New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ...
Autonomous Underwater Vehicles (AUVs) deployed close to the seafloor can acquire high-resolution geophysical data about the topography and shallow stratigraphy of the seabed, yet have had limited application within the fields of glacial geomorphology and ice sheet reconstruction. Here, we present mu...
Main Authors: | , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier BV
2020
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Subjects: | |
Online Access: | https://dx.doi.org/10.17863/cam.58295 https://www.repository.cam.ac.uk/handle/1810/311199 |
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author | Batchelor, CL Montelli, A Ottesen, D Evans, J Dowdeswell, EK Christie, FDW Dowdeswell, JA |
author_facet | Batchelor, CL Montelli, A Ottesen, D Evans, J Dowdeswell, EK Christie, FDW Dowdeswell, JA |
author_sort | Batchelor, CL |
collection | DataCite |
description | Autonomous Underwater Vehicles (AUVs) deployed close to the seafloor can acquire high-resolution geophysical data about the topography and shallow stratigraphy of the seabed, yet have had limited application within the fields of glacial geomorphology and ice sheet reconstruction. Here, we present multibeam echo-sounding, side-scan sonar, sub-bottom profiler and High-Resolution Synthetic Aperture Sonar (HISAS) data acquired during three AUV dives on the northeast Antarctic Peninsula continental shelf. These data enable glacial landforms, including mega-scale glacial lineations (MSGLs), grounding-zone wedges (GZWs) and iceberg ploughmarks, to be imaged at a horizontal resolution of a few tens of centimetres, allowing for the identification of subtle morphological features. We map tidal ridges that are interpreted as having been formed 1) along the ice-sheet grounding line by the squeezing up of soft seafloor sediments by vertical motion of the grounding line during tidal cycles, and 2) by the tidally driven ... |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Antarctic Peninsula Ice Sheet Iceberg* |
genre_facet | Antarc* Antarctic Antarctic Peninsula Ice Sheet Iceberg* |
geographic | Antarctic Antarctic Peninsula |
geographic_facet | Antarctic Antarctic Peninsula |
id | ftdatacite:10.17863/cam.58295 |
institution | Open Polar |
language | English |
op_collection_id | ftdatacite |
op_doi | https://doi.org/10.17863/cam.58295 |
op_rights | open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
publishDate | 2020 |
publisher | Elsevier BV |
record_format | openpolar |
spelling | ftdatacite:10.17863/cam.58295 2025-01-16T19:15:26+00:00 New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ... Batchelor, CL Montelli, A Ottesen, D Evans, J Dowdeswell, EK Christie, FDW Dowdeswell, JA 2020 https://dx.doi.org/10.17863/cam.58295 https://www.repository.cam.ac.uk/handle/1810/311199 en eng Elsevier BV open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 Autonomous Underwater Vehicles Glacial landforms Grounding-zone wedge Iceberg ploughmarks Corrugation ridges Antarctic Peninsula Article article-journal ScholarlyArticle JournalArticle 2020 ftdatacite https://doi.org/10.17863/cam.58295 2025-01-06T20:27:34Z Autonomous Underwater Vehicles (AUVs) deployed close to the seafloor can acquire high-resolution geophysical data about the topography and shallow stratigraphy of the seabed, yet have had limited application within the fields of glacial geomorphology and ice sheet reconstruction. Here, we present multibeam echo-sounding, side-scan sonar, sub-bottom profiler and High-Resolution Synthetic Aperture Sonar (HISAS) data acquired during three AUV dives on the northeast Antarctic Peninsula continental shelf. These data enable glacial landforms, including mega-scale glacial lineations (MSGLs), grounding-zone wedges (GZWs) and iceberg ploughmarks, to be imaged at a horizontal resolution of a few tens of centimetres, allowing for the identification of subtle morphological features. We map tidal ridges that are interpreted as having been formed 1) along the ice-sheet grounding line by the squeezing up of soft seafloor sediments by vertical motion of the grounding line during tidal cycles, and 2) by the tidally driven ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Sheet Iceberg* DataCite Antarctic Antarctic Peninsula |
spellingShingle | Autonomous Underwater Vehicles Glacial landforms Grounding-zone wedge Iceberg ploughmarks Corrugation ridges Antarctic Peninsula Batchelor, CL Montelli, A Ottesen, D Evans, J Dowdeswell, EK Christie, FDW Dowdeswell, JA New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ... |
title | New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ... |
title_full | New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ... |
title_fullStr | New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ... |
title_full_unstemmed | New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ... |
title_short | New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data ... |
title_sort | new insights into the formation of submarine glacial landforms from high-resolution autonomous underwater vehicle data ... |
topic | Autonomous Underwater Vehicles Glacial landforms Grounding-zone wedge Iceberg ploughmarks Corrugation ridges Antarctic Peninsula |
topic_facet | Autonomous Underwater Vehicles Glacial landforms Grounding-zone wedge Iceberg ploughmarks Corrugation ridges Antarctic Peninsula |
url | https://dx.doi.org/10.17863/cam.58295 https://www.repository.cam.ac.uk/handle/1810/311199 |