Wildfires in Northern Siberian Larch Dominated Communities

• Main Authors: Dvinskaya, Maria L., Im, Sergey T., Ranson, Kenneth J., Khaurk, Viacheslav I.
• Format: Other/Unknown Material
• Language: unknown
• Published: 2011
• Subjects: Meteorology and Climatology; Ice; permafrost; Siberia
• Online Access: http://hdl.handle.net/2060/20120003864

The fire history of the northern larch forests within the permafrost zone in a portion of northern Siberia (approx 66 deg N, 100 deg E) was studied. Since there is little to no human activities in this area fires within the study area were mostly caused by lightning. Fire return intervals (FRI) were estimated based on burn marks on tree stems and dates of tree natality. FRI values varied from 130 yr to 350 yr with 200 +/- 50 yr mean. In southerly larch dominated communities FRI was found to be shorter (77 +/- 20 yr at approx 61 deg. N, and 82 +/- 7 at 64 deg N), and longer at the northern boundary (approx 71 deg) of larch stands (320 +/- 50 yr). During the Little Ice Age period in the 16th to 18th centuries FRI was approximately twice as long as recorded in this study. Fire caused changes in the soil including increases in soil drainage and permafrost thawing depth and a radial growth increase of about 2 times (with more than 6 times observed). This effect may simulate the predicted warming impact on the larch growth in the permafrost zone.