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Transcript of Fires in the perspective of future changes: the contribute of CMCC to FUME Project
Fires in the perspective of future changes: the contribute of CMCC to FUME Project
Bacciu V.1,2*, Alcasena F.1, Arca B.3, Bosello F.1,4,5, Gualdi S.1,6, Noce S.1,Michetti M.1, Otrachshenko W.1, Parrado R. 1,4, Salis M.2,1, Santini M.1,
Scoccimarro E.1,7, Spano. D.2,1
1CMCC, Euro-Mediterranean Center on Climate Change, Italy, 2University of Sassari,
DIPNET – Italy, 3CNR, National Council of Research, IBIMET - Italy, 4Fondazione Eni
Enrico Mattei– Italy, 5University of Milan – Italy, 7INGV, Istituto Nazionale di Geofisica
e Vulcanologia - Italy
*Corresponding Author: [email protected]
Abstract
According to a number of authors, the primary factors determining and shaping fire
regime (climate, topography, fuel, and land use-land cover) were not stable during
the last decades, significantly determining modification in fire regime and fire
severity; however our understanding of how the fire driver changes affected fire
regime in the past is limited. In addition to that, these changes are projected to
continue, increasing fire danger and risk. FUME project (Forest fires under climate, social and economic changes in Europe,
the Mediterranean and other fire-affected areas of the world) aimed to learn from the
past to understand future fire impacts. In this paper, we present and summarize the
most important achievement reached by CMCC, a core partner of the project. The
main findings are that: (1) fire activity significantly changed, also thank to fire
management improvements; (2) future land use distribution, in not regulated, would
contribute to increase fire risk; (3) this increase would be counterbalanced by
projected reduction in wind speed, leading to a lower wildfire rate of spread and size;
(4) the projected average yearly damage induced by Mediterranean forest fires along
the 2020-2070 period ranges from $ 5286 to $ 7587 million.
Keywords: FUME project, fire regime, climate change, land use change, carbon losses
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1. INTRODUCTION
Fire is by far the most frequent and widespread disturbance to vegetation in the world
[1, 2]. This is particularly true in Mediterranean ecosystems [3, 4, 5]. In Southern
Europe, every year about 45000 forest fires occur, burning approximately 0.5 million
hectares of forests and other rural lands [6]. Fire occurrence varies considerably from
one year to the next, which clearly indicates how much the burnt area depends on
seasonal meteorological conditions [7]. On the other hand, the other driving factors
(e.g., land use, vegetation) have not been stable during the last decades, mainly due
to modifications in the territory caused by socioeconomic changes [8]. Looking at the
future, changes in climate and socioeconomics are projected to continue, exposing to
greater fire risk assets, values, and ecosystems [9].
The FUME project (Forest fires under climate, social and economic changes in
Europe, the Mediterranean and other fire-affected areas of the world, FP7, 2010-
2013), coordinated by the University of Castilla-La Mancha (Spain), highlighted how
the understanding of fire controlling factors, and their dynamics, is of utmost
importance for anticipating future fire risks. The project aims were to:
(i) investigate and disentangle the relationships between socioeconomic,
landscape and climate factors, and fires across various scales and
countries during the last decades;
(ii) translate scenarios of climate, land use and socio-economic changes to into
projections of modified fire potential and risk;
(iii) evaluate the capacity to cope with future forest fires and reduce the risk
through preventive or reactive measures [10] and appraised related
economic costs and policies at the European level.
This paper illustrates the most important achievement reached by CMCC (a core
partner of the project) in unraveling the influence of key drivers for fire activity and
regime, projecting future changes and proposing an economic assessment of future
fire damages. Also, the management implications are discussed, along with major
open challenges that still need to be addressed.
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Assessing past fire regimes and changes through time due to the different key
drivers required the collection and the harmonization of long-term databases to
permit analysis spanning over the last thirty years and to enable comparisons among
countries. After gathering information on fire, climate, land use, and socio-economic
data from the EU-Med to the local scale, CMCC concurred to understand, through
modeling and statistical analysis, how modifications occurred in the fire controlling
factors affected fire activity, considering both behavior and regime.
