Full text: Technical Commission VIII (B8)

  
ampling plots. The 
osen for analysis 
of northeast Iran 
naturally. Annual 
and the study site 
en 379203] |9"-— 
0"E. The elevation 
21 to 27 degrees. 
m) in a 13 x |3 
lomly chosen for 
ically 3-4 m high, 
These forests are 
sharpening) 
  
mpling plots. The 
ysen for analysis 
] in July 2008 by 
2006. ALOS data 
and multispectral 
ea, and are not too 
truments on-board 
trument for Stereo 
‘and Near Infrared 
r digital elevation 
ions, respectively. 
ith 2.5-m spatial 
| a wavelength of 
a visible and near 
yastal zones with a 
four multispectral 
0 pm), red (0.61- 
JAXA EORC). 
Vegetation indices 
In remote sensing applications, the most commonly used 
vegetation index for detecting vegetation. Here you can see the 
properties of each vegetation index that introduce by others 
scientist (Table 1). 
New vegetation index 
In arid and semi-arid regions, soil background has more 
reflectance in the near infrared (NIR) and red (RED) 
wavelengths of vegetation. Soil components that affect spectral 
reflectance include color, roughness, and water content. 
Roughness also has the effect of decreasing reflectance because 
of an increase in multiple scattering and shading. RED-NIR 
scattergrams, termed the “soil line”, are used as a reference 
point in most vegetation studies. The problem is that real soil 
surfaces are not homogeneous and contain a composite of 
several types. Analysis has shown that for a given soil 
characteristic, variability in one wavelength is often functionally 
related to reflectance in another wavelength. Vegetation cover is 
usually sparse compared to soil background and soil and plant 
spectral signatures tend to mix non-linearly. Thus, arid plants 
tend to lack the strong red edge found in plants of humid 
regions due to ecological adaptations to the harsh desert 
environment. We decided to introduce a new vegetation index 
based on total wavelength (visible and NIR). The TRVI is the 
ratio of NIR and the sum of visible and NIR wavelengths, and is 
calculated using the following equation: 
TRVIZ4 —— ——5——— — 
RR G+B) 
NIR-RED (1) 
where RED and NIR stand for spectral reflectance 
measurements acquired in the red and near-infrared regions, 
respectively. For this equation, the normalized difference is 
divided by the total of visible and near infrared wavelengths. In 
this equation, “4” is the measured reflectance. In fact, this 
équation shows the ratio of the normalized difference of 
reflectance and measured reflectance of all bands, i.e., the four 
bands in the multispectral image. In this study, TRVI was used 
fo estimate the stand density of Persian juniper and wild 
pistachio trees. 
  
Vls 
  
  
  
  
  
  
Formula Presented | Summary 
Ta Rouse et al. | RED and NIR stand for 
Differenee | A DVI = NIR- RED (1974) spectral reflectance 
Vegetation TT NIR+ RED measurements acquired 
Index in the red and near- 
(NDVI) infrared regions, 
respectively 
Soil- Heute (1988) L indicates the  soil- 
Adjusted brightness dependent 
Vegetation correction factor that 
Index (NIR - RED) (1 + L) compensates for differences 
(SAVD SAVIZ— AL in soil background 
NIR+RED+L condition, L=1 low 
vegetation densities, L=0.5 
intermediate vegetation 
densities and L=0.25 higher 
voi densities 
ae Qictal (1994) | The dynamic range of the 
: MSAVI - 12x; -((ZXNIR 3) -8x(NIR-RED)| inductive MSAVI was 
Sen BENANNT SUR RED] slightly lower than that of 
ue the empirical L function 
E due to differences in L 
NNI boundary conditions 
um Rondeaux et al. The value of 0.16 in this 
= NIR-RED (1996) formula was found to 
med OSAVI = . (NIR-RED) . produce a satisfactory 
VERTU NIR+RED+0.16 reduction in soil noise, both 
ANT for low and high vegetation 
L(OSAVD | cover 
  
  
  
  
  
Table 1. The properties of conventional vegetation indices 
    
   
   
   
   
   
   
   
   
    
  
    
   
     
     
    
     
    
   
   
   
     
   
      
   
  
  
  
  
  
     
       
    
      
  
    
  
  
   
    
    
     
  
   
  
  
Tree counting 
Using a GPS device, we located the centres and corners of each 
9-ha plot based on satellite imagery input to the GPS. Then, 
starting in a plot corner, we measured densities of juniper and 
pistachio trees on all the plots. This was done in cooperation 
with the regional natural resources organization. 
Methods of analysis 
We calculated linear regression coefficients between tree 
density and vegetation index values. Tree density for each plot 
was obtained from the field surveys. Vegetation indices were 
calculated using ALOS satellite data for each 9-ha plot (14400 
data points). Subsequently, we used 5x5 maximum filtering 
algorithms for vegetation index data from each plot to 
determine the optimum maximum spectral value for pistachio 
and juniper trees. We also calculated frequency results for 5x5 
maximum filtering of vegetation indices from each plot. Finally, 
simple linear regressions between tree density and vegetation 
index values were calculated based on the best threshold 
vegetation index values. All of these analyses were performed 
using ENVI (Environment for Visualizing Images) software, 
service pack 1, and Microsoft Excel 2007. 
3. RESULTS AND DISCUSSION 
3.1 Relationship between vegetation indices and tree 
density for the 5x5 maximum filtering algorithm for 
pistachio 
A simple linear regression between the conventional vegetation 
indices, new TRVI vegetation index and tree density based on 
the 5x5 maximum filtering algorithm was calculated. For all of 
the vegetation indices, the relationship between tree density and 
vegetation value was positive. NDVI and OSAVI had similar R? 
values and plot distributions and higher than other vegetation 
indices. 
According to Colwell (1974), background reflectance can have 
an important effect on canopy reflectance, especially with low 
values of percentage vegetation cover (Figure 5). 
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