incorporation of CLUB v2 **
20191018.A_WCYCL1850-DIB-ISMF_CMIP6.ne30_oECv3wLI.cori-knl.testNewGM
experiment:same as 20190306.A_WCYCL1850-DIB-ISMF_CMIP6.ne30_oECv3wLI.edison above but using newly tuned, 3d GM parameterization ** note atmos degradation / change here due to unintentional incorporation of CLUB v2 **