Geology Reference
In-Depth Information
(
)
X
N
y
¼
f
ð
x
Þ ¼
1 a i K
ð
x i ;
x
Þ
b
ð 4 : 61 Þ
i
¼
where K is the kernel function,
a i and b are parameters, N is the number of training
data, x i are vectors used in training process, and x is the independent vector. The
parameters
owchart
on the SVM model selection in general rainfall-runoff modeling is shown in
Fig. 4.17 as per the study by Bray and Han [ 14 ].
As shown in Fig. 4.17 , the whole system is complex, and the selection of a better
model structure would require a large number of trial and error attempts, such as
making adjustments to rainfall scale factor,
a i and b are derived by maximizing their objective function. A
flow scale factor, cost factor, kernel
functions, and the parameters for the kernel functions. Many of these factors are
very sensitive and a wrong setting could result in an extremely long training time
and unstable results. Hence, it is very dif
cult to automate the selection process.
Bray and Han [ 14 ] have made an attempt to explore the relationships among
different factors which in
c
catchment. Before going for modeling, the modeler needs to make decisions about
the modeling scheme and how to pre-process the data, what kernel to use, and
several setting of parameters.
uence the SVM model development under a speci
Fig. 4.17 Schematic flow chart showing modeling procedures in SVM modeling (case study
rainfall-runoff modeling)
 
Search WWH ::




Custom Search