Related Experiment Video
Updated: Apr 19, 2026

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites
Published on: June 24, 2019
Advances in Modelling Radiative Transfer, Heat Storage and Turbulent Transport to Evaluate CO2, Heat and Water Fluxes
Martin Béland1, Gordon B Bonan2, Tilden P Meyers3
1Digital Forest Lab, Department of Geomatics Sciences, Laval University, Quebec City, Quebec, Canada.
None:
Multilayer canopy models have been developed for several decades, and interest in this model class remains high despite their complexity because of their multiple advantages over big-leaf models. Nowadays, a number of scientific and technological advancements favour improving and evaluating these models. First, the advent of lidar technology has enabled detailed mapping of leaves and stems in forest canopies and enhanced the modelling of absorbed solar radiation by both elements within a canopy. Second, long-time series of eddy covariance measurements are available for model evaluation, capturing years with extreme conditions like droughts. Here we present a new version of the CanVeg model (CanVeg2) with three main modifications: (1) radiative transfer modelling using 3D ray tracing and ground lidar, (2) the addition of a stem energy balance module and (3) the use of a higher order closure model to provide profiles of horizontal wind velocity and variance in vertical wind velocity. We evaluate the CanVeg2 model at five broadleaf forest sites with contrasting canopy structures using long term eddy covariance records, and at two of the sites, soil temperature profiles and scalar vertical profiles. The modelled latent heat and CO2 flux densities closely matched the eddy covariance measurements. The sensible heat flux density had lower coefficients of determination across sites. The modelled soil heat flux densities were notably higher than the measurements at the three sites where this flux is measured. Divergences between modelled and measured scalars in the lower canopy layers suggest the model would benefit from improved information on soil-litter moisture content. The favourable results obtained in the model evaluation suggest it may be useful towards addressing new science questions by enabling the estimation of certain canopy states nearly impossible to measure at the canopy level like vertically resolved leaf and stem temperatures and to study the interactions between highly interconnected biophysical and physiological processes.
More Related Videos
08:31The Calibration and Use of Capacitance Sensors to Monitor Stem Water Content in Trees
Published on: December 27, 2017
13:27Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
Related Concept Videos
The Carbon Cycle
Mechanisms of Heat Transfer II
Regulation of Transpiration by Stomata
Mechanisms of Heat Transfer
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant...
Global Climate Change
Isothermal Processes
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...