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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Main Authors: Birnbaum, Janine, Keller, Tobias, Suckale, Jenny, Lev, Einat
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2019
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1907.02899
https://arxiv.org/abs/1907.02899
id ftdatacite:10.48550/arxiv.1907.02899
record_format openpolar
spelling 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)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
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
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