Response of a climate model to tidal mixing parameterization under present day and last glacial maximum conditions
Weaver, Andrew J.
Jayne, Steven R.
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Experiments with a climate model were conducted under present day and last glacial maximum conditions in order to examine the model’s response to a vertical mixing scheme based on internal tide energy dissipation. The increase in internal tide energy flux caused by a 120 m reduction in sea level had the expected effect on diffusivity values, which were higher under lower sea level conditions. The impact of this vertical diffusivity change on the Atlantic meridional overturning is not straightforward and no clear relationship between diffusivity and overturning is found. There exists a weak positive correlation between overturning and changes to the power consumed by vertical mixing. Most of the climatic response generated by sea level change was not related to alterations in the internal tide energy flux but rather to the direct change in sea level itself.
Author Posting. © Elsevier B.V., 2007. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Ocean Modelling 19 (2007): 125-137, doi:10.1016/j.ocemod.2007.06.009.
Suggested CitationPreprint: Montenegro, Álvaro, Eby, Michael, Weaver, Andrew J., Jayne, Steven R., "Response of a climate model to tidal mixing parameterization under present day and last glacial maximum conditions", 2007-06-27, https://doi.org/10.1016/j.ocemod.2007.06.009, https://hdl.handle.net/1912/2028
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