Abstract

Abstract. Despite recent advances in the development of detailed plant radiative transfer models, large-scale canopy models generally still rely on simplified one-dimensional (1-D) radiation models based on assumptions of horizontal homogeneity, including dynamic ecosystem models, crop models, and global circulation models. In an attempt to incorporate the effects of vegetation heterogeneity or “clumping” within these simple models, an empirical clumping factor, commonly denoted by the symbol Ω, is often used to effectively reduce the overall leaf area density and/or index value that is fed into the model. While the simplicity of this approach makes it attractive, Ω cannot in general be readily estimated for a particular canopy architecture and instead requires radiation interception data in order to invert for Ω. Numerous simplified geometric models have been previously proposed, but their inherent assumptions are difficult to evaluate due to the challenge of validating heterogeneous canopy models based on field data because of the high uncertainty in radiative flux measurements and geometric inputs. This work provides a critical review of the origin and theory of models for radiation interception in heterogeneous canopies and an objective comparison of their performance. Rather than evaluating their performance using field data, where uncertainty in the measured model inputs and outputs can be comparable to the uncertainty in the model itself, the models were evaluated by comparing against simulated data generated by a three-dimensional leaf-resolving model in which the exact inputs are known. A new model is proposed that generalizes existing theory and is shown to perform very well across a wide range of canopy types and ground cover fractions.

Highlights

  • Solar radiation drives plant growth and function, and quantification of fluxes of absorbed radiation is a critical component of describing a wide range of plant biophysical processes

  • Solar radiation provides the energy for plants to carry out photosynthesis and drives the energy balance and, the temperature of plant organs (Jones, 2014)

  • Kucharik et al (1999) evaluated the framework behind the OM_VAR model in a number of different canopies and found that it was able to fit the data well but that the model coefficients were highly species specific. One issue with their validation approach, which is symptomatic of many field validation studies of heterogeneous canopy radiation models, is that the data were collected in relatively dense canopies where heterogeneity is fairly low overall

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Summary

Introduction

Solar radiation drives plant growth and function, and quantification of fluxes of absorbed radiation is a critical component of describing a wide range of plant biophysical processes. Assuming that scattering of radiation is negligible and that leaf positions follow a uniform random distribution in space, the governing equation for radiation attenuation within a medium of vegetation is given by Beer’s law ( called Beer–Lambert law or Beer–Lambert– Bouguer law), which predicts an exponential decline in radiation with propagation distance. The importance of this equation in plant ecosystem models cannot be overstated and is incorporated within nearly every land surface model

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