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Estimates of carbon stored in harvested wood products from the United States forest service northern region, 1906-2010

机译:1906-2010年,美国北部森林服务区伐木产品中储存的碳的估计值

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Background Global forests capture and store significant amounts of CO2 through photosynthesis. When carbon is removed from forests through harvest, a portion of the harvested carbon is stored in wood products, often for many decades. The United States Forest Service (USFS) and other agencies are interested in accurately accounting for carbon flux associated with harvested wood products (HWP) to meet greenhouse gas monitoring commitments and climate change adaptation and mitigation objectives. This paper uses the Intergovernmental Panel on Climate Change (IPCC) production accounting approach and the California Forest Project Protocol (CFPP) to estimate HWP carbon storage from 1906 to 2010 for the USFS Northern Region, which includes forests in northern Idaho, Montana, South Dakota, and eastern Washington. Results Based on the IPCC approach, carbon stocks in the HWP pool were increasing at one million megagrams of carbon (MgC) per year in the mid 1960s, with peak cumulative storage of 28 million MgC occurring in 1995. Net positive flux into the HWP pool over this period is primarily attributable to high harvest levels in the mid twentieth century. Harvest levels declined after 1970, resulting in less carbon entering the HWP pool. Since 1995, emissions from HWP at solid waste disposal sites have exceeded additions from harvesting, resulting in a decline in the total amount of carbon stored in the HWP pool. The CFPP approach shows a similar trend, with 100-year average carbon storage for each annual Northern Region harvest peaking in 1969 at 937,900 MgC, and fluctuating between 84,000 and 150,000 MgC over the last decade. Conclusions The Northern Region HWP pool is now in a period of negative net annual stock change because the decay of products harvested between 1906 and 2010 exceeds additions of carbon to the HWP pool through harvest. However, total forest carbon includes both HWP and ecosystem carbon, which may have increased over the study period. Though our emphasis is on the Northern Region, we provide a framework by which the IPCC and CFPP methods can be applied broadly at sub-national scales to other regions, land management units, or firms.
机译:背景技术全球森林通过光合作用捕获和储存大量的二氧化碳。当通过采伐从森林中清除碳时,一部分采伐的碳通常存储在木制品中数十年。美国森林服务局(USFS)和其他机构对准确计算与采伐木材产品(HWP)相关的碳通量感兴趣,以满足温室气体监测承诺以及气候变化适应和缓解目标。本文使用政府间气候变化专门委员会(IPCC)的生产核算方法和加利福尼亚森林项目协议(CFPP)来估算USFS北部地区1906年至2010年的HWP碳存储,其中包括爱达荷州北部,蒙大拿州,南达科他州的森林和华盛顿东部。结果基于IPCC方法,HWP池中的碳储量在1960年代中期以每年100万毫克碳(MgC)的速度增长,1995年出现了2800万MgC的峰值累积存储。净流入HWP池的正流量这一时期的主要原因是二十世纪中叶的丰收水平。 1970年以后收成水平下降,导致进入HWP池的碳减少。自1995年以来,固体废物处置场的HWP排放量已超过收割时的增加量,导致HWP池中存储的碳总量下降。 CFPP方法显示出类似的趋势,北部地区每年的年度收获的100年平均碳储存量在1969年达到937,900 MgC的峰值,并且在过去十年间在84,000至150,000 MgC之间波动。结论北部地区HWP池现在处于年净净库存变化的时期,因为1906年至2010年之间收获的产品衰减超过了通过收获为HWP池增加的碳。但是,森林总碳包括HWP和生态系统碳,这在研究期间可能有所增加。尽管我们的重点是北部地区,但我们提供了一个框架,通过该框架,IPCC和CFPP方法可以在地方以下各级广泛应用于其他地区,土地管理部门或公司。

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