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The Quest for Kρ—Preliminary Results from Direct Measurements of Turbulent Fluxes in the Ocean

ScholarsArchive at Oregon State University

Field Value
Title The Quest for Kρ—Preliminary Results from Direct Measurements of Turbulent Fluxes in the Ocean
Names Moum, J. N. (creator)
Date Issued 1990-12 (iso8601)
Abstract Simultaneous measurements of vertical velocity fluctuations, w′, and temperature fluctuations, T′, on scales of three-dimensional turbulence yield a direct measure of the turbulent heat flux, J[subscript]q. The scales contributing most significantly to J[subscript]q are tens of centimeters or about 10 times larger than the scales contributing to the turbulent kinetic energy dissipation for the data examined. A limited sample indicates that, instantaneously, J[subscript]q is almost as frequently positive (countergradient) as negative (downgradient). In contrast, instantaneous estimates of J[subscript]q from microstructure measurements of ϵ or χ are always, by definition, downgradient.
Genre Article
Identifier Moum, J. N., 1990: The Quest for Kρ—Preliminary Results from Direct Measurements of Turbulent Fluxes in the Ocean. J. Phys. Oceanogr., 20, 1980–1984.

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