Pm. Teillet et al., EFFECTS OF SPECTRAL, SPATIAL, AND RADIOMETRIC CHARACTERISTICS ON REMOTE-SENSING VEGETATION INDEXES OF FORESTED REGIONS, Remote sensing of environment, 61(1), 1997, pp. 139-149
Vegetation indices derived from satellite image data have become one o
f the primary information sources for monitoring vegetation conditions
and mapping land cover change. The most widely used vegetation index
in this context is NDVI, the normalized difference vegetation index, w
hich is a function of red and near-infrared spectral bands. Given that
the spectral and spatial characteristics of imagery in the red and ne
ar-infrared vary from sensor to sensor, NDVI values based on data from
different instruments will not be directly comparable. The present st
udy demonstrates the impact of changes in spectral bandwidth and spati
al scale on NDVI derived from Airborne Visible/Infrared Imaging Spectr
ometer (AVRIS) data acquired at 20-m resolution over a forested region
in southeastern British Columbia. For this purpose, the 10-nm AVIRIS
data were spectrally and spatially aggregated in the red and near-infr
ared to simulate bandwidths from 10 nm to 150 nm for ground resolution
s varying from 20 m to 1100 m. Sensor-specific spectral bands and spat
ial resolutions such as those for SPOT HRV, Landsat TM, NOAA AVHRR, EO
S MODIS, and Envisat MERIS were also generated. NDVI values were then
calculated using atmospherically corrected surface reflectances for fo
restry-related targets for the entire simulated band set at the variou
s scales. The results indicate that the NDVI is significantly affected
by differences in spectral bandwidth, especially for the red band, an
d that changes in spatial resolution lead to less pervasive but more l
and cover specific effects on NDVI. Results for the forested regions a
lso indicate that NDVI is not very sensitive to the location of the ne
ar-infrared spectral band, provided that the bandwidth is no wider tha
n 50 nm and the atmospheric correction for water vapor absorption is a
dequate. If either proviso is relaxed, the wavelength placement of the
near-infrared spectral band is more critical, the optimum location be
ing in the 850-880 nm range. Finally, for the same forest targets, som
e results were also generated for several other vegetation indices tha
t make straightforward use of atmospherically corrected red and near-i
nfrared spectral bands. (C) Elsevier Science Inc. 1997.