Vegetation Spectral Feature Extraction Model
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Net height of infrared platform-HI: the difference between the averaged reflectance of NIR platform and the reflectance of point R. It can be substituted by the reflectance difference of R and the midpoint of line I1I and reflects the feature of platform I1I:
HI=(å((Ri+Ri+1)×(li+1-li)/2))/Dl-RR»(RI1+RI)/2-RR,
where liÎlI1-930nm, Dl is the width of NIR=930-lI1.
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FWFH of green peak-lwG: generally represents the width of green peak. It is approximately calculated as the horizontal interval between points B and Y:
lwG »lY-lB
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FWFH of red absorption peak-lwR: the reflection of the width of red "valley". It is calculated as the half width of continuum-removed red "valley" and can be replaced as the horizontal interval of line YV:
lwR»lV-lB
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Averaged reflectance of NIR platform-RIa: can be substituted by the reflectance average of I1 and I:
RIa=(å((Ri+Ri+1)×(li+1-li)/2))/Dl»(RI1+RI)/2=HI+RR
where liÎlI1-930nm, Dl is the width as 930-lI1.
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Area of green peak-AG: the integrated area under curve MBGYR. It is the embodiment of green peak intensity and can be approximately substituted by the area under multiline MBGYR:
AG=(å((Ri+Ri+1)×(li+1-li)/2))
»[(å(Rp+Rp+1)×(lp+1-lp)/2)),p=M,B,G,Y]
where liÎlM-lR.
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Pure area of green peak-AG': the integrated area enveloped by curve MBGYR and line MR. It is the net intensity of green peak and obviously can be replaced by the area of polygon MBGYRM:
AG'=AG-((RM+RR)×(lR-lM)/2)
»[(å(Rp+Rp+1)×(lp+1-lp)/2)],p=M,B,G,Y]
-((RM+RR)×(lR-lM)/2)
where liÎlM-lR
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Net area of red absorption peak-AR: the area enclosed by curve GYRVI1 and line GI1. It can estimate as the area of polygon GYRVI1G:
AR=SGYRVI1G
Other parameters can also be gotten if necessary. For instance, after removing the continuum, the 5 most intensive peaks can be extracted from the continuum-removed(named as
ldi with i increasing with intensity decrease) and normalized continuum-removed results(
lci).
It should be pointed out that the usually applied parameters in vegetation study such as NDVI, red edge
lre and red edge slope dr
re could also be obtained from these parameters as follows:
NDVI=(R
I1-R
R)/(R
I1+R
R) ,
lre=
lV , dr
re»S
V
Therefore, the definition of eight feature positions not only reflects the general feature of the reflectance data, but also can get many high-information-content feature parameters that may have good relationships with
some property parameters of vegetation such as chlorophyll concentration.
3.2 Analysis for Effectiveness of VSFEM---Relative Stability of Position
To study characteristics of the above feature positions and parameters , especially to study relationships between feature positions and vegetation types , as well as action of feature parameters for reflecting vegetation parameters . Based on above definitions and algorithms , more than 100 spectral data of about 20 types of vegetation in Chang Zhou were analyzed to get spectral feature positions and parameters.
Table 1 gives principle results , from which we can see that ,
under the research conditions of the experiment , all feature positions , especially 8 feature positions are stable , these positions are : M:404, B:525, G:556,Y:573,R:671,V:723,I1:758,I :900nm,
take I position as example , which has the largest change range , for 62 samples at different time and place , its confidence width is 6.4nm , others less than 3nm , even for standard deviation , are less than 6nm generally . This kind of confidence interval has been super than spectral resolution of many instruments .
Table 1 feature position statistics result based on 62 samples
| Feature position |
samp les |
aver age(nm) |
Stand ard devia tion |
Relat ive error(%) |
95%confid ence(nm) |
Range of 95%confidence(nm) |
Width of 95%confi dence(nm) |
| lB |
62 |
524.7 |
1.04 |
0.20 |
0.3 |
524.5 - 525.0 |
0.5 |
| lG |
62 |
556.2 |
3.67 |
0.66 |
0.9 |
555.3 - 557.1 |
1.8 |
| lI |
62 |
900.7 |
12.77 |
1.42 |
3.2 |
897.5 - 903.8 |
6.4 |
| lI1 |
62 |
758.3 |
7.01 |
0.92 |
1.7 |
756.5 - 760.0 |
3.5 |
| lM |
62 |
403.9 |
2.72 |
0.67 |
0.7 |
403.3 - 404.6 |
1.4 |
| lR |
62 |
671.4 |
2.40 |
0.36 |
0.6 |
670.8 - 672.0 |
1.2 |
| lV |
62 |
723.4 |
9.80 |
1.35 |
2.4 |
720.9 - 725.8 |
4.9 |
| lY |
59 |
573.2 |
0.81 |
0.14 |
0.2 |
572.9 - 573.4 |
0.4 |
3.3 Rediscussion for VSFEM---Reduction of Some Feature Positions
In addition , we calculate the correlation coefficients between different bands for all the spectral vegetation data measured by Se590 to show the independence of the bands and to select the most information-containing band group in order to indicate more efficiently the difference among different vegetation species , through which we can prove the effectiveness of VSFEM
where S is the correlation coefficient matrix of all bands, r
ij is the absolute value of correlation coefficient between band i and band j. Obviously:
r
ij=r
ji=|L
ij/SQRT(L
iix L
jj)|
where L
ij is the covariance between band i and band j.
Fig. 2 is the simulated image of the correlation coefficient matrix among 187 bands that is calculated on the base of 71 vegetation . Curves in
Fig. 2 are isolines , from diagonal line to outside , the values are 0.9999,0.999,0.99,0.95,0.9,0.5,0.3 and 0.1 in the order .
From
Fig. 2 we can see that ,
Except band 100(band number of Se590) to 126 , for vegetation , correlation coefficient are all very high (more than 99.99% generally) , that is to say, it's practical for band reduction .It shows two high-correlative platforms of 400-670nm and 760-950nm respectively, which means within these two regions , a few bands are enough to extract vegetation information . Moreover , around 550nm and 670nm , there are relatively wider areas . It's unnecessary to subdivide bands in these regions . but between 675nm---775nm and around 522nm and around 573nm , correlation coefficient are low generally . This shows more information here and bands should be subdivided . compared to 8 feature positions referred before , we can get that , for vegetation research , those regions that should be subdivided are just blue edge B , yellow edge Y and red edge V, while those regions that needn't be subdivided are blue absorption valley M , green peak G , red absorption valley R , and NIR platform I . In
Fig. 2 , position B , Y and V are located in the center of narrow regions of isolines , while M , G , R , I in the center of broad regions . The arrows in
Fig. 2 explain this clearly .