Full text: XVIIIth Congress (Part B7)

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pubescens. density between 35% and 70%), 6.4 broad-leaved 
high density forests (density greater than 70%), 6.5 coniferous 
veforestation . 6.6 broad-leaved reforestation.. 
The definition of the endmembers and vegetation continuum 
legend has been obtained starting from the nomenclature 
described above: this nomenclature has been further refined and 
integrated by iterative spectral analysis of the multitemporal 
dataset. evaluation of the classification results and assessment 
ofthe errors occurred in the mixing model analysis. 
1.2 Image data 
Two Landsat 5 - Thematic Mapper data quarter scenes (track 
193. frame 92) were acquired to obtain spectral and 
multitemporal discrimination of the vegetation canopies: in 
order to get discrimination capability in evergreen and 
deciduous quercus species. as well as for pasture classes and 
shrubs, a mid spring date and a deep summer date were chosen: 
31st March and 22nd August 1994. 
About half of the quarter scene (80Km X 40Km) was processed 
to obtain the land use and vegetation map. About 20% of this 
area resulted recently burnt in the August image. reporting 
highest fire events occurred at the beginning of that month. 
2. METHODS 
2.1 Geometric and radiometric preprocessing 
A first geometric rectification process was made in order to 
correlate the two Landsat scenes each other; due to the almost 
identical flight direction of the satellite overpasses the 
registration was performed with a simple 1st order polynomial 
transformation with a rotational coefficient very close to 0. 
The projection on the UTM 32 coordinate system was made 
after the classification process in order to limit the resampling 
effects on radiometry and on the multitemporal registration. 
During this last geometric rectification process no digital 
elevation model correction was applied due to the smooth 
landscape and low elevation range occurring in the study area; 
the estimated maximum planimetric error introduced by this 
approximation for such an elevation range is less than 20 mt, 
which is comparable to the planimetric location error obtained 
in the control points and test points used for the UTM 
projection transformation. This error is compatible with 
1:100000 scale products geometric specifications. 
Despite the low elevation range. the typical Mediterranean 
landscape is often characterized by steep slopes and 
discontinuities that create small but serious topographic effects 
that cannot be recovered easily without an accurate DEM 
(generally unavailable or extremely expensive) and a 
comparable spatial resolution in the imagery. To recover these 
effects spectral normalization has been applied to the two 
Landsat scenes by means of chromatic components computed 
Starting from each TM channel reflectance. 
The chromatic transformation, while giving generally good 
results in topographic effects normalization, maintains the 
linear relation originally existing among the total pixel 
reflectance and the sum of area-weighted reflectances for each 
endmember class. thus conserving the necessary hypothesis to 
allow the application of linear unmixing methods. 
575 
2.2 Training sets, endmembers and channel selection 
Within the study area, a square of 500 x 500 pixels was 
selected. This area is representative of the most important 
cover classes we put in the described legend. With the help of 
aerial phothograps, showing the same zone, a reasonable set of 
polygons were selected for each classes on a RGB 432 
composite of the Thematic Mapper august scene. In this way, a 
overall number of 73 polygons was defined. The standard 
statistical parameters, referred to each training-set, were then 
extracted from all original and all chromatic bands. Using 
different kinds of digital tools. e.g. scatterograms and plots, it 
was analyzed the spectral behavior of each cover classes within 
the available spectral space. This spectral analysis allowed to 
estimate the discrimination between the cover classes 
considered in the legend and it was very useful for the choice of 
the better set of bands to use in statistical classification. It was 
observed a good spectral separation between the land use-land 
cover classes hereinafter indicated. 
The definition of endmembers, which represents a crucial point 
in the unmixing method, has been driven starting from the 
analysis of typical vegetation components, the ground truth plot 
location on the imagery and the subsequent spectral distribution 
analysis using tools available with EarthView. While running 
this activity various interesting aspects arose among which the 
presence of further endmembers and the usefulness of 
visualization of spectral spaces in endmembers choice. 
In our experiment, after this analysis, five classes were 
indicated as endmembers: three species of woods (quercus ilex. 
quercus pubescens, quercus suber), a typical shrub association 
of secondary species (Cistus spp, Pinaccia Lentiscus) and an 
open pasture class were chosen as endmembers, since they 
represented the main vegetation species in this study area: 
other typical vegetation species, even present in the Sardinia 
district. (e.g. coastline maquis), were excluded for their 
extremely scarce presence in the study area. 
2.2 Land Use classification 
The general land -use classification has been driven by the 
following steps: a first raw classification allowed to separate 
water bodies, bare rock outcrops and permanently bare soils by 
multitemporal NDVI thresholding. Secondly, manual 
identification of urban areas, recently burnt areas and 
horticultural areas characterized by small-parcels was done. 
Finally the Mahalanobis classifier was applied to classify the 
remaining areas in the following other classes: quercus woods, 
shrubs, pasture, 3 crop types and coniferous reforestation. 
2.3 Linear unmixing classification 
The classification of natural vegetation continuum has been 
obtained using Linear Mixing Models. Linear Mixing Models 
allow to classify multispectral satellite images at subpixel level. 
For each pixel proportions between a number of different 
materials are determined recalling that the spectral radiance 
recorded by a satellite results from a mixture of the energy 
reflected by all surface types within the instantaneous field of 
view of the satellite sensor. The main problem with these 
methods is a correct identification and characterization of a 
reasonably small and representative number of surfaces whose 
mixture can reproduce the spectral distribution observed. It's 
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996 
 
	        
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