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The idea that the cumulative action of centimeter-scale mixing affects the ocean's largest scales guides Mike Gregg's
research.Evolving technology now enables the mixing to be put into the context of the meter-to-kilometer-scale
processes directly producing it,such as internal waves,bottom and surface boundary layers,thermohaline staircases
and intrusions,and hydraulic responses to flow constrictions.Because large-scale models,particularly coupled climate
models,have grid scales vastly larger than those of the mixing and even of the intermediate-scale processes
producing it,it is a goal to always try to work toward parameterizations that can be used in these models.
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Annual review of marine scienceno. 1 (2017): 443-473
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