Pennell Trough, Ross Sea bathymetry and glacial landforms
Bathymetry from multibeam echo sounding data in Pennell Trough, Ross Sea, Antarctica was collected onboard the RVIB Nathaniel B. Palmer (NBP) 15-02 cruise using a Kongsberg EM122 operating in dual swath mode at 12 kHz frequency with a 1°×1° beam width, swath angular coverage set to 62°×62°, and 30-6...
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U.S. Antarctic Program (USAP) Data Center
2021
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Online Access: | https://dx.doi.org/10.15784/601474 https://www.usap-dc.org/view/dataset/601474 |
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ftdatacite:10.15784/601474 2023-05-15T13:38:26+02:00 Pennell Trough, Ross Sea bathymetry and glacial landforms Simkins, Lauren 2021 https://dx.doi.org/10.15784/601474 https://www.usap-dc.org/view/dataset/601474 en eng U.S. Antarctic Program (USAP) Data Center Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY NBP1502 Bathymetry Geomorphology Glacial History R/V Nathaniel B. Palmer Bathymetry/Topography Glaciers/Ice Sheet Cryosphere Marine Geoscience Antarctica dataset Dataset 2021 ftdatacite https://doi.org/10.15784/601474 2022-02-08T11:47:00Z Bathymetry from multibeam echo sounding data in Pennell Trough, Ross Sea, Antarctica was collected onboard the RVIB Nathaniel B. Palmer (NBP) 15-02 cruise using a Kongsberg EM122 operating in dual swath mode at 12 kHz frequency with a 1°×1° beam width, swath angular coverage set to 62°×62°, and 30-60% overlap between survey lines. All raw, ping-edited geophysical data collected on NBP15-02 can be accessed using the Marine Geoscience Data System (Cruise DOI: 10.7284/901477). The bathymetry dataset here is gridded at 20-m resolution with a water depth-dependent vertical resolution on the order of decimeters. Two shapefiles are provided for ice-marginal landforms and meltwater landforms observable in the bathymetry data. The purpose of collecting the bathymetry data on cruise NBP15-02 was to better understand the glacial history of the Ross Sea, and the dataset, inclusive of bathymetry data and shapefiles of glacial landforms, from Pennell Trough are used to understand impacts on subglacial channel morphology and organization during the deglaciation of the region following the Last Glacial Maximum. The published dataset was used and analyzed in the article "Topographic controls on channelized meltwater in the subglacial environment" by Simkins, L.M., Greenwood, S.L., Munevar Garcia, S., Eareckson, E.A., Anderson, J.B., and Prothro, L.O, which was published in Geophysical Research Letters in 2021 (DOI: 10.1029/2021GL094678). Dataset Antarc* Antarctica Ice Sheet Ross Sea DataCite Metadata Store (German National Library of Science and Technology) Kongsberg ENVELOPE(19.082,19.082,69.123,69.123) Ross Sea |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
NBP1502 Bathymetry Geomorphology Glacial History R/V Nathaniel B. Palmer Bathymetry/Topography Glaciers/Ice Sheet Cryosphere Marine Geoscience Antarctica |
spellingShingle |
NBP1502 Bathymetry Geomorphology Glacial History R/V Nathaniel B. Palmer Bathymetry/Topography Glaciers/Ice Sheet Cryosphere Marine Geoscience Antarctica Simkins, Lauren Pennell Trough, Ross Sea bathymetry and glacial landforms |
topic_facet |
NBP1502 Bathymetry Geomorphology Glacial History R/V Nathaniel B. Palmer Bathymetry/Topography Glaciers/Ice Sheet Cryosphere Marine Geoscience Antarctica |
description |
Bathymetry from multibeam echo sounding data in Pennell Trough, Ross Sea, Antarctica was collected onboard the RVIB Nathaniel B. Palmer (NBP) 15-02 cruise using a Kongsberg EM122 operating in dual swath mode at 12 kHz frequency with a 1°×1° beam width, swath angular coverage set to 62°×62°, and 30-60% overlap between survey lines. All raw, ping-edited geophysical data collected on NBP15-02 can be accessed using the Marine Geoscience Data System (Cruise DOI: 10.7284/901477). The bathymetry dataset here is gridded at 20-m resolution with a water depth-dependent vertical resolution on the order of decimeters. Two shapefiles are provided for ice-marginal landforms and meltwater landforms observable in the bathymetry data. The purpose of collecting the bathymetry data on cruise NBP15-02 was to better understand the glacial history of the Ross Sea, and the dataset, inclusive of bathymetry data and shapefiles of glacial landforms, from Pennell Trough are used to understand impacts on subglacial channel morphology and organization during the deglaciation of the region following the Last Glacial Maximum. The published dataset was used and analyzed in the article "Topographic controls on channelized meltwater in the subglacial environment" by Simkins, L.M., Greenwood, S.L., Munevar Garcia, S., Eareckson, E.A., Anderson, J.B., and Prothro, L.O, which was published in Geophysical Research Letters in 2021 (DOI: 10.1029/2021GL094678). |
format |
Dataset |
author |
Simkins, Lauren |
author_facet |
Simkins, Lauren |
author_sort |
Simkins, Lauren |
title |
Pennell Trough, Ross Sea bathymetry and glacial landforms |
title_short |
Pennell Trough, Ross Sea bathymetry and glacial landforms |
title_full |
Pennell Trough, Ross Sea bathymetry and glacial landforms |
title_fullStr |
Pennell Trough, Ross Sea bathymetry and glacial landforms |
title_full_unstemmed |
Pennell Trough, Ross Sea bathymetry and glacial landforms |
title_sort |
pennell trough, ross sea bathymetry and glacial landforms |
publisher |
U.S. Antarctic Program (USAP) Data Center |
publishDate |
2021 |
url |
https://dx.doi.org/10.15784/601474 https://www.usap-dc.org/view/dataset/601474 |
long_lat |
ENVELOPE(19.082,19.082,69.123,69.123) |
geographic |
Kongsberg Ross Sea |
geographic_facet |
Kongsberg Ross Sea |
genre |
Antarc* Antarctica Ice Sheet Ross Sea |
genre_facet |
Antarc* Antarctica Ice Sheet Ross Sea |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.15784/601474 |
_version_ |
1766106204532113408 |