MagnaProbe snow thickness during a floe-scale walk on station PS81/506_GPS1 ...
Snow depth measured during a floe-scale walk (FSW) from Magnaprobe (MP), see Sturm and Holmgren (2018) for details. Floe-scale walks were performed to capture variability on a larger scale than the laser scan field. ... : Coordinates:============X and Y coordinates are relative to a GPS base station...
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Online Access: | https://dx.doi.org/10.1594/pangaea.933566 https://doi.pangaea.de/10.1594/PANGAEA.933566 |
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ftdatacite:10.1594/pangaea.933566 2024-09-30T14:43:11+00:00 MagnaProbe snow thickness during a floe-scale walk on station PS81/506_GPS1 ... Wever, Nander White, Seth Hunkeler, Priska A Maksym, Ted Leonard, Katherine C 2021 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.933566 https://doi.pangaea.de/10.1594/PANGAEA.933566 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.933584 https://dx.doi.org/10.1017/jog.2021.54 https://dx.doi.org/10.1029/2018wr023559 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Ice thickness Sea ice snow depth spatial variability Cartesian coordinate, x Cartesian coordinate, y Snow thickness Global positioning system MagnaProbe, Snow-Hydro ANT-XXIX/6 Polarstern Dataset dataset 2021 ftdatacite https://doi.org/10.1594/pangaea.93356610.1594/pangaea.93358410.1017/jog.2021.5410.1029/2018wr023559 2024-09-02T09:14:02Z Snow depth measured during a floe-scale walk (FSW) from Magnaprobe (MP), see Sturm and Holmgren (2018) for details. Floe-scale walks were performed to capture variability on a larger scale than the laser scan field. ... : Coordinates:============X and Y coordinates are relative to a GPS base station installed on each floe. Coordinates were determined using post-processing kinematic GPS (PPK-GPS), and corrected for floe ration and drift. Coordinates of measurements inside the laser scanning area were particularly carefully processed to collocate measurements as accurately as possible (within a few cm). The vertical height above sea level in the TLS data was determined by using reflectors on poles. Upon installation of these reflector poles, the ice was drilled through and the height of the reflector above sea level was determined. For details, see Wever et al. (2021).On the floe scale walk, magnaprobe coordinates have been equally processed as in the laser scanning area. However, for the GEM-2 instrument, the position of the magnaprobe was taken for the corresponding time stamp in the GEM-2 data. Since the GEM-2 instrument was following the Magnaprobe surveyor with a few m distance, this leads to less precise positioning. ... Dataset Sea ice DataCite Sturm ENVELOPE(162.967,162.967,-71.050,-71.050) Wever ENVELOPE(-62.700,-62.700,-72.164,-72.164) |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Ice thickness Sea ice snow depth spatial variability Cartesian coordinate, x Cartesian coordinate, y Snow thickness Global positioning system MagnaProbe, Snow-Hydro ANT-XXIX/6 Polarstern |
spellingShingle |
Ice thickness Sea ice snow depth spatial variability Cartesian coordinate, x Cartesian coordinate, y Snow thickness Global positioning system MagnaProbe, Snow-Hydro ANT-XXIX/6 Polarstern Wever, Nander White, Seth Hunkeler, Priska A Maksym, Ted Leonard, Katherine C MagnaProbe snow thickness during a floe-scale walk on station PS81/506_GPS1 ... |
topic_facet |
Ice thickness Sea ice snow depth spatial variability Cartesian coordinate, x Cartesian coordinate, y Snow thickness Global positioning system MagnaProbe, Snow-Hydro ANT-XXIX/6 Polarstern |
description |
Snow depth measured during a floe-scale walk (FSW) from Magnaprobe (MP), see Sturm and Holmgren (2018) for details. Floe-scale walks were performed to capture variability on a larger scale than the laser scan field. ... : Coordinates:============X and Y coordinates are relative to a GPS base station installed on each floe. Coordinates were determined using post-processing kinematic GPS (PPK-GPS), and corrected for floe ration and drift. Coordinates of measurements inside the laser scanning area were particularly carefully processed to collocate measurements as accurately as possible (within a few cm). The vertical height above sea level in the TLS data was determined by using reflectors on poles. Upon installation of these reflector poles, the ice was drilled through and the height of the reflector above sea level was determined. For details, see Wever et al. (2021).On the floe scale walk, magnaprobe coordinates have been equally processed as in the laser scanning area. However, for the GEM-2 instrument, the position of the magnaprobe was taken for the corresponding time stamp in the GEM-2 data. Since the GEM-2 instrument was following the Magnaprobe surveyor with a few m distance, this leads to less precise positioning. ... |
format |
Dataset |
author |
Wever, Nander White, Seth Hunkeler, Priska A Maksym, Ted Leonard, Katherine C |
author_facet |
Wever, Nander White, Seth Hunkeler, Priska A Maksym, Ted Leonard, Katherine C |
author_sort |
Wever, Nander |
title |
MagnaProbe snow thickness during a floe-scale walk on station PS81/506_GPS1 ... |
title_short |
MagnaProbe snow thickness during a floe-scale walk on station PS81/506_GPS1 ... |
title_full |
MagnaProbe snow thickness during a floe-scale walk on station PS81/506_GPS1 ... |
title_fullStr |
MagnaProbe snow thickness during a floe-scale walk on station PS81/506_GPS1 ... |
title_full_unstemmed |
MagnaProbe snow thickness during a floe-scale walk on station PS81/506_GPS1 ... |
title_sort |
magnaprobe snow thickness during a floe-scale walk on station ps81/506_gps1 ... |
publisher |
PANGAEA |
publishDate |
2021 |
url |
https://dx.doi.org/10.1594/pangaea.933566 https://doi.pangaea.de/10.1594/PANGAEA.933566 |
long_lat |
ENVELOPE(162.967,162.967,-71.050,-71.050) ENVELOPE(-62.700,-62.700,-72.164,-72.164) |
geographic |
Sturm Wever |
geographic_facet |
Sturm Wever |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
https://dx.doi.org/10.1594/pangaea.933584 https://dx.doi.org/10.1017/jog.2021.54 https://dx.doi.org/10.1029/2018wr023559 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.93356610.1594/pangaea.93358410.1017/jog.2021.5410.1029/2018wr023559 |
_version_ |
1811645094614269952 |