it is not possible to arrive at more detailed conclusions
regarding change in the Delta.
IMPLICATIONS FOR THE STUDY AREA
It is not possible to distinguish between all of the groups
delineated at a satisfactory level. Confusion between
classes may have occurred because of:
o misclassification of pixels
o large variation within some groups - This may be
caused by inclusion of two sub-groups within one
group (for example, grouping wet mudflats with
dry mudflats, or clear water with muddy water).
o too many classes were delineated - When the three
vegetated groups were put together, classification
accuracy improved significantly.
o complexity of the study was too great - This
method may be more suited to areas with fewer
classes to be distinguished, and with larger,
more homogeneous units.
o geomorphological analysis is, in many ways, a
discerning of pattern - To this extent, digital
analysis would be less productive than visual
analysis. Many of the important clues to unit
classification are in the relationship between
pixels .
Therefore, use of this method to monitor change in the
Athabasca Delta is not recommended unless major improvements
can be made to overcome some of the these problems.
IMPLICATIONS FOR DIGITAL ANALYSIS
The lack of success in classifying the study area does not
imply that the method could not be useful in other areas.
Boyd (1981) has successfully applied this method in other
parts of Alberta, particularly the parklands. Recommenda
tions for future projects using this method are:
o projects selected should ideally be concerned with
units which are large and homogeneous
o the units chosen, whether biophysical or geomorpho
logical should be related to one cover class; if
this is not possible, more than one subunit should
be delineated and these subunits amalgamated in the
production of maps - For example, clear water and
turbid water may have to be classified separately,
even if they are eventually to have the same classi-
fication.
o the number of classes should be as few as possible,
notwithstanding the above point
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