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量化美国西南部火灾多发地区在预估气候条件下森林恢复和野火的碳平衡

Quantifying the Carbon Balance of Forest Restoration and Wildfire under Projected Climate in the Fire-Prone Southwestern US.

作者信息

Hurteau Matthew D

机构信息

Department of Biology, University of New Mexico, Albuquerque, New Mexico, United States of America.

出版信息

PLoS One. 2017 Jan 3;12(1):e0169275. doi: 10.1371/journal.pone.0169275. eCollection 2017.

Abstract

Climate projections for the southwestern US suggest a warmer, drier future and have the potential to impact forest carbon (C) sequestration and post-fire C recovery. Restoring forest structure and surface fire regimes initially decreases total ecosystem carbon (TEC), but can stabilize the remaining C by moderating wildfire behavior. Previous research has demonstrated that fire maintained forests can store more C over time than fire suppressed forests in the presence of wildfire. However, because the climate future is uncertain, I sought to determine the efficacy of forest management to moderate fire behavior and its effect on forest C dynamics under current and projected climate. I used the LANDIS-II model to simulate carbon dynamics under early (2010-2019), mid (2050-2059), and late (2090-2099) century climate projections for a ponderosa pine (Pinus ponderosa) dominated landscape in northern Arizona. I ran 100-year simulations with two different treatments (control, thin and burn) and a 1 in 50 chance of wildfire occurring. I found that control TEC had a consistent decline throughout the simulation period, regardless of climate. Thin and burn TEC increased following treatment implementation and showed more differentiation than the control in response to climate, with late-century climate having the lowest TEC. Treatment efficacy, as measured by mean fire severity, was not impacted by climate. Fire effects were evident in the cumulative net ecosystem exchange (NEE) for the different treatments. Over the simulation period, 32.8-48.9% of the control landscape was either C neutral or a C source to the atmosphere and greater than 90% of the thin and burn landscape was a moderate C sink. These results suggest that in southwestern ponderosa pine, restoring forest structure and surface fire regimes provides a reasonable hedge against the uncertainty of future climate change for maintaining the forest C sink.

摘要

美国西南部的气候预测表明,未来气候将更温暖、更干燥,这有可能影响森林碳(C)固存和火灾后碳恢复。恢复森林结构和地表火灾状况最初会减少生态系统总碳(TEC),但可以通过调节野火行为来稳定剩余的碳。先前的研究表明,在有野火的情况下,与受到火灾抑制的森林相比,经火灾维持的森林随着时间的推移可以储存更多的碳。然而,由于未来气候不确定,我试图确定森林管理在调节火灾行为方面的功效及其对当前和预测气候下森林碳动态的影响。我使用LANDIS-II模型模拟了亚利桑那州北部以黄松(Pinus ponderosa)为主的景观在本世纪早期(2010 - 2019年)、中期(2050 - 2059年)和晚期(2090 - 2099年)气候预测下的碳动态。我进行了为期100年的模拟,采用两种不同的处理方式(对照、间伐和火烧),野火发生概率为五十分之一。我发现,无论气候如何,对照的TEC在整个模拟期内持续下降。间伐和火烧处理后的TEC在实施处理后增加,并且在对气候的响应上比对照表现出更多差异,本世纪晚期气候下的TEC最低。以平均火灾严重程度衡量的处理效果不受气候影响。不同处理的累积净生态系统交换(NEE)中火灾影响明显。在模拟期内,对照区域32.8 - 48.9%对大气而言碳中性或为碳源,而间伐和火烧区域超过90%是适度的碳汇。这些结果表明,在西南部的黄松林中,恢复森林结构和地表火灾状况为应对未来气候变化的不确定性以维持森林碳汇提供了合理的保障。

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