The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part B6b. Beijing 2008
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Where L d = radiance reflected from direct solar irradiance of
sloping pixel
E d ' = direct solar irradiance of sloping pixel
However, tree growth is oriented with the gravitational field
and always vertical to the horizontal plane, not vertical to the
slope. As a result, the solar incidence angle is constant and the
direct solar irradiance received by individual crown is
independent with the slope and aspect of the surface, which
means the radiance reflected is not affected by topography as
well. So equation (6) will be not applicable. But for the case of
a cluster of tree crowns, there is another type of topography
effect (Gu, 1998). Firstly, because of the mutual shading of tree
crowns, the pixel of tree crowns can be partitioned to sunlit part
and shadow part. The sunlit part can receive both direct and
diffuse irradiance, and the shadow part can only receive diffuse
irradiance. Secondly, the mutual shading effect is controlled by
terrain since the relative position of trees is affected by
topography. As a result, on Sun-facing slopes, the proportion of
sunlit tree crowns which exposed to the direct illumination is
larger than that on the slopes facing away from the Sun, which
eventually lead to the difference of reflected up radiance. So for
the case of tree crowns, the rate of reflected radiance from
direct irradiance between sloping pixel and level pixel equals
the rate of total area of sunlit part of the pixel. By Gu, the rate is:
L d _ A' cos i (7)
L. A cos 0 cos a
a s
Where A ’ = the total sunlit area of sloping pixel
A = the total sunlit area of level pixel
According to the analysis above, for tree crowns, equation (2)
can be modified as (The situation of circumsolar diffuse
irradiance is the same as direct irradiance):
r , COSÌ r . COSi T . T ,, . r
L — b L d +b KL f + (1 — K)VL f + L t
cos 6 S cos a cos 0 S cos a
(8)
From equation (8), the model can be modified as:
kL
(9)
cos 6. cos a
- E,+b-
cos 6, cos a
KE f + (l-K)VE +E,
This is the modified model for forest areas where tree crowns
cover, which is the combination of Sandmeier’s model and SCS
correction.
2.3 Parameter Calculation
The radiative transfer parameters E d , Ef, K can be calculated by
6S or MODTRAN 4 model etc. The total radiance reflected by
level pixel (L) can be calculated by:
L ( E d +E f)Pa (10)
7t
Where p a = atmospheric corrected reflectance by 6S or
MODTRAN 4 etc.
The slope angle and aspect angle can be calculated from DEM;
the accurate calculation of E, and V was discussed respectively
by Proy (1989) and Dozier (1990); Sandmeier’s model provides
the simplified calculation of them (Sandmeier, 1997).
3. MODEL VALIDATION
3.1 Validation Data and Implementation
The modified model in this paper is specifically for forested
areas, so it is necessary to use satellite data in forested area to
validate the effectiveness of the model. In the experiment, the
30m multi-spectral ETM image of Landsat 7 acquired on May
14th, 2000 as validation data. Lipin County, Guizhou province,
China was chosen to be the study area. The study area is typical
forest and mainly covered by Chinese fir. DEM with an original
spatial resolution of 25m were used here (see Figure 2). The
terrain in the area is quite rugged, where the average slope
angle is 22 degree and the maximal slope angle is 55 degree.
In this experiment, the radiative transfer parameters in the
model were calculated by 6S model. The dark objective method
(Kaufman, 1988; Tian Qingjiu, 1998) was used to estimate the
aerosol optical thickness, which is a very important input
parameter of 6S model. The programming tool of the
experiment is IDL.
0 m 300 m 600 m
Figure 2. DEM in the study area
3.2 Result and Discussion
In order to evaluate the efficiency of the model, the atmospheric
corrected image by 6S model was taken as the comparative
image without topographic correction. In addition, Sandmeier’s
model is also applied to the same data to make comparison with
the modified model.