Stratification, turbulence organisation and pressure-strain effects on surface-layer turbulence anisotropy
Abstract Content of image described in text. At large scales, the Reynolds stress tensor exhibits notable anisotropy, a key feature of all wall-bounded turbulent flows. Yet, how the drivers of this anisotropy evolve with shearing and thermal stratification in the atmospheric surface layer (ASL) remains a daunting challenge for theory and models alike. Here, the velocity variance budgets are used to explore the evolution of anisotropy in the daytime ASL close to the surface, a region known to be problematic for large-eddy simulations. A special focus is placed on the importance of slow and rapid pressure-strain correlations, and the role of transport on partitioning the turbulent kinetic energy among the velocity components. Results obtained from near-surface observations of four datasets over flat and horizontally homogeneous terrain show persistent anisotropy over a wide range of flux Richardson numbers italic Ri Subscript f Rif ${\textit{Ri}}_{\!f}$ and wall-normal distances, and highlight the importance of different processes in three distinct flow regimes, roughly related to dynamic ( StartAbsoluteValue italic Ri Subscript f Baseline EndAbsoluteValue much less than 1 |Rif|≪1 $|{\textit{Ri}}_{\!f}|\ll 1$ ), dynamic-convective ( StartAbsoluteValue italic Ri Subscript f Baseline EndAbsoluteValue tilde 1 |Rif|∼1 $|{\textit{Ri}}_{\!f}|\sim 1$ ) and convective ( StartAbsoluteValue italic Ri Subscript f Baseline EndAbsoluteValue much greater than 1 |Rif|≫1 $|{\textit{Ri}}_{\!f}|\gg 1$ ) regimes of the ASL. In particular, close to the surface in the dynamic-convective regime, a drop in wall-normal velocity variance and a substantial increase of spanwise velocity variance are shown to result from the increasing role of pressure transport and rapid distortion, related to turbulence organisation. This behaviour is not captured by the classic Rotta closure but requires the inclusion of both rapid pressure-strain and transport terms. In all regimes, wall blocking is found to influence turbulence close to the surface, thus requiring the adoption of an anisotropic Rotta model to accommodate its effects.