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As Area Burned By Wildfire Increases Washington’s Forests Will Lose Stored Carbon

July 26, 2012
Image Caption: A July 2012 PNW Research Station study explored how carbon dynamics in Washington State may be altered by more-frequent wildfires, triggered by a warming climate. The study looked at the effects of greater area burned on both live biomass and nonliving biomass, such as the dead standing trees and downed wood shown here. Credit: Tom Iraci, US Forest Service

Even small increases in area burned could have significant impacts on carbon storage

Forests in the Pacific Northwest store more carbon than any other region in the United States, but our warming climate may undermine their storage potential.

A new study conducted by the U.S. Forest Service’s Pacific Northwest Research Station and the Climate Impacts Group at the University of Washington has found that, by 2040, parts of Washington State could lose as much as a third of their carbon stores, as an increasing area of the state’s forests is projected to be burned by wildfire. The study–published in the July 2012 issue of the journal Ecological Applications–is the first to use statistical models and publicly available Forest Inventory and Analysis data to estimate the effects of a warming climate on carbon storage and fluxes on Washington’s forests.

“When considering the use of forests to store carbon, it will be critical to consider the increasing risk of wildfire,” said Crystal Raymond, a research biologist based at the station’s Pacific Wildland Fire Sciences Laboratory and lead author of the study. “Especially in the West, where climate-induced changes in fire are expected to be a key agent of change.”

Trees remove and sequester carbon from the atmosphere, in the form of carbon dioxide, acting as important stores, or “sinks,” of carbon that help to offset its accumulation in the atmosphere. When trees and other woody material in the forest are burned by fire, they release carbon back to the atmosphere, mostly as carbon dioxide, where it may once again act as a greenhouse gas that promotes warming. This land-atmosphere exchange of carbon is increasingly of interest to land managers seeking ways to actively manage forests to store carbon and help mitigate greenhouse gases.

To explore what effect climate-driven changes in wildfire might have on the ability of Washington’s forests to act as carbon sinks, Raymond and station research ecologist Don McKenzie used a novel approach. They combined published forest-inventory data, fire-history data, and statistical models of area burned to estimate historical and future carbon carrying capacity of three regions in Washington–the Western Cascades, the Eastern Cascades, and the Okanogan Highlands–based on potential forest productivity and projections of 21st century area burned.

“Forests on both the eastern and western slopes of the Cascade Range will lose carbon stored in live biomass because area burned across the state is expected to increase,” Raymond said. “Even small increases in area burned can have large consequences for carbon stored in living and dead biomass.”

The researchers looked at live biomass, which includes living trees and vegetation, as well as nonliving biomass in the form of coarse woody debris, which includes dead standing trees and downed logs. Both contribute to the carbon cycle, but in different ways–living biomass removes carbon from the atmosphere as vegetation grows, and coarse woody debris releases carbon over time as the material decomposes.

Raymond and McKenzie projected forests of the Western Cascades to be most sensitive to climate-driven increases in fire, losing anywhere from 24 to 37 percent of their live biomass and from 15 to 25 percent of their coarse woody debris biomass by 2040. These forests store significant carbon and typically burn with high severity, killing many trees and consuming coarse woody debris.

On the other side of the mountains, the researchers also projected a decrease in live biomass by 2040–of anywhere between 17 and 26 percent in the Eastern Cascades and in the Okanogan Highlands–but no change in coarse woody debris biomass, or possibly even an increase, because coarse woody debris biomass increases as trees are killed by fire and subsequent low-severity fires burn only a small portion of it.

“Changes in fire regimes in a warming climate can limit our potential to use forests in the Pacific Northwest to store additional carbon and to reduce atmospheric carbon dioxide,” Raymond said.

Understanding the possible effects of more area burned by fire can help managers decide whether forests need to be actively managed for their fire potential to minimize carbon loss.

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Source: USDA Forest Service - Pacific Northwest Research Station