Sensitivity of isochrones to surface mass balance and dynamics

Abstract 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 o...

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Published in:Journal of Glaciology
Main Authors: Theofilopoulos, Alexios, Born, Andreas
Other Authors: Trond Mohn Foundation
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2022
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2022.62
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000624
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spelling crcambridgeupr:10.1017/jog.2022.62 2024-03-03T08:45:23+00:00 Sensitivity of isochrones to surface mass balance and dynamics Theofilopoulos, Alexios Born, Andreas Trond Mohn Foundation 2022 http://dx.doi.org/10.1017/jog.2022.62 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000624 en eng Cambridge University Press (CUP) https://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 69, issue 274, page 311-323 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2022 crcambridgeupr https://doi.org/10.1017/jog.2022.62 2024-02-08T08:44:53Z Abstract 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. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 1 13
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Theofilopoulos, Alexios
Born, Andreas
Sensitivity of isochrones to surface mass balance and dynamics
topic_facet Earth-Surface Processes
description Abstract 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.
author2 Trond Mohn Foundation
format Article in Journal/Newspaper
author Theofilopoulos, Alexios
Born, Andreas
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 (CUP)
publishDate 2022
url http://dx.doi.org/10.1017/jog.2022.62
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000624
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 69, issue 274, page 311-323
ISSN 0022-1430 1727-5652
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2022.62
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 13
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