Stable-boundary-layer regimes from the perspective of the low-level jet

By R. Banta. 2008

134 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Engineering, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/4c417497f1dab8433d3f6a7b951e43d5adcc2e6a

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

1. Albert A. M. Holtslag
2. Gert-Jan Steeneveld
3. S. Basu
4. B. Grisogono
5. Fernando Port'e-Agel
6. V. Wiel
7. P. Baas
8. Harm J. J. Jonker

In Environmental Engineering

1. M. Bastankhah
2. Sina Shamsoddin
3. Fernando Port'e-Agel
4. S. Basu
5. V. Wiel
6. Albert A. M. Holtslag
7. P. Baas
8. Harm J. J. Jonker

In Global and Planetary Change

1. Albert A. M. Holtslag
2. Gert-Jan Steeneveld
3. B. Grisogono
4. Fernando Port'e-Agel
5. V. Wiel
6. P. Baas
7. Harm J. J. Jonker
8. Jielun Sun

Citations in the corpus

• Exchange Processes in the Atmospheric Boundary Layer Over Mountainous Terrain (2018, background): “Short-lived mixing events can occur when wind shear across the top of the cold pool becomes strong enough to make the Richardson number (Ri) subcritical [185] (yellow wind profiles and orange whirls in Figure 4).”
• Turbulence Regimes and Turbulence Intermittency in the Stable Boundary Layer during CASES-99 (2012, unknown): “11b), as shown by Banta et al. (2006) and Banta (2008). Consequently, sU at a constant height Z1 changes from a small constant value when the wind speed at Z1 is less than its threshold value to a value increasing with wind”
• The Minimum Wind Speed for Sustainable Turbulence in the Nocturnal Boundary Layer (2012, background): “Nevertheless, it seems to be useful to classify stable boundary layers into two major prototypes (Mahrt et al. 1998)—the weakly stable boundary layer (WSBL) and the very stable boundary layer (VSBL)—based on their generally observed characteristics.”
• Wind-Turbine and Wind-Farm Flows: A Review (2019, background): “The LLJ forms in and above the SBL when a maximum in the mean velocity profile emerges at the top of the boundary layer (Blackadar 1957).”
• A Conceptual View on Inertial Oscillations and Nocturnal Low-Level Jets (2010, background): “1 2010 American Meteorological Society by Banta et al. (2003, 2006) and Banta (2008) succeeded in relating jet-based properties, such as jet-nose height and speed, to major mixing characteristics of the NBL.”