Articles | Volume 11, issue 23
https://doi.org/10.5194/bg-11-6791-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/bg-11-6791-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Modeling the impediment of methane ebullition bubbles by seasonal lake ice
S. Greene
Department of Chemistry, the University of Chicago, Chicago, Illinois, USA
K. M. Walter Anthony
CORRESPONDING AUTHOR
Water and Environmental Research Center, Institute of Northern Engineering,University of Alaska Fairbanks, Fairbanks, Alaska, USA
D. Archer
Department of the Geophysical Sciences, the University of Chicago, Chicago, Illinois, USA
A. Sepulveda-Jauregui
Water and Environmental Research Center, Institute of Northern Engineering,University of Alaska Fairbanks, Fairbanks, Alaska, USA
K. Martinez-Cruz
Biotechnology and Bioengineering Department, Cinvestav, Mexico City, D. F., Mexico
Water and Environmental Research Center, Institute of Northern Engineering,University of Alaska Fairbanks, Fairbanks, Alaska, USA
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Latest update: 15 Aug 2024
Short summary
Methane (CH4) bubbles emitted from the anoxic sediments of northern lakes constitute a significant methane flux to the atmosphere, but entrapment by seasonal lake ice impedes bubble release to the atmosphere. Using numerical modeling and field measurement of a lake in Alaska, we found that 80% of CH4 in ice-trapped bubbles dissolves into the water column. Microbes consume half of that CH4. Emission by bubbling is greatest in summer but continues in winter through some open holes in lake ice.
Methane (CH4) bubbles emitted from the anoxic sediments of northern lakes constitute a...
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