Evaluating ice‐rafted debris as a proxy for glacier calving in Upernavik Isfjord, NW Greenland
International audience Records of ice‐rafted debris (IRD) in sediments are commonly used as a proxy for iceberg production and to reconstruct past changes of glacier stability. However, the interpretation of IRD is complex as multiple processes modulate its variability. This study investigates the r...
Published in: | Journal of Quaternary Science |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Online Access: | https://hal.science/hal-02357292 https://hal.science/hal-02357292/document https://hal.science/hal-02357292/file/jqs.3095.pdf https://doi.org/10.1002/jqs.3095 |
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ftunivnantes:oai:HAL:hal-02357292v1 2023-05-15T16:21:22+02:00 Evaluating ice‐rafted debris as a proxy for glacier calving in Upernavik Isfjord, NW Greenland Vermassen, Flor Wangner, David Dyke, Laurence, Schmidt, Sabine Cordua, Amalie Kjær, Kurt Haubner, Konstanze Andresen, Camilla Geological Survey of Denmark and Greenland (GEUS) UMR 5805 Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) 2019-03-12 https://hal.science/hal-02357292 https://hal.science/hal-02357292/document https://hal.science/hal-02357292/file/jqs.3095.pdf https://doi.org/10.1002/jqs.3095 en eng HAL CCSD Wiley info:eu-repo/semantics/altIdentifier/doi/10.1002/jqs.3095 hal-02357292 https://hal.science/hal-02357292 https://hal.science/hal-02357292/document https://hal.science/hal-02357292/file/jqs.3095.pdf doi:10.1002/jqs.3095 http://creativecommons.org/licenses/by-nc-nd/ info:eu-repo/semantics/OpenAccess CC-BY-NC-ND ISSN: 0267-8179 EISSN: 1099-1417 Journal of Quaternary Science https://hal.science/hal-02357292 Journal of Quaternary Science, 2019, 34 (3), pp.258-267. ⟨10.1002/jqs.3095⟩ [SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2019 ftunivnantes https://doi.org/10.1002/jqs.3095 2023-02-08T04:11:40Z International audience Records of ice‐rafted debris (IRD) in sediments are commonly used as a proxy for iceberg production and to reconstruct past changes of glacier stability. However, the interpretation of IRD is complex as multiple processes modulate its variability. This study investigates the relationship between IRD variability and glaciological change by measuring IRD records from Upernavik Fjord and comparing these to frontal positions of Upernavik Isstrøm during the past century. Results show that the spatial variability of IRD deposition throughout the fjord is high, indicating that randomness inherent to IRD distorts the calving signal. However, we investigate whether IRD records can be combined to improve the reconstruction, as previously suggested, and show the importance of core site selection and number of cores on this approach. The outer‐fjord core compares relatively well to the observed front positions and this is reflected in the composite record: increased IRD deposition in 1937–1946, 1968–1980, and 1996–1999 occurred during periods of faster retreat. Comparison with climatic records shows that the calving episodes in the late ‘30 s/early ‘40 s and late ‘90 s are related to warm ocean and air temperatures, whereas intensified retreat and calving during the ‘70 s reflects partly an internal glacier response to the fjord geometry. Article in Journal/Newspaper glacier Greenland Upernavik Université de Nantes: HAL-UNIV-NANTES Greenland Isfjord ENVELOPE(-26.917,-26.917,73.333,73.333) Upernavik Isfjord ENVELOPE(-55.417,-55.417,72.917,72.917) Upernavik Isstrøm ENVELOPE(-54.500,-54.500,72.917,72.917) Journal of Quaternary Science 34 3 258 267 |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
[SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
[SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Vermassen, Flor Wangner, David Dyke, Laurence, Schmidt, Sabine Cordua, Amalie Kjær, Kurt Haubner, Konstanze Andresen, Camilla Evaluating ice‐rafted debris as a proxy for glacier calving in Upernavik Isfjord, NW Greenland |
