31 results on '"Ruffault J"'
Search Results
2. Projections of fire danger under climate change over France: where do the greatest uncertainties lie?
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Fargeon, H., Pimont, F., Martin-StPaul, N., De Caceres, M., Ruffault, J., Barbero, R., and Dupuy, J-L.
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- 2020
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3. Correction to: Live fuel moisture content (LFMC) time series for multiple sites and species in the French Mediterranean area since 1996
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Martin-StPaul, N., Pimont, F., Dupuy, J. L., Rigolot, E., Ruffault, J., Fargeon, H., Cabane, E., Duché, Y., Savazzi, R., and Toutchkov, M.
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- 2018
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4. What do you mean, ‘megafire’?
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Linley, GD, Jolly, CJ, Doherty, Tim, Geary, William, Armenteras, D, Belcher, CM, Bliege Bird, R, Duane, A, Fletcher, MS, Giorgis, MA, Haslem, A, Jones, GM, Kelly, LT, Lee, CKF, Nolan, RH, Parr, CL, Pausas, JG, Price, JN, Regos, A, Ritchie, Euan, Ruffault, J, Williamson, GJ, Wu, Q, Nimmo, DG, Linley, GD, Jolly, CJ, Doherty, Tim, Geary, William, Armenteras, D, Belcher, CM, Bliege Bird, R, Duane, A, Fletcher, MS, Giorgis, MA, Haslem, A, Jones, GM, Kelly, LT, Lee, CKF, Nolan, RH, Parr, CL, Pausas, JG, Price, JN, Regos, A, Ritchie, Euan, Ruffault, J, Williamson, GJ, Wu, Q, and Nimmo, DG
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- 2022
5. A Bioeconomic Projection of Climate‐Induced Wildfire Risk in the Forest Sector
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Riviere, M., primary, Pimont, F., additional, Delacote, P., additional, Caurla, S., additional, Ruffault, J., additional, Lobianco, A., additional, Opitz, T., additional, and Dupuy, J. L., additional
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- 2022
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6. Modelling live fuel moisture content at leaf and canopy scale under extreme drought using a lumped plant hydraulic model
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Martin-StPaul, N, primary, Ruffault, J, additional, Blackmann, C, additional, Cochard, H, additional, De Cáceres, M, additional, Delzon, S, additional, Dupuy, JL, additional, Fargeon, H, additional, Lamarque, L, additional, Moreno, M, additional, Parsell, R, additional, Pimont, F, additional, Ourcival, JM, additional, Torres-Ruiz, J, additional, and Limousin, JM, additional
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- 2020
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7. Prediction of regional wildfire activity with a probabilistic Bayesian framework
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Pimont, F, primary, Fargeon, H, additional, Opitz, T, additional, Ruffault, J, additional, Barbero, R, additional, Martin StPaul, N, additional, Rigolot, E, additional, Rivière, M, additional, and Dupuy, JL, additional
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- 2020
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8. Increased likelihood of heat-induced large wildfires in the Mediterranean Basin
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Ruffault, J, Curt, T, Moron, V, Trigo, RM, Mouillot, F, Koutsias, N, Pimont, F, Martin-StPaul, NK, Barbero, R, Dupuy, J-L, Russo, A, Belhadj-Kheder, C, Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), Aix Marseille Université (AMU), Risques, Ecosystèmes, Vulnérabilité, Environnement, Résilience (RECOVER), Aix Marseille Université (AMU)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Universidade de Lisboa = University of Lisbon (ULISBOA), Centre d’Ecologie Fonctionnelle et Evolutive (CEFE), Université Paul-Valéry - Montpellier 3 (UPVM)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro - Montpellier SupAgro, Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro), University of Patras, Ecologie des Forêts Méditerranéennes (URFM), Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Université de la Manouba [Tunisie] (UMA), FCT (Fundação para a Ciência e a Tecnologia, Portugal) under project IMPECAF (PTDC/CTA-CLI/28902/2017), ANR-11-IDEX-0001,Amidex,INITIATIVE D'EXCELLENCE AIX MARSEILLE UNIVERSITE(2011), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD), Universidade de Lisboa (ULISBOA), Université Paul-Valéry - Montpellier 3 (UPVM)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro), Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), and University of Patras [Patras]
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Heat induced ,Ecology ,010504 meteorology & atmospheric sciences ,Fire ecology ,[SDE.MCG]Environmental Sciences/Global Changes ,lcsh:R ,Natural hazards ,lcsh:Medicine ,Climate change ,15. Life on land ,010501 environmental sciences ,Future climate ,01 natural sciences ,Mediterranean Basin ,Article ,Fire weather ,13. Climate action ,Climatology ,Environmental science ,lcsh:Q ,lcsh:Science ,Climate-change impacts ,0105 earth and related environmental sciences - Abstract
International audience; Wildfire activity is expected to increase across the Mediterranean Basin because of climate change. However, the effects of future climate change on the combinations of atmospheric conditions that promote wildfire activity remain largely unknown. Using a fire-weather based classification of wildfires, we show that future climate scenarios point to an increase in the frequency of two heat-induced fire-weather types that have been related to the largest wildfires in recent years. Heat-induced fire-weather types are characterized by compound dry and warm conditions occurring during summer heatwaves, either under moderate (heatwave type) or intense (hot drought type) drought. The frequency of heat-induced fire-weather is projected to increase by 14% by the end of the century (2071-2100) under the RCP4.5 scenario, and by 30% under the RCP8.5, suggesting that the frequency and extent of large wildfires will increase throughout the Mediterranean Basin. Wildfire is a complex phenomenon that occurs when three conditions are met: available fuel, an ignition source (due to lightning or human activities) and weather conditions conducive to fires (fire weather) 1. Climate and weather are important drivers of wildfire activity across a range of timescales 2-5 , and, consequently, current and potential future climate-induced changes in wildfire activity might threaten ecosystems and human well-being 6. In most Euro-Mediterranean countries, wildfire activity has been