to be composed of 57-meter-square pixels. Other investigators have warned of
problems in using Landsat data in this format for water quality studies (Olsen,
et al., 1981). They showed that resampling can alter band 6 and band 7 data
for water bodies by as much as seven counts. However, it was not possible to
obtain a copy of this image in a nonresampled format.
Table 1 lists the band passes sensed by the Landsat multispectral scanner.
Table 1. - Band passes sensed by the Landsat
multispectral scanner
Channel Wavelength band (um) Color/spectrum
4 9. 5-—-0. 60 Green
5 0.6 - 0.70 Red
6 0.7 - 0.80 Near infrared
7 0.8 - 1.10 Near infrared
About 25 percent of the surface area of the reservoir was obscured by clouds
and their shadows (see figure 1).* Also on September 9, 1981, the EPA acquired
imagery of the reservoir with an airborne Daedalus Model 1260 eleven channel
multispectral scanner. Six flight lines were flown between 9:40 and 10:50 a.m.
MDT, at an altitude of 6560 meters above mean sea level, yielding a nominal
pixel size of 11.5 meters square. Clouds and their shadows impaired the utility
of the data obtained for the lower reaches of the reservoir. Table 2 lists
the ten band passes used in this study. Figure 2 shows an example of this
imagery. The data were received in the remote sensing laboratory in the form of
computer compatible tapes produced at the EPA Environmental Monitoring Systems
Laboratory in Las Vegas, Nevada.
Table 2. - Airborne multispectral scanner
channels used in this study
Channel Wavelength band (um) Color/spectrum
1 0.38 - 0.42 Near ultraviolet
2 0.45 - 0.50 Blue
3 0.50 - 0.55 Green
4 0.55 - 0.60 Green
5 0.60 - 0.65 Red
6 0.65 - 0.70 Red
7 0.70 - 0.79 Near infrared
8 0.80 - 0.89 Near infrared
9 0.92 - 1.10 Near infrared
10 8.00 - 14.00 Thermal infrared
ANALYSIS OF LANDSAT DATA
The water quality specialists who had sampled the reservoir supplied the remote
sensing lab with 1:62 500 scale maps annotated to show sample site locations.
* Figures are at end of paper.
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