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首页> 外文期刊>Carbon balance and management >Mapping deep peat carbon stock from a LiDAR based DTM and field measurements, with application to eastern Sumatra
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Mapping deep peat carbon stock from a LiDAR based DTM and field measurements, with application to eastern Sumatra

机译:从基于LIDAR的DTM和现场测量的映射深泥炭碳储备,应用于东部Sumatra

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BACKGROUND:Reduction of carbon emissions from peatlands is recognized as an important factor in global climate change mitigation. Within the SE Asia region, areas of deeper peat present the greatest carbon stocks, and therefore the greatest potential for future carbon emissions from degradation and fire. They also support most of the remaining lowland swamp forest and its associated biodiversity. Accurate maps of deep peat are central to providing correct estimates of peat carbon stocks and to facilitating appropriate management interventions. We present a rapid and cost-effective approach to peat thickness mapping in raised peat bogs that applies a model of peat bottom elevation based on field measurements subtracted from a surface elevation model created from airborne LiDAR data.RESULTS:In two raised peat bog test areas in Indonesia, we find that field peat thickness measurements correlate well with surface elevation derived from airborne LiDAR based DTMs (Rsup2/sup 0.83-0.88), confirming that the peat bottom is often relatively flat. On this basis, we created a map of extent and depth of deep peat (?3?m) from a new DTM that covers two-thirds of Sumatran peatlands, applying a flat peat bottom of 0.61?m +MSL determined from the average of 2446 field measurements. A deep peat area coverage of 2.6?Mha or 60.1% of the total peat area in eastern Sumatra is mapped, suggesting that deep peat in this region is more common than shallow peat and its extent was underestimated in earlier maps. The associated deep peat carbon stock range is 9.0-11.5 Pg C in eastern Sumatra alone.CONCLUSION:We discuss how the deep peat map may be used to identify priority areas for peat and forest conservation and thereby help prevent major potential future carbon emissions and support the safeguarding of the remaining forest and biodiversity. We propose rapid application of this method to other coastal raised bog peatland areas in SE Asia in support of improved peatland zoning and management. We demonstrate that the upcoming global ICESat-2 and GEDI satellite LiDAR coverage will likely result in a global DTM that, within a few years, will be sufficiently accurate for this application.
机译:背景:泥炭地减少泥炭地的碳排放被认为是全球气候变化缓解的重要因素。在SE亚洲地区,深层泥炭的区域呈现最大的碳储量,因此是未来碳排放免于退化和火灾的最大潜力。他们还支持大部分剩余的低地沼泽森林及其相关的生物多样性。精确的深泥炭地图是提供正确估计的泥炭碳储存的核心,并促进适当的管理干预措施。我们提出了一种快速且经济高效的方法来涂抹覆盖的泥炭沼泽覆盖泥炭覆盖,该泥炭厚度映射,基于从机载LIDAR数据创建的表面高度模型中减去了泥炭底升高模型的泥炭底升高。结果:在两个凸起的泥炭沼泽测试区域在印度尼西亚,我们发现场泥炭厚度测量与基于空机激光雷达的DTMS(R 2 0.83-0.88)的表面升高相连,确认泥炭底部通常相对平坦。在此基础上,我们从一个新的DTM创建了一系列范围和深度深度(>?3?M),该地图覆盖了三分之二的Sumatran泥炭泥墙,施加扁平泥炭底部0.61Ωm+ MSL的底部确定2446个现场测量。深泥炭面积为2.6?MHA或60.1%的东部苏门答腊的总泥炭面积的覆盖率映射,表明该地区的深泥浆比浅泥炭更常见,并且在早期地图中被低估了它的程度。 Sondern Sumatra相关的深泥炭碳股票范围是9.0-11.5 pg C.结论:我们讨论深泥地图如何用于识别泥炭和森林保护的优先领域,从而有助于防止主要潜在的未来碳排放和支持保护剩余的森林和生物多样性。我们提出了快速将这种方法应用于SE亚洲其他沿海凸起的沼泽地地区,以支持改进的泥炭地分区和管理。我们证明即将到来的全球ICESAT-2和GEDI卫星激光乐队覆盖率可能导致全球DTM,即在几年内,将足够准确地对此申请。

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