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东西伯利亚落叶松林火灾产生的碳排放。

Carbon Emissions From Fires in Eastern Siberian Larch Forests.

作者信息

Delcourt Clement J F, Rogers Brendan M, Akhmetzyanov Linar, Izbicki Brian, Scholten Rebecca C, Shestakova Tatiana A, van Wees Dave, Mack Michelle C, Sass-Klaassen Ute, Veraverbeke Sander

机构信息

Faculty of Science, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands.

Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France.

出版信息

Glob Chang Biol. 2025 May;31(5):e70247. doi: 10.1111/gcb.70247.

DOI:10.1111/gcb.70247
PMID:40407008
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC12100588/
Abstract

Siberian boreal forests have experienced increases in fire extent and intensity in recent years, which may threaten their role as carbon (C) sinks. Larch forests (Larix spp.) cover approximately 2.6 million km across Siberia, yet little is known about the magnitude and drivers of carbon combustion in these ecosystems. To address the paucity of field-based estimates of fuel load and consumption in Siberian larch forests, we sampled 41 burned plots, one to two years after fire, in Cajander larch (Larix cajanderi) forests in the Republic of Sakha (Yakutia), Russia. We estimated pre-fire carbon stocks and combustion with the objective of identifying the main drivers of carbon emissions. Pre-fire aboveground (trees and woody debris) and belowground carbon stocks at our study plots were 3.12 ± 1.26 kg C m (mean ± standard deviation) and 3.50 ± 0.93 kg C m. We found that combustion averaged 3.20 ± 0.75 kg C m, of which 78% (2.49 ± 0.56 kg C m) stemmed from organic soil layers. These results suggest that severe fires in Cajander larch forests can result in combustion rates comparable to those observed in North American boreal forests and exceeding those previously reported for other forest types and burning conditions in Siberia. Carbon combustion was driven by both fire weather conditions and landscape variables, with pre-fire organic soil depth being the strongest predictor across our plots. Our study highlights the need to better account for Siberian larch forest fires and their impact on the carbon balance, especially given the expected climate-induced increase in fire extent and severity in this region.

摘要

近年来,西伯利亚北方森林的火灾范围和强度不断增加,这可能会威胁到它们作为碳汇的作用。落叶松林(落叶松属)覆盖了西伯利亚约260万平方公里的土地,但对于这些生态系统中碳燃烧的规模和驱动因素却知之甚少。为了填补西伯利亚落叶松林燃料负荷和消耗的实地估计的空白,我们在俄罗斯萨哈共和国(雅库特)的卡扬德落叶松(Larix cajanderi)林中,对41个火灾发生一到两年后的烧毁地块进行了采样。我们估计了火灾前的碳储量和燃烧情况,目的是确定碳排放的主要驱动因素。我们研究地块火灾前的地上(树木和木质残体)和地下碳储量分别为3.12±1.26千克碳/平方米(平均值±标准差)和3.50±0.93千克碳/平方米。我们发现,平均燃烧量为3.20±0.75千克碳/平方米,其中78%(2.49±0.56千克碳/平方米)来自有机土壤层。这些结果表明,卡扬德落叶松林的严重火灾导致的燃烧率与北美北方森林相当,且超过了此前报道的西伯利亚其他森林类型和燃烧条件下的燃烧率。碳燃烧受到火灾天气条件和景观变量的驱动,火灾前有机土壤深度是我们所有地块中最强的预测因子。我们的研究强调,需要更好地考虑西伯利亚落叶松林火灾及其对碳平衡的影响,特别是考虑到该地区预计因气候导致的火灾范围和严重程度的增加。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/c00f51e3a875/GCB-31-e70247-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/2a23b9a9552e/GCB-31-e70247-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/69f121f32b56/GCB-31-e70247-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/d656f14c5f63/GCB-31-e70247-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/b9464ab41634/GCB-31-e70247-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/64ab10a155f9/GCB-31-e70247-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/c00f51e3a875/GCB-31-e70247-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/2a23b9a9552e/GCB-31-e70247-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/69f121f32b56/GCB-31-e70247-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/d656f14c5f63/GCB-31-e70247-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/b9464ab41634/GCB-31-e70247-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/64ab10a155f9/GCB-31-e70247-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/34b3/12100588/c00f51e3a875/GCB-31-e70247-g002.jpg

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本文引用的文献

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Global rise in forest fire emissions linked to climate change in the extratropics.全球森林火灾排放增加与温带地区气候变化有关。
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