R.W. Stewart |
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Authors: | Blyth Hughes |
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Institution: | 1. KNMI , De Bilt, The Netherlands;2. Royal Netherlands Meteorological Institute , P.O. Box 201, De Bilt, 3730 AE, The Netherlands;3. KNMI , De Bilt, The Netherlands |
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Abstract: | Abstract The physical mechanism that causes an interdecadal oscillation in a coarse resolution sector ocean model forced by mixed boundary conditions is studied. The oscillation is characterized by large fluctuations in convective activity and air/sea heat exchange on a decadal timescale. Changes in the subsurface temperature and surface salinity are essential for the existence of the oscillation. It is shown that a large part of these variations can be explained with the hypothesis of a constant ocean velocity field. This may easily lead to the erroneous conclusion that the oscillation is mainly a “nondynamical” phenomenon. In this paper it is demonstrated that the ocean dynamics play an essential role in explaining decadal oscillations. |
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