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Sökning: L773:1814 9340 OR L773:1814 9359 > A Last Glacial Maxi...

A Last Glacial Maximum world-ocean simulation at eddy-permitting resolution – Part 1: Experimental design and basic evaluation

Ballarotta, Maxime, 1984- (författare)
Stockholms universitet,Meteorologiska institutionen (MISU)
Brodeau, Laurent (författare)
Stockholms universitet,Meteorologiska institutionen (MISU)
Brandefelt, Jenny (författare)
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Lundberg, Peter (författare)
Stockholms universitet,Meteorologiska institutionen (MISU)
Döös, Kristofer (författare)
Stockholms universitet,Meteorologiska institutionen (MISU)
visa färre...
 (creator_code:org_t)
Copernicus GmbH, 2013
2013
Engelska.
Ingår i: Climate of the Past Discussions. - : Copernicus GmbH. - 1814-9340 .- 1814-9359. ; 9, s. 297-328
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Most state-of-the-art climate models include a coarsely resolved oceanic compo- nent, 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, ∼26500 to 19000yr 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. Be- fore 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. 

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)

Nyckelord

atmosfärvetenskap och oceanografi
Atmospheric Sciences and Oceanography

Publikations- och innehållstyp

ref (ämneskategori)
art (ämneskategori)

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