Streamwise turbulent intensity under unstable atmospheric stratification explained by a spectral budget![]() Presentation: Session: Atmospheric turbulence 3 Room: Room C Session start: 10:30 Wed 26 Aug 2015 Tirtha Banerjee tirtha.b@duke.edu Affifliation: Duke University Marcelo Chamecki chamecki@meteo.psu.edu Affifliation: The Pennsylvania State University Gabriel Katul gaby@duke.edu Affifliation: Duke University Topics: - Atmospheric turbulence, - Geophysical and astrophysical turbulence, - Wall bounded flows, - Thermally driven turbulence Abstract: Because of its non-conformity to Monin-Obukhov Similarity Theory (MOST), the effects of thermal stratification on scaling laws describing the stream-wise turbulent intensity $\sigma_u$ normalized by the turbulent friction velocity ($u_*$) continues to draw research attention. The streamwise turbulent intensity happens to be of utmost importance as a direct measure of the intensity of turbulence and an analytical model able to predict its nature would be considered useful for a copious number of practical applications- ranging from industrial pipe flow to air pollution modeling among many. A spectral budget method used previously by \cite{Banerjee2013} was demonstrated as a suitable workhorse to analytically explain the `universal' logarithmic scaling law exhibited by $\sigma_u^2/u_*^2$ for neutral conditions as reported in different high Reynolds number experiments. In the present work \cite{Banerjee2014}, that theoretical framework has been expanded to assess the variability of $\sigma_u/u_*$ under unstable atmospheric stratification. At least three different length scales- the distance from the ground ($z$), the height of the atmospheric boundary layer ($\delta$), and the Obukhov length ($L$) are all found to be controlling parameters in the variation of $\sigma_u/u_*$. Analytical models have been developed and supported by experiments for two limiting conditions: $z/\delta<0.02$, $-z/L<0.5$ and $0.02 < |