The Minimum Wind Speed for Sustainable Turbulence in the Nocturnal Boundary Layer
By V. Wiel, A. Moene, Harm J. J. Jonker, P. Baas, S. Basu, Jmm Judith Donda, Jielun Sun, Albert A. M. Holtslag. 2012
159 citations recorded by the source corpus.
Subfields: Computational Mechanics, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/165bf040b16d4748c0806d25bca060b967a3f580
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Computational Mechanics
In Environmental Engineering
- Albert A. M. Holtslag
- P. Baas
- Anton Beljaars
- S. Basu
- T. Mauritsen
- Larry Mahrt
- Gert-Jan Steeneveld
- R. Banta
In Global and Planetary Change
- Albert A. M. Holtslag
- Gert-Jan Steeneveld
- Larry Mahrt
- P. Baas
- Irina Sandu
- Anton Beljaars
- S. Basu
- T. Mauritsen
Citations in the corpus
- Stable Atmospheric Boundary Layers and Diurnal Cycles: Challenges for Weather and Climate Models (2013, background): “Obviously, not all differences can be attributed to the representation of the boundary layer since cloudiness and land surface factors also play an important role (e.g., Van den Hurk et al. 2011).”
- Why is it so difficult to represent stably stratified conditions in numerical weather prediction (NWP) models? (2013, background): “The resulting positive feedback loop, which leads to increasingly colder temperatures near the surface, can ultimately be ceased only if the large-scale geostrophic forcing is sufficient to restore the turbulent mixing within the thinning boundary layer [Mauritsen, 2012; Van de Wiel et al., 2012].”
- Stably Stratified Atmospheric Boundary Layers (2014, background): “Van de Wiel et al. (2012b) posed this threshold in terms of a minimum wind speed needed to maintain continuous turbulence.”