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Energy input is primary controller of methane bubbling in subarctic lakes
Stockholm University, Sweden .
Stockholm University, Sweden .
Linköping University, The Tema Institute, Department of Water and Environmental Studies. Linköping University, Faculty of Arts and Sciences.
University of California, Santa Barbara, USA.
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2014 (English)In: Geophysical Research Letters, ISSN 0094-8276, Vol. 41, no 2, 555-560 p.Article in journal (Refereed) Published
Abstract [en]

Emission of methane (CH4) from surface waters is often dominated by ebullition (bubbling), a transport mode with high-spatiotemporal variability. Based on new and extensive CH4 ebullition data, we demonstrate striking correlations (r(2) between 0.92 and 0.997) when comparing seasonal bubble CH4 flux from three shallow subarctic lakes to four readily measurable proxies of incoming energy flux and daily flux magnitudes to surface sediment temperature (r(2) between 0.86 and 0.94). Our results after continuous multiyear sampling suggest that CH4 ebullition is a predictable process, and that heat flux into the lakes is the dominant driver of gas production and release. Future changes in the energy received by lakes and ponds due to shorter ice-covered seasons will predictably alter the ebullitive CH4 flux from freshwater systems across northern landscapes. This finding is critical for our understanding of the dynamics of radiatively important trace gas sources and associated climate feedback.

Place, publisher, year, edition, pages
Wiley-Blackwell, 2014. Vol. 41, no 2, 555-560 p.
Keyword [en]
methane; ebullition; energy flux; subarctic lakes
National Category
Natural Sciences
URN: urn:nbn:se:liu:diva-106297DOI: 10.1002/2013GL058510ISI: 000332991000051OAI: diva2:715716
Available from: 2014-05-06 Created: 2014-05-05 Last updated: 2015-03-12Bibliographically approved

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Bastviken, David
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Department of Water and Environmental StudiesFaculty of Arts and Sciences
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