Asymmetrical Lightning Fire Season Expansion in the Boreal Forest of Northeast China

All-season warming is assumed to advance snowmelt and delay snow accumulation; additionally, coupled with warming-induced drought stress, all-season warming could extend both the beginning and the end of the fire season. Using fire data updated for 1968–2018, we found an asymmetrical expansion of th...

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Published inForests Vol. 12; no. 8; p. 1023
Main Authors Gao, Cong, An, Ran, Wang, Wenqian, Shi, Chunming, Wang, Mingyu, Liu, Kezhen, Wu, Xiaoxu, Wu, Guocan, Shu, Lifu
Format Journal Article
LanguageEnglish
Published Basel MDPI AG 2021
Subjects
asymmetrical expansion
Asymmetry
boreal forest
Boreal forests
Climate change
Datasets
Drought
Evapotranspiration
Expansion
fire season
Fires
Forest & brush fires
Forest fires
Lightning
lightning fire
Precipitation
Seasonal variations
Seasons
Snow
Snow accumulation
Snowmelt
Soil moisture
Taiga
Temperature
Trends
China
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Abstract All-season warming is assumed to advance snowmelt and delay snow accumulation; additionally, coupled with warming-induced drought stress, all-season warming could extend both the beginning and the end of the fire season. Using fire data updated for 1968–2018, we found an asymmetrical expansion of the lightning fire season in the boreal forest of Northeast China. Lightning fires have not advanced into the early fire season (May–June) but have largely extended into the snowless late fire season (July–September) since the late 1990s (mean end Julian date delayed by 51.1 days for 1998–2018 compared with 1968–1997, p < 0.001). Despite significant warming, the Julian days of snowmelt have changed only slightly, which has prohibited the fire season from advancing into early spring. The expansion of lightning fires into July–September was associated with a warming-induced significant increase in evapotranspiration and a decrease in soil/fuel moisture.
AbstractList All-season warming is assumed to advance snowmelt and delay snow accumulation; additionally, coupled with warming-induced drought stress, all-season warming could extend both the beginning and the end of the fire season. Using fire data updated for 1968–2018, we found an asymmetrical expansion of the lightning fire season in the boreal forest of Northeast China. Lightning fires have not advanced into the early fire season (May–June) but have largely extended into the snowless late fire season (July–September) since the late 1990s (mean end Julian date delayed by 51.1 days for 1998–2018 compared with 1968–1997, p < 0.001). Despite significant warming, the Julian days of snowmelt have changed only slightly, which has prohibited the fire season from advancing into early spring. The expansion of lightning fires into July–September was associated with a warming-induced significant increase in evapotranspiration and a decrease in soil/fuel moisture.
Author Wang, Mingyu
Shi, Chunming
Wang, Wenqian
Wu, Guocan
Gao, Cong
Liu, Kezhen
Wu, Xiaoxu
An, Ran
Shu, Lifu
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Snippet All-season warming is assumed to advance snowmelt and delay snow accumulation; additionally, coupled with warming-induced drought stress, all-season warming...
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SubjectTerms asymmetrical expansion
Asymmetry
boreal forest
Boreal forests
Climate change
Datasets
Drought
Evapotranspiration
Expansion
fire season
Fires
Forest & brush fires
Forest fires
Lightning
lightning fire
Precipitation
Seasonal variations
Seasons
Snow
Snow accumulation
Snowmelt
Soil moisture
Taiga
Temperature
Trends
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Title Asymmetrical Lightning Fire Season Expansion in the Boreal Forest of Northeast China
URI https://www.proquest.com/docview/2565236911/abstract/
https://doaj.org/article/d228d09a894e4898a2482883a6c1854c
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