Variability of Marine Methane Bubble Emissions on the Clayoquot Slope, Offshore Vancouver Island, Between 2017 and 2021
Seabed methane gas emissions occur worldwide at cold seeps located along most continental margins. Fluxes of methane gas released from the seabed in the form of bubbles can be extremely variable even over short time intervals. Some factors controlling the variability are still poorly understood. Her...
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| Format: | Article |
| Language: | English |
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Frontiers Media S.A.
2022-03-01
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| Series: | Frontiers in Earth Science |
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| Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2022.864809/full |
| _version_ | 1818285283762765824 |
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| author | Yann Marcon Miriam Römer Martin Scherwath Michael Riedel Knut Ola Dølven Martin Heesemann |
| author_facet | Yann Marcon Miriam Römer Martin Scherwath Michael Riedel Knut Ola Dølven Martin Heesemann |
| author_sort | Yann Marcon |
| collection | DOAJ |
| description | Seabed methane gas emissions occur worldwide at cold seeps located along most continental margins. Fluxes of methane gas released from the seabed in the form of bubbles can be extremely variable even over short time intervals. Some factors controlling the variability are still poorly understood. Here, we report on the results of continuous long-term sonar monitoring of bubble emissions at a depth of 1,260 m on the Clayoquot Slope, northern Cascadia margin. With a total monitoring duration of 4 years and a sampling period of 1 h, this is by far the longest high temporal resolution monitoring of seabed methane gas release ever conducted. Our results provide evidence that the diurnal and semi-diurnal tides influence the timing of the onset and cessation of bubble emissions. However, gas emissions within the monitoring area are active more than 84% of the time, indicating that tides alone are not sufficient to make venting pause. We hypothesize that the gas fluxes are transient but generally sufficiently high to maintain ebullition independently of the tidally-induced bottom pressure variations. Results also show that the tides do not seem to modulate the vigor of active gas emissions. |
| first_indexed | 2024-12-13T01:06:15Z |
| format | Article |
| id | doaj.art-2f76a8f4092f44d787388e69ad09c9f1 |
| institution | Directory Open Access Journal |
| issn | 2296-6463 |
| language | English |
| last_indexed | 2024-12-13T01:06:15Z |
| publishDate | 2022-03-01 |
| publisher | Frontiers Media S.A. |
| record_format | Article |
| series | Frontiers in Earth Science |
| spelling | doaj.art-2f76a8f4092f44d787388e69ad09c9f12022-12-22T00:04:32ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632022-03-011010.3389/feart.2022.864809864809Variability of Marine Methane Bubble Emissions on the Clayoquot Slope, Offshore Vancouver Island, Between 2017 and 2021Yann Marcon0Miriam Römer1Martin Scherwath2Michael Riedel3Knut Ola Dølven4Martin Heesemann5MARUM Center for Marine Environmental Research and Department of Geosciences, University of Bremen, Bremen, GermanyMARUM Center for Marine Environmental Research and Department of Geosciences, University of Bremen, Bremen, GermanyOcean Networks Canada, University of Victoria, Victoria, BC, CanadaGEOMAR Helmholtz Centre for Ocean Research, Kiel, GermanyCentre for Arctic Gas Hydrate, Environment and Climate, UiT The Arctic University of Norway, Tromsø, NorwayOcean Networks Canada, University of Victoria, Victoria, BC, CanadaSeabed methane gas emissions occur worldwide at cold seeps located along most continental margins. Fluxes of methane gas released from the seabed in the form of bubbles can be extremely variable even over short time intervals. Some factors controlling the variability are still poorly understood. Here, we report on the results of continuous long-term sonar monitoring of bubble emissions at a depth of 1,260 m on the Clayoquot Slope, northern Cascadia margin. With a total monitoring duration of 4 years and a sampling period of 1 h, this is by far the longest high temporal resolution monitoring of seabed methane gas release ever conducted. Our results provide evidence that the diurnal and semi-diurnal tides influence the timing of the onset and cessation of bubble emissions. However, gas emissions within the monitoring area are active more than 84% of the time, indicating that tides alone are not sufficient to make venting pause. We hypothesize that the gas fluxes are transient but generally sufficiently high to maintain ebullition independently of the tidally-induced bottom pressure variations. Results also show that the tides do not seem to modulate the vigor of active gas emissions.https://www.frontiersin.org/articles/10.3389/feart.2022.864809/fullmethanegas emissionsseepbubble plumecascadia marginmultibeam |
| spellingShingle | Yann Marcon Miriam Römer Martin Scherwath Michael Riedel Knut Ola Dølven Martin Heesemann Variability of Marine Methane Bubble Emissions on the Clayoquot Slope, Offshore Vancouver Island, Between 2017 and 2021 Frontiers in Earth Science methane gas emissions seep bubble plume cascadia margin multibeam |
| title | Variability of Marine Methane Bubble Emissions on the Clayoquot Slope, Offshore Vancouver Island, Between 2017 and 2021 |
| title_full | Variability of Marine Methane Bubble Emissions on the Clayoquot Slope, Offshore Vancouver Island, Between 2017 and 2021 |
| title_fullStr | Variability of Marine Methane Bubble Emissions on the Clayoquot Slope, Offshore Vancouver Island, Between 2017 and 2021 |
| title_full_unstemmed | Variability of Marine Methane Bubble Emissions on the Clayoquot Slope, Offshore Vancouver Island, Between 2017 and 2021 |
| title_short | Variability of Marine Methane Bubble Emissions on the Clayoquot Slope, Offshore Vancouver Island, Between 2017 and 2021 |
| title_sort | variability of marine methane bubble emissions on the clayoquot slope offshore vancouver island between 2017 and 2021 |
| topic | methane gas emissions seep bubble plume cascadia margin multibeam |
| url | https://www.frontiersin.org/articles/10.3389/feart.2022.864809/full |
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