.cut River. Photo-
686-692.
& J.C. van Huis
.1 dune manage-
ITC Journal
C. Davis 1969.
'hotograiranetric
Symposium on Remote Sensing for Resources Development and Environmental Management / Enschede / August 1986
Spectral characterization of urban land covers
from Thematic Mapper data
iy of recreational
:higan Academy of
XVII, 1962,
lman 1973.
:ries. Tijdschrift
rrafie, 64, no 1:
and) 1977.
Friese meren.
onderzoek.
h to flourishing
rphotostudy of
nor peninsula,
pretation, work-
rzeewerken 1977.
ek naar patronen
evaart op het
aan de hand van
>ta nr 291, Lely-
rzeewerken 1979.
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op de randmeren
ion geography of
iew, vol LXII, no
urist market re-
erkehr, no 3: 89-
ion and Resources
9, part 3s 467-
s in the uplands.
York Moors.
ng Institute,
onderzoek Hel-
cten. Afdeling
hogeschool,
en vanuit vaste
vincien Gebied.
universiteit
f recreational
ial photographs.
ties and their
of the islands,
erference. In:
Flora and vege-
and coastal
erdam.
nvironmental Con-
c lecture given
e 20th, 1985 at
Douglas J.Wheeler
Utah State University, Logan, USA
ABSTRACT: Using Salt Lake City, Utah, as a test case, this study evaluates the capabilities of Landsat~~b
Thematic Mapper (TM) digital data for distinguishing urban land cover materials. This was accempfShed by
using a newly developed hierarchical clustering algorithm which statistically derived spectral classes from TM
channels 2, 3, 4, and 5 (visible, near infrared and middle infrared). The relationships between spectral
groups were further analyzed using three statistical evaluations: principal components analysis, cluster
analysis, and discriminant analysis. Through the use of component scores, cluster linkage diagrams, and
canonical discriminant function scatter plots; as well as TM spectral curves, aerial photography, and ground
investigation; the spectral classes were grouped into twelve predetermined land cover categories. The accuracy
of classification was assessed at approximately 80 percent (0.05 significance level). A significant
improvement in classification accuracy (91.5 percent) was achieved by stratifying the multispectral
classification with thresholds from the TM thermal channel introduced as ancillary data.
INTRODUCTION—DERIVING SPECTRAL CLASSES FROM TM
With a high proportion of the world's population
living in cities it is increasingly important to
understand the very complex ecological interactions
that are taking place within the urban environment.
One key to better understanding these relationships
is to characterize the land cover materials that
influence radiational and micro-climatological
balances. By monitoring successional changes in land
cover materials one may observe its effect on urban
ecosystem processes.
The value of Landsat's multispectral scanner (MSS)
in detecting land cover has been established (Todd
1978). Landsat 5's advanced multispectral scanner
called Thematic Mapper (TM) , with improved spatial
and spectral resolution over MSS, could be an even
better tool for detecting land cover characteristics
in complex urban environments. Although very little
is published at the present time on the use to TM
data in urban analysis, preliminary studies using
Thematic Mapper Simulator (IMS) data flown from
aircraft indicated that the 30 meter pixel size of TM
might be ideal for mapping urban land cover elements
(Clark 1980, Welch 1982). Two studies using TM data
for Mobile, Alabama, show promising results
(Quattrochi 1983, Wang 1985).
The urban region of Salt Lake County, Utah, was
chosen as the study area for this evaluation of TM
digital data due to the diversity of land activity
found within a relatively small area. The majority
of Salt Lake County's 1984 population of 650,000 is
found within a 15 kilometer wide strip stretching
north-south along the base of the Wasatch Mountains.
Salt Lake City contains the diversity of land
activities usually associated with metropolitan areas
of a much larger size. There are many heavy and
light industrial and commercial activities; diverse
multifamily, single-family, and rural residential
areas; extensive irrigated and nonirrigated
agricultural lands; as well as natural vegetation and
water features distributed throughout the county.
The central valley portion of the county consists of
several urban areas that are coalescing due to
ongoing urban development and suburbanization. Even
within the city limits of the communities in the Salt
Lake valley there are many agricultural and natural
areas that are being filled in with urban land use
activities.
A strip 15 kilometers wide and 25 kilometers long
was selected for the study area, extending through
the urban corridor of the valley. From within this
urban study area, 10 test windows were selected to be
used for generating spectral signatures from the raw
TM data. The principal data source for analysis wa c
the digital tape of a Thematic Mapper scene dated
July 27, 1984. Using test windows to break up the
study area into manageable size units made the field
investigation and computer processing more cost
effective. The 10 windows were carefully chosen from
aerial photography to represent the broadest spectrun
of cover materials found within the Salt Lake urban
environment. The 10 test windows accounted for
approximately 16 percent of the study area.
After the test windows were selected, several trips
to the field were made to identify land cover
materials. At that time, ocular estimates were made
of the percentages of surficial materials found in
association with one another, and which combinations
comprised various cover types. It was decided that
12 particular land cover classes would be desirable
to detect from the TM data of Salt Lake City. The 12
preliminary land cover classes decided upon for this
study included: (1) open water, (2) light inert
materials (e.g., bare soil, concrete, and reflective
metals and glass), (3) coal and slag, (4) dark inert
materials (e.g., railroads and blacktop surfaces),
(5) light asphalt-gravel surfaces, (6) mixed pixels
with mostly inert cover and little vegetation cover,
(7) mixed pixels with high vegetation cover, (8)
senesced weeds and natural grass, (9) healthy moist
vegetation, (10) drier or sparse vegetation with soil
showing, (11) short cropped grasses (lawns), and (12)
trees and shrubs.
A large portion of the computer processing of TM
data was accomplished using ELAS digital image
processing software obtained from NASA's Earth
Resources Laboratory. The TM data tape was
reformatted into an ELAS data file format to be
processed on a Prime 400 computer. Of the seven
original TM channels it was decided to generate
statistic files from data in spectral bands 2, 3, 4,
and 5, giving representation from the visible, near
infrared, and middle infrared wavelengths. The
thermal channel (band 6) was not used in determining
spectral classes because of its lower spatial
resolution (120 meters compared to 30 meters) and the
lack of differentiation in spectral values. While
there appear to be many opinions on which TM bands
are optimum for processing, there is considerable
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