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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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 |
_version_ |
1766029354664460288 |