A simplified scheme of the generalized layered radiative transfer model |
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| Authors: | Dai Qiudan Sun Shufen |
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| Institution: | State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,
Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 |
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| Abstract: | In this paper, firstly, a simplified version (SGRTM) of the generalized layered radiative transfer model
(GRTM) within the canopy, developed by us, is presented. It reduces the information requirement of inputted sky
diffuse radiation, as well as of canopy morphology, and in turn saves computer resources. Results from the SGRTM
agree perfectly with those of the GRTM. Secondly, by applying the linear superposition principle of the optics and
by using the basic solutions of the GRTM for radiative transfer within the canopy under the condition of assumed
zero soil reflectance, two sets of explicit analytical solutions of radiative transfer within the canopy with any
soil reflectance magnitude are derived: one for incident diffuse, and the other for direct beam radiation. The explicit
analytical solutions need two sets of basic solutions of canopy reflectance and transmittance under zero soil reflectance,
run by the model for both diffuse and direct beam radiation. One set of basic solutions is the canopy reflectance
$\alpha_{\text f}$ (written as $\alpha_1$ for direct beam radiation) and transmittance $\beta_{\text f}$ (written as
$\beta_1$ for direction beam radiation) with zero soil reflectance for the downward radiation from above the canopy (i.e.
sky), and the other set is the canopy reflectance ($\alpha_{\text b})$ and transmittance $\beta_{\text b}$ for the upward
radiation from below the canopy (i.e., ground). Under the condition of the same plant architecture in the vertical layers,
and the same leaf adaxial and abaxial optical properties in the canopies for the uniform diffuse radiation, the explicit
solutions need only one set of basic solutions, because under this condition the two basic solutions are equal, i.e.,
$\alpha_{\text f}=\alpha_{\text b}$ and $\beta_{\text f}=\beta_{\text b}$. Using the explicit analytical solutions, the
fractions of any kind of incident solar radiation reflected from (defined as surface albedo, or canopy reflectance),
transmitted through (defined as canopy transmittance), and absorbed by (defined as canopy absorptance) the canopy and
other properties pertinent to the radiative transfer within the canopy can be estimated easily on the ground surface
below the canopy (soil or snow surface) with any reflectance magnitudes. The simplified transfer model is proven to
have a similar accuracy compared to the detailed model, as well as very efficient computing. |
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| Keywords: | generalized layered canopy radiative transfer model simplified model analytical solutions basic solutions adaxial abaxial leaf optical properties |
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