declining owing to management and suppression measures undertaken since the 1980s 7. However, some recent extreme wildfire events, including those that occurred in 2016 in France 8 , 2017 in Spain and Portugal 9 and 2018 in Greece 10 have highlighted the limits of wildfire suppression capabilities under exceptional fire-weather conditions. Furthermore, studies show that wildfire activity is expected to increase across the Mediterranean Basin due to climate change 11,12. However, how the combinations of climate and weather conditions that promote the largest wildfires will respond to climate change remain largely unknown. Climate and weather are both drivers of wildfire activity. Soil moisture deficit over days to months increases fuel aridity and flammability 6,13 while a number of synoptic weather conditions associated to different combinations of short-term and instantaneous meteorological fields (precipitation, temperature, relative humidity and wind speed) influence wildfire behaviour 5,14. Most of the largest wildfires occur when these conditions are met 8. For instance, the combination of extreme drought with extreme wind or heatwaves have both been identified as crucial factors in the occurrence of crown wildfires in Mediterranean forests and shrublands 15-17. In this study, we focus on the frequency of current and future weather and climate conditions associated with wildfires in four countries (France, Portugal, Greece, Tunisia) of the Mediterranean basin covering most of its diverse biogeographic and climatic conditions (Supplementary Figs. S1-S3). Building on the insights gained open
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- 2020
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9. Impact des condition locales de sol et sou-sol sur le variabilité inter-individuelle de réponse à la sécheresse : apport de la tomographie de résistivité électrique
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Carrière, S. D., Ruffault, J., Pimont, F., Doussan, C., Simioni, G, CHALIKAKIS, Konstantinos, Limousin, J.-M, Scotti, I, Courdier, F, Cakpo, C.-B, Davi, H, Martin St-Paul, N. K., Environnement Méditerranéen et Modélisation des Agro-Hydrosystèmes (EMMAH), Avignon Université (AU)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Avignon Université (AU), Service National d'Observation sur le KARST (SNO Karst), Institut national des sciences de l'Univers (INSU - CNRS), Risques, Ecosystèmes, Vulnérabilité, Environnement, Résilience (RECOVER), Aix Marseille Université (AMU)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Institut National de la Recherche Agronomique (INRA), Unité de Recherches Forestières Méditerranéennes (URFM), Centre d’Ecologie Fonctionnelle et Evolutive (CEFE), Université Paul-Valéry - Montpellier 3 (UPVM)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro - Montpellier SupAgro, Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro), Unité de recherche Plantes et Systèmes de Culture Horticoles (PSH), Université Paul-Valéry - Montpellier 3 (UM3)-Institut National de la Recherche Agronomique (INRA)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-École pratique des hautes études (EPHE)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro), Institut de Recherche pour le Développement (IRD [France-Sud])-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE)-Université de Montpellier (UM)-Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro)-Institut National de la Recherche Agronomique (INRA)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-Université Paul-Valéry - Montpellier 3 (UM3), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Aix Marseille Université (AMU), Centre National de la Recherche Scientifique (CNRS)-Université de Montpellier (UM)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-Institut National de la Recherche Agronomique (INRA)-Université Paul-Valéry - Montpellier 3 (UPVM)-Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro), and Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut de Recherche pour le Développement (IRD [France-Sud])
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leaf traits ,[SDV.EE]Life Sciences [q-bio]/Ecology, environment ,Mediterranean forests ,[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] ,hydrogeophysics ,tree water status ,ERT ,drought response ,[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology ,[SDE.BE]Environmental Sciences/Biodiversity and Ecology ,[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study ,[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology - Abstract
International audience; Inter-individual variability of tree drought responses within a stand has received little attention. Here we explore whether the spatial variations in soil/subsoil properties assessed through electrical resistivity tomography (ERT) could explain variations in drought response traits among trees.We used ERT to compute the percent variation in resistivity (PVR) between dry and wet conditions as an indicator of spatial variability in total available water content. PVR was computed in two different depth ranges (0-2 and 2-5 m) for eleven Quercus ilex stools in a Mediterranean forest stand. PVR values were compared to biological traits, including tree water status (predawn water potential (Ψ)), leaf traits (δ 13 C, leaf mass area (LMA)), and canopy defoliation measured after intense drought.We found significant correlations between PVR and biological variables. For Ψ , the nature and strength of the correlations vary according to the level of drought intensity. The correlation between Ψ and PVR was positive during well-watered conditions in the upper layer (0-2 m) and during water-limited conditions in the deeper layer (2-5 m). During most severe droughts, however, the Ψ was negatively correlated with PVR in the upper layer. Trees with lower PVR in the upper layer were also associated with water use efficiency (higher δ 13 C), higher LMA, and a lower level of defoliation after extreme drought.Overall, our results indicate that local differences in soil/subsoil properties affect tree response to drought and suggest that less favorable soil/subsoil conditions (lower PVR) can lead to lower water stress during the driest period and to lower defoliation after extreme drought. Plausible explanations for this better acclimation include higher stomatal regulation and improved deep soil and subsoil water exploration by trees located in more adverse conditions. We encourage the development of ERT in ecological studies to further explore the interrelated relationships between soil/subsoil, climate, and tree functioning.
