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Carbon dynamics of forests in Washington, USA: 21st century projections based on climate-driven changes in fire regimes

机译:美国华盛顿森林的碳动态:基于气候变化的火势变化对21世纪的预测

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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.
机译:在21世纪,气候变化引起的火灾将是美国西北太平洋地区(PNW)森林变化的主要推动力。了解森林碳(C)动态对火灾增加的响应将有助于量化对森林碳储存对缓解气候变化的贡献的限制,并优先考虑森林类型以监测碳储存和火灾管理,以最大程度地减少碳损失。在这项研究中,我们使用了21世纪被烧面积的预测来探索火灾状况的变化对华盛顿州森林中碳动态的影响。我们使用了一种新颖的经验方法,利用C池和通量的时间序列以及火灾状况的统计特性,探索了年龄分布的变化对C动态的影响。与东部喀斯特山脉的森林相比,西部喀斯特山脉的森林预计对气候驱动的火灾增加更为敏感,因此对C动态的变化也更敏感。在喀斯喀特西部,到2040年代,平均活生物量C预计减少24-37%,粗木屑(CWD)生物量C减少15-25%。东部喀斯喀特山脉和Okanogan高地的森林中活生物量C的损失预计较低(17-26%),而CWD生物量预计将增加。在喀斯喀特西部的低海拔湿润森林中,景观平均净初级生产力预计将增加,但在其他地方则下降。这些森林和冈野高原的湿润森林预计在活生物量消耗中的增加百分比最大。在所有地区,CWD生物量消耗的增加百分比均大于50%,是活生物量消耗增加的四倍之多。 PNW森林中的碳固存对火势的增加非常敏感,这表明要谨慎管理这些森林的C固存以减轻人为的CO2排放。

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