Zhongwei Liu , Jonathan M. Eden , Bastien Dieppois , Igor Drobyshev , Folmer Krikken , Matthew Blackett
{"title":"极端火灾天气历史变化的全球评估:来自CMIP6集合的见解及其对全球变暖概率归因的影响","authors":"Zhongwei Liu , Jonathan M. Eden , Bastien Dieppois , Igor Drobyshev , Folmer Krikken , Matthew Blackett","doi":"10.1016/j.gloplacha.2025.104822","DOIUrl":null,"url":null,"abstract":"<div><div>In response to the occurrence of several large wildfire events across the world in recent years, the question of the extent to which climate change may be altering the meteorological conditions conducive to wildfires has become a hot topic of debate. Despite the development of detection and attribution methodologies for climate change impact assessment in the last decade, studies dedicated explicitly to wildfire, or otherwise extreme ‘fire weather’, are still relatively few. Here, for the first time, a global probabilistic framework is developed to examine the extent to which externally forced changes in historical global mean surface temperature anomalies (GMSTA) affected the intensity and duration of fire-conducive weather extremes, defined by the Fire Weather Index (FWI). We use six climate model large ensembles (>10 ensemble members) from the sixth phase of the Coupled Model Intercomparison Project (CMIP6), to extract the forced response of GMSTA. After evaluating the performances of these climate models in simulating fire weather extremes, we examine changes in the probability of fire weather extremes using extreme value distributions, fitted with annual maxima in both FWI intensity and duration, and scaled to externally forced GMSTA. Global probability ratio maps are used to quantify the influence of rising global temperatures on the changing frequency and duration of FWI extremes, and highlight the sensitivity of estimates of historical changes in extreme fire weather to the climate model ensemble chosen for the analysis. A multi-model synthesis accounting for performance of each model confirms an increasing trend in the probability and duration of extreme fire weather linked to externally forced changes in GMSTA, with the largest increases found in southern North America, south-eastern Europe and parts of Australia. The results of the selective synthesis differ from those obtained via a conventional multi-model averaging that does not account for model performance, thereby demonstrating the value added by model evaluation and selection in maximising the robustness of probabilistic attribution studies.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"252 ","pages":"Article 104822"},"PeriodicalIF":4.0000,"publicationDate":"2025-04-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Global assessment of historical changes in extreme fire weather: Insight from CMIP6 ensembles and implications for probabilistic attribution to global warming\",\"authors\":\"Zhongwei Liu , Jonathan M. Eden , Bastien Dieppois , Igor Drobyshev , Folmer Krikken , Matthew Blackett\",\"doi\":\"10.1016/j.gloplacha.2025.104822\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>In response to the occurrence of several large wildfire events across the world in recent years, the question of the extent to which climate change may be altering the meteorological conditions conducive to wildfires has become a hot topic of debate. Despite the development of detection and attribution methodologies for climate change impact assessment in the last decade, studies dedicated explicitly to wildfire, or otherwise extreme ‘fire weather’, are still relatively few. Here, for the first time, a global probabilistic framework is developed to examine the extent to which externally forced changes in historical global mean surface temperature anomalies (GMSTA) affected the intensity and duration of fire-conducive weather extremes, defined by the Fire Weather Index (FWI). We use six climate model large ensembles (>10 ensemble members) from the sixth phase of the Coupled Model Intercomparison Project (CMIP6), to extract the forced response of GMSTA. After evaluating the performances of these climate models in simulating fire weather extremes, we examine changes in the probability of fire weather extremes using extreme value distributions, fitted with annual maxima in both FWI intensity and duration, and scaled to externally forced GMSTA. Global probability ratio maps are used to quantify the influence of rising global temperatures on the changing frequency and duration of FWI extremes, and highlight the sensitivity of estimates of historical changes in extreme fire weather to the climate model ensemble chosen for the analysis. A multi-model synthesis accounting for performance of each model confirms an increasing trend in the probability and duration of extreme fire weather linked to externally forced changes in GMSTA, with the largest increases found in southern North America, south-eastern Europe and parts of Australia. The results of the selective synthesis differ from those obtained via a conventional multi-model averaging that does not account for model performance, thereby demonstrating the value added by model evaluation and selection in maximising the robustness of probabilistic attribution studies.</div></div>\",\"PeriodicalId\":55089,\"journal\":{\"name\":\"Global and Planetary Change\",\"volume\":\"252 \",\"pages\":\"Article 104822\"},\"PeriodicalIF\":4.0000,\"publicationDate\":\"2025-04-09\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Global and Planetary Change\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0921818125001316\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Global and Planetary Change","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0921818125001316","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
Global assessment of historical changes in extreme fire weather: Insight from CMIP6 ensembles and implications for probabilistic attribution to global warming
In response to the occurrence of several large wildfire events across the world in recent years, the question of the extent to which climate change may be altering the meteorological conditions conducive to wildfires has become a hot topic of debate. Despite the development of detection and attribution methodologies for climate change impact assessment in the last decade, studies dedicated explicitly to wildfire, or otherwise extreme ‘fire weather’, are still relatively few. Here, for the first time, a global probabilistic framework is developed to examine the extent to which externally forced changes in historical global mean surface temperature anomalies (GMSTA) affected the intensity and duration of fire-conducive weather extremes, defined by the Fire Weather Index (FWI). We use six climate model large ensembles (>10 ensemble members) from the sixth phase of the Coupled Model Intercomparison Project (CMIP6), to extract the forced response of GMSTA. After evaluating the performances of these climate models in simulating fire weather extremes, we examine changes in the probability of fire weather extremes using extreme value distributions, fitted with annual maxima in both FWI intensity and duration, and scaled to externally forced GMSTA. Global probability ratio maps are used to quantify the influence of rising global temperatures on the changing frequency and duration of FWI extremes, and highlight the sensitivity of estimates of historical changes in extreme fire weather to the climate model ensemble chosen for the analysis. A multi-model synthesis accounting for performance of each model confirms an increasing trend in the probability and duration of extreme fire weather linked to externally forced changes in GMSTA, with the largest increases found in southern North America, south-eastern Europe and parts of Australia. The results of the selective synthesis differ from those obtained via a conventional multi-model averaging that does not account for model performance, thereby demonstrating the value added by model evaluation and selection in maximising the robustness of probabilistic attribution studies.
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged.
Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.