Full text: Proceedings, XXth congress (Part 7)

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International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004 
‘Burned” in the aggregate image 1996 (AI 1996), 
*Background" in the AI 1997, 'Burned" in AI 1998, and 
"Background" in Als 1999 and 2000. There are 32 possible 
combinations of "Bs'or 'Gs" in a five-digit representation, 
indicating the status of any specific pixel in the aggregate 
images. From these 32 sequences, only 26 are of interest, since 
the sequence GGGGOG is discarded (no fires), as well as the five 
sequences which do not characterize recurrence (presence of a 
single 'B"in the sequence, such as BGGGO). The 26 remaining 
sequences were cross-referenced with the vegetation maps, so 
that the recurrence area could be estimated for each type of 
vegetation physiognomy. 
3.24. Permanence of the Fire Scars: The permanence of the 
fire. scars. was defined, «a priori, in periods of 16 days, 
corresponding to the revisit time of the TM/Landsat satellite. 
This definition implied in the elimination of year 1999 from the 
analysis, since in this year both TM or ETM images were 
included, and the time difference between acquisitions by 
Landsat 5 and 7 was only eight days. Theoretically, in order to 
cover the entire dry season (burning season), images acquired in 
times t+16, t+32, t+48, t+64, t+80, t+96, t+112, t+128, t+144 
and t+160 (in days) should be available. However, during the 
period considered, only partial sequences were obtained, as 
indicated in Table 1. 
  
Chapada dos Veadeiros site 
  
  
  
  
  
  
  
  
  
  
  
Year Sequences of revisit (days) 
i6 | 33. [48 | &4 | $0 | 96 [112 [128 [144 [ 160 
1996 | X X X X 
1997 | X X X X X X 
1998 X X X X X 
2000 | X ¥ IX [7 X 
Araguaia site 
1996 | X X X X X 
1997 X X X X 
1998 | X | X T= X 
OIX Ix Ix Ix [x X 
  
  
  
  
  
  
  
  
  
  
  
  
  
  
  
Table 1. Availability of Landsat 5 imagery during the dry 
season. 
The permanence of the fire scars was estimated on a pixel by 
pixel basis, by analyzing the spectral-textural variability of the 
fire scars along the dry season of each year. This was carried 
out by associating to each pixel in every image of a given year, 
the label *Burned" (B) or " Background" (G), if the interpreter 
could still identify the fire scar in the image, or not, 
respectively. In a year where five images were available, the 
sequence BBGGOG associated to a given pixel would indicate 
that the fire scar was spectrally visible for a period of two 
consecutive dates, and spectrally not discernible in the last three 
acquisition dates. Areas covered by clouds and shadows were 
disregarded from the analysis, as well as those associated to ‘B” 
in the first date of the sequence. 
This was due to the impossibility to determine the number of 
days between the occurrence of the fire and the satellite 
passage, thus creating uncertainties in the estimation. Hence, 
the observation of the fire scars started from the second image 
available (reference date). 
245 
4. RESULTS AND DISCUSSION 
4.1. Area Burnt 
The estimates of the burnt area indicated, for both Chapada dos 
Veadeiros (CV) and Araguaia (A) sites, a systematic decrease 
from 1996 to 2000, from approximately 4.186 km’ and 4,752 
km” in 1996 to 1,327 km? and 2,138 km? in 2000, respectively. 
The only exception to this pattern was the year 1998, with 
increases of 214% and 246% in relation to 1997, for CV and A 
sites, respectively. This increase may be due to the fact that 
1998 was possibly the warmest year of the decade (IPCC, 
2001), resulting in diminished soil moisture and water content 
in the vegetation. In the CV site, the physiognomies most 
affected by biomass burning were the campo cerrado and 
parque de cerrado (which correspond to approximately 8196 of 
this study area, being responsible for approximately 98% of the 
total area burned). These physiognomies were also the most 
affected ones in A site, covering approximately 61% of the arca 
of this site and concentrating approximately 95% of the total 
area burned. 
4.2. Recurrence of Burns 
Approximately 1696 and 1896 (4,703 km? and 5,373 km?) of the 
total area of the cerrado, in the CV and A sites, were affected by 
the recurrence of fires from 1996 to 2000, respectively. The 
sequences characterized by a single recurrence, independently 
of the year of the fire, were the most common (77% in CV site 
and 6296 in A site) and in both areas, the single recurrence, 
spaced by one year (ie., sequences of the type BGBGG, 
GBGBG or GGBGB), represented approximately 68% in CV 
site and 59% in A site. The second most frequent type of 
sequence was that characterized by two recurrences (19% in CV 
site and 31% in A site). It is interesting to note that in CV site, 
approximately 896 of this type of recurrence was sequential (i.e., 
BBBGG, GBBBG, or GGBBB), whereas in A site, the most 
frequent sequence (approximately 12%) was characterized by 
intercalated burns (i.e., BGBGB). The sequence characterized 
by four recurrences (BBBBB) was very minor (0.35% in CV 
site and 0.79% in A site). 
4.3. Mean Permanence of the Fire Scars 
The analysis of the data indicated that the mean permanence of 
the burnt scars is subject to significant annual variations. For the 
Chapada dos Veadeiros, the mean permanence for the period 
1996-1997-1998-2000 were 79, 55, 102 and 47 days. 
respectively, whereas the corresponding data for Araguaia were 
64, 96, 82 and 57 days. Regardless of the differences (in 
absolute terms) of the mean permanence for each year in the 
period analyzed, the physiognomy campo was the one that 
consistently presented the longest mean permanence of the fire 
scars, followed by the parque de cerrado and campo cerrado. 
5. CONCLUSIONS 
Although this study was carried out in two specific areas of the 
Brazilian cerrado, it introduces a methodology that can be 
applied to larger areas, being also adequate for use with data 
from other types of sensors, such as the MODIS. In this case, 
small burnt areas may not be detected due to the coarser spatial 
resolution of the MODIS (250 metres) relative to the TM (30 
metres). The range of mean permanence from one year to 
another in a same area indicates the difficulties to consistently 
characterize the permanence of the fire scars. 
 
	        
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