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Rob Gutro
Goddard Space Flight Center, Greenbelt, Md.
(Phone: 301/286-4044)

Barbra Rodriguez
The University of Texas at Austin
(Phone: 512/232-0675)

The Boreal Ecosystem-Atmosphere Study (BOREAS)

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The BOREAS-follow on Project to determine how carbon storage in boreal forests change in response to wildfire was set in the northern edge of the Canadian boreal forest in Manitoba, Canada, the former Northern Study Area (NSA) in Thompson Manitoba from BOREAS. CREDIT: Canadian Model Forest Program


Litvak and her colleagues used instruments positioned at various heights on towers like these one to measure how the transfer of carbon dioxide between the forest and the atmosphere changes with forest age. The towers also measured the transfer of heat and moisture and radiation. CREDIT: Marcy Litvak, University of Texas at Austin; Michael Goulden, University of California, Irvine

Caption for Image 4:

Scientists during the BOREAS follow-up project used probes like the one pictured below to measure the amount of carbon released from the forest tree trunks into the atmosphere. They also monitored air temperature and stem temperature to better understand factors that influence carbon exchange. Once the processes are understood, computer models can be developed that can predict future change. CREDIT: Marcy Litvak, University of Texas at Austin

Caption for Image 5: THE BOREAL FOREST AREA

The Boreal forest, rich in diversity of vegetation and wildlife, covers over one-tenth of the Earth's northern land surface, including one-third of Canada. Boreal forest (depicted in green) covers approximately 28% of the North American continent, north of Mexico. Today's boreal forests comprise 8% of global forestland.CREDIT: BOREAS project (From Hare and Ritchie (1972))

Caption for Image 6: NORTHERN STUDY AREA

This satellite image of the Northern Study Area, Manitoba, Canada was taken by the Landsat satellite on July 25, 1990. The bodies of water can be seen in blue. The landscape is a mosaic of different aged stands that are in various stages of recovery from wildfire. Each of the colored patches corresponds to a different aged stand. The years corresponding to the areas indicate the last year of forest fire. CREDIT: NASA/USGS

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March 21, 2003 - (date of web publication)



Canadian forest map

Image 1


Scientists studying trees ranging from saplings to 130 years old in Canada’s northern forests have discovered that the period since a fire last swept through an area determines how much carbon the forest can store. Twenty to forty year old stands absorb more carbon than those 70 years old and older, despite being smaller and having less biomass or plant material.

Boreal or northern forests account for close to 25 percent of total carbon stored in vegetation and soils in the Earth’s biosphere. Wildfires burn down individual areas every 40 to 250 years and are an important part of this ecosystem. Whether or not these forests are likely to lower or raise levels of carbon dioxide in the atmosphere depends on how these carbon reserves respond to, and recover from, both climate change and disturbances such as wildfires.



Images 2 and 3


NASA funded part of this study under its Earth Science Enterprise (ESE), whose mission is to understand and protect our home planet. Earth Science in NASA seeks to understand trends in land cover and land use, such as forest fires, that drive global climate. Another Earth Science program objective is to understand the Earth system’s response to natural and human-induced changes, and effects on global carbon cycle.

Marcy Litvak, plant ecologist at the University of Texas at Austin and lead author of the study that appeared in a recent issue of the Journal of Geophysical Research -
Atmospheres, said that the ability of tree stands to store carbon changes as they regenerate from fire. Forests will store more or less carbon depending on the dominant tree species, the amount of moss cover, and changes in forest structure due to fire. Those factors determine how much total carbon is exchanged with the atmosphere.


Image of a probe which measures the amount of carbon released from the forest tree trunks into the atmosphere.

Image 4


Carbon is transferred from the atmosphere to the forest through the process of photosynthesis. Carbon is returned to the atmosphere through the process of respiration as soil microorganisms decompose dead organic matter, and trees and mosses metabolize the products of photosynthesis. It is the balance between these two processes, taking in carbon during photosynthesis and "exhaling" carbon through respiration, that determines how much carbon is stored in the forest.

Between 1999-2000, Litvak and her colleagues, Scott Miller and Michael Goulden of the University of California, Irvine, and Steve Wofsy of Harvard University, used solar-powered anemometers and infrared gas analyzers mounted on towers to monitor carbon emissions over five black spruce stands in Manitoba, Canada. These stands ranged in age from 11 to 130 years old. Results indicate that the ability to store carbon is almost zero in the 11 year-old stand, increases to a maximum in the 36 year-old stand, then gradually falls back down to zero in the 130-year old stand. They concluded that most of the net carbon absorption appears to take place from 20-50 years after a fire.


The Boreal forest, rich in diversity of vegetation and wildlife, covers over one-tenth of the Earth's northern land surface, including one-third of Canada

Image 5


"Seedlings of Aspen, Jack Pine, and Black Spruce all regenerate simultaneously following wildfire in areas once dominated by mature black spruce forests in this region of Manitoba.    Aspen and Jack Pine tend to dominate in young stands where light is not limited. Black Spruce grow the slowest, but eventually out-compete the Aspen and Jack Pine by blocking the sunlight available to these species. By 70 years following a burn, these forests are dominated by Black Spruce once again," Litvak said.

Stands less than 20 years old store less carbon than older trees because they lack sufficient leaf area for rapid carbon accumulation. Carbon storage is highest in stands 20-50 years old that are dominated by rapidly growing aspen trees that take up carbon at higher rates than black spruce and jack pine trees.


This satellite image of the Northern Study Area, Manitoba, Canada was taken by the Landsat satellite on July 25, 1990.

Image 6


"Stands [of trees] older than 70 years are dominated by black spruce trees and thick moss cover that ‘exhale and inhale’ equal amounts of carbon. That means stands older than 70 years are in near carbon balance with the atmosphere," she said.

Knowing the rate at which trees respire will help scientists to better estimate the trees' contributions to the global carbon cycle. This is especially important because of the changing climate. "Increased fire frequency, as predicted from global warming scenarios, has the potential to significantly impact the contribution boreal forests make to the global carbon cycle," Miller said.

NASA data from the Boreal Ecosystem-Atmosphere Study (BOREAS) was also used in the study. BOREAS was a large-scale international experiment in the northern forests of Canada between 1993 and 1996, whose goal was to improve understanding of interactions between the boreal forest and the atmosphere, and clarify their roles in global change.

This work was supported by NASA, the National Science Foundation, and U.S. Department of Energy.

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