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- W2155622670 startingPage "18011" @default.
- W2155622670 abstract "Experiments with a low resolution, multilayered model of the oceanic general circulation with wind and thermal forcing were carried out in order to identify processes controlling important aspects of the general circulation. Emphasis was placed on the sensitivity of the model's solution to the sea surface thermal boundary condition. For long restoring time scale, wind‐driven circulation dominated the solution, resembling the circulation in the North Pacific. For short restoring time scale, strong thermohaline circulation driven by deep water formed at high latitude dominated the solution, resembling the circulation in the North Atlantic. Accordingly, other aspects of the circulation, such as the baroclinic structure of the currents and the meridional mass flux partition, changed with the restoring time scale." @default.
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- W2155622670 date "1989-12-15" @default.
- W2155622670 modified "2023-09-26" @default.
- W2155622670 title "Sensitivity of a multilayered oceanic general circulation model to the sea surface thermal boundary condition" @default.
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- W2155622670 doi "https://doi.org/10.1029/jc094ic12p18011" @default.
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