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J. A. Whitehead

-mass thickness in the ocean is intimately connected to the rate of mixing ( Huang 1999 ) and that quantification of mixing rate in the ocean is the subject of active research ( Polzin et al. 1996 , 1997 ). Our estimate of the amount of mixing in the experiment was made using data from controlled experiments of undermixed exchange flow ( Timmermans 1998 ). We estimate that the mixing in this experiment was less than half the rate needed for complete mixing. The slot experiment was heated from below and

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