59
<nown, but
ine process-
this re-
is the land
se polygon,
which might
, such as
Darks --
Dts may be
sa types
h enough
d-use map
sistently
nt accuracy
ownership
eneral
11y con-
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potential
use data
In this,
by census
ation zones,
ed following
f the classi-
puter-aided
functions
within the
ered.
East and
as gained in
nnecticut.
d West affect
ati ve cover,
s, is a pro
weathering
On the positive side, certain surfaces which are a product of their
environment form highly reliable spectral signatures. A good example is
illustrated in figure 2 of Terre Haute, Indiana where the old Central Business
District (C.B.D.), with its weathered (and soot encrusted) roof surfaces form
a cluster quite unlike anything else in the scene, either rural or urban. The
semi-circular adjacent ring of older residential land is also a distinctive
signature thanks to weathered surfaces, a uniform density of houses, and a
similar degree of landscaping, all of about the same age. The fact that hous
ing density is high enough for individual picture elements to have a pre
dominance of man-made surfaces is a further advantage.
The character of the natural environment may also be employed to advantage
in arid areas. In Phoenix, Arizona the scanner/computer combination correctly
identified single picture element size (.46 hectare) parcels of desert land
within generally built-up areas. Somewhat startling was the "discovery" of
numerous non-vegetated vacant lots within what was generally thought to be a
continuously built-up string commercial street development. Subsequent
ground checking proved the identifications correct.
On the negative side, the principal problem faced by the spectral inter
preter is how to distinguish between a man-made land use or land cover and the
natural cover to which it is most closely related in the natural environment
in which it is found. In an eastern city, for example, problems are met in
low density residential areas which are heavily wooded. During full foliage
they are nearly indistinguishable from uninhabited forest, and even in winter
the exposed surfaces of roof tops and driveways is either relatively too small
in area or too similar spectrally to surfaces found in nature; commonly, a
forest floor covered with highly reflective fallen leaves from broadleaf
deciduous trees behaves spectrally like bright man-made surfaces. In Western
desert areas, a flat factory or warehouse roof and its parking lot constructed
from local building materials may have nearly exactly the same spectral re
sponse as those materials in the natural environment.
ACKNOWLEDGEMENTS
The work reported on was undertaken by the United States Geological
Survey under a contract with Purdue University. Publication of this paper
is authorized by the Director, U.S. Geological Survey.
mces in
ze on advan-
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