topic_facet |
[SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience Records of ice‐rafted debris (IRD) in sediments are commonly used as a proxy for iceberg production and to reconstruct past changes of glacier stability. However, the interpretation of IRD is complex as multiple processes modulate its variability. This study investigates the relationship between IRD variability and glaciological change by measuring IRD records from Upernavik Fjord and comparing these to frontal positions of Upernavik Isstrøm during the past century. Results show that the spatial variability of IRD deposition throughout the fjord is high, indicating that randomness inherent to IRD distorts the calving signal. However, we investigate whether IRD records can be combined to improve the reconstruction, as previously suggested, and show the importance of core site selection and number of cores on this approach. The outer‐fjord core compares relatively well to the observed front positions and this is reflected in the composite record: increased IRD deposition in 1937–1946, 1968–1980, and 1996–1999 occurred during periods of faster retreat. Comparison with climatic records shows that the calving episodes in the late ‘30 s/early ‘40 s and late ‘90 s are related to warm ocean and air temperatures, whereas intensified retreat and calving during the ‘70 s reflects partly an internal glacier response to the fjord geometry. |
author2 |
Geological Survey of Denmark and Greenland (GEUS) UMR 5805 Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Vermassen, Flor Wangner, David Dyke, Laurence, Schmidt, Sabine Cordua, Amalie Kjær, Kurt Haubner, Konstanze Andresen, Camilla |
author_facet |
Vermassen, Flor Wangner, David Dyke, Laurence, Schmidt, Sabine Cordua, Amalie Kjær, Kurt Haubner, Konstanze Andresen, Camilla |
author_sort |
Vermassen, Flor |
title |
Evaluating ice‐rafted debris as a proxy for glacier calving in Upernavik Isfjord, NW Greenland |
title_short |
Evaluating ice‐rafted debris as a proxy for glacier calving in Upernavik Isfjord, NW Greenland |
title_full |
Evaluating ice‐rafted debris as a proxy for glacier calving in Upernavik Isfjord, NW Greenland |
title_fullStr |
Evaluating ice‐rafted debris as a proxy for glacier calving in Upernavik Isfjord, NW Greenland |
title_full_unstemmed |
Evaluating ice‐rafted debris as a proxy for glacier calving in Upernavik Isfjord, NW Greenland |
title_sort |
evaluating ice‐rafted debris as a proxy for glacier calving in upernavik isfjord, nw greenland |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://hal.science/hal-02357292 https://hal.science/hal-02357292/document https://hal.science/hal-02357292/file/jqs.3095.pdf https://doi.org/10.1002/jqs.3095 |
long_lat |
ENVELOPE(-26.917,-26.917,73.333,73.333) ENVELOPE(-55.417,-55.417,72.917,72.917) ENVELOPE(-54.500,-54.500,72.917,72.917) |
geographic |
Greenland Isfjord Upernavik Isfjord Upernavik Isstrøm |
geographic_facet |
Greenland Isfjord Upernavik Isfjord Upernavik Isstrøm |
genre |
glacier Greenland Upernavik |
genre_facet |
glacier Greenland Upernavik |
op_source |
ISSN: 0267-8179 EISSN: 1099-1417 Journal of Quaternary Science https://hal.science/hal-02357292 Journal of Quaternary Science, 2019, 34 (3), pp.258-267. ⟨10.1002/jqs.3095⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/jqs.3095 hal-02357292 https://hal.science/hal-02357292 https://hal.science/hal-02357292/document https://hal.science/hal-02357292/file/jqs.3095.pdf doi:10.1002/jqs.3095 |
op_rights |
http://creativecommons.org/licenses/by-nc-nd/ info:eu-repo/semantics/OpenAccess |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1002/jqs.3095 |
container_title |
Journal of Quaternary Science |
container_volume |
34 |
container_issue |
3 |
container_start_page |
258 |
op_container_end_page |
267 |
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1766009368638128128 |