Stable Boundary-Layer Scaling Regimes: The Sheba Data

By A. Grachev, Christopher W. Fairall, P. Persson, Edgar L. Andreas, P. Guest. 2005

224 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/722c2326afb0180e3b1e4b3d9e4991e4e1a59f72

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In Atmospheric Science

Citations in the corpus

Stably Stratified Atmospheric Boundary Layers (2014, methodology): “For polar nights with no diurnal variation, the structure might be well described by Ekman theory (Grachev et al. 2005).”
Parameterizing turbulent exchange over sea ice in winter (2010, methodology): “Through eddy-covariance measurements using standard turbulence processing, as described in Persson et al. (2002), Grachev et al. (2005, 2007a), and Andreas et al. (2006), we measured t and H s at each of the ﬁve tower levels and H L at one level [Eq.”
SHEBA flux–profile relationships in the stable atmospheric boundary layer (2007, methodology): “Grachev et al. (2005) noted that the observed dependence ϕm ∝ ζ 1/3 (Fig.”
Turbulent Velocity-Variance Profiles in the Stable Boundary Layer Generated by a Nocturnal Low-Level Jet (2006, background): “…et al. (1998) identified three regimes, weakly stable, transitional, and strongly stable, based on z / L , where L is the Monin–Obukhov length, and Grachev et al. (2005) added a fourth regime in the long-lived arctic SBL, a turbulent Ekman regime between the transitional and strongly stable…”
Turbulence Regimes and Turbulence Intermittency in the Stable Boundary Layer during CASES-99 (2012, unknown): “The weak turbulence allows strong large-scale temperature and vertical velocity oscillations and wind direction rotation with height in the direction consistent with the Ekman spiral discussed by Grachev et al. (2005).”
Stable-boundary-layer regimes from the perspective of the low-level jet (2008, background): “…h/L (e.g., Holtslag and Nieuwstadt 1986); z/L (e.g., Mahrt et al. 1998, Mahrt 1999); and bulk Richardson number RiB (e.g., Mahrt and Vickers 2006, Grachev et al. 2005, Ohya 2001), where h is the height of the SBL; L is the surface-layer Obukhov length; RiB = (g/θ)(∆θ/∆z)/(∆U/∆z)2 = (g/θ)(∆θ…”