Surface mass balance of Pine Island Glacier, West Antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ...
Airborne radar soundings of internal reflection layers were collected across the Pine Island (PIG) catchment area, West Antarctica, aboard the Polar 5 aircraft between 01 and 03 Dec 2014. An isochronal reflection layer was traced for a total distance of 2367 km to determine annual mean surface mass...
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ftdatacite:10.1594/pangaea.927004 2024-06-09T07:39:42+00:00 Surface mass balance of Pine Island Glacier, West Antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ... Kowalewski, Stefan Helm, Veit Morris, Elizabeth Mary Eisen, Olaf 2021 application/zip https://dx.doi.org/10.1594/pangaea.927004 https://doi.pangaea.de/10.1594/PANGAEA.927004 en eng PANGAEA https://store.pangaea.de/Publications/KowalewskiS-etal_2021/ReadMe_Metadata.zip https://dx.doi.org/10.5194/tc-15-1285-2021 https://store.pangaea.de/Publications/KowalewskiS-etal_2021/ReadMe_Metadata.zip https://dx.doi.org/10.5194/tc-14-229-2020 https://dx.doi.org/10.5194/tc-12-1479-2018 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Airborne Radar ASIRAS Pine Island Glacier SMB surface mass balance Publication Series of Datasets article Collection 2021 ftdatacite https://doi.org/10.1594/pangaea.92700410.5194/tc-15-1285-202110.5194/tc-14-229-202010.5194/tc-12-1479-2018 2024-05-13T12:44:57Z Airborne radar soundings of internal reflection layers were collected across the Pine Island (PIG) catchment area, West Antarctica, aboard the Polar 5 aircraft between 01 and 03 Dec 2014. An isochronal reflection layer was traced for a total distance of 2367 km to determine annual mean surface mass balance (SMB) for the period from approx. Nov 2004 to Dec 2014. Vertical firn density profiles were collected during the same measurement season along the flight track in the frame of the iSTAR campaign by means of Neutron Probe (NP) measurements. Annual markers were extracted from these profiles and used for the layer dating. A regional scale density-depth profile was estimated from all NP measurements and used for the conversion of two-way travel times (TWT) of the traced layer to mean annual SMB. Catchment wide SMB interpolation estimates were calculated by means of an ordinary logarithmic kriging (OLK) algorithm, which is applied to the alongtrack SMB estimates. Due to a data gap in the southern interior of ... : The results include complementary model results according to Donat-Magnin et al. (2020) and van Wessem et al. (2018). ... Article in Journal/Newspaper Antarc* Antarctica Pine Island Pine Island Glacier West Antarctica DataCite Metadata Store (German National Library of Science and Technology) Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) West Antarctica |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Airborne Radar ASIRAS Pine Island Glacier SMB surface mass balance |
spellingShingle |
Airborne Radar ASIRAS Pine Island Glacier SMB surface mass balance Kowalewski, Stefan Helm, Veit Morris, Elizabeth Mary Eisen, Olaf Surface mass balance of Pine Island Glacier, West Antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ... |
topic_facet |
Airborne Radar ASIRAS Pine Island Glacier SMB surface mass balance |
description |
Airborne radar soundings of internal reflection layers were collected across the Pine Island (PIG) catchment area, West Antarctica, aboard the Polar 5 aircraft between 01 and 03 Dec 2014. An isochronal reflection layer was traced for a total distance of 2367 km to determine annual mean surface mass balance (SMB) for the period from approx. Nov 2004 to Dec 2014. Vertical firn density profiles were collected during the same measurement season along the flight track in the frame of the iSTAR campaign by means of Neutron Probe (NP) measurements. Annual markers were extracted from these profiles and used for the layer dating. A regional scale density-depth profile was estimated from all NP measurements and used for the conversion of two-way travel times (TWT) of the traced layer to mean annual SMB. Catchment wide SMB interpolation estimates were calculated by means of an ordinary logarithmic kriging (OLK) algorithm, which is applied to the alongtrack SMB estimates. Due to a data gap in the southern interior of ... : The results include complementary model results according to Donat-Magnin et al. (2020) and van Wessem et al. (2018). ... |
format |
Article in Journal/Newspaper |
author |
Kowalewski, Stefan Helm, Veit Morris, Elizabeth Mary Eisen, Olaf |
author_facet |
Kowalewski, Stefan Helm, Veit Morris, Elizabeth Mary Eisen, Olaf |
author_sort |
Kowalewski, Stefan |
title |
Surface mass balance of Pine Island Glacier, West Antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ... |
title_short |
Surface mass balance of Pine Island Glacier, West Antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ... |
title_full |
Surface mass balance of Pine Island Glacier, West Antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ... |
title_fullStr |
Surface mass balance of Pine Island Glacier, West Antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ... |
title_full_unstemmed |
Surface mass balance of Pine Island Glacier, West Antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ... |
title_sort |
surface mass balance of pine island glacier, west antarctica over the period 2005-2014, derived from airborne radar soundings and neutron probe measurements ... |
publisher |
PANGAEA |
publishDate |
2021 |
url |
https://dx.doi.org/10.1594/pangaea.927004 https://doi.pangaea.de/10.1594/PANGAEA.927004 |
long_lat |
ENVELOPE(-101.000,-101.000,-75.000,-75.000) |
geographic |
Pine Island Glacier West Antarctica |
geographic_facet |
Pine Island Glacier West Antarctica |
genre |
Antarc* Antarctica Pine Island Pine Island Glacier West Antarctica |
genre_facet |
Antarc* Antarctica Pine Island Pine Island Glacier West Antarctica |
op_relation |
https://store.pangaea.de/Publications/KowalewskiS-etal_2021/ReadMe_Metadata.zip https://dx.doi.org/10.5194/tc-15-1285-2021 https://store.pangaea.de/Publications/KowalewskiS-etal_2021/ReadMe_Metadata.zip https://dx.doi.org/10.5194/tc-14-229-2020 https://dx.doi.org/10.5194/tc-12-1479-2018 |
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.92700410.5194/tc-15-1285-202110.5194/tc-14-229-202010.5194/tc-12-1479-2018 |
_version_ |
1801381204853784576 |