Waterfall ice: formation, structure and evolution
International audience For the first time, to our knowledge, a scientific study of the formation and evolution of waterfall ice, the ephemeral ice structures that form from the freezing of liquid water seeping on steep rock, was performed. We surveyed and analysed three waterfall ice structures near...
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ftinsu:oai:HAL:hal-01746981v1 2024-04-28T08:26:48+00:00 Waterfall ice: formation, structure and evolution Montagnat, M. Weiss, J. Cinquin-Lapierre, B. Labory, P, A Moreau, L. Damilano, F. Lavigne, D. Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Mountain Guide, Chamonix 2010-02-24 https://hal.science/hal-01746981 https://hal.science/hal-01746981/document https://hal.science/hal-01746981/file/montagnat2010_waterfallIce.pdf https://doi.org/10.3189/002214310791968412 en eng HAL CCSD International Glaciological Society info:eu-repo/semantics/altIdentifier/doi/10.3189/002214310791968412 hal-01746981 https://hal.science/hal-01746981 https://hal.science/hal-01746981/document https://hal.science/hal-01746981/file/montagnat2010_waterfallIce.pdf doi:10.3189/002214310791968412 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0022-1430 EISSN: 1727-5652 Journal of Glaciology https://hal.science/hal-01746981 Journal of Glaciology, 2010, pp.225-234. ⟨10.3189/002214310791968412⟩ [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2010 ftinsu https://doi.org/10.3189/002214310791968412 2024-04-05T00:46:12Z International audience For the first time, to our knowledge, a scientific study of the formation and evolution of waterfall ice, the ephemeral ice structures that form from the freezing of liquid water seeping on steep rock, was performed. We surveyed and analysed three waterfall ice structures near Glacier d'Argentière, Mont Blanc massif, France, between winter 2007 and spring 2009. We reconstruct the global evolution of two vertical ice structures using automatic digital cameras, while the internal ice microstructure was analysed using ice coring and sampling. Macro-and microstructural observations are considered, along with temperature conditions recorded at a nearby meteorological station and directly within the ice structure. They reveal that vertical structures initially grow rapidly from the aggregation of stalactites with microstructures indicative of temperature conditions during their crystallization. After this initial stage, the volume of the ice structure reaches an asymptotic value, as water continues to flow inside the structure, isolated from the outside cold ice; the outer surface remains dry. At the end of the season, the collapse of the free-standing structure does not occur by progressive melting, but is initiated by a horizontal crack propagation at the top. The initiation of this crack seems to be triggered by a drastic temperature decrease. Article in Journal/Newspaper Journal of Glaciology Institut national des sciences de l'Univers: HAL-INSU Journal of Glaciology 56 196 225 234 |
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Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
spellingShingle |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology Montagnat, M. Weiss, J. Cinquin-Lapierre, B. Labory, P, A Moreau, L. Damilano, F. Lavigne, D. Waterfall ice: formation, structure and evolution |
topic_facet |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
description |
International audience For the first time, to our knowledge, a scientific study of the formation and evolution of waterfall ice, the ephemeral ice structures that form from the freezing of liquid water seeping on steep rock, was performed. We surveyed and analysed three waterfall ice structures near Glacier d'Argentière, Mont Blanc massif, France, between winter 2007 and spring 2009. We reconstruct the global evolution of two vertical ice structures using automatic digital cameras, while the internal ice microstructure was analysed using ice coring and sampling. Macro-and microstructural observations are considered, along with temperature conditions recorded at a nearby meteorological station and directly within the ice structure. They reveal that vertical structures initially grow rapidly from the aggregation of stalactites with microstructures indicative of temperature conditions during their crystallization. After this initial stage, the volume of the ice structure reaches an asymptotic value, as water continues to flow inside the structure, isolated from the outside cold ice; the outer surface remains dry. At the end of the season, the collapse of the free-standing structure does not occur by progressive melting, but is initiated by a horizontal crack propagation at the top. The initiation of this crack seems to be triggered by a drastic temperature decrease. |
author2 |
Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Mountain Guide, Chamonix |
format |
Article in Journal/Newspaper |
author |
Montagnat, M. Weiss, J. Cinquin-Lapierre, B. Labory, P, A Moreau, L. Damilano, F. Lavigne, D. |
author_facet |
Montagnat, M. Weiss, J. Cinquin-Lapierre, B. Labory, P, A Moreau, L. Damilano, F. Lavigne, D. |
author_sort |
Montagnat, M. |
title |
Waterfall ice: formation, structure and evolution |
title_short |
Waterfall ice: formation, structure and evolution |
title_full |
Waterfall ice: formation, structure and evolution |
title_fullStr |
Waterfall ice: formation, structure and evolution |
title_full_unstemmed |
Waterfall ice: formation, structure and evolution |
title_sort |
waterfall ice: formation, structure and evolution |
publisher |
HAL CCSD |
publishDate |
2010 |
url |
https://hal.science/hal-01746981 https://hal.science/hal-01746981/document https://hal.science/hal-01746981/file/montagnat2010_waterfallIce.pdf https://doi.org/10.3189/002214310791968412 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
ISSN: 0022-1430 EISSN: 1727-5652 Journal of Glaciology https://hal.science/hal-01746981 Journal of Glaciology, 2010, pp.225-234. ⟨10.3189/002214310791968412⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.3189/002214310791968412 hal-01746981 https://hal.science/hal-01746981 https://hal.science/hal-01746981/document https://hal.science/hal-01746981/file/montagnat2010_waterfallIce.pdf doi:10.3189/002214310791968412 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.3189/002214310791968412 |
container_title |
Journal of Glaciology |
container_volume |
56 |
container_issue |
196 |
container_start_page |
225 |
op_container_end_page |
234 |
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1797586039074717696 |