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- 2020
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10. Increased likelihood of heat-induced large wildfires in the Mediterranean Basin
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Ruffault, J, primary, Curt, T, additional, Moron, V, additional, Trigo, RM, additional, Mouillot, F, additional, Koutsias, N, additional, Pimont, F, additional, Martin-StPaul, NK, additional, Barbero, R, additional, Dupuy, J-L, additional, Russo, A, additional, and Belhadj-Kheder, C, additional
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- 2020
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11. Why is the effect of live fuel moisture content on fire rate of spread underestimated in field experiments in shrublands?
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Pimont, F., primary, Ruffault, J., additional, Martin-StPaul, N. K., additional, and Dupuy, J.-L., additional
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- 2019
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12. A Cautionary Note Regarding the Use of Cumulative Burnt Areas for the Determination of Fire Danger Index Breakpoints
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Pimont, F., primary, Ruffault, J., additional, Martin-StPaul, N.K., additional, and Dupuy, J.-L., additional
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- 2019
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13. Live fuel moisture content (LFMC) time series for multiple sites and species in the French Mediterranean area since 1996
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Martin-StPaul, N., primary, Pimont, F., additional, Dupuy, J. L., additional, Rigolot, E., additional, Ruffault, J., additional, Fargeon, H., additional, Cabane, E., additional, Duché, Y., additional, Savazzi, R., additional, and Toutchkov, M., additional
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- 2018
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14. Daily synoptic conditions associated with large fire occurrence in Mediterranean France: evidence for a wind-driven fire regime
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Ruffault, J., Moron, Vincent, Trigo, R., Curt, T., Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA), Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS), Faculdade de Ciências [Lisboa], Universidade de Lisboa (ULISBOA), Risques, Ecosystèmes, Vulnérabilité, Environnement, Résilience (RECOVER), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Collège de France (CdF)-Institut national des sciences de l'Univers (INSU - CNRS)-Aix Marseille Université (AMU)-Institut National de la Recherche Agronomique (INRA), and Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
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[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology ,GRANDS INCENDIES ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,MÉTÉOROLOGIE ,ComputingMilieux_MISCELLANEOUS - Abstract
[Departement_IRSTEA]Territoires [TR1_IRSTEA]SEDYVIN [ADD1_IRSTEA]Adaptation des territoires au changement global [Departement_IRSTEA]Territoires [TR1_IRSTEA]SEDYVIN [ADD1_IRSTEA]Adaptation des territoires au changement global; International audience; Changes in wildfire activity in the Mediterranean area over recent decades increase the need for a better understanding of the fire weather relationships and for the development of reliable models to improve fire danger prediction. This study analyses daily synoptic and local weather conditions associated with the occurrence of summer large fires (LFs) in Mediterranean France during recent decades (1973-2013). The links between large fire occurrence and synoptic conditions are analysed with composites of sea level pressure and winds at 925 hPa and a parsimonious synoptic weather type (WT) classification based on these variables. A cluster analysis is used to identify five homogeneous regions with similar inter-annual variations in lire activity. Our results reveal a dominant wind-driven lire regime, i.e. wind conditions are the main factor explaining why fire become large, though substantial temporal and spatial variations are observed. Thus, most LFs occur under the `Atlantic Ridge' WT that combines an anticyclonic ridge over eastern Atlantic and a cyclonic anomaly stretched from the North Sea to Central/Eastern Europe and Mediterranean basin. This pattern is significantly related at local scale to fast continental dry winds. By contrast, only few LFs occur under WT's characterized by anomalously warm local-scale conditions ('Blocking'), except under very warm and dry conditions such as during the outstanding 2003 summer. These results offer promising developments for the improvement of fire danger predictions and operational management.
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- 2017
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15. Can We Go Beyond Burned Area in the Assessment of Global Remote Sensing Products with Fire Patch Metrics?
