Register      Login
International Journal of Wildland Fire International Journal of Wildland Fire Society
Journal of the International Association of Wildland Fire
RESEARCH ARTICLE

Fire return intervals within the northern boundary of the larch forest in Central Siberia

Vyacheslav I. Kharuk A C , Mariya L. Dvinskaya A and K. Jon Ranson B
+ Author Affiliations
- Author Affiliations

A VN Sukachev Institute of Forest, Siberian Federal University, Krasnoyarsk, 660036 Russia.

B NASA’s Goddard Space Flight Center, Code 618, Greenbelt, MD 20771, USA.

C Corresponding author. Email: kharuk@ksc.krasn.ru

International Journal of Wildland Fire 22(2) 207-211 https://doi.org/10.1071/WF11181
Submitted: 22 December 2011  Accepted: 10 July 2012   Published: 11 September 2012

Abstract

A fire history of northern larch forests was studied. These larch forests are found near the northern limit of their range at ~71°N, where fires are predominantly caused by lightning strikes rather than human activity. Fire-return intervals (FRIs) were calculated based on fire scars and dates of tree natality. Tree natality was used as an approximation of the date of the last fire. The average FRI was found to be 295 ± 57 years, which is the longest reported for larch-dominated stands. Prior studies reported 80–90-year FRIs at 64°N and ~200 years near the latitude of the Arctic Circle. Comparing data from fires that occurred in 1700–1849 (end of the Little Ice Age, LIA) and 1850–1999 (post-LIA warming) indicates approximately twice as many fires occurred during the latter period. This agrees with the hypothesis that observed climatic warming will result in an increase in fire frequency. Our results also indicate that fires that did not leave visible fire scars on the tree stem may be identified based on the date of growth release revealed from dendrochronology.

Additional keywords: Larix gmelinii, wildfires.


References

Bergeron Y, Gauthier S, Flannigan M, Kafka V (2004) Fire regimes at the transition between mixed wood and coniferous boreal forest in Northwestern Quebec. Ecology 85, 1916–1932.
Fire regimes at the transition between mixed wood and coniferous boreal forest in Northwestern Quebec.Crossref | GoogleScholarGoogle Scholar |

Buechling A, Baker WL (2004) A fire history from tree rings in a high-elevation forest of Rocky Mountain National Park. Canadian Journal of Forest Research 34, 1259–1273.
A fire history from tree rings in a high-elevation forest of Rocky Mountain National Park.Crossref | GoogleScholarGoogle Scholar |

Conard SG, Ivanova GA (1997) Wildfire in Russian boreal forests – potential impacts of fire regime characteristics on emissions and global carbon balance estimates. Environmental Pollution 98, 305–313.
Wildfire in Russian boreal forests – potential impacts of fire regime characteristics on emissions and global carbon balance estimates.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaK1cXitlequrc%3D&md5=b658b513b2f898dfd12a3601313e991aCAS |

Conard SG, Sukhinin AI, Stocks BJ, Cahoon DR, Davidenko EP, Ivanova GA (2002) Determining effects of area burned and fire severity on carbon cycling and emissions in Siberia. Climatic Change 55, 197–211.
Determining effects of area burned and fire severity on carbon cycling and emissions in Siberia.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD38XntVKqt7o%3D&md5=95240a82751de0c1e58dde5124a6c9a1CAS |

Cook ER, Kairiukstis LA (1990) ‘Methods of Dendrochronology. Applications in the Environmental Sciences.’ (Kluwer Academic Publishers: London)

Fomchenkov VF, Sdobnova VV, Danilov NK, Danilova SV, Kurdina GV, Beljakova TF (2003) Forest Fund of Russia (data of State Forest Account, state by 1 January 2003), Reference Book. (All-Russia Research Institute of Forestry and Mechanisation: Moscow) [in Russian]

Gillett NP, Weaver AJ, Zwiers FW, Flannigan MD (2004) Detecting the effect of climate change on Canadian forest fires. Geophysical Research Letters 31, L18211
Detecting the effect of climate change on Canadian forest fires.Crossref | GoogleScholarGoogle Scholar |

Girardin MP, Ali AA, Carcaillet C, Mudelsee M, Drobyshev I, Hely C, Bergeron Y (2009) Heterogeneous response of circumboreal wildfire risk to climate change since the early 1900s. Global Change Biology 15, 2751–2769.
Heterogeneous response of circumboreal wildfire risk to climate change since the early 1900s.Crossref | GoogleScholarGoogle Scholar |

Heyerdahl EK, Beubaker LB, Agee JK (2001) Spatial controls of historical fire regimes: a multiscale example from the interior west, USA. Ecology 82, 660–678.
Spatial controls of historical fire regimes: a multiscale example from the interior west, USA.Crossref | GoogleScholarGoogle Scholar |

Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bulletin 43, 69–78.