Outcomes resulting from investigating the past guided projections about future fire
risk and fire regime due to climate and other social and economic changes.
Specifically, CMCC developed global and regional climate simulations over the
FUME spatial domain (Fig. 1). In turn, climate projections were used to drive future
land use change (LUC) scenarios produced also taking into account the results of the
CMCC economic-energy model. LUC scenarios were then used by impact models
(from vegetation to fires) to produce future fire risk scenarios.
2.1. Forest fire regime recent trends, changes and weather relationships
Fire regime across the Mediterranean Basin (from EU-Med to National level down to
NUTS2 scale) was described according to major fire characteristics (fire seasonality,
frequency, and inter-annual variability) using fire statistics derived from different
sources. The existence of significant trends and shifts in fire occurrence was also
investigated. Throughout the analyzed time interval (1985-2005), summer (JJAS)
resulted the main burning period, although several countries presented a secondary
peak in early spring. More than the 80% of fires burned less than 10 hectares,
accounting for a small portion (about 11%) of the total burned area. Fire incidence
(burned area over the land area) was higher in Portugal, followed by Spain and Italy.
The whole study area exhibited a general increase in the number of fires. Portugal
(1989 and 1994) and Greece (2000) show an upward trend, while Italy (1994)
exhibits a downward trend [11] (Fig. 2). The burned area had an opposite trend, with
a generalized slight decrease throughout the period considered, significantly in Italy,
Greece, and Turkey. At NUTS2 level, a significant increase in the number of fires
was observed only in Attica and Peloponnese, while burned area followed a general
decrease in all the study areas.
2. ANALYSING THE PAST TO PROJECT THE FUTURE
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CMCC coordinated the analyses of the relationships between weather/climate
conditions and fire through the application of different algorithms and methodologies
at several scales, from the Euro-Mediterranean level, to national, NUT02, and local
scale. At Eu-Med level, precipitation was the variable that more influenced the
multiple linear regression models, while at National level, meteorological conditions,
both antecedent (such as droughts) and during the fire season (such as strong wind,
heat waves), seemed to have a strong influence on seasonal severity (i.e., area
burned) [12]. Several results suggested the dual role of precipitation in fuel build-up
and dryness [13]. Overall, in spite of the use of such a wide range of methodologies
and spatial scales, the importance of similar fire season climatic factors was
observed at all scales. In particular, seasonal droughts in months prior to the fire
season peak, occurrence of heat waves, and strong winds during the fire season had
a strong influence on fire occurrence and seasonal severity across scales [14]. A
specific case study was performed for the Italian domain to investigate, with
statistical techniques, the relevance of socio-economic and meteorological variables
in generating fire occurrence and magnitude during 2000-2008 [15]. Italy is divided
into north, center, and south, to capture local-specific characteristics in fire regimes.
Results highlight the importance of railway networks, livestock presence and fuel
management. Fire containment may derive from limiting illegal activities in the south.
2.2. Climate models and simulations
CMCC developed global and regional climate simulations covering the period 1970-
2100. These were performed using the CMCC-MED CGCM, whereas the regional
ones were produced using the COSMO-CLM RCM. CMCC-MED [16,17] is a coupled
atmosphere-ocean general circulation model. It focuses on the Mediterranean region
and includes a very high-resolution model for the Mediterranean Sea to better
represent the dynamical processes that characterize this region. The COSMO-CLM
[18] is the climate version of the regional COSMO model [19], which is the
operational non-hydrostatic mesoscale weather forecast model developed by the
German Weather Service, further updated by the CLM-Community in order to
develop also climatic applications. In the COSMO-CLM version the horizontal
resolution is 14 Km, thus orography is better described with respect to the global
CMCC-MED model, where there is an over-/underestimation of valley/mountain
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heights resulting in errors for orographic precipitation estimation. The non-hydrostatic
modeling allows providing a good description of the convective phenomena, which
can redistribute significant amounts of moisture, heat and mass on small temporal
and spatial scales. Furthermore, convection can cause severe precipitation events
(as thunderstorm or cluster of thunderstorms). Implementing these two climate
models CMCC i) provided global and regional climate simulations to be used as input
in fire regime and LULC future projections; ii) defined indexes to characterize
extreme events useful to determine fire development conditions [20].
