1. Climate-biosphere system in colder tundra state
2. Climate-biosphere system in warmer boreal forest state
This study describes the boreal forest-tundra boundary in a positive feedback system. Boreal forest decreases albedo relative to tundra, thereby increasing total net surface radiation and temperature. The presence of trees masks the high reflectance of snow. Simulations suggest that boreal forests raise both winter and summer temperatures relative to tundra, leading to conditions more favourable for boreal forest. Tundra has a higher albedo, which decreases net radiation and temperature, thereby leading to conditions more favourable for tundra.
Future changes to the distribution of boreal forest and tundra vegetation, such as from extensive logging or the influence of global warming, could alter the climate feedback mechanisms.
Contact
Jacqui Meyers
Email
jacqui.meyers@csiro.au
CSIRO Sustainable Ecosystems,
PO Box 284,
Canberra ACT 2601
Keywords
Ecosystem Feedback Mechanism, empirical data, Physical/Climate