Seismologically Observed Spatiotemporal Drainage Activity at Moulins
Hydrology is important for glacier dynamics, but it is difficult to monitor the subsurface drainage systems of glaciers by direct observations. Since meltwater drainage generates seismic signals, passive seismic analysis has the potential to be used to monitor these processes. To study continuous se...
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ftcaltechauth:oai:authors.library.caltech.edu:maedx-h8w03 2024-06-23T07:53:05+00:00 Seismologically Observed Spatiotemporal Drainage Activity at Moulins Aso, Naofumi Tsai, Victor C. Schoof, Christian Flowers, Gwenn E. Whiteford, Arran Rada, Camilo 2017-11 https://doi.org/10.1002/2017JB014578 unknown American Geophysical Union https://doi.org/10.1002/2017JB014578 oai:authors.library.caltech.edu:maedx-h8w03 eprintid:84374 resolverid:CaltechAUTHORS:20180117-155132585 info:eu-repo/semantics/openAccess Other Journal of Geophysical Research. Solid Earth, 122(11), 9095-9108, (2017-11) cryoseismology ambient noise backprojection glacier hydrology moulins info:eu-repo/semantics/article 2017 ftcaltechauth https://doi.org/10.1002/2017JB014578 2024-06-12T03:10:27Z Hydrology is important for glacier dynamics, but it is difficult to monitor the subsurface drainage systems of glaciers by direct observations. Since meltwater drainage generates seismic signals, passive seismic analysis has the potential to be used to monitor these processes. To study continuous seismic radiation from the drainage, we analyze geophone data from six stations deployed at the Kaskawulsh Glacier in Yukon, Canada, during the summer of 2014 using ambient noise cross-correlation techniques. We locate the noise sources by backprojecting the amplitude of the cross correlation to the glacier surface. Most of the ambient noise sequences are found in two clusters, with each cluster located in the vicinity of a moulin identified at the surface. Stronger seismic radiation is observed during the day, consistent with expected variability in melt rates. We demonstrate that the sparse seismic network array with 2 km station separation has the ability to detect moulins within the array with a precision of 50 m. We confirm that seismic activity is correlated with air temperature, and thus, melt, on a diurnal timescale, and precipitation correlates with the activity at longer timescales. Our results highlight the potential of passive seismic observations for monitoring water flow into subglacial channels through moulins with an affordable number of seismic stations, but quantification of water flow rates still remains a challenge. The cross-correlation backprojection technique described here can also potentially be applied to any localized source of ambient noise such as ocean noise, tectonic tremor, and volcanic tremor. © 2017 American Geophysical Union. Received 17 JUN 2017; Accepted 17 OCT 2017; Accepted article online 19 OCT 2017; Published online 11 NOV 2017. We thank C. Zdanowicz and L. Copland for the meteorological data at the weather station at the confluence. We acknowledge the Natural Sciences and Engineering Research Council (NSERC) of Canada, the Canada Research Chairs Program, the California ... Article in Journal/Newspaper glacier* Yukon Caltech Authors (California Institute of Technology) Canada Kaskawulsh Glacier ENVELOPE(-139.104,-139.104,60.749,60.749) Yukon Journal of Geophysical Research: Solid Earth 122 11 9095 9108 |
institution |
Open Polar |
collection |
Caltech Authors (California Institute of Technology) |
op_collection_id |
ftcaltechauth |
language |
unknown |
topic |
cryoseismology ambient noise backprojection glacier hydrology moulins |
spellingShingle |
cryoseismology ambient noise backprojection glacier hydrology moulins Aso, Naofumi Tsai, Victor C. Schoof, Christian Flowers, Gwenn E. Whiteford, Arran Rada, Camilo Seismologically Observed Spatiotemporal Drainage Activity at Moulins |
topic_facet |
cryoseismology ambient noise backprojection glacier hydrology moulins |
description |
Hydrology is important for glacier dynamics, but it is difficult to monitor the subsurface drainage systems of glaciers by direct observations. Since meltwater drainage generates seismic signals, passive seismic analysis has the potential to be used to monitor these processes. To study continuous seismic radiation from the drainage, we analyze geophone data from six stations deployed at the Kaskawulsh Glacier in Yukon, Canada, during the summer of 2014 using ambient noise cross-correlation techniques. We locate the noise sources by backprojecting the amplitude of the cross correlation to the glacier surface. Most of the ambient noise sequences are found in two clusters, with each cluster located in the vicinity of a moulin identified at the surface. Stronger seismic radiation is observed during the day, consistent with expected variability in melt rates. We demonstrate that the sparse seismic network array with 2 km station separation has the ability to detect moulins within the array with a precision of 50 m. We confirm that seismic activity is correlated with air temperature, and thus, melt, on a diurnal timescale, and precipitation correlates with the activity at longer timescales. Our results highlight the potential of passive seismic observations for monitoring water flow into subglacial channels through moulins with an affordable number of seismic stations, but quantification of water flow rates still remains a challenge. The cross-correlation backprojection technique described here can also potentially be applied to any localized source of ambient noise such as ocean noise, tectonic tremor, and volcanic tremor. © 2017 American Geophysical Union. Received 17 JUN 2017; Accepted 17 OCT 2017; Accepted article online 19 OCT 2017; Published online 11 NOV 2017. We thank C. Zdanowicz and L. Copland for the meteorological data at the weather station at the confluence. We acknowledge the Natural Sciences and Engineering Research Council (NSERC) of Canada, the Canada Research Chairs Program, the California ... |
format |
Article in Journal/Newspaper |
author |
Aso, Naofumi Tsai, Victor C. Schoof, Christian Flowers, Gwenn E. Whiteford, Arran Rada, Camilo |
author_facet |
Aso, Naofumi Tsai, Victor C. Schoof, Christian Flowers, Gwenn E. Whiteford, Arran Rada, Camilo |
author_sort |
Aso, Naofumi |
title |
Seismologically Observed Spatiotemporal Drainage Activity at Moulins |
title_short |
Seismologically Observed Spatiotemporal Drainage Activity at Moulins |
title_full |
Seismologically Observed Spatiotemporal Drainage Activity at Moulins |
title_fullStr |
Seismologically Observed Spatiotemporal Drainage Activity at Moulins |
title_full_unstemmed |
Seismologically Observed Spatiotemporal Drainage Activity at Moulins |
title_sort |
seismologically observed spatiotemporal drainage activity at moulins |
publisher |
American Geophysical Union |
publishDate |
2017 |
url |
https://doi.org/10.1002/2017JB014578 |
long_lat |
ENVELOPE(-139.104,-139.104,60.749,60.749) |
geographic |
Canada Kaskawulsh Glacier Yukon |
geographic_facet |
Canada Kaskawulsh Glacier Yukon |
genre |
glacier* Yukon |
genre_facet |
glacier* Yukon |
op_source |
Journal of Geophysical Research. Solid Earth, 122(11), 9095-9108, (2017-11) |
op_relation |
https://doi.org/10.1002/2017JB014578 oai:authors.library.caltech.edu:maedx-h8w03 eprintid:84374 resolverid:CaltechAUTHORS:20180117-155132585 |
op_rights |
info:eu-repo/semantics/openAccess Other |
op_doi |
https://doi.org/10.1002/2017JB014578 |
container_title |
Journal of Geophysical Research: Solid Earth |
container_volume |
122 |
container_issue |
11 |
container_start_page |
9095 |
op_container_end_page |
9108 |
_version_ |
1802644570653065216 |