ENSO modulates wildfire activity in China

China is a key region for understanding fire activity and the drivers of its variability under strict fire suppression policies. Here, we present a detailed fire occurrence dataset for China, the Wildfire Atlas of China (WFAC; 2005–2018), based on continuous monitoring from multiple satellites and c...

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Veröffentlicht in:Nature communications 2021-03, Vol.12 (1), p.1764-1764, Article 1764
Hauptverfasser: Fang, Keyan, Yao, Qichao, Guo, Zhengtang, Zheng, Ben, Du, Jianhua, Qi, Fangzhong, Yan, Ping, Li, Jie, Ou, Tinghai, Liu, Jane, He, Maosheng, Trouet, Valerie
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Sprache:eng
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Zusammenfassung:China is a key region for understanding fire activity and the drivers of its variability under strict fire suppression policies. Here, we present a detailed fire occurrence dataset for China, the Wildfire Atlas of China (WFAC; 2005–2018), based on continuous monitoring from multiple satellites and calibrated against field observations. We find that wildfires across China mostly occur in the winter season from January to April and those fire occurrences generally show a decreasing trend after reaching a peak in 2007. Most wildfires (84%) occur in subtropical China, with two distinct clusters in its southwestern and southeastern parts. In southeastern China, wildfires are mainly promoted by low precipitation and high diurnal temperature ranges, the combination of which dries out plant tissue and fuel. In southwestern China, wildfires are mainly promoted by warm conditions that enhance evaporation from litter and dormant plant tissues. We further find a fire occurrence dipole between southwestern and southeastern China that is modulated by the El Niño-Southern Oscillation (ENSO). Fire activity in China and its associations with climate are not well quantified at a local scale. Here, the authors present a detailed fire occurrence dataset for China and find a dipole fire pattern between southwestern and southeastern China that is modulated by the El Niño-Southern Oscillation (ENSO).
ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-021-21988-6