Lab
#3 - Reflectance, Energy
Interactions & Earth Surface Features
The purpose
of this exercise is to gain an awareness of several fundamental
aspects of reflected radiation and spectral response patterns for
different features, e.g. vegetation, soil and water. Although satellite
images of this type, with the different ranges of the spectrum separated,
are different than aerial photography, which combines all the colors,
knowledge of how different surfaces reflect in certain wavelength
regions is important for air photo interpretation.
In this exercise, it is assumed
that filters are used to effectively block out all available energy
except the wavelength regions given, i.e. the "blue band" is only
the reflected blue light, the "red band" is only the reflected red
light etc.
The idea here is to familiarize
yourself with which wavelengths maximize class separability, knowledge
of this may be able to help you choose the proper film and/or filter
combinations for a given aerial photographic application.
Band 1
(0.45 to 0.515um, 30m), Band 2
(0.525 to 0.605um, 30m, Band 3
(0.63 to .69um, 30m),
Band 4
(0.75 to .90, 30m), Band 5
(1.55 to 1.75um, 30m), Band 6
(10.40 to 12.5um, 60m),
Band 7
(2.09 to 2.35um, 30m), Band Pan
(0.52 to 0.90um, 15m)
More information, and images, available
on this
page
(http://www.geog.ucsb.edu/~jeff/115a/remote_sensing/landsat7/landsat7bandspalmsprings.html)
In principle, the higher the reflectance
contrast between two objects, the easier it should be to distinguish
between them. The Santa Barbara satellite image that will be used
for this exercise was acquired in September of 1999 by the Landsat
Enhanced Thematic Mapper (ETM) Instrument. The multispectral
image characteristics are broken apart into six different wavelength
images, one for each band of wavelengths.
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