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International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B4. Istanbul 2004
Atmospheric | dependent good band relative
correction | variables combinations qpeíficien
SS R1/In(R3) 0.292
No Chia In(R1+R3)/In(R2) 0.51
In(R1*R3)/In(R2) (0.572
d R1/In(R3) 0.411
Yes (R1+In(R2))/In(R3) 0.428
Chl-a In(R1+R3)/In(R2) 0.64
Tablel. Results of Regression analysis
3.2 Analysis
Table 1 showed that:
€ Most combinations had bad relative coefficients between
concentration of water quality component and remote
sensing. data.
€ As Table l, only six combinations were extracted from
the total 356, but their relative coefficient were still not
good.
€ Relative coefficient could be improved a little after
atmospheric correction.
€ It was hard to build an applicable regression model for
quantitative analysis of Case II water body.
The main reason was:
€ Water components interacted each other strongly.
Relations between image bands and water components
were crossed and non-corresponding relative.
€ The wider band width also decreased their relativities.
4. THE ARTIFICIAL NEURAL NETWORK
INVERSING MODEL
Theoretical research has proved that if an ANN includes biases,
at least a S-style cryptic layer and a linear output layer, it can
approach any rational function (Cong, 1998). And theoretical
research of water color remote sensing indicates that remote
sensing data are correlated with water body components and
their concentrations directly after atmospheric effect is
removed . However, because water body ingredients affect each
other, traditional inversing method, such as building a relative
function between band data and components cannot solve it.
The artificial neural network is suitable to simulate such
complicated relationship. Therefore, theoretically, it is feasible
to use ANN in water color remote sensing inversing research.
4.1 Model Structure
Figure 4 showed a concept chart of artificial neural network
structure used in this study. Every input node represented a TM
band, and these input data were distributed to each node of
cryptic layer to operate. Output values of cryptic layer were
inputted into output layer and operated again. The output values
of output layer were parameters interested by users.
t Kuang, C., 1999. Identification of Water Color Remote
Sensing Theoretical Model and Several Aspects in Its
Solution. Tsinghua University doctoral dissertations, pp.
15~86.
679
Figure 4. The structure of artificial neural network
In detail, the paper adopted a two layer BP artificial neural
network.
p; (i-1* r), r-5, represented five inputs which were bandl to
band5 of TM image data;
IW, , represented the weight between inputs and neural cells of
first layer. lw, represented the weight between outputs of
first layer and neural cells of second layer.
2
b and b^ were biases of neural cells of first and second layer
respectively.
f^ f was transfer functions. f! often adopted S-style
transfer function, in this paper the model used hyperbolic
2
tangent S-style transfer function. f adopted linear transfer
function. Theoretical research has proved that an ANN, which
has biases and at least a S-style cryptic layer and a linear output
layer, can approach any rational function (Cong, 1998);
2 ^
a! and a? were output values of first and second layer (see also
Figure 4):
a - f'üW, "pb
a mf" LW *a vb)
m, the number of neural cells in the second layer, was
determined by amounts of object of ANN model object. The
paper hoped that this ANN model could simulate SS, CODy,,,
DO, TP, TN and chl-a, so m=6;
s, the number of neural cells in the first layer, was determined
by neural network training process. According to results of the
paper, s was equal to 10.
4.2 Training Results and Its Analysis
4.2.1 Data of Model Training and Verifying
Generally the input data should be normalized in order to
improve training efficiency and accuracy of neural network
(Zhan ,2000). Table 2 gave the input data and object values.