{"@context":{"content":"http://purl.org/rss/1.0/modules/content/","dc":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","og":"http://ogp.me/ns#","rdfs":"http://www.w3.org/2000/01/rdf-schema#","sioc":"http://rdfs.org/sioc/ns#","sioct":"http://rdfs.org/sioc/types#","skos":"http://www.w3.org/2004/02/skos/core#","xsd":"http://www.w3.org/2001/XMLSchema#","owl":"http://www.w3.org/2002/07/owl#","rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","rss":"http://purl.org/rss/1.0/","site":"https://osprey.bco-dmo.org/ns#","odo":"http://ocean-data.org/schema/","emo":"http://ocean-data.org/schema/entity-matching#","bibo":"http://purl.org/ontology/bibo/","crypto":"http://id.loc.gov/vocabulary/preservation/cryptographicHashFunctions/","bcodmo":"http://lod.bco-dmo.org/id/","tw":"http://tw.rpi.edu/schema/","dcat":"http://www.w3.org/ns/dcat#","time":"http://www.w3.org/2006/time#","geo":"http://www.w3.org/2003/01/geo/wgs84_pos#","geosparql":"http://www.opengis.net/ont/geosparql#","sf":"http://www.opengis.net/ont/sf#","void":"http://rdfs.org/ns/void#","sd":"http://www.w3.org/ns/sparql-service-description#","dctype":"http://purl.org/dc/dcmitype/","prov":"http://www.w3.org/ns/prov#","schema":"http://schema.org/","geolink":"http://schema.geolink.org/1.0/base/main#","spdx":"http://spdx.org/rdf/terms#","bcodmo_vocab":"http://schema.bco-dmo.org/"},"@id":"http://lod.bco-dmo.org/id/dataset/706167#graph","@graph":[{"http://lod.bco-dmo.org/id/dataset/706167":{"@id":"http://lod.bco-dmo.org/id/dataset/706167","@type":["http://ocean-data.org/schema/DeploymentDatasetCollection","http://www.w3.org/ns/dcat#Dataset","http://ocean-data.org/schema/Dataset"],"http://ocean-data.org/schema/hasAcquisitionDescription":[{"@value":"<div><p>All experiments were performed\u00a0using the MIT General Circulation Model (MITgcm) [Marshall et al., 1997a, b]. The model was configured to allow non-hydrostatic dynamics to explicitly resolve deep convection, and the set-up was modified from Jones and Marshall [1993]. The model domain was a box with periodic boundary conditions in the x\u00a0and y\u00a0directions of 32 x 32 km with a horizontal\u00a0resolution of 250 m. The box had a uniform depth of 2 km with 41 z-levels with increasing thickness\u00a0from 10 m at\u00a0surface\u00a0to 100 m near the bottom. The linear equation of state was\u00a0used throughout this study. 16 sensitivity experiments were designed to explore the behavior of oxygen uptake during the deep convection events under different cooling conditions. Two validation runs were also applied by forcing the model using observational data from Argo <a href=\"http://www.argo.net/\">(http://www.argo.net/</a>). Detailed information about all simulations can be found in Sun et al [2017]. In this data set, horizontally averaged profiles and vertical transport of dissolved oxygen and temperature from all experiments are included. A few transect of dissolved oxygen and temperature are also included to demonstrate the evolution of the convection event.\u00a0<br />\n\u00a0<br />\n<strong>\u00a0References:\u00a0</strong></p>\n<p>Jones, H., and J. Marshall (1993), Convection with rotation in a neutral ocean: A study of open-ocean deep convection, Journal of Physical Oceanography, 23(6), 1009\u20131039.</p>\n<p>Marshall, J., C. Hill, L. Perelman, and A. Adcroft (1997a), Hydrostatic, quasi-hydrostatic, and\u00a0non-hydrostatic\u00a0ocean modeling, Journal of Geophysical Research: Oceans, 102(C3), 5733\u20135752.