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首页> 外文期刊>Forest Ecology and Management >Late-successional and old-growth forest carbon temporal dynamics in the Northern Forest (Northeastern USA).
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Late-successional and old-growth forest carbon temporal dynamics in the Northern Forest (Northeastern USA).

机译:北部森林(美国东北部)的后继森林和老林森林碳时间动态。

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摘要

Comprehensive data on the capacity and rates of change for carbon pools in managed and unmanaged forests is essential for evaluating climate change mitigation options being considered by policy makers at regional and national levels. We currently lack real and long-term data on forest carbon dynamics covering a wide range of forest management practices and conditions. Because of this, selecting the best policies for conserving forest carbon must rely on forest growth and yield models such as US Forest Service (USFS) Forest Vegetation Simulator (FVS) to predict the future forest carbon impacts of management actions. FVS may underestimate the capacity of older stands to accumulate carbon because the model relies on USFS Forest Inventory and Analysis data that lack data from late-successional and old-growth (LSOG) stands. Improving these models will increase the likelihood of selecting policies that successfully use forests to reduce atmospheric carbon. From 1995 to 2002, Manomet Center for Conservation Sciences conducted research on 65 10 m by 50 m permanent plots to evaluate forest structure (standing live and dead trees, and down coarse woody material) in LSOG stands across northern Maine. We re-measured these plots in 2011 to assess long-term carbon sequestration trends in LSOG stands of common forest types in the Northern Forest region for above ground alive, standing dead, and coarse woody material carbon pools. Late-successional (LS) and Old-growth (OG) aboveground live carbon (C) stocks were very high relative to regional mean C stocks (2.0-2.5 times the mean), LS plots were accumulating aboveground live C at a positive rate (0.61 Mg ha-1 year-1), while C stocks on OG plots are declining (-0.54 Mg ha-1 year-1). This change is driven by the presence of beech bark fungus (Nectria sp.) that is leading to mortality in larger diameter American beech (Fagus grandifolia) trees. We also found that the Northeast Variant of the Forest Vegetation Simulator is not a reliable predictor of aboveground live carbon accumulation rates in Northeastern LS and OG stands. This work provides important baselines for understanding the role of older forests and forest management within climate change mitigation strategies in the northeastern US. Late-successional and old-growth forests can play an important role in mitigating climate change, but understanding and quantifying natural disturbance risk to forest carbon stocks is critical for successful implementation of mitigation strategies. Further, regional forest carbon models will need calibration to accurately predict carbon accumulation rates in older forests.
机译:关于区域和国家决策者正在考虑的减缓气候变化方案的评估,关于有管理和无管理森林中碳库的能力和变化速率的综合数据至关重要。目前,我们缺乏有关森林碳动态的真实和长期数据,无法涵盖广泛的森林管理实践和条件。因此,选择最佳的森林碳保护政策必须依靠森林的生长和产量模型(例如美国森林服务局(USFS)森林植被模拟器(FVS))来预测经营活动对未来森林碳的影响。 FVS可能低估了旧林分积聚碳的能力,因为该模型依赖于USFS森林清单和分析数据,而这些数据缺少后期更新林和旧林分(LSOG)林分的数据。改善这些模型将增加选择成功使用森林减少大气碳的政策的可能性。从1995年到2002年,马诺梅特自然保护中心对65个10 m x 50 m永久样地进行了研究,以评估缅因州北部LSOG林分中的森林结构(生活树和枯死树,以及下层粗木料)。我们在2011年对这些土地进行了重新测量,以评估北部森林地区常见森林类型的LSOG林分的长期固碳趋势,这些林地中地面上还存在着活着的,枯死的和粗糙的木质材料碳库。相对于区域平均C储量(平均值的2.0-2.5倍),地上后期(LS)和旧增长(OG)的活碳(C)储量非常高,LS地块以正速率积累了地下活C( 0.61 Mg ha -1 年 -1 ),而OG地块上的C储量正在下降(-0.54 Mg ha -1 年 -1 )。这种变化是由山毛榉树皮真菌(Nectria sp。)的存在驱动的,这导致了直径更大的美洲山毛榉(Fagus grandifolia)树的死亡。我们还发现,森林植被模拟器的东北变种不是东北LS和OG林分中地上活碳积累速率的可靠预测指标。这项工作为理解美国东北部的老龄森林和森林管理在减缓气候变化战略中的作用提供了重要的基准。后期森林和旧森林在缓解气候变化中可以发挥重要作用,但是了解和量化对森林碳储量的自然干扰风险对于成功实施缓解策略至关重要。此外,区域森林碳模型将需要校准,以准确预测较老森林中的碳积累速率。

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