2.3. Land use models and simulations
Interactions between land use/cover dynamics and biophysical (including climate) to
socioeconomic factors were investigated, reproduced and projected for the
Mediterranean basin, comprising Southern European (EU), Middle East (ME) and
North African (NA) countries bordering the Mediterranean Sea. The LUC@CMCC
model [21], forced by the economic-energy model ICES@CMCC [22] provided
spatially-explicit LUC scenarios as inputs to future-fire risk modelling activities in
FUME. The LUC@CMCC model code, suitable for regional applications, was
implemented at about 10 km resolution within two spatial sub-domains of the above
defined Mediterranean basin domain: EU-Med, comprising EU countries; and
EUMENA-Med, also including ME and NA countries. In the first case, the CORINE
land cover dataset was used as reference to calibrate/validate the LUC@CMCC
model between 1990, 2000 and 2006, respecting the CORINE class re-aggregation
as agreed within FUME. In the second case, the MODIS land cover product was
used considering years 2000 and 2006, requiring weaker assumptions for
associating MODIS land cover categories to FUME selected land use/cover classes.
In both cases, also the likely influence of restrictions in protected areas was tested.
In order to assess drivers governing land use allocation, a logistic regression (LR)
analysis verified by Receiving Operating Characteristic test was applied considering
between 10 and 15 explanatory factors, divided into dynamical (climatic and socio-
economic) and static (like accessibility and topographic/geographic location). After
the calibration/validation phase, where mainly temperature and slope demonstrated
to influence land use allocation, observed and model simulated land use in 2000
matched for 84.8% of the area, considered as a good model fit. The statistical
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relationships derived from the LR were thus used to drive the spatial allocation of
land use in the future simulations, considering changes in the dynamical explanatory
factors in terms of population density and especially climate variables, coming from
above regional CMCC and two additional ENSEMBLES project simulations as bias-
corrected and provided to FUME partners.
Future aggregated land use demands to drive LUC@CMCC model were developed
for forestry, pasture, and agriculture using the economic-energy model ICES@CMCC
based on future socio-economic trends, for EU-Med and EUMENA-Med regions. Such
demands, produced for 2035 and 2050 reference years, were interpolated every 10
years up to 2070 and 2100. Results indicate that higher LUCs apply to agriculture-tree,
agro-forestry and shrublands in EU-Med, and to forests in EUMENA-Med. This
implies that during the period ranging from 2000 to 2100, 18.5 and 106 Mha of land in
EU-Med and EUMENA-Med, respectively, should be converted into different uses.
Looking at the results of the EU-Med domain experiment (more robust thanks to the
higher spatial and classification detail of CORINE dataset taken as input, and to the
higher homogeneity of data across EU countries), decadal LUC simulations from
2000 to 2100 showed that, more than 10% of the territory (almost 20 Mha) could
undergo changes (Fig. 3). When assuming protected area as territories preserved
from changes, land modifications were reduced to 9% of the region, with about 2 Mha
saved from any LUC. This confirms how land protection and regulation can favor
more balanced demands and allocation of lands, avoiding overpressure and loss of
natural suitability for specific uses, functions or services. Fuel spatial distribution is a
key factor of these future changes: ensemble results show a future increase of land
surface with medium to high fire hazard (Fig. 4). Successively, a further ensemble of
simulations at local level (100 m resolution), based on combination of multiple climate
change and socioeconomic projections, were performed for selected case studies (2
in Spain, 1 in France, 1 in Italy, and 1 in Greece), adapting the LUC model for local
evaluations on fire hazard at finer spatial detail.
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In the context of recent changes occurred in the Mediterranean area, fire activity and
burned area are expected to be influenced by changes in fuel types and
characteristics, in addition to climatic conditions. Two fire spread simulators based on
the Rothermel’s model (FARSITE [23] and FlamMap [24]) were used in different
configurations with the aim to (i) calibrate wildfire models along the Mediterranean
basin considering a set of historical wildfires, and then to (ii) analyze the effects
through time of the main environmental factors (wind speed, wind direction, fuel
moisture, land use changes, ignition locations) on wildfire likelihood and intensity [25,
26, 27]. For the predictive objective, two time periods were used to provide input data
for simulations: the past conditions of land use and key factors between 1950 and
2000, and the future conditions, from the present to 2070. Spatial and temporal
variations in wildfire size and burn probabilities, derived from the simulated fire
perimeters, and fire intensity, derived from simulated flame length, were evaluated
and associated to the key factors, analyzing the anomalies induced by both land
uses, and predicted variation in fuel moisture and weather conditions.
