Analysis of short-term closure of the surface energy balance above short vegetation

By D. Cava, D. Contini, A. Donateo, P. Martano. 2008

89 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/945585b9311512a72ce493c2fd063a86b0538b4a

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Citations in the corpus

Relative Humidity Effect on the High-Frequency Attenuation of Water Vapor Flux Measured by a Closed-Path Eddy Covariance System (2009, unknown): “Therefore, other factors, which were not considered here and are widely discussed in other studies (Cava et al. 2007; Foken 2008), can determine the lack of energy balance closure.”
A data-driven analysis of energy balance closure across FLUXNET research sites: The role of landscape-scale heterogeneity (2013, background): “The question remains, why is the energy balance not closed at most tower sites? One might expect forests to have lower or at least significantly different CEB,s than short-statured vegetation, because the role of heat storage in the larger canopy, lower average G, and possible advection and/or decou”
Effects of different eddy covariance correction schemes on energy balance closure and comparisons with the modified Bowen ratio system (2008, background): “…period is an additional facet of the EC processing that can have a substantial effect on the observed energy balance (Finnigan et al., 2003; Cava et al., 2007), because short averaging intervals act as a high pass filter that can remove low-frequency components of the turbulent flux under…”
Random and systematic CO2 flux sampling errors for tower measurements over forests in the convective boundary layer (2009, background): “Cava et al. (2008) found significant daytime CO2 transport on timescales between 30 min and 2 h, and attributed it to large convective eddies.”
Corrections and data quality control (2012, background): “The application of this correction increases the fluxes significantly (Cava et al. 2008).”