The Changing Strength and Nature of Fire-Climate Relationships in the Northern Rocky Mountains, USA, 1902-2008

被引:91
作者
Higuera, Philip E. [1 ]
Abatzoglou, John T. [2 ]
Littell, Jeremy S. [3 ]
Morgan, Penelope [1 ]
机构
[1] Univ Idaho, Coll Nat Resources, Moscow, ID 83843 USA
[2] Univ Idaho, Dept Geog, Moscow, ID 83843 USA
[3] USGS, Alaska Climate Sci Ctr, Anchorage, AK USA
来源
PLOS ONE | 2015年 / 10卷 / 06期
基金
美国国家科学基金会;
关键词
VEGETATION DISTRIBUTION; BURNED AREA; WESTERN US; FOREST; WILDFIRE; REGIME; PYROGEOGRAPHY; 20TH-CENTURY; VARIABILITY; REGRESSION;
D O I
10.1371/journal.pone.0127563
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
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.
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页数:21
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