The efficacy of wildfire simulators as tools in wildfire analysis and prediction was
confirmed by the modeling activities, at different temporal and spatial scales. The
results revealed that both accurate wind field data and custom fuel models are critical
in predicting wildfire spread and behavior, allowing to increase the reliability of the
predicted outputs.
In addition, the application of simulators in a probabilistic configuration considering
past conditions of land use and other key factors highlighted significant reductions in
wildfire size and increases in wildfire intensity in recent time steps in comparison with
simulations performed in ‘60s and ‘70s, mainly due to land use changes and fuel
dryness increase (Fig. 5). In fact, future changes in land use projected a limited but
generalized increase of sclerophyllous vegetation and forests, along with a reduction
in grasslands and open pastures, with an increase in fuel load and continuity. On the
other hand, the projected reduction in wind speed for future scenario will result in
lower wildfire rate of spread and size.
2.4. Fire drivers influencing fire activity: investigation of the past and outlook of the
future
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CMCC social economic assessment of the direct costs implied by future fire events in
the Mediterranean area is based upon area burned, direct carbon releases and
change in carbon sequestered due to future fire events derived from the model
SPITFIRE [28]. The economic assessment focuses on: the non use, non market cost
associated to the loss of forest ecosystems; the social cost implied by damages
induced by carbon emissions from forest fires; the potential value added loss
consequent to the fire-induced disruption of forest areas.
Passive value losses are estimated computing the existence value per forest hectare
in the different Mediterranean countries through meta analysis of the stated
preference literature and value transfer methodologies. In 2070, the Mediterranean
area can experience an average loss of non use value of $ 200 million and of $ 97
million in RCP 8.5 and 2.6 respectively. Losses are notably higher in the richer
countries, accordingly in the EU Med area, and particularly in Spain, which combines
high willingness to pay (high marginal passive value attached to the forest hectare)
with huge amounts of burnt hectares.
Market losses are even higher. Starting from the contribution that forestry sectors
provide to national value added and extracting from this an estimate of the value
added generated by an hectare of forest in each Mediterranean country it turns out
that the burnt area can originate a loss ranging between $ 848 million in 2035 and $
2418 million in 2070 in RCP 8.5.
The social damage implied by fire-related emissions in the Mediterranean is
computed using a comprehensive set of estimated of the social cost of carbon. What
is evaluated is the loss of carbon sequestered by vegetation in burnt areas. All in all,
the average yearly damage induced globally by Mediterranean forest fires along the
2020-2070 period amounts to $ 7587 million in the RCP8.5 and to $ 5286 million in
RCP 2.6. This average figure hides however huge differences across social cost of
carbon estimates which largely depend upon the pure rate of time preferences
adopted by the different assessments.
Finally, it is shown that if additional emissions from Euro-Mediterranean forest fires
had to be part of the EU emission reduction targets for 2030, policy costs would
increase between 0.3 and 0.9 additional per cent points of GDP depending on the
climatic model used.
2.5. Economic assessment of future fire regime driven by climate-change
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3. POLICY AND MANAGEMENT IMPLICATIONS
In this paragraph, the management implication deriving from CMCC results in FUME
project are presented:
One of the main limitations for the analysis of long-term fire regimes was the
lack of long-term comparable and harmonized historical records. Further
efforts towards harmonized definitions, formats and methodologies in fire data
acquisition and assemblage across countries are needed.
Fire activity has been changing in the Euro Mediterranean countries, also
thank to the law enforcement and the improvement of fire management
services and monitoring systems across the analysed countries [e.g. 26].
