Computing turbulent fluxes near the surface: Needed improvements

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A data-driven analysis of energy balance closure across FLUXNET research sites: The role of landscape-scale heterogeneity (2013, background): “The connection the flux footprint and energy balance closure is discussed dix B. lusions ux community has made substantial advances in underthe mechanisms underlying the energy balance closure (Foken et al., 2011; Leuning et al., 2012), but additional ds to be done (Mahrt, 2010).”
On the Nature of the Transition Between Roll and Cellular Organization in the Convective Boundary Layer (2017, background): “…al. 2009) have demonstrated that large-scale structures in the logarithmic layer of a turbulent boundary layer can modulate near-wall turbulence and thereby affect the generation of surface shear stress, paving the way for new models (Marusic et al. 2010) to predict near-wall velocity statistics.”
Review of wave‐turbulence interactions in the stable atmospheric boundary layer (2015, background): “In addition, wave motions near the surface are characterized by small flow angles with respect to a horizontal surface, in which case even small misalignment of the sonic anemometers can lead to large relative errors in vertical wave motions [e.g., Mahrt, 2010b].”