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

机译:1902-2008年美国北落基山脉的气候变化与气候变化关系的强度和性质。

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摘要

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.
机译:时变的气候与气候的关系可能代表着火势变化的重要组成部分,与理解火势控制和预测全球变化场景下的火势活动有关。在美国西部最易燃的森林地区之一中,我们使用时变统计模型来评估1902-2008年之间的火-气关系是否以及如何变化,火险和水平衡度量标准将标定精度和预测年度面积建模的技巧被烧毁。火灾-气候关系的强度在数十年尺度上显着变化,模型解释了年燃烧面积变化的<40%至88%。 20世纪初(1902-1942)和最近二十年(1985-2008)表现出很强的火气-气候关系,而在20世纪中期(1943-1984)的大部分时间里这种关系较弱,同时燃烧减少,火势减少有利的气候,并开始了现代消防。在1980年代中期,燃烧的土地和与火势的关系强度急剧增加,这与温度升高和潜在的火季延长有关。与20世纪初的数十年高燃烧不同,使用早期几十年来高估面积的火-气候关系开发的模型应用于早期。火对气候的这种放大反应是火-气候关系改变的标志,并且在最近的转变中牵涉到非气候因素。在异常低火活动超过40年后,甚至在土地使用之后,燃料结构和可用性的变化可能导致火灾脆弱性增加,超出了仅出于气候因素的预期。我们的结果凸显了非气候因素改变着火与气候之间关系的潜力,并需要通过适应性统计或基于过程的模型来考虑此类动态,以准确预测未来的着火活动。

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