The shape of change: an EOF approach to identifying sources of transient thickness change in an ice shelf
Ross Ice Shelf (RIS) is known to experience transient thickness change due to changes in the flow of its tributary ice streams and glaciers and this may complicate identification of external, climate-forced signals in contemporary observations of ice shelf thinning and thickening. Flux changes at th...
Published in: | Annals of Glaciology |
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Cambridge University Press
2017
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Online Access: | https://doi.org/10.1017/aog.2017.16 https://doaj.org/article/c0e9e2cf491042a1923b9bfe5f127b60 |
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ftdoajarticles:oai:doaj.org/article:c0e9e2cf491042a1923b9bfe5f127b60 2023-05-15T13:29:34+02:00 The shape of change: an EOF approach to identifying sources of transient thickness change in an ice shelf Adam J. Campbell Christina L. Hulbe Choon-Ki Lee 2017-04-01T00:00:00Z https://doi.org/10.1017/aog.2017.16 https://doaj.org/article/c0e9e2cf491042a1923b9bfe5f127b60 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305517000167/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2017.16 0260-3055 1727-5644 https://doaj.org/article/c0e9e2cf491042a1923b9bfe5f127b60 Annals of Glaciology, Vol 58, Pp 21-27 (2017) glaciological model experiments ice shelves laser altimetry Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/aog.2017.16 2023-03-12T01:31:57Z Ross Ice Shelf (RIS) is known to experience transient thickness change due to changes in the flow of its tributary ice streams and glaciers and this may complicate identification of external, climate-forced signals in contemporary observations of ice shelf thinning and thickening. Flux changes at the lateral boundaries produce both instantaneous and longer timescale adjustments in the coupled velocity and thickness fields. Here, we adapt a statistical approach to output from a numerical model of ice shelf flow to identify characteristic patterns (spatial response surfaces) associated with stepped and cyclic perturbations to boundary fluxes. Once known, characteristic patterns identified in observational data may be attributed to specific sources. An example involving discharge of Byrd Glacier into RIS is described. We find that spatial response surfaces for thickness and velocity generated in individual flow model experiments appear to be independent of flux perturbation shape and magnitude. Additionally, recent acceleration of Byrd Glacier is apparent in ICESat-detected change in RIS thickness. Article in Journal/Newspaper Annals of Glaciology Byrd Glacier Ice Shelf Ice Shelves Ross Ice Shelf Directory of Open Access Journals: DOAJ Articles Ross Ice Shelf Byrd Byrd Glacier ENVELOPE(160.333,160.333,-80.250,-80.250) Annals of Glaciology 58 74 21 27 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
glaciological model experiments ice shelves laser altimetry Meteorology. Climatology QC851-999 |
spellingShingle |
glaciological model experiments ice shelves laser altimetry Meteorology. Climatology QC851-999 Adam J. Campbell Christina L. Hulbe Choon-Ki Lee The shape of change: an EOF approach to identifying sources of transient thickness change in an ice shelf |
topic_facet |
glaciological model experiments ice shelves laser altimetry Meteorology. Climatology QC851-999 |
description |
Ross Ice Shelf (RIS) is known to experience transient thickness change due to changes in the flow of its tributary ice streams and glaciers and this may complicate identification of external, climate-forced signals in contemporary observations of ice shelf thinning and thickening. Flux changes at the lateral boundaries produce both instantaneous and longer timescale adjustments in the coupled velocity and thickness fields. Here, we adapt a statistical approach to output from a numerical model of ice shelf flow to identify characteristic patterns (spatial response surfaces) associated with stepped and cyclic perturbations to boundary fluxes. Once known, characteristic patterns identified in observational data may be attributed to specific sources. An example involving discharge of Byrd Glacier into RIS is described. We find that spatial response surfaces for thickness and velocity generated in individual flow model experiments appear to be independent of flux perturbation shape and magnitude. Additionally, recent acceleration of Byrd Glacier is apparent in ICESat-detected change in RIS thickness. |
format |
Article in Journal/Newspaper |
author |
Adam J. Campbell Christina L. Hulbe Choon-Ki Lee |
author_facet |
Adam J. Campbell Christina L. Hulbe Choon-Ki Lee |
author_sort |
Adam J. Campbell |
title |
The shape of change: an EOF approach to identifying sources of transient thickness change in an ice shelf |
title_short |
The shape of change: an EOF approach to identifying sources of transient thickness change in an ice shelf |
title_full |
The shape of change: an EOF approach to identifying sources of transient thickness change in an ice shelf |
title_fullStr |
The shape of change: an EOF approach to identifying sources of transient thickness change in an ice shelf |
title_full_unstemmed |
The shape of change: an EOF approach to identifying sources of transient thickness change in an ice shelf |
title_sort |
shape of change: an eof approach to identifying sources of transient thickness change in an ice shelf |
publisher |
Cambridge University Press |
publishDate |
2017 |
url |
https://doi.org/10.1017/aog.2017.16 https://doaj.org/article/c0e9e2cf491042a1923b9bfe5f127b60 |
long_lat |
ENVELOPE(160.333,160.333,-80.250,-80.250) |
geographic |
Ross Ice Shelf Byrd Byrd Glacier |
geographic_facet |
Ross Ice Shelf Byrd Byrd Glacier |
genre |
Annals of Glaciology Byrd Glacier Ice Shelf Ice Shelves Ross Ice Shelf |
genre_facet |
Annals of Glaciology Byrd Glacier Ice Shelf Ice Shelves Ross Ice Shelf |
op_source |
Annals of Glaciology, Vol 58, Pp 21-27 (2017) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0260305517000167/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2017.16 0260-3055 1727-5644 https://doaj.org/article/c0e9e2cf491042a1923b9bfe5f127b60 |
op_doi |
https://doi.org/10.1017/aog.2017.16 |
container_title |
Annals of Glaciology |
container_volume |
58 |
container_issue |
74 |
container_start_page |
21 |
op_container_end_page |
27 |
_version_ |
1766001258944004096 |