Intergovernmental Panel on Climate Change (IPCC) (2007) ‘Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change.’ (Ed. S Solomon, D Qin, M Manning, Z Chen, M Marquis, KB Averyt, M Tignor, HL Miller) (Cambridge University Press: Cambridge, UK, and New York)

Kharuk VI, Dvinskaya ML, Ranson KJ, Im ST (2005) Expansion of evergreen conifers to the larch-dominated zone and climatic trends. Russian Journal of Ecology 36, 164–170.
Expansion of evergreen conifers to the larch-dominated zone and climatic trends.Crossref | GoogleScholarGoogle Scholar |

Kharuk VI, Ranson KJ, Dvinskaya ML (2008) Wildfires dynamic in the larch dominance zone. Geophysical Research Letters 35, L01402
Wildfires dynamic in the larch dominance zone.Crossref | GoogleScholarGoogle Scholar |

Kharuk VI, Ranson KJ, Dvinskaya ML, Im ST (2011) Wildfires in northern Siberian larch dominated communities. Environmental Research Letters 6, 045208
Wildfires in northern Siberian larch dominated communities.Crossref | GoogleScholarGoogle Scholar |

Kloeppel BD, Gower ST, Trechel IW, Kharuk V (1998) Foliar carbon isotope discrimination in Larix species and sympatric evergreen conifers: a global comparison. Oecologia 114, 153–159.
Foliar carbon isotope discrimination in Larix species and sympatric evergreen conifers: a global comparison.Crossref | GoogleScholarGoogle Scholar |

Kovacs K, Ranson KJ, Sun G, Kharuk VI (2004) The relationship of the Terra MODIS fire product and anthropogenic features in the Central Siberian landscape. Earth Interactions 8, 1–25.
The relationship of the Terra MODIS fire product and anthropogenic features in the Central Siberian landscape.Crossref | GoogleScholarGoogle Scholar |

Larsen CPS (1997) Spatial and temporal variations in boreal forest fire frequency in northern Alberta. Journal of Biogeography 24, 663–673.
Spatial and temporal variations in boreal forest fire frequency in northern Alberta.Crossref | GoogleScholarGoogle Scholar |

Lombardo KJ, Swetnam TW, Baisan CH, Borchert MI (2009) Using bigcone Douglas-fir fire scars and tree rings to reconstruct interior chaparral fire history. Fire Ecology 5, 35–56.
Using bigcone Douglas-fir fire scars and tree rings to reconstruct interior chaparral fire history.Crossref | GoogleScholarGoogle Scholar |

Naurzbaev MM, Vaganov EA (2000) Variations in early summer and annual temperature in the East Taymir and Putoran (Siberia) over the last two millennia inferred from tree-rings. Journal of Geophysical Research 105, 7317–7326.
Variations in early summer and annual temperature in the East Taymir and Putoran (Siberia) over the last two millennia inferred from tree-rings.Crossref | GoogleScholarGoogle Scholar |

Naurzbaev MM, Vaganov EA, Sidorova OV (2003) Variability of the air temperature in the north of Eurasia inferred from millennial tree-ring chronologies. Earth Cryosphere 7, 84–91. [in Russian]

Payette S (1992) Fire as a controlling process in the North American boreal forest. In ‘A systems analysis of the boreal forest’. (Eds HH Shugart, R Leemans, GB Bonan) pp.144–169. (Cambridge University Press: Cambridge, UK)

Rinn F (1996) ‘Tsap V 3.6 Reference manual: computer program for tree-ring analysis and presentation.’ (RINNTECH: Heidelberg, Germany)

Shvidenko A, Schepaschenko D, McCallum I, Nilsson S (2007) Russian forests and forestry. (CD-ROM) (International Institute for Applied Systems Analysis and the Russian Academy of Science: Laxenburg, Austria)

Sofronov MA, Volokitina AV, Kajimoto T (1999) Ecology of wildland fires and permafrost: their interdependence in the northern part of Siberia. In: ‘Proceedings of the Eighth Symposium on the Joint Siberian Permafrost Studies between Japan and Russia in 1999’, 19–20 January 2000, Tsukuba, Japan. (Eds G Ioue, A Takenaka) pp. 211–218. (National Institute of Environmental Sciences: Tzukuba, Japan)

Swetnam TW (1996) Fire and climate history in the central Yenisey Region, Siberia. In ‘Fire in ecosystems of boreal Eurasia’. (Eds JG Goldammer, VV Furyaev) pp. 90–104. (Kluwer Academic Publisher: Dordrecht, the Netherlands)

Vaganov EA, Arbatskaya MK (1996) The climate history and wildfire frequency in the Mid of Krasnoyarsky Kray. I. Growing seasons climatic conditions and seasonal wild fire-distribution. Siberian Journal of Ecology 3, 9–18.

Wallenius T, Larjavaara M, Heikkinen J, Shibistova O (2011) Declining fires in Larix-dominated forests in northern Irkutsk district. International Journal of Wildland Fire 20, 248–254.
Declining fires in Larix-dominated forests in northern Irkutsk district.Crossref | GoogleScholarGoogle Scholar |

Weir JMH, Johnson EA, Miyanishi K (2000) Fire frequency and the spatial age mosaic of the mixed-wood boreal forest in western Canada. Ecological Applications 10, 1162–1177.
Fire frequency and the spatial age mosaic of the mixed-wood boreal forest in western Canada.Crossref | GoogleScholarGoogle Scholar |