Ocean wave blocking by periodic surface rolls fortifies Arctic ice shelves

The Ward Hunt and Milne ice shelves are the present-day remnants of a much larger ice shelf that once fringed the coast of Ellesmere Island, Canada. These ice shelves possess a unique surface morphology consisting of wave-like rolls that run parallel to the shoreline. Setting aside the question of h...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Peter Nekrasov, Douglas R. MacAyeal
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press
Subjects:
Online Access:https://doi.org/10.1017/jog.2023.58
https://doaj.org/article/82bdc5b20e604c4eb468ad51605053ff
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spelling ftdoajarticles:oai:doaj.org/article:82bdc5b20e604c4eb468ad51605053ff 2023-09-05T13:16:57+02:00 Ocean wave blocking by periodic surface rolls fortifies Arctic ice shelves Peter Nekrasov Douglas R. MacAyeal https://doi.org/10.1017/jog.2023.58 https://doaj.org/article/82bdc5b20e604c4eb468ad51605053ff EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143023000588/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2023.58 0022-1430 1727-5652 https://doaj.org/article/82bdc5b20e604c4eb468ad51605053ff Journal of Glaciology, Pp 1-11 Arctic glaciology ice/ocean interactions ice shelves ice-shelf break-up seismology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article ftdoajarticles https://doi.org/10.1017/jog.2023.58 2023-08-20T00:35:49Z The Ward Hunt and Milne ice shelves are the present-day remnants of a much larger ice shelf that once fringed the coast of Ellesmere Island, Canada. These ice shelves possess a unique surface morphology consisting of wave-like rolls that run parallel to the shoreline. Setting aside the question of how these rolls originally developed, we consider the impact of this roll morphology on the stability of the ice shelf. In particular, we examine whether periodic variations in ice-shelf thickness and water depth implied by the rolls prevent the excitation of Lamb waves in the ice shelf. Using a hierarchy of numerical models, we find that there are band gaps in the flexural and extensional modes of the ice shelf, implying the existence of frequency ranges that lack wave motion. We show that an ice shelf with rolls is able to reflect waves in these frequency ranges that are incident upon its ice front, thereby mitigating undue stress and calving. We speculate that the roll morphology provides a “fitness” for survival that explains why rolls are observed in the oldest and thickest multiyear sea ice of the Arctic. Article in Journal/Newspaper Arctic Ellesmere Island Ice Shelf Ice Shelves Journal of Glaciology Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Canada Ellesmere Island Journal of Glaciology 1 11
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic glaciology
ice/ocean interactions
ice shelves
ice-shelf break-up
seismology
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Arctic glaciology
ice/ocean interactions
ice shelves
ice-shelf break-up
seismology
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Peter Nekrasov
Douglas R. MacAyeal
Ocean wave blocking by periodic surface rolls fortifies Arctic ice shelves
topic_facet Arctic glaciology
ice/ocean interactions
ice shelves
ice-shelf break-up
seismology
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description The Ward Hunt and Milne ice shelves are the present-day remnants of a much larger ice shelf that once fringed the coast of Ellesmere Island, Canada. These ice shelves possess a unique surface morphology consisting of wave-like rolls that run parallel to the shoreline. Setting aside the question of how these rolls originally developed, we consider the impact of this roll morphology on the stability of the ice shelf. In particular, we examine whether periodic variations in ice-shelf thickness and water depth implied by the rolls prevent the excitation of Lamb waves in the ice shelf. Using a hierarchy of numerical models, we find that there are band gaps in the flexural and extensional modes of the ice shelf, implying the existence of frequency ranges that lack wave motion. We show that an ice shelf with rolls is able to reflect waves in these frequency ranges that are incident upon its ice front, thereby mitigating undue stress and calving. We speculate that the roll morphology provides a “fitness” for survival that explains why rolls are observed in the oldest and thickest multiyear sea ice of the Arctic.
format Article in Journal/Newspaper
author Peter Nekrasov
Douglas R. MacAyeal
author_facet Peter Nekrasov
Douglas R. MacAyeal
author_sort Peter Nekrasov
title Ocean wave blocking by periodic surface rolls fortifies Arctic ice shelves
title_short Ocean wave blocking by periodic surface rolls fortifies Arctic ice shelves
title_full Ocean wave blocking by periodic surface rolls fortifies Arctic ice shelves
title_fullStr Ocean wave blocking by periodic surface rolls fortifies Arctic ice shelves
title_full_unstemmed Ocean wave blocking by periodic surface rolls fortifies Arctic ice shelves
title_sort ocean wave blocking by periodic surface rolls fortifies arctic ice shelves
publisher Cambridge University Press
url https://doi.org/10.1017/jog.2023.58
https://doaj.org/article/82bdc5b20e604c4eb468ad51605053ff
geographic Arctic
Canada
Ellesmere Island
geographic_facet Arctic
Canada
Ellesmere Island
genre Arctic
Ellesmere Island
Ice Shelf
Ice Shelves
Journal of Glaciology
Sea ice
genre_facet Arctic
Ellesmere Island
Ice Shelf
Ice Shelves
Journal of Glaciology
Sea ice
op_source Journal of Glaciology, Pp 1-11
op_relation https://www.cambridge.org/core/product/identifier/S0022143023000588/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2023.58
0022-1430
1727-5652
https://doaj.org/article/82bdc5b20e604c4eb468ad51605053ff
op_doi https://doi.org/10.1017/jog.2023.58
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 11
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