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Scientists Measure "Breathing" Of The Biosphere
SISTERS, OR (AP) - In the ponderosa pine forest near Black Butte, a skinny scaffolding
tower rises above the trees.
From the top of the 100-foot-tall tower, the panoramic views of the butte
and Three Sisters in the distance are some of the best in the area. But the
instruments
attached along the span of the tower are providing scientists with information
about an unseen side of nature.
The equipment measures how much carbon dioxide is passing back and forth
between the atmosphere and the trees, shrubs, soils and dead vegetation in
the forest.
It’s one station in a nationwide network that, when the data is compiled,
helps scientists investigate how much carbon dioxide forests across the continent
remove from the atmosphere every year.
And in this era of concern about global warming, it’s information that
interests researchers and forest managers alike.
For instance, the information from stations in Oregon has shown that forests
take in the equivalent of between 30 percent and 50 percent of carbon released
statewide annually in fossil fuel emissions.
And through measuring this carbon exchange in the Metolius Basin and other
types of forests, Bev Law and others hope to understand more about their role.
“
We call it the breathing of the biosphere,” said Law, a professor at
Oregon State University in Corvallis and the science chairwoman for AmeriFlux,
the network
of more than 100 such carbon measuring sites across the United States and other
countries.
Through their studies, the researchers can figure out when forests start
acting as a storage site for carbon dioxide, a greenhouse gas, and how much
of that
gas is released into the atmosphere when forests burn or are cut down.
“
The goal of the program is to be able to quantify and understand the role of
terrestrial ecosystems in the global carbon balance,” Law said.
The Metolius Basin was the site of one of the first stations in the AmeriFlux
program, which started in 1996.
Law, who had previously done work across Oregon, chose the site because of
its ponderosa pines.
“
We were intrigued by ponderosa pine because it’s very widely distributed
globally, so it’s an important species,” she said, mentioning that
the trees are found in places as diverse as Arizona and southern Europe.
And by placing these towers and instruments near the Metolius, Law and her
colleagues have been able to determine differences between young and old forests,
between
wet and dry years, and also contribute to regional studies of the movements
of carbon dioxide.
The instruments collect information about the precise levels of carbon dioxide
in the air, recording measurements as frequently as 20 times a second. But
the equipment on the tower gathers other kinds of information as well.
The researchers are studying water vapor as well to see how it relates to
carbon dioxide levels, Law said, and are looking at different layers of wind
speeds
and temperatures through the forest canopy.
Wind speed is also measured because it can affect how much carbon dioxide
can be picked up by the instruments, said Christoph Thomas, a research associate
with OSU who works on the project.
From all this information, researchers can get results about how much carbon
the forest is absorbing or releasing.
Trees absorb carbon through photosynthesis, Law said, but they also release
it through respiration.
And then there’s the rest of the organic matter in the forest, like soil,
roots and vegetative litter that’s being chewed up by microbes, which
people sometimes forget about when they think of carbon cycles in forests,
she said.
“
There’s a lot of focus on the trees, but they’re not thinking about
the other stuff that’s in there,” Law said.
And all this other stuff releases a large amount of carbon dioxide. The researchers
found, for instance, that at the Metolius site about 70 percent of the carbon
dioxide released into the atmosphere was from the soil.
“
It’s just the cost of doing business,” for the forest, she said.
They also found that in dry years, the forests took in less carbon than they
did in wet years.
One question that scientists had been considering, she said, was how long
it takes a new forest to go from being a carbon source, where it releases more
carbon to the atmosphere than it takes in, to being a carbon sink, where the
ecosystem
absorbs more carbon than it releases.
And through studies at the Metolius site, Law and her colleagues have found
that in a ponderosa pine forest that has been disturbed by fire or harvest,
it can
take a while.
“
It took those sites somewhere between 15 and 20 years before they became carbon
neutral again,” she said.
From there, forests continue taking in increasing amounts of carbon until
they’re
between about 70 and 150 years old, Thomas said. At that point, they still
store more carbon than they release.
But that doesn’t mean older forests are no longer useful for storing
carbon.
“
People need to understand that these old-growth forests are very important,” Thomas
said.
Studies in both Western and Eastern Oregon have shown that after a major
disturbance in a mature forest, like a catastrophic fire or a clearcut, it
could take between
100 and 200 years to get back the amount of carbon that had previously been
stored in the ecosystem, Law said.
Information like this can be useful on multiple levels, Thomas said. It answers
some scientific curiosity, about things like what happens in forests that are
different ages.
But when information from across the AmeriFlux network is compiled, it can
also be used to help answer larger-scale questions, he said, such as how much
carbon
dioxide forests across the continent remove from the atmosphere every year.
Determining when carbon is stored in trees and how much is stored there,
is a complex question, said Brian Tandy, silviculturist with the Sisters Ranger
District.
But it’s something that people could start thinking about, he said, adding
that he recently had a conversation about the possibility of setting up a carbon
credit program, where people could reforest areas and get a credit for the
carbon that would be absorbed by the trees in future years.
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