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Nogueira, J. M. P., Ruffault, J., Chuvieco, E., and Mouillot, Florent
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LANDSAT ,remote sensing ,burned patch ,Science ,patch indices ,patch shape ,MODIS MCD45A1 ,ESA FIRE_CCI ,fire ,savannas - Abstract
Global burned area (BA) datasets from satellite Earth observations provide information for carbon emission and for Dynamic Global Vegetation Model (DGVM) benchmarking. Fire patch identification from pixel-level information recently emerged as an additional way of providing informative features about fire regimes through the analysis of patch size distribution. We evaluated the ability of global BA products to accurately represent morphological features of fire patches, in the fire-prone Brazilian savannas. We used the pixel-level burned area from LANDSAT images, as well as two global products: MODIS MCD45A1 and the European Space Agency (ESA) fire Climate Change Initiative (FIRE_CCI) product for the 2002-2009 time period. Individual fire patches were compared by linear regressions to test the consistency of global products as a source of burned patch shape information. Despite commission and omission errors respectively reaching 0.74 and 0.81 for ESA FIRE_CCI and 0.64 and 0.62 for MCD45A1 when compared to LANDSAT due to missing small fires, correlations between patch areas showed R-2 > 0.6 for all comparisons, with a slope of 0.99 between ESA FIRE_CCI and MCD45A1 but a lower slope (0.6-0.8) when compared to the LANDSAT data. Shape complexity between global products was less correlated (R-2 = 0.5) with lower values (R-2 = 0.2) between global products and LANDSAT data, due to their coarser resolution. For the morphological features of the ellipse fitted over fire patches, R-2 reached 0.6 for the ellipse's eccentricity and varied from 0.4 to 0.8 for its azimuthal directional angle. We conclude that global BA products underestimate total BA as they miss small fires, but they also underestimate burned patch areas. Patch complexity is the least correlated variable, but ellipse features appear to provide information to be further used for quality product assessment, global pyrogeography or DGVM benchmarking.
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- 2016
16. Objective identification of multiple large fire climatologies: an application to a Mediterranean ecosystem
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Ruffault, J., Moron, Vincent, Trigo, R., Curt, T., Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS), Faculdade de Ciências [Lisboa], Universidade de Lisboa (ULISBOA), Risques, Ecosystèmes, Vulnérabilité, Environnement, Résilience (RECOVER), and Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)
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[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology ,ComputingMilieux_MISCELLANEOUS - Abstract
International audience
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- 2016
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17. Classification objective des conditions météorologiques associées aux grands incendies de forêts : une application à un écosystème méditerranéen
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Ruffault, J., Moron, V., Trigo, R., Curt, T., Risques, Ecosystèmes, Vulnérabilité, Environnement, Résilience (RECOVER), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Aix Marseille Université (AMU)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Instituto Dom Luiz, Universidade de Lisboa = University of Lisbon (ULISBOA), Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Collège de France (CdF)-Institut national des sciences de l'Univers (INSU - CNRS)-Aix Marseille Université (AMU)-Institut National de la Recherche Agronomique (INRA), Universidade de Lisboa (ULISBOA), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA), and Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)
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modelling ,climatic change ,RISQUE D'INCENDIE ,[SDE.IE]Environmental Sciences/Environmental Engineering ,[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology ,FACTEUR METEOROLOGIQUE ,CHANGEMENT CLIMATIQUE ,fire risk ,FORET MEDITERRANEENNE ,[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology ,MODELISATION ,mediterranean forest - Abstract
[Departement_IRSTEA]Territoires [TR1_IRSTEA]SEDYVIN; International audience; Here we classify summer LFs (>120 ha) in Mediterranean France for the period 1973 to 2012, according to their local-scale weather conditions (i.e. temperature, relative humidity, wind speed and fuel moisture proxies). Three distinct climatologies were identified, and were referred as fire weather types (FWTs).; Nous avons analysé les conditions météorologiques synoptiques associées aux grands incendies de forêt dans le sud-est de la France (1973-2013) et distingué trois grands types de conditions : les conditions dominées par de fortes températures (HD), celles dominées par des vents forts (WD), et celles proches de la normale météorologique (NN). Les conditions de type WD et NN diminuent fortement depuis plusieurs décennies alors que les conditions HD augmentent, pouvant indiquer ainsi l'occurrence future de plus grands incendies en conditions thermiques très chaudes et très intenses.
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- 2016
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18. How a new fire-suppression policy can abruptly reshape the fire-weather relationship
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Ruffault, J. and Mouillot, Florent
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global changes ,Mediterranean ecosystems ,fire regime changes ,large fires ,fire-suppression policy ,abrupt changes ,fire weather - Abstract
Understanding how the interactions between anthropogenic and biophysical factors control fire regimes is increasingly becoming a major concern in a context of climate, economic and social changes. On a short time scale, fire activity is mainly driven by the variations in weather conditions. But while the assessment of this fire-weather relationship is an essential step towards fire hazard estimations, reconstructions or projections, still little is known about the impact of human practices on this relationship. In this study, we examined the recent fire history in southern France where a new fire policy, introduced during the 1980s, suddenly brought new fire suppression and prevention practices. We aimed at assessing the impact of these changes on fire activity and on the relationships between fire and weather, usually assumed to be constant over time. To do so, we used a statistical framework based on spatially explicit daily fire occurrence data, the corresponding weather variables and the associated fuel moisture derived from a process-based model. Our results showed that the introduction of the new fire policy resulted in a sharp decrease in fire activity but also impacted the daily fire-weather relationship in two main ways. On the one hand, fewer wildfires ignited for similar weather conditions. On the other hand, the probability of a fire to spread over significant surfaces shifted from a fuel-dryness driven system to a system driven by the concomitance of fuel dryness and strong winds. These observations suggest that mid-term (decadal) social factors can affect the short-term (seasonal to daily) relationship between weather conditions and fire activity. Thus, the interactions between human and climate factors should be taken into account when reconstructing or projecting fire activity and including the impact of fire policies on the fire-weather relationships in fire models would be an important step towards more realistic fire regimes simulations.