However, fire extreme events under severe weather conditions occurred in
recent years (e.g., 2007, 2009) seemed to overwhelm the fire-fighting
agencies. Progress in weather forecasting, as well as long-range predictions,
may be used to enhance fire danger and risk prediction and anticipate fire
season dynamics.
LUC modeling results suggest that Mediterranean future land use distribution,
if not appropriately regulated, and if combined to expected climate trends,
would contribute to continuously increase land vulnerability to fires. On the
other hand, modeling is confirmed a valuable tool in land protection planning,
including fire hazard/vulnerability reduction strategies.
Socio-economic, climate and biophysical aspects should be all considered
when assessing future fire risk scenarios. Indeed, our results showed the
relevance of each standalone driver-category as well as the importance of
accounting for their interconnection.
Wildfire simulators can provide data, maps, and guidelines that can be used
from tactical and strategic planning of wildfire management, to firefighter
training, and even to real-time firefighting. Throughout the output of these
tools, policy makers and management agencies can plan investments and
activities and evaluate the responses at fine scale, even in a perspective of
future climate changes and/or other changes.
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Forest fire events can entail and induce non-negligible economic losses.
Moreover, the values highlighted in this research should be considered lower
bound estimates of the cost involved, as for instance they do not account for
impact on health and loss of human life. This calls for pro-active policy
interventions at the national and local level to put in place appropriated
anticipatory measures.
4. ACKNOWLEDGMENTS
This work was funded by the European Union Seventh Framework Programme
(FP7/2007-2013) under Grant Agreement 243888 (FUME Project - Forest fires under
climate, social and economic changes in Europe, the Mediterranean and other fire-
affected areas of the world).
5. REFERENCES
1 Bowman DM, Balch JK, Artaxo P, Bond WJ, Carlson JM, Cochrane MA,
D'Antonio CM, Defries RS, Doyle JC, Harrison SP, Johnston FH, Keeley JE,
Krawchuk MA, Kull CA, Marston JB, Moritz MA, Prentice IC, Roos CI, Scott AC,
Swetnam TW, van der Werf GR, Pyne SJ., 2009. Fire in the Earth system.
Science. 2009 Apr 24;324(5926):481-4.
2 Krawchuk, M.A., Moritz, M.A., Parisien, M.A., Van Dorn, J., Hayhoe, K., 2009.
Global Pyrogeography: the Current and Future Distribution of Wildfire. PLoS ONE
4(4): e5102. doi:10.1371/journal.pone.0005102)
3 San-Miguel, J. and Camia, A., 2009. Forest fires at a glance: Facts, figures and
trend in the EU. In: Living with wildfires: What science can tell us? Y. Birot (ed).
European Forest institute, Discussion paper 15, pp 11-18
4 Keeley J.E, Fotheringham C.J., Morais M., 1999. Reexamining Fire
Suppression Impacts on Brushland Fire Regimes SCIENCE VOL 284 11 JUNE
1829-1832
5 van Wilgen, B.W., Forsyth, G.G., De Klerk, H., Das, S., Khuluse, S., and
Schmitz, P., 2010. Fire management in Mediterranean-climate shrublands: a case
study from the Cape fynbos, South Africa. Journal of Applied Ecology 47:631-638.
Impacts & implications of Climate Change
SISC, Second Annual Conference Climate change: scenarios, impacts and policy
1014
6 Camia, A., Amatulli, G. and San-Miguel-Ayanz, J. (2008) Past and future trends
of forest fire danger in Europe (JRC 46533, EUR 23427 EN). European
Commission, Joint Research Centre.
7 European Commission, Joint Research Centre, Institute for Environment and
Sustainability 2010. Forest fire in Europe. doi:10.2788/46294
8 Moreira F., Viedma O., Arianoutsou M., Curt T., Koutsias N., Rigolot E., Barbati
A., Corona P., Vaz P., Xanthopoulos G., Mouillot F. and Bilgili E. (2011)
Landscape – wildfire interactions in Southern Europe: implications for landscape
management, Journal of Environmental Management, vol. 92, 2389-2402,
doi:10.1016/j.jenvman.2011.06.028
9 IPCC, 2014 Impacts, Adaptation, and Vulnerability. Volume II: Regional
Aspects. Ch. 23 Europe
10 Moreno JM 2014 Introduction. In: Josè M. Moreno (ED), Lesson learned and
Outlook, ISBN: 9788469597590.
