摘要:This study focused on structural analysis of ground carbon storage following fires in light
conifer stands of the Lower Angara region (Siberia, Russia). Experimental fires of
varying frontal intensity were conducted at Scots pine and mixed larch forests of
southern taiga. Considerable amounts of surface and ground forest fuels (21–38 tC ha − 1)
enhanced low- to high-intensity fires. Post-fire carbon storage decreased by 16–49% depending on fire
intensity and rate of spread, with depth of burn being 0.9–6.6 cm. Carbon emissions varied from 4.48
to 15.89 t ha − 1 depending on fire intensity and forest type. Depth of burn and carbon emissions for four
major site types were correlated with a weather-based fire hazard index.