News Release 04-056
Arctic Carbon a Potential Wild Card in Climate Change Scenarios
April 20, 2004
This material is available primarily for archival purposes. Telephone numbers or other contact information may be out of date; please see current contact information at media contacts.
ARLINGTON, Va.—The Arctic Ocean receives about 10 percent of Earth's river water and with it some 25 teragrams [28 million tons] per year of dissolved organic carbon that had been held in far northern bogs and other soils.
Now an international team of U.S. and German scientists, including some funded by the National Science Foundation, have used carbon-14 dating techniques to determine that most of that carbon is fairly young and not likely to affect the balance of global climate.
They reported their findings in the March issue of Geophysical Research Letters, a publication of the American Geophysical Union.
Although the current carbon load does not seem likely to affect global climate significantly, they caution in their report that a well-documented Arctic warming trend could result in ancient carbon—a reservoir of the gas currently locked into peat bogs—being added to the mix and contributing to the well- documented Arctic warming trend.
"If current warming trends in the Arctic continue, we can expect to see more of the old carbon now sequestered in northern soils enter the carbon cycle as carbon dioxide. This will act as a positive feedback, tending to enhance the greenhouse effect and accelerate global warming," said Ronald Benner, an NSF-funded researcher at the University of South Carolina.
NSF is an independent federal agency that supports fundamental research and education across all fields of science and engineering, with an annual budget of nearly $5.58 billion. National Science Foundation funds reach all 50 states through grants to nearly 2,000 universities and institutions.
The team studied rivers in northern Russia and Alaska, along with the Arctic Ocean itself. Benner conducted some of his research as part of the Western Shelf-Basin Interactions research project, which is jointly funded by NSF and the U.S. Office of Naval Research.
Previously, scientists had not known the age of the carbon that reaches the ocean. Was it recently derived from contemporary plant material, or had it been locked in soils for hundreds or thousands of years and therefore not part of Earth's recent carbon cycle?
The new findings complement recently published work by Laurence C. Smith, an NSF-funded researcher at the University of California, Los Angeles, indicating that massive Siberian peat bogs, widely known as the permanently frozen home of untold kilometers of moss and uncountable hordes of mosquitoes, also are huge repositories for gases that are thought to play an important role in the Earth's climate balance.
Those gases, carbon dioxide and methane, are known to trap heat in the Earth's atmosphere, but the enormous amounts of the gases contained in the bogs haven't previously been accounted for in climate-change models.
The full story of that finding is here: http://www.nsf.gov/od/lpa/newsroom/pr.cfm?ni=36
To read an abstract of the full article in Geophysical Research Letters, see: http://www.agu.org/pubs/crossref/2004.../2003GLO19251.shtml
To read the full text of the AGU news release, see: http://www.agu.org/ sci_soc/prrl/prrl0412.html/.
What the researchers say:
"Many scientists are wondering whether current warming trends in the Arctic will pick the lock on aged soil carbon and release this material back into the active carbon cycle and the atmosphere. Our results suggest this hasn't happened yet, but we need to monitor this situation closely using multiple approaches."—Ronald Benner, principal investigator.
NSF comments regarding the research discovery:
"Identifying the fate of carbon compounds mobilized from the vast areas of frozen wetlands in the Arctic will be a critical step in understanding the Arctic system and how it will respond to the climatic forces acting upon it. How much carbon goes to the ocean, and how much to the atmosphere and in what form, are key questions we need to answer in order to see the directions the future holds for us."—Nell Swanberg, director of NSF's Arctic System Science(ARCSS) Program.
-NSF-
Images/B-Roll: For b-roll of scientists studying the Arctic carbon cycle as part of the NSF-funded Western Shelf-Basin Interactions project and of freshwater streams in Greenland, please contact Dena Headlee, (703) 292-7739, dheadlee@nsf.gov
Still images from the Western Shelf-Basin Interactions project are available at print resolution from the NSF media officer listed above.
Ronald Benner, University of South Carolina, (803) 777-9561, benner@biol.sc.edu
Jackie Grebmeier, University of Tennessee, (865) 974-2592, jgrebmei@utk.edu
Laurence C. Smith, University of California, Los Angeles (310) 825-3154, Ismith@qeoq.ucla.edu
For more information about the Western Shelf-Basin Interactions project, see: http://sbi.utk.edu
Media Contacts
Peter West, NSF, (703) 292-7761, email: pwest@nsf.gov
Harvey Leifert, AGU, (202) 777-7507, email: hleifert@agu.org
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