Correction Of Eddy-Covariance Measurements Incorporating Both Advective Effects And Density Fluxes
By K. Paw U, Dennis D. Baldocchi, T. Meyers, K. Wilson. Boundary-layer Meteorology, 2000
423 citations recorded by the source corpus.
Subfields: Atmospheric Science, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/d6e7f9a95ed3d93ec66d59a857148aac6985ef2c
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In Atmospheric Science
In Environmental Engineering
In Global and Planetary Change
- Beverly E. Law
- Christoph K. Thomas
- Shaozhong Kang
- Fusheng Li
- Ling Tong
- D. Vickers
- R. Banta
- A. Martínez-cob
Citations in the corpus
- Documentation and Instruction Manual of the Eddy-Covariance Software Package TK3 (update) (2011, neutral): “0-30 0-30 1 0-30 31-75 2 31-75 31-75 3 31-75 76-250 4 >75 >250 5 The scheme after Rebmann et al. (2005) is a simplified version of the scheme after Foken (1999).”
- Random and systematic CO2 flux sampling errors for tower measurements over forests in the convective boundary layer (2009, methodology): “A tilt correction based on the long-term average wind direction dependence of the tilt angle is applied to the fast-response wind components (Paw U et al., 2000; Mahrt et al., 2000; Feigenwinter et al., 2004).”
- Comparison of dual crop coefficient method and Shuttleworth–Wallace model in evapotranspiration partitioning in a vineyard of northwest China (2015, methodology): “The procedures for correcting the EC measurements are as follows: planar fit method for coordinate rotation (Paw et al., 2000; Finnigan et al., 2003) and density correction according to the method of Webb et al.”