Ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine ice drilling site Colle Gnifetti, Swiss/Italian Alps

Ice-flow modeling studies were conducted to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine drilling site Colle Gnifetti, Swiss/Italian Alps. Backwards trajectories starting from the borehole sites at different depths are calculated in order to estimate ice-core...

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Main Authors: Licciulli, Carlo, Bohleber, Pascal, Lier, Josef, Gagliardini, Olivier, Hoelzle, Martin, Eisen, Olaf
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.906016
https://doi.org/10.1594/PANGAEA.906016
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record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.906016 2023-05-15T16:38:59+02:00 Ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine ice drilling site Colle Gnifetti, Swiss/Italian Alps Licciulli, Carlo Bohleber, Pascal Lier, Josef Gagliardini, Olivier Hoelzle, Martin Eisen, Olaf MEDIAN LATITUDE: 45.929014 * MEDIAN LONGITUDE: 7.875899 * SOUTH-BOUND LATITUDE: 45.928190 * WEST-BOUND LONGITUDE: 7.873650 * NORTH-BOUND LATITUDE: 45.929720 * EAST-BOUND LONGITUDE: 7.876960 * DATE/TIME START: 2005-08-28T00:00:00 * DATE/TIME END: 2013-08-11T00:00:00 2019-09-17 application/zip, 7 datasets https://doi.pangaea.de/10.1594/PANGAEA.906016 https://doi.org/10.1594/PANGAEA.906016 en eng PANGAEA Licciulli, Carlo (2018): Full Stokes ice-flow modeling of the high-Alpine glacier saddle Colle Gnifetti, Monte Rosa: Flow field characterization for an improved interpretation of the ice-core records. Dissertation, Ruperto-Carola University of Heidelberg, Germany, Combined Faculties for the Natural Sciences and for Mathematics, 138 pp, https://doi.org/10.11588/heidok.00023981 https://doi.pangaea.de/10.1594/PANGAEA.906016 https://doi.org/10.1594/PANGAEA.906016 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Licciulli, Carlo; Bohleber, Pascal; Lier, Josef; Gagliardini, Olivier; Hoelzle, Martin; Eisen, Olaf (2019): A full Stokes ice-flow model to assist the interpretation of millennial-scale ice cores at the high-Alpine drilling site Colle Gnifetti, Swiss/Italian Alps. Journal of Glaciology, 1-14, https://doi.org/10.1017/jog.2019.82 Glacier modelling Ice dynamics Mountain glaciers Paleoclimate Dataset 2019 ftpangaea https://doi.org/10.1594/PANGAEA.906016 https://doi.org/10.1017/jog.2019.82 https://doi.org/10.11588/heidok.00023981 2023-01-20T07:34:25Z Ice-flow modeling studies were conducted to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine drilling site Colle Gnifetti, Swiss/Italian Alps. Backwards trajectories starting from the borehole sites at different depths are calculated in order to estimate ice-core catchment areas. The position of source points identified on the glacier surface is provided in the Swiss coordinate system (LV03) and in the UTM system. The uncertainty of the position of the source points is about 10% of the distance from the corresponding drill site. The ice-flow model also provides ice-core chronologies with an uncertainty of about 20%. Apart from the KCI core, the other four model chronologies are well in agreement with experimental results. Inclination angles of the boreholes KCC and KCI were measured in September 2016 (i.e. 3 and 11 years after drilling, respectively) to validate the modeled velocity field. The measurements were performed twice: downwards (from the top to the bottom of the borehole) and upwards. The uncertainty of the measurements is 1.9° and is estimated considering the diameter of the borehole and the size of the inclinometer probe. The uncertainty of the measurements is dominated by the potentially wrong (i.e. non-parallel to the borehole walls) positioning of the inclinometer probe inside the borehole. The quantity "Q orientation" indicates whether the inclinometer probe was likely correctly aligned with the borehole walls (Q orientation=1) or not (Q orientation=0). Dataset ice core Journal of Glaciology PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(7.873650,7.876960,45.929720,45.928190)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Glacier modelling
Ice dynamics
Mountain glaciers
Paleoclimate
spellingShingle Glacier modelling
Ice dynamics
Mountain glaciers
Paleoclimate
Licciulli, Carlo
Bohleber, Pascal
Lier, Josef
