Sensitivity of isochrones to surface mass balance and dynamics

The interior of an ice sheet consists of layers of accumulated snow, which contain important information on accumulation and ice dynamics that are imprinted on layer shapes over time. This work describes how changes in accumulation influence the stratigraphy of an ice sheet. The thickness of each la...

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Published in:Journal of Glaciology
Main Authors: Theofilopoulos, Alexios, Born, Andreas
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://hdl.handle.net/11250/3145228
https://doi.org/10.1017/jog.2022.62
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spelling ftunivbergen:oai:bora.uib.no:11250/3145228 2024-09-15T18:12:12+00:00 Sensitivity of isochrones to surface mass balance and dynamics Theofilopoulos, Alexios Born, Andreas 2023 application/pdf https://hdl.handle.net/11250/3145228 https://doi.org/10.1017/jog.2022.62 eng eng Cambridge University Press urn:issn:0022-1430 https://hdl.handle.net/11250/3145228 https://doi.org/10.1017/jog.2022.62 cristin:2139053 Journal of Glaciology. 2023, 69 (274), 311-323. Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no Copyright 2022 The Author(s) Journal of Glaciology 311-323 69 274 Journal article Peer reviewed 2023 ftunivbergen https://doi.org/10.1017/jog.2022.62 2024-08-13T23:41:38Z The interior of an ice sheet consists of layers of accumulated snow, which contain important information on accumulation and ice dynamics that are imprinted on layer shapes over time. This work describes how changes in accumulation influence the stratigraphy of an ice sheet. The thickness of each layer at present day depends both on accumulation and on the effect of dynamic thinning after its deposition. An isochronal numerical model is used to simulate the evolution of a 2-D, idealized ice sheet while explicitly representing the layers. A series of simulations was carried out to quantify the changes that anomalous accumulation at different locations and times has on the stratigraphy. These simulations form the basis of a linear response function. A second set of simulations with more sustained changes in accumulation is then used to describe large-scale and long-term impacts on the layering of the ice sheet as well as to test the quality of the linear approximation. The aim is to examine whether long-term effects can be extrapolated from small differential changes. The result confirms a certain degree of linearity between changes in accumulation and layer thickness that may be exploited for future inverse modeling applications. publishedVersion Article in Journal/Newspaper Ice Sheet Journal of Glaciology University of Bergen: Bergen Open Research Archive (BORA-UiB) Journal of Glaciology 69 274 311 323
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description The interior of an ice sheet consists of layers of accumulated snow, which contain important information on accumulation and ice dynamics that are imprinted on layer shapes over time. This work describes how changes in accumulation influence the stratigraphy of an ice sheet. The thickness of each layer at present day depends both on accumulation and on the effect of dynamic thinning after its deposition. An isochronal numerical model is used to simulate the evolution of a 2-D, idealized ice sheet while explicitly representing the layers. A series of simulations was carried out to quantify the changes that anomalous accumulation at different locations and times has on the stratigraphy. These simulations form the basis of a linear response function. A second set of simulations with more sustained changes in accumulation is then used to describe large-scale and long-term impacts on the layering of the ice sheet as well as to test the quality of the linear approximation. The aim is to examine whether long-term effects can be extrapolated from small differential changes. The result confirms a certain degree of linearity between changes in accumulation and layer thickness that may be exploited for future inverse modeling applications. publishedVersion
format Article in Journal/Newspaper
author Theofilopoulos, Alexios
Born, Andreas
spellingShingle Theofilopoulos, Alexios
Born, Andreas
Sensitivity of isochrones to surface mass balance and dynamics
author_facet Theofilopoulos, Alexios
Born, Andreas
author_sort Theofilopoulos, Alexios
title Sensitivity of isochrones to surface mass balance and dynamics
title_short Sensitivity of isochrones to surface mass balance and dynamics
title_full Sensitivity of isochrones to surface mass balance and dynamics
title_fullStr Sensitivity of isochrones to surface mass balance and dynamics
title_full_unstemmed Sensitivity of isochrones to surface mass balance and dynamics
title_sort sensitivity of isochrones to surface mass balance and dynamics
publisher Cambridge University Press
publishDate 2023
url https://hdl.handle.net/11250/3145228
https://doi.org/10.1017/jog.2022.62
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
311-323
69
274
op_relation urn:issn:0022-1430
https://hdl.handle.net/11250/3145228
https://doi.org/10.1017/jog.2022.62
cristin:2139053
Journal of Glaciology. 2023, 69 (274), 311-323.
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
Copyright 2022 The Author(s)
op_doi https://doi.org/10.1017/jog.2022.62
container_title Journal of Glaciology
container_volume 69
container_issue 274
container_start_page 311
op_container_end_page 323
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