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- 2015
19. Daily synoptic conditions associated with large fire occurrence in Mediterranean France: evidence for a wind-driven fire regime
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Ruffault, J., primary, Moron, V., additional, Trigo, R. M., additional, and Curt, T., additional
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- 2016
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20. Differential regional responses in drought lenght, intensity and timing to recent climate changes in a Mediterranean forested ecosystem
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Ruffault, J., Martin-StPaul, N.K., Rambal, S., and Mouillot, Florent
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FORET ,SECHERESSE ,POTENTIEL HYDRIQUE ,DEFICIT HYDRIQUE ,CLIMAT ,PRECIPITATION ,CHANGEMENT CLIMATIQUE ,HUMIDITE DU SOL ,BILAN HYDRIQUE ,VARIATION SPATIALE ,FONCTIONNEMENT DE L'ECOSYSTEME ,VEGETATION ,TEMPERATURE - Abstract
The Mediterranean area is one of the regions of the world where GCMs agree the most on precipitation changes due to climate change. In this study we aim to assess the impact of recent climate change on drought features of Mediterranean ecosystems in Southern France. Regional climatic trends for the 1971-2006 period are compared to drought trends based on a water balance model accounting for soil properties, vegetation structure and functioning. Drought, defined here as periods when soil water potentials drop below -0.5 MPa, is described in terms of intensity, duration and timing, which are integrative of both climate variability and site conditions. Temporal trends in precipitation, temperature and solar radiation lead altogether to drier and warmer conditions over the region but with a high spatial heterogeneity; for similar climatic trends, a significant increase in drought intensity was detected in the wettest areas of the region, whereas drought intensity in the driest areas did not change. Indeed, in the wettest areas, we observed an earlier onset of drought by about 1 month, but a constant end of drought. In the driest areas of the region, we observed the same earlier onset of drought but combined with an earlier end of drought, thus leading to a shift of the dry season without increasing its duration. The definition of drought features both in terms of intensity but also of seasonal timing appears relevant to capture historical or forecasted changes in ecosystem functioning. Studies concerning climate change impacts on forested ecosystems should be interpreted with caution when using climate proxies alone.
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- 2013
21. How a new fire-suppression policy can abruptly reshape the fire-weather relationship
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Ruffault, J., primary and Mouillot, F., additional
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- 2015
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22. Hydraulic plasticity and water use regulation act to maintain the hydraulic safety margins of Mediterranean trees in rainfall exclusion experiments.
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Moreno M, Limousin JM, Simioni G, Badel E, Rodríguez-Calcerrada J, Cochard H, Torres-Ruiz JM, Dupuy JL, Ruffault J, Ormeno E, Delzon S, Fernandez C, Ourcival JM, and Martin-StPaul N
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- Droughts, Mediterranean Region, Plant Transpiration physiology, Plant Leaves physiology, Quercus physiology, Water physiology, Water metabolism, Trees physiology, Pinus physiology, Rain, Xylem physiology
- Abstract
Hydraulic failure due to xylem embolism has been identified as one of the main mechanisms involved in drought-induced forest decline. Trees vulnerability to hydraulic failure depends on their hydraulic safety margin (HSM). While it has been shown that HSM globally converges between tree species and biomes, there is still limited knowledge regarding how HSM can adjust locally to varying drought conditions within species. In this study, we relied on three long-term partial rainfall exclusion experiments to investigate the plasticity of hydraulic traits and HSM for three Mediterranean tree species (Quercus ilex L., Quercus pubescens Willd., and Pinus halepensis Mill.). For all species, a homeostasis of HSM in response to rainfall reduction was found, achieved through different mechanisms. For Q. ilex, the convergence in HSM is attributed to the adjustment of both the turgor loss point (Ψtlp) and the water potential at which 50% of xylem conductivity is lost due to embolism (P50). In contrast, the maintenance of HSM for P. halepensis and Q. pubescens is related to its isohydric behavior for the first and leaf area adjustment for the latter. It remains to be seen whether this HSM homeostasis can be generalized and if it will be sufficient to withstand extreme droughts expected in the Mediterranean region., (© 2024 John Wiley & Sons Ltd.)
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- 2024
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23. Tree drought-mortality risk depends more on intrinsic species resistance than on stand species diversity.
