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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Bibliographic Details
Main Authors: Kowalewski, Stefan, Helm, Veit, Morris, Elizabeth Mary, Eisen, Olaf
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2021
Subjects:
SMB
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.927004
https://doi.org/10.1594/PANGAEA.927004
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.927004
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
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 PIG, complementary SMB estimates from RACMO (doi:10.5194/tc-12-1479-2018) and MAR (doi:10.5194/tc-14-229-2020) regional climate models were used to produce a catchment wide mean annual SMB map. Amongst others, total mass input can be derived from this map to assess the mass balance of PIG for the considered SMB averaging period. This dataset includes the level 1b processed radargrams, the traced layer in units of TWT and mean annual SMB, and SMB OLK maps. The latter include error grids as well as the partitioning map between OLK SMB estimates and complementary simulated SMB estimates for the PIG catchment area.
format Other/Unknown Material
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://doi.pangaea.de/10.1594/PANGAEA.927004
https://doi.org/10.1594/PANGAEA.927004
op_coverage MEDIAN LATITUDE: -75.265692 * MEDIAN LONGITUDE: -93.439438 * SOUTH-BOUND LATITUDE: -79.758250 * WEST-BOUND LONGITUDE: -100.775130 * NORTH-BOUND LATITUDE: -67.566470 * EAST-BOUND LONGITUDE: -68.128550 * DATE/TIME START: 2014-12-01T16:59:00 * DATE/TIME END: 2014-12-03T16:47:00
long_lat ENVELOPE(-100.775130,-68.128550,-67.566470,-79.758250)
genre Antarc*
Antarctica
Pine Island
Pine Island Glacier
The Cryosphere
West Antarctica
genre_facet Antarc*
Antarctica
Pine Island
Pine Island Glacier
The Cryosphere
West Antarctica
op_relation Kowalewski, Stefan; Helm, Veit; Morris, Elizabeth Mary; Eisen, Olaf (2021): The regional-scale surface mass balance of Pine Island Glacier, West Antarctica, over the period 2005–2014, derived from airborne radar soundings and neutron probe measurements. The Cryosphere, 15(3), 1285-1305, https://doi.org/10.5194/tc-15-1285-2021
Surface mass balance of Pine Island Glacier - ReadMe and Metadata. https://store.pangaea.de/Publications/KowalewskiS-etal_2021/ReadMe_Metadata.zip
Donat-Magnin, Marion; Jourdain, Nicolas C; Gallée, Hubert; Amory, Charles; Kittel, Christoph; Fettweis, Xavier; Wille, Jonathan D; Favier, Vincent; Drira, Amine; Agosta, Cécile (2020): Interannual variability of summer surface mass balance and surface melting in the Amundsen sector, West Antarctica. The Cryosphere, 14, 229-249, https://doi.org/10.5194/tc-14-229-2020
van Wessem, Jan Melchior; van de Berg, Willem Jan; Noël, Brice P Y; van Meijgaard, Erik; Amory, Charles; Birnbaum, Gerit; Jakobs, Constantijn L; Krüger, Konstantin; Lenaerts, Jan T M; Lhermitte, Stef; Ligtenberg, Stefan R M; Medley, Brooke; Reijmer, Carleen H; Van Tricht, Kristof; Trusel, L D; Wouters, Bert; van Ulft, Hubertus H; Wuite, Jan; van den Broeke, Michiel R (2018): Modelling the climate and surface mass balance of polar ice sheets using RACMO2 – Part 2: Antarctica (1979–2016). The Cryosphere, 12(4), 1479-1498, https://doi.org/10.5194/tc-12-1479-2018
https://doi.pangaea.de/10.1594/PANGAEA.927004
https://doi.org/10.1594/PANGAEA.927004
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.92700410.5194/tc-15-1285-202110.5194/tc-14-229-202010.5194/tc-12-1479-2018
_version_ 1810289096697839616
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.927004 2024-09-15T17:48:05+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 MEDIAN LATITUDE: -75.265692 * MEDIAN LONGITUDE: -93.439438 * SOUTH-BOUND LATITUDE: -79.758250 * WEST-BOUND LONGITUDE: -100.775130 * NORTH-BOUND LATITUDE: -67.566470 * EAST-BOUND LONGITUDE: -68.128550 * DATE/TIME START: 2014-12-01T16:59:00 * DATE/TIME END: 2014-12-03T16:47:00 2021 application/zip, 24 datasets https://doi.pangaea.de/10.1594/PANGAEA.927004 https://doi.org/10.1594/PANGAEA.927004 en eng PANGAEA Kowalewski, Stefan; Helm, Veit; Morris, Elizabeth Mary; Eisen, Olaf (2021): The regional-scale surface mass balance of Pine Island Glacier, West Antarctica, over the period 2005–2014, derived from airborne radar soundings and neutron probe measurements. The Cryosphere, 15(3), 1285-1305, https://doi.org/10.5194/tc-15-1285-2021 Surface mass balance of Pine Island Glacier - ReadMe and Metadata. https://store.pangaea.de/Publications/KowalewskiS-etal_2021/ReadMe_Metadata.zip Donat-Magnin, Marion; Jourdain, Nicolas C; Gallée, Hubert; Amory, Charles; Kittel, Christoph; Fettweis, Xavier; Wille, Jonathan D; Favier, Vincent; Drira, Amine; Agosta, Cécile (2020): Interannual variability of summer surface mass balance and surface melting in the Amundsen sector, West Antarctica. The Cryosphere, 14, 229-249, https://doi.org/10.5194/tc-14-229-2020 van Wessem, Jan Melchior; van de Berg, Willem Jan; Noël, Brice P Y; van Meijgaard, Erik; Amory, Charles; Birnbaum, Gerit; Jakobs, Constantijn L; Krüger, Konstantin; Lenaerts, Jan T M; Lhermitte, Stef; Ligtenberg, Stefan R M; Medley, Brooke; Reijmer, Carleen H; Van Tricht, Kristof; Trusel, L D; Wouters, Bert; van Ulft, Hubertus H; Wuite, Jan; van den Broeke, Michiel R (2018): Modelling the climate and surface mass balance of polar ice sheets using RACMO2 – Part 2: Antarctica (1979–2016). The Cryosphere, 12(4), 1479-1498, https://doi.org/10.5194/tc-12-1479-2018 https://doi.pangaea.de/10.1594/PANGAEA.927004 https://doi.org/10.1594/PANGAEA.927004 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Airborne Radar ASIRAS Pine Island Glacier SMB surface mass balance dataset publication series 2021 ftpangaea https://doi.org/10.1594/PANGAEA.92700410.5194/tc-15-1285-202110.5194/tc-14-229-202010.5194/tc-12-1479-2018 2024-07-24T02:31:21Z 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 PIG, complementary SMB estimates from RACMO (doi:10.5194/tc-12-1479-2018) and MAR (doi:10.5194/tc-14-229-2020) regional climate models were used to produce a catchment wide mean annual SMB map. Amongst others, total mass input can be derived from this map to assess the mass balance of PIG for the considered SMB averaging period. This dataset includes the level 1b processed radargrams, the traced layer in units of TWT and mean annual SMB, and SMB OLK maps. The latter include error grids as well as the partitioning map between OLK SMB estimates and complementary simulated SMB estimates for the PIG catchment area. Other/Unknown Material Antarc* Antarctica Pine Island Pine Island Glacier The Cryosphere West Antarctica PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-100.775130,-68.128550,-67.566470,-79.758250)