Calculation Of The Height Of The Stable Boundary Layer In Practical Applications

By Sergej Zilitinkevich, A. Baklanov. 2002

182 citations recorded by the source corpus.

Subfields: Atmospheric Science, Computational Mechanics, Environmental Engineering

View Paper: https://www.semanticscholar.org/paper/3b5bf5d744404c8fbc6a98b0f28e142baebdd03d

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. Christopher W. Fairall
2. A. Grachev
3. Igor Esau
4. P. Guest
5. Sergej Zilitinkevich
6. B. Galperin
7. B. Grisogono
8. S. Sukoriansky

In Computational Mechanics

1. Igor Esau
2. Sergej Zilitinkevich
3. S. Sukoriansky
4. V. Perov
5. B. Galperin
6. P. Persson
7. Christopher W. Fairall
8. A. Grachev

In Environmental Engineering

1. Igor Esau
2. S. Sukoriansky
3. V. Perov
4. B. Galperin
5. P. Persson
6. Christopher W. Fairall
7. A. Grachev
8. P. Guest

Citations in the corpus

• The Critical Richardson Number and Limits of Applicability of Local Similarity Theory in the Stable Boundary Layer (2012, unknown): “16 (Handorf et al. 1999; Zilitinkevich and Baklanov 2002; Vickers and Mahrt 2004).”
• Resistance and heat‐transfer laws for stable and neutral planetary boundary layers: Old theory advanced and re‐evaluated (2005, methodology): “In non-steady regimes, h can be calculated using prognostic relaxation-type equation: dh/dt ∼ t−1∗ (hE − h), where t∗ ∼ h/u∗ is the PBL relaxation time-scale (see subsection 3.2 in Zilitinkevich and Baklanov 2002).”
• On the computation of planetary boundary-layer height using the bulk Richardson number method (2014, methodology): “In previous studies, the value of Ribc varies from 0.15 to 1.0 (Zilitinkevich and Baklanov, 2002; Jericevic and Grisogono, 2006; Esau and Zilitinkevich, 2010), with values of 0.25 and 0.5 most widely used (e.g., Troen and Mahrt, 1986; Holtslag and Boville, 1993).”
• A Total Turbulent Energy Closure Model for Neutrally and Stably Stratified Atmospheric Boundary Layers (2007, background): “which takes the distance from ground, the Coriolis effect and static stability into account (Rossby and Montgomery 1935; Zilitinkevich 1972; Nieuwstadt 1984; Hunt et al. 1985; Zilitinkevich and Mironov 1996; Zilitinkevich and Baklanov 2002; Zilitinkevich and Esau 2005).”
• SHEBA flux–profile relationships in the stable atmospheric boundary layer (2007, background): “Furthermore, several different definitions are possible for the SBL height (e.g., Zilitinkevich and Mironov 1996; Zilitinkevich and Baklanov 2002).”
• Review of wave‐turbulence interactions in the stable atmospheric boundary layer (2015, unknown): “…generation [e.g., Howard and Maslowe, 1973; Thorpe, 1977; Abarbanel et al., 1984; Grisogono, 1994b; Strang and Fernando, 2001; Andreas, 2002; Zilitinkevich and Baklanov, 2002; Fernando, 2003; Troy and Koseff , 2005; Achatz, 2007; Galperin et al., 2007; Mauritsen and Svensson, 2007;…”
• ‘Application of a New Spectral Theory of Stably Stratified Turbulence to the Atmospheric Boundary Layer over Sea Ice’ (2005, background): “…such SBLs become very shallow, down to 10 m or less (Kitaigorodskii and Joffre, 1988; King, 1990; Zilitinkevich and Mironov, 1996; Zilitinkevich et al., 2002a; Zilitinkevich and Baklanov, 2002; Zilitinkevich and Esau, 2002, 2003), they still maintain well-developed turbulence (e.g., Larsen, 1990).”