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Decarsin R, Guillemot J, le Maire G, Blondeel H, Meredieu C, Achard E, Bonal D, Cochard H, Corso D, Delzon S, Doucet Z, Druel A, Grossiord C, Torres-Ruiz JM, Bauhus J, Godbold DL, Hajek P, Jactel H, Jensen J, Mereu S, Ponette Q, Rewald B, Ruffault J, Sandén H, Scherer-Lorenzen M, Serrano-León H, Simioni G, Verheyen K, Werner R, and Martin-StPaul N
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- Europe, Climate Change, Xylem physiology, Droughts, Biodiversity, Trees physiology, Forests
- Abstract
Increasing tree diversity is considered a key management option to adapt forests to climate change. However, the effect of species diversity on a forest's ability to cope with extreme drought remains elusive. In this study, we assessed drought tolerance (xylem vulnerability to cavitation) and water stress (water potential), and combined them into a metric of drought-mortality risk (hydraulic safety margin) during extreme 2021 or 2022 summer droughts in five European tree diversity experiments encompassing different biomes. Overall, we found that drought-mortality risk was primarily driven by species identity (56.7% of the total variability), while tree diversity had a much lower effect (8% of the total variability). This result remained valid at the local scale (i.e within experiment) and across the studied European biomes. Tree diversity effect on drought-mortality risk was mediated by changes in water stress intensity, not by changes in xylem vulnerability to cavitation. Significant diversity effects were observed in all experiments, but those effects often varied from positive to negative across mixtures for a given species. Indeed, we found that the composition of the mixtures (i.e., the identities of the species mixed), but not the species richness of the mixture per se, is a driver of tree drought-mortality risk. This calls for a better understanding of the underlying mechanisms before tree diversity can be considered an operational adaption tool to extreme drought. Forest diversification should be considered jointly with management strategies focussed on favouring drought-tolerant species., (© 2024 John Wiley & Sons Ltd.)
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- 2024
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24. Isohydricity and hydraulic isolation explain reduced hydraulic failure risk in an experimental tree species mixture.
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Moreno M, Simioni G, Cochard H, Doussan C, Guillemot J, Decarsin R, Fernandez-Conradi P, Dupuy JL, Trueba S, Pimont F, Ruffault J, Jean F, Marloie O, and Martin-StPaul NK
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- Plant Roots physiology, Plant Leaves physiology, Plant Transpiration physiology, Models, Biological, Species Specificity, Dehydration, Quercus physiology, Pinus physiology, Water metabolism, Trees physiology, Droughts, Plant Stomata physiology, Soil chemistry
- Abstract
Species mixture is promoted as a crucial management option to adapt forests to climate change. However, there is little consensus on how tree diversity affects tree water stress, and the underlying mechanisms remain elusive. By using a greenhouse experiment and a soil-plant-atmosphere hydraulic model, we explored whether and why mixing the isohydric Aleppo pine (Pinus halepensis, drought avoidant) and the anisohydric holm oak (Quercus ilex, drought tolerant) affects tree water stress during extreme drought. Our experiment showed that the intimate mixture strongly alleviated Q. ilex water stress while it marginally impacted P. halepensis water stress. Three mechanistic explanations for this pattern are supported by our modeling analysis. First, the difference in stomatal regulation between species allowed Q. ilex trees to benefit from additional soil water in mixture, thereby maintaining higher water potentials and sustaining gas exchange. By contrast, P. halepensis exhibited earlier water stress and stomatal regulation. Second, P. halepensis trees showed stable water potential during drought, although soil water potential strongly decreased, even when grown in a mixture. Model simulations suggested that hydraulic isolation of the root from the soil associated with decreased leaf cuticular conductance was a plausible explanation for this pattern. Third, the higher predawn water potentials for a given soil water potential observed for Q. ilex in mixture can-according to model simulations-be explained by increased soil-to-root conductance, resulting from higher fine root length. This study brings insights into the mechanisms involved in improved drought resistance of mixed species forests., Competing Interests: Conflict of interest statement. None declared., (© The Author(s) 2024. Published by Oxford University Press on behalf of American Society of Plant Biologists.)
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- 2024
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25. Plant hydraulics at the heart of plant, crops and ecosystem functions in the face of climate change.
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Torres-Ruiz JM, Cochard H, Delzon S, Boivin T, Burlett R, Cailleret M, Corso D, Delmas CEL, De Caceres M, Diaz-Espejo A, Fernández-Conradi P, Guillemot J, Lamarque LJ, Limousin JM, Mantova M, Mencuccini M, Morin X, Pimont F, De Dios VR, Ruffault J, Trueba S, and Martin-StPaul NK
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- Water physiology, Soil, Crops, Agricultural, Droughts, Ecosystem, Climate Change
- Abstract
Plant hydraulics is crucial for assessing the plants' capacity to extract and transport water from the soil up to their aerial organs. Along with their capacity to exchange water between plant compartments and regulate evaporation, hydraulic properties determine plant water relations, water status and susceptibility to pathogen attacks. Consequently, any variation in the hydraulic characteristics of plants is likely to significantly impact various mechanisms and processes related to plant growth, survival and production, as well as the risk of biotic attacks and forest fire behaviour. However, the integration of hydraulic traits into disciplines such as plant pathology, entomology, fire ecology or agriculture can be significantly improved. This review examines how plant hydraulics can provide new insights into our understanding of these processes, including modelling processes of vegetation dynamics, illuminating numerous perspectives for assessing the consequences of climate change on forest and agronomic systems, and addressing unanswered questions across multiple areas of knowledge., (© 2023 The Authors. New Phytologist © 2023 New Phytologist Foundation.)
