Impact of tides on calving patterns at Kronebreen, Svalbard – insights from three-dimensional ice dynamical modelling

Understanding calving processes and their controls is of importance for reducing uncertainty in sea level rise estimates. The impact of tidal fluctuations and frontal melt on calving patterns has been researched through both modelling and observational studies but remains uncertain and may vary from...

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Published in:The Cryosphere
Main Authors: Holmes, Felicity A., Dongen, Eef, Noormets, Riko, Pętlicki, Michał, Kirchner, Nina
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-1853-2023
https://tc.copernicus.org/articles/17/1853/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc105329 2023-06-11T04:11:58+02:00 Impact of tides on calving patterns at Kronebreen, Svalbard – insights from three-dimensional ice dynamical modelling Holmes, Felicity A. Dongen, Eef Noormets, Riko Pętlicki, Michał Kirchner, Nina 2023-05-05 application/pdf https://doi.org/10.5194/tc-17-1853-2023 https://tc.copernicus.org/articles/17/1853/2023/ eng eng doi:10.5194/tc-17-1853-2023 https://tc.copernicus.org/articles/17/1853/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-1853-2023 2023-05-08T16:23:11Z Understanding calving processes and their controls is of importance for reducing uncertainty in sea level rise estimates. The impact of tidal fluctuations and frontal melt on calving patterns has been researched through both modelling and observational studies but remains uncertain and may vary from glacier to glacier. In this study, we isolate various different impacts of tidal fluctuations on a glacier terminus to understand their influence on the timing of calving events in a model of Kronebreen, Svalbard, for the duration of 1 month. In addition, we impose a simplified frontal melt parameterisation onto the calving front in order to allow for an undercut to develop over the course of the simulations. We find that calving events show a tidal signal when there is a small or no undercut, but, after a critical point, undercut-driven calving becomes dominant and drowns out the tidal signal. However, the relationship is complex, and large calving events show a tidal signal even with a large modelled undercut. The modelled undercut sizes are then compared to observational profiles, showing that undercuts of up to ca. 25 m are plausible but with a more complex geometry being evident in observations than that captured in the model. These findings highlight the complex interactions occurring at the calving front of Kronebreen and suggest further observational data and modelling work is needed to fully understand the hierarchy of controls on calving. Text glacier Svalbard Copernicus Publications: E-Journals Svalbard Kronebreen ENVELOPE(13.333,13.333,78.833,78.833) The Cryosphere 17 5 1853 1872
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Understanding calving processes and their controls is of importance for reducing uncertainty in sea level rise estimates. The impact of tidal fluctuations and frontal melt on calving patterns has been researched through both modelling and observational studies but remains uncertain and may vary from glacier to glacier. In this study, we isolate various different impacts of tidal fluctuations on a glacier terminus to understand their influence on the timing of calving events in a model of Kronebreen, Svalbard, for the duration of 1 month. In addition, we impose a simplified frontal melt parameterisation onto the calving front in order to allow for an undercut to develop over the course of the simulations. We find that calving events show a tidal signal when there is a small or no undercut, but, after a critical point, undercut-driven calving becomes dominant and drowns out the tidal signal. However, the relationship is complex, and large calving events show a tidal signal even with a large modelled undercut. The modelled undercut sizes are then compared to observational profiles, showing that undercuts of up to ca. 25 m are plausible but with a more complex geometry being evident in observations than that captured in the model. These findings highlight the complex interactions occurring at the calving front of Kronebreen and suggest further observational data and modelling work is needed to fully understand the hierarchy of controls on calving.
format Text
author Holmes, Felicity A.
Dongen, Eef
Noormets, Riko
Pętlicki, Michał
Kirchner, Nina
spellingShingle Holmes, Felicity A.
Dongen, Eef
Noormets, Riko
Pętlicki, Michał
Kirchner, Nina
Impact of tides on calving patterns at Kronebreen, Svalbard – insights from three-dimensional ice dynamical modelling
author_facet Holmes, Felicity A.
Dongen, Eef
Noormets, Riko
Pętlicki, Michał
Kirchner, Nina
author_sort Holmes, Felicity A.
title Impact of tides on calving patterns at Kronebreen, Svalbard – insights from three-dimensional ice dynamical modelling
title_short Impact of tides on calving patterns at Kronebreen, Svalbard – insights from three-dimensional ice dynamical modelling
title_full Impact of tides on calving patterns at Kronebreen, Svalbard – insights from three-dimensional ice dynamical modelling
title_fullStr Impact of tides on calving patterns at Kronebreen, Svalbard – insights from three-dimensional ice dynamical modelling
title_full_unstemmed Impact of tides on calving patterns at Kronebreen, Svalbard – insights from three-dimensional ice dynamical modelling
title_sort impact of tides on calving patterns at kronebreen, svalbard – insights from three-dimensional ice dynamical modelling
publishDate 2023
url https://doi.org/10.5194/tc-17-1853-2023
https://tc.copernicus.org/articles/17/1853/2023/
long_lat ENVELOPE(13.333,13.333,78.833,78.833)
geographic Svalbard
Kronebreen
geographic_facet Svalbard
Kronebreen
genre glacier
Svalbard
genre_facet glacier
Svalbard
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-1853-2023
https://tc.copernicus.org/articles/17/1853/2023/
op_doi https://doi.org/10.5194/tc-17-1853-2023
container_title The Cryosphere
container_volume 17
container_issue 5
container_start_page 1853
op_container_end_page 1872
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