Impact of atmospheric pressure variations on methane ebullition and lake turbidity during ice‐cover

Methane ebullition (bubbling) from lake sediments is an important methane flux into the atmosphere. Previous studies have focused on the open‐water season, showing that temperature variations, pressure fluctuations, and wind‐induced currents can affect ebullition. However, ebullition surveys during...

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Bibliographic Details
Published in:Limnology and oceanography letters Vol. 6; no. 5; pp. 253 - 261
Main Authors: Zhao, Kai, Tedford, Edmund W., Zare, Marjan, Lawrence, Gregory A.
Format: Journal Article
Language:English
Published: Hoboken, USA John Wiley & Sons, Inc 01-10-2021
Wiley
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Summary:Methane ebullition (bubbling) from lake sediments is an important methane flux into the atmosphere. Previous studies have focused on the open‐water season, showing that temperature variations, pressure fluctuations, and wind‐induced currents can affect ebullition. However, ebullition surveys during the ice‐cover are rare despite the prevalence of seasonally ice‐covered lakes, and the factors controlling ebullition are poorly understood. Here, we present a month‐long, high frequency record of acoustic ebullition data from an ice‐covered lake. The record shows that ebullition occurs almost exclusively when atmospheric pressure drops below a threshold that is approximately equal to the long‐term average pressure. The intensity of ebullition is proportional to the amount by which the pressure drops below this threshold. In addition, field measurements of turbidity, in conjunction with laboratory experiments, provide evidence that ebullition is responsible for previously unexplained elevated levels of turbidity during ice‐cover.
Bibliography:Associate editor
Data Availability Statement
https://datadryad.org/stash/share/45pLzeJmUwiAdM5P78iR_AqthtjgClZNXN9USJUF8U8
Stephen Monismith
The manuscript was written through contributions of all authors. K.Z., G.A.L., and E.W.T. designed the study. K.Z. did the data analysis, conducted laboratory experiments, and wrote the manuscript with extensive discussions with E.W.T. and G.A.L. E.W.T. led the field data collection and M.Z. led the laboratory experiment. G.A.L. and E.W.T. made extensive revisions of the manuscript and M.Z. provided feedback on the revision.
Data and metadata are available in Dryad repository at
Author Contribution Statement
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ISSN:2378-2242
2378-2242
DOI:10.1002/lol2.10201