The thinness of oceanic temperature gradients Public Deposited

http://ir.library.oregonstate.edu/concern/defaults/j098zc40n

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  • A test of the scaling of the extent of the thinnest vertical temperature gradients, in the near-bottom boundary layer on the Oregon shelf, shows that the Batchelor wave number determines the cutoff wave number in vertical temperature gradient spectra. In combination with previous results, in other words, this test shows that the smallest scale at which significant temperature variance due to turbulence exists at any given point in the ocean is determined by the Batchelor scale, (vD²/ε)^(1/4), v being the kinematic viscosity, D the thermal diffusivity, and ε the kinetic energy dissipation per unit mass. Stress measurements in the viscous sublayer provide estimates of ε.
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  • Caldwell, D. R., Chriss, T. M., Newberger, P. A., & Dillon, T. M. (1981). The thinness of oceanic temperature gradients. Journal of Geophysical Research, 86(C5), 4290-4292.
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  • description.provenance : Made available in DSpace on 2010-09-29T18:52:35Z (GMT). No. of bitstreams: 1 Caldwell_et_al_JGR_1981.pdf: 205517 bytes, checksum: c20654b0d33f45c4c293c3b3d1ccc006 (MD5) Previous issue date: 1981-05-20
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