5. FIRE EFFECTS ASSESSMENT
One of the main problems affecting fire
management is the lack of appropriate statistics
on burned land. Even the countries more
severely affected by this problem do not have
proper data on fire incidence, as most of the
times fires are not mapped and only general
Statistics are available. On the other hand, data
are not available until several weeks (or even
months) after the fire event. As a result,
vegetation recovery is not assessed, and a lack
of regrowth may constitute a severe soil
erosion hazard (Isaacson et al., 1982).
Moreover, these field inventories are often
very general. Usually, only the scorched
perimeter is drawn, but no information about
the species affected or severity of damage is
provided. Furthermore, studies on vegetation
succession after fire are seldom done.
The growing interest in global effects of fire
processes demands a quantitative evaluation of
the spatial and temporal distribution of fire
patterns (Levine, 1991): a wide range of
disciplines, such as fire ecology, fire
management, atmospheric chemistry and
forestry, will benefit from burned land maps at
global and local scale.
Most of the fire mapping projects have been
based on channel 3 data. However, as it was
stated before, this channel presents several
difficulties for fire detection and, therefore, for
burned land mapping. Another approach for
burned land evaluation is based in measuring
the consequences of the fire, rather than
detecting the fire itself, by multitemporal
comparison of vegetation indices acquired from
before and after the fire.
Several studies have shown that spectral
characteristics of burned land contrast sharply
with the response of healthy vegetation. Burned
land shows a severe decrease in near infrared
reflectance, as a consequence of leaf
deterioration, and an increase in red reflectance
because of the lack of pigments' absorption
48
(Tanaka et al., 1983). Therefore, the NDVI
values of burned vegetation are much lower
than those of healthy plants, and multitemporal
analysis should clearly portray fire alteration.
Some studies have proven this hypothesis,
obtaining adequate results from both high and
low resolution sensors (Kasischke et al., 1993;
Martin et al., 1994; Pereira et al., 1994).
7. FUTURE PROSPECTS
Future availability of better spatial, spectral and
temporal resolution sensors will overcome
some of the present limitations of satellite data
for fire management. MODIS data will
increase spatial and spectral detail currently
provided by the AVHRR sensor for both short-
term fire danger estimation and fire mapping.
This sensor, along with the Meteosat Second
Generation, will also very valuable for
operational fire detection, even in European
countries. The growing tendency toward the
combined analysis of GIS and Remote Sensing
data will benefit fire risk and fire effects
assessment as well.
8. REFERENCES
Belward, A.S, 1991. Remote sensing for
vegetation monitoring on regional and global
scales. In: Remote Sensing and Geographical
Information Systems for Resource Management
in Developing countries, (A.S.Belward, and
C.R.Valenzuela, editors), Kluwer Academic
Publishers, Dordrecht, pp. 169-187.
Burgan, R.E. and Rothermel, R.C., 1984.
BEHAVE: Fire Behaviour Prediction and Fuel
Modeling System. Fuel Subsystem, USDA
Forest Service, Ogden, Utah.
Burgan, R.E. and Shasby, M.B., 1984.
Mapping broad-area fire potential from digital
fuel, terrain and weather data. Journal of
Forestry, Vol. 82, pp. 228-231.
Chou, Y.H. 1992. Management of wildfires
with a Geographical Information System.
International Journal of Geographic
Information Systems, Vol. 6, pp. 123-40.
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B6. Vienna 1996
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