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of strong thermocline and weak halocline, resulting in very little density contrast
betweentheuppercoldlayer,andtheunderlyingwarmlayer.Finally,Chapter9ex-
plores using a steady-state version of the IOBL model to “scale up” measurements
made in a particular location on a floe (often chosen for ease of deployment)to be
representativeoftheentirefloeorsurroundingregion.
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