The structure of the near neutral atmospheric surface layer as observed during the CASES'99 experiment

By Philippe Drobinski, P. Carlotti, R. Newsom, R. Banta, Ralph C. Foster, J. Redelsperger. 2004

155 citations recorded by the source corpus.

Subfields: Atmospheric Science, Computational Mechanics, Environmental Engineering

View Paper: https://www.semanticscholar.org/paper/f7ec038d6888b9e4ceec30b1a808a6ff6f7a7081

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Citations in the corpus

Stable-boundary-layer regimes from the perspective of the low-level jet (2008, background): “structure (Banta et al. 2002, 2003, 2006, 2007), atmospheric waves (Blumen et al. 2001, Newsom and Banta 2003, Fritts et al. 2003, Sun et al. 2004), density currents (Sun et al. 2002), late-afternoon near-neutral boundary-layer structure ( Drobinski et al. 2004, 2007 ), and as a dataset for demonstr”
Towards Reconciling the Large-Scale Structure of Turbulent Boundary Layers in the Atmosphere and Laboratory (2012, methodology): “Large-scale streaks in the ASL have been observed in both field experiments (Drobinski et al. 2004; Newsom et al. 2008) and numerical simulations (e.g. Moeng and Sullivan 1994; Khanna and Brasseur 1998; Carlotti 2002; Foster et al. 2006; Lu and Porté-Agel 2010).”
Evidence of very long meandering features in the logarithmic region of turbulent boundary layers (2007, background): “Tomkins & Adrian (2003) and Ganapathisubramani et al. (2003) show instantaneous PIV examples of the u stripiness in the log region. Long regions of streamwise momentum deficit are found, with high-speed fluid seeming to fill the separation between neighbouring motions. Further investigations have su”
Three-dimensional conditional structure of a high-Reynolds-number turbulent boundary layer (2011, background): “Measurements within the atmospheric surface layer have also revealed the presence of surprisingly large elongated features (Young et al. 2002; Drobinski et al. 2004).”
Coherent Structures and the Dissimilarity of Turbulent Transport of Momentum and Scalars in the Unstable Atmospheric Surface Layer (2011, background): “produce fluxes and not only contribute to variances) in the surface layer of the high Reynolds number ABL (Hunt and Morrison 2000; Hunt and Carlotti 2001; Hogstrom et al. 2002; McNaughton and Brunet 2002;Drobinski et al. 2004; Smedman et al. 2007;Drobinski et al. 2007), the classic andmore”