Full text: Resource and environmental monitoring (A)

  
   
   
  
   
  
  
   
  
  
  
  
  
  
  
  
  
  
  
  
  
    
    
  
    
     
   
   
  
  
  
   
    
   
     
   
    
   
  
  
   
    
   
   
   
  
  
    
   
     
  
    
   
  
    
   
  
  
  
   
  
   
  
  
  
    
DEL 
ARTS OF 
along with IRS - 
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nodel parameters 
sses are extracted 
asthan along with 
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ngle independent 
the BRDF model 
; have been made 
r of parameters, 
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-empirical BRDF 
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it is capable of 
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s including LAI, 
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egistered MODIS 
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k and Li-Sparse 
ngth regions, at a 
BD). These three 
ne and geometric 
IAPRS & SIS, Vol.34, Part 7, *Resource and Environmental Monitoring", Hyderabad, India,2002 
  
components of radiation reflected from the target respectively, 
and have physical interpretation in terms of underlying surface 
parameters such as LAI (Leaf Area Index), leaf reflectance, soil 
reflectance etc. The isotropic (angle independent) term 
represents surface reflectance with sun at zenith and nadir view, 
while the volume and geometric terms represent the anisotropic 
contributions to surface reflectance. While semi-empirical 
BRDF models have been used quite widely to normalize multi- 
angular remotely sensed data of wide swath sensors to a 
common geometry (Leroy and Roujean 1993), there have been: 
relatively few attempts to explore the inherent information 
content of the model coefficients (Roujean et al, 1997). 
In this paper, an attempt has been made to analyze empirically 
the relation between MODIS BRDF model coefficients in the 
red and near infrared wavelengths with different land cover 
classes as well as LAI field measurements carried out at the 
Central State Farm, Suratgarh, Rajasthan, India. 
2. STUDY AREA AND DATA USED 
2. Study Area 
The study area consists of parts of Western India, viz. Gujarat 
and Rajasthan. The area is mostly semi-arid with an average 
annual rainfall of 20 to 25 cms. During the month of December, 
the period under study, wheat was in the crown root initiation 
stage while mustard and gram crops were at flowering stage. 
2.2 Data Used 
A 10 deg by 10 deg tile MODIS BRDF product (MOD43BI 
version 003) covering the study area (-1200 *1200 km) was 
used along with the corresponding IRS WiFS and LISS-III data. 
The geographical bounds of the study area are 20 deg N — 30 
deg N and 69 deg E — 80.deg E. The details are given in 
Tablel. 
Table 1: Satellite sensors used in the study 
  
  
  
  
  
S.No | Satellite/ Date of Wave- Spatial 
sensor acquisition length resolution 
(Path/ (nm) (m) 
Row) 
1 EOS/MO Dec 01- 620-670, 925.6 
DIS 015, 01 841-876 
BRDF 
product 
2 IRS- 14 Dec 01 | 620-680, 180.0 
1D/WiFS 770-860 
(P94-R53) 
3 IRS- 11 Dec 01 | 620-680, 239 
1D/LISS- 770-860 
III(P93- 
R50) 
  
  
  
  
  
  
3. METHODOLOGY 
3.1 Extraction of BRDF Model Coefficients 
As mentioned above, the MODIS BRDF product (MOD 43B1) 
available in HDF-EOS format in ISIN (Integerised Sinusoidal) 
Grid consists of three BRDF model coefficients, viz., the iso- 
tropic (fiso), Ross-Thick (fvol) and Li-Sparse (fgeo) coeffi- 
cients representing the angle-independent, volume and geomet- 
ric contributions to surface reflected reflectance. These 
coefficients are given for each of seven spectral bands and three 
broad bands and shape parameters representing surface anisot- 
ropy in the red and NIR wavelengths are also available in the 
product. The BRDF model coefficients as well as the shape pa- 
rameters corresponding to red and NIR bands were extracted 
from the MODIS BRDF product and converted into GeoTiff 
format in geographic latitude-longitude coordinates using the 
Modis Reprojection Tool (MRT). 
3.2 Comparison with IRS-1D WiFS data 
The IRS-1D WiFS data of spatial resolution 188 m was 
resampled to ~ lkm resolution using relevant modules of 
ERDAS-IMAGINE software operating on SGI workstation. 
The degraded WiFS image was registered to MODIS image 
using a number of GCP's distributed throughout the image. The 
maximium error in the scan and pixel directions was less than a 
pixel in scan and pixel directions. Various land cover classes 
such as sand, crops (mustard), shallow water and deep water 
were identified on the WiFS image and corresponding three 
BRDF model coefficients along with three shape parameters 
were noted from the MODIS BRDF product for further 
analysis. 
3.3 Field measurements of LAI 
Field measurements of LAI were carried out during December 
14-17, 2001 at the Central State Farm, Suratgarh using the 
LICOR-2000 Plant Canopy Analyser. The Central State Farm 
spans an area of ~ 12, 000 ha with an average field size of 250 
* 250 m. The dominant crop in the rabi season is gram followed 
by mustard and wheat crops. For each field, measurements 
were carried out at four locations, and for each location six A 
and B readings of LICOR-2000 were taken to obtain 
representative LAI values for that location. The field LAI was 
computed as an average of LAI values of the four locations. 
Measurements were carried out for seven fields including 
mustard, gram and wheat crop. The measured LAI values 
ranged from 1.152 to 3.235 with combined standard deviation 
range of 0.198 to 0.90. 
3.4 Comparison with IRS-1D LISS-III data 
A sub scene (540 lines * 540 pixels) containing the Central 
State Farm, Suratgarh, Rajasthan farm was extracted from the 
IRS 1D LISS-III data and was registered to a georeferenced 
LISS-IH scene of the same area with sub-pixel accuracy 
(RMSE=0.19 and 0.26 in the pixel and scan directions 
respectively). Using the gain and offset of the IRS LISS-III 
sensor along with extraterrestrial irradiance in red & NIR 
wavelengths and solar zenith angle, an apparent reflectance 
image was generated in the red & NIR wavelengths. 
Atmospheric path radiance effects were taken into account 
approximately by subtracting deep-water body reflectance at 
both wavelengths (~ 6.6 % in red and 5.2 % in NIR) and 
subsequently the NDVI image was generated. The fields where 
LAI measurements were carried out were delineated in the 
image, a linear regression relation was developed between 
NDVI, and field measured LAI, which is given below: 
LAI = 3.0486 * NDVI — 0.8256 (N=6, R*=0.81) (1)
	        
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