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GEOMAR Library Ocean Research Information Access

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  • OceanRep  (4)
  • CLIVAR  (2)
  • IOP  (1)
  • Springer  (1)
  • Bornträger
  • 2000-2004  (2)
  • 1990-1994  (2)
  • 1
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    IOP
    In:  Reports on Progress in Physics, 55 . pp. 1-37.
    Publication Date: 2018-03-02
    Description: The authors aim to acquaint the reader with the current state of ocean circulation models, their ability to model the present climate state and its variability, and their major shortcomings and uncertainties. They limit the discussion to three-dimensional models of the physical system. They begin by describing the basic structure of circulation models, and discussing various problems with their implementation. They give a brief overview of the types of observational data in oceanography, and the ways in which the data are used. Some results from models of the wind-driven circulation are discussed, with particular emphasis on the dynamics of mesoscale eddies. Considerable progress has been made in understanding short-term variability associated with ENSO, and the authors describe ocean-atmosphere interactions in the tropics as well as results from coupled ocean-atmosphere models for ENSO variability. Models of the thermohaline circulation are described and some emerging ideas regarding long-term changes are given.
    Type: Article , PeerReviewed
    Format: text
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  • 2
    Publication Date: 2019-02-01
    Type: Article , NonPeerReviewed
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  • 3
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    CLIVAR
    In:  CLIVAR Exchanges, 26 (8 (2-3)). pp. 3-5.
    Publication Date: 2019-02-01
    Type: Article , NonPeerReviewed
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  • 4
    Publication Date: 2018-03-02
    Description: The dependence of results from coarse-resolution models of the North Atlantic circulation on the numerical advection algorithm is studied. In particular, the sensitivity of parameters relevant for climate simulations as e.g., meridional transport of mass and heat and main thermocline thickness is investigated. Three algorithms were considered: (a) a central difference scheme with constant values for horizontal and vertical diffusion, (b) an upstream scheme with no explicit diffusion, and (c) a flux-corrected transport (FCT) scheme with constant and strictly isopycnal diffusion. The temporal evolution of the three models on time scales of centuries is markedly different, the upstream scheme resulting in much shorter adjustment time whereas the central difference scheme is slower and controlled by vertical diffusion rather than advection. In the steady state, the main thermocline structure is much less diffusive in the FCT calculation which also has much lower heat transport. Both horizontal circulation and overturning in the meridional-vertical plane are strongest in the upstream-model. The results are discussed in terms of the effective vertical (diapycnal) mixing in the different models. A significant increase in vertical resolution would be required to eliminate the high sensitivity due to the numerical algorithms, and allow physically motivated mixing formulations to become effective.
    Type: Article , PeerReviewed
    Format: text
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