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1902 - 2008年美国北落基山脉火灾与气候关系的强度和性质变化

The Changing Strength and Nature of Fire-Climate Relationships in the Northern Rocky Mountains, U.S.A., 1902-2008.

作者信息

Higuera Philip E, Abatzoglou John T, Littell Jeremy S, Morgan Penelope

机构信息

College of Natural Resources, University of Idaho, Moscow, Idaho, United States of America.

Department of Geography, University of Idaho, Moscow, Idaho, United States of America.

出版信息

PLoS One. 2015 Jun 26;10(6):e0127563. doi: 10.1371/journal.pone.0127563. eCollection 2015.

Abstract

Time-varying fire-climate relationships may represent an important component of fire-regime variability, relevant for understanding the controls of fire and projecting fire activity under global-change scenarios. We used time-varying statistical models to evaluate if and how fire-climate relationships varied from 1902-2008, in one of the most flammable forested regions of the western U.S.A. Fire-danger and water-balance metrics yielded the best combination of calibration accuracy and predictive skill in modeling annual area burned. The strength of fire-climate relationships varied markedly at multi-decadal scales, with models explaining < 40% to 88% of the variation in annual area burned. The early 20th century (1902-1942) and the most recent two decades (1985-2008) exhibited strong fire-climate relationships, with weaker relationships for much of the mid 20th century (1943-1984), coincident with diminished burning, less fire-conducive climate, and the initiation of modern fire fighting. Area burned and the strength of fire-climate relationships increased sharply in the mid 1980s, associated with increased temperatures and longer potential fire seasons. Unlike decades with high burning in the early 20th century, models developed using fire-climate relationships from recent decades overpredicted area burned when applied to earlier periods. This amplified response of fire to climate is a signature of altered fire-climate-relationships, and it implicates non-climatic factors in this recent shift. Changes in fuel structure and availability following 40+ yr of unusually low fire activity, and possibly land use, may have resulted in increased fire vulnerability beyond expectations from climatic factors alone. Our results highlight the potential for non-climatic factors to alter fire-climate relationships, and the need to account for such dynamics, through adaptable statistical or processes-based models, for accurately predicting future fire activity.

摘要

时变的火灾-气候关系可能是火灾 regime 变异性的一个重要组成部分,对于理解火灾的控制因素以及预测全球变化情景下的火灾活动具有重要意义。我们使用时变统计模型来评估在美国西部最易燃的森林地区之一,1902 年至 2008 年期间火灾-气候关系是否以及如何发生变化。火灾危险和水平衡指标在模拟年烧毁面积时,在校准精度和预测技能方面产生了最佳组合。火灾-气候关系的强度在数十年尺度上有显著变化,模型解释了年烧毁面积变化的 40%至 88%。20 世纪早期(1902 年至 1942 年)和最近二十年(1985 年至 2008 年)呈现出较强的火灾-气候关系,而 20 世纪中叶的大部分时间(1943 年至 1984 年)关系较弱,这与燃烧减少、不利于火灾的气候以及现代灭火行动的开始相吻合。20 世纪 80 年代中期,烧毁面积和火灾-气候关系的强度急剧增加,这与气温升高和潜在火灾季节延长有关。与 20 世纪早期高燃烧的几十年不同,使用近几十年火灾-气候关系开发的模型应用于早期时,高估了烧毁面积。火灾对气候的这种放大响应是火灾-气候关系改变的一个特征,这意味着非气候因素在最近的这种转变中起到了作用。在 40 多年异常低火灾活动之后,燃料结构和可利用性的变化,以及可能的土地利用变化,可能导致火灾脆弱性增加,超出了仅由气候因素预期的范围。我们的结果强调了非气候因素改变火灾-气候关系的可能性,以及通过适应性统计模型或基于过程的模型来考虑这种动态变化以准确预测未来火灾活动的必要性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/729a/4482589/fc69620257b4/pone.0127563.g001.jpg

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