The Cospectral Gap and Turbulent Flux Calculations

By D. Vickers, Larry Mahrt. 2003

306 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/ad488c5bd2eaf73b9aac5df475ce7b970fa7a80d

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Citations in the corpus

Flux–gradient relationship, self‐correlation and intermittency in the stable boundary layer (2004, background): “The ideal averaging window for flux calculation depends on the stability and heig ht above ground ( Vickers and Mahrt 2003 ).”
Stable-boundary-layer regimes from the perspective of the low-level jet (2008, methodology): “The SBL in these instances is often less than 25 m deep, and may be less than 10 m deep (Smedman 1988, Mahrt and Vickers 2006, Banta et al. 2007), as shown in the CASES-99 tower data in Fig. 14. The turbulence in this shallow SBL is weak and intermittent, and is best studied using specialized analys”
Turbulence Regimes and Turbulence Intermittency in the Stable Boundary Layer during CASES-99 (2012, unknown): “Tur-bulent ﬂuxes based on 10-min data segments were calculated after removing mesoscale ﬂuctuations, such as gravity waves, based on the method of Vickers and Mahrt (2003, 2006).”
Exchange Processes in the Atmospheric Boundary Layer Over Mountainous Terrain (2018, methodology): “Adjusting the TAS to the data instead of using a constant averaging interval has been shown to improve the consistency of turbulence statistics, in particular by reducing the scatter of observational data around theoretical similarity relationships [76].”
A Solution for Flux Contamination by Mesoscale Motions With Very Weak Turbulence (2006, methodology): “The decomposition represents the τ dependence of the flux averaged over the flux averaging time scale τF (Vickers and Mahrt, 2003).”
Random and systematic CO2 flux sampling errors for tower measurements over forests in the convective boundary layer (2009, methodology): “…t, and the averaging associated with the brackets defines the flux averaging timescale tF. Choice of the perturbation timescale t sets an upper-limit on the range of scales included in the computed flux (e.g., Friehe et al., 1991; Oncley et al., 1996; Howell and Sun, 1999; Vickers and Mahrt, 2003).”
Relationship between Low-Level Jet Properties and Turbulence Kinetic Energy in the Nocturnal Stable Boundary Layer (2003, methodology): “HRDL was described by Grund et al. (2001) and Wulfmeyer et al. (2000), and its use in CASES-99 was discussed by Blumen et al. (2001), Banta et al. (2002), Newsom and Banta (2003), Poulos et al. (2002), and Sun et al. (2002, 2003).”