Figure 1. location of the five SIR-A data strips:
(1) St. Joseph, Mo., (2) Mobile, Al., (3) Tallulah,
ia., (4) Louisville, Ky. and (5) Stirling, Co. 1
Figure 2. An extract shewing settlements of the
Baoding area in North China as recorded on
the SIR-A image.
4 RESULTS
4.1 Detectability of human settlements
It ~ is interesting to note that the detectability
of human settlements from the SIR-A data varied
considerably from region to region. A striking
difference was observed if human settlements in
the North China Plain were compared with those
recorded on the five different United States
strips. The human settlements in the North China
Plain exhibited such strong backscatter that a
complete range of them could be detected (Fig.
2). Even the very small villages could be mapped
without much trouble. A comparison with the
1:250,000 scale topographical map for this part of
China suggested near 100 percent success rate of
detectability. It Is also noteworthy that these
Chinese settlements are highly compacted and
mostly walled in the past. The plain is so very
flat that it is almost at sea level -- the danger
of flooding was revealed by the levees built along
the rivers which were readily visible from the
images (Fig. 2).
Figure 3. An extract from St. Joseph, Mo. strip.
Note the variations in building density detectable
in some settlements.
Figure 4. An extract frean the Mobile, Al. strip.
Note the city of Mobile is difficult to delineate.
Notice aiso the bright return from the industrial
area and the weak return frean the air fields.
In contrast, the United States environment
appeared to show a greater diversity and
variability in the detection of human settlements
from the SIR-A data (Figs 3-7 and Table 1).
Tne settlements normally distinguished
themselves by the very strong backscatter which
may have been caused by the corner reflector
effect of some structures. It has long been
recognized that the orientation of the radar
antenna in relation to the cultural features being
imaged can affect the strength of the microwave
backscatter, hence variations In the grey tone of
the objects in the images (Bryan, 1979; Hardaway
et al., 1982). It was noted that when linear
features were oriented perpendicular to the radar
beam very strong backscatter called cardinal
effect occurred. Henderson and Amita (1930) also
observed that settlement detectability was
significantly influenced by radar azimuth angle on