Evaluation of the inverse method
To evaluate the accuracy of the iteration method, diffuse reflection
and total transmission were calculated using the adding-doubling
technique for a variety of optical properties (Table 3.4 and
3.5). These calculated values were used in place of measured
reflection and transmission, and consequently, the true optical
properties
characterizing each set of reflection and transmission are known.
Two separate evaluations were performed: one for a known anisotropy
gHG and one for known collimated transmission. Either the anisotropy
or the collimated transmission was known accurately and any errors
presented in Tables 6.1 and 6.2 do not include possible errors
in determining these known values.
Figure 6.4:
Detailed flowchart for the inversion algorithm when
the collimated transmission is known. This flowchart illustrates
the changes in variables necessary to vary all the parameters
during each iteration.
|
|
Figure 6.5:
Detailed flowchart for the inversion algorithm when
the anisotropy is known. This flowchart illustrates the changes
in variables necessary to vary all the parameters properly during
the iteration process.
|
|
Table:
Differences and percent errors between calculated and true optical
thickness
and albedo a. The Henyey-Greenstein anisotropy
is
assumed known. The reflection and transmission used as truth were taken from
Tables 3.4 and 3.5.
| |
g=0.0 |
g=0.5 |
g=0.875 |
| n |
a=.6 |
a=.9 |
a=.99 |
a=.6 |
a=.9 |
a=.99 |
a=.6 |
a=.9 |
a=.99 |
| |
|
|
|
|
|
|
|
|
|
| acalc-a |
| -2 |
0.04 |
-0.00 |
0.01 |
0.13 |
0.02 |
0.01 |
0.31 |
0.08 |
0.01 |
| -1 |
-0.01 |
-0.02 |
0.01 |
0.05 |
-0.01 |
0.01 |
0.25 |
0.05 |
0.01 |
| 0 |
-0.03 |
-0.02 |
-0.00 |
0.01 |
-0.02 |
0.00 |
0.20 |
0.02 |
0.01 |
| 1 |
-0.02 |
-0.02 |
-0.00 |
0.01 |
-0.01 |
-0.00 |
0.17 |
0.00 |
0.00 |
| 2 |
-0.02 |
-0.01 |
-0.00 |
0.01 |
-0.01 |
-0.00 |
0.17 |
0.00 |
-0.00 |
| 3 |
-0.02 |
-0.01 |
-0.00 |
0.01 |
-0.01 |
-0.00 |
0.17 |
0.00 |
-0.00 |
| 4 |
-0.02 |
-0.01 |
-0.00 |
0.01 |
-0.01 |
-0.00 |
0.17 |
0.00 |
-0.00 |
| |
|
|
|
|
|
|
|
|
|
| Percent Errors |
| -2 |
7 |
-0 |
1 |
21 |
3 |
1 |
52 |
9 |
1 |
| -1 |
-2 |
-3 |
1 |
8 |
-1 |
1 |
42 |
6 |
1 |
| 0 |
-4 |
-3 |
-0 |
2 |
-2 |
0 |
33 |
2 |
1 |
| 1 |
-4 |
-2 |
-0 |
1 |
-2 |
-0 |
28 |
0 |
0 |
| 2 |
-3 |
-1 |
-0 |
1 |
-1 |
-0 |
28 |
0 |
-0 |
| 3 |
-3 |
-1 |
-0 |
1 |
-1 |
-0 |
29 |
0 |
-0 |
| 4 |
-3 |
-1 |
-0 |
1 |
-1 |
-0 |
29 |
0 |
-0 |
 |
| -2 |
0.07 |
0.07 |
0.09 |
0.12 |
0.11 |
0.14 |
0.54 |
0.45 |
0.52 |
| -1 |
0.07 |
0.07 |
0.07 |
0.10 |
0.09 |
0.11 |
0.56 |
0.38 |
0.43 |
| 0 |
0.06 |
0.05 |
0.05 |
0.08 |
0.07 |
0.09 |
0.63 |
0.27 |
0.29 |
| 1 |
0.03 |
0.00 |
-0.01 |
0.07 |
0.04 |
0.06 |
0.90 |
0.16 |
0.20 |
| 2 |
-0.08 |
-0.15 |
-0.12 |
0.00 |
-0.10 |
-0.07 |
1.71 |
0.18 |
0.25 |
| 3 |
-0.39 |
-0.52 |
-0.25 |
-0.22 |
-0.46 |
-0.25 |
3.28 |
0.25 |
0.29 |
| 4 |
-2.18 |
-1.42 |
-0.52 |
0.36 |
-1.21 |
-0.48 |
6.21 |
-0.13 |
-0.30 |
| |
|
|
|
|
|
|
|
|
|
| Percent Errors |
| -2 |
29 |
29 |
36 |
46 |
44 |
57 |
217 |
181 |
208 |
| -1 |
14 |
14 |
13 |
20 |
19 |
22 |
112 |
76 |
87 |
| 0 |
6 |
5 |
5 |
8 |
7 |
9 |
63 |
27 |
29 |
| 1 |
2 |
0 |
-0 |
3 |
2 |
3 |
45 |
8 |
10 |
| 2 |
-2 |
-4 |
-3 |
0 |
-2 |
-2 |
43 |
5 |
6 |
| 3 |
-5 |
-7 |
-3 |
-3 |
-6 |
-3 |
41 |
3 |
4 |
| 4 |
-14 |
-9 |
-3 |
2 |
-8 |
-3 |
39 |
-1 |
-2 |
|
Table:
Differences and percent errors between calculated and true
Henyey-Greenstein anisotropies
and albedos (a). The collimated transmission is
assumed known for various optical depths .
