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- W4254307248 abstract "The authors report an interdecadal oscillation in a wind- and thermally-driven ocean general circulation model (OGCM). The oscillation is tantalizing in that it occurs under a relatively strong thermal damping (26.3 W m−2 K−1). Examinations involving a two-dimensional OGCM, a simple thermal ‘flip–flop’ model, and a three-dimensional OGCM with and without the nonlinear effect of temperature in the state equation of sea water demonstrate that the oscillation is not driven by mechanisms such as the so-called convective oscillator, or the advective overshooting oscillator. Instead, the oscillation is associated with the propagation of modelled long Rossby-waves with westward phase velocity. It is found that the north–south basin extent of the OGCM is an important factor; a larger north–south basin extent is conducive to the generation of thermal wind flows crucial for initiating the propagation of disturbances. The geophysical relevance of these results is discussed." @default.
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- W4254307248 date "1998-04-01" @default.
- W4254307248 modified "2023-10-09" @default.
- W4254307248 title "A thermal oscillation under a restorative forcing" @default.
- W4254307248 doi "https://doi.org/10.1256/smsqj.54706" @default.
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