The role of peatland degradation, protection and restoration for climate change mitigation in the SSP scenarios

J. Doelman, W. Verhagen, E. Stehfest, D. V. van Vuuren
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Abstract

Peatlands only cover a small fraction of the global land surface (∼3%) but store large amounts of carbon (∼600 GtC). Drainage of peatlands for agriculture results in the decomposition of organic matter, leading to greenhouse gas (GHG) emissions. As a result, degraded peatlands are currently responsible for 2%–3% of global anthropogenic emissions. Preventing further degradation of peatlands and restoration (i.e. rewetting) are therefore important for climate change mitigation. In this study, we show that land-use change in three SSP scenarios with optimistic, recent trends, and pessimistic assumptions leads to peatland degradation between 2020 and 2100 ranging from −7 to +10 Mha (−23% to +32%), and a continuation or even an increase in annual GHG emissions (−0.1 to +0.4 GtCO2-eq yr−1). In default mitigation scenarios without a specific focus on peatlands, peatland degradation is reduced due to synergies with forest protection and afforestation policies. However, this still leaves large amounts of GHG emissions from degraded peatlands unabated, causing cumulative CO2 emissions from 2020 to 2100 in an SSP2-1.5 °C scenario of 73 GtCO2. In a mitigation scenario with dedicated peatland restoration policy, GHG emissions from degraded peatlands can be reduced to nearly zero without major effects on projected land-use dynamics. This underlines the opportunity of peatland protection and restoration for climate change mitigation and the need to synergistically combine different land-based mitigation measures. Peatland location and extent estimates vary widely in the literature; a sensitivity analysis implementing various spatial estimates shows that especially in tropical regions degraded peatland area and peatland emissions are highly uncertain. The required protection and mitigation efforts are geographically unequally distributed, with large concentrations of peatlands in Russia, Europe, North America and Indonesia (33% of emission reductions are located in Indonesia). This indicates an important role for only a few countries that have the opportunity to protect and restore peatlands with global benefits for climate change mitigation.
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在可持续战略计划情景中,泥炭地退化、保护和恢复对减缓气候变化的作用
泥炭地仅覆盖全球陆地表面的一小部分(约3%),但储存了大量的碳(约600 GtC)。泥炭地用于农业的排水导致有机物分解,导致温室气体排放。因此,退化的泥炭地目前占全球人为排放的2%-3%。因此,防止泥炭地进一步退化和恢复(即再湿润)对减缓气候变化非常重要。在本研究中,我们表明,在乐观、近期趋势和悲观假设的三种SSP情景下,土地利用变化导致泥炭地在2020年至2100年间退化,范围为- 7至+10 Mha(- 23%至+32%),年温室气体排放量持续甚至增加(- 0.1至+0.4 GtCO2-eq年- 1)。在没有特别关注泥炭地的默认缓解情景中,由于与森林保护和造林政策的协同作用,泥炭地退化得以减少。然而,退化泥炭地的大量温室气体排放仍未减少,在SSP2-1.5°C情景下,从2020年到2100年的累计二氧化碳排放量为73亿吨二氧化碳。在有专门泥炭地恢复政策的缓解情景下,退化泥炭地的温室气体排放可以减少到几乎为零,而不会对预计的土地利用动态产生重大影响。这强调了泥炭地保护和恢复对缓解气候变化的机会,以及需要协同结合不同的陆基缓解措施。泥炭地的位置和范围估计在文献中差异很大;实施各种空间估算的敏感性分析表明,特别是在热带地区,退化的泥炭地面积和泥炭地排放具有高度的不确定性。所需的保护和缓解努力在地理上分布不均,泥炭地主要集中在俄罗斯、欧洲、北美和印度尼西亚(33%的减排在印度尼西亚)。这表明,只有少数国家有机会保护和恢复泥炭地,为减缓气候变化带来全球利益,它们可以发挥重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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