Figure 4 (a)
Figure 4 (a)
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Figure 4 (b)
Figure 4 (b)
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Figure 4. Principal solar plane BRDF for the Southern Old Aspen BOREAS site in the red band as measured by the PARABOLA and POLDER instruments and modeled by the 4-Scale model. The model reproduces accurately the red reflectance features: the hotspot from the POLDER and the PARABOLA bowl shape in the forward scattering.

 

Figure 5 (a)
Figure 5 (a)
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Figure 5 (b)
Figure 5 (b)
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Figure 5. Comparison of Modelled and POLDER Distribution of Near-Infrared (NIR) Reflectance at the Southern Old Black Spruce BOREAS site near Candle Lake, Saskatchewan.

Radiative Transfer Model (4-Scale)


A geometric-optical forest canopy model named "4-Scale" was developed for LAI and FPAR algorithm refinement and for parameterizing radiative transfer sub-model in BEPS.


What is a radiative transfer model?

A radiative transfer model simulates radiation transfer processes in certain media, such as vegetation and atmosphere. For vegetation, it computes the interaction between solar radiation and plants. Solar radiation reflected from the Earth's surfaces and measured by satellites depends strongly on the angles of the sun and the satellite in relation to the surface. This bi-directional behaviour is quantified using the Bi-directional Reflectance Distribution Function (BRDF).

4-Scale is a radiative transfer model that simulates the BRDF according to the structural properties of the vegetation.

Figure 1
a b c
Figure 1. BRDF rendering of a forest canopy composed of opaque cone and cylindrical objects viewed from 3 angles:

(a) backward scattering, where the sun and the viewer are on the same side, hiding most of the shadows;
(b) nadir view, where a maximum of the background can be seen; and
(c) forward scattering where the sun and the viewer are on the opposite side.

Figure 2
Figure 2. 4-Scale simulated reflectance from a forest canopy at different view zenith angles on the plane parallel to the sun with the corresponding cases from Figure 1.


Why our model is named "4-Scale"?

In forest canopies, the solar radiation is interacting with the foliage at four different scales: within groups of trees, within individual crowns, within branches, and within shoots.

Figure 3

Figure 3. Scales of plant canopy architecture considered in reflectance models:
1-scale: turbid media;
2-scale: randomly distributed discrete objects containing turbid media;
3-scale: non-random discrete objects containing turbid media; and
4-scale: non-random discrete objects with internal structures (such as branches and shoots).

4-Scale was developed with emphasis on the structural composition of forest canopies at these scales and is a step forward from existing 2-scale geometrical-optical models. It employs the following modeling methodologies:

  1. The non-random spatial distribution of trees is simulated using the Neyman type A distribution (Neyman, 1939) that creates patches of a forest stand. The model simulates tree crowns as discrete geometrical objects: cone and cylinder for conifers, spheroid for deciduous species. The size of the crowns decreases when the trees are found in large clusters, and the tree locations are also subject to the repulsion effects to better represent the competition for light.
  2. Inside the crowns, a branch architecture defined by a single inclination angle is included to improve the calculation of light penetration from the geometric-optical model of Li and Strahler (1992) with the assumption of random leaf distribution inside tree crowns. A branch is in turn composed of foliage elements (individual leaves in deciduous and shoots in conifer canopies) with a given angle distribution pattern.
  3. The hotspot, where the view zenith and solar zenith angles coincide, is computed both on the ground and for the foliage with gap size distributions between and inside the crowns, respectively.
  4. The crown is treated as a complex medium where shadowed foliage can be observed on the sunlit side, and sunlit foliage can be seen from the shaded side.
  5. A multiple scattering scheme, based on view factors, is used to compute the amount of light reaching the shaded foliage and background.
4-Scale has been validated with remote sensing data taken during BOREAS from the PARABOLA and POLDER. (Figure 4 and Figure 5)

4-Scale has been used to study the influence of different canopy parameters on the retrieval of biophysical properties with remotely sensed data (Leblanc et al 1997; Leblanc et al 1999); to correct the BRDF effect of airborne data used in the retrieval of leaf area index (Chen et al, 1998); and to derive an improved BRDF correction for NOAA AVHRR data (Chen and Cihlar, 1997).

4-Scale's code and a Microsoft Windows 95/98/NT version are available on request from Jing Chen.

Figure 4
Screen shot of 4-Scale for Windows 95/98/NT.


References

Chen J.M. and J. Cihlar, 1997. "A hotspot function in a simple bidirectional reflectance model for satellite applications." Journal of Geophysical Research 102 (D22), pp. 25,907-25,913

Chen J.M. and S. G. Leblanc, 1997. "A Four-Scale Bidirectional Reflectance Model Based on Canopy Architecture." IEEE Transactions on Geoscience & Remote Sensing 35, pp. 1316-1337.

Chen J.M., S.G. Leblanc, J.R Miller, J. Freemantle, S.E. Loechel, C.L. Walthall, K.A. Innanen, and H.P White. 1998 "Compact Airborne Spectrographic Imager (CASI) used for Mapping Biophysical Parameters of Boreal Forests"  To appear in the second BOREAS special issue of Journal of Geophysical Research-Atmosphere.

Leblanc, S. G., J. M. Chen  and J. Cihlar, 1997. "NDVI Directionality in Boreal Forests: A Model Interpretation of Measurements". Canadian Journal of Remote Sensing 23, pp. 368-379.

Leblanc S.G., P. Bicheron, J.M. Chen, M. Leroy and J. Cihlar, 1999. "Investigation of Directional Reflectance in Boreal Forests with an Improved 4-Scale Model and Airborne POLDER Data."  IEEE Transactions on Geoscience & Remote Sensing (in press)

Li, X. and A.H. Strahler, 1992. "Geometric-Optical Bidirectional Reflectance Modeling of the Discrete Crown Vegetation Canopy: Effect of Crown Shape and Mutual Shadowing.", IEEE Transactions on Geoscience & Remote Sensing 30, pp. 276-292.

Neyman, J., 1939. "On a New Class of ¡®Contagious¡¯ Distribution Applicable in Entomology and Bacteriology", Annals of Mathematical Statistics 10, pp. 35-57.


© Revised: Mar., 2005