Flux-profile Relationships for Wind Speed and Temperature in the Stable Atmospheric Boundary Layer
By Yinguo Chenge, W. Brutsaert. 2005
217 citations recorded by the source corpus.
Subfields: Atmospheric Science, Computational Mechanics, Environmental Engineering
View Paper: https://www.semanticscholar.org/paper/452dff0e2e2a33ac419553c8f617daa803176eae
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Christopher W. Fairall
- A. Grachev
- Charles Meneveau
- Jan Kleissl
- Vijayant Kumar
- Marc B. Parlange
- P. Guest
- Pedro A. Jimenez
In Computational Mechanics
- Charles Meneveau
- Vijayant Kumar
- Jan Kleissl
- Marc B. Parlange
- A. Grachev
- Christopher W. Fairall
- P. Guest
- Edgar L. Andreas
In Environmental Engineering
- Charles Meneveau
- Vijayant Kumar
- Jan Kleissl
- Marc B. Parlange
- A. Grachev
- Edgar L. Andreas
- Christopher W. Fairall
- P. Guest
Citations in the corpus
- Large‐eddy simulation of a diurnal cycle of the atmospheric boundary layer: Atmospheric stability and scaling issues (2006, methodology): “1988], and hence the modified formulation of Cheng and Brutsaert [2005] is used.”
- A Revised Scheme for the WRF Surface Layer Formulation (2012, background): “For this reason, extensions to highly stable situations (e.g., Webb 1970; van Ulden and Holtslag 1985; Holtslag and de Bruin 1988; Beljaars and Holtslag 1991; Cheng and Brutsaert 2005) as well as highly unstable conditions (e.”
- SHEBA flux–profile relationships in the stable atmospheric boundary layer (2007, background): “The dashed line represents ϕm = ϕh = 1 + βζ with β = 5(ζ Cheng and Brutsaert (2005) parameterization ( ζ< 5). The solid line is ϕm SHEBA, Eq. 9a. Function ϕm (1) and L1 (upper panel) are based on the ‘surface fluxes’, whereas ϕm (n) and Ln (bottom panel) are based on the ‘local fluxes’.”