International Archives of Photogrammetry and Remote Sensing. Vol. XXXII Part 7C2, UNISPACE III, Vienna, 1999
19
I5PR5
UNISPACE III - ISPRS Workshop on
“Resource Mapping from Space”
9:00 am -12:00 pm, 22 July 1999, VIC Room B
Vienna, Austria
ISPRS
Figure 7: Mapping from Satellite Imagery' from Spot MS (France), Spot Pan (France), KFA 1000 (Russia), aerial photography
1:20 000, existing map 1:25 00
The suitability for mapping from a particular type of imagery
has already been investigated in the early 1980’s. There are
three criteria to be met:
■ planimetric accuracy, which is scale dependent
■ elevation accuracy, which depends on parallaxes created
by the different image geometry from two different
imaging positions
■ detectability, which relates to the spatial resolution, which
may be achieved by a particular sensor system.
Even though aerial photography, which has been digitized into
different pixel sizes on the ground can hardly distinguish more
than 6 bits of grey values as opposed to recent digital sensors
with 10 or more bit of grey level distinction these early results
are still generally valid:
Planimetric accuracy of a map is generally related to ±0.2 mm
at publishing scale according to U.S. mapping standards. This
criterion mainly relates to worldwide mapping practices for the
original mapping scale, but not for generalized maps at smaller,
derived scales, in which the planimetry is often shifted to
accommodate conflicts in the depiction of objects. Even in the
original mapping scales buildings or building blocks, roads and
rivers are shifted in some national map bases for this purpose.
But in general this means from the data acquisition side, that the
following planimetric standards are usually accepted:
wmm
1: 10 000
± 2 m
1: 25 000
± 5m
1: 50 000
± 10 m
1:100 000
± 20 m
1:200 000
± 40 m
Elevation accuracy is generally a function of terrain slope.
Depending on terrain slope a certain contour interval is
specified. The reliability of contouring is generally accepted as
being 5 times the point measuring accuracy in height, regardless
of whether the contours are originally measured in a
photogrammetric plotting instrument, or whether they are
interpolated on the basis of a measured digital elevation model
(D.E.M.) grid.
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1 m
± 0.2 m
flood plane
2m
± 0.4 m
“
5 m
± 1 m
“
10 m
± 2 m
20 m
± 4 m
“
50 m
±10 m
100 m
±20 m
high mountains
The detectability of objects, given sufficient contrast as a
function of grey level discrimination, was formerly measured in
terms of photographic resolution stated as line pairs per mm
(lp/mm). Nowadays this photographic resolution must be
compared to 2 to 5 pixels at image scale related to IFOV on the
ground.
Early tests with photographic resolutions have been carried out
for specific objects to be recognized and identified from the
imagery. They established a minimum pixel size for the
detectability of the following objects: