Department of Earth and Ocean Sciences, University of North Carolina Wilmington, Wilmington, NC, USA.
US Geological Survey, Southeast Climate Adaptation Science Center, Raleigh, NC, USA; Department of Applied Ecology, North Carolina State University, Raleigh, NC, USA.
Sci Total Environ. 2021 Oct 1;789:147872. doi: 10.1016/j.scitotenv.2021.147872. Epub 2021 May 21.
Globally increasing wildfires have been attributed to anthropogenic climate change. However, providing decision makers with a clear understanding of how future planetary warming could affect fire regimes is complicated by confounding land use factors that influence wildfire and by uncertainty associated with model simulations of climate change. We use an ensemble of statistically downscaled Global Climate Models in combination with the Physical Chemistry Fire Frequency Model (PC2FM) to project changing potential fire probabilities in the conterminous United States for two scenarios representing lower (RCP 4.5) and higher (RCP 8.5) greenhouse gas emission futures. PC2FM is a physically-based and scale-independent model that predicts mean fire return intervals from both fire reactant and reaction variables, which are largely dependent on a locale's climate. Our results overwhelmingly depict increasing potential fire probabilities across the conterminous US for both climate scenarios. The primary mechanism for the projected increases is rising temperatures, reflecting changes in the chemical reaction environment commensurate with enhanced photosynthetic rates and available thermal molecular energy. Existing high risk areas, such as the Cascade Range and the Coastal California Mountains, are projected to experience greater annual fire occurrence probabilities, with relative increases of 122% and 67%, respectively, under RCP 8.5 compared to increases of 63% and 38% under RCP 4.5. Regions not currently associated with frequently occurring wildfires, such as New England and the Great Lakes, are projected to experience a doubling of occurrence probabilities by 2100 under RCP 8.5. This high resolution, continental-scale modeling study of climate change impacts on potential fire probability accounts for shifting background environmental conditions across regions that will interact with topographic drivers to significantly alter future fire probabilities. The ensemble modeling approach presents a useful planning tool for mitigation and adaptation strategies in regions of increasing wildfire risk.
全球范围内,野火的增加归因于人为气候变化。然而,由于影响野火的土地利用因素以及与气候变化模型模拟相关的不确定性,向决策者清晰地展示未来行星变暖将如何影响火灾发生的频率变得十分复杂。我们使用一套统计学上的降尺度全球气候模型与物理化学火灾频率模型(PC2FM)结合,来预测在两个温室气体排放未来情景(较低情景 RCP4.5 和较高情景 RCP8.5)下,美国本土潜在火灾概率的变化。PC2FM 是一种基于物理和独立于尺度的模型,它可以预测火灾反应物和反应变量的平均火灾回归间隔,而这些变量主要取决于当地的气候。我们的结果压倒性地表明,在美国本土范围内,两个气候情景的潜在火灾概率都在增加。预测火灾概率增加的主要机制是温度升高,这反映了化学反应环境的变化,与增强的光合速率和可用的热分子能量相一致。现有的高风险地区,如喀斯喀特山脉和加利福尼亚沿海山脉,预计将经历更高的年火灾发生概率,在 RCP8.5 情景下,相对增加分别为 122%和 67%,而在 RCP4.5 情景下,相对增加分别为 63%和 38%。目前与频繁发生的野火无关的地区,如新英格兰和五大湖地区,预计在 RCP8.5 情景下,火灾发生概率将在 2100 年前翻一番。本研究采用高分辨率、大陆尺度的气候模型,评估了气候变化对潜在火灾概率的影响,该模型考虑了跨区域背景环境条件的变化,这些变化将与地形驱动因素相互作用,显著改变未来的火灾概率。该集合建模方法为增加野火风险地区的缓解和适应策略提供了有用的规划工具。