Haixiao Zhang , Xu Yue , Bin He , Jun Zhu , Chenguang Tian
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引用次数: 0
摘要
火灾及其碳排放对陆地表面、气候系统和空气质量有重大影响。然而,由于卫星观测的持续时间短和基于过程的模式的不确定性,具有详细时空火灾记录的长期数据集是有限的。在这里,我们采用了一种数据驱动的方法,将机器学习算法(MLA)与八个火灾模型的输出相结合,以重建1901-2012年的火灾二氧化碳排放。我们基于mla的数据集显示,全球火灾排放的二氧化碳下降幅度为- 7.45±0.12 Tg C / yr - 2 (- 0.29% / yr - 1),主要发生在南美洲和非洲。土地利用变化是主要驱动因素,减少了- 6.07±0.23 Tg C / yr - 2,其次是人口增长,减少了- 3.60±0.54 Tg C / yr - 2。人口增长通常会抑制农业和城市地区的火灾,但会增加雨林边缘发生森林砍伐的火灾风险。尽管气候变化对全球火灾CO2减少的影响有限(- 0.39±0.19 Tg C yr - 2),但它仍然是北方火灾的关键驱动因素,受降水变化的强烈影响。这些研究结果强调需要可靠的数据和知情的管理来支持防火和减缓气候变化的努力。
Centennial-scale decline in global fire emissions driven by land use and population growth
Fires and their carbon emissions have substantial impacts on land surface, climate systems, and air quality. However, long-term datasets with detailed spatiotemporal fire records are limited due to the short duration of satellite observations and uncertainties in process-based models. Here, we employ a data-driven approach that integrates machine learning algorithm (MLA) with outputs from eight fire models to reconstruct fire CO2 emissions in 1901–2012. Our MLA-based dataset reveals a global decline in fire-emitted CO2 at −7.45 ± 0.12 Tg C yr−2 (−0.29 % yr−1), mainly in South America and Africa. Land use change emerges as the primary driver, reducing fire CO2 emissions by −6.07 ± 0.23 Tg C yr−2, followed by population growth, which contributes −3.60 ± 0.54 Tg C yr−2. Population growth typically suppresses fires in agricultural and urban areas but raises fire risks at rainforest edges where deforestation occurs. Although climate change has a limited impact on global fire CO2 reduction (−0.39 ± 0.19 Tg C yr−2), it remains a key driver for boreal fires, strongly influenced by precipitation changes. These findings underscore the need for robust data and informed management to support fire prevention and climate change mitigation efforts.
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged.
Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.