{"database":"biostudies-literature","file_versions":[],"scores":null,"additional":{"omics_type":["Unknown"],"volume":["9"],"submitter":["Prakash A"],"pubmed_abstract":["Three-dimensional numerical simulation of circulation in fjords hosting marine-terminating ice shelves is challenging because of the complexity of processes involved in such environments. This often requires a comprehensive model setup. The following elements are needed: bathymetry (usually unknown beneath the glacier tongue), ice shelf draft (impacting water column thickness), oceanographic state (including tidal elevation, salinity, temperature and velocity of the water masses), sea ice and atmospheric forcing. Moreover, a high spatial resolution is needed, at least locally, which may be augmented with a coarser and computationally cheaper (nested) model that provides sufficiently realistic conditions at the boundaries. Here, we describe procedures to systematically create such a setup t"],"journal":["MethodsX"],"pagination":["101668"],"full_dataset_link":["https://www.ebi.ac.uk/biostudies/studies/S-EPMC8980345"],"repository":["biostudies-literature"],"pubmed_title":["A nested high-resolution unstructured grid 3-D ocean-sea ice-ice shelf setup for numerical investigations of the Petermann ice shelf and fjord."],"pmcid":["PMC8980345"],"pubmed_authors":["Hattermann T","Prakash A","Zhou Q","Bao W","Kirchner N","Graversen R"],"additional_accession":[]},"is_claimable":false,"name":"A nested high-resolution unstructured grid 3-D ocean-sea ice-ice shelf setup for numerical investigations of the Petermann ice shelf and fjord.","description":"Three-dimensional numerical simulation of circulation in fjords hosting marine-terminating ice shelves is challenging because of the complexity of processes involved in such environments. This often requires a comprehensive model setup. The following elements are needed: bathymetry (usually unknown beneath the glacier tongue), ice shelf draft (impacting water column thickness), oceanographic state (including tidal elevation, salinity, temperature and velocity of the water masses), sea ice and atmospheric forcing. Moreover, a high spatial resolution is needed, at least locally, which may be augmented with a coarser and computationally cheaper (nested) model that provides sufficiently realistic conditions at the boundaries. Here, we describe procedures to systematically create such a setup t","dates":{"release":"2022-01-01T00:00:00Z","publication":"2022","modification":"2025-04-26T13:12:03.679Z","creation":"2025-04-06T14:08:29.045Z"},"accession":"S-EPMC8980345","cross_references":{"pubmed":["35392103"],"doi":["10.1016/j.mex.2022.101668"]}}