Full text: XVIIIth Congress (Part B7)

  
Level 
0 land-cover 
eer quA omes, MD 
1 non-vegetated vegetated 
2 water road blond sand wood herbaceous 
3 deciduous hs1 thin grass/herb cover with blond sand 
coniferous 
sea buckthorn 
privet/creeping willow 
hs2 intermediate herb/moss cover with grey sand 
hs3 high moss cover 
hs4 high moss and low grass cover 
hs5 high grass/herb cover with litter 
Fig 3. Example land cover hierarchy. 
3.3 Aggregation of fuzzy data 
The image interpretation in the previous section yields 
a 7-fold vector of membership values (MV... ,, MV,.,, 
MV, MV, .,, MV, MV,.,, MV, ,,,) for each image pixel. 
Although it is possible to detect temporal changes in 
membership values on the pixel level, it is usually better 
to aggregate the membership values to larger cell sizes 
in order to minimize the effects of classification errors 
on the temporal analysis. 
The aggregation of fuzzy data is dealt with by 
Klir and Folger (1988). First step is the calculation of a 
pseudo-frequency N(c) for each state of the aggregate c 
€ (sand, hs1, ..hs5, wood]. Since values of N(c) need not 
be whole numbers, it is better not to use the therm 
frequency. In order to accomplish that each cell 
contributes equally to the pseudo-frequencies the 
membership values of a single cell have to sum to one. 
If not so, the membership values have to be normalized 
in this sense. The pseudo-frequency for each state or 
class is calculated as the sum taken over ail cells within 
the segment defining the spatial extent of the 
aggregate. 
The pseudo-frequencies are now used to 
estimate the value of a fuzzy measure, i.e. possibility or 
probability, indicating the strength of the relationship 
between the aggregate and a class. The (pseudo- 
probability distribution is calculated by dividing a 
pseudo-frequency by the sum of all pseudo-fre- 
quencies: 
p(c) = N(c)/ Y, N(z) 
z c HS 
The aggregation did not change the vector of attribute 
names, unlike their measure for quantification, which 
changed from membership values to pseudo- 
probability values (p. Phe Phe Pus Psst Phssr Pood): 
Note that the link between the concept of fuzzy sets 
and fuzzy measures is effectuated by the pseudo- 
frequency distribution. See table 2 for an example. 
Tab. 2. Illustration of probability (p) distribution 
estimates derived from a pseudo-frequency distribution 
N calculated over 5 cells. 
  
cicell..4- 2.3.44: 5 N(c) p(c) 
sand 0:0: 0:10 15:0:5,1 1.0 0.20 
herb1 02 03.05 .0,.:0 1.0... 0.20 
herb2 - 0.8..0:2.-0:15-01: 50 3.6,,0.32 
herb3 > +0:<::0:: 04:0 11.0 0.4 0.08 
herb4 :: 0.0. -.0,+0-+<0 0.0 0.00 
herb5 4:045 :0::50./0 0/540 0.0 0.00 
wood Qs po: Oiosdos 1.0... 0.20 
  
4 QUANTIFICATION OF ECOLOGICAL PROCESSES 
By the proposed aggregation procedure the objects 
and fields are converted in a field. In this field the 
presence of each vegetation type is expressed by a 
probability, resuiting in a vector of 7 probability values 
(Psand Phstr Pur Phsar Pusar Press! Prod)” Obviously, this 
vector specifies a point in a 7-dimensional vegetation 
space, where each vegetation type defines an axis of 
this space. 
Changes in the vegetation composition. on a 
specific site (x,y) from date t to t+At result in a move 
through this space from point (P_, , Du, Du Phy Pres 
Phes/ Progehsy to point (m Pu Puy Pus; Pu Pus 
woody Tespectively. Each cell shows a specific 
change in the vegetation space and from all these 
movements general processes of vegetation change 
can be calculated. Because a single vegetation 
composition on different sites might develop into 
different directions, each vegetation composition on 
time t relates to many possible vegetation compositions 
on time t+At. This set of possible future compositions 
forms a cluster in the vegetation space. The cluster of 
possible vegetation compositions can be conveniently 
described by its point of gravity and standard deviation. 
218 
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996 
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