GREE
Axis N GVI IPVI ND TVI
NESS
I 0.7340 | -0.9673 | -0.2756 | 0.8746 | 0.8622
2 0.1738 | 0.1960 | -0.9519 | 0.1359 | 0.2095
3 0.5125 | 0.1605 | 0.1340 | 0.4491 | 0.4354
4 |-0.4101 | 0.0071 | 0.0015 | 0.1178 | 0.0580
5. |-0.0131 | 0.0000 | 0.0016 | -0.0321 | 0.1404
Table 2. Correlation Between Input Rasters and Principal
Components
The relationship between vegetation cover and the indices
appears to change over the area according to the certain
conditions such as soil cover type. To minimize the effect
of soil on vegetation reflectance, second set of indices
were used. These indices were Soil Adjusted Vegetation
Index (SAVI), Modified Soil Adjusted Vegetation Index 1
(MSAVII), and Modified Soil Adjusted Vegetation Index
2 (MSAVI2) (Table 1). For this study the first PC acquired
from the 3 soil indices contains the spectral information
adequate for the classification to normalize the effects that
emerge due to the different soil types of the areas with low
canopy of vegetation.
(Table 3)
Axis| MSAVI | MSAVD | SAVI ses
0
L| 0,9999 | 0.0789 | 0.0046 | 84.4805
2 | 0.0145 | 0.9969 |-0.0629| 15.5186
3 | -0.0000 | 0.0000 | 0.9980 | 0.0009
Table 3. Correlation Between Soil Adjusted Vegetation
Indices and Principal Components
Besides these feature extraction oriented indices, PCA
were performed on raw bands in order to find if vegetation
related information could be collected in few explanatory
bands. In this transformation, examination of principal
components eigenvector loadings determine which PC
possesses information related directly to the spectral
signatures of vegetation. Eigenvector loadings for PC2 in
Table 4 indicate that PC2 describes the difference between
the visible channels (TM1, 2, and 3) and the infrared (IR)
channels (TM5 and 7) and also this component is
commonly thought to be related to vegetation. Eigenvector
loadings for PC3 (in Table 3) indicate that PC3 is
dominated by vegetation. In this component both the
loading values of TM3 and TM4 is negative but the
difference between these two band were high because in
TM3 chlorophyll is absorbed, on the contrary chlorophyll
is highly reflected in the near infrared band. Therefore
PC2 and PC3 were selected as feature components.
206
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004
Eigen
Axis | TMI TM2 TM3 TM4 TM7 TMS | values
(%)
: : 4 85.731
] 0.9160 | 0.9667 | 0.9781 0.6093 | 0.9615 | 0.9329 0
2 -0.3436 | -0.2114 | -0.1570 | 0.6718 | 0.1201 | 0.3008 | 9.2461
3 ]|-0.1460 | -0.1245 | -0.0459 | -0.4201 | 0.2347 | 0.1756 | 3.9920
4 -0.1408 | 0.0019 | 0.1247 | -0.0047 | -0.0164 | -0.0336 | 0.6456
5 -0.0100 | 0.0107 | -0.0155 | 0.0286 | 0.0756 | -0.0846 | 0.2556
6 0.0394 | -0.0720 | 0.0284 | 0.0104 | 0.0070 | -0.0099 | 0.1296
Table 4. Correlation Between Input Rasters and Principal
Components
In addition to principal component bands, Decorrelation
Stretched (DS) bands were used in this study. Even though
these bands still show the properties of the original bands,
the color separation of these bands are enhanced with
significant band to band correlation. Decreasing the
correlation of spectral data corresponds to exaggerating
the color saturation without changing the distribution of
hues (or relative color composition) (Gillespe et al., 1987).
At the end of these analyses it is assumed that; selecting
PCI and PC2 of vegetation indices, PCI of soil indices,
PC2 and PC3 of raw bands and DC3 and DC4 as feature
components will remove the redundant data among
multivariate datasets, such as multispectral remote sensing
images and increase the accuracy of the classification.
Classification with Raw Bands
EN Black Pine
EEE] Calabrian Pine
(7) Taurus Cedar
2] Taurus Fir |
CZ) Sparse Vegetation |
LL Bare Area i
L i
ES Fannland
Figure 2. Classification results of both raw bands and
feature components.
By using these feature components overall accuracy was
increased to 76.92 %. This rise shows that the new formed
bands were very successful in the discrimination of
vegetation classes with very similar spectral reflectance
values.
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