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The aqueous thermal boundary layer

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Abstract

This article reviews the available data, measurement techniques, and present understanding of the millimeter thick aqueous thermal boundary layer. A temperature difference between the surface and lower strata, δT, of the order of a few tenths to −1 °C have been observed. Techniques ranging from miniature mercury thermometers and electrical point sensors to optical interferometry and infrared radiometry have been employed. Many processes influence the temperature structure in this thin boundary layer. Among them are: the net upward heat flux due to evaporation and sensible heat transfer; infrared and solar radiation; and the turbulence near the interface due to wind mixing, wave breaking and current shear. Presence of solute and surface-active materials stimulate or dampen these mixing processes thereby influencing boundary-layer thickness and temperature structure.

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  1. Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA

    Kristina B. Katsaros

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Department of Atmospheric Sciences Contribution Number 354.

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Katsaros, K.B. The aqueous thermal boundary layer. Boundary-Layer Meteorol 18, 107–127 (1980). https://doi.org/10.1007/BF00117914

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