11 SPANO D., CAMIA A. BACCIU V., MASALA F., DUGUY B., TRIGO R.,
SOUSA P., VENÄLÄINEN A., MOUILLOT F., CURT T., MORENO J.M., ZAVALA
G., URBIETA I.R., KOUTSIAS N., XYSTRAKIS F. (2014). Recent trends in forest
fires in Mediterranean areas and associated changes in fire regimes. In: Josè M.
Moreno (ED), FUME Lesson learned and Outlook. p. 6-7, ISBN: 9788469597590.
12 Pereira M.G., Calado T.J., DaCamara C.C., and T. Calheiros, 2013. Effects of
regional climate change on rural fires in Portugal. Climate Research, 57: 187–
200.
13 Xystrakis F., Kallimanis A.S., Dimopoulos P., Halley J.M., and N. Koutsias,
2013. Precipitation dominates fire occurrence in Greece (1900–2010): its dual
role in fuel build-up and dryness. Natural Hazards and Earth System Sciences, 1
(2): 693–720.16 Gualdi et al. 2010,
14 BACCIU V., TRIGO R., SPANO D., MASALA F., DUGUY B., PASTOR P.,
SOUSA P., VENÄLÄINEN A., MOUILLOT F., MORENO J.M., ZAVALA G.,
URBIETA I.R., KOUTSIAS N., XYSTRAKIS F., ARIANOUTSOU M., MALLINIS
G., GONZÁLEZ M.E., URRUTIA R., LARA A., KAVCACI A., MIDGLEY G., GUO
D., LE MAITRE D., FORSYTH G., SOUTHEY D., ARCA B., BONORA L.,
Impacts & implications of Climate Change
SISC, Second Annual Conference Climate change: scenarios, impacts and policy
1015
CONESE C., DA CAMARA C., PEREIRA M.G., GOUVEIA C., CAMIA A.,
AMATULLI G., VILAR L., SAN MIGUEL-AYANZ J., HAIRECH T., ASSALI F.,
MOKSSIT A., CHERKI K., ALAOUI H. (2014). Fire and weather relationships:
present climate. In: Josè M. Moreno (ED), FUME Lesson learned and Outlook. p.
18-19, ISBN: 9788469597590.
15 Michetti M., Pinar M., (2012) Forest fires in Italy: an econometric analysis of
major driving factors. CMCC Research Paper, RP052, 2012
16 Gualdi S., Scoccimarro E., Navarra A., 2008. Changes in Tropical Cyclone
Activity due to Global Warming: Results from a High-Resolution Coupled General
Circulation Model. J. of Clim., 21, 5204-5228.
17 Scoccimarro E., S. Gualdi, A. Bellucci, A. Sanna , P.G. Fogli,E. Manzini, M.
Vichi, P. Oddo, A. Navarra (2011) Effects of Tropical Cyclones on Ocean Heat
Transport in a High Resolution Coupled General Circulation Model. Journal of
Climate, doi: 10.1175/2011JCLI4104.1
18 Rockel B., Will A., Hense A., 2008. The regional Climate Model COSMO-CLM
(CCLM), Meteorologische Zeitschrift, 17 (4): 347-348.
19 Steppeler J., Doms G., Schättler U., Bitzer H.W., Gassmann A., Damrath U.,
Gregoric G., 2003. Meso-gamma scale forecasts using the nonhydrostatic model
LM, Meteorol. Atmos. Phys., 82 75-96.
