29 November 2016 Understanding of counter-gradient heat flux in lower atmosphere based on the second order RANS-approach
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Proceedings Volume 10035, 22nd International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics; 100355L (2016) https://doi.org/10.1117/12.2248144
Event: XXII International Symposium Atmospheric and Ocean Optics. Atmospheric Physics, 2016, Tomsk, Russian Federation
Abstract
The nonlocality of the mechanism of turbulent heat transfer in the atmospheric boundary layer over a rough surface manifests itself in the form of bounded areas of countergradient heat transfer, which are diagnosed from analysis of balance items in the transport equation for the variance of temperature fluctuations and from calculation of the coefficients of turbulent momentum and heat transfer invoking the model of gradient diffusion. It is shown that countergradient heat transfer in local regions is caused by turbulent diffusion or by the term of the divergence of triple correlation in the balance equation for the temperature variance.
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A. Kurbatskii, L. Kurbatskaya, "Understanding of counter-gradient heat flux in lower atmosphere based on the second order RANS-approach", Proc. SPIE 10035, 22nd International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, 100355L (29 November 2016); doi: 10.1117/12.2248144; https://doi.org/10.1117/12.2248144
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