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7th Workshop on Forest Fire Management - EARSeL, European ...

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128<br />

II - VALIDATION OF RS PRODUCTS FOR FIRE MANAGEMENT<br />

pre-fire seas<strong>on</strong> may therefore represent an added value for fire management<br />

in Portugal (Gouveia et al., 2009). In fact, the Iberian Peninsula is recurrently<br />

affected by drought episodes and a combined effect of lack of precipitati<strong>on</strong><br />

over a certain period with other climatic anomalies, such as high<br />

temperature, high wind and low relative humidity over a particular area may<br />

result in reduced green vegetati<strong>on</strong> cover. In fact, major fire events in Iberia<br />

are frequently preceded by drought periods, reflected by the decrease of<br />

vegetati<strong>on</strong> activity before the fire episode. This effect is further aggravated<br />

by a quick resp<strong>on</strong>se of dead fuels to changing meteorological c<strong>on</strong>diti<strong>on</strong>s,<br />

such that even short periods of drought may lead to an exp<strong>on</strong>ential<br />

increase in fire risk.<br />

2 - Results<br />

Burned area (BA) data covering the period 1982-2006 were obtained from<br />

the official data supplied by the Nati<strong>on</strong>al <strong>Forest</strong> Authority (AFN). Figure 1<br />

presents the inter-annual variability of burned area over Portugal during the<br />

c<strong>on</strong>sidered period. The close resemblance between the annual and the summer<br />

curves implies that the annual fire regime in Portugal is mostly dominated<br />

by events occurring in July and August. Vegetati<strong>on</strong> stress prior to the<br />

begining of the fire seas<strong>on</strong> was assessed using averaged values in May of<br />

the Normalized Difference Vegetati<strong>on</strong> Index (NDVI) as obtained from the<br />

Global Inventory Modelling and Mapping Studies (GIMMS) database (Zhou<br />

et al., 2001), covering the c<strong>on</strong>sidered 25-year period. Values of NDVI in May<br />

were then spatially averaged over the forested regi<strong>on</strong>s of Portugal as identified<br />

by downgrading the Global Land Cover (GLC) for the year 2000<br />

(Bartholome et al., 2002) to the GIMMS scale. Meteorological fire danger in<br />

summer 1982-2006 was estimated using July + August means of the Daily<br />

Sevirity Rating (DSR), an index that may be derived from the so-called<br />

Canadian <strong>Fire</strong> Weather Index (FWI) system (van Wagner, 1987). DSR is a<br />

numeric rating of the difficulty of c<strong>on</strong>trolling fires and reflects the expected<br />

efforts required for fire suppressi<strong>on</strong> (CFS, 2007).<br />

Regressi<strong>on</strong> tree analysis was used to assess how yearly amounts of BA in<br />

the fire seas<strong>on</strong> could be related with vegetati<strong>on</strong> stress prior to the fire seas<strong>on</strong><br />

and meteorological c<strong>on</strong>diti<strong>on</strong>s during the fire seas<strong>on</strong>. Regressi<strong>on</strong> tree<br />

(Breiman et al., 1984) is a n<strong>on</strong>parametric technique that is very effective<br />

in selecting from given variables the interacti<strong>on</strong>s am<strong>on</strong>g them that are<br />

most important in determining the outcome variable to be explained.<br />

Figure 2 presents a scatter plot of NDVI in May versus DSR in summer 1982-<br />

2006 (left panel) together with the recorded amounts of BA during the<br />

same period(right panel). Figure 3 provides a schematic overview of the<br />

obtained regressi<strong>on</strong> tree. It may be noted that years of weak activity are<br />

associated to both low values of NDVI in May (i.e. low biomass) and DSR in<br />

summer (i.e. meteorological c<strong>on</strong>diti<strong>on</strong>s that do not favour the <strong>on</strong>set and<br />

spreading of fire). The largest event (in 2003) is, <strong>on</strong> the c<strong>on</strong>trary, associ-

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