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Previous Atlantic Multidecadal Oscillation (AMO) modulates the lightning-ignited fire regime in the boreal forest of Northeast China

Dados Bibliográficos

ID15544115
AutoresCong Gao (0000-0003-2170-4800, Beijing Normal University), Fengjun Zhao (0000-0001-7795-9795, Chinese Academy of Forestry), Chunming Shi (0000-0002-6609-7058, Beijing Normal University, autor correspondente), Kezhen Liu (0000-0003-3840-0416, Nanjing Forest Police College), Xiaoxu Wu (0000-0003-0598-4697, Beijing Normal University), Guocan Wu (0000-0001-7979-6379, Beijing Normal University), Ying Liang (0000-0002-1314-8261, Xinjiang Academy of Forestry), Lifu Shu (Schlumberger (Ireland))
Ano2021
Volume16
Fascículo2
Páginas024054-024054
Data de publicação2021-01-20
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoEnvironmental Research Letters (JOURNAL)
Identificadores do periódicoISSN: 1748-9326 • E-ISSN: 1748-9326
EditoraIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/abde09
OpenAlexW3124956851
IdiomaEN
Referências citadas67

Lightning-ignited fire is sensitive to climatic change and responsible for large fires in boreal forests. In addition to global-warming caused fire increase, large-scale climate oscillations have significantly contributed to fire variability. However, the leading climate oscillation driving lightning-ignited fire and the mechanisms connecting regional and large-scale climate in the boreal forest of Northeast China, the most fire-prone biome of China, are still unclear. By compositing fire, climate, and atmospheric data, we found that the previous Atlantic Multidecadal Oscillation (AMO) was significantly coherent with the May to August temperature–evapotranspiration variability and lightning-ignited fire occurrence. These connections were valid at both the interannual and multidecadal time scales. Different from previous viewpoints, we found no connection of fire occurrence with the El Niño-Southern Oscillation and Pacific Decadal Oscillation. A warm AMO was followed by high sea level pressure and geopotential height over the study region. We assume these atmospheric anomalies are associated with descending atmospheric motion, producing adiabatic warming and less precipitation on the land surface, both of which favour high fuel aridity and lightning ignition. Therefore, we believe that the winter AMO could be a promising predictor for lightning-ignited fire occurrences in the following summer

Arctic oscillation · Atlantic multidecadal oscillation · Atmospheric sciences · Boreal · Climatology · Ecosystem · Fire regime · Geography · Hindcast · Lightning (connector · North Atlantic oscillation · Northern Hemisphere · Pacific decadal oscillation · Sea surface temperature · Taiga · Climate variability and models · Environmental Science · Fire effects on ecosystems · Plant Water Relations and Carbon Dynamics · Geology

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