Abstract Potential for using remote sensing to estimate carbon fluxes across northern peatlands - A review
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Potential for using remote sensing to estimate carbon fluxes across northern peatlands - A review

机译:利用遥感估算北部泥炭地碳通量的潜力-评论

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AbstractPeatlands store large amounts of terrestrial carbon and any changes to their carbon balance could cause large changes in the greenhouse gas (GHG) balance of the Earth's atmosphere. There is still much uncertainty about how the GHG dynamics of peatlands are affected by climate and land use change. Current field-based methods of estimating annual carbon exchange between peatlands and the atmosphere include flux chambers and eddy covariance towers. However, remote sensing has several advantages over these traditional approaches in terms of cost, spatial coverage and accessibility to remote locations. In this paper, we outline the basic principles of using remote sensing to estimate ecosystem carbon fluxes and explain the range of satellite data available for such estimations, considering the indices and models developed to make use of the data. Past studies, which have used remote sensing data in comparison with ground-based calculations of carbon fluxes over Northern peatland landscapes, are discussed, as well as the challenges of working with remote sensing on peatlands. Finally, we suggest areas in need of future work on this topic. We conclude that the application of remote sensing to models of carbon fluxes is a viable research method over Northern peatlands but further work is needed to develop more comprehensive carbon cycle models and to improve the long-term reliability of models, particularly on peatland sites undergoing restoration.Graphical abstractDisplay OmittedHighlightsOptical data can be used to drive models of peatland carbon flux.Water, temperature and vegetation indices are important model factors.Challenges from peatland heterogeneity and vegetation compositionRemote sensing driven models have the potential to fill gaps in current research
机译: 摘要 泥炭地存储了大量的陆地碳,其碳平衡的任何变化都可能导致该地区的温室气体(GHG)平衡发生较大变化。地球的大气层。泥炭地温室气体动态如何受到气候和土地利用变化的影响仍然存在很多不确定性。当前估算泥炭地与大气之间年度碳交换的基于现场的方法包括通量室和涡流协方差塔。但是,在成本,空间覆盖范围和对远程位置的可访问性方面,遥感比这些传统方法具有多个优势。在本文中,我们概述了使用遥感估算生态系统碳通量的基本原理,并考虑了为利用这些数据而开发的指标和模型,解释了可用于此类估算的卫星数据的范围。讨论了过去的研究,这些研究使用遥感数据与北部泥炭地景观的地面碳通量计算进行了比较,以及在泥炭地上进行遥感工作面临的挑战。最后,我们建议需要在此主题上进行进一步工作的领域。我们得出结论,将遥感技术应用到碳通量模型上是北部​​泥炭地上可行的研究方法,但是还需要进一步的工作来开发更全面的碳循环模型并提高模型的长期可靠性,尤其是在经历恢复的泥炭地上。 图形摘要 省略显示 突出显示 光学数据可用于驱动泥炭地碳通量模型。 水,温度和植被指数是重要的模型因素。 泥炭地异质性和植被组成带来的挑战 由远程感应驱动模型具有填补当前研究空白的潜力

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