Intermittent Turbulence and Oscillations in the Stable Boundary Layer over Land. Part I: A Bulk Model

By B. V. D. Wiel, Reinder J. Ronda, A. Moene, H. D. Bruin, Albert A. M. Holtslag. 2002

184 citations recorded by the source corpus.

Subfields: Computational Mechanics, Environmental Engineering, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a2dfbff5fd7e356be1e890b96969d520904e2f73

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In Computational Mechanics

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Citations in the corpus

Intermittent Turbulence in the Stable Boundary Layer over Land. Part III: A Classification for Observations during CASES-99 (2003, background): “Intermittency can be generated by several physical mechanisms (see Van de Wiel et al. 2002a): by local shear effects (Ha and Mahrt 2001), by instability on the scale of the entire surface inversion layer, or by turbulence generated aloft diffusing to the surface [see the review on SBL issues by…”
Large-eddy simulation of stably stratified atmospheric boundary layer turbulence: A scale-dependent dynamic modeling approach (2005, background): “Contemporary SBL research has revealed that in very stable regimes the relative importance of radiative cooling and heat exchange with the underlying soil becomes as significant as turbulent mixing (van de Wiel 2002).”
Stable Atmospheric Boundary Layers and Diurnal Cycles: Challenges for Weather and Climate Models (2013, background): “…of stable boundary layers is quite diverse—for example, shallow and deep boundary layers with continuous turbulence through most of their depth and boundary layers with very weak and/or intermittent turbulence in very stable cases at night (e.g., Mahrt 1985; Van de Wiel et al. 2003, 2007).”
The Minimum Wind Speed for Sustainable Turbulence in the Nocturnal Boundary Layer (2012, methodology): “In turn, those processes are externally driven by the incoming longwave radiation at the top of the boundary layer, which is mainly dictated by the presence or absence of clouds, and by the synoptic pressure gradient (Van de Wiel et al. 2002a; Svensson et al. 2011).”
Stable-boundary-layer regimes from the perspective of the low-level jet (2008, background): “Recently van de Wiel et al. (2002b, 2003) defined a two-dimensional space, where one dimension is the surface stress (as a proxy for the large-scale pressure gradient) and the other is the surface net radiation Rnet.”