Fire Ecology and Fire Regimes in Boreal Ecosystems Oct 19, 2010

Fire ecology of boreal region Black spruce (Picea mariana) – serotinous cones, highly flamable – Early successional White spruce (Picea glauca) – Non serotinous cones – Late successional Other species: larch, birch, alder, willow, aspen

Soil temperature, moisture, and fire influence vegetation types

Boreal region: land of fire & ice Vegetation shaped by fire and permafrost – Heat and cold – Aridity and moisture Permafrost: permanently frozen ground – Impermeable boundary between surface and ground waters – Active layer (thaw zone) – allows for shallow soil, rooted vegetation Dynamic equilibrium between vegetation and permafrost determined by fire

Boreal Forests Fire Regime Wildfires are episodic Some years very large wildfires Relatively frequent fires Continuous layer of fuels: grasses, moss, shrubs, black spruce (~ lodgepole pine *) Dry summers Lightning, long days (midnight sun) Mixed fire-regime high intensity stand-replacing crown fires + ground fires (smoldering in deep organic layers) Natural fire cycles: ~ years After human use/protection: 500 in heavily protected (Beniston 2003)

Smoldering?

Boreal fires: high energy release rates

Effects of fire on boreal landscape Fire is the dominant disturbance in boreal forests Allows for massive decomposition and recycling of water and nutrients Fires cause active zone of permafrost to increase temporarily (vegetation = insulation) Replaces forest stands

Loss of protective insulation from vegetation

Post-fire permafrost thaw: recycling of nutrients & water

Fire creates mosaic of vegetation…

and mosaic of stand types…

Human influence on Boreal fires Fires deliberately set by Native Americans and settlers – Signal fires, campfires, hunting (ring of fire – moose, caribou), mosquito control – Gold rush in 1896 – “epidemic of forest fires” Railroad construction Expose mine deposits Create/improve pasture After railroad completed (1923) – new emphasis on fire suppression and control

Fire management in Alaska ’s – emphasis on fire control – Patrols and strong military presence 1950’s = enormous fires, mostly lightening caused (5 mill acres burned in 1957) – Smoke shut down “the state” for 2 weeks 1960’s and 70’s fire control in Alaska reached similar levels as the lower 48 (under BLM) – Emphasis on aircraft, helicopters, smokejumpers 17% of land is designated for fire suppression: “valued areas” (proximity to communities and roads) 83% of land (interior Alaska) under a natural fire regime.

Fire and Climate Change in the Boreal Region TTYGroup on potential general impacts of CC on fire dynamics: What has been predicted for temperature and precipitation due to climate change in North American boreal region? What does this mean for the fire weather of the N. A. boreal region? What are the direct effects of climate change on the vegetation composition of boreal forests? What does this mean for fire behavior?

Relationship between climate change and fire in Boreal regions (1) Climate change increases fire activity: – Warmer and drier climate (Higher T, lower PP) = drier fuels – Longer fire season – Increased lightening More fire = positive feedback on global warming – Increased greenhouse gas emissions enhancing warming. – Increased CO 2 = greater biomass production, more fuel (controversial)

Relationship between climate change and fire in Boreal regions (2) Indirect effects of climate change – More fuel loads ? CO 2 fertilization insect outbreaks tree line expansion into tundra – Less fuel loads / different fuel loads? = negative feedback Deciduous vs. coniferous – Longer fire season = drier forest floor = potential to alter depth of burn + deeper thaw of permafrost

Boreal forests: Carbon sink or source? TTYGroup: 1. What factors determine whether a region (or ecosystem) is a “sink” or “source,” and why? 2. What does it mean to refer to the boreal region as a “carbon sink” or a “carbon source”?

Boreal forests: Carbon sink or source? Forests sequester carbon via photosynthesis – Carbon stored in biomass – Long-term carbon storage: soil, permafrost, peat Carbon released to atmosphere by: – Respiration – Fire – Decomposition of soil organic matter, melting of permafrost Downward carbon flux: carbon sequestration Upward carbon flux: carbon emission Net carbon flux: sink or source Balance between CO 2 sequestration and emissions = complex!

Sink Source

CO2 fert Climate Fire CO2, Climate, fire

Effects of post-fire succession and human activities on future fire regimes in the boreal region? Rate of biomass recovery Species composition (deciduous vs. coniferous) Tree line expansion into tundra Fire severity – depth of burn, permafrost – feedbacks Fire suppression efforts – successful? Insects and disease – increase with warming?

Climate change effects on permafrost…