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Detecting changes in climate forcing on the fire regime of a North American mixed-pine forest: A case study of Seney National Wildlife Refuge, Upper Michigan

机译:检测气候变化迫使北美地区的火灾 松树林:塞尼国家野生动物保护区的案例研究, 上密歇根州

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摘要

The study of forests dominated by red pine (Pinus resinosa Ait.), one of the few fire-resistant tree species of eastern North America, provides an opportunity to reconstruct long-term fire histories and examine the temporal dynamics of climate forcing upon forest fire regimes. We used a 300-year long spatially explicit dendrochronological reconstruction of the fire regime for Seney National Wildlife Refuge (SNWR, 38,531 ha), eastern Upper Michigan to: (1) identify fire size thresholds with strong vs. weak climate controls, (2) evaluate effect of landform type (outwash channel vs. sand ridges) in modifying climate–fire associations, and (3) check for the presence of temporal changes in the climate control of large fire events over the time period 1700–1983. We used a summer drought sensitive red pine chronology (ITRDB code can037) as a proxy of past fire-related climate variability. Results indicated that fires \u3e60 ha in sand-ridge-dominated portions of SNWR and \u3e100 ha in outwash channels were likely climatically driven events. Climate–fire associations varied over time with significant climate–fire linkages observed for the periods 1700–1800 (pre-EuroAmerican), 1800–1900 (EuroAmerican settlement) and 1900–1983 (modern era). Although an increase in fire activity at the turn of 20th century is commonly associated with human sources of ignitions, our results suggest that such an increase was also likely a climatically driven episode.
机译:对北美东部为数不多的耐火树种之一的红松(Pinus resinosa Ait。)占主导地位的森林的研究为重建长期的火灾历史和研究气候对森林火灾造成的时间动态提供了机会。政权。我们对上密歇根州东部的塞尼国家野生动物保护区(SNWR,38,531公顷)使用了长达300年的空间显式树状年代学重建火力制度,以:(1)确定强气候控制与弱气候控制的火势阈值,(2)评估地貌类型(冲刷河道与沙脊)在改变气候-火灾关联中的作用,以及(3)检查1700-1983年期间大火事件的气候控制中是否存在时间变化。我们使用了夏季干旱敏感的赤松年表(ITRDB代码can037)作为过去与火有关的气候变化的代理。结果表明,SNWR沙岭为主的部分发生火灾,而冲刷渠道中发生的火灾可能是气候驱动的事件。气候-火灾协会随时间变化,在1700-1800年(欧洲前),1800-1900年(欧洲人定居)和1900-1983年(现代)期间观察到明显的气候-火灾联系。尽管20世纪之交的火活动增加通常与人的点火源有关,但我们的结果表明,这种增加也很可能是气候驱动的事件。

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