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多日期、多传感器遥感揭示了厄瓜多尔帕拉莫地区富含碳的高山泥炭地的高密度。

Multidate, multisensor remote sensing reveals high density of carbon-rich mountain peatlands in the páramo of Ecuador.

机构信息

Michigan Technological University, School of Forest Resources and Environmental Science, Houghton, MI, USA.

Instituto Biósfera USFQ, Colegio de Ciencias Biológicas y Ambientales, Universidad San Francisco de Quito, Ecuador.

出版信息

Glob Chang Biol. 2017 Dec;23(12):5412-5425. doi: 10.1111/gcb.13807. Epub 2017 Jul 26.

Abstract

Tropical peatlands store a significant portion of the global soil carbon (C) pool. However, tropical mountain peatlands contain extensive peat soils that have yet to be mapped or included in global C estimates. This lack of data hinders our ability to inform policy and apply sustainable management practices to these peatlands that are experiencing unprecedented high rates of land use and land cover change. Rapid large-scale mapping activities are urgently needed to quantify tropical wetland extent and rate of degradation. We tested a combination of multidate, multisensor radar and optical imagery (Landsat TM/PALSAR/RADARSAT-1/TPI image stack) for detecting peatlands in a 2715 km area in the high elevation mountains of the Ecuadorian páramo. The map was combined with an extensive soil coring data set to produce the first estimate of regional peatland soil C storage in the páramo. Our map displayed a high coverage of peatlands (614 km ) containing an estimated 128.2 ± 9.1 Tg of peatland belowground soil C within the mapping area. Scaling-up to the country level, páramo peatlands likely represent less than 1% of the total land area of Ecuador but could contain as much as ~23% of the above- and belowground vegetation C stocks in Ecuadorian forests. These mapping approaches provide an essential methodological improvement applicable to mountain peatlands across the globe, facilitating mapping efforts in support of effective policy and sustainable management, including national and global C accounting and C management efforts.

摘要

热带泥炭地储存了全球土壤碳 (C) 库的很大一部分。然而,热带山区泥炭地含有广泛的泥炭土壤,这些泥炭土壤尚未被绘制或包含在全球 C 估计中。这种数据的缺乏阻碍了我们向这些泥炭地提供政策信息和应用可持续管理实践的能力,这些泥炭地正经历着前所未有的土地利用和土地覆被变化速度。迫切需要开展大规模快速制图活动,以量化热带湿地的范围和退化速度。我们测试了多日期、多传感器雷达和光学图像(Landsat TM/PALSAR/RADARSAT-1/TPI 图像堆叠)的组合,以检测厄瓜多尔帕拉莫高海拔山区 2715 公里范围内的泥炭地。该地图与广泛的土壤取芯数据集相结合,首次估算了帕拉莫地区的泥炭地土壤 C 储量。我们的地图显示了高覆盖率的泥炭地(614 公里),在制图区域内估计含有 128.2±9.1 百万吨泥炭地地下土壤 C。在全国范围内进行扩展,帕拉莫泥炭地可能只占厄瓜多尔总土地面积的不到 1%,但可能包含厄瓜多尔森林中高达~23%的地上和地下植被 C 储量。这些制图方法提供了一种重要的方法改进,适用于全球山区泥炭地,为支持有效政策和可持续管理的制图工作提供了便利,包括国家和全球 C 核算和 C 管理工作。

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