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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Bibliographic Details
Main Author: Simkins, Lauren
Format: Dataset
Language:English
Published: U.S. Antarctic Program (USAP) Data Center 2021
Subjects:
Online Access:https://dx.doi.org/10.15784/601474
https://www.usap-dc.org/view/dataset/601474
id ftdatacite:10.15784/601474
record_format openpolar
spelling 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
institution 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
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