School of Forest Resources, University of Washington, Box 352100, Seattle, Washington 98195-2100, USA.
Ecol Appl. 2012 Jul;22(5):1589-611. doi: 10.1890/11-1851.1.
During the 21st century, climate-driven changes in fire regimes will be a key agent of change in forests of the U.S. Pacific Northwest (PNW). Understanding the response of forest carbon (C) dynamics to increases in fire will help quantify limits on the contribution of forest C storage to climate change mitigation and prioritize forest types for monitoring C storage and fire management to minimize C loss. In this study, we used projections of 21st century area burned to explore the consequences of changes in fire regimes on C dynamics in forests of Washington State. We used a novel empirical approach that takes advantage of chronosequences of C pools and fluxes and statistical properties of fire regimes to explore the effects of shifting age class distributions on C dynamics. Forests of the western Cascades are projected to be more sensitive to climate-driven increases in fire, and thus projected changes in C dynamics, than forests of the eastern Cascades. In the western Cascades, mean live biomass C is projected to decrease by 24-37%, and coarse woody debris (CWD) biomass C by 15-25% for the 2040s. Loss of live biomass C is projected to be lower for forests of the eastern Cascades and Okanogan Highlands (17-26%), and CWD biomass is projected to increase. Landscape mean net primary productivity is projected to increase in wet low-elevation forests of the western Cascades, but decrease elsewhere. These forests, and moist forests of the Okanogan Highlands, are projected to have the greatest percentage increases in consumption of live biomass. Percentage increases in consumption of CWD biomass are greater than 50% for all regions and up to four times greater than increases in consumption of live biomass. Carbon sequestration in PNW forests will be highly sensitive to increases in fire, suggesting a cautious approach to managing these forests for C sequestration to mitigate anthropogenic CO2 emissions.
在 21 世纪,气候驱动的火灾格局变化将成为美国太平洋西北地区(PNW)森林变化的关键因素。了解森林碳(C)动态对火灾增加的响应将有助于量化森林 C 储存对减缓气候变化的贡献限制,并优先考虑森林类型进行 C 储存监测和火灾管理,以最大限度地减少 C 损失。在这项研究中,我们使用 21 世纪火烧面积的预测来探索火灾格局变化对华盛顿州森林 C 动态的影响。我们使用了一种新颖的经验方法,该方法利用 C 池和通量的时间序列以及火灾格局的统计特性来探索年龄类分布变化对 C 动态的影响。西部喀斯喀特山脉的森林预计比东部喀斯喀特山脉的森林对气候驱动的火灾增加更为敏感,因此预计 C 动态变化也更大。在西部喀斯喀特山脉,预计活生物量 C 将减少 24-37%,粗木质残体(CWD)生物质 C 将减少 15-25%,为 2040 年代。东部喀斯喀特山脉和奥卡诺根高地的活生物量 C 损失预计较低(17-26%),而 CWD 生物质预计增加。预计西部喀斯喀特山脉湿润低海拔森林的景观平均净初级生产力将增加,但其他地方则减少。预计这些森林和奥卡诺根高地的湿润森林将有最大的活生物量消耗百分比增加。所有地区的 CWD 生物质消耗百分比增加都超过 50%,而活生物量消耗百分比增加则高达 4 倍。PNW 森林的碳固存对火灾的增加非常敏感,这表明在为减缓人为 CO2 排放而管理这些森林以进行碳固存时应采取谨慎态度。