Climatic controls of fire activity in the red pine forests of Eastern North America

Daniela Robles, Yves Bergeron, Jed Meunier, Michael Stamburgh, Patricia Raymond, Alexander Kryshen, Charles Goebel, Jonathan Eden, Igor Drobyshev

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4 Citations (Scopus)
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Abstract

Large-scale modes of climate variability influence forest fire activity and may modulate the future patterns of natural disturbances. We studied the effects of long-term changes in climate upon the fire regime in the red pine forests of eastern North America using (a) a network of sites with dendrochronological reconstructions of fire histories over 1700–1900 A.D., (b) reconstructed chronologies of climate indices (1700–1900), and (c) 20th century observational records of climate indices, local surface climate and fire (1950s-2021). We hypothesized that (H1) there are states of atmospheric circulation that are consistently associated with increased fire activity, (H2) these states mark periods of increased climatological fire hazard, and (H3) the observed decline in fire activity in the 20th century is associated with a long-term decline in the frequency of fire-prone states.

At the annual scale, years with significantly higher fire activity in the reconstructed and modern fire records were consistently associated with the positive phases of the Pacific North American pattern (PNA), either independently or in combination with the positive phase of the El Niño-Southern Oscillation index (ENSO). During years with both ENSO and PNA in their positive state, the region experienced positive mid-tropospheric heights and temperature anomalies resulting in drought conditions. The fire-prone climate states identified in the reconstructed records became less frequent in 1850 but re-emerged in the 20th century. While our study did not demonstrate a direct influence of climate on the observed decrease in fire activity in the 20th century, it does reveal a clear climate signal embedded within the fire history reconstruction of the region over the past centuries. This study underscores the importance of considering large-scale climatic patterns in understanding historical fire regimes and highlights their role for future fire dynamics in the region and shaping ecological effects of future fires.
Original languageEnglish
Article number110219
Number of pages16
JournalAgricultural and Forest Meteorology
Volume358
Early online date10 Sept 2024
DOIs
Publication statusPublished - 15 Nov 2024

Bibliographical note

Publisher Copyright:
© 2024 The Author(s)

Funder

The study was funded by NSERC (project RGPIN-2018–06637 to I.D.) and Research Fund of the University of Quebec at Abitibi-Temiscamingue (FUQAT).

Funding

The study was funded by NSERC (project RGPIN-2018\u201306637 to I.D.) and Research Fund of the University of Quebec at Abitibi-Temiscamingue (FUQAT). The study was done within the framework of the PREREAL project funded by EU JPI Climate program and Belmont Forum. We thank Marie Robles for the help with laboratory analyses. The paper is a publication of the SNS NordicFireFuels and GDRI ColdForests networks. The study was funded by NSERC (project RGPIN-2018-06637 to I.D.) and Research Fund of the University of Quebec at Abitibi-Temiscamingue (FUQAT) . The study was done within the framework of the PREREAL project funded by EU JPI Climate program and Belmont Forum. We thank Marie Robles for the help with laboratory analyses. The paper is a publication of the SNS NordicFireFuels and GDRI ColdForests networks.

FundersFunder number
Natural Sciences and Engineering Research Council of CanadaRGPIN-2018–06637
Université du Québec en Abitibi-Témiscamingue

    Keywords

    • Climate-fire link
    • Climate oscillation indices
    • ENSO
    • Eastern North America
    • Fire history
    • Mixed-pine forests
    • PNA
    • PDO

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