Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica
Persistently active lava lakes show continuous outgassing and open convection over years to decades. Ray Lake, the lava lake at Mount Erebus, Ross Island, Antarctica, maintains long-term, near steady-state behavior in temperature, heat flux, gas flux, lake level, and composition. This activity is su...
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ftdatacite:10.48550/arxiv.1907.02899 2023-05-15T14:05:09+02:00 Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica Birnbaum, Janine Keller, Tobias Suckale, Jenny Lev, Einat 2019 https://dx.doi.org/10.48550/arxiv.1907.02899 https://arxiv.org/abs/1907.02899 unknown arXiv https://dx.doi.org/10.1016/j.epsl.2019.115903 arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Geophysics physics.geo-ph Fluid Dynamics physics.flu-dyn FOS Physical sciences article-journal Article ScholarlyArticle Text 2019 ftdatacite https://doi.org/10.48550/arxiv.1907.02899 https://doi.org/10.1016/j.epsl.2019.115903 2022-03-10T16:43:29Z Persistently active lava lakes show continuous outgassing and open convection over years to decades. Ray Lake, the lava lake at Mount Erebus, Ross Island, Antarctica, maintains long-term, near steady-state behavior in temperature, heat flux, gas flux, lake level, and composition. This activity is superposed by periodic small pulses of gas and hot magma every 5-18 minutes and disrupted by sporadic Strombolian eruptions. The periodic pulses have been attributed to a variety of potential processes including unstable bidirectional flow in the conduit feeding the lake. In contrast to hypotheses invoking a conduit source for the observed periodicity, we test the hypothesis that the behavior could be the result of dynamics within the lake itself, independent of periodic influx from the conduit. We perform numerical simulations of convection in Ray Lake driven by both constant and periodic inflow of gas-rich magma from the conduit to identify whether the two cases have different observational signatures at the surface. Our simulations show dripping diapirs or pulsing plumes leading to observable surface behavior with periodicities in the range of 5-20 minutes. We conclude that a convective speed faster than the inflow speed can result in periodic behavior without requiring periodicity in conduit dynamics. This finding suggests that the surface behavior of lava lakes might be less indicative of volcanic conduit processes in persistently outgassing volcanoes than previously thought, and that dynamics within the lava lake itself may modify or overprint patterns emerging from the conduit. Article in Journal/Newspaper Antarc* Antarctica Ross Island DataCite Metadata Store (German National Library of Science and Technology) Ross Island Lava Lake ENVELOPE(-128.996,-128.996,55.046,55.046) Mount Erebus ENVELOPE(167.167,167.167,-77.533,-77.533) Lava Lakes ENVELOPE(-130.904,-130.904,56.433,56.433) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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topic |
Geophysics physics.geo-ph Fluid Dynamics physics.flu-dyn FOS Physical sciences |
spellingShingle |
Geophysics physics.geo-ph Fluid Dynamics physics.flu-dyn FOS Physical sciences Birnbaum, Janine Keller, Tobias Suckale, Jenny Lev, Einat Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica |
topic_facet |
Geophysics physics.geo-ph Fluid Dynamics physics.flu-dyn FOS Physical sciences |
description |
Persistently active lava lakes show continuous outgassing and open convection over years to decades. Ray Lake, the lava lake at Mount Erebus, Ross Island, Antarctica, maintains long-term, near steady-state behavior in temperature, heat flux, gas flux, lake level, and composition. This activity is superposed by periodic small pulses of gas and hot magma every 5-18 minutes and disrupted by sporadic Strombolian eruptions. The periodic pulses have been attributed to a variety of potential processes including unstable bidirectional flow in the conduit feeding the lake. In contrast to hypotheses invoking a conduit source for the observed periodicity, we test the hypothesis that the behavior could be the result of dynamics within the lake itself, independent of periodic influx from the conduit. We perform numerical simulations of convection in Ray Lake driven by both constant and periodic inflow of gas-rich magma from the conduit to identify whether the two cases have different observational signatures at the surface. Our simulations show dripping diapirs or pulsing plumes leading to observable surface behavior with periodicities in the range of 5-20 minutes. We conclude that a convective speed faster than the inflow speed can result in periodic behavior without requiring periodicity in conduit dynamics. This finding suggests that the surface behavior of lava lakes might be less indicative of volcanic conduit processes in persistently outgassing volcanoes than previously thought, and that dynamics within the lava lake itself may modify or overprint patterns emerging from the conduit. |
format |
Article in Journal/Newspaper |
author |
Birnbaum, Janine Keller, Tobias Suckale, Jenny Lev, Einat |
author_facet |
Birnbaum, Janine Keller, Tobias Suckale, Jenny Lev, Einat |
author_sort |
Birnbaum, Janine |
title |
Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica |
title_short |
Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica |
title_full |
Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica |
title_fullStr |
Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica |
title_full_unstemmed |
Periodic outgassing as a result of unsteady convection in Ray Lava Lake, Mount Erebus, Antarctica |
title_sort |
periodic outgassing as a result of unsteady convection in ray lava lake, mount erebus, antarctica |
publisher |
arXiv |
publishDate |
2019 |
url |
https://dx.doi.org/10.48550/arxiv.1907.02899 https://arxiv.org/abs/1907.02899 |
long_lat |
ENVELOPE(-128.996,-128.996,55.046,55.046) ENVELOPE(167.167,167.167,-77.533,-77.533) ENVELOPE(-130.904,-130.904,56.433,56.433) |
geographic |
Ross Island Lava Lake Mount Erebus Lava Lakes |
geographic_facet |
Ross Island Lava Lake Mount Erebus Lava Lakes |
genre |
Antarc* Antarctica Ross Island |
genre_facet |
Antarc* Antarctica Ross Island |
op_relation |
https://dx.doi.org/10.1016/j.epsl.2019.115903 |
op_rights |
arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ |
op_doi |
https://doi.org/10.48550/arxiv.1907.02899 https://doi.org/10.1016/j.epsl.2019.115903 |
_version_ |
1766276830242799616 |