The reflection and transmission
used as truth were taken from Tables 3.4 and 3.5.
| |
g=0.0 |
g=0.5 |
g=0.875 |
| n |
a=.6 |
a=.9 |
a=.99 |
a=.6 |
a=.9 |
a=.99 |
a=.6 |
a=.9 |
a=0.99 |
| |
|
|
|
|
|
|
|
|
|
| acalc-a |
| -2 |
0.12 |
0.10 |
0.01 |
0.01 |
-0.01 |
0.01 |
0.11 |
0.06 |
0.01 |
| -1 |
0.01 |
0.01 |
0.01 |
-0.04 |
-0.03 |
0.01 |
0.08 |
0.02 |
0.01 |
| 0 |
-0.02 |
-0.02 |
0.01 |
-0.03 |
-0.03 |
0.00 |
0.06 |
0.00 |
0.01 |
| 1 |
-0.02 |
-0.02 |
-0.00 |
-0.01 |
-0.02 |
-0.00 |
0.06 |
-0.00 |
0.00 |
| 2 |
-0.00 |
-0.01 |
-0.00 |
0.01 |
-0.01 |
-0.00 |
0.06 |
-0.00 |
-0.00 |
| 3 |
0.00 |
-0.00 |
-0.00 |
0.02 |
-0.00 |
-0.00 |
0.07 |
-0.00 |
-0.00 |
| 4 |
0.00 |
-0.00 |
-0.00 |
0.04 |
-0.00 |
-0.00 |
0.07 |
0.00 |
-0.08 |
| |
|
|
|
|
|
|
|
|
|
| Percent Errors |
| -2 |
20 |
11 |
1 |
2 |
-1 |
1 |
19 |
6 |
1 |
| -1 |
1 |
1 |
1 |
-6 |
-4 |
1 |
13 |
2 |
1 |
| 0 |
-4 |
-2 |
1 |
-5 |
-3 |
0 |
10 |
0 |
1 |
| 1 |
-4 |
-2 |
-0 |
-2 |
-2 |
-0 |
10 |
-1 |
0 |
| 2 |
-0 |
-1 |
-0 |
1 |
-1 |
-0 |
11 |
-0 |
-0 |
| 3 |
0 |
-0 |
-0 |
4 |
-0 |
-0 |
11 |
-0 |
-0 |
| 4 |
0 |
-0 |
-0 |
7 |
-0 |
-0 |
12 |
0 |
-8 |
| |
|
|
|
|
|
|
|
|
|
| gcalc-g |
| -2 |
0.00 |
0.00 |
0.00 |
-0.50 |
-0.36 |
-0.44 |
-0.46 |
-0.27 |
-0.30 |
| -1 |
0.00 |
0.00 |
0.00 |
-0.23 |
-0.14 |
-0.14 |
-0.23 |
-0.11 |
-0.12 |
| 0 |
0.00 |
0.00 |
0.00 |
-0.09 |
-0.05 |
-0.06 |
-0.12 |
-0.04 |
-0.04 |
| 1 |
0.00 |
0.00 |
0.00 |
-0.03 |
-0.01 |
-0.02 |
-0.09 |
-0.01 |
-0.01 |
| 2 |
0.05 |
0.05 |
0.03 |
-0.00 |
0.01 |
0.01 |
-0.08 |
-0.01 |
-0.01 |
| 3 |
0.05 |
0.07 |
0.03 |
0.02 |
0.03 |
0.02 |
-0.07 |
-0.00 |
-0.00 |
| 4 |
0.05 |
0.09 |
0.03 |
0.05 |
0.04 |
0.02 |
-0.07 |
0.00 |
-0.84 |
| |
|
|
|
|
|
|
|
|
|
| Percent Errors |
| -2 |
-- |
-- |
-- |
-100 |
-73 |
-87 |
-53 |
-31 |
-35 |
| -1 |
-- |
-- |
-- |
-45 |
-27 |
-28 |
-26 |
-13 |
-14 |
| 0 |
-- |
-- |
-- |
-17 |
-10 |
-11 |
-14 |
-4 |
-4 |
| 1 |
-- |
-- |
-- |
-6 |
-3 |
-4 |
-10 |
-1 |
-2 |
| 2 |
-- |
-- |
-- |
-0 |
3 |
2 |
-9 |
-1 |
-1 |
| 3 |
-- |
-- |
-- |
5 |
6 |
3 |
-8 |
-0 |
-1 |
| 4 |
-- |
-- |
-- |
11 |
8 |
3 |
-8 |
0 |
-96 |
|
Tables 6.1 and 6.2 indicate how the approximate delta-Eddington
model used in the iteration procedure affects the optical properties
calculated. For both cases (fixed collimated transmission and
fixed anisotropy) the errors are least when the albedos are large.
Changes in the anisotropy have little affect upon the accuracy
of the calculated optical properties. Increasing optical thickness
tends to decrease percent error. The method should not be used
with thin samples ( 1) because of the large errors in the
calculated values. However for any albedo, any anisotropy, and
optical thicknesses larger than one, the inverse method has intrinsic
errors less than ten percent when the collimated transmission
is known (Table 6.2).
|