Theory And Measurements For Turbulence Spectra And Variances In The Atmospheric Neutral Surface Layer

By U. Högström, Julian C. R. Hunt, A. Smedman. 2002

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Towards Reconciling the Large-Scale Structure of Turbulent Boundary Layers in the Atmosphere and Laboratory (2012, background): “According to Högström et al. (2002), the increase of vertical velocity variance with height is caused by detached eddies of relatively large scale that are being brought down from the upper surface layer.”
Scaling of the streamwise velocity component in turbulent pipe flow (2004, background): “Its often-published appearance (see, for instance, Kader & Yaglom 1991; Katul & Chiu 1998; Nikora 1999; Hunt & Carlotti 2001; Högström et al. 2002) leads to the obvious question of why this might be so.”
Coherent Structures and the Dissimilarity of Turbulent Transport of Momentum and Scalars in the Unstable Atmospheric Surface Layer (2011, methodology): “Fig. 8 Ratios of bulk transfer coefficients of momentum and scalars using the lake data; the black line is the empirical equation for the ratio of diffusivities from Hogstrom (1988 ) a nd thedashed line is the equivalent equation from Brutsaert (2005)”