Abstract
By measuring the time rate of change of temperature in the upper 65 m of the sea at night with a precision sounding device, the amount of heat transported upward at various depths and through the sea surface as a function of time during the night was determined. The heat flux through any surface of depth z was given by e−αt (1−Az⅔) for z
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CITATION STYLE
APA
Kaiser, J. A. C., & Williams, K. G. (1974). Measurements of the Vertical Heat Flux in the Upper Ocean Layer. Journal of Physical Oceanography, 4(2), 137–144. https://doi.org/10.1175/1520-0485(1974)004<0137:motvhf>2.0.co;2
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