Gagliardini, Olivier
Hoelzle, Martin
Eisen, Olaf
Ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine ice drilling site Colle Gnifetti, Swiss/Italian Alps
topic_facet Glacier modelling
Ice dynamics
Mountain glaciers
Paleoclimate
description Ice-flow modeling studies were conducted to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine drilling site Colle Gnifetti, Swiss/Italian Alps. Backwards trajectories starting from the borehole sites at different depths are calculated in order to estimate ice-core catchment areas. The position of source points identified on the glacier surface is provided in the Swiss coordinate system (LV03) and in the UTM system. The uncertainty of the position of the source points is about 10% of the distance from the corresponding drill site. The ice-flow model also provides ice-core chronologies with an uncertainty of about 20%. Apart from the KCI core, the other four model chronologies are well in agreement with experimental results. Inclination angles of the boreholes KCC and KCI were measured in September 2016 (i.e. 3 and 11 years after drilling, respectively) to validate the modeled velocity field. The measurements were performed twice: downwards (from the top to the bottom of the borehole) and upwards. The uncertainty of the measurements is 1.9° and is estimated considering the diameter of the borehole and the size of the inclinometer probe. The uncertainty of the measurements is dominated by the potentially wrong (i.e. non-parallel to the borehole walls) positioning of the inclinometer probe inside the borehole. The quantity "Q orientation" indicates whether the inclinometer probe was likely correctly aligned with the borehole walls (Q orientation=1) or not (Q orientation=0).
format Dataset
author Licciulli, Carlo
Bohleber, Pascal
Lier, Josef
Gagliardini, Olivier
Hoelzle, Martin
Eisen, Olaf
author_facet Licciulli, Carlo
Bohleber, Pascal
Lier, Josef
Gagliardini, Olivier
Hoelzle, Martin
Eisen, Olaf
author_sort Licciulli, Carlo
title Ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine ice drilling site Colle Gnifetti, Swiss/Italian Alps
title_short Ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine ice drilling site Colle Gnifetti, Swiss/Italian Alps
title_full Ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine ice drilling site Colle Gnifetti, Swiss/Italian Alps
title_fullStr Ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine ice drilling site Colle Gnifetti, Swiss/Italian Alps
title_full_unstemmed Ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-Alpine ice drilling site Colle Gnifetti, Swiss/Italian Alps
title_sort ice-flow modeling results to assist the interpretation of millennial-scale ice cores recovered at the high-alpine ice drilling site colle gnifetti, swiss/italian alps
publisher PANGAEA
publishDate 2019
url https://doi.pangaea.de/10.1594/PANGAEA.906016
https://doi.org/10.1594/PANGAEA.906016
op_coverage MEDIAN LATITUDE: 45.929014 * MEDIAN LONGITUDE: 7.875899 * SOUTH-BOUND LATITUDE: 45.928190 * WEST-BOUND LONGITUDE: 7.873650 * NORTH-BOUND LATITUDE: 45.929720 * EAST-BOUND LONGITUDE: 7.876960 * DATE/TIME START: 2005-08-28T00:00:00 * DATE/TIME END: 2013-08-11T00:00:00
long_lat ENVELOPE(7.873650,7.876960,45.929720,45.928190)
genre ice core
Journal of Glaciology
genre_facet ice core
Journal of Glaciology
op_source Supplement to: Licciulli, Carlo; Bohleber, Pascal; Lier, Josef; Gagliardini, Olivier; Hoelzle, Martin; Eisen, Olaf (2019): A full Stokes ice-flow model to assist the interpretation of millennial-scale ice cores at the high-Alpine drilling site Colle Gnifetti, Swiss/Italian Alps. Journal of Glaciology, 1-14, https://doi.org/10.1017/jog.2019.82
op_relation Licciulli, Carlo (2018): Full Stokes ice-flow modeling of the high-Alpine glacier saddle Colle Gnifetti, Monte Rosa: Flow field characterization for an improved interpretation of the ice-core records. Dissertation, Ruperto-Carola University of Heidelberg, Germany, Combined Faculties for the Natural Sciences and for Mathematics, 138 pp, https://doi.org/10.11588/heidok.00023981
https://doi.pangaea.de/10.1594/PANGAEA.906016
https://doi.org/10.1594/PANGAEA.906016
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.906016
https://doi.org/10.1017/jog.2019.82
https://doi.org/10.11588/heidok.00023981
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