Warren Matthew, Frolking Steve, Dai Zhaohua, Kurnianto Sofyan
1USDA Forest Service, Northern Research Station, 271 Mast Rd., Durham, NH 03824 USA.
2Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH USA.
Mitig Adapt Strateg Glob Chang. 2017;22(7):1041-1061. doi: 10.1007/s11027-016-9712-1. Epub 2016 May 13.
The climate mitigation potential of tropical peatlands has gained increased attention as Southeast Asian peatlands are being deforested, drained and burned at very high rates, causing globally significant carbon dioxide (CO) emissions to the atmosphere. We used a process-based dynamic tropical peatland model to explore peat carbon (C) dynamics of several management scenarios within the context of simulated twenty-first century climate change. Simulations of all scenarios with land use, including restoration, indicated net C losses over the twenty-first century ranging from 10 to 100 % of pre-disturbance values. Fire can be the dominant C-loss pathway, particularly in the drier climate scenario we tested. Simulated 100 years of oil palm () cultivation with an initial prescribed burn resulted in 2400-3000 Mg CO ha total emissions. Simulated restoration following one 25-year oil palm rotation reduced total emissions to 440-1200 Mg CO ha, depending on climate. These results suggest that even under a very optimistic scenario of hydrological and forest restoration and the wettest climate regime, only about one third of the peat C lost to the atmosphere from 25 years of oil palm cultivation can be recovered in the following 75 years if the site is restored. Emissions from a simulated land degradation scenario were most sensitive to climate, with total emissions ranging from 230 to 10,600 Mg CO ha over 100 years for the wettest and driest dry season scenarios, respectively. The large difference was driven by increased fire probability. Therefore, peat fire suppression is an effective management tool to maintain tropical peatland C stocks in the near term and should be a high priority for climate mitigation efforts. In total, we estimate emissions from current cleared peatlands and peatlands converted to oil palm in Southeast Asia to be 8.7 Gt CO over 100 years with a moderate twenty-first century climate. These emissions could be minimized by effective fire suppression and hydrological restoration.
随着东南亚泥炭地正以极高的速度被砍伐、排水和焚烧,导致大量二氧化碳排放到大气中,对全球气候产生重大影响,热带泥炭地在减缓气候变化方面的潜力日益受到关注。我们使用基于过程的动态热带泥炭地模型,在模拟的21世纪气候变化背景下,探索了几种管理情景下的泥炭碳(C)动态。对包括恢复在内的所有土地利用情景的模拟表明,在21世纪,碳净损失量相当于干扰前值的10%至100%。火灾可能是主要的碳损失途径,特别是在我们测试的较干燥气候情景中。模拟100年的油棕种植(初始规定燃烧)导致总排放量为2400 - 3000 Mg CO₂/公顷。在经过25年油棕轮作后进行模拟恢复,根据气候条件,总排放量降至440 - 1200 Mg CO₂/公顷。这些结果表明,即使在水文和森林恢复非常乐观的情景以及最湿润的气候条件下,如果进行恢复,在接下来的75年里,因25年油棕种植而排放到大气中的泥炭碳,只有约三分之一能够被回收。模拟土地退化情景的排放对气候最为敏感,在最湿润和最干燥的旱季情景下,100年内的总排放量分别为230至10600 Mg CO₂/公顷。这种巨大差异是由火灾发生概率增加导致的。因此,抑制泥炭火灾是短期内维持热带泥炭地碳储量的有效管理工具,应成为减缓气候变化努力的高度优先事项。总体而言,我们估计在21世纪气候适中的情况下,东南亚目前已开垦的泥炭地和转为油棕种植的泥炭地在100年内的排放量为87亿吨CO₂。通过有效的火灾抑制和水文恢复,可以将这些排放量降至最低。