e., the Alpine Space projects ALPFFIRS (fire danger rating and prediction; www.alpffirs.eu) and MANFRED (management adaptation strategies to climate change; http://www.manfredproject.eu). This recent interest for the fire issue has been arising from new evidences

observed in fire regime dynamics; for example, the extremely hot summer 2003 and other hotspots occurring during 2006, demonstrated that under suitable fire weather conditions it can burn in Austrian forests nearly everywhere (Gossow et al., 2007), and gave rise to a systematic data collection still not addressed (Arpaci et al., 2013). Furthermore, regional and national fire organizations are providing costly fire fighting RG7420 ic50 services and must provide a safe work environment to fire-fighters. In this key, important steps have been also moved in the direction of cooperation at the national, or regional, boundaries. In fact, fire management

in the Alpine region is fragmented in many different fire organizations; only in Italy, seven regional authorities share 100,000 km2 of http://www.selleckchem.com/products/Everolimus(RAD001).html land to manage, what makes also challenging to get harmonized forest fire datasets as to provide an exhaustive picture at Alpine level. Global change, i.e., current changes in land-use, climate and society, poses several new issues and challenges to fire management in Europe, including the Alpine area (Fernandes et al., 2013). In addition to the long-term ongoing land-use change, pronounced climatic shifts are predicted for mountainous areas of Europe (Reinhard et al., 2005 and Moriondo et al., 2006). Climate warming is likely to selleck antibody interact with land-use changes and alter fire regimes in the Alpine region in unpredicted ways (Schumacher and Bugmann, 2006 and Wastl et al., 2012), with potentially serious consequences on ecosystem services, including economic losses and social

impacts. Higher frequency of exceptional droughts and heat waves in the Alps may increase the occurrence of high intensity fires of relatively large size, particularly on southern slopes (Moser et al., 2010, Ascoli et al., 2013a and Vacchiano et al., 2014a). Unlike in other regions, for instance the Mediterranean basin, the future scenario of large wildfires in the Alps is more likely to be similar to the third generation (sensu Castellnou and Miralles, 2009) than to the fourth and fifth ones. The reason lies in the relatively milder fire-weather, also in a climate change scenario, less flammable fuels and the lower extent and different structure of the wildland–urban interface. Despite this, a change towards the third generation might entail negative consequences on soil stability ( Conedera et al., 2003) and timber quality ( Beghin et al., 2010 and Ascoli et al.