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Free Content Impacts on the global ocean circulation from vertical mixing and a collapsing ice sheet

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The current view of the global meridional overturning circulation (MOC) is one where the Atlantic is a dominant basin for deep water formation, but with the potential for bipolar seesaws between the Southern Ocean and the North Atlantic during catastrophic freshening events in either hemisphere. Here we investigate the stability of this paradigm through the response of an intermediate complexity coupled climate model, set in an oceanically more sensitive glacial configuration, to variation in the vertical mixing rates. It is found that the convective basin is set by the upper ocean diffusivity, with higher such diffusivities leading to a Pacific-dominated MOC. The upper ocean diffusivity is found to have a larger impact on the MOC than catastrophic flood events. It is known that deep ocean mixing rates were enhanced during glacial periods due to greater deep ocean tidal dissipation in the shallower oceans, with less extensive continental shelves. It is hypothesized that, combined with modified atmospheric states, there has been potential for the MOC to significantly alter between different glacial periods.

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Document Type: Research Article

Publication date: March 1, 2011

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  • The Journal of Marine Research, one of the oldest journals in American marine science, publishes peer-reviewed research articles covering a broad array of topics in physical, biological and chemical oceanography. Articles that deal with processes, as well as those that report significant observations, are welcome. Biological studies involving coupling between ecological and physical processes are preferred over those that report systematics. The editors strive always to serve authors and readers in the academic oceanographic community by publishing papers vital to the marine research in the long and rich tradition of the Sears Foundation for Marine Research. We welcome you to the Journal of Marine Research.
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