20 Sanna A., Scoccimarro E., Gualdi S., Bellucci A., Montesarchio M.,
Bucchignani E. (2012) Extreme events as represented by high resolution CMCC
climate models at global and regional (Euro-Mediterranean) scale. In: Spano D.,
Bacciu V., Salis M., Sirca C. (eds.). Modelling Fire Behaviour and Risk, pag. 99-
105. ISBN: 978-88-904409-7-7.
21 Santini M, Valentini R (2011) Predicting hot-spots of land use change in Italy
by ensemble forecasting. Regional Environmental Change, 11(3): 483-502
22 Michetti M., Parrado R., (2012) Improving land use modelling within CGE to
assess forest-based mitigation potential and costs. FEEM Note di Lavoro,
2012.019
23 Finney MA (2002). Fire growth using minimum travel time methods. Canadian
Journal of Forest Research 32(8): 1420-1424
Impacts & implications of Climate Change
SISC, Second Annual Conference Climate change: scenarios, impacts and policy
1016
24 Finney MA (2006). An overview of FlamMap fire modeling capabilities. In: Fuels
management—how to measure success: conference proceedings. 2006 March 28-
30; Portland, Oregon. Proceedings RMRS-P-41. Fort Collins, CO: U.S. Department
of Agriculture, Forest Service, Rocky Mountain Research Station: 213-220.
25 Arca B., Pellizzaro G., Duce P., Salis M., Bacciu V., Spano D., Ager A.,
Scoccimarro E. (2012) Potential changes in fire probability and severity under
climate change scenarios in Mediterranean areas- In: Spano D., Bacciu V., Salis
M., Sirca C. (eds.). Modelling Fire Behaviour and Risk, pag. 92-98. ISBN: 978-88-
904409-7-7.
26 Salis M, Alcasena F., Ager A.A., Casula F., Arca B., Bacciu V., and Spano D.
(2013) Analyzing changes in wildfire likelihood and intensity in Mediterranean
areas: a case study from central Sardinia, Italy. Proceedings of the SISC 2013
27 Salis M, Ager AA, Finney MA, Arca B, Spano D (2014) Analyzing
spatiotemporal changes in wildfire regimes and exposure across a Mediterranean
fire-prone area. Natural Hazards 71(3): 1389-1418. ISSN: 0921-030X
28 Thonicke, K, Spessa, A., Prentice, I.C., Harrison, S.P., Dong5, L. and C.
Carmona-Moreno (2010) The influence of vegetation, fire spread and fire
behaviour on biomass burning and trace gas emissions: results from a process-
based model”, Biogeosciences, 7, 1991–2011
29 ARCA B., SALIS M., BENOIT J., DUGUY B., ALCASENA F., KOUTSIAS N.,
MALLINIS G., ZAVALA G., URBIETA I.R., CURT T, SPANO D. (2014). Assessing
changes in fire hazard in Mediterranean landscapes by fire modelling. In: Josè M.
Moreno (ED), Forest fires under climate, social and economic changes in Europe,
the Mediterranean and other fire-affected areas of the world. p. 24-25, ISBN:
9788469597590.
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6. IMAGES AND TABLES
Fig. 1 The FUME spatial domain
Fig. 2 Evolution of average fire number and area burned by time steps (1985-1989, 1990-1994,1995-1999, 2000-2005) in FUME EU-Med study areas (modified from 11)
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Fig. 3 EU-Med scale maps show simulated changes in land use distribution from year 2000 (a)to 2100 (b).
10
20
30
40
50
60
70
80
90
100
2000 2040 2070 2100
Mha
years
Fire Hazard
very lowlowmediumhigh
LegendAgriculture-CropsAgriculture-TreesAgroforestryAgriculture-Natural VegetationHerbaceous vegetation ForestsShrubsShrubs (with scattered trees)Burnt areas Urban with vegetationOpen spacesArtificialWetlandsWater
Fig. 4 Spatial distribution in surface (Mha) of fire hazard classes based on LUC classification and projections. The base year 2000 is compared with three future periods in the short (2040), medium (2070) and long (2100) term.
Impacts & implications of Climate Change
SISC, Second Annual Conference Climate change: scenarios, impacts and policy
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Fig. 5 On the left, maps of the North Sardinia (Italy) study area showing FlamMap flame length (m) estimates using different scenarios of fuel moisture and wind speed; the fuel model map was derived from 1977 land cover and land use data. On the right, temporal variation (%) of FlamMap burn probabilities calculated between 1977 and 2000 using different scenarios of fuel moisture and wind speed. The burn probability is the chance that a pixel will burn considering one ignition in the whole study area (from 29)
Impacts & implications of Climate Change
SISC, Second Annual Conference Climate change: scenarios, impacts and policy
1020