Autonomous phase-sensitive radar (ApRES) measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica between 2016/17 and 2017/18
The dataset consists of raw data from six autonomous phase-sensitive radar (ApRES) measurements. The ApRES with two bow-tie antennas were operated at a basal melt channel of the southern Filchner Ice Shelf, Antarctica near the Support Force Glacier. Five short-period ApRES were located at a cross-se...
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Format: | Dataset |
Language: | English |
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PANGAEA
2021
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.932413 https://doi.org/10.1594/PANGAEA.932413 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.932413 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Antarctica ANT-Land_2016/17_FISP ANT-Land_2016/17_FISP_ApRES_low ANT-Land_2016/17_FISP_ApRES_oe ANT-Land_2016/17_FISP_ApRES_ow ANT-Land_2016/17_FISP_ApRES_se ANT-Land_2016/17_FISP_ApRES_sw ANT-Land_2017_FISP_ApRES_oe_long ApRES ApRES_low ApRES_oe ApRES_ow ApRES_se ApRES_sw Autonomous phase-sensitive radio-echo sounder AWI Antarctic Land Expedition Basal melt rates Binary Object Binary Object (File Size) Date/Time of event Date/Time of event 2 Event label Filchner Ice Shelf Filchner Ice Shelf Project FISP Latitude of event Longitude of event |
spellingShingle |
Antarctica ANT-Land_2016/17_FISP ANT-Land_2016/17_FISP_ApRES_low ANT-Land_2016/17_FISP_ApRES_oe ANT-Land_2016/17_FISP_ApRES_ow ANT-Land_2016/17_FISP_ApRES_se ANT-Land_2016/17_FISP_ApRES_sw ANT-Land_2017_FISP_ApRES_oe_long ApRES ApRES_low ApRES_oe ApRES_ow ApRES_se ApRES_sw Autonomous phase-sensitive radio-echo sounder AWI Antarctic Land Expedition Basal melt rates Binary Object Binary Object (File Size) Date/Time of event Date/Time of event 2 Event label Filchner Ice Shelf Filchner Ice Shelf Project FISP Latitude of event Longitude of event Zeising, Ole Steinhage, Daniel Humbert, Angelika Autonomous phase-sensitive radar (ApRES) measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica between 2016/17 and 2017/18 |
topic_facet |
Antarctica ANT-Land_2016/17_FISP ANT-Land_2016/17_FISP_ApRES_low ANT-Land_2016/17_FISP_ApRES_oe ANT-Land_2016/17_FISP_ApRES_ow ANT-Land_2016/17_FISP_ApRES_se ANT-Land_2016/17_FISP_ApRES_sw ANT-Land_2017_FISP_ApRES_oe_long ApRES ApRES_low ApRES_oe ApRES_ow ApRES_se ApRES_sw Autonomous phase-sensitive radio-echo sounder AWI Antarctic Land Expedition Basal melt rates Binary Object Binary Object (File Size) Date/Time of event Date/Time of event 2 Event label Filchner Ice Shelf Filchner Ice Shelf Project FISP Latitude of event Longitude of event |
description |
The dataset consists of raw data from six autonomous phase-sensitive radar (ApRES) measurements. The ApRES with two bow-tie antennas were operated at a basal melt channel of the southern Filchner Ice Shelf, Antarctica near the Support Force Glacier. Five short-period ApRES were located at a cross-section of the channel, located east outside the channel (ApRES_oe), at the eastern steepest flank of the surface depression (ApRES_se), within the channel at the lowest surface depression (ApRES_low), at the western steepest flank (ApRES_sw) and west outside the channel (ApRES_we). All four ApRES operated for 9 to 13 days with a measuring interval of 15 minutes. The long-period ApRES (ApRES_oe_long) operated east outside the channel for 361 days with a measuring interval of 2 hours. The short-period ApRES were operated parallel to GPS stations (see doi:10.1594/PANGAEA.932441). These Lagrangian measurements allow the estimation of basal melt rates based on estimated vertical displacements of englacial and basal reflections. The ApRES is an autonomous operating frequency-modulated continuous wave (FMCW) radar that transmits a tone sweep – called chirp – ranging from 200 to 400 MHz over a period of one second. In order to improve the signal-to-noise ratio, 100 chirps were transmitted within a single measurement. These measurements were repeated every 24 hours. Background of the ApRES-system is published by Brennan et al. (2014) and Nicholls et al. (2015). The processing of the data is described in Stewart (2018), Stewart et al. (2019) and Vankova et al. (2020). |
format |
Dataset |
