Portugal Portugal Portugal Portugal

Forest fires Portugal

Vulnerabilities - Changes in the past - Mediterranean

In the last decades, there has been a noticeable increase in the number of wildfires in the Mediterranean countries (1). The total area burnt also increased in Spain (2), and in the other Mediterranean countries of the European Union (3,17). However, the increase in the total area burnt is not as sustained as the increase in the fire frequency, but there are periods of low annual area burnt punctuated with years of extraordinary fire activity, like 2003 in Portugal or 1994 in eastern Spain (4).

An increase in the area burnt is not necessarily related to an increase in the ignition frequency. Results from research have been reported that show that the number of ignitions had very little effect on the total area burnt. The results indicate that the total area burnt will be more or less the same despite any effort to reduce it by reducing the number of ignitions, extinguishing fires or by using prescribed burning. This annual area burnt appears to be determined by the characteristics of the vegetation (maximum biomass and rate of the accumulation of biomass) and by the meteorological characteristics (average and standard deviation of the meteorological conditions). Furthermore, reducing the number of ignitions had the perverse effect of increasing the proportion of area burnt in large fires: there were less fires, but these were larger (4).

The main determinant of the fire regime is probably the accumulation of fuel in the vegetation. Processes that allow the natural accumulation of fuel, like reducing the number of ignitions or increasing the fire fighting capacity, permit the creation of continuous areas with a high fuel load, which will burn under adverse meteorological conditions and produce large fires. On the contrary, processes that eliminate patches of fuel, like a high number of ignitions, non-fire suppression, or prescribed burning, create a patchy mosaic in the vegetation that can behave as fuel-breaks under some circumstances, and reduce the extension of some fires that, otherwise, would become large fires (4).

Vulnerabilities - Changes in the past - Portugal

A new era of forest fires since the 1980s 

Before the 1980s fires in mainland Portugal had never reached 10,000 ha of burned area in a single occurrence, according to available data on forest fires. In the last decade two forest fires occurred that covered an area of over 20,000 ha (19). The number of large forest fires in Portugal is increasing, and the extent of these fires is increasing as well. According to scientists a new era of forest fires has begun in Portugal, and it started somewhere around 1987 (20).

Climate change can be an important driver of greater fire activity (21,22), but it’s not the only one. In fact, in southern Europe climate change seems to be a far less important driver than socio-economic factors and changes in land use (22). Important socio-economic factors are depopulation and ageing of rural populace. Important changes in land use are agricultural abandonment, expansion of highly flammable tree species, and renewed growth of woody vegetation in cleared landscapes. Also, the success in suppressing small and medium size fires is producing landscapes with higher flammability and more fuel loads that contribute to larger and more severe forest fires (23).

Degraded areas become more likely to be affected by fires. These areas are characterized by herbaceous plant and shrubs, which are extremely susceptible to fire because of their low moisture content and flammable fuel load (24). This is a vicious cycle. The rural exodus led to an increase in abandoned farmlands and growth of woody vegetation. This soil degradation as a result leads to more and larger fires that consequently further degrade the soil. Many of these rural areas became liable to the occurrence of devastating fires as a result of the high quantities of biomass accumulated over the years, which could fuel catastrophic fires during the summer months (25). The proportion of uncultivated land, due to the population exodus from rural areas to coastal cities and other European countries since the 1950s, was the most important factor affecting burnt areas in Portugal (26). 

During the summer of 2003 more than 25,000 fires were recorded in Portugal, Spain, Italy, France, Austria, Finland, Denmark and Ireland. The estimation of EU forest areas destroyed reached 647,069 hectares (5). Portugal was the worst hit, Spain came second. This was by far the worst forest fire season that Portugal had faced in the last 23 years. In October 2003, the financial impact estimated by Portugal exceeded 1 billion euros (6). It should be stressed that Portugal and the northwestern provinces of Spain presented the largest number of fires in Europe in 2003 (nearly 50%). These fires were directly responsible, among other consequences, for the loss of 21 lives (7).

The large fires of 2003

Forest fires associated with the heat wave of 2003 resulted in an extremely large burnt area of land - 425 000 ha, corresponding to approximately 13% of the total forest area in the country.The frequency of fires and amount of burnt land in Portugal has increased since 1992, though this trend has been moderately decreasing in the last years (8).

Damage and costs 

In the period (1980-2004), fires have burned over around 2.7 million hectares of Portuguese forest land. Considering only the direct losses associated with primary production, the estimated costs have been about €300 million per year. The total investments in fire fighting and prevention amounted to €479 million in this five-year period (€17.8/hectare/year). In 2001 alone, the damage caused by forest fires amounted to about €137 million (e.g. costs of fire prevention, fire fighting and reforestation, and losses of forest products) (9).

Vulnerabilities - Projections for the future - Mediterranean

Forest fire danger, length of the fire season, and fire frequency and severity are very likely to increase in the Mediterranean (10,11), and will lead to increased dominance of shrubs over trees (12).

Dry weather and damaged ecosystem with accumulation of dead biomass increase the risk of forest fires. Increased climate variability, therefore, will augment the risk of forest fires (13). In addition, forest fires are expected to encourage the spread of invasive species which in turn, have been shown to fuel more frequent and more intense forest fires (14).

