On production and dissipation of thermal variance in the oceans
On production and dissipation of thermal variance in the oceans
Date
1980-11
Authors
Joyce, Terrence M.
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DOI
10.1575/1912/9596
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Keywords
Ocean-atmosphere interaction
Abstract
An integral relationship is derived expressing the total dissipation of thermal variance by oceanic
microstructure in terms of the large-scale forcing at the ocean surface by air/sea heat exchange. The
net heat gain by the ocean over warm water and heat loss over cold water is evaluated using zonal
averages of annual oceanic heat fluxes and temperatures between 60°N and 60°S. If thermal dissipation
occurs in the upper ocean, with a scale depth of 600 m, the average dissipation χ is estimated to be
10- 7 °C2 s- 1. This value compares favorably with published observations of oceanic microstructure
dissipation. The prediction is independent of any dynamical model of turbulent cascade from large to
small scales in the ocean.
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Also published as: Journal of Physical Oceanography (1980) 10: 460-463
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Joyce, T. M. (1980). On production and dissipation of thermal variance in the oceans. Woods Hole Oceanographic Institution. https://doi.org/10.1575/1912/9596