Plant development and maturity (as opposed to growth or increase
in size) cause many changes in canopy geometry, moisture content, and
pigmentation of leaves which are also manifested in the reflectance |
characteristics of canopies. Figure 3 shows the spectra of spring |
wheat at several different maturity stages. A plot of spectral re- ;
sponses through the season in selected wavelength bands is shown in
Figure 4. The temporal pattern of changes in spectral response has :
been demonstrated by the LACIE project to be an important feature for
identifying wheat from Landsat MSS data. |
Plant maturity affects canopy reflectance throughout the growing ;
season; however, the variation early in the growing season caused by |
different planting dates was considerably reduced by the time of plant
heading. Percent soil cover, leaf area index, and plant water content 1
had high linear correlations with reflectance in most wavelength bands
and reflectance was sensitive to changes in these variables throughout
the growing season. On the other hand, reflectance was only sensitive
to changes in fresh and dry biomass early in the season. The 0.76-0.90
um wavelength band has a high correlation with each crop canopy variable
early in the growing season indicating a sensitivity to small amounts
of biomass. As the canopy begins to ripen there was a significant de-
crease in the capability to estimate the amount of vegetation present.
Leamer et al.(1978) reported a similar decrease in the correlation of
spectral response with canopy variables after heading for winter wheat.
Correlation of Canopy Variables with Reflectance
The linear correlation of the five different crop canopy variables
with the thematic mapper and Landsat MSS bands are summarized in Table l.
The relationships of four of these with spectral reflectance are illus-
trated in Figures 5 and 6. Percent soil cover, leaf area index, and
plant water have a high correlation with spectral reflectance in each
of the six thematic mapper bands (Figures 5 and 6). The relationship
of reflectance to fresh and dry biomass is non-linear, resulting in
lower correlation values (Figure 6).
The middle infrared band, 2.08-2.35 um, has the highest correlation
of the six individual thematic mapper bands with fresh biomass, dry
biomass, and plant water, and is highly correlated with leaf area index
and percent soil cover. These results illustrate the importance of
making measurements in several regions of the spectrum, espe-
cially in the middle infrared wavelength region which is not measured
by the present Landsat multispectral scanners.
Correlations of the four Landsat MSS bands with the same five crop
canopy variables are also shown in Table 1. The correlation of canopy
variables with each Landsat MSS band is less than with the corresponding
thematic mapper band. The lower correlation is attributed to the width
and location of the bands with respect to the spectral characteristics
of vegetation.