Environmental conditions for snow cornice formation in a wind tunnel
Snow cornices are common snow patterns in mountain ridge, which have potential to trigger snow avalanches. In this work, we present a series of wind tunnel experiments in a cold laboratory to simulate the formation processes of snow cornices. We quantitatively investigated the growth rates of snow c...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5016693 2023-06-11T04:17:12+02:00 Environmental conditions for snow cornice formation in a wind tunnel Yu, H. Li, G. Walter, B. Michael, L. Zhang, J. Huang, N. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016693 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0797 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016693 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-0797 2023-05-07T23:38:37Z Snow cornices are common snow patterns in mountain ridge, which have potential to trigger snow avalanches. In this work, we present a series of wind tunnel experiments in a cold laboratory to simulate the formation processes of snow cornices. We quantitatively investigated the growth rates of snow cornice in length and in thickness, as well as the airborne particle concentration by using a COMOS camera. From a micro view, we also observed the snow particle trajectory that can stick on the edge and form the cornice through high-speed camera. Based on the experimental results, we explained the mechanism of the formation and development of snow cornices, and the effects of the environmental factors on the cornice growth such as air temperature, wind speed. A conceptual model that can predict the horizontal growth rate of snow cornice in field is established. Our predicted results are in good agreement with the field observation data from Gruvefjellet, Svalbard. Based on the physics of drifting snow, our results provide a new insight into snow cornice formation and improve the understanding of cornice processes that can influence avalanche activities. The experimental results and the conceptual model can be useful in future snow cornice simulation and prediction work for cornice-induced avalanches. Conference Object Svalbard GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Gruvefjellet ENVELOPE(15.633,15.633,78.200,78.200) Svalbard |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
English |
description |
Snow cornices are common snow patterns in mountain ridge, which have potential to trigger snow avalanches. In this work, we present a series of wind tunnel experiments in a cold laboratory to simulate the formation processes of snow cornices. We quantitatively investigated the growth rates of snow cornice in length and in thickness, as well as the airborne particle concentration by using a COMOS camera. From a micro view, we also observed the snow particle trajectory that can stick on the edge and form the cornice through high-speed camera. Based on the experimental results, we explained the mechanism of the formation and development of snow cornices, and the effects of the environmental factors on the cornice growth such as air temperature, wind speed. A conceptual model that can predict the horizontal growth rate of snow cornice in field is established. Our predicted results are in good agreement with the field observation data from Gruvefjellet, Svalbard. Based on the physics of drifting snow, our results provide a new insight into snow cornice formation and improve the understanding of cornice processes that can influence avalanche activities. The experimental results and the conceptual model can be useful in future snow cornice simulation and prediction work for cornice-induced avalanches. |
format |
Conference Object |
author |
Yu, H. Li, G. Walter, B. Michael, L. Zhang, J. Huang, N. |
spellingShingle |
Yu, H. Li, G. Walter, B. Michael, L. Zhang, J. Huang, N. Environmental conditions for snow cornice formation in a wind tunnel |
author_facet |
Yu, H. Li, G. Walter, B. Michael, L. Zhang, J. Huang, N. |
author_sort |
Yu, H. |
title |
Environmental conditions for snow cornice formation in a wind tunnel |
title_short |
Environmental conditions for snow cornice formation in a wind tunnel |
title_full |
Environmental conditions for snow cornice formation in a wind tunnel |
title_fullStr |
Environmental conditions for snow cornice formation in a wind tunnel |
title_full_unstemmed |
Environmental conditions for snow cornice formation in a wind tunnel |
title_sort |
environmental conditions for snow cornice formation in a wind tunnel |
publishDate |
2023 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016693 |
long_lat |
ENVELOPE(15.633,15.633,78.200,78.200) |
geographic |
Gruvefjellet Svalbard |
geographic_facet |
Gruvefjellet Svalbard |
genre |
Svalbard |
genre_facet |
Svalbard |
op_source |
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0797 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016693 |
op_doi |
https://doi.org/10.57757/IUGG23-0797 |
_version_ |
1768376128804749312 |