Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models

Abstract The fastest projected rates of sea level rise appear in models which include “the marine ice cliff instability (MICI),” a hypothesized but mostly unobserved process defined by rapid fracture and wastage of terminal ice cliffs that outpaces viscous relaxation and ice‐shelf formation. Crane G...

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Published in:Geophysical Research Letters
Main Authors: C. Needell, N. Holschuh
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2022GL102400
https://doaj.org/article/f1dae5b65d8640869dd3c9c918c0c227
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spelling ftdoajarticles:oai:doaj.org/article:f1dae5b65d8640869dd3c9c918c0c227 2024-09-15T18:02:59+00:00 Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models C. Needell N. Holschuh 2023-02-01T00:00:00Z https://doi.org/10.1029/2022GL102400 https://doaj.org/article/f1dae5b65d8640869dd3c9c918c0c227 EN eng Wiley https://doi.org/10.1029/2022GL102400 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL102400 https://doaj.org/article/f1dae5b65d8640869dd3c9c918c0c227 Geophysical Research Letters, Vol 50, Iss 4, Pp n/a-n/a (2023) ice sheets ice cliff MICI Crane Glacier altimetry Larsen B Ice Shelf Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2022GL102400 2024-08-05T17:49:23Z Abstract The fastest projected rates of sea level rise appear in models which include “the marine ice cliff instability (MICI),” a hypothesized but mostly unobserved process defined by rapid fracture and wastage of terminal ice cliffs that outpaces viscous relaxation and ice‐shelf formation. Crane Glacier's response to the Larsen B Ice Shelf collapse has been invoked as evidence of MICI in the observational record. Using available remote sensing data, we analyze Crane's retreat, arrest, and regrowth over the last two decades. Much of Crane's terminus retreat occurred in floating, not grounded ice. Retreat accelerated by at least 54% during the 2 years following ice shelf collapse. This is inconsistent with contemporaneous regional forcing that promoted ice shelf growth during this period, but consistent with a geometrically controlled positive feedback. We infer a maximum possible cliff height of 111 m, which according to process models, could enable cliff calving assuming damaged ice. Article in Journal/Newspaper Crane Glacier Ice Shelf Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 4
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic ice sheets
ice cliff
MICI
Crane Glacier
altimetry
Larsen B Ice Shelf
Geophysics. Cosmic physics
QC801-809
spellingShingle ice sheets
ice cliff
MICI
Crane Glacier
altimetry
Larsen B Ice Shelf
Geophysics. Cosmic physics
QC801-809
C. Needell
N. Holschuh
Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models
topic_facet ice sheets
ice cliff
MICI
Crane Glacier
altimetry
Larsen B Ice Shelf
Geophysics. Cosmic physics
QC801-809
description Abstract The fastest projected rates of sea level rise appear in models which include “the marine ice cliff instability (MICI),” a hypothesized but mostly unobserved process defined by rapid fracture and wastage of terminal ice cliffs that outpaces viscous relaxation and ice‐shelf formation. Crane Glacier's response to the Larsen B Ice Shelf collapse has been invoked as evidence of MICI in the observational record. Using available remote sensing data, we analyze Crane's retreat, arrest, and regrowth over the last two decades. Much of Crane's terminus retreat occurred in floating, not grounded ice. Retreat accelerated by at least 54% during the 2 years following ice shelf collapse. This is inconsistent with contemporaneous regional forcing that promoted ice shelf growth during this period, but consistent with a geometrically controlled positive feedback. We infer a maximum possible cliff height of 111 m, which according to process models, could enable cliff calving assuming damaged ice.
format Article in Journal/Newspaper
author C. Needell
N. Holschuh
author_facet C. Needell
N. Holschuh
author_sort C. Needell
title Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models
title_short Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models
title_full Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models
title_fullStr Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models
title_full_unstemmed Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models
title_sort evaluating the retreat, arrest, and regrowth of crane glacier against marine ice cliff process models
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2022GL102400
https://doaj.org/article/f1dae5b65d8640869dd3c9c918c0c227
genre Crane Glacier
Ice Shelf
genre_facet Crane Glacier
Ice Shelf
op_source Geophysical Research Letters, Vol 50, Iss 4, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2022GL102400
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2022GL102400
https://doaj.org/article/f1dae5b65d8640869dd3c9c918c0c227
op_doi https://doi.org/10.1029/2022GL102400
container_title Geophysical Research Letters
container_volume 50
container_issue 4
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