Modelled 3D calving at Kronebreen, Svalbard, driven by tidal fluctuations and frontal melt

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 remain uncertain and may vary from...

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Main Authors: Holmes, Felicity Alice, Dongen, Eef, Noormets, Riko, Pętlicki, Michał, Kirchner, Nina
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-2022-152
https://tc.copernicus.org/preprints/tc-2022-152/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd105329 2023-05-15T16:22:11+02:00 Modelled 3D calving at Kronebreen, Svalbard, driven by tidal fluctuations and frontal melt Holmes, Felicity Alice Dongen, Eef Noormets, Riko Pętlicki, Michał Kirchner, Nina 2022-08-31 application/pdf https://doi.org/10.5194/tc-2022-152 https://tc.copernicus.org/preprints/tc-2022-152/ eng eng doi:10.5194/tc-2022-152 https://tc.copernicus.org/preprints/tc-2022-152/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-2022-152 2022-09-05T16:22:54Z 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 remain 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 calving dynamics at Kronebreen, Svalbard, for the duration of one month. In addition, we impose frontal melt 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 c. 25 m are plausible. 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 Kronebreen ENVELOPE(13.333,13.333,78.833,78.833) Svalbard
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 remain 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 calving dynamics at Kronebreen, Svalbard, for the duration of one month. In addition, we impose frontal melt 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 c. 25 m are plausible. 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 Alice
Dongen, Eef
Noormets, Riko
Pętlicki, Michał
Kirchner, Nina
spellingShingle Holmes, Felicity Alice
Dongen, Eef
Noormets, Riko
Pętlicki, Michał
Kirchner, Nina
Modelled 3D calving at Kronebreen, Svalbard, driven by tidal fluctuations and frontal melt
author_facet Holmes, Felicity Alice
Dongen, Eef
Noormets, Riko
Pętlicki, Michał
Kirchner, Nina
author_sort Holmes, Felicity Alice
title Modelled 3D calving at Kronebreen, Svalbard, driven by tidal fluctuations and frontal melt
title_short Modelled 3D calving at Kronebreen, Svalbard, driven by tidal fluctuations and frontal melt
title_full Modelled 3D calving at Kronebreen, Svalbard, driven by tidal fluctuations and frontal melt
title_fullStr Modelled 3D calving at Kronebreen, Svalbard, driven by tidal fluctuations and frontal melt
title_full_unstemmed Modelled 3D calving at Kronebreen, Svalbard, driven by tidal fluctuations and frontal melt
title_sort modelled 3d calving at kronebreen, svalbard, driven by tidal fluctuations and frontal melt
publishDate 2022
url https://doi.org/10.5194/tc-2022-152
https://tc.copernicus.org/preprints/tc-2022-152/
long_lat ENVELOPE(13.333,13.333,78.833,78.833)
geographic Kronebreen
Svalbard
geographic_facet Kronebreen
Svalbard
genre glacier
Svalbard
genre_facet glacier
Svalbard
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2022-152
https://tc.copernicus.org/preprints/tc-2022-152/
op_doi https://doi.org/10.5194/tc-2022-152
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