author |
Zeising, Ole Steinhage, Daniel Humbert, Angelika |
author_facet |
Zeising, Ole Steinhage, Daniel Humbert, Angelika |
author_sort |
Zeising, Ole |
title |
Autonomous phase-sensitive radar (ApRES) measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica between 2016/17 and 2017/18 |
title_short |
Autonomous phase-sensitive radar (ApRES) measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica between 2016/17 and 2017/18 |
title_full |
Autonomous phase-sensitive radar (ApRES) measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica between 2016/17 and 2017/18 |
title_fullStr |
Autonomous phase-sensitive radar (ApRES) measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica between 2016/17 and 2017/18 |
title_full_unstemmed |
Autonomous phase-sensitive radar (ApRES) measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica between 2016/17 and 2017/18 |
title_sort |
autonomous phase-sensitive radar (apres) measurements at a basal melt channel of the southern filchner ice shelf, antarctica between 2016/17 and 2017/18 |
publisher |
PANGAEA |
publishDate |
2021 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.932413 https://doi.org/10.1594/PANGAEA.932413 |
op_coverage |
MEDIAN LATITUDE: -82.373050 * MEDIAN LONGITUDE: -45.776600 * SOUTH-BOUND LATITUDE: -82.375400 * WEST-BOUND LONGITUDE: -45.921000 * NORTH-BOUND LATITUDE: -82.370200 * EAST-BOUND LONGITUDE: -45.662900 * DATE/TIME START: 2016-12-27T14:04:00 * DATE/TIME END: 2018-01-06T20:11:00 |
long_lat |
ENVELOPE(-40.000,-40.000,-79.000,-79.000) ENVELOPE(-47.500,-47.500,-83.083,-83.083) ENVELOPE(-45.921000,-45.662900,-82.370200,-82.375400) |
geographic |
Antarctic Filchner Ice Shelf Support Force Glacier |
geographic_facet |
Antarctic Filchner Ice Shelf Support Force Glacier |
genre |
Antarc* Ice Shelf Support Force Glacier |
genre_facet |
Antarc* Ice Shelf Support Force Glacier |
op_relation |
Brennan, Paul V; Lok, Lai Bun; Nicholls, Keith W; Corr, Hugh F J (2014): Phase‐sensitive FMCW radar system for high‐precision Antarctic ice shelf profile monitoring. IET Radar, Sonar & Navigation, 8(7), 776-786, https://doi.org/10.1049/iet-rsn.2013.0053 Nicholls, Keith W; Corr, Hugh F J; Stewart, Craig L; Lok, Lai Bun; Brennan, Paul V; Vaughan, David G (2015): A ground-based radar for measuring vertical strain rates and time-varying basal melt rates in ice sheets and shelves. Journal of Glaciology, 61(230), 1079-1087, https://doi.org/10.3189/2015JoG15J073 Stewart, Craig L (2018): Ice-ocean interactions beneath the north-western Ross Ice Shelf, Antarctica. Apollo-University Of Cambridge Repository, https://doi.org/10.17863/CAM.21483 Stewart, Craig L; Christoffersen, Poul; Nicholls, Keith W; Williams, Michael J M; Dowdeswell, Julian A (2019): Basal melting of Ross Ice Shelf from solar heat absorption in an ice-front polynya. Nature Geoscience, 12, 435-440, https://doi.org/10.1038/s41561-019-0356-0 Vankova, Irena; Nicholls, Keith W; Corr, Hugh F J; Makinson, Keith; Brennan, Paul V (2020): Observations of Tidal Melt and Vertical Strain at the Filchner‐Ronne Ice Shelf, Antarctica. Journal of Geophysical Research-Earth Surface, 125(1), https://doi.org/10.1029/2019JF005280 Zeising, Ole; Helm, Veit; Steinhage, Daniel; Humbert, Angelika (2021): GNSS measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.932441 https://doi.pangaea.de/10.1594/PANGAEA.932413 https://doi.org/10.1594/PANGAEA.932413 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.93241310.3189/2015JoG15J07310.17863/CAM.2148310.1038/s41561-019-0356-010.1029/2019JF00528010.1594/PANGAEA.932441 |
_version_ |
1814279085562527744 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.932413 2024-10-29T17:41:42+00:00 Autonomous phase-sensitive radar (ApRES) measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica between 2016/17 and 2017/18 Zeising, Ole Steinhage, Daniel Humbert, Angelika MEDIAN LATITUDE: -82.373050 * MEDIAN LONGITUDE: -45.776600 * SOUTH-BOUND LATITUDE: -82.375400 * WEST-BOUND LONGITUDE: -45.921000 * NORTH-BOUND LATITUDE: -82.370200 * EAST-BOUND LONGITUDE: -45.662900 * DATE/TIME START: 2016-12-27T14:04:00 * DATE/TIME END: 2018-01-06T20:11:00 2021 text/tab-separated-values, 6 data points https://doi.pangaea.de/10.1594/PANGAEA.932413 https://doi.org/10.1594/PANGAEA.932413 