LARGE
VOLCANIC ERUPTIONS HELP PLANTS ABSORB MORE CARBON
DIOXIDE FROM THE ATMOSPHERE
New
NASA-funded research shows that when the atmosphere
gets hazy, like it did after the eruption of Mt.
Pinatubo in the Philippines in June 1991, plants
photosynthesize more efficiently, thereby absorbing
more carbon dioxide from the atmosphere.
When Mount
Pinatubo erupted, scientists noticed the rate at
which carbon dioxide (CO2) filled the atmosphere
slowed down for the next two years. Also during
1992 and 1993, ash and other particles from the
volcano created a haze around the planet and
slightly reduced the sunlight reaching Earth's
surface and made the sun's radiation less direct
and more diffuse.
Many
scientists previously thought the reduction in
sunlight lowered the Earth's temperature and slowed
plant and soil respiration, a process where plants
and soil emit CO2. But this new research shows that
when faced with diffuse sunlight, plants actually
become more efficient, drawing more carbon dioxide
out of the air.
"There is
evidence indicating that the drop in the
atmospheric CO2 growth rate was probably too big to
be explained by a reduction in respiration alone,"
said the study's lead author, Lianhong Gu, a
researcher at the University of California
Berkeley's Department of Environmental Science,
Policy and Management.
Gu added that
the respiration rates of plants and soil are
sensitive to temperature changes. But "in order to
explain the drop in atmospheric growth rate of CO2,
we would need an average drop in global
temperatures of about 3.6 degrees Fahrenheit (2°
C), but the temperatures only dropped by about one
degree (0.9) Fahrenheit (0.5°C) globally."
Plants take in
carbon dioxide during photosynthesis in the day,
and release it during respiration at night. But
they don't necessarily photosynthesize and respire
at the same rates. Since decreased plant and soil
respiration could not explain the drop in carbon
dioxide entering the atmosphere in 1992 and 1993,
Gu and his colleagues deduced that enhanced
photosynthesis by plants must be involved.
[Karl
Note: Why couldn't they simply look at the
millions of tons of rock dust that flew around the
planet -- providing the needed trace minerals for
the depleted soil? Why?]
After Mount
Pinatubo erupted, while overall solar radiation was
reduced by less than five percent, data showed a
reduction of direct radiation by as much as 30
percent. So, instead of direct light, the sun's
rays were reaching leaves after colliding with
particles in the air.
"Diffuse
radiation has advantages for plants," Gu said.
That's because when plants receive too much direct
light, they become saturated by radiation and their
ability to photosynthesize levels off. In the
layers of leaves from top to bottom, called the
plant canopy, only a small percentage of the leaves
at the top actually get hit by direct light. In the
presence of diffuse light, plants photosynthesize
more efficiently and can draw more than twice as
much carbon from the air than when radiated by
direct light.
Gu and his
colleagues tested the CO2 uptake in various plant
ecosystems around the world-including Aspen
forests, mixed deciduous forests, Scots pine
forests, tallgrass prairies, and a winter wheat
field-based on the amount of solar radiation
striking the leaves. From these analyses, they
generated parameters necessary for evaluating
impacts of the Pinatubo eruption. On clear days
following the eruption, they found that in all of
the ecosystems, photosynthesis increased under the
diffuse light.
While large
volcanic eruptions are rare, this research has big
implications for
more regular phenomena such as the effects of
aerosols and clouds on an ecosystem's ability to
pull carbon from the atmosphere. Aerosols, or
microscopic particles like soot or black carbon in
the air, occur naturally but have also been
increasing due to human activities since the
industrial revolution. Gu's research indicates that
the maximum uptake of carbon dioxide by plant
ecosystems occurs when cloud cover is about 50
percent.
The research
will be presented at a poster session of the
American Geophysical Union (AGU) Fall Meeting in
San Francisco, Calif. on December 14, 2001. A paper
will be published soon in the Journal of
Geophysical Research.
Aside from
NASA, the study was also funded by the National
Oceanic and Atmospheric Administration (NOAA), the
Department of Energy, and other organizations,
through the FLUXNET program. |