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Observation of Trends in Biomass Loss as a Result of Disturbance in the Conterminous US: 1986-2004

机译:在美国本土,由于干扰引起的生物量损失趋势的观察:1986-2004年

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The critical role of forests in the global carbon cycle is well known, but significant uncertainties remain about the specific role of disturbance, in part because of the challenge of incorporating spatial and temporal detail in the characterization of disturbance processes. In this study, we link forest inventory data to remote sensing data to derive estimates of pre- and post-disturbance biomass, and then use near-annual remote sensing observations of forest disturbance to characterize biomass loss associated with disturbance across the conterminous U.S. between 1986 and 2004. Nationally, year-to-year variability in the amount of live aboveground carbon lost as a result of disturbance ranged from a low of 61 T-g C (+/- 16) in 1991 to a high of 84 T-g C (+/- 33) in 2003. Eastern and western forest strata were relatively balanced in terms of their proportional contribution to national-level trends, despite eastern forests having more than twice the area of western forests. In the eastern forest stratum, annual biomass loss tracked closely with the area of disturbance, whereas in the western forest stratum, annual biomass loss showed more year-to-year variability that did not directly correspond to the area of disturbance, suggesting that the biomass density of forests affected by disturbance in the west was more spatially and temporally variable. Eastern and western forest strata exhibited somewhat opposing trends in biomass loss, potentially corresponding to the implementation of the Northwest Forest Plan in the mid 1990s that resulted in a shift of timber harvesting from public lands in the northwest to private lands in the south. Overall, these observations document modest increases in disturbance rates and associated carbon consequences over the 18-year period. These changes are likely not significant enough to weaken a growing forest carbon sink in the conterminous U.S. based largely on increased forest growth rates and biomass densities.
机译:森林在全球碳循环中的关键作用是众所周知的,但是关于干扰的具体作用仍然存在很大的不确定性,部分原因是要在干扰过程的表征中纳入时空细节的挑战。在这项研究中,我们将森林资源调查数据与遥感数据联系起来,以得出干扰前和干扰后生物量的估计值,然后使用对森林扰动的近年遥感观测来表征与1986年之间整个美国本土扰动相关的生物量损失和2004年。在全国范围内,由于扰动造成的地上活碳损失量逐年变化,范围从1991年的低61 Tg C(+/- 16)到最高的84 Tg C(+ / -33)2003年。尽管东部和西部森林的面积是西方森林的两倍多,但东部和西部森林对国家水平趋势的贡献却相对平衡。在东部森林地层中,年生物量损失与干扰区域密切相关,而在西部森林地层中,年生物量损失显示出更多的逐年变化性,并不直接对应于干扰区域,这表明生物量西部受干扰影响的森林密度在空间和时间上更具可变性。东部和西部森林地层的生物量流失趋势相反,这可能与1990年代中期实施的西北森林计划相对应,从而导致木材采伐从西北的公共土地转向南部的私有土地。总体而言,这些观察结果表明,在18年的时间里,干扰率和相关的碳排放影响适度增加。这些变化可能不足以削弱美国本土森林中不断增加的森林碳汇,而这主要是基于森林增长率和生物量密度的增加。

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