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Landscapes Forest and Global Change - ESA - Escola Superior ...

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P.M. Fern<strong>and</strong>es et al. 2010. Testing the fire paradox: is fire incidence in Portugal affected by fuel age<br />

706<br />

dominated by shrubl<strong>and</strong> where fire is a tool routinely used in traditional l<strong>and</strong> management. The<br />

existing spatial <strong>and</strong> temporal information can thus be analyzed to detect relationships between<br />

fuel age <strong>and</strong> fire incidence. Our objective is to analyze contemporary fire history data to<br />

determine how fire recurrence, hence fuel age, relates with burn probability in Portugal.<br />

2. Methodology<br />

The study area is the entire Portuguese mainl<strong>and</strong>, 89 x 10 3 km 2 . The analysis of burn probability<br />

was based on all wildfire events with an area equal to or larger than 10 ha occurring in Portugal<br />

from 1998 to 2008, i.e. during a 11-year period. We used the mapped fire history of the<br />

Portuguese <strong>Forest</strong> Service <strong>and</strong> GIS software to process the spatial information. Fire recurrence<br />

maps were created for each year under analysis, fire recurrence being the number of fires<br />

experienced by each 625-m 2 pixel (25 x 25 m) since 1975. For the area within each individual<br />

fire perimeter we have determined an area-weighed mean fire recurrence <strong>and</strong> the corresponding<br />

fire return interval (FRI). Then we used survival analysis by fitting a two-parameter Weibull<br />

function to the FRI distribution based on maximum likelihood. We have modelled FRI from<br />

individual fire events, rather than from patches defined by their unique fire history, because the<br />

former offers the possibility of assessing if the time-dependency of burn probability changes<br />

with fire size, i.e. with weather conditions.<br />

A fire interval distribution can be described in a cumulative form, F(t), the probability of fire<br />

occurrence before or at time t, <strong>and</strong> as a probability density, f(t), which reflects the frequency of<br />

burning in a given time interval (e.g. Moritz 2003; Moritz et al. 2009):<br />

F(t) = 1-exp[-(t/b) c ] (1)<br />

f(t) = (ct c-1 /b c ) exp[-(t/b) c ] (2)<br />

where t > 0, b > 0 <strong>and</strong> c ≥ 0. Parameters b <strong>and</strong> c have ecological meaning. The scale parameter<br />

(b) has the dimensions of time <strong>and</strong> is the typical fire return interval (FRI) that will be surpassed<br />

36.79% of the time. The shape parameter (c) is dimensionless <strong>and</strong> describes the change in fire<br />

probability through time. The negative exponential distribution is a special case of the Weibull<br />

model that corresponds to c = 1. The probability of burning increases with time when c > 1,<br />

increasing linearly when c = 2 <strong>and</strong> exponentially when c > 2. Vegetation types that are<br />

simultaneously fire-prone <strong>and</strong> fire-dependent are expected to have high c values (Polakow et al.<br />

1999) <strong>and</strong> c > 4 qualifies a fire regime as highly age-dependent (Moritz 2003). The Weibull<br />

median fire-free interval (MEI) gives a probabilistic estimate of fire-return intervals for<br />

asymmetrical fire interval distributions (Grissino-Mayer 1999). The “hazard of<br />

burning“ function λ(t) gives the instantaneous probability of a fire occurring in a specific time<br />

interval <strong>and</strong> is useful to measure how time since the last fire event affects the subsequent<br />

likelihood of burning:<br />

λ(t) = ct c-1 /b c (3)<br />

Data was truncated to consider only those fires whose majority of pixels had burnt at least twice<br />

since 1975, thus reducing the existing asymmetry that otherwise would have biased parameters<br />

b <strong>and</strong> c (Moritz 2003); note that fire incidence in Portugal was quite low before the 1970s. The<br />

Weibull model was fitted separately to two sub-divisions of Portugal − northern <strong>and</strong> centraleastern<br />

(N-CE) <strong>and</strong> central-western <strong>and</strong> southern (CW-S) − mainly on the basis of their relative<br />

fire incidence, high in N-CE <strong>and</strong> relatively low in CW-S (Verde <strong>and</strong> Zêzere 2010).<br />

<strong>Forest</strong> <strong>L<strong>and</strong>scapes</strong> <strong>and</strong> <strong>Global</strong> <strong>Change</strong>-New Frontiers in Management, Conservation <strong>and</strong> Restoration. Proceedings of the IUFRO L<strong>and</strong>scape Ecology<br />

Working Group International Conference, September 21-27, 2010, Bragança, Portugal. J.C. Azevedo, M. Feliciano, J. Castro & M.A. Pinto (eds.)<br />

2010, Instituto Politécnico de Bragança, Bragança, Portugal.

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