Mel Boyd at BNZ_photo by Xanthe Walker
Mel Boyd measures the remnants of burned shrubs along a transect line across the Shovel Creek fire scar near Fairbanks, Alaska. Xanthe Walker
Mel Boyd measures the remnants of burned shrubs along a transect line across the Shovel Creek fire scar near Fairbanks, Alaska. Xanthe Walker
A boreal forest near Bonanza Creek LTER after a fire. Jill Johnstone, BNZ LTER
Smoke from a forest fire in an Alaskan boreal forest near Bonanza Creek LTER JIll Johnstone, BNZ LTER
Climate-related changes in environmental conditions are challenging rural residents’ ability to traverse the land and access subsistence resources.
Browsing by snowshoe hares and moose have dramatic top-down influences on vegetation composition, successional dynamics, and ecosystem function throughout interior Alaska. Knut Kielland
Recent models indicate that lengthening of the snow-free season and associated declines in surface albedo constitutes the largest positive feedback to climate warming in the boreal forest. Roger Ruess
Increases in air temperatures and depth of insulating snow cover during winter are accelerating the rate of permafrost thaw. In areas of ice-rich permafrost, widespread thermokarst is having significant consequences for biogeochemical cycling and surface hydrology. Ted Schuur
A recent shift in the Alaska fire regime has increased the frequency and size of high-severity fires that combust deep organic layers, exposing mineral soil and favoring the invasion of hardwoods. Within the BNZ LTER Regional Site Network, many sites that were dominated by black spruce prior to burning in 2004 have now converted to dense birch stands with very different vegetation and ecosystem characteristics (BD1 site). Roger Ruess