Rk. Dixon et On. Krankina, FOREST-FIRES IN RUSSIA - CARBON-DIOXIDE EMISSIONS TO THE ATMOSPHERE, Canadian journal of forest research, 23(4), 1993, pp. 700-705
Boreal forests of Russia play a prominent role in the global carbon cy
cle and the flux of greenhouse gases to the atmosphere. Large areas of
Russian forest burn annually, and contributions to the net flux of ca
rbon to the atmosphere may be significant. Forest fire emissions were
calculated for the years 1971-1991 using fire frequency and distributi
on data and fuel and carbon density for different forest ecoregions of
Russia. Both direct carbon release and indirect post-fire biogenic ca
rbon flux were estimated. From 1971 to 1991 the annual total forest ar
ea burned by wildfire ranged from 1.41 X 10(6) to 10.0 X 10(6) ha. App
roximately 15 000 - 25 000 forest fires occurred annually during this
period. Mean annual direct CO2-C emissions from wildfire was approxima
tely 0.05 Pg over this 21 -year period. Total post-fire biogenic CO2-C
emissions for 1971-1991 ranged from 2.5 to 5.9 Pg (0.12-0.28 Pg annua
lly). Forest fires and other disturbances are expected to be a primary
mechanism driving vegetation change associated with projected global
climate change. Future forest fire scenarios in Russia based on genera
l circulation model projections suggest that up to 30-50% of the land
surface area, or 334 x 10(6) to 631 x 10(6) ha of forest, will be affe
cted. An additional 6.7 x 10(6) to 12.6 x 10(6) ha of Russian boreal f
orest are projected to burn annually if general circulation model base
d vegetation-change scenarios are achieved within the next 50 years. T
he direct flux Of CO2-C from future forest fires is estimated to total
6.1-10.7 Pg over a 50-year period. Indirect post-fire biogenic releas
e of greenhouse gases in the future is expected to be two to six times
greater than direct emissions. Forest management and fire-control act
ivities may help reduce wildfire severity and mitigate the associated
pulse of greenhouse gases into the atmosphere.