A new $26-million NASA project led by a University of
Michigan researcher aims to help clarify how ecosystems exchange
carbon with the atmosphere, an important piece of missing
knowledge in the quest to understand, predict, and adapt to
climate change.
The project’s goal is to provide crucial missing information
that will help determine whether the North American continent is
a net source or sink of carbon. Researchers from U-M, NASA’s Jet
Propulsion Laboratory, Harvard University, MIT, Oregon State
University, NASA’s Goddard Space Flight Center, the U.S.
Department of Agriculture, and Purdue University are taking
part.
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The AirMOSS radar will be packaged in a small pod
(bottom left) carried by a Gulfstream aircraft (top
left). On the right, a possible pod layout is shown
with the electronics bay and location of the electronics
subsystems. The antenna would be on the back side of
the electronics bay. Credit: NASA Jet Propulsion
Laboratory. |
Over the next five years, a radar instrument called the
Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS)
will collect data in nine North American regions from aboard a
Gulfstream-III aircraft. The radar data will be converted to
measurements of soil moisture by using sophisticated computer
simulations. The radar, to be built during the first
year-and-a-half of the project, generates signals that can
penetrate up to four feet beneath the ground surface. This
state-of-the-art low-frequency radar will be the most compact
and versatile radar of its kind built to-date, says principal
investigator Mahta Moghaddam, a professor in the Department of
Electrical Engineering and Computer Science.
Root-zone soil moisture levels directly affect how well a
plant is functioning.
“Even your houseplant has its own net exchange of carbon,”
Moghaddam said. “It takes carbon dioxide in during the day
through photosynthesis, provided there is sunlight and it’s warm
enough. And breathes out some carbon dioxide at night. How much
net carbon it sequesters, and therefore how much the plant
grows, has to do with how much water is available to its roots:
No water, no growth.”
Scientists don’t understand exactly when and where this net
carbon exchange process is most efficient, or how much the net
exchange differs across ecosystems. They might know it for a few
selected locations across North America where they have manually
sampled, but not on the large scale that AirMOSS will enable.
Lack of current knowledge about root zone soil moisture is
believed to contribute 60-80 percent of the uncertainty about
how much the ecosystems exchange carbon with the atmosphere.
Collaborating researchers will incorporate Moghaddam’s root
zone soil moisture measurements into hydrology and ecosystem
models to produce a continental estimate of the net ecosystem
exchange. The results, which will show whether the continent
takes in or releases more carbon and by how much, are expected
by May 2015.
Moghaddam will oversee the design and fabrication of the
AirMOSS instrument, a table-top-sized, high-powered,
low-frequency radar that NASA/JPL collaborators will build for
the project. She has also developed computational techniques to
analyze the signals it sends back. Moghaddam’s research group is
a leader in developing radar algorithms for subsurface
characterization.
“This work will help us understand a piece of the carbon
cycle puzzle,” Moghaddam said. “We may know that different areas
in north America act as sinks or sources of carbon, but we don’t
know how large the net carbon exchange is, how fast it’s
changing, or how big it’s going to get. Today, we rely on model
estimates and there is huge uncertainty.”
Beyond this project, Moghaddam envisions other applications
for this radar instrument, including surveillance and resource
exploration.
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