http://www.cnr.it/ontology/cnr/individuo/prodotto/ID291979
Temporal patterns of wildfire probability and intensity in Northern Sardinia, Italy (Abstract/Poster in atti di convegno)
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- Temporal patterns of wildfire probability and intensity in Northern Sardinia, Italy (Abstract/Poster in atti di convegno) (literal)
- Anno
- 2014-01-01T00:00:00+01:00 (literal)
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Bachisio Arca, Michele Salis, Alan A. Ager, Grazia Pellizzaro, Gian Valeriano Pintus, Fermin Alcasena, Donatella Spano, Pierpaolo Duce (2014)
Temporal patterns of wildfire probability and intensity in Northern Sardinia, Italy
in EGU General Assembly 2014, Vienna, 27 April - 02 May 2014
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Bachisio Arca, Michele Salis, Alan A. Ager, Grazia Pellizzaro, Gian Valeriano Pintus, Fermin Alcasena, Donatella Spano, Pierpaolo Duce (literal)
- Pagina inizio
- EGU2014-13179-2 (literal)
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- EGU2014-13179-2 (literal)
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- Book of Abstracts of the EGU General Assembly 2014 (literal)
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- Abstract (literal)
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- Institute of Biometeorology, National Research Council, CNR-IBIMET, Sassari, Italy; University of Sassari, Department of Science for Nature and Environmental Resources (DIPNET), Sassari, Italy; Euro-Mediterranean
Center on Climate Change (CMCC), IAFENT Division, Sassari, Italy; USDA Forest Service, Pacific Northwest Research Station, Western Wildland Environmental Threat Assessment Center, Prineville, OR, USA (literal)
- Titolo
- Temporal patterns of wildfire probability and intensity in Northern Sardinia, Italy (literal)
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- European Geosciences Union (literal)
- Abstract
- The prediction of burn probability and intensity by the use of wildfire simulators is a valuable method to capture
the large variability of fire spread and behavior produced by weather and fuel conditions, especially when
extreme weather conditions, and their effects on fuel characteristics, leads to large fires. The planning of fireprone
landscapes is the main area when the evaluation of the burn probability and intensity can provide additional
information for the decision makers. In addition, policy makers and management agencies could use wildfire simulators
at landscape level to monitor and evaluate the impact of prevention plans. In this work we estimated the
past variations of burn probability and intensity using the scenarios of the key wildfire factors (wind field, fuel
moisture, fuel characteristics, and ignition patterns) historically observed during severe and extreme conditions.
Simulations of fire spread were performed using the FlamMap fire mapping and analysis system, based on the
fire spread model of Rothermel and the fire growth method of minimum travel time. The set of simulations were
conducted using the landscape characteristics existing in the year 2000, and were replicated for two time steps in
the past: 1954 and 1977. The wind data required by the simulator were developed by the analysis of the weather
records collected near the experimental area, and using the wind data to simulate the spatial distribution of wind
by a mass-consistent model. The sets of ignition points were generated by sampling algorithms based on random
sampling process, and alternatively considering the historical probability of fire to stratify the random sample. The
fuel moisture condition typical of very dry and extreme days were estimated by the analysis of weather data and
considering local representative data on fuel moisture conditions. Both graphical and analytical methods were used
to highlight the main variations of burn probability and severity, and to find the relationships with the variations of
the main landscape characteristics. The experimental data provided by the simulator shows a clear increase of both
burn probability magnitude and spatial extension induced by the extreme conditions, in particular by the extreme
fuel moisture scenarios. This trend is more evident for the data simulated using the historical ignition scenario. The
experimental data showed also that the land use change observed throughout the study period (from 1954 to 2000)
determined a reduction of burn probability in the last time step (2000), while limited differences were observed
from 1954 to 1977. The recent variation of burn probability was more evident when the historical ignition scenario
was used to perform the simulations, and can be attributed to the modifications of the landscape generated by
the increase of the human activities in the coastal areas, where regional Forest Service statistics show the highest
number of ignitions. In addition, in the last time step we observed a general decrease of the areas characterized by
herbaceous vegetation, more prone to large fire sizes and able to produce large values of burn probability. (literal)
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