Timescales of outlet-glacier flow with negligible basal friction: Theory, observations and modeling ...
The timescales of the flow and retreat of Greenland's and Antarctica's outlet glaciers and their potential instabilities are arguably the largest uncertainty in future sea-level projections. Here we derive a scaling relation that allows the comparison of the timescales of observed complex...
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2023
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Online Access: | https://dx.doi.org/10.34657/11319 https://oa.tib.eu/renate/handle/123456789/12287 |
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ftdatacite:10.34657/11319 2023-07-23T04:15:53+02:00 Timescales of outlet-glacier flow with negligible basal friction: Theory, observations and modeling ... Feldmann, Johannes Levermann, Anders 2023 https://dx.doi.org/10.34657/11319 https://oa.tib.eu/renate/handle/123456789/12287 unknown Katlenburg-Lindau : Copernicus Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 flow field friction glacier flow ice flow observational method sea level change timescale Antarctica 910 CreativeWork article 2023 ftdatacite https://doi.org/10.34657/11319 2023-07-03T16:38:48Z The timescales of the flow and retreat of Greenland's and Antarctica's outlet glaciers and their potential instabilities are arguably the largest uncertainty in future sea-level projections. Here we derive a scaling relation that allows the comparison of the timescales of observed complex ice flow fields with geometric similarity. The scaling relation is derived under the assumption of fast, laterally confined, geometrically similar outlet-glacier flow over a slippery bed, i.e., with negligible basal friction. According to the relation, the time scaling of the outlet flow is determined by the product of the inverse of (1) the fourth power of the width-To-length ratio of its confinement, (2) the third power of the confinement depth and (3) the temperature-dependent ice softness. For the outflow at the grounding line of streams with negligible basal friction, this means that the volume flux is proportional to the ice softness and the bed depth, but goes with the fourth power of the gradient of the bed and with ... Article in Journal/Newspaper Antarc* Antarctica DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
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topic |
flow field friction glacier flow ice flow observational method sea level change timescale Antarctica 910 |
spellingShingle |
flow field friction glacier flow ice flow observational method sea level change timescale Antarctica 910 Feldmann, Johannes Levermann, Anders Timescales of outlet-glacier flow with negligible basal friction: Theory, observations and modeling ... |
topic_facet |
flow field friction glacier flow ice flow observational method sea level change timescale Antarctica 910 |
description |
The timescales of the flow and retreat of Greenland's and Antarctica's outlet glaciers and their potential instabilities are arguably the largest uncertainty in future sea-level projections. Here we derive a scaling relation that allows the comparison of the timescales of observed complex ice flow fields with geometric similarity. The scaling relation is derived under the assumption of fast, laterally confined, geometrically similar outlet-glacier flow over a slippery bed, i.e., with negligible basal friction. According to the relation, the time scaling of the outlet flow is determined by the product of the inverse of (1) the fourth power of the width-To-length ratio of its confinement, (2) the third power of the confinement depth and (3) the temperature-dependent ice softness. For the outflow at the grounding line of streams with negligible basal friction, this means that the volume flux is proportional to the ice softness and the bed depth, but goes with the fourth power of the gradient of the bed and with ... |
format |
Article in Journal/Newspaper |
author |
Feldmann, Johannes Levermann, Anders |
author_facet |
Feldmann, Johannes Levermann, Anders |
author_sort |
Feldmann, Johannes |
title |
Timescales of outlet-glacier flow with negligible basal friction: Theory, observations and modeling ... |
title_short |
Timescales of outlet-glacier flow with negligible basal friction: Theory, observations and modeling ... |
title_full |
Timescales of outlet-glacier flow with negligible basal friction: Theory, observations and modeling ... |
title_fullStr |
Timescales of outlet-glacier flow with negligible basal friction: Theory, observations and modeling ... |
title_full_unstemmed |
Timescales of outlet-glacier flow with negligible basal friction: Theory, observations and modeling ... |
title_sort |
timescales of outlet-glacier flow with negligible basal friction: theory, observations and modeling ... |
publisher |
Katlenburg-Lindau : Copernicus |
publishDate |
2023 |
url |
https://dx.doi.org/10.34657/11319 https://oa.tib.eu/renate/handle/123456789/12287 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_rights |
Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.34657/11319 |
_version_ |
1772177042175950848 |