Full text: Proceedings of the Symposium on Global and Environmental Monitoring (Pt. 1)

787 
The method being prototyped involves the production 
of three themes: ground cover, present land use and 
topographic features. The area chosen for this initial 
work is in the southern interior of the Province, 
specifically NTS map sheets 82 E (1:250 000) and 82 
L/3 (a 1:50 000 map sheet, but mapped at 1:20 000). 
The ground cover database provides the generalized 
type, extent and distribution of present vegetation 
cover. The main criteria for classification is vegetation 
structure and composition (i.e. physiognomy). The 
initial classification from the satellite imagery is refined 
using the relationship between specific vegetation 
distribution and topography. The ground cover theme 
is extended to include some detail on water bodies, 
wetlands, rock outcrops and the like. A ground cover 
classification schema is given in appendix "A". 
The present land use theme is based on a modified 
form of the "Land Use Classification in British 
Columbia" (Sawicki et al., 1986). The level of 
classification is restricted to area-based uses versus site 
uses. Site uses of the land are generally not extensive 
enough to be identified on satellite imagery. It should 
be noted that a combination of spectral classification 
of satellite imagery and interpretation is used to 
produce the present land use classification. 
The topographic features database is derived by 
segmenting the digital elevation model (DEM) into 
significant landscape units. These units are described 
in both raster and vector format. Watershed 
boundaries are delineated. Attributes that are attached 
to these units are the maximum, minimum, and mean 
values for: elevation, slope and aspect. Also included 
are: area, surface irregularity, and surface shape. 
Potential solar radiation received is also calculated. It 
is anticipated that these attributes will significantly add 
value to the final Baseline Thematic Map product for 
many users. 
The satellite imagery utilized is presently Landsat TM, 
which has good spectral information for the 
identification of ground cover and for interpreting 
present land use. Two versions of the product are 
being prototyped, corresponding to the two available 
topographic data sets. The digital elevation model and 
base map for the 1:250 000 version will be supplied 
from scanned 1:250 000 NTS map sheets. Energy 
Mines and Resources Canada has scanned all of the 
84 sheets covering B.C. and these digital map files are 
available from them. The Terrain Resources 
Information Management (TRIM) program (the 
creation of 1:20 000 digital base mapping for B.C.) will 
supply the digital elevation model and the base map 
for the 1:20 000 version. Presently there are about 
1200 of the 7000 map sheets completed with a current 
production rate of approximately 500 map sheets per 
year. 
3 METHODOLOGY 
For the 1:20 000 version the new digital mapping from 
the TRIM program forms the base map. For the 
1:250 000 version product, scanned 1:250 000 NTS map 
sheets will provide the base map. The datum for the 
prototype work is NAD 83 (North American Datum 
1983). It is envisioned that all provincial mapping will 
migrate to NAD 83 over the next five years. 
Transformations to other datums (NAD 27) and 
projections are well defined for those users desiring 
them. 
The first manipulation of the input data is to co 
register the different data sets (imagery, DEM’s, and 
other ancillary map data). To avoid any systematic 
subpixel mis-registration all rasters follow the same 
convention about the origin with respect to the 
reference UTM grid. UTM coordinates ending in 00 
(i.e. every 100 metres) align with the boundary 
between pixels. Pixel sizes are chosen in a nested 
hierarchy as follows: 6.25, 12.5, 25, 50, and 100 metres. 
The actual size is dependant upon the data utilized 
and the map scale produced. 
For areas of high relief Landsat TM imagery has 
geometric distortions due to the panoramic view of the 
sensor. At the edge of the 185 kilometre wide image 
swath the look angle is 7.47 degrees, causing a 
horizontal displacement of 30 m for every 230 m 
change in ground elevation (Wong et al. 1981). Many 
parts of B.C. have relief in the order of thousands of 
metres. This is an unacceptable amount of distortion 
for 1:20 000 mapping. 
Correcting for relief displacement is accomplished 
using a DEM. We have demonstrated that the 
1:20 000 TRIM data produces a DEM that is 
sufficiently precise to allow correction of Landsat TM 
to plus or minus one pixel (25m) accuracy. Currently 
we are investigating the precision obtainable utilizing 
1:250 000 topographic data. 
The present land use classification was produced 
through interpretation of a transparency of the Landsat 
TM imagery using the PROCOM projection device. 
The transparency was the same date as the digital data 
with bands 3, 4 and 5 portrayed as blue, green and 
red. The interpretation depends upon colour, tone and 
pattern recognition and adjacency considerations. The 
initial interpretation work was done at 1:100 000 scale 
with the results then being digitized into the existing 
digital base maps. 
Image classification for ground cover identification 
proceeds from field work to selection and refinement 
of training sites on the satellite imagery. To reduce the 
complexity of the task the classifications where 
stratified according to the land use classification. Thus 
many separate classifications (eg. agricultural, 
rangeland, logging clear cuts, etc.) with a restricted 
number of classes where performed. Within these 
strata single ground cover classes are described by 
more than one set of training sites so illumination and 
ecological differences due to topographic position are 
accounted for. After classification with these separate 
training sites, the results are merged into a single class 
type. 
Post-classification processing is of two main types: 
context filtering to transform the raw image 
classification into a more acceptable map like product 
and modification of the resulting classification through 
the use of ancillary (primarily topographic) data. 
Context filtering makes use of the similarity between 
classes as well as length of common boundary and
	        
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