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The climate, the fuel and the land use: long-term regional variability of biomass burning in boreal forests

Molinari, Chiara LU orcid ; Lehsten, Veiko LU ; Blarquez, Olivier ; Carcaillet, Christopher ; Davis, Basil A.S. ; Kaplan, Jed O. ; Clear, Jennifer and Bradshaw, Richard LU (2018) In Global Change Biology 24(10). p.4929-4945
Abstract
The influence of different drivers on changes in North American and European boreal forests biomass burning (BB) during the Holocene was investigated based on the following hypotheses: land use was important only in the southernmost regions, while elsewhere climate was the main driver modulated by changes in fuel type. BB was reconstructed by means of 88 sedimentary charcoal records divided into six different site clusters. A statistical approach was used to explore the relative contribution of (a) pollen‐based mean July/summer temperature and mean annual precipitation reconstructions, (b) an independent model‐based scenario of past land use (LU), and (c) pollen‐based reconstructions of plant functional types (PFTs) on BB. Our hypotheses... (More)
The influence of different drivers on changes in North American and European boreal forests biomass burning (BB) during the Holocene was investigated based on the following hypotheses: land use was important only in the southernmost regions, while elsewhere climate was the main driver modulated by changes in fuel type. BB was reconstructed by means of 88 sedimentary charcoal records divided into six different site clusters. A statistical approach was used to explore the relative contribution of (a) pollen‐based mean July/summer temperature and mean annual precipitation reconstructions, (b) an independent model‐based scenario of past land use (LU), and (c) pollen‐based reconstructions of plant functional types (PFTs) on BB. Our hypotheses were tested with: (a) a west‐east northern boreal sector with changing climatic conditions and a homogeneous vegetation, and (b) a north‐south European boreal sector characterized by gradual variation in both climate and vegetation composition. The processes driving BB in boreal forests varied from one region to another during the Holocene. However, general trends in boreal biomass burning were primarily controlled by changes in climate (mean annual precipitation in Alaska, northern Quebec, and northern Fennoscandia, and mean July/summer temperature in central Canada and central Fennoscandia) and, secondarily, by fuel composition (BB positively correlated with the presence of boreal needleleaf evergreen
trees in Alaska and in central and southern Fennoscandia). Land use played
only a marginal role. A modification towards less flammable tree species (by promoting deciduous stands over fire‐prone conifers) could contribute to reduce circumboreal wildfire risk in future warmer periods. (Less)
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author
; ; ; ; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
biomass burning, boreal biome, climate variations, Holocene, land use, plant functional types
in
Global Change Biology
volume
24
issue
10
pages
4929 - 4945
publisher
Wiley-Blackwell
external identifiers
  • scopus:85050938958
  • pmid:29959810
ISSN
1365-2486
DOI
10.1111/gcb.14380
language
English
LU publication?
yes
id
678308f2-78e1-4b79-8823-7f0721bf203a
date added to LUP
2018-07-23 10:56:24
date last changed
2022-04-25 08:23:57
@article{678308f2-78e1-4b79-8823-7f0721bf203a,
  abstract     = {{The influence of different drivers on changes in North American and European boreal forests biomass burning (BB) during the Holocene was investigated based on the following hypotheses: land use was important only in the southernmost regions, while elsewhere climate was the main driver modulated by changes in fuel type. BB was reconstructed by means of 88 sedimentary charcoal records divided into six different site clusters. A statistical approach was used to explore the relative contribution of (a) pollen‐based mean July/summer temperature and mean annual precipitation reconstructions, (b) an independent model‐based scenario of past land use (LU), and (c) pollen‐based reconstructions of plant functional types (PFTs) on BB. Our hypotheses were tested with: (a) a west‐east northern boreal sector with changing climatic conditions and a homogeneous vegetation, and (b) a north‐south European boreal sector characterized by gradual variation in both climate and vegetation composition. The processes driving BB in boreal forests varied from one region to another during the Holocene. However, general trends in boreal biomass burning were primarily controlled by changes in climate (mean annual precipitation in Alaska, northern Quebec, and northern Fennoscandia, and mean July/summer temperature in central Canada and central Fennoscandia) and, secondarily, by fuel composition (BB positively correlated with the presence of boreal needleleaf evergreen<br/>trees in Alaska and in central and southern Fennoscandia). Land use played<br/>only a marginal role. A modification towards less flammable tree species (by promoting deciduous stands over fire‐prone conifers) could contribute to reduce circumboreal wildfire risk in future warmer periods.}},
  author       = {{Molinari, Chiara and Lehsten, Veiko and Blarquez, Olivier and Carcaillet, Christopher and Davis, Basil A.S. and Kaplan, Jed O. and Clear, Jennifer and Bradshaw, Richard}},
  issn         = {{1365-2486}},
  keywords     = {{biomass burning; boreal biome; climate variations; Holocene; land use; plant functional types}},
  language     = {{eng}},
  number       = {{10}},
  pages        = {{4929--4945}},
  publisher    = {{Wiley-Blackwell}},
  series       = {{Global Change Biology}},
  title        = {{The climate, the fuel and the land use: long-term regional variability of biomass burning in boreal forests}},
  url          = {{http://dx.doi.org/10.1111/gcb.14380}},
  doi          = {{10.1111/gcb.14380}},
  volume       = {{24}},
  year         = {{2018}},
}