</p>\n<p>Marshall, J., A. Adcroft, C. Hill, L. Perelman, and C. Heisey (1997b), A finite-volume, incompressible\u00a0navier\u00a0stokes\u00a0model for studies of the ocean on parallel computers, Journal of Geophysical Research: Oceans, 102(C3), 5753\u20135766.</p>\n<p>Sun, D., T. Ito and B. Annalisa, Oxygen flux and vertical transport during deep convection events,\u00a0submitted\u00a0to Global Biogeochemical Cycles.</p></div>","@type":"rdf:HTML"}],"http://ocean-data.org/schema/hasBriefDescription":[{"@value":"MITgcm model deep convection simulation output","@language":"en-US"}],"http://purl.org/dc/terms/description":[{"@value":"<div><p>This dataset includes deep convection simulation output from the MITgcm (MIT General Circulation Model). The data include profiles under different situations in an idealized domain. \u00a0The experiment was based on\u00a0winter Labrador Sea\u00a0conditions.</p>\n<p>Model output\u00a0is\u00a0available to download as MATLAB .mat files by clicking the \"Get Data\" link. \u00a0Each file includes the output of one run covering 90 days.<br />\n* Contents of .mat files described in \u00a0<a href=\"http://dmoserv3.whoi.edu/data_docs/IVOMLS/MITgcm/mat_file_variables.csv\" target=\"_blank\">mat_file_variables.csv</a></p></div>","@type":"rdf:HTML"}],"http://www.w3.org/2000/01/rdf-schema#label":[{"@value":"Deep convection simulation using MITgcm","@type":"xsd:string"}],"http://ocean-data.org/schema/hasProcessingDescription":[{"@value":"<div><p>Arithmetic means calculated using Matlab software.</p>\n<p>BCO-DMO Data Manager Processing notes:<br />\n27 Jun 2017: Metadata descriptions provided here are preliminary and have not yet been reviewed by the data contributor.<br />\n* model output files indexed with file sizes and download links added to the dataset.</p></div>","@type":"rdf:HTML"}],"http://purl.org/dc/terms/identifier":[{"@value":"706167","@type":"xsd:int"}],"http://purl.org/dc/terms/title":[{"@value":"Deep convection simulation using MITgcm"}],"http://purl.org/dc/terms/date":[{"@value":"2017-06-27T12:16:32-04:00","@type":"xsd:dateTime"}],"http://purl.org/dc/terms/created":[{"@value":"2017-06-27T12:16:32-04:00","@type":"xsd:dateTime"}],"http://purl.org/dc/terms/modified":[{"@value":"2023-07-07T16:10:26-04:00","@type":"xsd:dateTime"}],"http://rdfs.org/ns/void#inDataset":[{"@id":"http://www.bco-dmo.org/"}],"http://ocean-data.org/schema/namedGraph":[{"@value":"urn:bcodmo:dataset:706167","@type":"xsd:token"}],"http://ocean-data.org/schema/osprey_page":[{"@id":"https://osprey.bco-dmo.org/dataset/706167"}],"http://ocean-data.org/schema/identifier":[{"@id":"urn:bcodmo:osprey:v2:node:identifier:706167"}],"http://ocean-data.org/schema/datasetTitle":[{"@value":"Deep convection simulation from the MITgcm (MIT General Circulation Model) (IVOMLS project)","@language":"en-US"}],"http://ocean-data.org/schema/abstract":[{"@value":"","@language":"en-US"}],"http://purl.org/dc/terms/rights":[{"@id":"https://creativecommons.org/licenses/by/4.0/"}],"http://ocean-data.org/schema/deprecated":[{"@value":"false","@type":"xsd:boolean"}],"http://ocean-data.org/schema/spatialCoverage":[{"@id":"urn:bcodmo:dataset:706167:spatialCoverage"}],"http://purl.org/dc/terms/bibliographicCitation":[{"@value":"Ito, T., Bracco, A., Sun, D. 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