Interaction of marine ice-sheet instabilities in two drainage basins: Simple scaling of geometry and transition time
The initiation of a marine ice-sheet instability (MISI) is generally discussed from the ocean side of the ice sheet. It has been shown that the reduction in ice-shelf buttressing and softening of the coastal ice can destabilize a marine ice sheet if the bedrock is sloping upward towards the ocean. U...
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ftleibnizopen:oai:oai.leibnizopen.de:edJDfYoBNQPDO7WIsWtp 2023-10-09T21:52:22+02:00 Interaction of marine ice-sheet instabilities in two drainage basins: Simple scaling of geometry and transition time Feldmann, J. Levermann, A. 2015 application/pdf https://doi.org/10.34657/1037 https://oa.tib.eu/renate/handle/123456789/684 eng eng München : European Geopyhsical Union CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ The Cryosphere, Volume 9, Issue 2, Page 631-645 bedrock conceptual framework drainage basin elevation ice sheet ice shelf three-dimensional flow topography transition zone 550 article Text 2015 ftleibnizopen https://doi.org/10.34657/1037 2023-09-10T23:34:28Z The initiation of a marine ice-sheet instability (MISI) is generally discussed from the ocean side of the ice sheet. It has been shown that the reduction in ice-shelf buttressing and softening of the coastal ice can destabilize a marine ice sheet if the bedrock is sloping upward towards the ocean. Using a conceptional flow-line geometry, we investigate the possibility of whether a MISI can be triggered from the direction of the ice divide as opposed to coastal forcing and explore the interaction between connected basins. We find that the initiation of a MISI in one basin can induce a destabilization in the other. The underlying mechanism of basin interaction is based on dynamic thinning and a consecutive motion of the ice divide which induces a thinning in the adjacent basin and a successive initiation of the instability. Our simplified and symmetric topographic setup allows scaling both the geometry and the transition time between both instabilities. We find that the ice profile follows a universal shape that is scaled with the horizontal extent of the ice sheet and that the same exponent of 1/2 applies for the scaling relation between central surface elevation and horizontal extent as in the pure shallow ice approximation (Vialov profile). Altering the central bed elevation, we find that the extent of grounding-line retreat in one basin determines the degree of interaction with the other. Different scenarios of basin interaction are discussed based on our modeling results as well as on a conceptual flux-balance analysis. We conclude that for the three-dimensional case, the possibility of drainage basin interaction on timescales on the order of 1 kyr or larger cannot be excluded and hence needs further investigation. publishedVersion Article in Journal/Newspaper Ice Sheet Ice Shelf The Cryosphere LeibnizOpen (The Leibniz Association) Misi ENVELOPE(26.683,26.683,66.617,66.617) |
institution |
Open Polar |
collection |
LeibnizOpen (The Leibniz Association) |
op_collection_id |
ftleibnizopen |
language |
English |
topic |
bedrock conceptual framework drainage basin elevation ice sheet ice shelf three-dimensional flow topography transition zone 550 |
spellingShingle |
bedrock conceptual framework drainage basin elevation ice sheet ice shelf three-dimensional flow topography transition zone 550 Feldmann, J. Levermann, A. Interaction of marine ice-sheet instabilities in two drainage basins: Simple scaling of geometry and transition time |
topic_facet |
bedrock conceptual framework drainage basin elevation ice sheet ice shelf three-dimensional flow topography transition zone 550 |
description |
The initiation of a marine ice-sheet instability (MISI) is generally discussed from the ocean side of the ice sheet. It has been shown that the reduction in ice-shelf buttressing and softening of the coastal ice can destabilize a marine ice sheet if the bedrock is sloping upward towards the ocean. Using a conceptional flow-line geometry, we investigate the possibility of whether a MISI can be triggered from the direction of the ice divide as opposed to coastal forcing and explore the interaction between connected basins. We find that the initiation of a MISI in one basin can induce a destabilization in the other. The underlying mechanism of basin interaction is based on dynamic thinning and a consecutive motion of the ice divide which induces a thinning in the adjacent basin and a successive initiation of the instability. Our simplified and symmetric topographic setup allows scaling both the geometry and the transition time between both instabilities. We find that the ice profile follows a universal shape that is scaled with the horizontal extent of the ice sheet and that the same exponent of 1/2 applies for the scaling relation between central surface elevation and horizontal extent as in the pure shallow ice approximation (Vialov profile). Altering the central bed elevation, we find that the extent of grounding-line retreat in one basin determines the degree of interaction with the other. Different scenarios of basin interaction are discussed based on our modeling results as well as on a conceptual flux-balance analysis. We conclude that for the three-dimensional case, the possibility of drainage basin interaction on timescales on the order of 1 kyr or larger cannot be excluded and hence needs further investigation. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Feldmann, J. Levermann, A. |
author_facet |
Feldmann, J. Levermann, A. |
author_sort |
Feldmann, J. |
title |
Interaction of marine ice-sheet instabilities in two drainage basins: Simple scaling of geometry and transition time |
title_short |
Interaction of marine ice-sheet instabilities in two drainage basins: Simple scaling of geometry and transition time |
title_full |
Interaction of marine ice-sheet instabilities in two drainage basins: Simple scaling of geometry and transition time |
title_fullStr |
Interaction of marine ice-sheet instabilities in two drainage basins: Simple scaling of geometry and transition time |
title_full_unstemmed |
Interaction of marine ice-sheet instabilities in two drainage basins: Simple scaling of geometry and transition time |
title_sort |
interaction of marine ice-sheet instabilities in two drainage basins: simple scaling of geometry and transition time |
publisher |
München : European Geopyhsical Union |
publishDate |
2015 |
url |
https://doi.org/10.34657/1037 https://oa.tib.eu/renate/handle/123456789/684 |
long_lat |
ENVELOPE(26.683,26.683,66.617,66.617) |
geographic |
Misi |
geographic_facet |
Misi |
genre |
Ice Sheet Ice Shelf The Cryosphere |
genre_facet |
Ice Sheet Ice Shelf The Cryosphere |
op_source |
The Cryosphere, Volume 9, Issue 2, Page 631-645 |
op_rights |
CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ |
op_doi |
https://doi.org/10.34657/1037 |
_version_ |
1779315535543009280 |