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  • 1
    Monograph available for loan
    Monograph available for loan
    Los Angeles : University of California, Department of Meteorology
    Associated volumes
    Call number: MOP 40322 / Mitte
    In: Numerical simulation of weather and climate : technical report, 9
    Type of Medium: Monograph available for loan
    Pages: 99 Seiten , Illustrationen
    Series Statement: Numerical simulation of weather and climate : technical report 9
    Language: English
    Branch Library: GFZ Library
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  • 2
    Publication Date: 2011-08-19
    Description: Anomalies in ocean surface temperature have been identified as possible causes of variations in the climate of particular seasons or as a source of interannual climatic variability, and attempts have been made to forecast seasonal climate by using ocean temperatures as predictor variables. However, the seasonal atmospheric response to ocean temperature anomalies has not yet been systematically investigated with nonlinear models. The present investigation is concerned with ten-year integrations involving a model of intermediate complexity, the Held-Suarez climate model. The calculations have been performed to investigate the changes in seasonal climate which result from a fixed anomaly imposed on a seasonally varying, global ocean temperature field. Part I of the paper provides a report on the results of these decadal integrations. Attention is given to model properties, the experimental design, and the anomaly experiments.
    Keywords: METEOROLOGY AND CLIMATOLOGY
    Type: Journal of the Atmospheric Sciences (ISSN 0022-4928); 41; 2605-261
    Format: text
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  • 3
    Publication Date: 2019-06-27
    Description: Oceanographic field measurements have revealed intense, transient mesoscale motions in many parts of the world ocean. The circulation of the western North Atlantic, considered in the present study as a rectangular basin, is simulated with a primitive equation model that has five levels and a horizontal grid size of 37 km. The model ocean is driven by a 2.5 gyre pattern of steady zonal wind stress and by a Newtonian-type surface heating. Two cases are considered: the first uses a Laplacian formulation for the subgrid-scale lateral diffusions of heat and momentum; the second uses a highly scale-selective biharmonic formulation for these diffusions. An analysis of the heat transport, in the biharmonic experiment, shows that the horizontal transport of heat by eddies is much larger than the subgrid-scale horizontal heat diffusion. In the Gulf Stream region, the eddy heat transport is comparable to the effect of a lateral diffusion coefficient of 10 to the 7th sq cm/s.
    Keywords: OCEANOGRAPHY
    Type: Journal of Physical Oceanography; 7; Mar. 197
    Format: text
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