Diagnosing ice sheet grounding line stability from landform morphology
The resilience of a marine-based ice sheet is strongly governed by the stability of its grounding lines, which are in turn sensitive to ocean-induced melting, calving, and flotation of the ice margin. Since the grounding line is also a sedimentary environment, the constructional landforms that are b...
Published in: | The Cryosphere |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2018
|
Subjects: | |
Online Access: | https://doi.org/10.5194/tc-12-2707-2018 https://www.the-cryosphere.net/12/2707/2018/tc-12-2707-2018.pdf https://doaj.org/article/df6a11c5ffa043c2a572b75339aabeea |
id |
fttriple:oai:gotriple.eu:oai:doaj.org/article:df6a11c5ffa043c2a572b75339aabeea |
---|---|
record_format |
openpolar |
spelling |
fttriple:oai:gotriple.eu:oai:doaj.org/article:df6a11c5ffa043c2a572b75339aabeea 2023-05-15T16:40:42+02:00 Diagnosing ice sheet grounding line stability from landform morphology L. M. Simkins S. L. Greenwood J. B. Anderson 2018-08-01 https://doi.org/10.5194/tc-12-2707-2018 https://www.the-cryosphere.net/12/2707/2018/tc-12-2707-2018.pdf https://doaj.org/article/df6a11c5ffa043c2a572b75339aabeea en eng Copernicus Publications doi:10.5194/tc-12-2707-2018 1994-0416 1994-0424 https://www.the-cryosphere.net/12/2707/2018/tc-12-2707-2018.pdf https://doaj.org/article/df6a11c5ffa043c2a572b75339aabeea undefined The Cryosphere, Vol 12, Pp 2707-2726 (2018) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/10.5194/tc-12-2707-2018 2023-01-22T18:48:45Z The resilience of a marine-based ice sheet is strongly governed by the stability of its grounding lines, which are in turn sensitive to ocean-induced melting, calving, and flotation of the ice margin. Since the grounding line is also a sedimentary environment, the constructional landforms that are built here may reflect elements of the processes governing this dynamic and potentially vulnerable environment. Here we analyse a large dataset (n = 6275) of grounding line landforms mapped on the western Ross Sea continental shelf from high-resolution geophysical data. The population is divided into two distinct morphotypes by their morphological properties: recessional moraines (consistently narrow, closely spaced, low amplitude, symmetric, and straight) and grounding zone wedges (broad, widely spaced, higher amplitude, asymmetric, sinuous, and highly variable). Landform morphotypes cluster with alike forms that transition abruptly between morphotypes both spatially and within a retreat sequence. Their form and distribution are largely independent of water depth, bed slope, and position relative to glacial troughs. Similarly, we find no conclusive evidence for morphology being determined by the presence or absence of an ice shelf. Instead, grounding zone wedge construction is favoured by a higher sediment flux and a longer-held grounding position. We propose two endmember modes of grounding line retreat: (1) an irregular mode, characterised by grounding zone wedges with longer standstills and accompanied by larger-magnitude retreat events, and (2) a steady mode, characterised by moraine sequences that instead represent more frequent but smaller-magnitude retreat events. We suggest that while sediment accumulation and progradation may prolong the stability of a grounding line position, progressive development of sinuosity in the grounding line due to spatially variable sediment delivery likely destabilises the grounding position by enhanced ablation, triggering large-magnitude retreat events. Here, the concept of ... Article in Journal/Newspaper Ice Sheet Ice Shelf Ross Sea The Cryosphere Unknown Ross Sea The Cryosphere 12 8 2707 2726 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
envir geo |
spellingShingle |
envir geo L. M. Simkins S. L. Greenwood J. B. Anderson Diagnosing ice sheet grounding line stability from landform morphology |
topic_facet |
envir geo |
description |
The resilience of a marine-based ice sheet is strongly governed by the stability of its grounding lines, which are in turn sensitive to ocean-induced melting, calving, and flotation of the ice margin. Since the grounding line is also a sedimentary environment, the constructional landforms that are built here may reflect elements of the processes governing this dynamic and potentially vulnerable environment. Here we analyse a large dataset (n = 6275) of grounding line landforms mapped on the western Ross Sea continental shelf from high-resolution geophysical data. The population is divided into two distinct morphotypes by their morphological properties: recessional moraines (consistently narrow, closely spaced, low amplitude, symmetric, and straight) and grounding zone wedges (broad, widely spaced, higher amplitude, asymmetric, sinuous, and highly variable). Landform morphotypes cluster with alike forms that transition abruptly between morphotypes both spatially and within a retreat sequence. Their form and distribution are largely independent of water depth, bed slope, and position relative to glacial troughs. Similarly, we find no conclusive evidence for morphology being determined by the presence or absence of an ice shelf. Instead, grounding zone wedge construction is favoured by a higher sediment flux and a longer-held grounding position. We propose two endmember modes of grounding line retreat: (1) an irregular mode, characterised by grounding zone wedges with longer standstills and accompanied by larger-magnitude retreat events, and (2) a steady mode, characterised by moraine sequences that instead represent more frequent but smaller-magnitude retreat events. We suggest that while sediment accumulation and progradation may prolong the stability of a grounding line position, progressive development of sinuosity in the grounding line due to spatially variable sediment delivery likely destabilises the grounding position by enhanced ablation, triggering large-magnitude retreat events. Here, the concept of ... |
format |
Article in Journal/Newspaper |
author |
L. M. Simkins S. L. Greenwood J. B. Anderson |
author_facet |
L. M. Simkins S. L. Greenwood J. B. Anderson |
author_sort |
L. M. Simkins |
title |
Diagnosing ice sheet grounding line stability from landform morphology |
title_short |
Diagnosing ice sheet grounding line stability from landform morphology |
title_full |
Diagnosing ice sheet grounding line stability from landform morphology |
title_fullStr |
Diagnosing ice sheet grounding line stability from landform morphology |
title_full_unstemmed |
Diagnosing ice sheet grounding line stability from landform morphology |
title_sort |
diagnosing ice sheet grounding line stability from landform morphology |
publisher |
Copernicus Publications |
publishDate |
2018 |
url |
https://doi.org/10.5194/tc-12-2707-2018 https://www.the-cryosphere.net/12/2707/2018/tc-12-2707-2018.pdf https://doaj.org/article/df6a11c5ffa043c2a572b75339aabeea |
geographic |
Ross Sea |
geographic_facet |
Ross Sea |
genre |
Ice Sheet Ice Shelf Ross Sea The Cryosphere |
genre_facet |
Ice Sheet Ice Shelf Ross Sea The Cryosphere |
op_source |
The Cryosphere, Vol 12, Pp 2707-2726 (2018) |
op_relation |
doi:10.5194/tc-12-2707-2018 1994-0416 1994-0424 https://www.the-cryosphere.net/12/2707/2018/tc-12-2707-2018.pdf https://doaj.org/article/df6a11c5ffa043c2a572b75339aabeea |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-12-2707-2018 |
container_title |
The Cryosphere |
container_volume |
12 |
container_issue |
8 |
container_start_page |
2707 |
op_container_end_page |
2726 |
_version_ |
1766031106029649920 |