An indication of the forest fire risk under the future climate scenarios has been calculated(14). Under both A2 and B2 (IPPC SRES) scenarios, fire risk is shown to increase nearly everywhere in the Mediterranean region, especially in inland locations. The southern Mediterranean is at risk of forest fire all year round. In the Iberian Peninsula, northern Italy and over the Balkans, the period of extreme fire risk lengthens substantially. The only region that shows little change in fire risk is in the southeastern Mediterranean.

In the Iberian Peninsula, mean burnt areas could be about two to three times larger by 2075  than in the present, taking into account current climate projections for the end of this century, and non-significant changes in other external factors, such as human activity, fire suppression or land use (18).

Projections of forest fire risk in 2030-2060 compared with 1961-1990 suggest that (14):

  • The increase is higher during the summer, with maximum increase in August in the North Mediterranean inland;
  • Balkans, Maghreb, North Adriatic, Central Spain, and Turkey are the most affected regions;
  • The south of France is as strongly affected as Spain, but only in August and September;
  • The islands of Crete, Sardinia, Sicily (southernmost Italy too), Peloponnese, and Cyprus see no increase or decrease. Cyprus may even see a small decrease every month;
  • There will be 2 to 6 additional weeks of fire risk everywhere, except for the south of Italy and Cyprus. The maximum increase is again inland (Spain, Maghreb, Balkans, North Italy, and Central Turkey), where at least an additional month with risk of fire is expected. A significant proportion of this increase in fire risk is actually extreme fire risk;
  • The south of France, Crete, and the coastal area of the rest of Mediterranean Region also show a significant increase in the number of days with fire risk (1-4 weeks), but not in the number of extreme fire risk.

Since 1980 an area equivalent to 3/5 of the forested surface in Portugal has burned. The burnt areas in July and August account for 71% of the total burnt area in Portugal (15). The interannual variability of burnt area in Portugal is largely determined by 2 different atmospheric factors, namely (1) the amount of precipitation during spring (i.e. in the pre-fire season) and (2) the occurrence of atmospheric circulation patterns that induce extremely hot and dry spells over western Iberia throughout the summer season (i.e. throughout the fire season) (16).

Projections of the impact of climate change in Portugal (based on a Global Climate Model and the IPCC emission scenario B1) indicate that the mean burnt area in July and August may increase by 7 and 11% for the periods 2051−2080 and 2071−2100, respectively, when compared with the period 1980−2011. The standard deviation for these data are projected to decrease by 32% for 2051−2080 and stay the same for 2071−2100. These results thus point towards an increasing risk of fire under future climate conditions, and an increasing likelihood of much larger burnt areas (15).

Adaptation strategies

Current policies in all Mediterranean countries, based only in reducing the number of ignitions by suppressing fires, will not reduce the extension of the area burnt in large, catastrophic fires. Firefighters can extinguish most of the fires, but when there is one out of the extinction capacity, it burns larger areas than when fire-exclusion policies were not as powerful as today. Fire-exclusion policies have to be inevitably complemented with fuel-reduction techniques and fire prevention management of the forest. Strategic areas with different fuel loads would probably help in the extinction of large wildfires and might help to prevent catastrophic events to occur as frequently as they have been occurring in the Mediterranean basin in the last 20 years (4).


The references below are cited in full in a separate map 'References'. Please click here if you are looking for the full references for Portugal.

  1. Xanthopoulos (2000); Viegas (1998, 2004); Moreno et al. (1998); Piñol et al. (1998) Pausas (2004), all in: Oliveras et al. (2005)
  2. Moreno et al. (1998), in: Oliveras et al. (2005)
  3. Xanthopoulos (2000); Viegas (2004), both in: Oliveras et al. (2005)
  4. Oliveras et al. (2005)
  5. Eisenreich (2005)
  6. UNEP (2004)
  7. Pereira et al. (2005)
  8. Portuguese Environment Agency with the cooperation of Ecoprogresso – Environment and Development Consultants, SA (2006)
  9. Anderson (ed.) (2007)
  10. Santos et al. (2002); Pausas (2004); Moreno (2005); Pereira et al. (2005); Moriondo et al. (2006), all in: Alcamo et al. (2007)
  11. Oficina Española de Cambio Climático (2008)
  12. Mouillot et al. (2002), in: Alcamo et al. (2007)
  13. Ministry for the Environment, Land and Sea of Italy (2007)
  14. Giannakopoulos et al. (2005)
  15. Pereira et al. (2013)
  16. Pereira et al. (2005), in: Pereira et al. (2013)
  17. Camia and Amatulli (2009); Hoinka et al. (2009); Costa et al. (2011); Koutsias et al. (2012), all in: IPCC (2014)
  18. Sousa et al. (2015)
  19. Ferreira-Leite et al. (2016)
  20. Ferreira-Leite et al. (2013a,b), in: Ferreira-Leite et al. (2016)
  21. Piñol et al. (1998), in: Ferreira-Leite et al. (2016)
  22. Pausas (2004), in: Ferreira-Leite et al. (2016)
  23. Pausas and Vallejo (1999); Moreno et al. (1998), both in: Ferreira-Leite et al. (2016)
  24. Catry et al. (2010), in: Ferreira-Leite et al. (2016)
  25. Beverly and Martell (2005); Keeley and Rundel (2005), both in: Ferreira-Leite et al. (2016)
  26. Nunes et al. (2005); Sebastián-López et al. (2008); Catry et al. (2009); Moreira et al. (2009); Bajocco and Ricotta (2008); Nunes (2012); Carmo et al. (2011); Ganteaume and Jappiot (2013), all in: Ferreira-Leite et al. (2016)