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...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Alexios Theofilopoulos, Andreas Born
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.62
https://doaj.org/article/c26b8005334f494cab2c09878d86f4f4
id ftdoajarticles:oai:doaj.org/article:c26b8005334f494cab2c09878d86f4f4
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:c26b8005334f494cab2c09878d86f4f4 2023-05-15T16:39:52+02:00 Sensitivity of isochrones to surface mass balance and dynamics Alexios Theofilopoulos Andreas Born 2023-04-01T00:00:00Z https://doi.org/10.1017/jog.2022.62 https://doaj.org/article/c26b8005334f494cab2c09878d86f4f4 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000624/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.62 0022-1430 1727-5652 https://doaj.org/article/c26b8005334f494cab2c09878d86f4f4 Journal of Glaciology, Vol 69, Pp 311-323 (2023) Accumulation ice dynamics ice-sheet modeling paleoclimate Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.62 2023-03-19T01:31:51Z 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 Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 69 274 311 323
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Accumulation
ice dynamics
ice-sheet modeling
paleoclimate
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Accumulation
ice dynamics
ice-sheet modeling
paleoclimate
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Alexios Theofilopoulos
Andreas Born
Sensitivity of isochrones to surface mass balance and dynamics
topic_facet Accumulation
ice dynamics
ice-sheet modeling
paleoclimate
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
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.
format Article in Journal/Newspaper
author Alexios Theofilopoulos
Andreas Born
author_facet Alexios Theofilopoulos
Andreas Born
author_sort Alexios Theofilopoulos
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://doi.org/10.1017/jog.2022.62
https://doaj.org/article/c26b8005334f494cab2c09878d86f4f4
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 311-323 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022000624/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.62
0022-1430
1727-5652
https://doaj.org/article/c26b8005334f494cab2c09878d86f4f4
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
_version_ 1766030210813132800