Mind the gap: reconciling tropical forest carbon flux estimates from earth observation and national reporting requires transparency

IF 3.9 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Viola Heinrich, Jo House, David A. Gibbs, Nancy Harris, Martin Herold, Giacomo Grassi, Roberta Cantinho, Thais M. Rosan, Barbara Zimbres, Julia Z. Shimbo, Joana Melo, Tristram Hales, Stephen Sitch, Luiz E. O. C. Aragão
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Abstract

Background

The application of different approaches calculating the anthropogenic carbon net flux from land, leads to estimates that vary considerably. One reason for these variations is the extent to which approaches consider forest land to be “managed” by humans, and thus contributing to the net anthropogenic flux. Global Earth Observation (EO) datasets characterising spatio-temporal changes in land cover and carbon stocks provide an independent and consistent approach to estimate forest carbon fluxes. These can be compared against results reported in National Greenhouse Gas Inventories (NGHGIs) to support accurate and timely measuring, reporting and verification (MRV). Using Brazil as a primary case study, with additional analysis in Indonesia and Malaysia, we compare a Global EO-based dataset of forest carbon fluxes to results reported in NGHGIs.

Results

Between 2001 and 2020, the EO-derived estimates of all forest-related emissions and removals indicate that Brazil was a net sink of carbon (− 0.2 GtCO2yr−1), while Brazil’s NGHGI reported a net carbon source (+ 0.8 GtCO2yr−1). After adjusting the EO estimate to use the Brazilian NGHGI definition of managed forest and other assumptions used in the inventory’s methodology, the EO net flux became a source of + 0.6 GtCO2yr−1, comparable to the NGHGI. Remaining discrepancies are due largely to differing carbon removal factors and forest types applied in the two datasets. In Indonesia, the EO and NGHGI net flux estimates were similar (+ 0.6 GtCO2 yr−1), but in Malaysia, they differed in both magnitude and sign (NGHGI: -0.2 GtCO2 yr−1; Global EO: + 0.2 GtCO2 yr−1). Spatially explicit datasets on forest types were not publicly available for analysis from either NGHGI, limiting the possibility of detailed adjustments.

Conclusions

By adjusting the EO dataset to improve comparability with carbon fluxes estimated for managed forests in the Brazilian NGHGI, initially diverging estimates were largely reconciled and remaining differences can be explained. Despite limited spatial data available for Indonesia and Malaysia, our comparison indicated specific aspects where differing approaches may explain divergence, including uncertainties and inaccuracies. Our study highlights the importance of enhanced transparency, as set out by the Paris Agreement, to enable alignment between different approaches for independent measuring and verification.

注意差距:协调来自地球观测和国家报告的热带森林碳通量估算需要透明度。
背景:计算陆地人为碳净通量的不同方法导致估算值差异很大。造成这些差异的一个原因是,各种方法认为林地在多大程度上是由人类“管理”的,从而对人为净通量有所贡献。描述土地覆盖和碳储量时空变化特征的全球地球观测数据集为估算森林碳通量提供了一种独立和一致的方法。这些可以与国家温室气体清单(NGHGIs)报告的结果进行比较,以支持准确和及时的测量、报告和核查(MRV)。我们以巴西为主要案例研究,并对印度尼西亚和马来西亚进行了进一步分析,将基于全球生态系统的森林碳通量数据集与全球温室气体地理信息系统报告的结果进行了比较。结果:2001年至2020年期间,由eo得出的所有森林相关排放和清除的估计表明,巴西是碳的净汇(- 0.2亿吨二氧化碳年-1),而巴西的NGHGI报告的净碳源(+ 0.8亿吨二氧化碳年-1)。在使用巴西国家温室气体指数(NGHGI)对管理森林的定义和清单方法中使用的其他假设对估算值进行调整后,估算值的净通量为+ 0.6亿吨二氧化碳年-1,与国家温室气体指数相当。剩下的差异主要是由于两个数据集使用的碳去除因子和森林类型不同。在印度尼西亚,EO和NGHGI净通量估算值相似(+ 0.6 GtCO2年-1),但在马来西亚,它们在量级和符号上都不同(NGHGI: -0.2 GtCO2年-1;全球EO: + 0.2 GtCO2年-1)。关于森林类型的空间明确数据集没有公开提供,供两种全球温室气体指数分析,限制了详细调整的可能性。结论:通过调整EO数据集以提高与巴西NGHGI管理森林碳通量估计值的可比性,最初的分歧估计值在很大程度上得到了调和,其余差异可以解释。尽管印度尼西亚和马来西亚可用的空间数据有限,但我们的比较表明了不同方法可能解释差异的具体方面,包括不确定性和不准确性。我们的研究强调了《巴黎协定》所规定的提高透明度的重要性,以使不同的方法能够协调一致,进行独立的测量和验证。
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来源期刊
Carbon Balance and Management
Carbon Balance and Management Environmental Science-Management, Monitoring, Policy and Law
CiteScore
7.60
自引率
0.00%
发文量
17
审稿时长
14 weeks
期刊介绍: Carbon Balance and Management is an open access, peer-reviewed online journal that encompasses all aspects of research aimed at developing a comprehensive policy relevant to the understanding of the global carbon cycle. The global carbon cycle involves important couplings between climate, atmospheric CO2 and the terrestrial and oceanic biospheres. The current transformation of the carbon cycle due to changes in climate and atmospheric composition is widely recognized as potentially dangerous for the biosphere and for the well-being of humankind, and therefore monitoring, understanding and predicting the evolution of the carbon cycle in the context of the whole biosphere (both terrestrial and marine) is a challenge to the scientific community. This demands interdisciplinary research and new approaches for studying geographical and temporal distributions of carbon pools and fluxes, control and feedback mechanisms of the carbon-climate system, points of intervention and windows of opportunity for managing the carbon-climate-human system. Carbon Balance and Management is a medium for researchers in the field to convey the results of their research across disciplinary boundaries. Through this dissemination of research, the journal aims to support the work of the Intergovernmental Panel for Climate Change (IPCC) and to provide governmental and non-governmental organizations with instantaneous access to continually emerging knowledge, including paradigm shifts and consensual views.
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