The intrinsic depth of horizontal convection |
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Authors: | Chen Chen Wei Wang Dexing Wu |
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Institution: | (1) Graduate School of Bioresource and Bioenvironmental Sciences, Kyusyu University, Hakozaki 6-10-1, Higashi-ku, Fukuoka 812-8581, Japan;(2) Faculty of Agriculture, Kyushu University, Hakozaki 6-10-1, Higashi-ku, Fukuoka 812-8581, Japan |
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Abstract: | The mainstream depth of a return flow can be viewed as an intrinsic depth of horizontal convection. By using a theoretical
tube model combined with the application of the Maximum Entropy Production Principle (MaxEPP) in thermodynamics, the following
statements can be made. Under fixed external forcing, the system chooses a particular depth as the mainstream depth of its
return flow, the depth of which not only satisfies the maximum circulation rate and the maximum heat transport, but also satisfies
the maximum entropy production rate. A comparison between this intrinsic depth and the container height leads to the definition
of a relative partial and full-penetration pattern of the circulation. Moreover, this intrinsic depth is found to vary with
the external forcing; the regulation of this variation is related to the Modified Rayleigh number. |
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Keywords: | |
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