FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2078990018> ?p ?o ?g. }

• W2078990018 abstract "Abstract. Most state-of-the-art climate models include a coarsely resolved oceanic component, which has difficulties in capturing detailed dynamics, and therefore eddy-permitting/eddy-resolving simulations have been developed to reproduce the observed World Ocean. In this study, an eddy-permitting numerical experiment is conducted to simulate the global ocean state for a period of the Last Glacial Maximum (LGM, ~ 26 500 to 19 000 yr ago) and to investigate the improvements due to taking into account these higher spatial scales. The ocean general circulation model is forced by a 49-yr sample of LGM atmospheric fields constructed from a quasi-equilibrated climate-model simulation. The initial state and the bottom boundary condition conform to the Paleoclimate Modelling Intercomparison Project (PMIP) recommendations. Before evaluating the model efficiency in representing the paleo-proxy reconstruction of the surface state, the LGM experiment is in this first part of the investigation, compared with a present-day eddy-permitting hindcast simulation as well as with the available PMIP results. It is shown that the LGM eddy-permitting simulation is consistent with the quasi-equilibrated climate-model simulation, but large discrepancies are found with the PMIP model analyses, probably due to the different equilibration states. The strongest meridional gradients of the sea-surface temperature are located near 40° N and S, this due to particularly large North-Atlantic and Southern-Ocean sea-ice covers. These also modify the locations of the convection sites (where deep-water forms) and most of the LGM Conveyor Belt circulation consequently takes place in a thinner layer than today. Despite some discrepancies with other LGM simulations, a glacial state is captured and the eddy-permitting simulation undertaken here yielded a useful set of data for comparisons with paleo-proxy reconstructions." @default.
• W2078990018 created "2016-06-24" @default.
• W2078990018 creator A5017128759 @default.
• W2078990018 creator A5029805389 @default.
• W2078990018 creator A5046311656 @default.
• W2078990018 creator A5063554675 @default.
• W2078990018 creator A5090958422 @default.
• W2078990018 date "2013-01-18" @default.
• W2078990018 modified "2023-09-30" @default.
• W2078990018 title "A Last Glacial Maximum world-ocean simulation at eddy-permitting resolution – Part 1: Experimental design and basic evaluation" @default.
• W2078990018 cites W1504581063 @default.
• W2078990018 cites W1529264670 @default.
• W2078990018 cites W1662063040 @default.
• W2078990018 cites W1920243763 @default.
• W2078990018 cites W1964016826 @default.
• W2078990018 cites W1979156498 @default.
• W2078990018 cites W1983289295 @default.
• W2078990018 cites W1996766174 @default.
• W2078990018 cites W1999281562 @default.
• W2078990018 cites W2000766006 @default.
• W2078990018 cites W2001072306 @default.
• W2078990018 cites W2009412734 @default.
• W2078990018 cites W2032658276 @default.
• W2078990018 cites W2035888601 @default.
• W2078990018 cites W2042476750 @default.
• W2078990018 cites W2044130592 @default.
• W2078990018 cites W2055886783 @default.
• W2078990018 cites W2080987679 @default.
• W2078990018 cites W2086251236 @default.
• W2078990018 cites W2089476216 @default.
• W2078990018 cites W2094665897 @default.
• W2078990018 cites W2101005049 @default.
• W2078990018 cites W2112363056 @default.
• W2078990018 cites W2113090896 @default.
• W2078990018 cites W2114687263 @default.
• W2078990018 cites W2119620050 @default.
• W2078990018 cites W2125600063 @default.
• W2078990018 cites W2133050257 @default.
• W2078990018 cites W2133751091 @default.
• W2078990018 cites W2136645316 @default.
• W2078990018 cites W2137509798 @default.
• W2078990018 cites W2139143774 @default.
• W2078990018 cites W2150855373 @default.
• W2078990018 cites W2158626702 @default.
• W2078990018 cites W2332715557 @default.
• W2078990018 cites W4245105424 @default.
• W2078990018 doi "https://doi.org/10.5194/cpd-9-297-2013" @default.
• W2078990018 hasPublicationYear "2013" @default.
• W2078990018 type Work @default.
• W2078990018 sameAs 2078990018 @default.
• W2078990018 citedByCount "2" @default.
• W2078990018 countsByYear W20789900182013 @default.
• W2078990018 countsByYear W20789900182014 @default.
• W2078990018 crossrefType "posted-content" @default.
• W2078990018 hasAuthorship W2078990018A5017128759 @default.
• W2078990018 hasAuthorship W2078990018A5029805389 @default.
• W2078990018 hasAuthorship W2078990018A5046311656 @default.
• W2078990018 hasAuthorship W2078990018A5063554675 @default.
• W2078990018 hasAuthorship W2078990018A5090958422 @default.
• W2078990018 hasBestOaLocation W20789900181 @default.
• W2078990018 hasConcept C111368507 @default.
• W2078990018 hasConcept C114793014 @default.
• W2078990018 hasConcept C127313418 @default.
• W2078990018 hasConcept C132651083 @default.
• W2078990018 hasConcept C15739521 @default.
• W2078990018 hasConcept C168754636 @default.
• W2078990018 hasConcept C187599188 @default.
• W2078990018 hasConcept C188291805 @default.
• W2078990018 hasConcept C39432304 @default.
• W2078990018 hasConcept C49204034 @default.
• W2078990018 hasConcept C83002819 @default.
• W2078990018 hasConceptScore W2078990018C111368507 @default.
• W2078990018 hasConceptScore W2078990018C114793014 @default.
• W2078990018 hasConceptScore W2078990018C127313418 @default.
• W2078990018 hasConceptScore W2078990018C132651083 @default.
• W2078990018 hasConceptScore W2078990018C15739521 @default.
• W2078990018 hasConceptScore W2078990018C168754636 @default.
• W2078990018 hasConceptScore W2078990018C187599188 @default.
• W2078990018 hasConceptScore W2078990018C188291805 @default.
• W2078990018 hasConceptScore W2078990018C39432304 @default.
• W2078990018 hasConceptScore W2078990018C49204034 @default.
• W2078990018 hasConceptScore W2078990018C83002819 @default.
• W2078990018 hasLocation W20789900181 @default.
• W2078990018 hasLocation W20789900182 @default.
• W2078990018 hasOpenAccess W2078990018 @default.
• W2078990018 hasPrimaryLocation W20789900181 @default.
• W2078990018 hasRelatedWork W1586357844 @default.
• W2078990018 hasRelatedWork W1616279305 @default.
• W2078990018 hasRelatedWork W1983728093 @default.
• W2078990018 hasRelatedWork W2052922882 @default.
• W2078990018 hasRelatedWork W2058355572 @default.
• W2078990018 hasRelatedWork W2113163701 @default.
• W2078990018 hasRelatedWork W2127599527 @default.
• W2078990018 hasRelatedWork W2129629557 @default.
• W2078990018 hasRelatedWork W2955244819 @default.
• W2078990018 hasRelatedWork W4322767029 @default.
• W2078990018 isParatext "false" @default.
• W2078990018 isRetracted "false" @default.
• W2078990018 magId "2078990018" @default.
• W2078990018 workType "article" @default.