CASES-99: a comprehensive investigation of the stable nocturnal boundary layer
By G. Poulos, W. Blumen, Dave Fritts, J. Lundquist, Jielun Sun, S. Burns, C. Nappo, R. Banta, R. Newsom, Joan Cuxart and 3 more. 2002
563 citations recorded by the source corpus.
Subfields: Atmospheric Science, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/1fe7103ffd71554be2a47c8c99e4715546e85d5c
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Citations in the corpus
- Stable-boundary-layer regimes from the perspective of the low-level jet (2008, background): “wave packet (5 October 1999: Blumen et al. 2001, Poulos et al. 2002, Newsom and Banta 2003).”
- Intermittent Turbulence in the Stable Boundary Layer over Land. Part III: A Classification for Observations during CASES-99 (2003, methodology): “For a general description of the experiment we refer to Poulos et al. (2002) and to the official CASES-99 Internet site at http://www. colorado-research.com/cases/CASES-99.html (data freely available).”
- Turbulence energetics in stably stratified geophysical flows: Strong and weak mixing regimes (2008, methodology): “Figure 3. Turbulent Prandtl number PrT = KM /KH versus Ri. Blue points and curve – meteorological campaigns SHEBA (Uttal et al., 2002, mostly for Ri Poulos et al., 2002, for 0.1 < Ri < 100); green – laboratory sheared flow (Ohya, 2001); red – new LES using NERSC code (Esau, 2004); grey – direct nu”
- Flux–gradient relationship, self‐correlation and intermittency in the stable boundary layer (2004, methodology): “(a) Self-correlation analysis of subsets of the CASES99 data Since φm = 1 + βz/L is expected to be most valid at small z/L and may be less accurate for large z/L, the data for each observational level are divided into two subsets: one for z/L less than a cut-off value, the other for z/L greater than”
- Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes (2006, background): “…observations: squares [CME = Carbon in the Mountains Experiment, Mahrt and Vickers (2005)], circles [SHEBA = Surface Heat Budget of the Arctic Ocean, Uttal et al. (2002)] and overturned triangles [CASES-99 = Cooperative AtmosphereSurface Exchange Study, Poulos et al. (2002), Banta et al. (2002)].”