Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica
We use seismic refraction data to investigate the firn structure across a suture zone on the AmeryIce Shelf, East Antarctica, and the possible role of glacier dynamics in firn evolution. In the downstreamdirection, the data reveal decreasing compressional-wave velocities and increasing penetrationde...
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ftunivtasmania:oai:eprints.utas.edu.au:45696 2023-05-15T13:22:07+02:00 Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica Hollmann, H Treverrow, A Peters, LE Reading, AM Kulessa, B 2021 application/pdf https://eprints.utas.edu.au/45696/ https://eprints.utas.edu.au/45696/1/147933%20-%20Seismic%20observations%20of%20a%20complex%20firn%20structure.pdf en eng Int Glaciol Soc https://eprints.utas.edu.au/45696/1/147933%20-%20Seismic%20observations%20of%20a%20complex%20firn%20structure.pdf Hollmann, H, Treverrow, A orcid:0000-0003-4666-0488 , Peters, LE, Reading, AM orcid:0000-0002-9316-7605 and Kulessa, B 2021 , 'Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica' , Journal of Glaciology, vol. 67, no. 265 , pp. 777-787 , doi:10.1017/jog.2021.21 <http://dx.doi.org/10.1017/jog.2021.21>. polar firn seismics snow mechanics Article PeerReviewed 2021 ftunivtasmania https://doi.org/10.1017/jog.2021.21 2022-05-09T22:16:33Z We use seismic refraction data to investigate the firn structure across a suture zone on the AmeryIce Shelf, East Antarctica, and the possible role of glacier dynamics in firn evolution. In the downstreamdirection, the data reveal decreasing compressional-wave velocities and increasing penetrationdepth of the propagating wave in the firn layer, consistent with ~1m firn thickeningevery 6 km. The boundary between the Lambert Glacier unit to the west and a major suturezone and the Mawson Escarpment Ice Stream unit to the east, is marked by differences in firnthicknesses, compressional-wave velocities and seismic anisotropy in the across-flow direction.The latter does not contradict the presence of a single-maximum crystal orientation fabricoriented 45–90◦ away from the flow direction. This is consistent with the presence of transversesimple shear governing the region’s underlying ice flow regime, in association with elevated strainalong the suture zone. The confirmation and quantification of the implied dynamic couplingbetween firn and the underlying ice requires integration of future seismic refraction, coringand modelling studies. Because firn is estimated to cover ~ 98% of the Antarctic continent anysuch coupling may have widespread relevance to ice-sheet evolution and flow. Article in Journal/Newspaper Amery Ice Shelf Antarc* Antarctic Antarctica Antarctica Journal East Antarctica Ice Sheet Ice Shelf Journal of Glaciology Lambert Glacier University of Tasmania: UTas ePrints Antarctic The Antarctic East Antarctica Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Amery Ice Shelf ENVELOPE(71.000,71.000,-69.750,-69.750) Lambert Glacier ENVELOPE(67.490,67.490,-73.065,-73.065) Mawson Escarpment ENVELOPE(68.167,68.167,-73.083,-73.083) Journal of Glaciology 67 265 777 787 |
institution |
Open Polar |
collection |
University of Tasmania: UTas ePrints |
op_collection_id |
ftunivtasmania |
language |
English |
topic |
polar firn seismics snow mechanics |
spellingShingle |
polar firn seismics snow mechanics Hollmann, H Treverrow, A Peters, LE Reading, AM Kulessa, B Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica |
topic_facet |
polar firn seismics snow mechanics |
description |
We use seismic refraction data to investigate the firn structure across a suture zone on the AmeryIce Shelf, East Antarctica, and the possible role of glacier dynamics in firn evolution. In the downstreamdirection, the data reveal decreasing compressional-wave velocities and increasing penetrationdepth of the propagating wave in the firn layer, consistent with ~1m firn thickeningevery 6 km. The boundary between the Lambert Glacier unit to the west and a major suturezone and the Mawson Escarpment Ice Stream unit to the east, is marked by differences in firnthicknesses, compressional-wave velocities and seismic anisotropy in the across-flow direction.The latter does not contradict the presence of a single-maximum crystal orientation fabricoriented 45–90◦ away from the flow direction. This is consistent with the presence of transversesimple shear governing the region’s underlying ice flow regime, in association with elevated strainalong the suture zone. The confirmation and quantification of the implied dynamic couplingbetween firn and the underlying ice requires integration of future seismic refraction, coringand modelling studies. Because firn is estimated to cover ~ 98% of the Antarctic continent anysuch coupling may have widespread relevance to ice-sheet evolution and flow. |
format |
Article in Journal/Newspaper |
author |
Hollmann, H Treverrow, A Peters, LE Reading, AM Kulessa, B |
author_facet |
Hollmann, H Treverrow, A Peters, LE Reading, AM Kulessa, B |
author_sort |
Hollmann, H |
title |
Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica |
title_short |
Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica |
title_full |
Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica |
title_fullStr |
Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica |
title_full_unstemmed |
Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica |
title_sort |
seismic observations of a complex firn structure across the amery ice shelf, east antarctica |
publisher |
Int Glaciol Soc |
publishDate |
2021 |
url |
https://eprints.utas.edu.au/45696/ https://eprints.utas.edu.au/45696/1/147933%20-%20Seismic%20observations%20of%20a%20complex%20firn%20structure.pdf |
long_lat |
ENVELOPE(-94.063,-94.063,56.565,56.565) ENVELOPE(71.000,71.000,-69.750,-69.750) ENVELOPE(67.490,67.490,-73.065,-73.065) ENVELOPE(68.167,68.167,-73.083,-73.083) |
geographic |
Antarctic The Antarctic East Antarctica Amery Amery Ice Shelf Lambert Glacier Mawson Escarpment |
geographic_facet |
Antarctic The Antarctic East Antarctica Amery Amery Ice Shelf Lambert Glacier Mawson Escarpment |
genre |
Amery Ice Shelf Antarc* Antarctic Antarctica Antarctica Journal East Antarctica Ice Sheet Ice Shelf Journal of Glaciology Lambert Glacier |
genre_facet |
Amery Ice Shelf Antarc* Antarctic Antarctica Antarctica Journal East Antarctica Ice Sheet Ice Shelf Journal of Glaciology Lambert Glacier |
op_relation |
https://eprints.utas.edu.au/45696/1/147933%20-%20Seismic%20observations%20of%20a%20complex%20firn%20structure.pdf Hollmann, H, Treverrow, A orcid:0000-0003-4666-0488 , Peters, LE, Reading, AM orcid:0000-0002-9316-7605 and Kulessa, B 2021 , 'Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica' , Journal of Glaciology, vol. 67, no. 265 , pp. 777-787 , doi:10.1017/jog.2021.21 <http://dx.doi.org/10.1017/jog.2021.21>. |
op_doi |
https://doi.org/10.1017/jog.2021.21 |
container_title |
Journal of Glaciology |
container_volume |
67 |
container_issue |
265 |
container_start_page |
777 |
op_container_end_page |
787 |
_version_ |
1766363368850980864 |