Marine outlet glacier dynamics, steady states and steady-state stability

Laterally confined marine outlet glaciers exhibit a diverse range of behaviours. This study investigates time-evolving and steady configurations of such glaciers. Using simplified analytic models, it determines conditions for steady states, their stability and expressions for the rate of the calving...

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Published in:Journal of Glaciology
Main Author: O. V. Sergienko
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2022
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.13
https://doaj.org/article/8103795a2a1e41f4be27a0f857214103
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spelling ftdoajarticles:oai:doaj.org/article:8103795a2a1e41f4be27a0f857214103 2023-05-15T16:57:33+02:00 Marine outlet glacier dynamics, steady states and steady-state stability O. V. Sergienko 2022-10-01T00:00:00Z https://doi.org/10.1017/jog.2022.13 https://doaj.org/article/8103795a2a1e41f4be27a0f857214103 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000132/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.13 0022-1430 1727-5652 https://doaj.org/article/8103795a2a1e41f4be27a0f857214103 Journal of Glaciology, Vol 68, Pp 946-960 (2022) Glacier flow glacier modelling ice dynamics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.1017/jog.2022.13 2023-03-12T01:30:54Z Laterally confined marine outlet glaciers exhibit a diverse range of behaviours. This study investigates time-evolving and steady configurations of such glaciers. Using simplified analytic models, it determines conditions for steady states, their stability and expressions for the rate of the calving-front migration for three widely used calving rules. It also investigates the effects of ice mélange when it is present. The results show that ice flux at the terminus is an implicit function of ice thickness that depends on the glacier geometric and dynamic parameters. As a consequence, stability of steady-state configurations is determined by a complex combination of these parameters, specifics of the calving rule and the details of mélange stress conditions. The derived expressions of the rate of terminus migration suggest a non-linear feedback between the migration rate and the calving-front position. A close agreement between the obtained analytic expressions and numerical simulations suggests that these expressions can be used to gain insights into the observed behaviour of the glaciers and also to use observations to improve understanding of calving conditions. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 15
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Glacier flow
glacier modelling
ice dynamics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Glacier flow
glacier modelling
ice dynamics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
O. V. Sergienko
Marine outlet glacier dynamics, steady states and steady-state stability
topic_facet Glacier flow
glacier modelling
ice dynamics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Laterally confined marine outlet glaciers exhibit a diverse range of behaviours. This study investigates time-evolving and steady configurations of such glaciers. Using simplified analytic models, it determines conditions for steady states, their stability and expressions for the rate of the calving-front migration for three widely used calving rules. It also investigates the effects of ice mélange when it is present. The results show that ice flux at the terminus is an implicit function of ice thickness that depends on the glacier geometric and dynamic parameters. As a consequence, stability of steady-state configurations is determined by a complex combination of these parameters, specifics of the calving rule and the details of mélange stress conditions. The derived expressions of the rate of terminus migration suggest a non-linear feedback between the migration rate and the calving-front position. A close agreement between the obtained analytic expressions and numerical simulations suggests that these expressions can be used to gain insights into the observed behaviour of the glaciers and also to use observations to improve understanding of calving conditions.
format Article in Journal/Newspaper
author O. V. Sergienko
author_facet O. V. Sergienko
author_sort O. V. Sergienko
title Marine outlet glacier dynamics, steady states and steady-state stability
title_short Marine outlet glacier dynamics, steady states and steady-state stability
title_full Marine outlet glacier dynamics, steady states and steady-state stability
title_fullStr Marine outlet glacier dynamics, steady states and steady-state stability
title_full_unstemmed Marine outlet glacier dynamics, steady states and steady-state stability
title_sort marine outlet glacier dynamics, steady states and steady-state stability
publisher Cambridge University Press
publishDate 2022
url https://doi.org/10.1017/jog.2022.13
https://doaj.org/article/8103795a2a1e41f4be27a0f857214103
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 68, Pp 946-960 (2022)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022000132/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.13
0022-1430
1727-5652
https://doaj.org/article/8103795a2a1e41f4be27a0f857214103
op_doi https://doi.org/10.1017/jog.2022.13
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 15
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