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- 2024
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26. Drivers and implications of the extreme 2022 wildfire season in Southwest Europe.
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Rodrigues M, Cunill Camprubí À, Balaguer-Romano R, Coco Megía CJ, Castañares F, Ruffault J, Fernandes PM, and Resco de Dios V
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- Climate Change, Forests, Seasons, Europe, Fires, Wildfires
- Abstract
Wildfire is a common phenomenon in Mediterranean countries but the 2022 fire season has been extreme in southwest Europe (Portugal, Spain and France). Here we provide a preliminary but comprehensive analysis of 2022's wildfire season in southwest Europe. Burned area has exceeded the 2001-2021 median by a factor of 52 in some regions and large wildfires (>500 ha) started to occur in June-July, earlier than the traditional fire season. These anomalies were associated with record-breaking values of fuel dryness, atmospheric water demand and pyrometeorological conditions. Live fuel moisture content was below the historical minima for almost 50 % of the season in some regions. A few large wildfires were responsible for 82 % of the burned area and, in turn, 47 % of the area burned occurred in protected areas. Shrublands, transitional woodlands and conifer forests (but not eucalypt plantations) were the land cover types most affected by extreme fires. As climate change intensifies, we can expect such fire seasons to become the new normal in large parts of the continent, potentially leading to major negative impacts on rural economies. These results highlight the need for landscape level fuel management also in protected areas, to avoid fire-induced biodiversity losses and landscape scale degradation. Our results have important policy implications and indicate that fire prevention should be explicitly addressed within continental forest legislation and strategies., Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2022 Elsevier B.V. All rights reserved.)
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- 2023
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27. Plant hydraulic modelling of leaf and canopy fuel moisture content reveals increasing vulnerability of a Mediterranean forest to wildfires under extreme drought.
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Ruffault J, Limousin JM, Pimont F, Dupuy JL, De Càceres M, Cochard H, Mouillot F, Blackman CJ, Torres-Ruiz JM, Parsons RA, Moreno M, Delzon S, Jansen S, Olioso A, Choat B, and Martin-StPaul N
- Subjects
- Forests, Trees physiology, Plant Leaves physiology, Water physiology, Droughts, Wildfires
- Abstract
Fuel moisture content (FMC) is a crucial driver of forest fires in many regions world-wide. Yet, the dynamics of FMC in forest canopies as well as their physiological and environmental determinants remain poorly understood, especially under extreme drought. We embedded a FMC module in the trait-based, plant-hydraulic SurEau-Ecos model to provide innovative process-based predictions of leaf live fuel moisture content (LFMC) and canopy fuel moisture content (CFMC) based on leaf water potential ( ψ Leaf ). SurEau-Ecos-FMC relies on pressure-volume (p-v) curves to simulate LFMC and vulnerability curves to cavitation to simulate foliage mortality. SurEau-Ecos-FMC accurately reproduced ψ Leaf and LFMC dynamics as well as the occurrence of foliage mortality in a Mediterranean Quercus ilex forest. Several traits related to water use (leaf area index, available soil water, and transpiration regulation), vulnerability to cavitation, and p-v curves (full turgor osmotic potential) had the greatest influence on LFMC and CFMC dynamics. As the climate gets drier, our results showed that drought-induced foliage mortality is expected to increase, thereby significantly decreasing CFMC. Our results represent an important advance in our capacity to understand and predict the sensitivity of forests to wildfires., (© 2022 The Authors. New Phytologist © 2022 New Phytologist Foundation. This article has been contributed to by US Government employees and their work is in the public domain in the USA.)
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- 2023
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28. Prediction of regional wildfire activity in the probabilistic Bayesian framework of Firelihood.
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Pimont F, Fargeon H, Opitz T, Ruffault J, Barbero R, Martin-StPaul N, Rigolot E, RiviÉre M, and Dupuy JL
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- Bayes Theorem, Ecosystem, Forests, Fires, Wildfires
- Abstract
Modeling wildfire activity is crucial for informing science-based risk management and understanding the spatiotemporal dynamics of fire-prone ecosystems worldwide. Models help disentangle the relative influences of different factors, understand wildfire predictability, and provide insights into specific events. Here, we develop Firelihood, a two-component, Bayesian, hierarchically structured, probabilistic model of daily fire activity, which is modeled as the outcome of a marked point process: individual fires are the points (occurrence component), and fire sizes are the marks (size component). The space-time Poisson model for occurrence is adjusted to gridded fire counts using the integrated nested Laplace approximation (INLA) combined with the stochastic partial differential equation (SPDE) approach. The size model is based on piecewise-estimated Pareto and generalized Pareto distributions, adjusted with INLA. The Fire Weather Index (FWI) and forest area are the main explanatory variables. Temporal and spatial residuals are included to improve the consistency of the relationship between weather and fire occurrence. The posterior distribution of the Bayesian model provided 1,000 replications of fire activity that were compared with observations at various temporal and spatial scales in Mediterranean France. The number of fires larger than 1 ha across the region was coarsely reproduced at the daily scale, and was more accurately predicted on a weekly basis or longer. The regional weekly total number of larger fires (10-100 ha) was predicted as well, but the accuracy degraded with size, as the model uncertainty increased with event rareness. Local predictions of fire numbers or burned areas also required a longer aggregation period to maintain model accuracy. The estimation of fires larger than 1 ha was also consistent with observations during the extreme fire season of the 2003 unprecedented heat wave, but the model systematically underrepresented large fires and burned areas, which suggests that the FWI does not consistently rate the actual danger of large fire occurrence during heat waves. Firelihood enabled a novel analysis of the stochasticity underlying fire hazard, and offers a variety of applications, including fire hazard predictions for management and projections in the context of climate change., (© 2021 by the Ecological Society of America.)