en eng PANGAEA Brennan, Paul V; Lok, Lai Bun; Nicholls, Keith W; Corr, Hugh F J (2014): Phase‐sensitive FMCW radar system for high‐precision Antarctic ice shelf profile monitoring. IET Radar, Sonar & Navigation, 8(7), 776-786, https://doi.org/10.1049/iet-rsn.2013.0053 Nicholls, Keith W; Corr, Hugh F J; Stewart, Craig L; Lok, Lai Bun; Brennan, Paul V; Vaughan, David G (2015): A ground-based radar for measuring vertical strain rates and time-varying basal melt rates in ice sheets and shelves. Journal of Glaciology, 61(230), 1079-1087, https://doi.org/10.3189/2015JoG15J073 Stewart, Craig L (2018): Ice-ocean interactions beneath the north-western Ross Ice Shelf, Antarctica. Apollo-University Of Cambridge Repository, https://doi.org/10.17863/CAM.21483 Stewart, Craig L; Christoffersen, Poul; Nicholls, Keith W; Williams, Michael J M; Dowdeswell, Julian A (2019): Basal melting of Ross Ice Shelf from solar heat absorption in an ice-front polynya. Nature Geoscience, 12, 435-440, https://doi.org/10.1038/s41561-019-0356-0 Vankova, Irena; Nicholls, Keith W; Corr, Hugh F J; Makinson, Keith; Brennan, Paul V (2020): Observations of Tidal Melt and Vertical Strain at the Filchner‐Ronne Ice Shelf, Antarctica. Journal of Geophysical Research-Earth Surface, 125(1), https://doi.org/10.1029/2019JF005280 Zeising, Ole; Helm, Veit; Steinhage, Daniel; Humbert, Angelika (2021): GNSS measurements at a basal melt channel of the southern Filchner Ice Shelf, Antarctica [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.932441 https://doi.pangaea.de/10.1594/PANGAEA.932413 https://doi.org/10.1594/PANGAEA.932413 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Antarctica ANT-Land_2016/17_FISP ANT-Land_2016/17_FISP_ApRES_low ANT-Land_2016/17_FISP_ApRES_oe ANT-Land_2016/17_FISP_ApRES_ow ANT-Land_2016/17_FISP_ApRES_se ANT-Land_2016/17_FISP_ApRES_sw ANT-Land_2017_FISP_ApRES_oe_long ApRES ApRES_low ApRES_oe ApRES_ow ApRES_se ApRES_sw Autonomous phase-sensitive radio-echo sounder AWI Antarctic Land Expedition Basal melt rates Binary Object Binary Object (File Size) Date/Time of event Date/Time of event 2 Event label Filchner Ice Shelf Filchner Ice Shelf Project FISP Latitude of event Longitude of event dataset 2021 ftpangaea https://doi.org/10.1594/PANGAEA.93241310.3189/2015JoG15J07310.17863/CAM.2148310.1038/s41561-019-0356-010.1029/2019JF00528010.1594/PANGAEA.932441 2024-10-02T00:42:44Z The dataset consists of raw data from six autonomous phase-sensitive radar (ApRES) measurements. The ApRES with two bow-tie antennas were operated at a basal melt channel of the southern Filchner Ice Shelf, Antarctica near the Support Force Glacier. Five short-period ApRES were located at a cross-section of the channel, located east outside the channel (ApRES_oe), at the eastern steepest flank of the surface depression (ApRES_se), within the channel at the lowest surface depression (ApRES_low), at the western steepest flank (ApRES_sw) and west outside the channel (ApRES_we). All four ApRES operated for 9 to 13 days with a measuring interval of 15 minutes. The long-period ApRES (ApRES_oe_long) operated east outside the channel for 361 days with a measuring interval of 2 hours. The short-period ApRES were operated parallel to GPS stations (see doi:10.1594/PANGAEA.932441). These Lagrangian measurements allow the estimation of basal melt rates based on estimated vertical displacements of englacial and basal reflections. The ApRES is an autonomous operating frequency-modulated continuous wave (FMCW) radar that transmits a tone sweep – called chirp – ranging from 200 to 400 MHz over a period of one second. In order to improve the signal-to-noise ratio, 100 chirps were transmitted within a single measurement. These measurements were repeated every 24 hours. Background of the ApRES-system is published by Brennan et al. (2014) and Nicholls et al. (2015). The processing of the data is described in Stewart (2018), Stewart et al. (2019) and Vankova et al. (2020). Dataset Antarc* Ice Shelf Support Force Glacier PANGAEA - Data Publisher for Earth & Environmental Science Antarctic Filchner Ice Shelf ENVELOPE(-40.000,-40.000,-79.000,-79.000) Support Force Glacier ENVELOPE(-47.500,-47.500,-83.083,-83.083) ENVELOPE(-45.921000,-45.662900,-82.370200,-82.375400) |