Carbon dioxide emissions through land use change, fire, and oxidative peat decomposition in Borneo

被引:3
|
作者
Shiraishi, Tomohiro [1 ,2 ]
Hirata, Ryuichi [1 ]
Hayashi, Masato [3 ]
Hirano, Takashi [4 ]
机构
[1] Natl Inst Environm Studies NIES, Earth Syst Div, Ibaraki 3058506, Japan
[2] Nippon Bunri Univ, Sch Engn, Oita 8700397, Japan
[3] Japan Aerosp Explorat Agcy JAXA, Earth Observat Res Ctr, Ibaraki 3058505, Japan
[4] Hokkaido Univ, Res Fac Agr, Sapporo, Hokkaido 0608589, Japan
关键词
SOUTHEAST-ASIA; FOREST LOSS; INDONESIA; BIOMASS; PEATLANDS; BALANCE; EXPANSION; IMPACTS; EXTENT; SINK;
D O I
10.1038/s41598-023-40333-z
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Borneo has accumulated an abundance of woody carbon in its forests and peat. However, agricultural land conversion accompanied by plantation development, dead wood burning, and peat drying from drainage are major challenges to climate change mitigation. This study aimed to develop a method of estimating carbon dioxide (CO2) emissions from land use change, forest and peat fires, and oxidative peat decomposition, and CO2 uptake from biomass growth across Borneo using remote sensing data from 2001 to 2016. Although CO2 uptake by biomass growth in vast forests has shown a significant increasing trend, an annual net release of 461.10 +/- 436.51 (average +/- 1 standard deviation) Tg CO2 year(-1) was observed. The estimated emissions were predominantly characterized by land use changes from 2001 to 2003, with the highest emissions in 2001. Land use change was evaluated from annual land use maps with an accuracy of 92.0 +/- 1.0% (average +/- 1 standard deviation). Forest and peat fires contributed higher emissions in 2002, 2006, 2009, 2014, and 2015 compared to other years and were strongly correlated with the Southern Oscillation Indexes. These results suggest that more CO2 may have been released into the atmosphere than previously thought.
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页数:12
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