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- 2021
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29. Increased likelihood of heat-induced large wildfires in the Mediterranean Basin.
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Ruffault J, Curt T, Moron V, Trigo RM, Mouillot F, Koutsias N, Pimont F, Martin-StPaul N, Barbero R, Dupuy JL, Russo A, and Belhadj-Khedher C
- Abstract
Wildfire activity is expected to increase across the Mediterranean Basin because of climate change. However, the effects of future climate change on the combinations of atmospheric conditions that promote wildfire activity remain largely unknown. Using a fire-weather based classification of wildfires, we show that future climate scenarios point to an increase in the frequency of two heat-induced fire-weather types that have been related to the largest wildfires in recent years. Heat-induced fire-weather types are characterized by compound dry and warm conditions occurring during summer heatwaves, either under moderate (heatwave type) or intense (hot drought type) drought. The frequency of heat-induced fire-weather is projected to increase by 14% by the end of the century (2071-2100) under the RCP4.5 scenario, and by 30% under the RCP8.5, suggesting that the frequency and extent of large wildfires will increase throughout the Mediterranean Basin.
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- 2020
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30. Recent climate hiatus revealed dual control by temperature and drought on the stem growth of Mediterranean Quercus ilex.
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Lempereur M, Limousin JM, Guibal F, Ourcival JM, Rambal S, Ruffault J, and Mouillot F
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- Climate, Climate Change, Plant Stems, Seasons, Water, Droughts, Quercus growth & development, Temperature
- Abstract
A better understanding of stem growth phenology and its climate drivers would improve projections of the impact of climate change on forest productivity. Under a Mediterranean climate, tree growth is primarily limited by soil water availability during summer, but cold temperatures in winter also prevent tree growth in evergreen forests. In the widespread Mediterranean evergreen tree species Quercus ilex, the duration of stem growth has been shown to predict annual stem increment, and to be limited by winter temperatures on the one hand, and by the summer drought onset on the other hand. We tested how these climatic controls of Q. ilex growth varied with recent climate change by correlating a 40-year tree ring record and a 30-year annual diameter inventory against winter temperature, spring precipitation, and simulated growth duration. Our results showed that growth duration was the best predictor of annual tree growth. We predicted that recent climate changes have resulted in earlier growth onset (-10 days) due to winter warming and earlier growth cessation (-26 days) due to earlier drought onset. These climatic trends partly offset one another, as we observed no significant trend of change in tree growth between 1968 and 2008. A moving-window correlation analysis revealed that in the past, Q. ilex growth was only correlated with water availability, but that since the 2000s, growth suddenly became correlated with winter temperature in addition to spring drought. This change in the climate-growth correlations matches the start of the recent atmospheric warming pause also known as the 'climate hiatus'. The duration of growth of Q. ilex is thus shortened because winter warming has stopped compensating for increasing drought in the last decade. Decoupled trends in precipitation and temperature, a neglected aspect of climate change, might reduce forest productivity through phenological constraints and have more consequences than climate warming alone., (© 2016 John Wiley & Sons Ltd.)
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- 2017
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31. Photosynthetic sensitivity to drought varies among populations of Quercus ilex along a rainfall gradient.
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Martin-StPaul NK, Limousin JM, Rodr Guez-Calcerrada JS, Ruffault J, Rambal S, Letts MG, and Misson L
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Drought frequency and intensity are expected to increase in the Mediterranean as a consequence of global climate change. To understand how photosynthetic capacity responds to long-term water stress, we measured seasonal patterns of stomatal (SL), mesophyll (MCL) and biochemical limitations (BL) to net photosynthesis (Amax) in three Quercus ilex (L.) populations from sites differing in annual rainfall. In the absence of water stress, stomatal conductance (gs), maximum carboxylation capacity (Vcmax), photosynthetic electron transport rate (Jmax) and Amax were similar among populations. However, as leaf predawn water potential (Ψl,pd) declined, the population from the wettest site showed steeper declines in gs, Vcmax, Jmax and Amax than those from the drier sites. Consequently, SL, MCL and BL increased most steeply in response to decreasing Ψl,pd in the population from the wettest site. The higher sensitivity of Amax to drought was primarily the result of stronger stomatal regulation of water loss. Among-population differences were not observed when gs was used instead of Ψl,pd as a drought stress indicator. Given that higher growth rates, stature and leaf area index were observed at the wettest site, we speculate that hydraulic architecture may explain the greater drought sensitivity of this population. Collectively, these results highlight the importance of considering among-population differences in photosynthetic responses to seasonal drought in large scale process-based models of forest ecosystem function.
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- 2012
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